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In numerical experiments an ice-marginal lake drains through a subglacial channel, producing... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_12989017" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">A model subglacial drainage system, coupled to an ice-dammed reservoir that receives a time-varying meltwater input, is described and analysed. In numerical experiments an ice-marginal lake drains through a subglacial channel, producing periodic floods, and fills with meltwater at a rate<br />dependent on air temperature, which varies seasonally with a peak value of Tm. The analysis reveals regions of Tm parameter space corresponding to ‘mode locking’, where flood repeat time is independent of Tm; resonance, where decreasing Tm counter-intuitively increases flood size; and chaotic dynamics,<br />where flood cycles are sensitive to initial conditions, never repeat and exhibit phase-space mixing. Bifurcations associated with abrupt changes in flood size and timing within the year separate these regions. This is the first time these complex dynamics have been displayed by a glaciohydraulic model<br />and these findings have implications for our understanding of ice-marginal lakes, moulins and subglacial lakes.</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/12989017" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="328ffff4a164ebcfff14a16aed33811f" rel="nofollow" data-download="{"attachment_id":37908504,"asset_id":12989017,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/37908504/download_file?st=MTczMjM2NjYxNyw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="6383794" href="https://antarctica.academia.edu/JonathanKingslake">Jonathan Kingslake</a><script data-card-contents-for-user="6383794" type="text/json">{"id":6383794,"first_name":"Jonathan","last_name":"Kingslake","domain_name":"antarctica","page_name":"JonathanKingslake","display_name":"Jonathan Kingslake","profile_url":"https://antarctica.academia.edu/JonathanKingslake?f_ri=400","photo":"/images/s65_no_pic.png"}</script></span></span></li><li class="js-paper-rank-work_12989017 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="12989017"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 12989017, container: ".js-paper-rank-work_12989017", }); 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In numerical experiments an ice-marginal lake drains through a subglacial channel, producing periodic floods, and fills with meltwater at a rate\ndependent on air temperature, which varies seasonally with a peak value of Tm. The analysis reveals regions of Tm parameter space corresponding to ‘mode locking’, where flood repeat time is independent of Tm; resonance, where decreasing Tm counter-intuitively increases flood size; and chaotic dynamics,\nwhere flood cycles are sensitive to initial conditions, never repeat and exhibit phase-space mixing. Bifurcations associated with abrupt changes in flood size and timing within the year separate these regions. This is the first time these complex dynamics have been displayed by a glaciohydraulic model\nand these findings have implications for our understanding of ice-marginal lakes, moulins and subglacial lakes.","downloadable_attachments":[{"id":37908504,"asset_id":12989017,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":6383794,"first_name":"Jonathan","last_name":"Kingslake","domain_name":"antarctica","page_name":"JonathanKingslake","display_name":"Jonathan Kingslake","profile_url":"https://antarctica.academia.edu/JonathanKingslake?f_ri=400","photo":"/images/s65_no_pic.png"}],"research_interests":[{"id":400,"name":"Earth Sciences","url":"https://www.academia.edu/Documents/in/Earth_Sciences?f_ri=400","nofollow":false},{"id":402,"name":"Environmental 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href="https://www.academia.edu/1489088/Mass_transfer_and_fluid_flow_during_detachment_faulting_and_development_of_an_oceanic_core_complex_Atlantis_Massif_MAR_30_N_">Mass transfer and fluid flow during detachment faulting and development of an oceanic core complex, Atlantis Massif (MAR 30°N)</a></div></div><div class="u-pb4x u-mt3x"></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/1489088" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="46b28bc4d763e07b1679ea92664834d5" rel="nofollow" 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$(".js-view-count-work_1489088").removeClass('hidden') })</script></div></li><li class="InlineList-item u-positionRelative" style="max-width: 250px"><div class="u-positionAbsolute" data-has-card-for-ri-list="1489088"><i class="fa fa-tag InlineList-item-icon u-positionRelative"></i>  <a class="InlineList-item-text u-positionRelative">10</a>  </div><span class="InlineList-item-text u-textTruncate u-pl10x"><a class="InlineList-item-text" data-has-card-for-ri="400" href="https://www.academia.edu/Documents/in/Earth_Sciences">Earth Sciences</a>, <script data-card-contents-for-ri="400" type="text/json">{"id":400,"name":"Earth Sciences","url":"https://www.academia.edu/Documents/in/Earth_Sciences?f_ri=400","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="1419" href="https://www.academia.edu/Documents/in/Structural_Geology">Structural