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class="affiliations-container fake-truncate js-profile-affiliations"><div><a class="u-tcGrayDarker" href="https://uni-muenster.academia.edu/">University of Münster</a>, <a class="u-tcGrayDarker" href="https://uni-muenster.academia.edu/Departments/Institute_of_Landscape_Ecology/Documents">Institute of Landscape Ecology</a>, <span class="u-tcGrayDarker">Faculty Member</span></div></div></div></div><div class="sidebar-cta-container"><button class="ds2-5-button hidden profile-cta-button grow js-profile-follow-button" data-broccoli-component="user-info.follow-button" data-click-track="profile-user-info-follow-button" data-follow-user-fname="Klaus-Holger" data-follow-user-id="195561" data-follow-user-source="profile_button" data-has-google="false"><span class="material-symbols-outlined" style="font-size: 20px" translate="no">add</span>Follow</button><button class="ds2-5-button hidden profile-cta-button grow js-profile-unfollow-button" data-broccoli-component="user-info.unfollow-button" 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class="stat-container"><p class="label"><span class="js-profile-total-view-text">Public Views</span></p><p class="data"><span class="js-profile-view-count"></span></p></div></span></div><div class="user-bio-container"><div class="profile-bio fake-truncate js-profile-about" style="margin: 0px;">I am a peatland biogeochemist, focusing on anaerobic carbon mineralization, redox processes, organic matter, and the coupling of biogeochemistry with hydrology.<br /><span class="u-fw700">Phone: </span>+49-251-8330207<br /><b>Address: </b>Institute for Landscape Ecology <br />Hydrology Group <br />Heisenbergstr. 2 <br />48149 Münster <br />Germany<br /><div class="js-profile-less-about u-linkUnstyled u-tcGrayDarker u-textDecorationUnderline u-displayNone">less</div></div></div><div class="suggested-academics-container"><div class="suggested-academics--header"><p class="ds2-5-body-md-bold">Related Authors</p></div><ul class="suggested-user-card-list"><div class="suggested-user-card"><div 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deduced from calcareous lake deposits" 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/63440828/Late_Holocene_periods_of_copper_mining_in_the_Eisenerz_Alps_Austria_deduced_from_calcareous_lake_deposits">Late Holocene periods of copper mining in the Eisenerz Alps (Austria) deduced from calcareous lake deposits</a></div><div class="wp-workCard_item"><span>Anthropocene</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="63440828"><a 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data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/59238795/Methane_Production_Rate_during_Anoxic_Litter_Decomposition_Depends_on_Si_Mass_Fractions_Nutrient_Stoichiometry_and_Carbon_Quality"><img alt="Research paper thumbnail of Methane Production Rate during Anoxic Litter Decomposition Depends on Si Mass Fractions, Nutrient Stoichiometry, and Carbon Quality" class="work-thumbnail" src="https://attachments.academia-assets.com/73263894/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/59238795/Methane_Production_Rate_during_Anoxic_Litter_Decomposition_Depends_on_Si_Mass_Fractions_Nutrient_Stoichiometry_and_Carbon_Quality">Methane Production Rate during Anoxic Litter Decomposition Depends on Si Mass Fractions, Nutrient Stoichiometry, and Carbon Quality</a></div><div class="wp-workCard_item"><span>Plants</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">While Si influences nutrient stoichiometry and decomposition of graminoid litter, it is still unc...</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">While Si influences nutrient stoichiometry and decomposition of graminoid litter, it is still unclear how Si influences anoxic litter decomposition and CH4 formation in graminoid dominated fen peatlands. First, Eriophorum vaginatum plants were grown under different Si and P availabilities, then shoots and roots were characterized regarding their proportions of C, Si, N and P and regarding C quality. Subsequently the Eriophorum shoots were subjected to anoxic decomposition. We hypothesized; that (I) litter grown under high Si availability would show a higher Si but lower nutrient mass fractions and a lower share of recalcitrant carbon moieties; (II) high-Si litter would show higher CH4 and CO2 production rates during anoxic decomposition; (III) methanogenesis would occur earlier in less recalcitrant high-Si litter, compared to low-Si litter. We found a higher Si mass fraction that coincides with a general decrease in C and N mass fractions and decreased share of recalcitrant organic ...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="f0ad735426356b1b99c0e990932c75ee" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":73263894,"asset_id":59238795,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/73263894/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="59238795"><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="59238795"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 59238795; 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</script> <div class="js-work-strip profile--work_container" data-work-id="59238791"><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/59238791/Anthropogenic_and_climate_signals_in_late_Holocene_peat_layers_of_an_ombrotrophic_bog_in_the_Styrian_Enns_valley_Austrian_Alps_"><img alt="Research paper thumbnail of Anthropogenic and climate signals in late-Holocene peat layers of an ombrotrophic bog in the Styrian Enns valley (Austrian Alps)" class="work-thumbnail" src="https://attachments.academia-assets.com/73263888/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/59238791/Anthropogenic_and_climate_signals_in_late_Holocene_peat_layers_of_an_ombrotrophic_bog_in_the_Styrian_Enns_valley_Austrian_Alps_">Anthropogenic and climate signals in late-Holocene peat layers of an ombrotrophic bog in the Styrian Enns valley (Austrian Alps)</a></div><div class="wp-workCard_item"><span>E&amp;G Quaternary Science Journal</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Using peat bogs as palaeoenvironmental archives is a well-established practice for reconstructing...</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">Using peat bogs as palaeoenvironmental archives is a well-established practice for reconstructing changing climate and anthropogenic activity in the past. In this paper, we present multi-proxy analyses (element geochemistry, pollen, non-pollen palynomorphs, stable Pb isotopes, humification, ash content) of a 500 cm long, 14 C-dated peat core covering the past ∼ 5000 years from the ombrotrophic Pürgschachen Moor in the Styrian Enns valley (Austrian Alps). Early indications of low settlement and agricultural activity date to ∼ 2900 cal BCE. An early enrichment of Cu was found in peat layers corresponding to the late Copper Age (∼ 2500 cal BCE). These enrichments are attributed to Cu mining activities in the Eisenerz Alps. More pronounced increases in cultural indicators (cultivated plants, shrubs, herbs, charcoal) in the pollen record and enrichments of trace metals suggest significant human impact in the vicinity of Pürgschachen Moor in the middle Bronze Age (∼ 1450-1250 cal BCE), in the late Bronze Age (∼ 1050-800 cal BCE) and in the period of the late La Tène culture (∼ 300 cal BCE-1 cal CE). The greater part of the Iron Age and the Roman imperial period are each characterized by a general decline in anthropogenic indicators