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class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/90904262/To_the_southern_margin_of_the_last_northern_glaciation_a_field_trip_through_the_young_moraine_area_south_east_of_Berlin"><img alt="Research paper thumbnail of To the southern margin of the (last) northern glaciation – a field trip through the young moraine area south-east of Berlin" class="work-thumbnail" src="https://attachments.academia-assets.com/94338120/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/90904262/To_the_southern_margin_of_the_last_northern_glaciation_a_field_trip_through_the_young_moraine_area_south_east_of_Berlin">To the southern margin of the (last) northern glaciation – a field trip through the young moraine area south-east of Berlin</a></div><div class="wp-workCard_item"><span>DEUQUA Special Publications</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The young moraine area to the southeast of Berlin was repeatedly overrun and covered by Scandinav...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">The young moraine area to the southeast of Berlin was repeatedly overrun and covered by Scandinavian ice sheets (SISs). The last glaciation took place during the Last Glacial Maximum (LGM), when the last/most recent SIS reached its furthest southern extent. An incompletely formed chain of terminal moraines marks the Brandenburg ice stage. The most recent glacier had its greatest environmental impact due to the large quantities of released meltwaters. Many subglacial channels, massive proglacial sands and huge meltwater streamways (Urstromtäler) were formed at that time. During the Holocene, the landscape was finally shaped mainly by the rivers Dahme and Spree.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="b5bac7cdd6732dcf6849640c0efa4d39" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":94338120,"asset_id":90904262,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/94338120/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="90904262"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item 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class="wp-workCard_item"><span class="js-work-more-abstract-truncated">4.3.3.6 Die Entwicklung der glazifluvialen Abflussverhältnisse um Lübben-Das Trockenfallen des Ba...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">4.3.3.6 Die Entwicklung der glazifluvialen Abflussverhältnisse um Lübben-Das Trockenfallen des Baruther Abschnittes 4.3.4 Die Entwicklung der Schmelzwasserabflussbahnen zwischen dem Baruther und dem Berliner Urstromtal 4.3.4.1 Einführung 4.3.4.2 Die Abflussphase in Richtung Beelitz 4.3.4.3 Die Abflussphase in Richtung Potsdam 4.3.4.4 Der Abfluss vom Unterspreewald in Richtung Berlin 4.3.4.5 Gemeinsamkeiten der Abflussbahnen zwischen dem Baruther und dem Berliner Urstromtal 4.3.5 Der Kontakt Baruther Urstromtal-Fläming bei Klein Ziescht VII 4.3.6 Zusammenfassung der Forschungsergebnisse zur Entwicklung der Urstromtalungen im Jungmoränenland südlich Berlins 4.4 Die Oberflächenformen der Platten im Jungmoränenland südlich Berlins 4.4.1 Einführung 4.4.2 Die Platten im Bereich der Brandenburger Eisrandlage 4.4.2.1 Das Neuendorfer Becken 4.4.2.2 Das Eisstaubecken von Zesch am See 4.4.3 Die Oberflächenformen der Platten nördlich der Brandenburger Eisrandlage 4.5 Der geologische Bau der Platten im Jungmoränenland südlich Berlins 4.5.1 Aufschlüsse in saalezeitlichen Sedimenten 4.5.2 Aufschlussprofile mit geringmächtigen weichselzeitlichen Sedimenten 4.5.3 Aufschlussprofile mit mächtigeren weichselzeitlichen Sedimenten 4.5.4 Gemeinsamkeiten im geologischen Bau der Platten 4.5.5 Auswertung der Geschiebeanalysen 4.5.5.1 Einführung 4.5.5.2 Die Geschiebespektren des unteren Geschiebemergels 4.5.5.3 Auswertung der Proben aus dem oberen Till 4.5.6 Zusammenfassung der Untersuchungsergebnisse zur Entstehung der Platten im Jungmoränenland südlich Berlins 4.6 Glaziale Rinnen im Jungmoränenland südlich Berlins 4.6.1 Zur Genese der Glazialen Rinnen im Arbeitsgebiet 4.6.1.1 Breitrinnen 4.6.1.2 Schmalrinnen 4.6.2 Zusammenfassung 4.7 Untersuchungen zur spätglazial-frühholozänen Entwicklung des Gewässernetzes im Jungmoränenland südlich Berlins 4.7.1 Einleitung 4.7.2 Der Töpchiner See 4.7.2.1 Beschreibung des Seebeckens 4.7.2.2 Das Pollendiagramm der Bohrung TÖP K1 4.7.3 Zur spätglazial-frühholozänen Entwicklung der Spree im Unterspreewald 4.7.3.1 Einleitung 4.7.3.2 Die braided river-Strukturen der Landgraben-Urspree 4.7.3.3 Die Pretschener Urspree 4.7.3.4 Der Großmäander am Köthener See 4.7.3.5 Die Lubolz-Krausnicker Urspree 4.7.3.6 Zur Ursache der Spreeablenkung 4.7.4 Zusammenfassung der Untersuchungsergebnisse zur spätglazialfrühholozänen Entwicklung des Gewässernetzes 5 Zusammenfassung und Ausblick 5.1 Chronologische Zusammenfassung der Untersuchungsergebnisse zur jungquartären Entwicklung des Untersuchungsgebietes 5.1.1 Zur präweichselzeitlichen Entwicklung des Arbeitsgebietes 5.1.2 Zur Entwicklung während des weichselzeitlichen Eisvorstoßes VIII 5.1.3 Die Entwicklung während des Weichselmaximalvorstoßes-Der Älteste Baruther Urstrom 5.1.4 Die Brandenburger Eisrandlage-Der Ältere Baruther Urstrom 5.1.5 Die Aufgabe der Brandenburger Eisrandlage-Der Jüngere Baruther Urstrom 5.1.6 Der Jüngste Baruther Urstrom 5.1.7 Die Abflussphasen zwischen dem Baruther und dem Berliner Urstromtal</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="3e7d39b23efbd92e2dc19bd0511a0981" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":94338171,"asset_id":90904259,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/94338171/download_file?s=profile"><span><i class="fa 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The owner o...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">El'gygytgyn"-Chukchi word for "White Lake" storage and various scientific activities. The owner of the cabin (Yuri Gopkalo) was hired as a care-keeper and cook. He arrived on June 12, via a helicopter trip of the Pevek Gold Mining Company, and remained with the expedition until finished. I@ spring 1998</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="01a910157e4370431ddc949ddc5d304f" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":94338053,"asset_id":90904196,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/94338053/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="90904196"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="90904196"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 90904196; 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="90904130"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/90904130/Klassifikation_und_Aufbau_ausgew%C3%A4hlter_Vorkommen_glazilimnischer_Sedimente_n%C3%B6rdlich_der_Pommerschen_Eisrandlage_im_brandenburgischen_Abschnitt_der_Erdgasfernleitung_OPAL"><img alt="Research paper thumbnail of Klassifikation und Aufbau ausgewählter Vorkommen glazilimnischer Sedimente nördlich der Pommerschen Eisrandlage im brandenburgischen Abschnitt der Erdgasfernleitung OPAL" class="work-thumbnail" src="https://attachments.academia-assets.com/94337981/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/90904130/Klassifikation_und_Aufbau_ausgew%C3%A4hlter_Vorkommen_glazilimnischer_Sedimente_n%C3%B6rdlich_der_Pommerschen_Eisrandlage_im_brandenburgischen_Abschnitt_der_Erdgasfernleitung_OPAL">Klassifikation und Aufbau ausgewählter Vorkommen glazilimnischer Sedimente nördlich der Pommerschen Eisrandlage im brandenburgischen Abschnitt der Erdgasfernleitung OPAL</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">1. Einführung Die Ostsee-Pipeline-Anbindungsleitung (OPAL) verläuft über 470 km von Lubmin bei Gr...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">1. Einführung Die Ostsee-Pipeline-Anbindungsleitung (OPAL) verläuft über 470 km von Lubmin bei Greifswald bis nach Olbernhau an der deutsch-tschechischen Grenze (vgl. Höhlschen 2011). 270 km der Leitung durchziehen von Nord nach Süd das östliche Brandenburg (Abb. 1). Die Pipeline mit einem Durchmesser von 1,40 m wurde im brandenburger Abschnitt zwischen April 2010 und April 2011 verlegt. Im Zuge des Leitungsbaus wurde ein nahezu kontinuierlicher Aufschluss von 2,5 bis 3,5 m Tiefe geschaffen, der einmalige Einblicke in die oberflächennah anstehenden Ablagerungen bot. Ein erster, zusammenfassender Überblick der Ergebnisse wurde für Brandenburg von Juschus et al. 2011 gegeben, für den nördlich angrenzenden Abschnitt Vorpommerns von Börner et al. 2011. Der folgende Artikel konzentriert sich auf die glazilimnischen Ablagerungen zwischen der nördlichen Landesgrenze Brandenburgs und der Pommerschen Eisrandlage bei Oderberg. 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="90904129"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/90904129/Morphotectonics_of_the_European_Lowland_Areas_MELA_Project_background_and_results"><img alt="Research paper thumbnail of Morphotectonics of the European Lowland Areas (MELA) Project - background and results" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/90904129/Morphotectonics_of_the_European_Lowland_Areas_MELA_Project_background_and_results">Morphotectonics of the European Lowland Areas (MELA) Project - background and results</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The Project was prepared within HUMAN RESOURCES AND MOBILITY (HRM) ACTIVITY; MARIE CURIE ACTIONS;...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">The Project was prepared within HUMAN RESOURCES AND MOBILITY (HRM) ACTIVITY; MARIE CURIE ACTIONS; Marie Curie Host Fellowships for the Transfer of Knowledge (ToK), Development Host Scheme. Several partner institution from different European countries have participated in the project, among them: Polish Geological Institute, Pomeranian Branch, Szczecin (co-ordinator), Technische Universitä t Berlin, Civil Engineering and Applied Geosciences, Freie Universitä t Berlin, Institut f r Geologische Wissenschaften, Hydrogeologie, Humboldt-Universitä t zu Berlin, Geographisches Institut,University of Aarhus, Department of Earth Sciences, Landesamt f r Bergbau, Geologii und Rohstoffe, Lithuanian Geological Survey LGS and IRPI - Bari. The project has enabled to create in PGI a new research team involved in elaboration of a new methodologies for construction of a Morphotectonic Map of European Lowland Area. PGI was the co-ordinator of the research works aimed at construction of the map. The pro...