Geology</a>, <script data-card-contents-for-ri="1419" type="text/json">{"id":1419,"name":"Structural 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core complex, Atlantis Massif (MAR 30°N)","created_at":"2012-03-27T19:24:43.528-07:00","url":"https://www.academia.edu/1489088/Mass_transfer_and_fluid_flow_during_detachment_faulting_and_development_of_an_oceanic_core_complex_Atlantis_Massif_MAR_30_N_?f_ri=400","dom_id":"work_1489088","summary":null,"downloadable_attachments":[{"id":50950767,"asset_id":1489088,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":1383142,"first_name":"Chiara","last_name":"Boschi","domain_name":"cnr-it","page_name":"ChiaraBoschi","display_name":"Chiara Boschi","profile_url":"https://cnr-it.academia.edu/ChiaraBoschi?f_ri=400","photo":"https://0.academia-photos.com/1383142/502845/632290/s65_chiara.boschi.jpg"}],"research_interests":[{"id":400,"name":"Earth Sciences","url":"https://www.academia.edu/Documents/in/Earth_Sciences?f_ri=400","nofollow":false},{"id":1419,"name":"Structural 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})();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_23847924" data-work_id="23847924" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/23847924/Postglacial_deltaic_sediments_southern_Fraser_River_delta_British_Columbia">Postglacial deltaic sediments, southern Fraser River delta, British Columbia</a></div></div><div class="u-pb4x u-mt3x"></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/23847924" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" 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data-has-card-for-user="30937520" href="https://sfu.academia.edu/JohnClague">John Clague</a><script data-card-contents-for-user="30937520" type="text/json">{"id":30937520,"first_name":"John","last_name":"Clague","domain_name":"sfu","page_name":"JohnClague","display_name":"John Clague","profile_url":"https://sfu.academia.edu/JohnClague?f_ri=400","photo":"https://0.academia-photos.com/30937520/18648109/18835474/s65_john.clague.jpg"}</script></span></span></li><li class="js-paper-rank-work_23847924 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="23847924"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 23847924, container: ".js-paper-rank-work_23847924", }); });</script></li><li class="js-percentile-work_23847924 InlineList-item InlineList-item--bordered hidden u-tcGrayDark"><span class="percentile-widget hidden"><span 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$(".js-view-count[data-work-id=23847924]").text(description); $(".js-view-count-work_23847924").attr('title', description).tooltip(); }); });</script></span><script>$(function() { $(".js-view-count-work_23847924").removeClass('hidden') })</script></div></li><li class="InlineList-item u-positionRelative" style="max-width: 250px"><div class="u-positionAbsolute" data-has-card-for-ri-list="23847924"><i class="fa fa-tag InlineList-item-icon u-positionRelative"></i></div><span class="InlineList-item-text u-textTruncate u-pl6x"><a class="InlineList-item-text" data-has-card-for-ri="400" href="https://www.academia.edu/Documents/in/Earth_Sciences">Earth Sciences</a><script data-card-contents-for-ri="400" type="text/json">{"id":400,"name":"Earth Sciences","url":"https://www.academia.edu/Documents/in/Earth_Sciences?f_ri=400","nofollow":false}</script></span></li><script>(function(){ if (false) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=23847924]'), work: {"id":23847924,"title":"Postglacial deltaic sediments, southern Fraser River delta, British Columbia","created_at":"2016-03-30T20:09:05.008-07:00","url":"https://www.academia.edu/23847924/Postglacial_deltaic_sediments_southern_Fraser_River_delta_British_Columbia?f_ri=400","dom_id":"work_23847924","summary":null,"downloadable_attachments":[{"id":44243164,"asset_id":23847924,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":30937520,"first_name":"John","last_name":"Clague","domain_name":"sfu","page_name":"JohnClague","display_name":"John Clague","profile_url":"https://sfu.academia.edu/JohnClague?f_ri=400","photo":"https://0.academia-photos.com/30937520/18648109/18835474/s65_john.clague.jpg"}],"research_interests":[{"id":400,"name":"Earth Sciences","url":"https://www.academia.edu/Documents/in/Earth_Sciences?f_ri=400","nofollow":false}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_4750292" data-work_id="4750292" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/4750292/Numerical_simulation_of_groundwater_flow_in_regional_rock_aquifers_southwestern_Quebec_Canada">Numerical simulation of groundwater flow in regional rock aquifers, southwestern Quebec, Canada</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest"><div class="summarized">The St. Lawrence Lowlands platform, Quebec, Canada, is a densely-populated area, heavily dependent on groundwater resources. In 1999, the Geological Survey of Canada initiated a large-scale hydrogeological assessment study over a... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_4750292" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">The St. Lawrence Lowlands platform, Quebec, Canada, is a densely-populated area, heavily dependent on groundwater resources. In 1999, the Geological Survey of Canada initiated a large-scale hydrogeological assessment study over a 1,500 km2 region northwest of Montreal. The objectives were to define the regional groundwater flow, and to give quantitative estimates of the groundwater dynamic parameters and of the available groundwater resources. The applied approach consisted of defining the hydrogeologic framework, hydraulic properties of the aquifer units, and groundwater dynamic components. Lower Paleozoic sedimentary rocks represent regional aquifer units. Coarse Quaternary fluvio-glacial sediments locally overlay the rock sequence and constitute an interface aquifer unit. Fine marine sediments confine most of the regional aquifers. Collected GIS based information was synthesized in a finite element numerical model. The regional saturated steady-state flow was calibrated under current stress conditions assuming an equivalent porous medium approach. Water budget calculations show that the total groundwater flow in regional aquifers amounts to 97.7 Mm3/y. Infiltration from precipitation provides 86.6% of the groundwater supply, while 9.6% comes from subsurface inflow and the remaining 3.8% is induced recharge from surface waters. Discharge from regional aquifers occurs through flow to streams (76.9%), groundwater withdrawal (18.4%), and underground outflow (4.7%). La plateforme Lowllands du Saint-Laurent, Québec, Canada, est une aire densément peuplée, dépendant grandement des ressources en eau souterraine. En 1999, le Service Géologique du Canada a initié une étude hydrogéologique à grande-échelle sur 1500 km2 au Nord-Ouest de Montréal. Le sobjectifs ont été de définir la dynamique de l’écoulement régional, et de donner des estimations quantitatives des paramètres dynamiques des ressources disponibles en eau souterraine. L’approche utilisée consista à définir le cadre hydrogéologique de travail, les propriétés hydrauliques des unités aquifères, et les composantes dynamiques des eaux souterraines. Les roches sédimentaires du Paléozoïque Inférieur représentent les unités aquifères régionales. Les sédiments marins fins confinent la plus grande partie des aquifères régionaux. Les informations de base, collectées dans un SIG, ont été synthétisées dans un modèle numérique aux éléments finis. L’écoulement permanent régional, en zone saturée, a été calibré en conditions de stress en assumant une approche de milieu poreu équivalent. Les calculs du bilan hydrologique montrent que l’écoulement total des eaux souterraines dans les aquifères régionaux atteind 97,7 Mm3/an. L’infiltration à partir des précipitations apporte 86.6% de l’eau souterraine exploitée; sachant que 9,6% proviennent d’écoulement de subsurfaces, et que les 3,8% restants proviennent de la recharge via les eaux de surface. Le débit pompé des aquifères régionaux apparaît à travers l’écoulement des cours d’eau, le rabattement des eaux souterraines (18.4%), et l’écoulement ascendant (4.7%). La plataforma de Tierras Bajas San Lorenzo, Quebec, Canadá, es un área densamente poblada que depende fuertemente de recursos de agua subterránea. En 1999 el Servicio Geológico de Canadá inició un estudio de evaluación hidrogeológica a gran escala sobre un área de 1,500 km2 en la región noroeste de Montreal. Los objetivos fueron definir el flujo regional de agua subterránea y aportar estimados cuantitativos de los parámetros dinámicos de agua subterráne y de los recursos disponibles de agua subterránea. El enfoque aplicado consistió en definir el marco hidrogeológico, propiedades hidráulicas de las unidades acuíferas, y los componentes dinámicos de agua subterránea. Rocas sedimentarias del Paleozoico Inferior representan unidades regionales de acuíferos. Sedimentos fluvio-glaciares Cuaternarios gruesos sobreyacen localmente la secuencia rocosa y constituyen una unidad acuífera interfacial. Sedimentos marinos finos confinan la mayoría de acuíferos regionales. Información colectada basada en SIG se sintetizó en un modelo numérico de elemento finito. El flujo regional saturado en régimen permanente se calibró bajo condiciones de stress asumiendo un enfoque de medio poroso equivalente. Los cálculos de balance hídrico muestran que el flujo total de agua subterránea en acuíferos regional alcanza 97.7 Mm3/año. Infiltración a partir de lluvia aporta el 86.6% del abastecimiento al agua subterránea, mientras que el 9.6% proviene de entradas subsuperficiales y el restante 3.8% consiste de recarga inducida a partir de aguas superficiales. La descarga proveniente de acuíferos regionales ocurre a través de flujo a ríos (76.9%), utilización de agua subterránea (18.4%), y salida subterránea (4.7%).