compared to previous periods. Distinct enrichments of Pb and Sb in the sample that corresponds to ∼ 900 cal CE are attributed to medieval siderite mining activity in the immediate vicinity of Pürgschachen Moor. The results of this interdisciplinary study provide evidence that strong, climate-controlled interrelations exist between the pollen record, the humification degree and the ash content in an ombrotrophic environment. Human activity, in contrast, is Published by Copernicus Publications on behalf of the Deutsche Quartärvereinigung (DEUQUA) e.V. 122 W. Knierzinger et al.: Anthropogenic and climate signals in peat layers mainly reflected in the pollen record and by enrichments of heavy metals. The study indicates a dry period in the region of the bog around ∼ 1950 cal BCE. Kurzfassung: Hochmoore eignen sich zur Rekonstruktion des Paläoklimas und anthropogener Aktivität in der Vergangenheit. In der vorliegenden Arbeit werden Multiproxy-Analysen (Elementchemie, Pollen, Mikrofossilien, stabile Pb-Isotope, Humifizierung, Aschegehalt) eines 500 cm langen und mittels der C-14-Methode datierten Torfkerns aus dem ombrotrophen Pürgschachener Moor im steirischen Ennstal (Österreichische Alpen) vorgelegt und diskutiert. Der Bohrkern umfasst einen Zeitraum von ∼ 5000 Jahren. Frühe Hinweise auf Besiedelung und landwirtschaftliche Nutzung datieren auf ∼ 2900 cal BCE. Erste markante Cu-Anreicherungen, die auf Cu-Bergbau in den angrenzenden Eisenerzer Alpen zurückgeführt werden, zeigen sich in Torfschichten aus der späten Kupfersteinzeit (∼ 2500 cal BCE). Deutlichere Zunahmen von Kulturindikatoren (Kulturpflanzen, Sträucher, Kräuter, Holzkohle) im Pollendiagram und Anreicherungen von Spurenmetallen lassen auf signifikanten menschlichen Einfluss in der Umgebung des Pürgschachener Moores in der Mittelbronzezeit (∼ 1450-1250 cal BCE), in der Spätbronzezeit und (∼ 1050-800 cal BCE) sowie in der Periode der späten Latènezeit (∼ 300 cal BCE-1 cal CE) schließen. Der größte Teil der Eisenzeit sowie die römische Kaiserzeit sind durch einen allgemeinen Rückgang von anthropogenen Indikatoren im Vergleich zu früheren Perioden gekennzeichnet. Anreicherungen von Pb und Sb in einer Torfprobe aus dem Mittelalter (∼ 900 cal CE) können mit Sideritabbau in unmittelbarer Nähe des Pürgschachener Moores in Verbindung gebracht werden. Die Ergebnisse dieser interdisziplinären Studie belegen starke klimagesteuerte Wechselbeziehungen zwischen Pollen, dem Humifizierungsgrad und dem Aschegehalt. Menschliche Aktivität in der Umgebung des Moores zeigt eine geringe Korrelation mit Humifizierung und Aschegehalt, findet allerdings stärkeren Niederschlag in den Pollen-und Schwermetalldaten. Die vorliegende Studie weist auf eine ausgedehnte Trockenperiode in der Umgebung des Pürgschachener Moors um ∼ 1950 cal BCE hin.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="13888fe3005e676bf312e58f3d8f780e" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":73263888,"asset_id":59238791,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/73263888/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="59238791"><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="59238791"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 59238791; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=59238791]").text(description); $(".js-view-count[data-work-id=59238791]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 59238791; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='59238791']"); 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 (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "13888fe3005e676bf312e58f3d8f780e" } } $('.js-work-strip[data-work-id=59238791]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":59238791,"title":"Anthropogenic and climate signals in late-Holocene peat layers of an ombrotrophic bog in the Styrian Enns valley (Austrian Alps)","translated_title":"","metadata":{"publisher":"Copernicus GmbH","grobid_abstract":"Using peat bogs as palaeoenvironmental archives is a well-established practice for reconstructing changing climate and anthropogenic activity in the past. In this paper, we present multi-proxy analyses (element geochemistry, pollen, non-pollen palynomorphs, stable Pb isotopes, humification, ash content) of a 500 cm long, 14 C-dated peat core covering the past ∼ 5000 years from the ombrotrophic Pürgschachen Moor in the Styrian Enns valley (Austrian Alps). Early indications of low settlement and agricultural activity date to ∼ 2900 cal BCE. An early enrichment of Cu was found in peat layers corresponding to the late Copper Age (∼ 2500 cal BCE). These enrichments are attributed to Cu mining activities in the Eisenerz Alps. More pronounced increases in cultural indicators (cultivated plants, shrubs, herbs, charcoal) in the pollen record and enrichments of trace metals suggest significant human impact in the vicinity of Pürgschachen Moor in the middle Bronze Age (∼ 1450-1250 cal BCE), in the late Bronze Age (∼ 1050-800 cal BCE) and in the period of the late La Tène culture (∼ 300 cal BCE-1 cal CE). The greater part of the Iron Age and the Roman imperial period are each characterized by a general decline in anthropogenic indicators compared to previous periods. Distinct enrichments of Pb and Sb in the sample that corresponds to ∼ 900 cal CE are attributed to medieval siderite mining activity in the immediate vicinity of Pürgschachen Moor. The results of this interdisciplinary study provide evidence that strong, climate-controlled interrelations exist between the pollen record, the humification degree and the ash content in an ombrotrophic environment. Human activity, in contrast, is Published by Copernicus Publications on behalf of the Deutsche Quartärvereinigung (DEUQUA) e.V. 122 W. Knierzinger et al.: Anthropogenic and climate signals in peat layers mainly reflected in the pollen record and by enrichments of heavy metals. The study indicates a dry period in the region of the bog around ∼ 1950 cal BCE. Kurzfassung: Hochmoore eignen sich zur Rekonstruktion des Paläoklimas und anthropogener Aktivität in der Vergangenheit. In der vorliegenden Arbeit werden Multiproxy-Analysen (Elementchemie, Pollen, Mikrofossilien, stabile Pb-Isotope, Humifizierung, Aschegehalt) eines 500 cm langen und mittels der C-14-Methode datierten Torfkerns aus dem ombrotrophen Pürgschachener Moor im steirischen Ennstal (Österreichische Alpen) vorgelegt und diskutiert. Der Bohrkern umfasst einen Zeitraum von ∼ 5000 Jahren. Frühe Hinweise auf Besiedelung und landwirtschaftliche Nutzung datieren auf ∼ 2900 cal BCE. Erste markante Cu-Anreicherungen, die auf Cu-Bergbau in den angrenzenden Eisenerzer Alpen zurückgeführt werden, zeigen sich in Torfschichten aus der späten Kupfersteinzeit (∼ 2500 cal BCE). Deutlichere Zunahmen von Kulturindikatoren (Kulturpflanzen, Sträucher, Kräuter, Holzkohle) im Pollendiagram und Anreicherungen von Spurenmetallen lassen auf signifikanten menschlichen Einfluss in der Umgebung des Pürgschachener Moores in der Mittelbronzezeit (∼ 1450-1250 cal BCE), in der Spätbronzezeit und (∼ 1050-800 cal BCE) sowie in der Periode der späten Latènezeit (∼ 300 cal BCE-1 cal CE) schließen. Der größte Teil der Eisenzeit sowie die römische Kaiserzeit sind durch einen allgemeinen Rückgang von anthropogenen Indikatoren im Vergleich zu früheren Perioden gekennzeichnet. Anreicherungen von Pb und Sb in einer Torfprobe aus dem Mittelalter (∼ 900 cal CE) können mit Sideritabbau in unmittelbarer Nähe des Pürgschachener Moores in Verbindung gebracht werden. Die Ergebnisse dieser interdisziplinären Studie belegen starke klimagesteuerte Wechselbeziehungen zwischen Pollen, dem Humifizierungsgrad und dem Aschegehalt. Menschliche Aktivität in der Umgebung des Moores zeigt eine geringe Korrelation mit Humifizierung und Aschegehalt, findet allerdings stärkeren Niederschlag in den Pollen-und Schwermetalldaten. 