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="90904129"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="90904129"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 90904129; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=90904129]").text(description); $(".js-view-count[data-work-id=90904129]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 90904129; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='90904129']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=90904129]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":90904129,"title":"Morphotectonics of the European Lowland Areas (MELA) Project - background and results","internal_url":"https://www.academia.edu/90904129/Morphotectonics_of_the_European_Lowland_Areas_MELA_Project_background_and_results","owner_id":40921523,"coauthors_can_edit":true,"owner":{"id":40921523,"first_name":"Olaf","middle_initials":null,"last_name":"Juschus","page_name":"OlafJuschus","domain_name":"independent","created_at":"2016-01-04T08:18:07.331-08:00","display_name":"Olaf Juschus","url":"https://independent.academia.edu/OlafJuschus"},"attachments":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="90904128"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/90904128/Geological_and_pedological_investigations_along_the_OPAL_pipeline_trench_in_Brandenburg_preliminary_Results_in_German_"><img alt="Research paper thumbnail of Geological and pedological investigations along the OPAL pipeline trench in Brandenburg – preliminary Results (in German)" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/90904128/Geological_and_pedological_investigations_along_the_OPAL_pipeline_trench_in_Brandenburg_preliminary_Results_in_German_">Geological and pedological investigations along the OPAL pipeline trench in Brandenburg – preliminary Results (in German)</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The 270 km long OPAL Pipeline crosses the federal state of Brandenburg from North to South. Its c...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">The 270 km long OPAL Pipeline crosses the federal state of Brandenburg from North to South. Its construction trench presented a more or less continuous outcrop 3-4 m deep that traverses all major Quaternary landscapes of Brandenburg. The main goal of this article is a first overview about the main geological and pedological findings along the pipeline. Besides the known geological and pedological structures of Brandenburg, a number of detailed and partly unexpected insights were documented along the outcrop. Within the gentle rolling Weichselian till plains of the Uckermark, the investigated Weichselian tills reveal abundant deformation structures that can be primarily related to shear deformation. Basins filled with glaciolimnic or anthropogenic colluvial sediments were repeatedly documented. A new finding is the comparably common occurrence of periglacial structures to the north of the Pomeranian Ice Stage. Although Luvisols represent the most common soils of this region, the prop...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="90904128"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="90904128"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 90904128; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=90904128]").text(description); $(".js-view-count[data-work-id=90904128]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 90904128; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='90904128']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=90904128]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":90904128,"title":"Geological and pedological investigations along the OPAL pipeline trench in Brandenburg – preliminary Results (in German)","internal_url":"https://www.academia.edu/90904128/Geological_and_pedological_investigations_along_the_OPAL_pipeline_trench_in_Brandenburg_preliminary_Results_in_German_","owner_id":40921523,"coauthors_can_edit":true,"owner":{"id":40921523,"first_name":"Olaf","middle_initials":null,"last_name":"Juschus","page_name":"OlafJuschus","domain_name":"independent","created_at":"2016-01-04T08:18:07.331-08:00","display_name":"Olaf Juschus","url":"https://independent.academia.edu/OlafJuschus"},"attachments":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="90904127"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/90904127/Wysoczyzna_Pojezierza_Mysliborskiego_i_Dolina_Dolnej_Odry_w_okolicy_Cedyni"><img alt="Research paper thumbnail of Wysoczyzna Pojezierza Mysliborskiego i Dolina Dolnej Odry w okolicy Cedyni" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/90904127/Wysoczyzna_Pojezierza_Mysliborskiego_i_Dolina_Dolnej_Odry_w_okolicy_Cedyni">Wysoczyzna Pojezierza Mysliborskiego i Dolina Dolnej Odry w okolicy Cedyni</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The aim of the article is the description o Lower Odra Valley geological structures as well as ad...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">The aim of the article is the description o Lower Odra Valley geological structures as well as adjacent morainic plateau. Presented issues will concentrate on geological structures both lithology and stratigraphy of Pleistocene. Also, the sedimental processes will be considered as being responsible for shaping Vistulian Glaciation deposits. The description of sub–Quaternary basement is presented throughout whole region and between the borders of Pomerania, Brandenburg and Meklemburg–Vorpomern either. Introduced issue concentrates on the connection between topography basement and tectonic structures of different stages. The origins of basement morphology seems to be very complicated, not only being tectonical but also polygenetic. Three types of erosion which influence the basement morphology: fluvial and glaciofluvial erosion, glacial abrasion. In the process of glacisostasy both ice – sweet loading and de–loading resulted in reversal linking. The ice – sweet was then influence by b...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="90904127"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="90904127"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 90904127; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=90904127]").text(description); $(".js-view-count[data-work-id=90904127]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 90904127; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='90904127']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=90904127]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":90904127,"title":"Wysoczyzna Pojezierza Mysliborskiego i Dolina Dolnej Odry w okolicy Cedyni","internal_url":"https://www.academia.edu/90904127/Wysoczyzna_Pojezierza_Mysliborskiego_i_Dolina_Dolnej_Odry_w_okolicy_Cedyni","owner_id":40921523,"coauthors_can_edit":true,"owner":{"id":40921523,"first_name":"Olaf","middle_initials":null,"last_name":"Juschus","page_name":"OlafJuschus","domain_name":"independent","created_at":"2016-01-04T08:18:07.331-08:00","display_name":"Olaf Juschus","url":"https://independent.academia.edu/OlafJuschus"},"attachments":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="90904073"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/90904073/Hydrochemistry_at_water_sample_station_Lz1079_in_lake_Elgygytgyn_Siberia"><img alt="Research paper thumbnail of Hydrochemistry at water sample station Lz1079 in lake Elgygytgyn, Siberia" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/90904073/Hydrochemistry_at_water_sample_station_Lz1079_in_lake_Elgygytgyn_Siberia">Hydrochemistry at water sample station Lz1079 in lake Elgygytgyn, Siberia</a></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="90904073"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="90904073"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 90904073; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=90904073]").text(description); $(".js-view-count[data-work-id=90904073]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 90904073; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='90904073']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=90904073]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":90904073,"title":"Hydrochemistry at water sample station Lz1079 in lake Elgygytgyn, Siberia","internal_url":"https://www.academia.edu/90904073/Hydrochemistry_at_water_sample_station_Lz1079_in_lake_Elgygytgyn_Siberia","owner_id":40921523,"coauthors_can_edit":true,"owner":{"id":40921523,"first_name":"Olaf","middle_initials":null,"last_name":"Juschus","page_name":"OlafJuschus","domain_name":"independent","created_at":"2016-01-04T08:18:07.331-08:00","display_name":"Olaf Juschus","url":"https://independent.academia.edu/OlafJuschus"},"attachments":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="20013587"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/20013587/A_microscopical_study_of_diatom_phytoplankton_in_deep_crater_Lake_Elgygytgyn_Northeast_Siberia"><img alt="Research paper thumbnail of A microscopical study of diatom phytoplankton in deep crater Lake El'gygytgyn, Northeast Siberia" class="work-thumbnail" src="https://attachments.academia-assets.com/41176474/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/20013587/A_microscopical_study_of_diatom_phytoplankton_in_deep_crater_Lake_Elgygytgyn_Northeast_Siberia">A microscopical study of diatom phytoplankton in deep crater Lake El'gygytgyn, Northeast Siberia</a></div><div class="wp-workCard_item"><span>Algological Studies</span><span>, 2005</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">A survey of the planktonic diatom community was carried out during summer 2003 in Lake El'gygytgy...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">A survey of the planktonic diatom community was carried out during summer 2003 in Lake El'gygytgyn, a deep, cold, low conductive and oligotrophic crater lake in the Northeast Siberian Arctic. Five planktonic diatom species were identified: Cyclostephanos dubius, Cyclotella ocellata, Cyclotella tripartita, Pliocaenicus costatus, and Stephanocostis chantaicus. The morphological details of the five taxa are documented by light and partly also scanning electron micrographs. Additionally, ecological and biogeographic data are provided. This is the first evidence of S. chantaicus in a northeast Siberian lake and one of the first findings of P. costatus outside the Baikal Lake region. The diatom community in summer 2003 was almost monospecificly dominated by Cyclotella ocellata (> 96 %), a species that displays a tremendous morphological variability. High concentrations and accumulation rates of diatom frustules during the ice-covered period (May-June 2003) indicated considerable under-ice phytoplankton growth.