</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/4750292" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="6f2e4720f2739f44633c5e8f255cf67c" rel="nofollow" data-download="{"attachment_id":49645818,"asset_id":4750292,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/49645818/download_file?st=MTczMjM2NjYxNyw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="6086303" href="https://independent.academia.edu/AnaRivera4">Ana Rivera</a><script data-card-contents-for-user="6086303" type="text/json">{"id":6086303,"first_name":"Ana","last_name":"Rivera","domain_name":"independent","page_name":"AnaRivera4","display_name":"Ana Rivera","profile_url":"https://independent.academia.edu/AnaRivera4?f_ri=400","photo":"/images/s65_no_pic.png"}</script></span></span></li><li class="js-paper-rank-work_4750292 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="4750292"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 4750292, container: ".js-paper-rank-work_4750292", }); 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$(".js-view-count[data-work-id=4750292]").text(description); $(".js-view-count-work_4750292").attr('title', description).tooltip(); }); });</script></span><script>$(function() { $(".js-view-count-work_4750292").removeClass('hidden') })</script></div></li><li class="InlineList-item u-positionRelative" style="max-width: 250px"><div class="u-positionAbsolute" data-has-card-for-ri-list="4750292"><i class="fa fa-tag InlineList-item-icon u-positionRelative"></i>  <a class="InlineList-item-text u-positionRelative">13</a>  </div><span class="InlineList-item-text u-textTruncate u-pl10x"><a class="InlineList-item-text" data-has-card-for-ri="48" href="https://www.academia.edu/Documents/in/Engineering">Engineering</a>, <script data-card-contents-for-ri="48" type="text/json">{"id":48,"name":"Engineering","url":"https://www.academia.edu/Documents/in/Engineering?f_ri=400","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="400" href="https://www.academia.edu/Documents/in/Earth_Sciences">Earth Sciences</a>, <script data-card-contents-for-ri="400" type="text/json">{"id":400,"name":"Earth Sciences","url":"https://www.academia.edu/Documents/in/Earth_Sciences?f_ri=400","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="411" href="https://www.academia.edu/Documents/in/Hydrogeology">Hydrogeology</a>, <script data-card-contents-for-ri="411" type="text/json">{"id":411,"name":"Hydrogeology","url":"https://www.academia.edu/Documents/in/Hydrogeology?f_ri=400","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="23042" href="https://www.academia.edu/Documents/in/Finite_Element">Finite Element</a><script data-card-contents-for-ri="23042" type="text/json">{"id":23042,"name":"Finite Element","url":"https://www.academia.edu/Documents/in/Finite_Element?f_ri=400","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=4750292]'), work: {"id":4750292,"title":"Numerical simulation of groundwater flow in regional rock aquifers, southwestern Quebec, Canada","created_at":"2013-10-11T12:16:10.950-07:00","url":"https://www.academia.edu/4750292/Numerical_simulation_of_groundwater_flow_in_regional_rock_aquifers_southwestern_Quebec_Canada?f_ri=400","dom_id":"work_4750292","summary":"The St. Lawrence Lowlands platform, Quebec, Canada, is a densely-populated area, heavily dependent on groundwater resources. In 1999, the Geological Survey of Canada initiated a large-scale hydrogeological assessment study over a 1,500 km2 region northwest of Montreal. The objectives were to define the regional groundwater flow, and to give quantitative estimates of the groundwater dynamic parameters and of the available groundwater resources. The applied approach consisted of defining the hydrogeologic framework, hydraulic properties of the aquifer units, and groundwater dynamic components. Lower Paleozoic sedimentary rocks represent regional aquifer units. Coarse Quaternary fluvio-glacial sediments locally overlay the rock sequence and constitute an interface aquifer unit. Fine marine sediments confine most of the regional aquifers. Collected GIS based information was synthesized in a finite element numerical model. The regional saturated steady-state flow was calibrated under current stress conditions assuming an equivalent porous medium approach. Water budget calculations show that the total groundwater flow in regional aquifers amounts to 97.7 Mm3/y. Infiltration from precipitation provides 86.6% of the groundwater supply, while 9.6% comes from subsurface inflow and the remaining 3.8% is induced recharge from surface waters. Discharge from regional aquifers occurs through flow to streams (76.9%), groundwater withdrawal (18.4%), and underground outflow (4.7%). La plateforme Lowllands du Saint-Laurent, Québec, Canada, est une aire densément peuplée, dépendant grandement des ressources en eau souterraine. En 1999, le Service Géologique du Canada a initié une étude hydrogéologique à grande-échelle sur 1500 km2 au Nord-Ouest de Montréal. Le sobjectifs ont été de définir la dynamique de l’écoulement régional, et de donner des estimations quantitatives des paramètres dynamiques des ressources disponibles en eau souterraine. L’approche utilisée consista à définir le cadre hydrogéologique de travail, les propriétés hydrauliques des unités aquifères, et les composantes dynamiques des eaux souterraines. Les roches sédimentaires du Paléozoïque Inférieur représentent les unités aquifères régionales. Les sédiments marins fins confinent la plus grande partie des aquifères régionaux. Les informations de base, collectées dans un SIG, ont été synthétisées dans un modèle numérique aux éléments finis. L’écoulement