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The greater part of the Iron Age and the Roman imperial period are each characterized by a general decline in anthropogenic indicators compared to previous periods. Distinct enrichments of Pb and Sb in the sample that corresponds to ∼ 900 cal CE are attributed to medieval siderite mining activity in the immediate vicinity of Pürgschachen Moor. The results of this interdisciplinary study provide evidence that strong, climate-controlled interrelations exist between the pollen record, the humification degree and the ash content in an ombrotrophic environment. Human activity, in contrast, is Published by Copernicus Publications on behalf of the Deutsche Quartärvereinigung (DEUQUA) e.V. 122 W. Knierzinger et al.: Anthropogenic and climate signals in peat layers mainly reflected in the pollen record and by enrichments of heavy metals. The study indicates a dry period in the region of the bog around ∼ 1950 cal BCE. Kurzfassung: Hochmoore eignen sich zur Rekonstruktion des Paläoklimas und anthropogener Aktivität in der Vergangenheit. In der vorliegenden Arbeit werden Multiproxy-Analysen (Elementchemie, Pollen, Mikrofossilien, stabile Pb-Isotope, Humifizierung, Aschegehalt) eines 500 cm langen und mittels der C-14-Methode datierten Torfkerns aus dem ombrotrophen Pürgschachener Moor im steirischen Ennstal (Österreichische Alpen) vorgelegt und diskutiert. Der Bohrkern umfasst einen Zeitraum von ∼ 5000 Jahren. Frühe Hinweise auf Besiedelung und landwirtschaftliche Nutzung datieren auf ∼ 2900 cal BCE. Erste markante Cu-Anreicherungen, die auf Cu-Bergbau in den angrenzenden Eisenerzer Alpen zurückgeführt werden, zeigen sich in Torfschichten aus der späten Kupfersteinzeit (∼ 2500 cal BCE). Deutlichere Zunahmen von Kulturindikatoren (Kulturpflanzen, Sträucher, Kräuter, Holzkohle) im Pollendiagram und Anreicherungen von Spurenmetallen lassen auf signifikanten menschlichen Einfluss in der Umgebung des Pürgschachener Moores in der Mittelbronzezeit (∼ 1450-1250 cal BCE), in der Spätbronzezeit und (∼ 1050-800 cal BCE) sowie in der Periode der späten Latènezeit (∼ 300 cal BCE-1 cal CE) schließen. Der größte Teil der Eisenzeit sowie die römische Kaiserzeit sind durch einen allgemeinen Rückgang von anthropogenen Indikatoren im Vergleich zu früheren Perioden gekennzeichnet. Anreicherungen von Pb und Sb in einer Torfprobe aus dem Mittelalter (∼ 900 cal CE) können mit Sideritabbau in unmittelbarer Nähe des Pürgschachener Moores in Verbindung gebracht werden. Die Ergebnisse dieser interdisziplinären Studie belegen starke klimagesteuerte Wechselbeziehungen zwischen Pollen, dem Humifizierungsgrad und dem Aschegehalt. Menschliche Aktivität in der Umgebung des Moores zeigt eine geringe Korrelation mit Humifizierung und Aschegehalt, findet allerdings stärkeren Niederschlag in den Pollen-und Schwermetalldaten. 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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=59232875]").text(description); $(".js-view-count[data-work-id=59232875]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 59232875; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='59232875']"); 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" } } $('.js-work-strip[data-work-id=59232875]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":59232875,"title":"Effect of Reduced Sulfur Species on Chemolithoautotrophic Pyrite Oxidation with Nitrate","internal_url":"https://www.academia.edu/59232875/Effect_of_Reduced_Sulfur_Species_on_Chemolithoautotrophic_Pyrite_Oxidation_with_Nitrate","owner_id":195561,"coauthors_can_edit":true,"owner":{"id":195561,"first_name":"Klaus-Holger","middle_initials":null,"last_name":"Knorr","page_name":"KlausHolgerKnorr","domain_name":"uni-muenster","created_at":"2010-06-01T01:48:47.579-07:00","display_name":"Klaus-Holger Knorr","url":"https://uni-muenster.academia.edu/KlausHolgerKnorr"},"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="51343514"><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/51343514/Multi_proxy_analyses_of_a_minerotrophic_fen_to_reconstruct_prehistoric_periods_of_human_activity_associated_with_salt_mining_in_the_Hallstatt_region_Austria"><img alt="Research paper thumbnail of Multi-proxy analyses of a minerotrophic fen to reconstruct prehistoric periods of human activity associated with salt mining in the Hallstatt region (Austria" 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/51343514/Multi_proxy_analyses_of_a_minerotrophic_fen_to_reconstruct_prehistoric_periods_of_human_activity_associated_with_salt_mining_in_the_Hallstatt_region_Austria">Multi-proxy analyses of a minerotrophic fen to reconstruct prehistoric periods of human activity associated with salt mining in the Hallstatt region (Austria</a></div><div class="wp-workCard_item"><span>Journal of Archaeological Science: Reports</span><span>, 2021</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">In this study, periods of prehistoric anthropogenic activity in the Hallstatt salt mining area (U...</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">In this study, periods of prehistoric anthropogenic activity in the Hallstatt salt mining area (Upper Austria) are reconstructed from elemental (XRF-scanning, Q-ICP-MS) and Pb isotopic analyses (206 Pb, 207 Pb, 208 Pb) of a radiocarbon-dated, 137-cm-long peat core covering the past ~7,000 years. The peat core was retrieved from a minerotrophic fen in the Hallstatt High Valley. Distinct metal enrichments attributed to low anthropogenic impact in Hallstatt can be traced back to a time around 2350 cal BCE and to another period around 1800 cal BCE. The period from the Late Bronze Age to the Early Iron Age (~1300 cal BCE to ~500 cal BCE) is characterised by increased anthropogenic activity. Relatively high Sn concentrations between ~1210 cal BCE and ~540 cal BCE) point towards intensive bronze casting processes, probably associated with the production of bronze picks that were used for local salt mining during this time. Intense human impact was also determined for the early Roman imperi...