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="d67607d8fed76de5492ce507fbb3fa83" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":41176474,"asset_id":20013587,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/41176474/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="20013587"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="20013587"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 20013587; 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="20013586"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/20013586/Late_Quaternary_mass_movement_events_in_Lake_El%C3%A2_gygytgyn_North_eastern_Siberia"><img alt="Research paper thumbnail of Late Quaternary mass movement events in Lake Elâ²gygytgyn, North-eastern Siberia" class="work-thumbnail" src="https://attachments.academia-assets.com/41176288/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/20013586/Late_Quaternary_mass_movement_events_in_Lake_El%C3%A2_gygytgyn_North_eastern_Siberia">Late Quaternary mass movement events in Lake Elâ²gygytgyn, North-eastern Siberia</a></div><div class="wp-workCard_item"><span>Sedimentology</span><span>, 2009</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Lake El¢gygytgyn is situated in a 3AE6 Myr old impact crater in North-eastern Siberia. Its sedime...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Lake El¢gygytgyn is situated in a 3AE6 Myr old impact crater in North-eastern Siberia. Its sedimentary record probably represents the most complete archive of Pliocene and Quaternary climate change in the terrestrial Arctic. In order to investigate the influence of gravitational sediment transport on the pelagic sediment record in the lake centre, two sediment cores were recovered from the lower western lake slope. The cores penetrate a sub-recent mass movement deposit that was identified by 3AE5 kHz echo sounding. In the proximal part of this deposit, deformed sediments reflect an initial debris flow characterized by limited sediment mixture. Above and in front of the debrite, a wide massive densite indicates a second stage with a liquefied dense flow. The mass movement event led to basal erosion of ca 1 m thick unconsolidated sediments along parts of its flow path. The event produced a suspension cloud, whose deposition led to the formation of a turbidite. The occurrence of the turbidite throughout the lake and the limited erosion at its base mainly suggest deposition by 'pelagic rain' following Stokes' Law. Very similar radiocarbon dates obtained in the sediments directly beneath and above the turbidite in the central lake confirm this interpretation. When applying the depositional model for the Late Quaternary sediment record of Lake El¢gygytgyn, the recovered turbidites allow reconstruction of the frequency and temporal distribution of large mass movement events at the lake slopes. In total, 28 turbidites and related deposits were identified in two, 12AE9 and 16AE6 m long, sediment cores from the central lake area covering approximately 300 kyr.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="8d20cc08a0d7c14909e87c87ba4e9dbd" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":41176288,"asset_id":20013586,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/41176288/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="20013586"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="20013586"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 20013586; 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="20013585"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/20013585/A_combined_oxygen_and_silicon_diatom_isotope_record_of_Late_Quaternary_change_in_Lake_Elgygytgyn_North_East_Siberia"><img alt="Research paper thumbnail of A combined oxygen and silicon diatom isotope record of Late Quaternary change in Lake El'gygytgyn, North East Siberia" class="work-thumbnail" src="https://attachments.academia-assets.com/41176457/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/20013585/A_combined_oxygen_and_silicon_diatom_isotope_record_of_Late_Quaternary_change_in_Lake_Elgygytgyn_North_East_Siberia">A combined oxygen and silicon diatom isotope record of Late Quaternary change in Lake El'gygytgyn, North East Siberia</a></div><div class="wp-workCard_item"><span>Quaternary Science Reviews</span><span>, 2010</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Determining the response of sites within the Arctic Circle to long-term climatic change remains a...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Determining the response of sites within the Arctic Circle to long-term climatic change remains an essential pre-requisite for assessing the susceptibility of these regions to future global warming and Arctic amplification. To date, existing records from North East Russia have demonstrated significant spatial variability across the region during the late Quaternary. Here we present diatom δ 18 O and δ 30 Si data from Lake El'gygytgyn, Russia, and suggest environmental changes that would have impacted across West Beringia from the Last Glacial Maximum to the modern day. In combination with other records, the results raise the potential for climatic teleconnections to exist between the region and sites in the North Atlantic.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="ede454d895ee8917bc454f0c7ceeac80" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":41176457,"asset_id":20013585,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/41176457/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="20013585"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="20013585"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 20013585; 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dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "ede454d895ee8917bc454f0c7ceeac80" } } $('.js-work-strip[data-work-id=20013585]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":20013585,"title":"A combined oxygen and silicon diatom isotope record of Late Quaternary change in Lake El'gygytgyn, North East Siberia","internal_url":"https://www.academia.edu/20013585/A_combined_oxygen_and_silicon_diatom_isotope_record_of_Late_Quaternary_change_in_Lake_Elgygytgyn_North_East_Siberia","owner_id":40921523,"coauthors_can_edit":true,"owner":{"id":40921523,"first_name":"Olaf","middle_initials":null,"last_name":"Juschus","page_name":"OlafJuschus","domain_name":"independent","created_at":"2016-01-04T08:18:07.331-08:00","display_name":"Olaf Juschus","url":"https://independent.academia.edu/OlafJuschus"},"attachments":[{"id":41176457,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/41176457/thumbnails/1.jpg","file_name":"A_combined_oxygen_and_silicon_diatom_iso20160115-557-eq8e6c.pdf","download_url":"https://www.academia.edu/attachments/41176457/download_file","bulk_download_file_name":"A_combined_oxygen_and_silicon_diatom_iso.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/41176457/A_combined_oxygen_and_silicon_diatom_iso20160115-557-eq8e6c-libre.pdf?1452845689=\u0026response-content-disposition=attachment%3B+filename%3DA_combined_oxygen_and_silicon_diatom_iso.pdf\u0026Expires=1740575340\u0026Signature=IeZ1xDbsrbiOaegmSRy~w~b-6qtyad1uIpYVGg~Cdw59tz3j189CJ-n0DK7QvxF3LLcV5DsdkBJm5nZlNk14lxsNMMLO67ICajClT86sPaGWgcU2tOjW4qqzqOmrnRM7PDr4PqTQ040dnlOtHyxA2Lwox5LT~pjGzbQtBhdRCZNQU1dTOc8OYozdCFA4s3VDxfjcMOS6CXBxRvh1gkqe1gP-LVZLzsomV8Mi9Z3ysWvJR71v2Irfc7anNdp39BIQmOg6y~fxUNiKQFQU~9aycGFck3KRjXtwbfpUFJKt50VkGCQ93Ks6xSqBomUrNSZEsl36ESaHoCWGUzt1dqeUNQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="20013584"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/20013584/Late_Quaternary_lake_level_changes_of_Lake_Elgygytgyn_NE_Siberia"><img alt="Research paper thumbnail of Late Quaternary lake-level changes of Lake El'gygytgyn, NE Siberia" class="work-thumbnail" src="https://attachments.academia-assets.com/41176305/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/20013584/Late_Quaternary_lake_level_changes_of_Lake_Elgygytgyn_NE_Siberia">Late Quaternary lake-level changes of Lake El'gygytgyn, NE Siberia</a></div><div class="wp-workCard_item wp-workCard--coauthors"><span>by </span><span><a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/OlafJuschus">Olaf Juschus</a> and <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/FedorovGrigory">Grigory Fedorov</a></span></div><div class="wp-workCard_item"><span>Quaternary Research</span><span>, 2011</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Lake El'gygytgyn is situated in a 3.6 Ma old impact crater in northeastern Siberia. Presented her...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Lake El'gygytgyn is situated in a 3.6 Ma old impact crater in northeastern Siberia. Presented here is a reconstruction of the Quaternary lake-level history as derived from sediment cores from the southern lake shelf. There, a cliff-like bench 10 m below the modern water level has been investigated. Deep-water sediments on the shelf indicate high lake levels during a warm Mid-Pleistocene period. One period with low lake level prior to Marine Oxygen Isotope Stage (MIS) 3 has been identified, followed by a period of high lake level (10 m above present). In the course of MIS 2 the lake level dropped to − 10 m. At the end of MIS 2 the bench was formed and coarse beach sedimentation occurred. Subsequently, the lake level rose rapidly to the Holocene level. Changes in water level are likely linked to climate variability. During relatively temperate periods the lake becomes free of ice in summer. Strong wave actions transport sediment parallel to the coast and towards the outlet, where the material tends to accumulate, resulting in lake level rise. During cold periods the perennial lake ice cover hampers any wave activity and pebble-transport, keeping the outlet open and causing the lake level to drop.