permanent régional, en zone saturée, a été calibré en conditions de stress en assumant une approche de milieu poreu équivalent. Les calculs du bilan hydrologique montrent que l’écoulement total des eaux souterraines dans les aquifères régionaux atteind 97,7 Mm3/an. L’infiltration à partir des précipitations apporte 86.6% de l’eau souterraine exploitée; sachant que 9,6% proviennent d’écoulement de subsurfaces, et que les 3,8% restants proviennent de la recharge via les eaux de surface. Le débit pompé des aquifères régionaux apparaît à travers l’écoulement des cours d’eau, le rabattement des eaux souterraines (18.4%), et l’écoulement ascendant (4.7%). La plataforma de Tierras Bajas San Lorenzo, Quebec, Canadá, es un área densamente poblada que depende fuertemente de recursos de agua subterránea. En 1999 el Servicio Geológico de Canadá inició un estudio de evaluación hidrogeológica a gran escala sobre un área de 1,500 km2 en la región noroeste de Montreal. Los objetivos fueron definir el flujo regional de agua subterránea y aportar estimados cuantitativos de los parámetros dinámicos de agua subterráne y de los recursos disponibles de agua subterránea. El enfoque aplicado consistió en definir el marco hidrogeológico, propiedades hidráulicas de las unidades acuíferas, y los componentes dinámicos de agua subterránea. Rocas sedimentarias del Paleozoico Inferior representan unidades regionales de acuíferos. Sedimentos fluvio-glaciares Cuaternarios gruesos sobreyacen localmente la secuencia rocosa y constituyen una unidad acuífera interfacial. Sedimentos marinos finos confinan la mayoría de acuíferos regionales. Información colectada basada en SIG se sintetizó en un modelo numérico de elemento finito. El flujo regional saturado en régimen permanente se calibró bajo condiciones de stress asumiendo un enfoque de medio poroso equivalente. Los cálculos de balance hídrico muestran que el flujo total de agua subterránea en acuíferos regional alcanza 97.7 Mm3/año. Infiltración a partir de lluvia aporta el 86.6% del abastecimiento al agua subterránea, mientras que el 9.6% proviene de entradas subsuperficiales y el restante 3.8% consiste de recarga inducida a partir de aguas superficiales. La descarga proveniente de acuíferos regionales ocurre a través de flujo a ríos (76.9%), utilización de agua subterránea (18.4%), y salida subterránea (4.7%).","downloadable_attachments":[{"id":49645818,"asset_id":4750292,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":6086303,"first_name":"Ana","last_name":"Rivera","domain_name":"independent","page_name":"AnaRivera4","display_name":"Ana Rivera","profile_url":"https://independent.academia.edu/AnaRivera4?f_ri=400","photo":"/images/s65_no_pic.png"}],"research_interests":[{"id":48,"name":"Engineering","url":"https://www.academia.edu/Documents/in/Engineering?f_ri=400","nofollow":false},{"id":400,"name":"Earth Sciences","url":"https://www.academia.edu/Documents/in/Earth_Sciences?f_ri=400","nofollow":false},{"id":411,"name":"Hydrogeology","url":"https://www.academia.edu/Documents/in/Hydrogeology?f_ri=400","nofollow":false},{"id":23042,"name":"Finite Element","url":"https://www.academia.edu/Documents/in/Finite_Element?f_ri=400","nofollow":false},{"id":60658,"name":"Numerical Simulation","url":"https://www.academia.edu/Documents/in/Numerical_Simulation?f_ri=400"},{"id":142810,"name":"Surface Water","url":"https://www.academia.edu/Documents/in/Surface_Water?f_ri=400"},{"id":234860,"name":"Steady state","url":"https://www.academia.edu/Documents/in/Steady_state?f_ri=400"},{"id":333942,"name":"Marine Sediment","url":"https://www.academia.edu/Documents/in/Marine_Sediment?f_ri=400"},{"id":420417,"name":"Groundwater flow","url":"https://www.academia.edu/Documents/in/Groundwater_flow?f_ri=400"},{"id":497452,"name":"Numerical Model","url":"https://www.academia.edu/Documents/in/Numerical_Model?f_ri=400"},{"id":758278,"name":"Large Scale","url":"https://www.academia.edu/Documents/in/Large_Scale?f_ri=400"},{"id":771600,"name":"Porous Medium","url":"https://www.academia.edu/Documents/in/Porous_Medium?f_ri=400"},{"id":1726489,"name":"Water budget","url":"https://www.academia.edu/Documents/in/Water_budget?f_ri=400"}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_24652858" data-work_id="24652858" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/24652858/Emission_of_N2O_N2_CH4_and_CO2_from_constructed_wetlands_for_wastewater_treatment_and_from_riparian_buffer_zones">Emission of N2O, N2, CH4, and CO2 from constructed wetlands for wastewater treatment and from riparian buffer zones</a></div></div><div class="u-pb4x u-mt3x"></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" 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type="text/json">{"id":48,"name":"Engineering","url":"https://www.academia.edu/Documents/in/Engineering?f_ri=400","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="79" href="https://www.academia.edu/Documents/in/Ecological_Engineering">Ecological Engineering</a>, <script data-card-contents-for-ri="79" type="text/json">{"id":79,"name":"Ecological Engineering","url":"https://www.academia.edu/Documents/in/Ecological_Engineering?f_ri=400","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="400" href="https://www.academia.edu/Documents/in/Earth_Sciences">Earth