</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="51343514"><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="51343514"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 51343514; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=51343514]").text(description); $(".js-view-count[data-work-id=51343514]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 51343514; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='51343514']"); 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" } } $('.js-work-strip[data-work-id=51343514]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":51343514,"title":"Multi-proxy analyses of a minerotrophic fen to reconstruct prehistoric periods of human activity associated with salt mining in the Hallstatt region (Austria","internal_url":"https://www.academia.edu/51343514/Multi_proxy_analyses_of_a_minerotrophic_fen_to_reconstruct_prehistoric_periods_of_human_activity_associated_with_salt_mining_in_the_Hallstatt_region_Austria","owner_id":195561,"coauthors_can_edit":true,"owner":{"id":195561,"first_name":"Klaus-Holger","middle_initials":null,"last_name":"Knorr","page_name":"KlausHolgerKnorr","domain_name":"uni-muenster","created_at":"2010-06-01T01:48:47.579-07:00","display_name":"Klaus-Holger Knorr","url":"https://uni-muenster.academia.edu/KlausHolgerKnorr"},"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="46000396"><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/46000396/Can_we_expect_pristine_mountain_peatland_ecosystems_in_Central_Europe_Evidence_from_multi_proxy_palaeoecological_studies_on_the_Holocene_peatland_development"><img alt="Research paper thumbnail of Can we expect pristine mountain peatland ecosystems in Central Europe? Evidence from multi-proxy palaeoecological studies on the Holocene peatland development" 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/46000396/Can_we_expect_pristine_mountain_peatland_ecosystems_in_Central_Europe_Evidence_from_multi_proxy_palaeoecological_studies_on_the_Holocene_peatland_development">Can we expect pristine mountain peatland ecosystems in Central Europe? Evidence from multi-proxy palaeoecological studies on the Holocene peatland development</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="46000396"><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="46000396"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 46000396; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=46000396]").text(description); $(".js-view-count[data-work-id=46000396]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 46000396; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='46000396']"); 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" } } $('.js-work-strip[data-work-id=46000396]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":46000396,"title":"Can we expect pristine mountain peatland ecosystems in Central Europe? Evidence from multi-proxy palaeoecological studies on the Holocene peatland development","internal_url":"https://www.academia.edu/46000396/Can_we_expect_pristine_mountain_peatland_ecosystems_in_Central_Europe_Evidence_from_multi_proxy_palaeoecological_studies_on_the_Holocene_peatland_development","owner_id":195561,"coauthors_can_edit":true,"owner":{"id":195561,"first_name":"Klaus-Holger","middle_initials":null,"last_name":"Knorr","page_name":"KlausHolgerKnorr","domain_name":"uni-muenster","created_at":"2010-06-01T01:48:47.579-07:00","display_name":"Klaus-Holger Knorr","url":"https://uni-muenster.academia.edu/KlausHolgerKnorr"},"attachments":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="46000393"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/46000393/Evaluating_biogeochemical_indicators_of_methanogenic_conditions_and_thermodynamic_constraints_in_peat"><img alt="Research paper thumbnail of Evaluating biogeochemical indicators of methanogenic conditions and thermodynamic constraints in peat" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/46000393/Evaluating_biogeochemical_indicators_of_methanogenic_conditions_and_thermodynamic_constraints_in_peat">Evaluating biogeochemical indicators of methanogenic conditions and thermodynamic constraints in peat</a></div><div class="wp-workCard_item"><span>Applied Geochemistry</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="46000393"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="46000393"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 46000393; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=46000393]").text(description); $(".js-view-count[data-work-id=46000393]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 46000393; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='46000393']"); 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); 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</script> <div class="js-work-strip profile--work_container" data-work-id="46000390"><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/46000390/Methane_Gas_Emission_from_an_Artificial_Reservoir_under_Asian_Monsoon_Climate_Conditions_with_a_Focus_on_the_Ebullition_Pathway"><img alt="Research paper thumbnail of Methane Gas Emission from an Artificial Reservoir under Asian Monsoon Climate Conditions, with a Focus on the Ebullition Pathway" 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/46000390/Methane_Gas_Emission_from_an_Artificial_Reservoir_under_Asian_Monsoon_Climate_Conditions_with_a_Focus_on_the_Ebullition_Pathway">Methane Gas Emission from an Artificial Reservoir under Asian Monsoon Climate Conditions, with a Focus on the Ebullition Pathway</a></div><div class="wp-workCard_item"><span>Korean Journal of Ecology and Environment</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="46000390"><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="46000390"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 46000390; 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$(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="46000374"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/46000374/Plant_rhizosphere_oxidation_reduces_methane_production_and_emission_in_rewetted_peatlands"><img alt="Research paper thumbnail of Plant rhizosphere oxidation reduces methane production and emission in rewetted peatlands" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/46000374/Plant_rhizosphere_oxidation_reduces_methane_production_and_emission_in_rewetted_peatlands">Plant rhizosphere oxidation reduces methane production and emission in rewetted peatlands</a></div><div class="wp-workCard_item"><span>Soil Biology and Biochemistry</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="46000374"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="46000374"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 46000374; 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</script> <div class="js-work-strip profile--work_container" data-work-id="59238795"><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/59238795/Methane_Production_Rate_during_Anoxic_Litter_Decomposition_Depends_on_Si_Mass_Fractions_Nutrient_Stoichiometry_and_Carbon_Quality"><img alt="Research paper thumbnail of Methane Production Rate during Anoxic Litter Decomposition Depends on Si Mass Fractions, Nutrient Stoichiometry, and Carbon Quality" class="work-thumbnail" src="https://attachments.academia-assets.com/73263894/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/59238795/Methane_Production_Rate_during_Anoxic_Litter_Decomposition_Depends_on_Si_Mass_Fractions_Nutrient_Stoichiometry_and_Carbon_Quality">Methane Production Rate during Anoxic Litter Decomposition Depends on Si Mass Fractions, Nutrient Stoichiometry, and Carbon Quality</a></div><div class="wp-workCard_item"><span>Plants</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">While Si influences nutrient stoichiometry and decomposition of graminoid litter, it is still unc...</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">While Si influences nutrient stoichiometry and decomposition of graminoid litter, it is still unclear how Si influences anoxic litter decomposition and CH4 formation in graminoid dominated fen peatlands. First, Eriophorum vaginatum plants were grown under different Si and P availabilities, then shoots and roots were characterized regarding their proportions of C, Si, N and P and regarding C quality. Subsequently the Eriophorum shoots were subjected to anoxic decomposition. We hypothesized; that (I) litter grown under high Si availability would show a higher Si but lower nutrient mass fractions and a lower share of recalcitrant carbon moieties; (II) high-Si litter would show higher CH4 and CO2 production rates during anoxic decomposition; (III) methanogenesis would occur earlier in less recalcitrant high-Si litter, compared to low-Si litter. We found a higher Si mass fraction that coincides with a general decrease in C and N mass fractions and decreased share of recalcitrant organic ...