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="9af88e485066dff8f4affd351ae3a7d5" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":41176305,"asset_id":20013584,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/41176305/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="20013584"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="20013584"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 20013584; 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="20013583"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/20013583/Applying_SAR_IRSL_methodology_for_dating_fine_grained_sediments_from_Lake_El_gygytgyn_north_eastern_Siberia"><img alt="Research paper thumbnail of Applying SAR-IRSL methodology for dating fine-grained sediments from Lake El’gygytgyn, north-eastern Siberia" class="work-thumbnail" src="https://attachments.academia-assets.com/41176291/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/20013583/Applying_SAR_IRSL_methodology_for_dating_fine_grained_sediments_from_Lake_El_gygytgyn_north_eastern_Siberia">Applying SAR-IRSL methodology for dating fine-grained sediments from Lake El’gygytgyn, north-eastern Siberia</a></div><div class="wp-workCard_item"><span>Quaternary Geochronology</span><span>, 2007</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Lake El'gygytgyn is situated in a 3.6 Ma old impact crater in north-eastern Siberia and probably ...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Lake El'gygytgyn is situated in a 3.6 Ma old impact crater in north-eastern Siberia and probably represents one of the most complete archives of Arctic climate change. Investigated here is the potential of infra-red stimulated luminescence (IRSL) using the single-aliquot regenerative-dose (SAR) approach for dating sediments from this lake. Independent age control is available from a published age model of a parallel core that is based on tuning sediment proxies with regional insolation and the results of previous multiple aliquot IRSL dating. Although the site is located within volcanic bedrock, anomalous fading seems to have little effect on the calculated ages. The modelled water content for the entire time of burial is seen as the most prominent uncertainty at this particular site. Despite these potential error sources, SAR-IRSL ages are in acceptable agreement with the given timeframe and clearly point to the possibility to establish independent chronologies at this site up to at least 400,000 years. r</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="edb9f44d473bef2c519805b56b269238" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":41176291,"asset_id":20013583,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/41176291/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="20013583"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="20013583"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 20013583; 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="20013582"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/20013582/Climatic_variability_during_the_last_interglacial_inferred_from_geochemical_proxies_in_the_Lake_Elgygytgyn_sediment_record"><img alt="Research paper thumbnail of Climatic variability during the last interglacial inferred from geochemical proxies in the Lake El'gygytgyn sediment record" class="work-thumbnail" src="https://attachments.academia-assets.com/41177027/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/20013582/Climatic_variability_during_the_last_interglacial_inferred_from_geochemical_proxies_in_the_Lake_Elgygytgyn_sediment_record">Climatic variability during the last interglacial inferred from geochemical proxies in the Lake El'gygytgyn sediment record</a></div><div class="wp-workCard_item wp-workCard--coauthors"><span>by </span><span><a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/OlafJuschus">Olaf Juschus</a> and <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/LauraCunningham1">Laura Cunningham</a></span></div><div class="wp-workCard_item"><span>Palaeogeography, Palaeoclimatology, Palaeoecology</span><span>, 2013</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The Last Interglacial Period (LIP) is often regarded as a good analogue for potential climatic co...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">The Last Interglacial Period (LIP) is often regarded as a good analogue for potential climatic conditions under predicted global warming scenarios. Despite this, there is still debate over the nature, duration and frequency of climatic changes during this period. One particularly contentious issue has been the apparent evidence of climatic instability identified in many marine cores but seemingly lacking from many terrestrial archives, especially within the Arctic, a key region for global climate change research. In this paper, geochemical records from Lake El'gygytgyn, north-eastern Russia, are used to infer past climatic changes during the LIP from within the high Arctic. With a sampling resolution of~20-~90 years, these records offer the potential for detailed, high-resolution palaeoclimate reconstruction. This study shows that the LIP commenced in central Chukotkã 129 thousand years ago (ka), with the warmest climatic conditions occurring between~128 and 127 ka before being interrupted by a short-lived cold reversal. Mild climatic conditions then persisted until~122 ka when a marked reduction in the sedimentation rate suggests a decrease in precipitation. A further climatic deterioration at~118 ka marks the return to glacial conditions. This study highlights the value of incorporating several geochemical proxies when inferring past climatic conditions, thus providing the potential to identify signals related to environmental change within the catchment. We also demonstrate the importance of considering how changes in sedimentation rate influence proxy records, in order to develop robust palaeoenvironmental reconstructions.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="c1ddc5f67ee49526713b1faabec422f9" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":41177027,"asset_id":20013582,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/41177027/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="20013582"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="20013582"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 20013582; 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="2557038"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/2557038/Modern_sedimentation_patterns_in_Lake_El_gygytgyn_NE_Russia_derived_from_surface_sediment_and_inlet_streams_samples"><img alt="Research paper thumbnail of Modern sedimentation patterns in Lake El’gygytgyn, NE Russia, derived from surface sediment and inlet streams samples" class="work-thumbnail" src="https://attachments.academia-assets.com/30569893/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/2557038/Modern_sedimentation_patterns_in_Lake_El_gygytgyn_NE_Russia_derived_from_surface_sediment_and_inlet_streams_samples">Modern sedimentation patterns in Lake El’gygytgyn, NE Russia, derived from surface sediment and inlet streams samples</a></div><div class="wp-workCard_item wp-workCard--coauthors"><span>by </span><span><a class="" data-click-track="profile-work-strip-authors" href="https://uni-koeln.academia.edu/VolkerWennrich">Volker Wennrich</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/OlafJuschus">Olaf Juschus</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/PavelMinyuk">Pavel Minyuk</a></span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Lake El'gygytgyn/NE Russia holds a continuous 3.58 Ma sediment record, which is regarded as the m...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Lake El'gygytgyn/NE Russia holds a continuous 3.58 Ma sediment record, which is regarded as the most longlasting climate archive of the terrestrial Arctic. Based on multi-proxy geochemical, mineralogical, and granulometric analyses of surface sediment, inlet stream and bedrock samples, supplemented by statistical methods, major processes influencing the modern sedimentation in the lake were investigated. Grain-size parameters and chemical elements linked to the input of feldspars from acidic bedrock indicate a windinduced two-cell current system as major driver of sediment transport and accumulation processes in Lake El'gygytgyn. The distribution of mafic rock related elements in the sediment on the lake floor can be traced back to the input of weathering products of basaltic rocks in the catchment. Obvious similarities in the spatial variability of manganese and heavy metals indicate sorption or co-precipitation of these elements with Fe and Mn hydroxides and oxides. But the similar distribution of organic matter and clay contents might also point to a fixation to organic components and clay minerals. An enrichment of mercury in the inlet streams might be indicative of neotectonic activity around the lake. The results of this study add to the fundamental knowledge of the modern lake processes of Lake El'gygytgyn and its lakecatchment interactions, and thus, yield crucial insights for the interpretation of paleo-data from this unique archive. , 2013 <a href="http://www.clim-past.net/9/135/2013/" rel="nofollow">www.clim-past.net/9/135/2013/</a> <a href="http://www.clim-past.net/9/135/2013/" rel="nofollow">www.clim-past.net/9/135/2013/</a> Clim. Past, 9, 135-148, 2013 Clim. 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</script> </div><div class="profile--tab_content_container js-tab-pane tab-pane" data-section-id="4348493" id="papers"><div class="js-work-strip profile--work_container" data-work-id="90904262"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/90904262/To_the_southern_margin_of_the_last_northern_glaciation_a_field_trip_through_the_young_moraine_area_south_east_of_Berlin"><img alt="Research paper thumbnail of To the southern margin of the (last) northern glaciation – a field trip through the young moraine area south-east of Berlin" class="work-thumbnail" src="https://attachments.academia-assets.com/94338120/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/90904262/To_the_southern_margin_of_the_last_northern_glaciation_a_field_trip_through_the_young_moraine_area_south_east_of_Berlin">To the southern margin of the (last) northern glaciation – a field trip through the young moraine area south-east of Berlin</a></div><div class="wp-workCard_item"><span>DEUQUA Special Publications</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The young moraine area to the southeast of Berlin was repeatedly overrun and covered by Scandinav...