Sciences</a>, <script data-card-contents-for-ri="400" type="text/json">{"id":400,"name":"Earth Sciences","url":"https://www.academia.edu/Documents/in/Earth_Sciences?f_ri=400","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="4594" href="https://www.academia.edu/Documents/in/Carbon_Dioxide">Carbon Dioxide</a><script data-card-contents-for-ri="4594" type="text/json">{"id":4594,"name":"Carbon Dioxide","url":"https://www.academia.edu/Documents/in/Carbon_Dioxide?f_ri=400","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=24652858]'), work: {"id":24652858,"title":"Emission of N2O, N2, CH4, and CO2 from constructed wetlands for wastewater treatment and from riparian buffer zones","created_at":"2016-04-22T01:35:37.237-07:00","url":"https://www.academia.edu/24652858/Emission_of_N2O_N2_CH4_and_CO2_from_constructed_wetlands_for_wastewater_treatment_and_from_riparian_buffer_zones?f_ri=400","dom_id":"work_24652858","summary":null,"downloadable_attachments":[{"id":44980508,"asset_id":24652858,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":28036136,"first_name":"Ülo","last_name":"Mander","domain_name":"ut-ee","page_name":"ÜloMander","display_name":"Ülo Mander","profile_url":"https://ut-ee.academia.edu/%C3%9CloMander?f_ri=400","photo":"https://0.academia-photos.com/28036136/20756095/20318690/s65__lo.mander.jpg"}],"research_interests":[{"id":48,"name":"Engineering","url":"https://www.academia.edu/Documents/in/Engineering?f_ri=400","nofollow":false},{"id":79,"name":"Ecological Engineering","url":"https://www.academia.edu/Documents/in/Ecological_Engineering?f_ri=400","nofollow":false},{"id":400,"name":"Earth Sciences","url":"https://www.academia.edu/Documents/in/Earth_Sciences?f_ri=400","nofollow":false},{"id":4594,"name":"Carbon Dioxide","url":"https://www.academia.edu/Documents/in/Carbon_Dioxide?f_ri=400","nofollow":false},{"id":9991,"name":"Wastewater Treatment","url":"https://www.academia.edu/Documents/in/Wastewater_Treatment?f_ri=400"},{"id":58054,"name":"Environmental Sciences","url":"https://www.academia.edu/Documents/in/Environmental_Sciences?f_ri=400"},{"id":123865,"name":"Global warming potential","url":"https://www.academia.edu/Documents/in/Global_warming_potential?f_ri=400"},{"id":156347,"name":"Methane","url":"https://www.academia.edu/Documents/in/Methane?f_ri=400"},{"id":355465,"name":"Constructed Wetland","url":"https://www.academia.edu/Documents/in/Constructed_Wetland?f_ri=400"},{"id":387920,"name":"Nitrous Oxide","url":"https://www.academia.edu/Documents/in/Nitrous_Oxide?f_ri=400"},{"id":803009,"name":"Domestic Wastewater","url":"https://www.academia.edu/Documents/in/Domestic_Wastewater?f_ri=400"},{"id":958451,"name":"Subsurface Flow","url":"https://www.academia.edu/Documents/in/Subsurface_Flow?f_ri=400"},{"id":1359503,"name":"CO 2 Emission","url":"https://www.academia.edu/Documents/in/CO_2_Emission?f_ri=400"}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_18116014" data-work_id="18116014" itemscope="itemscope" 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new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=13498796]'), work: {"id":13498796,"title":"Oceanic core complex development at the ultraslow spreading Mid-Cayman Spreading Center","created_at":"2015-07-01T07:39:40.250-07:00","url":"https://www.academia.edu/13498796/Oceanic_core_complex_development_at_the_ultraslow_spreading_Mid_Cayman_Spreading_Center?f_ri=400","dom_id":"work_13498796","summary":null,"downloadable_attachments":[{"id":45265743,"asset_id":13498796,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":32702906,"first_name":"Michael","last_name":"Perfit","domain_name":"florida","page_name":"MichaelPerfit","display_name":"Michael Perfit","profile_url":"https://florida.academia.edu/MichaelPerfit?f_ri=400","photo":"https://0.academia-photos.com/32702906/9767027/10881017/s65_michael.perfit.jpg"}],"research_interests":[{"id":400,"name":"Earth Sciences","url":"https://www.academia.edu/Documents/in/Earth_Sciences?f_ri=400","nofollow":false},{"id":118582,"name":"Physical sciences","url":"https://www.academia.edu/Documents/in/Physical_sciences?f_ri=400","nofollow":false}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_2908264" data-work_id="2908264" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/2908264/Early_Middle_Pleistocene_environmental_changes_and_human_evolution_in_the_Italian_peninsula">Early–Middle Pleistocene environmental changes and human evolution in the Italian peninsula</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest"><div class="summarized">This paper is aimed to elucidate the ecological scenario in Italy in the Early to Middle Pleistocene, when species of the genus Homo are known to spread across Europe in two distinct waves: earlier than 1.2 Ma and at about 600 ka,... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_2908264" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">This paper is aimed to elucidate the ecological scenario in Italy in the Early to Middle Pleistocene, when species of the genus Homo are known to spread across Europe in two distinct waves: earlier than 1.2 Ma and at about 600 ka, respectively. This topic represents both (1) a fundamental aspect for a better understanding of the factors that allowed humans to colonize the middle latitudes of Eurasia, and (2) a reasonable frontier for current Quaternary palaeobiology, thanks to increasing knowledge of regional and local patterns. As for Italy, a combination of palaeobotanical and palaeontological data sets shows on the one hand a general complexity in both space and time, and on the other hand changes of considerable importance within and among the biological communities. These changes had a major importance during the worldwide change in the Earth climatic system known as “Middle Pleistocene Revolution”, which according to our data culminates with crucial effects of the extreme conditions of MIS 16. Subsequently, during great part of the Middle Pleistocene, the peculiar features of the Italian territory may have favoured isolation and a local persistence of plant populations and possibly mammal taxa, humans included, as for instance suggested by the corrected chronology of the Ceprano calvarium.</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/2908264" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="b9635c140f2efcafacb717bf012491e3" rel="nofollow" data-download="{"attachment_id":37667837,"asset_id":2908264,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/37667837/download_file?st=MTczMjM2NjYxNyw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="3421427" href="https://uniroma1.academia.edu/DonatellaMagri">Donatella Magri</a><script data-card-contents-for-user="3421427" type="text/json">{"id":3421427,"first_name":"Donatella","last_name":"Magri","domain_name":"uniroma1","page_name":"DonatellaMagri","display_name":"Donatella Magri","profile_url":"https://uniroma1.academia.edu/DonatellaMagri?f_ri=400","photo":"https://0.academia-photos.com/3421427/10110370/11280589/s65_donatella.magri.jpg"}</script></span></span></li><li class="js-paper-rank-work_2908264 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="2908264"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 2908264, container: ".js-paper-rank-work_2908264", }); 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$(".js-view-count[data-work-id=2908264]").text(description); $(".js-view-count-work_2908264").attr('title', description).tooltip(); }); });</script></span><script>$(function() { $(".js-view-count-work_2908264").removeClass('hidden') })</script></div></li><li class="InlineList-item u-positionRelative" style="max-width: 250px"><div class="u-positionAbsolute" data-has-card-for-ri-list="2908264"><i class="fa fa-tag InlineList-item-icon u-positionRelative"></i>  <a class="InlineList-item-text u-positionRelative">6</a>  </div><span class="InlineList-item-text u-textTruncate u-pl9x"><a class="InlineList-item-text" data-has-card-for-ri="400" href="https://www.academia.edu/Documents/in/Earth_Sciences">Earth Sciences</a>, <script data-card-contents-for-ri="400" type="text/json">{"id":400,"name":"Earth Sciences","url":"https://www.academia.edu/Documents/in/Earth_Sciences?f_ri=400","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="772" href="https://www.academia.edu/Documents/in/Human_Evolution">Human Evolution</a>, <script data-card-contents-for-ri="772" type="text/json">{"id":772,"name":"Human Evolution","url":"https://www.academia.edu/Documents/in/Human_Evolution?f_ri=400","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="28157" href="https://www.academia.edu/Documents/in/Environmental_Change">Environmental Change</a>, <script data-card-contents-for-ri="28157" type="text/json">{"id":28157,"name":"Environmental Change","url":"https://www.academia.edu/Documents/in/Environmental_Change?f_ri=400","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="93755" href="https://www.academia.edu/Documents/in/History_and_archaeology">History and archaeology</a><script data-card-contents-for-ri="93755" type="text/json">{"id":93755,"name":"History and archaeology","url":"https://www.academia.edu/Documents/in/History_and_archaeology?f_ri=400","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=2908264]'), work: {"id":2908264,"title":"Early–Middle Pleistocene environmental changes and human evolution in the Italian peninsula","created_at":"2013-03-05T00:41:14.777-08:00","url":"https://www.academia.edu/2908264/Early_Middle_Pleistocene_environmental_changes_and_human_evolution_in_the_Italian_peninsula?f_ri=400","dom_id":"work_2908264","summary":"This paper is aimed to elucidate the ecological scenario in Italy in the Early to Middle Pleistocene, when species of the genus Homo are known to spread across Europe in two distinct waves: earlier than 1.2 Ma and at about 600 ka, respectively. This topic represents both (1) a fundamental aspect for a better understanding of the factors that allowed humans to colonize the middle latitudes of Eurasia, and (2) a reasonable frontier for current Quaternary palaeobiology, thanks to increasing knowledge of regional and local patterns. As for Italy, a combination of palaeobotanical and palaeontological data sets shows on the one hand a general complexity in both space and time, and on the other hand changes