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="f0ad735426356b1b99c0e990932c75ee" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":73263894,"asset_id":59238795,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/73263894/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="59238795"><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="59238795"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 59238795; 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$a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="59238792"><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/59238792/A_novel_belowground_in_situ_gas_labeling_approach_CH4_oxidation_in_deep_peat_using_passive_diffusion_chambers_and_13C_excess"><img alt="Research paper thumbnail of A novel belowground in-situ gas labeling approach: CH4 oxidation in deep peat using passive diffusion chambers and 13C excess" 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/59238792/A_novel_belowground_in_situ_gas_labeling_approach_CH4_oxidation_in_deep_peat_using_passive_diffusion_chambers_and_13C_excess">A novel belowground in-situ gas labeling approach: CH4 oxidation in deep peat using passive diffusion chambers and 13C excess</a></div><div class="wp-workCard_item"><span>Science of The Total Environment</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="59238792"><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="59238792"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 59238792; 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</script> <div class="js-work-strip profile--work_container" data-work-id="59238791"><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/59238791/Anthropogenic_and_climate_signals_in_late_Holocene_peat_layers_of_an_ombrotrophic_bog_in_the_Styrian_Enns_valley_Austrian_Alps_"><img alt="Research paper thumbnail of Anthropogenic and climate signals in late-Holocene peat layers of an ombrotrophic bog in the Styrian Enns valley (Austrian Alps)" class="work-thumbnail" src="https://attachments.academia-assets.com/73263888/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/59238791/Anthropogenic_and_climate_signals_in_late_Holocene_peat_layers_of_an_ombrotrophic_bog_in_the_Styrian_Enns_valley_Austrian_Alps_">Anthropogenic and climate signals in late-Holocene peat layers of an ombrotrophic bog in the Styrian Enns valley (Austrian Alps)</a></div><div class="wp-workCard_item"><span>E&amp;G Quaternary Science Journal</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">Using peat bogs as palaeoenvironmental archives is a well-established practice for reconstructing...</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">Using peat bogs as palaeoenvironmental archives is a well-established practice for reconstructing changing climate and anthropogenic activity in the past. In this paper, we present multi-proxy analyses (element geochemistry, pollen, non-pollen palynomorphs, stable Pb isotopes, humification, ash content) of a 500 cm long, 14 C-dated peat core covering the past ∼ 5000 years from the ombrotrophic Pürgschachen Moor in the Styrian Enns valley (Austrian Alps). Early indications of low settlement and agricultural activity date to ∼ 2900 cal BCE. An early enrichment of Cu was found in peat layers corresponding to the late Copper Age (∼ 2500 cal BCE). These enrichments are attributed to Cu mining activities in the Eisenerz Alps. More pronounced increases in cultural indicators (cultivated plants, shrubs, herbs, charcoal) in the pollen record and enrichments of trace metals suggest significant human impact in the vicinity of Pürgschachen Moor in the middle Bronze Age (∼ 1450-1250 cal BCE), in the late Bronze Age (∼ 1050-800 cal BCE) and in the period of the late La Tène culture (∼ 300 cal BCE-1 cal CE). The greater part of the Iron Age and the Roman imperial period are each characterized by a general decline in anthropogenic indicators compared to previous periods. Distinct enrichments of Pb and Sb in the sample that corresponds to ∼ 900 cal CE are attributed to medieval siderite mining activity in the immediate vicinity of Pürgschachen Moor. The results of this interdisciplinary study provide evidence that strong, climate-controlled interrelations exist between the pollen record, the humification degree and the ash content in an ombrotrophic environment. Human activity, in contrast, is Published by Copernicus Publications on behalf of the Deutsche Quartärvereinigung (DEUQUA) e.V. 122 W. Knierzinger et al.: Anthropogenic and climate signals in peat layers mainly reflected in the pollen record and by enrichments of heavy metals. The study indicates a dry period in the region of the bog around ∼ 1950 cal BCE. Kurzfassung: Hochmoore eignen sich zur Rekonstruktion des Paläoklimas und anthropogener Aktivität in der Vergangenheit. In der vorliegenden Arbeit werden Multiproxy-Analysen (Elementchemie, Pollen, Mikrofossilien, stabile Pb-Isotope, Humifizierung, Aschegehalt) eines 500 cm langen und mittels der C-14-Methode datierten Torfkerns aus dem ombrotrophen Pürgschachener Moor im steirischen Ennstal (Österreichische Alpen) vorgelegt und diskutiert. Der Bohrkern umfasst einen Zeitraum von ∼ 5000 Jahren. Frühe Hinweise auf Besiedelung und landwirtschaftliche Nutzung datieren auf ∼ 2900 cal BCE. Erste markante Cu-Anreicherungen, die auf Cu-Bergbau in den angrenzenden Eisenerzer Alpen zurückgeführt werden, zeigen sich in Torfschichten aus der späten Kupfersteinzeit (∼ 2500 cal BCE). Deutlichere Zunahmen von Kulturindikatoren (Kulturpflanzen, Sträucher, Kräuter, Holzkohle) im Pollendiagram und Anreicherungen von Spurenmetallen lassen auf signifikanten menschlichen Einfluss in der Umgebung des Pürgschachener Moores in der Mittelbronzezeit (∼ 1450-1250 cal BCE), in der Spätbronzezeit und (∼ 1050-800 cal BCE) sowie in der Periode der späten Latènezeit (∼ 300 cal BCE-1 cal CE) schließen. Der größte Teil der Eisenzeit sowie die römische Kaiserzeit sind durch einen allgemeinen Rückgang von anthropogenen Indikatoren im Vergleich zu früheren Perioden gekennzeichnet. Anreicherungen von Pb und Sb in einer Torfprobe aus dem Mittelalter (∼ 900 cal CE) können mit Sideritabbau in unmittelbarer Nähe des Pürgschachener Moores in Verbindung gebracht werden. Die Ergebnisse dieser interdisziplinären Studie belegen starke klimagesteuerte Wechselbeziehungen zwischen Pollen, dem Humifizierungsgrad und dem Aschegehalt. Menschliche Aktivität in der Umgebung des Moores zeigt eine geringe Korrelation mit Humifizierung und Aschegehalt, findet allerdings stärkeren Niederschlag in den Pollen-und Schwermetalldaten. Die vorliegende Studie weist auf eine ausgedehnte Trockenperiode in der Umgebung des Pürgschachener Moors um ∼ 1950 cal BCE hin.