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">The young moraine area to the southeast of Berlin was repeatedly overrun and covered by Scandinavian ice sheets (SISs). The last glaciation took place during the Last Glacial Maximum (LGM), when the last/most recent SIS reached its furthest southern extent. An incompletely formed chain of terminal moraines marks the Brandenburg ice stage. The most recent glacier had its greatest environmental impact due to the large quantities of released meltwaters. Many subglacial channels, massive proglacial sands and huge meltwater streamways (Urstromtäler) were formed at that time. During the Holocene, the landscape was finally shaped mainly by the rivers Dahme and Spree.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="b5bac7cdd6732dcf6849640c0efa4d39" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":94338120,"asset_id":90904262,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/94338120/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="90904262"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item 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class="wp-workCard_item"><span class="js-work-more-abstract-truncated">4.3.3.6 Die Entwicklung der glazifluvialen Abflussverhältnisse um Lübben-Das Trockenfallen des Ba...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">4.3.3.6 Die Entwicklung der glazifluvialen Abflussverhältnisse um Lübben-Das Trockenfallen des Baruther Abschnittes 4.3.4 Die Entwicklung der Schmelzwasserabflussbahnen zwischen dem Baruther und dem Berliner Urstromtal 4.3.4.1 Einführung 4.3.4.2 Die Abflussphase in Richtung Beelitz 4.3.4.3 Die Abflussphase in Richtung Potsdam 4.3.4.4 Der Abfluss vom Unterspreewald in Richtung Berlin 4.3.4.5 Gemeinsamkeiten der Abflussbahnen zwischen dem Baruther und dem Berliner Urstromtal 4.3.5 Der Kontakt Baruther Urstromtal-Fläming bei Klein Ziescht VII 4.3.6 Zusammenfassung der Forschungsergebnisse zur Entwicklung der Urstromtalungen im Jungmoränenland südlich Berlins 4.4 Die Oberflächenformen der Platten im Jungmoränenland südlich Berlins 4.4.1 Einführung 4.4.2 Die Platten im Bereich der Brandenburger Eisrandlage 4.4.2.1 Das Neuendorfer Becken 4.4.2.2 Das Eisstaubecken von Zesch am See 4.4.3 Die Oberflächenformen der Platten nördlich der Brandenburger Eisrandlage 4.5 Der geologische Bau der Platten im Jungmoränenland südlich Berlins 4.5.1 Aufschlüsse in saalezeitlichen Sedimenten 4.5.2 Aufschlussprofile mit geringmächtigen weichselzeitlichen Sedimenten 4.5.3 Aufschlussprofile mit mächtigeren weichselzeitlichen Sedimenten 4.5.4 Gemeinsamkeiten im geologischen Bau der Platten 4.5.5 Auswertung der Geschiebeanalysen 4.5.5.1 Einführung 4.5.5.2 Die Geschiebespektren des unteren Geschiebemergels 4.5.5.3 Auswertung der Proben aus dem oberen Till 4.5.6 Zusammenfassung der Untersuchungsergebnisse zur Entstehung der Platten im Jungmoränenland südlich Berlins 4.6 Glaziale Rinnen im Jungmoränenland südlich Berlins 4.6.1 Zur Genese der Glazialen Rinnen im Arbeitsgebiet 4.6.1.1 Breitrinnen 4.6.1.2 Schmalrinnen 4.6.2 Zusammenfassung 4.7 Untersuchungen zur spätglazial-frühholozänen Entwicklung des Gewässernetzes im Jungmoränenland südlich Berlins 4.7.1 Einleitung 4.7.2 Der Töpchiner See 4.7.2.1 Beschreibung des Seebeckens 4.7.2.2 Das Pollendiagramm der Bohrung TÖP K1 4.7.3 Zur spätglazial-frühholozänen Entwicklung der Spree im Unterspreewald 4.7.3.1 Einleitung 4.7.3.2 Die braided river-Strukturen der Landgraben-Urspree 4.7.3.3 Die Pretschener Urspree 4.7.3.4 Der Großmäander am Köthener See 4.7.3.5 Die Lubolz-Krausnicker Urspree 4.7.3.6 Zur Ursache der Spreeablenkung 4.7.4 Zusammenfassung der Untersuchungsergebnisse zur spätglazialfrühholozänen Entwicklung des Gewässernetzes 5 Zusammenfassung und Ausblick 5.1 Chronologische Zusammenfassung der Untersuchungsergebnisse zur jungquartären Entwicklung des Untersuchungsgebietes 5.1.1 Zur präweichselzeitlichen Entwicklung des Arbeitsgebietes 5.1.2 Zur Entwicklung während des weichselzeitlichen Eisvorstoßes VIII 5.1.3 Die Entwicklung während des Weichselmaximalvorstoßes-Der Älteste Baruther Urstrom 5.1.4 Die Brandenburger Eisrandlage-Der Ältere Baruther Urstrom 5.1.5 Die Aufgabe der Brandenburger Eisrandlage-Der Jüngere Baruther Urstrom 5.1.6 Der Jüngste Baruther Urstrom 5.1.7 Die Abflussphasen zwischen dem Baruther und dem Berliner Urstromtal</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="3e7d39b23efbd92e2dc19bd0511a0981" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":94338171,"asset_id":90904259,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/94338171/download_file?s=profile"><span><i class="fa 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The owner o...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">El'gygytgyn"-Chukchi word for "White Lake" storage and various scientific activities. The owner of the cabin (Yuri Gopkalo) was hired as a care-keeper and cook. He arrived on June 12, via a helicopter trip of the Pevek Gold Mining Company, and remained with the expedition until finished. 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="90904130"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/90904130/Klassifikation_und_Aufbau_ausgew%C3%A4hlter_Vorkommen_glazilimnischer_Sedimente_n%C3%B6rdlich_der_Pommerschen_Eisrandlage_im_brandenburgischen_Abschnitt_der_Erdgasfernleitung_OPAL"><img alt="Research paper thumbnail of Klassifikation und Aufbau ausgewählter Vorkommen glazilimnischer Sedimente nördlich der Pommerschen Eisrandlage im brandenburgischen Abschnitt der Erdgasfernleitung OPAL" class="work-thumbnail" src="https://attachments.academia-assets.com/94337981/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/90904130/Klassifikation_und_Aufbau_ausgew%C3%A4hlter_Vorkommen_glazilimnischer_Sedimente_n%C3%B6rdlich_der_Pommerschen_Eisrandlage_im_brandenburgischen_Abschnitt_der_Erdgasfernleitung_OPAL">Klassifikation und Aufbau ausgewählter Vorkommen glazilimnischer Sedimente nördlich der Pommerschen Eisrandlage im brandenburgischen Abschnitt der Erdgasfernleitung OPAL</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">1. Einführung Die Ostsee-Pipeline-Anbindungsleitung (OPAL) verläuft über 470 km von Lubmin bei Gr...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">1. Einführung Die Ostsee-Pipeline-Anbindungsleitung (OPAL) verläuft über 470 km von Lubmin bei Greifswald bis nach Olbernhau an der deutsch-tschechischen Grenze (vgl. Höhlschen 2011). 270 km der Leitung durchziehen von Nord nach Süd das östliche Brandenburg (Abb. 1). Die Pipeline mit einem Durchmesser von 1,40 m wurde im brandenburger Abschnitt zwischen April 2010 und April 2011 verlegt. Im Zuge des Leitungsbaus wurde ein nahezu kontinuierlicher Aufschluss von 2,5 bis 3,5 m Tiefe geschaffen, der einmalige Einblicke in die oberflächennah anstehenden Ablagerungen bot. Ein erster, zusammenfassender Überblick der Ergebnisse wurde für Brandenburg von Juschus et al. 2011 gegeben, für den nördlich angrenzenden Abschnitt Vorpommerns von Börner et al. 2011. Der folgende Artikel konzentriert sich auf die glazilimnischen Ablagerungen zwischen der nördlichen Landesgrenze Brandenburgs und der Pommerschen Eisrandlage bei Oderberg. In der Literatur wurden bisher vor allem die Staubeckensedimente i...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="21d9815fd3618026f21b488fff320cd1" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":94337981,"asset_id":90904130,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/94337981/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="90904130"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="90904130"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 90904130; 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="90904129"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/90904129/Morphotectonics_of_the_European_Lowland_Areas_MELA_Project_background_and_results"><img alt="Research paper thumbnail of Morphotectonics of the European Lowland Areas (MELA) Project - background and results" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/90904129/Morphotectonics_of_the_European_Lowland_Areas_MELA_Project_background_and_results">Morphotectonics of the European Lowland Areas (MELA) Project - background and results</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The Project was prepared within HUMAN RESOURCES AND MOBILITY (HRM) ACTIVITY; MARIE CURIE ACTIONS;...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">The Project was prepared within HUMAN RESOURCES AND MOBILITY (HRM) ACTIVITY; MARIE CURIE ACTIONS; Marie Curie Host Fellowships for the Transfer of Knowledge (ToK), Development Host Scheme. Several partner institution from different European countries have participated in the project, among them: Polish Geological Institute, Pomeranian Branch, Szczecin (co-ordinator), Technische Universitä t Berlin, Civil Engineering and Applied Geosciences, Freie Universitä t Berlin, Institut f r Geologische Wissenschaften, Hydrogeologie, Humboldt-Universitä t zu Berlin, Geographisches Institut,University of Aarhus, Department of Earth Sciences, Landesamt f r Bergbau, Geologii und Rohstoffe, Lithuanian Geological Survey LGS and IRPI - Bari. The project has enabled to create in PGI a new research team involved in elaboration of a new methodologies for construction of a Morphotectonic Map of European Lowland Area. PGI was the co-ordinator of the research works aimed at construction of the map. The pro...