</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="13888fe3005e676bf312e58f3d8f780e" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":73263888,"asset_id":59238791,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/73263888/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="59238791"><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="59238791"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 59238791; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=59238791]").text(description); $(".js-view-count[data-work-id=59238791]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 59238791; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='59238791']"); 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 (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "13888fe3005e676bf312e58f3d8f780e" } } $('.js-work-strip[data-work-id=59238791]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":59238791,"title":"Anthropogenic and climate signals in late-Holocene peat layers of an ombrotrophic bog in the Styrian Enns valley (Austrian Alps)","translated_title":"","metadata":{"publisher":"Copernicus GmbH","grobid_abstract":"Using peat bogs as palaeoenvironmental archives is a well-established practice for reconstructing changing climate and anthropogenic activity in the past. In this paper, we present multi-proxy analyses (element geochemistry, pollen, non-pollen palynomorphs, stable Pb isotopes, humification, ash content) of a 500 cm long, 14 C-dated peat core covering the past ∼ 5000 years from the ombrotrophic Pürgschachen Moor in the Styrian Enns valley (Austrian Alps). Early indications of low settlement and agricultural activity date to ∼ 2900 cal BCE. An early enrichment of Cu was found in peat layers corresponding to the late Copper Age (∼ 2500 cal BCE). These enrichments are attributed to Cu mining activities in the Eisenerz Alps. More pronounced increases in cultural indicators (cultivated plants, shrubs, herbs, charcoal) in the pollen record and enrichments of trace metals suggest significant human impact in the vicinity of Pürgschachen Moor in the middle Bronze Age (∼ 1450-1250 cal BCE), in the late Bronze Age (∼ 1050-800 cal BCE) and in the period of the late La Tène culture (∼ 300 cal BCE-1 cal CE). The greater part of the Iron Age and the Roman imperial period are each characterized by a general decline in anthropogenic indicators compared to previous periods. Distinct enrichments of Pb and Sb in the sample that corresponds to ∼ 900 cal CE are attributed to medieval siderite mining activity in the immediate vicinity of Pürgschachen Moor. The results of this interdisciplinary study provide evidence that strong, climate-controlled interrelations exist between the pollen record, the humification degree and the ash content in an ombrotrophic environment. Human activity, in contrast, is Published by Copernicus Publications on behalf of the Deutsche Quartärvereinigung (DEUQUA) e.V. 122 W. Knierzinger et al.: Anthropogenic and climate signals in peat layers mainly reflected in the pollen record and by enrichments of heavy metals. The study indicates a dry period in the region of the bog around ∼ 1950 cal BCE. Kurzfassung: Hochmoore eignen sich zur Rekonstruktion des Paläoklimas und anthropogener Aktivität in der Vergangenheit. In der vorliegenden Arbeit werden Multiproxy-Analysen (Elementchemie, Pollen, Mikrofossilien, stabile Pb-Isotope, Humifizierung, Aschegehalt) eines 500 cm langen und mittels der C-14-Methode datierten Torfkerns aus dem ombrotrophen Pürgschachener Moor im steirischen Ennstal (Österreichische Alpen) vorgelegt und diskutiert. Der Bohrkern umfasst einen Zeitraum von ∼ 5000 Jahren. Frühe Hinweise auf Besiedelung und landwirtschaftliche Nutzung datieren auf ∼ 2900 cal BCE. Erste markante Cu-Anreicherungen, die auf Cu-Bergbau in den angrenzenden Eisenerzer Alpen zurückgeführt werden, zeigen sich in Torfschichten aus der späten Kupfersteinzeit (∼ 2500 cal BCE). Deutlichere Zunahmen von Kulturindikatoren (Kulturpflanzen, Sträucher, Kräuter, Holzkohle) im Pollendiagram und Anreicherungen von Spurenmetallen lassen auf signifikanten menschlichen Einfluss in der Umgebung des Pürgschachener Moores in der Mittelbronzezeit (∼ 1450-1250 cal BCE), in der Spätbronzezeit und (∼ 1050-800 cal BCE) sowie in der Periode der späten Latènezeit (∼ 300 cal BCE-1 cal CE) schließen. Der größte Teil der Eisenzeit sowie die römische Kaiserzeit sind durch einen allgemeinen Rückgang von anthropogenen Indikatoren im Vergleich zu früheren Perioden gekennzeichnet. Anreicherungen von Pb und Sb in einer Torfprobe aus dem Mittelalter (∼ 900 cal CE) können mit Sideritabbau in unmittelbarer Nähe des Pürgschachener Moores in Verbindung gebracht werden. Die Ergebnisse dieser interdisziplinären Studie belegen starke klimagesteuerte Wechselbeziehungen zwischen Pollen, dem Humifizierungsgrad und dem Aschegehalt. Menschliche Aktivität in der Umgebung des Moores zeigt eine geringe Korrelation mit Humifizierung und Aschegehalt, findet allerdings stärkeren Niederschlag in den Pollen-und Schwermetalldaten. Die vorliegende Studie weist auf eine ausgedehnte Trockenperiode in der Umgebung des Pürgschachener Moors um ∼ 1950 cal BCE hin.","publication_name":"E\u0026amp;G Quaternary Science Journal","grobid_abstract_attachment_id":73263888},"translated_abstract":null,"internal_url":"https://www.academia.edu/59238791/Anthropogenic_and_climate_signals_in_late_Holocene_peat_layers_of_an_ombrotrophic_bog_in_the_Styrian_Enns_valley_Austrian_Alps_","translated_internal_url":"","created_at":"2021-10-21T00:33:35.169-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":195561,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":73263888,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/73263888/thumbnails/1.jpg","file_name":"egqsj-69-121-2020.pdf","download_url":"https://www.academia.edu/attachments/73263888/download_file","bulk_download_file_name":"Anthropogenic_and_climate_signals_in_lat.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/73263888/egqsj-69-121-2020-libre.pdf?1634802739=\u0026response-content-disposition=attachment%3B+filename%3DAnthropogenic_and_climate_signals_in_lat.pdf\u0026Expires=1738799875\u0026Signature=gJF8AmuIgKFVqRc9rAyIonca02LfQCzxletPoXYyO9x~UA99QXQ1MtzTQlyjzpxKSFsgfhMSu39RBpCsBVMKjg2dqmfJu9sAb4oBnj8DJXc1fEMl4PO4glA4w1eaxQiMSPYhXBNiCjYr52b0ZI5K9tNspkLb3jPDlcKUV4kE3Pqu6EQxPEJ7C5sPyV5x6BfKmYOX-Nc-YeaRKfyNbwhGIFHqhKX-Qw4GeSK5SYZcGSqf5p224hyQsHE~X2Z-oC3Q8Q7Iv9AWvIyNDM0ydqs0BX37YJKOuLZMAVcIuw1PoRezynqHmxYUXQ8-nrl0B~H~ZDThHSsgW31FV0HlhYO~YQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Anthropogenic_and_climate_signals_in_late_Holocene_peat_layers_of_an_ombrotrophic_bog_in_the_Styrian_Enns_valley_Austrian_Alps_","translated_slug":"","page_count":17,"language":"en","content_type":"Work","summary":"Using peat bogs as palaeoenvironmental archives is a well-established practice for reconstructing changing climate and anthropogenic activity in the past. In this paper, we present multi-proxy analyses (element geochemistry, pollen, non-pollen palynomorphs, stable Pb isotopes, humification, ash content) of a 500 cm long, 14 C-dated peat core covering the past ∼ 5000 years from the ombrotrophic Pürgschachen Moor in the Styrian Enns valley (Austrian Alps). Early indications of low settlement and agricultural activity date to ∼ 2900 cal BCE. An early enrichment of Cu was found in peat layers corresponding to the late Copper Age (∼ 2500 cal BCE). These enrichments are attributed to Cu mining activities in the Eisenerz Alps. More pronounced increases in cultural indicators (cultivated plants, shrubs, herbs, charcoal) in the pollen record and enrichments of trace metals suggest significant human impact in the vicinity of Pürgschachen Moor in the middle Bronze Age (∼ 1450-1250 cal BCE), in the late Bronze Age (∼ 1050-800 cal BCE) and in the period of the late La Tène culture (∼ 300 cal BCE-1 cal CE). The greater part of the Iron Age and the Roman imperial period are each characterized by a general decline in anthropogenic indicators compared to previous periods. Distinct enrichments of Pb and Sb in the sample that corresponds to ∼ 900 cal CE are attributed to medieval siderite mining activity in the immediate vicinity of Pürgschachen Moor. The results of this interdisciplinary study provide evidence that strong, climate-controlled interrelations exist between the pollen record, the humification degree and the ash content in an ombrotrophic environment. Human activity, in contrast, is Published by Copernicus Publications on behalf of the Deutsche Quartärvereinigung (DEUQUA) e.V. 122 W. Knierzinger et al.: Anthropogenic and climate signals in peat layers mainly reflected in the pollen record and by enrichments of heavy metals. The study indicates a dry period in the region of the bog around ∼ 1950 cal BCE. Kurzfassung: Hochmoore eignen sich zur Rekonstruktion des Paläoklimas und anthropogener Aktivität in der Vergangenheit. In der vorliegenden Arbeit werden Multiproxy-Analysen (Elementchemie, Pollen, Mikrofossilien, stabile Pb-Isotope, Humifizierung, Aschegehalt) eines 500 cm langen und mittels der C-14-Methode datierten Torfkerns aus dem ombrotrophen Pürgschachener Moor im steirischen Ennstal (Österreichische Alpen) vorgelegt und diskutiert. Der Bohrkern umfasst einen Zeitraum von ∼ 5000 Jahren. Frühe Hinweise auf Besiedelung und landwirtschaftliche Nutzung datieren auf ∼ 2900 cal BCE. Erste markante Cu-Anreicherungen, die auf Cu-Bergbau in den angrenzenden Eisenerzer Alpen zurückgeführt werden, zeigen sich in Torfschichten aus der späten Kupfersteinzeit (∼ 2500 cal BCE). Deutlichere Zunahmen von Kulturindikatoren (Kulturpflanzen, Sträucher, Kräuter, Holzkohle) im Pollendiagram und Anreicherungen von Spurenmetallen lassen auf signifikanten menschlichen Einfluss in der Umgebung des Pürgschachener Moores in der Mittelbronzezeit (∼ 1450-1250 cal BCE), in der Spätbronzezeit und (∼ 1050-800 cal BCE) sowie in der Periode der späten Latènezeit (∼ 300 cal BCE-1 cal CE) schließen. Der größte Teil der Eisenzeit sowie die römische Kaiserzeit sind durch einen allgemeinen Rückgang von anthropogenen Indikatoren im Vergleich zu früheren Perioden gekennzeichnet. Anreicherungen von Pb und Sb in einer Torfprobe aus dem Mittelalter (∼ 900 cal CE) können mit Sideritabbau in unmittelbarer Nähe des Pürgschachener Moores in Verbindung gebracht werden. Die Ergebnisse dieser interdisziplinären Studie belegen starke klimagesteuerte Wechselbeziehungen zwischen Pollen, dem Humifizierungsgrad und dem Aschegehalt. Menschliche Aktivität in der Umgebung des Moores zeigt eine geringe Korrelation mit Humifizierung und Aschegehalt, findet allerdings stärkeren Niederschlag in den Pollen-und Schwermetalldaten. Die vorliegende Studie weist auf eine ausgedehnte Trockenperiode in der Umgebung des Pürgschachener Moors um ∼ 1950 cal BCE hin.","owner":{"id":195561,"first_name":"Klaus-Holger","middle_initials":null,"last_name":"Knorr","page_name":"KlausHolgerKnorr","domain_name":"uni-muenster","created_at":"2010-06-01T01:48:47.579-07:00","display_name":"Klaus-Holger Knorr","url":"https://uni-muenster.academia.edu/KlausHolgerKnorr"},"attachments":[{"id":73263888,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/73263888/thumbnails/1.jpg","file_name":"egqsj-69-121-2020.pdf","download_url":"https://www.academia.edu/attachments/73263888/download_file","bulk_download_file_name":"Anthropogenic_and_climate_signals_in_lat.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/73263888/egqsj-69-121-2020-libre.pdf?1634802739=\u0026response-content-disposition=attachment%3B+filename%3DAnthropogenic_and_climate_signals_in_lat.pdf\u0026Expires=1738799875\u0026Signature=gJF8AmuIgKFVqRc9rAyIonca02LfQCzxletPoXYyO9x~UA99QXQ1MtzTQlyjzpxKSFsgfhMSu39RBpCsBVMKjg2dqmfJu9sAb4oBnj8DJXc1fEMl4PO4glA4w1eaxQiMSPYhXBNiCjYr52b0ZI5K9tNspkLb3jPDlcKUV4kE3Pqu6EQxPEJ7C5sPyV5x6BfKmYOX-Nc-YeaRKfyNbwhGIFHqhKX-Qw4GeSK5SYZcGSqf5p224hyQsHE~X2Z-oC3Q8Q7Iv9AWvIyNDM0ydqs0BX37YJKOuLZMAVcIuw1PoRezynqHmxYUXQ8-nrl0B~H~ZDThHSsgW31FV0HlhYO~YQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"},{"id":73263889,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/73263889/thumbnails/1.jpg","file_name":"egqsj-69-121-2020.pdf","download_url":"https://www.academia.edu/attachments/73263889/download_file","bulk_download_file_name":"Anthropogenic_and_climate_signals_in_lat.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/73263889/egqsj-69-121-2020-libre.pdf?1634802739=\u0026response-content-disposition=attachment%3B+filename%3DAnthropogenic_and_climate_signals_in_lat.pdf\u0026Expires=1738799876\u0026Signature=fDCGz2wReKCh0cd2kH4gBayaXtQfuZPBGidcKVnUlKYtY~-7tBB6oiccyD88r2BUXrtuz-M85ChmTbSet34Pb6wpXYizW3gCeCpc56V6UOASfQEERzLIDS5nVCABOeb4Ov12joJh5I554iqOLgXUtg8jbLIbkJ79C-P35i3x~qg4PDMbrqW0RHnsVEPwC29gFGxBI-7PMPd7DPwJ~geU-EljEHVYqIKZm8kCdq19oJvgZkbxYLaXMzP0Ev6M6veRbdwQSLck1Cg8hVu9WrGTAvKk2ViMyEdqEXlDr2cyCcjqN7kp0~rLTSmlUEVn0pLDxf6ZpIfxVYE6yBEFNEzcNQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[],"urls":[{"id":13454290,"url":"https://egqsj.copernicus.org/articles/69/121/2020/egqsj-69-121-2020.pdf"}]}, dispatcherData: dispatcherData }); 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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=59238785]").text(description); $(".js-view-count[data-work-id=59238785]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 59238785; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='59238785']"); 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" } } $('.js-work-strip[data-work-id=59238785]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":59238785,"title":"Plant communities control long term carbon accumulation and biogeochemical gradients in a Patagonian bog","internal_url":"https://www.academia.edu/59238785/Plant_communities_control_long_term_carbon_accumulation_and_biogeochemical_gradients_in_a_Patagonian_bog","owner_id":195561,"coauthors_can_edit":true,"owner":{"id":195561,"first_name":"Klaus-Holger","middle_initials":null,"last_name":"Knorr","page_name":"KlausHolgerKnorr","domain_name":"uni-muenster","created_at":"2010-06-01T01:48:47.579-07:00","display_name":"Klaus-Holger Knorr","url":"https://uni-muenster.academia.edu/KlausHolgerKnorr"},"attachments":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="59238784"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/59238784/The_effect_of_long_term_fertilization_on_peat_in_an_ombrotrophic_bog"><img alt="Research paper thumbnail of The effect of long-term fertilization on peat in an ombrotrophic bog" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/59238784/The_effect_of_long_term_fertilization_on_peat_in_an_ombrotrophic_bog">The effect of long-term fertilization on peat in an ombrotrophic bog</a></div><div class="wp-workCard_item"><span>Geoderma</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="59238784"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="59238784"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 59238784; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=59238784]").text(description); $(".js-view-count[data-work-id=59238784]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 59238784; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='59238784']"); 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" } } $('.js-work-strip[data-work-id=59238784]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":59238784,"title":"The effect of long-term fertilization on peat in an