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="90904129"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="90904129"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 90904129; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=90904129]").text(description); $(".js-view-count[data-work-id=90904129]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 90904129; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='90904129']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=90904129]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":90904129,"title":"Morphotectonics of the European Lowland Areas (MELA) Project - background and results","internal_url":"https://www.academia.edu/90904129/Morphotectonics_of_the_European_Lowland_Areas_MELA_Project_background_and_results","owner_id":40921523,"coauthors_can_edit":true,"owner":{"id":40921523,"first_name":"Olaf","middle_initials":null,"last_name":"Juschus","page_name":"OlafJuschus","domain_name":"independent","created_at":"2016-01-04T08:18:07.331-08:00","display_name":"Olaf Juschus","url":"https://independent.academia.edu/OlafJuschus"},"attachments":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="90904128"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/90904128/Geological_and_pedological_investigations_along_the_OPAL_pipeline_trench_in_Brandenburg_preliminary_Results_in_German_"><img alt="Research paper thumbnail of Geological and pedological investigations along the OPAL pipeline trench in Brandenburg – preliminary Results (in German)" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/90904128/Geological_and_pedological_investigations_along_the_OPAL_pipeline_trench_in_Brandenburg_preliminary_Results_in_German_">Geological and pedological investigations along the OPAL pipeline trench in Brandenburg – preliminary Results (in German)</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The 270 km long OPAL Pipeline crosses the federal state of Brandenburg from North to South. Its c...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">The 270 km long OPAL Pipeline crosses the federal state of Brandenburg from North to South. Its construction trench presented a more or less continuous outcrop 3-4 m deep that traverses all major Quaternary landscapes of Brandenburg. The main goal of this article is a first overview about the main geological and pedological findings along the pipeline. Besides the known geological and pedological structures of Brandenburg, a number of detailed and partly unexpected insights were documented along the outcrop. Within the gentle rolling Weichselian till plains of the Uckermark, the investigated Weichselian tills reveal abundant deformation structures that can be primarily related to shear deformation. Basins filled with glaciolimnic or anthropogenic colluvial sediments were repeatedly documented. A new finding is the comparably common occurrence of periglacial structures to the north of the Pomeranian Ice Stage. Although Luvisols represent the most common soils of this region, the prop...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="90904128"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="90904128"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 90904128; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=90904128]").text(description); $(".js-view-count[data-work-id=90904128]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 90904128; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='90904128']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=90904128]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":90904128,"title":"Geological and pedological investigations along the OPAL pipeline trench in Brandenburg – preliminary Results (in German)","internal_url":"https://www.academia.edu/90904128/Geological_and_pedological_investigations_along_the_OPAL_pipeline_trench_in_Brandenburg_preliminary_Results_in_German_","owner_id":40921523,"coauthors_can_edit":true,"owner":{"id":40921523,"first_name":"Olaf","middle_initials":null,"last_name":"Juschus","page_name":"OlafJuschus","domain_name":"independent","created_at":"2016-01-04T08:18:07.331-08:00","display_name":"Olaf Juschus","url":"https://independent.academia.edu/OlafJuschus"},"attachments":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="90904127"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/90904127/Wysoczyzna_Pojezierza_Mysliborskiego_i_Dolina_Dolnej_Odry_w_okolicy_Cedyni"><img alt="Research paper thumbnail of Wysoczyzna Pojezierza Mysliborskiego i Dolina Dolnej Odry w okolicy Cedyni" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/90904127/Wysoczyzna_Pojezierza_Mysliborskiego_i_Dolina_Dolnej_Odry_w_okolicy_Cedyni">Wysoczyzna Pojezierza Mysliborskiego i Dolina Dolnej Odry w okolicy Cedyni</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The aim of the article is the description o Lower Odra Valley geological structures as well as ad...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">The aim of the article is the description o Lower Odra Valley geological structures as well as adjacent morainic plateau. Presented issues will concentrate on geological structures both lithology and stratigraphy of Pleistocene. Also, the sedimental processes will be considered as being responsible for shaping Vistulian Glaciation deposits. The description of sub–Quaternary basement is presented throughout whole region and between the borders of Pomerania, Brandenburg and Meklemburg–Vorpomern either. Introduced issue concentrates on the connection between topography basement and tectonic structures of different stages. The origins of basement morphology seems to be very complicated, not only being tectonical but also polygenetic. Three types of erosion which influence the basement morphology: fluvial and glaciofluvial erosion, glacial abrasion. In the process of glacisostasy both ice – sweet loading and de–loading resulted in reversal linking. The ice – sweet was then influence by b...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="90904127"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="90904127"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 90904127; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=90904127]").text(description); $(".js-view-count[data-work-id=90904127]").attr('title', description).tooltip(); 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window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=90904073]").text(description); $(".js-view-count[data-work-id=90904073]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 90904073; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='90904073']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-a9bf3a2bc8c89fa2a77156577594264ee8a0f214d74241bc0fcd3f69f8d107ac.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=90904073]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":90904073,"title":"Hydrochemistry at water sample station Lz1079 in lake Elgygytgyn, Siberia","internal_url":"https://www.academia.edu/90904073/Hydrochemistry_at_water_sample_station_Lz1079_in_lake_Elgygytgyn_Siberia","owner_id":40921523,"coauthors_can_edit":true,"owner":{"id":40921523,"first_name":"Olaf","middle_initials":null,"last_name":"Juschus","page_name":"OlafJuschus","domain_name":"independent","created_at":"2016-01-04T08:18:07.331-08:00","display_name":"Olaf Juschus","url":"https://independent.academia.edu/OlafJuschus"},"attachments":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="20013587"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/20013587/A_microscopical_study_of_diatom_phytoplankton_in_deep_crater_Lake_Elgygytgyn_Northeast_Siberia"><img alt="Research paper thumbnail of A microscopical study of diatom phytoplankton in deep crater Lake El'gygytgyn, Northeast Siberia" class="work-thumbnail" src="https://attachments.academia-assets.com/41176474/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/20013587/A_microscopical_study_of_diatom_phytoplankton_in_deep_crater_Lake_Elgygytgyn_Northeast_Siberia">A microscopical study of diatom phytoplankton in deep crater Lake El'gygytgyn, Northeast Siberia</a></div><div class="wp-workCard_item"><span>Algological Studies</span><span>, 2005</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">A survey of the planktonic diatom community was carried out during summer 2003 in Lake El'gygytgy...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">A survey of the planktonic diatom community was carried out during summer 2003 in Lake El'gygytgyn, a deep, cold, low conductive and oligotrophic crater lake in the Northeast Siberian Arctic. Five planktonic diatom species were identified: Cyclostephanos dubius, Cyclotella ocellata, Cyclotella tripartita, Pliocaenicus costatus, and Stephanocostis chantaicus. The morphological details of the five taxa are documented by light and partly also scanning electron micrographs. Additionally, ecological and biogeographic data are provided. This is the first evidence of S. chantaicus in a northeast Siberian lake and one of the first findings of P. costatus outside the Baikal Lake region. The diatom community in summer 2003 was almost monospecificly dominated by Cyclotella ocellata (> 96 %), a species that displays a tremendous morphological variability. High concentrations and accumulation rates of diatom frustules during the ice-covered period (May-June 2003) indicated considerable under-ice phytoplankton growth.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="d67607d8fed76de5492ce507fbb3fa83" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":41176474,"asset_id":20013587,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/41176474/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="20013587"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="20013587"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 20013587; 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dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "d67607d8fed76de5492ce507fbb3fa83" } } $('.js-work-strip[data-work-id=20013587]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":20013587,"title":"A microscopical study of diatom phytoplankton in deep crater Lake El'gygytgyn, Northeast Siberia","internal_url":"https://www.academia.edu/20013587/A_microscopical_study_of_diatom_phytoplankton_in_deep_crater_Lake_Elgygytgyn_Northeast_Siberia","owner_id":40921523,"coauthors_can_edit":true,"owner":{"id":40921523,"first_name":"Olaf","middle_initials":null,"last_name":"Juschus","page_name":"OlafJuschus","domain_name":"independent","created_at":"2016-01-04T08:18:07.331-08:00","display_name":"Olaf Juschus","url":"https://independent.academia.edu/OlafJuschus"},"attachments":[{"id":41176474,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/41176474/thumbnails/1.jpg","file_name":"A_microscopical_study_of_diatom_phytopla20160115-6094-1wj3w65.pdf","download_url":"https://www.academia.edu/attachments/41176474/download_file","bulk_download_file_name":"A_microscopical_study_of_diatom_phytopla.