ombrotrophic bog","internal_url":"https://www.academia.edu/59238784/The_effect_of_long_term_fertilization_on_peat_in_an_ombrotrophic_bog","owner_id":195561,"coauthors_can_edit":true,"owner":{"id":195561,"first_name":"Klaus-Holger","middle_initials":null,"last_name":"Knorr","page_name":"KlausHolgerKnorr","domain_name":"uni-muenster","created_at":"2010-06-01T01:48:47.579-07:00","display_name":"Klaus-Holger Knorr","url":"https://uni-muenster.academia.edu/KlausHolgerKnorr"},"attachments":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="59232875"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" rel="nofollow" href="https://www.academia.edu/59232875/Effect_of_Reduced_Sulfur_Species_on_Chemolithoautotrophic_Pyrite_Oxidation_with_Nitrate"><img alt="Research paper thumbnail of Effect of Reduced Sulfur Species on Chemolithoautotrophic Pyrite Oxidation with Nitrate" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" rel="nofollow" href="https://www.academia.edu/59232875/Effect_of_Reduced_Sulfur_Species_on_Chemolithoautotrophic_Pyrite_Oxidation_with_Nitrate">Effect of Reduced Sulfur Species on Chemolithoautotrophic Pyrite Oxidation with Nitrate</a></div><div class="wp-workCard_item"><span>Geomicrobiology Journal</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="59232875"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="59232875"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 59232875; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=59232875]").text(description); $(".js-view-count[data-work-id=59232875]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 59232875; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='59232875']"); 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" } } $('.js-work-strip[data-work-id=59232875]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":59232875,"title":"Effect of Reduced Sulfur Species on Chemolithoautotrophic Pyrite Oxidation with Nitrate","internal_url":"https://www.academia.edu/59232875/Effect_of_Reduced_Sulfur_Species_on_Chemolithoautotrophic_Pyrite_Oxidation_with_Nitrate","owner_id":195561,"coauthors_can_edit":true,"owner":{"id":195561,"first_name":"Klaus-Holger","middle_initials":null,"last_name":"Knorr","page_name":"KlausHolgerKnorr","domain_name":"uni-muenster","created_at":"2010-06-01T01:48:47.579-07:00","display_name":"Klaus-Holger Knorr","url":"https://uni-muenster.academia.edu/KlausHolgerKnorr"},"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="51343514"><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/51343514/Multi_proxy_analyses_of_a_minerotrophic_fen_to_reconstruct_prehistoric_periods_of_human_activity_associated_with_salt_mining_in_the_Hallstatt_region_Austria"><img alt="Research paper thumbnail of Multi-proxy analyses of a minerotrophic fen to reconstruct prehistoric periods of human activity associated with salt mining in the Hallstatt region (Austria" 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/51343514/Multi_proxy_analyses_of_a_minerotrophic_fen_to_reconstruct_prehistoric_periods_of_human_activity_associated_with_salt_mining_in_the_Hallstatt_region_Austria">Multi-proxy analyses of a minerotrophic fen to reconstruct prehistoric periods of human activity associated with salt mining in the Hallstatt region (Austria</a></div><div class="wp-workCard_item"><span>Journal of Archaeological Science: Reports</span><span>, 2021</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">In this study, periods of prehistoric anthropogenic activity in the Hallstatt salt mining area (U...</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">In this study, periods of prehistoric anthropogenic activity in the Hallstatt salt mining area (Upper Austria) are reconstructed from elemental (XRF-scanning, Q-ICP-MS) and Pb isotopic analyses (206 Pb, 207 Pb, 208 Pb) of a radiocarbon-dated, 137-cm-long peat core covering the past ~7,000 years. The peat core was retrieved from a minerotrophic fen in the Hallstatt High Valley. Distinct metal enrichments attributed to low anthropogenic impact in Hallstatt can be traced back to a time around 2350 cal BCE and to another period around 1800 cal BCE. The period from the Late Bronze Age to the Early Iron Age (~1300 cal BCE to ~500 cal BCE) is characterised by increased anthropogenic activity. Relatively high Sn concentrations between ~1210 cal BCE and ~540 cal BCE) point towards intensive bronze casting processes, probably associated with the production of bronze picks that were used for local salt mining during this time. Intense human impact was also determined for the early Roman imperi...</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="51343514"><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="51343514"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 51343514; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=51343514]").text(description); $(".js-view-count[data-work-id=51343514]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 51343514; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='51343514']"); 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" } } $('.js-work-strip[data-work-id=51343514]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":51343514,"title":"Multi-proxy analyses of a minerotrophic fen to reconstruct prehistoric periods of human activity associated with salt mining in the Hallstatt region (Austria","internal_url":"https://www.academia.edu/51343514/Multi_proxy_analyses_of_a_minerotrophic_fen_to_reconstruct_prehistoric_periods_of_human_activity_associated_with_salt_mining_in_the_Hallstatt_region_Austria","owner_id":195561,"coauthors_can_edit":true,"owner":{"id":195561,"first_name":"Klaus-Holger","middle_initials":null,"last_name":"Knorr","page_name":"KlausHolgerKnorr","domain_name":"uni-muenster","created_at":"2010-06-01T01:48:47.579-07:00","display_name":"Klaus-Holger Knorr","url":"https://uni-muenster.academia.edu/KlausHolgerKnorr"},"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="46000396"><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/46000396/Can_we_expect_pristine_mountain_peatland_ecosystems_in_Central_Europe_Evidence_from_multi_proxy_palaeoecological_studies_on_the_Holocene_peatland_development"><img alt="Research paper thumbnail of Can we expect pristine mountain peatland ecosystems in Central Europe? Evidence from multi-proxy palaeoecological studies on the Holocene peatland development" 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/46000396/Can_we_expect_pristine_mountain_peatland_ecosystems_in_Central_Europe_Evidence_from_multi_proxy_palaeoecological_studies_on_the_Holocene_peatland_development">Can we expect pristine mountain peatland ecosystems in Central Europe? Evidence from multi-proxy palaeoecological studies on the Holocene peatland development</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="46000396"><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="46000396"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 46000396; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=46000396]").text(description); $(".js-view-count[data-work-id=46000396]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 46000396; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='46000396']"); 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" } } $('.js-work-strip[data-work-id=46000396]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":46000396,"title":"Can we expect pristine mountain peatland ecosystems in Central Europe? 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