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/41176474/A_microscopical_study_of_diatom_phytopla20160115-6094-1wj3w65-libre.pdf?1452845686=\u0026response-content-disposition=attachment%3B+filename%3DA_microscopical_study_of_diatom_phytopla.pdf\u0026Expires=1740575339\u0026Signature=eW0h~pG4j5JOueiNpgmOGrVF~NwtXFt2VHRLnAJXUKFEXAj-mWnCisoNrSrsEq5epycE3sABpPruHqk-VoOp5mhwrssWGHfgr1M19xXRL77LFrmItTDPDsBdNCUFW~u1KZG4QCgB9uSFFBXp9wUS-9ksT4FSC3aW5v5GfWz5VdAWq1LOI~pvKPYlXdg2h1FMBgcW489MkucZe-gsKBOdkkWkT2h-qbOh3rISrJCalkhByWTGDYw8htK03Vv6bLiZbedTj0DUyuUv7ntFA-9nxJN8bqopvoCnmPUOq5wWg2QNmtDO3u4MAJTHYNhF4J0GLKLaZVD0Lbt4WqC0YNZvWA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="20013586"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/20013586/Late_Quaternary_mass_movement_events_in_Lake_El%C3%A2_gygytgyn_North_eastern_Siberia"><img alt="Research paper thumbnail of Late Quaternary mass movement events in Lake Elâ²gygytgyn, North-eastern Siberia" class="work-thumbnail" src="https://attachments.academia-assets.com/41176288/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/20013586/Late_Quaternary_mass_movement_events_in_Lake_El%C3%A2_gygytgyn_North_eastern_Siberia">Late Quaternary mass movement events in Lake Elâ²gygytgyn, North-eastern Siberia</a></div><div class="wp-workCard_item"><span>Sedimentology</span><span>, 2009</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Lake El¢gygytgyn is situated in a 3AE6 Myr old impact crater in North-eastern Siberia. Its sedime...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Lake El¢gygytgyn is situated in a 3AE6 Myr old impact crater in North-eastern Siberia. Its sedimentary record probably represents the most complete archive of Pliocene and Quaternary climate change in the terrestrial Arctic. In order to investigate the influence of gravitational sediment transport on the pelagic sediment record in the lake centre, two sediment cores were recovered from the lower western lake slope. The cores penetrate a sub-recent mass movement deposit that was identified by 3AE5 kHz echo sounding. In the proximal part of this deposit, deformed sediments reflect an initial debris flow characterized by limited sediment mixture. Above and in front of the debrite, a wide massive densite indicates a second stage with a liquefied dense flow. The mass movement event led to basal erosion of ca 1 m thick unconsolidated sediments along parts of its flow path. The event produced a suspension cloud, whose deposition led to the formation of a turbidite. The occurrence of the turbidite throughout the lake and the limited erosion at its base mainly suggest deposition by 'pelagic rain' following Stokes' Law. Very similar radiocarbon dates obtained in the sediments directly beneath and above the turbidite in the central lake confirm this interpretation. When applying the depositional model for the Late Quaternary sediment record of Lake El¢gygytgyn, the recovered turbidites allow reconstruction of the frequency and temporal distribution of large mass movement events at the lake slopes. In total, 28 turbidites and related deposits were identified in two, 12AE9 and 16AE6 m long, sediment cores from the central lake area covering approximately 300 kyr.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="8d20cc08a0d7c14909e87c87ba4e9dbd" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":41176288,"asset_id":20013586,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/41176288/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="20013586"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="20013586"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 20013586; 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dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "8d20cc08a0d7c14909e87c87ba4e9dbd" } } $('.js-work-strip[data-work-id=20013586]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":20013586,"title":"Late Quaternary mass movement events in Lake Elâ²gygytgyn, North-eastern Siberia","internal_url":"https://www.academia.edu/20013586/Late_Quaternary_mass_movement_events_in_Lake_El%C3%A2_gygytgyn_North_eastern_Siberia","owner_id":40921523,"coauthors_can_edit":true,"owner":{"id":40921523,"first_name":"Olaf","middle_initials":null,"last_name":"Juschus","page_name":"OlafJuschus","domain_name":"independent","created_at":"2016-01-04T08:18:07.331-08:00","display_name":"Olaf Juschus","url":"https://independent.academia.edu/OlafJuschus"},"attachments":[{"id":41176288,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/41176288/thumbnails/1.jpg","file_name":"Late_Quaternary_mass_movement_events_in_20160115-14312-1pl7isc.pdf","download_url":"https://www.academia.edu/attachments/41176288/download_file","bulk_download_file_name":"Late_Quaternary_mass_movement_events_in.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/41176288/Late_Quaternary_mass_movement_events_in_20160115-14312-1pl7isc-libre.pdf?1452845698=\u0026response-content-disposition=attachment%3B+filename%3DLate_Quaternary_mass_movement_events_in.pdf\u0026Expires=1740575339\u0026Signature=TU0z6OHJh7IqNG9mlnB7hww6roFCq0H1I7OE~kXHbqAFNR0B2JOV7qSVmmWk~27YLpSyNtTDs-dumRR3Kyh02v4YlPIZXrLZgtNp~IKXO2LScP3pdaVexhikqU-FInSEDAufzwH1f8EtiY1KpHPkjCs2ds3SyQOdcI87PQipWOfYRAMv8rpaZQF7DDLhtdOjWPs5rOT~~prmxIe6vepa6QCcLpkkdoZmgcs34WUk0DmU8UpXW9Pv~vs4fkKvmTZ~N1jdsZ-iQP83b9Z9Skbw6-W8jCu10mnE1OUWY5KPShuIP5d9Ll08B6l5hxt~PDm7WXs2AYZwxab8-qnI6DGH8w__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="20013585"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/20013585/A_combined_oxygen_and_silicon_diatom_isotope_record_of_Late_Quaternary_change_in_Lake_Elgygytgyn_North_East_Siberia"><img alt="Research paper thumbnail of A combined oxygen and silicon diatom isotope record of Late Quaternary change in Lake El'gygytgyn, North East Siberia" class="work-thumbnail" src="https://attachments.academia-assets.com/41176457/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/20013585/A_combined_oxygen_and_silicon_diatom_isotope_record_of_Late_Quaternary_change_in_Lake_Elgygytgyn_North_East_Siberia">A combined oxygen and silicon diatom isotope record of Late Quaternary change in Lake El'gygytgyn, North East Siberia</a></div><div class="wp-workCard_item"><span>Quaternary Science Reviews</span><span>, 2010</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Determining the response of sites within the Arctic Circle to long-term climatic change remains a...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Determining the response of sites within the Arctic Circle to long-term climatic change remains an essential pre-requisite for assessing the susceptibility of these regions to future global warming and Arctic amplification. To date, existing records from North East Russia have demonstrated significant spatial variability across the region during the late Quaternary. Here we present diatom δ 18 O and δ 30 Si data from Lake El'gygytgyn, Russia, and suggest environmental changes that would have impacted across West Beringia from the Last Glacial Maximum to the modern day. In combination with other records, the results raise the potential for climatic teleconnections to exist between the region and sites in the North Atlantic.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="ede454d895ee8917bc454f0c7ceeac80" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":41176457,"asset_id":20013585,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/41176457/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="20013585"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="20013585"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 20013585; 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="20013584"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/20013584/Late_Quaternary_lake_level_changes_of_Lake_Elgygytgyn_NE_Siberia"><img alt="Research paper thumbnail of Late Quaternary lake-level changes of Lake El'gygytgyn, NE Siberia" class="work-thumbnail" src="https://attachments.academia-assets.com/41176305/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/20013584/Late_Quaternary_lake_level_changes_of_Lake_Elgygytgyn_NE_Siberia">Late Quaternary lake-level changes of Lake El'gygytgyn, NE Siberia</a></div><div class="wp-workCard_item wp-workCard--coauthors"><span>by </span><span><a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/OlafJuschus">Olaf Juschus</a> and <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/FedorovGrigory">Grigory Fedorov</a></span></div><div class="wp-workCard_item"><span>Quaternary Research</span><span>, 2011</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Lake El'gygytgyn is situated in a 3.6 Ma old impact crater in northeastern Siberia. Presented her...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Lake El'gygytgyn is situated in a 3.6 Ma old impact crater in northeastern Siberia. Presented here is a reconstruction of the Quaternary lake-level history as derived from sediment cores from the southern lake shelf. There, a cliff-like bench 10 m below the modern water level has been investigated. Deep-water sediments on the shelf indicate high lake levels during a warm Mid-Pleistocene period. One period with low lake level prior to Marine Oxygen Isotope Stage (MIS) 3 has been identified, followed by a period of high lake level (10 m above present). In the course of MIS 2 the lake level dropped to − 10 m. At the end of MIS 2 the bench was formed and coarse beach sedimentation occurred. Subsequently, the lake level rose rapidly to the Holocene level. Changes in water level are likely linked to climate variability. During relatively temperate periods the lake becomes free of ice in summer. Strong wave actions transport sediment parallel to the coast and towards the outlet, where the material tends to accumulate, resulting in lake level rise. During cold periods the perennial lake ice cover hampers any wave activity and pebble-transport, keeping the outlet open and causing the lake level to drop.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="9af88e485066dff8f4affd351ae3a7d5" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":41176305,"asset_id":20013584,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/41176305/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="20013584"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="20013584"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 20013584; 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="20013583"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/20013583/Applying_SAR_IRSL_methodology_for_dating_fine_grained_sediments_from_Lake_El_gygytgyn_north_eastern_Siberia"><img alt="Research paper thumbnail of Applying SAR-IRSL methodology for dating fine-grained sediments from Lake El’gygytgyn, north-eastern Siberia" class="work-thumbnail" src="https://attachments.academia-assets.com/41176291/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/20013583/Applying_SAR_IRSL_methodology_for_dating_fine_grained_sediments_from_Lake_El_gygytgyn_north_eastern_Siberia">Applying SAR-IRSL methodology for dating fine-grained sediments from Lake El’gygytgyn, north-eastern Siberia</a></div><div class="wp-workCard_item"><span>Quaternary Geochronology</span><span>, 2007</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Lake El'gygytgyn is situated in a 3.6 Ma old impact crater in north-eastern Siberia and probably ...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Lake El'gygytgyn is situated in a 3.6 Ma old impact crater in north-eastern Siberia and probably represents one of the most complete archives of Arctic climate change. Investigated here is the potential of infra-red stimulated luminescence (IRSL) using the single-aliquot regenerative-dose (SAR) approach for dating sediments from this lake. Independent age control is available from a published age model of a parallel core that is based on tuning sediment proxies with regional insolation and the results of previous multiple aliquot IRSL dating. Although the site is located within volcanic bedrock, anomalous fading seems to have little effect on the calculated ages. The modelled water content for the entire time of burial is seen as the most prominent uncertainty at this particular site. Despite these potential error sources, SAR-IRSL ages are in acceptable agreement with the given timeframe and clearly point to the possibility to establish independent chronologies at this site up to at least 400,000 years. r</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="edb9f44d473bef2c519805b56b269238" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":41176291,"asset_id":20013583,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/41176291/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="20013583"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="20013583"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 20013583; 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="20013582"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/20013582/Climatic_variability_during_the_last_interglacial_inferred_from_geochemical_proxies_in_the_Lake_Elgygytgyn_sediment_record"><img alt="Research paper thumbnail of Climatic variability during the last interglacial inferred from geochemical proxies in the Lake El'gygytgyn sediment record" class="work-thumbnail" src="https://attachments.academia-assets.com/41177027/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/20013582/Climatic_variability_during_the_last_interglacial_inferred_from_geochemical_proxies_in_the_Lake_Elgygytgyn_sediment_record">Climatic variability during the last interglacial inferred from geochemical proxies in the Lake El'gygytgyn sediment record</a></div><div class="wp-workCard_item wp-workCard--coauthors"><span>by </span><span><a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/OlafJuschus">Olaf Juschus</a> and <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/LauraCunningham1">Laura Cunningham</a></span></div><div class="wp-workCard_item"><span>Palaeogeography, Palaeoclimatology, Palaeoecology</span><span>, 2013</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The Last Interglacial Period (LIP) is often regarded as a good analogue for potential climatic co...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">The Last Interglacial Period (LIP) is often regarded as a good analogue for potential climatic conditions under predicted global warming scenarios. Despite this, there is still debate over the nature, duration and frequency of climatic changes during this period. One particularly contentious issue has been the apparent evidence of climatic instability identified in many marine cores but seemingly lacking from many terrestrial archives, especially within the Arctic, a key region for global climate change research. In this paper, geochemical records from Lake El'gygytgyn, north-eastern Russia, are used to infer past climatic changes during the LIP from within the high Arctic. With a sampling resolution of~20-~90 years, these records offer the potential for detailed, high-resolution palaeoclimate reconstruction. This study shows that the LIP commenced in central Chukotkã 129 thousand years ago (ka), with the warmest climatic conditions occurring between~128 and 127 ka before being interrupted by a short-lived cold reversal. Mild climatic conditions then persisted until~122 ka when a marked reduction in the sedimentation rate suggests a decrease in precipitation. A further climatic deterioration at~118 ka marks the return to glacial conditions. This study highlights the value of incorporating several geochemical proxies when inferring past climatic conditions, thus providing the potential to identify signals related to environmental change within the catchment. We also demonstrate the importance of considering how changes in sedimentation rate influence proxy records, in order to develop robust palaeoenvironmental reconstructions.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="c1ddc5f67ee49526713b1faabec422f9" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":41177027,"asset_id":20013582,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/41177027/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="20013582"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="20013582"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 20013582; 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="20013581"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/20013581/Identification_of_a_widespread_Kamchatkan_tephra_A_middle_Pleistocene_tie_point_between_Arctic_and_Pacific_paleoclimatic_records"><img alt="Research paper thumbnail of Identification of a widespread Kamchatkan tephra: A middle Pleistocene tie-point between Arctic and Pacific paleoclimatic records" class="work-thumbnail" src="https://attachments.academia-assets.com/41176628/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/20013581/Identification_of_a_widespread_Kamchatkan_tephra_A_middle_Pleistocene_tie_point_between_Arctic_and_Pacific_paleoclimatic_records">Identification of a widespread Kamchatkan tephra: A middle Pleistocene tie-point between Arctic and Pacific paleoclimatic records</a></div><div class="wp-workCard_item"><span>Geophysical Research Letters</span><span>, 2013</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Very few age controls exist for Quaternary deposits over the vast territory of the East Russian 17</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="78026020a28541e8efa165271def7e24" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":41176628,"asset_id":20013581,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/41176628/download_file?s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="20013581"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="20013581"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 20013581; 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="2557038"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/2557038/Modern_sedimentation_patterns_in_Lake_El_gygytgyn_NE_Russia_derived_from_surface_sediment_and_inlet_streams_samples"><img alt="Research paper thumbnail of Modern sedimentation patterns in Lake El’gygytgyn, NE Russia, derived from surface sediment and inlet streams samples" class="work-thumbnail" src="https://attachments.academia-assets.com/30569893/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/2557038/Modern_sedimentation_patterns_in_Lake_El_gygytgyn_NE_Russia_derived_from_surface_sediment_and_inlet_streams_samples">Modern sedimentation patterns in Lake El’gygytgyn, NE Russia, derived from surface sediment and inlet streams samples</a></div><div class="wp-workCard_item wp-workCard--coauthors"><span>by </span><span><a class="" data-click-track="profile-work-strip-authors" href="https://uni-koeln.academia.edu/VolkerWennrich">Volker Wennrich</a>, <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/OlafJuschus">Olaf Juschus</a>, and <a class="" data-click-track="profile-work-strip-authors" href="https://independent.academia.edu/PavelMinyuk">Pavel Minyuk</a></span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Lake El'gygytgyn/NE Russia holds a continuous 3.58 Ma sediment record, which is regarded as the m...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">Lake El'gygytgyn/NE Russia holds a continuous 3.58 Ma sediment record, which is regarded as the most longlasting climate archive of the terrestrial Arctic. Based on multi-proxy geochemical, mineralogical, and granulometric analyses of surface sediment, inlet stream and bedrock samples, supplemented by statistical methods, major processes influencing the modern sedimentation in the lake were investigated. Grain-size parameters and chemical elements linked to the input of feldspars from acidic bedrock indicate a windinduced two-cell current system as major driver of sediment transport and accumulation processes in Lake El'gygytgyn. The distribution of mafic rock related elements in the sediment on the lake floor can be traced back to the input of weathering products of basaltic rocks in the catchment. Obvious similarities in the spatial variability of manganese and heavy metals indicate sorption or co-precipitation of these elements with Fe and Mn hydroxides and oxides. But the similar distribution of organic matter and clay contents might also point to a fixation to organic components and clay minerals. An enrichment of mercury in the inlet streams might be indicative of neotectonic activity around the lake. The results of this study add to the fundamental knowledge of the modern lake processes of Lake El'gygytgyn and its lakecatchment interactions, and thus, yield crucial insights for the interpretation of paleo-data from this unique archive. , 2013 <a href="http://www.clim-past.net/9/135/2013/" rel="nofollow">www.clim-past.net/9/135/2013/</a> <a href="http://www.clim-past.net/9/135/2013/" rel="nofollow">www.clim-past.net/9/135/2013/</a> Clim. Past, 9, 135-148, 2013 Clim. 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