of considerable importance within and among the biological communities. These changes had a major importance during the worldwide change in the Earth climatic system known as “Middle Pleistocene Revolution”, which according to our data culminates with crucial effects of the extreme conditions of MIS 16. Subsequently, during great part of the Middle Pleistocene, the peculiar features of the Italian territory may have favoured isolation and a local persistence of plant populations and possibly mammal taxa, humans included, as for instance suggested by the corrected chronology of the Ceprano calvarium.","downloadable_attachments":[{"id":37667837,"asset_id":2908264,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":3421427,"first_name":"Donatella","last_name":"Magri","domain_name":"uniroma1","page_name":"DonatellaMagri","display_name":"Donatella Magri","profile_url":"https://uniroma1.academia.edu/DonatellaMagri?f_ri=400","photo":"https://0.academia-photos.com/3421427/10110370/11280589/s65_donatella.magri.jpg"}],"research_interests":[{"id":400,"name":"Earth Sciences","url":"https://www.academia.edu/Documents/in/Earth_Sciences?f_ri=400","nofollow":false},{"id":772,"name":"Human Evolution","url":"https://www.academia.edu/Documents/in/Human_Evolution?f_ri=400","nofollow":false},{"id":28157,"name":"Environmental Change","url":"https://www.academia.edu/Documents/in/Environmental_Change?f_ri=400","nofollow":false},{"id":93755,"name":"History and archaeology","url":"https://www.academia.edu/Documents/in/History_and_archaeology?f_ri=400","nofollow":false},{"id":256351,"name":"Plant population ecology","url":"https://www.academia.edu/Documents/in/Plant_population_ecology?f_ri=400"},{"id":373417,"name":"Quaternary Science Reviews","url":"https://www.academia.edu/Documents/in/Quaternary_Science_Reviews?f_ri=400"}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_18946483" data-work_id="18946483" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/18946483/Development_and_validation_of_a_gas_chromatography_negative_chemical_ionization_tandem_mass_spectrometry_method_for_the_determination_of_ethyl_glucuronide_in_hair_and_its_application_to_forensic_toxicology">Development and validation of a gas chromatography–negative chemical ionization tandem mass spectrometry method for the determination of ethyl glucuronide in hair and its application to forensic toxicology</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest"><div class="summarized">Ethyl glucuronide (EtG) is a minor and direct metabolite of ethanol. EtG is incorporated into the growing hair allowing retrospective investigation of chronic alcohol abuse. In this study, we report the development and the validation of a... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_18946483" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">Ethyl glucuronide (EtG) is a minor and direct metabolite of ethanol. EtG is incorporated into the growing hair allowing retrospective investigation of chronic alcohol abuse. In this study, we report the development and the validation of a method using gas chromatography–negative chemical ionization tandem mass spectrometry (GC–NCI-MS/MS) for the quantification of EtG in hair. EtG was extracted from about 30mg</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/18946483" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="43283531f31887f5aa95ad5febc46cfb" rel="nofollow" data-download="{"attachment_id":42125395,"asset_id":18946483,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/42125395/download_file?st=MTczMjM2NjYxNyw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="39079515" href="https://independent.academia.edu/MarcAugsburger">Marc Augsburger</a><script data-card-contents-for-user="39079515" type="text/json">{"id":39079515,"first_name":"Marc","last_name":"Augsburger","domain_name":"independent","page_name":"MarcAugsburger","display_name":"Marc Augsburger","profile_url":"https://independent.academia.edu/MarcAugsburger?f_ri=400","photo":"/images/s65_no_pic.png"}</script></span></span></li><li class="js-paper-rank-work_18946483 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="18946483"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 18946483, container: ".js-paper-rank-work_18946483", }); 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EtG is incorporated into the growing hair allowing retrospective investigation of chronic alcohol abuse. In this study, we report the development and the validation of a method using gas chromatography–negative chemical ionization tandem mass spectrometry (GC–NCI-MS/MS) for the quantification of EtG in hair. EtG was extracted from about 30mg","downloadable_attachments":[{"id":42125395,"asset_id":18946483,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":39079515,"first_name":"Marc","last_name":"Augsburger","domain_name":"independent","page_name":"MarcAugsburger","display_name":"Marc Augsburger","profile_url":"https://independent.academia.edu/MarcAugsburger?f_ri=400","photo":"/images/s65_no_pic.png"}],"research_interests":[{"id":400,"name":"Earth Sciences","url":"https://www.academia.edu/Documents/in/Earth_Sciences?f_ri=400","nofollow":false},{"id":524,"name":"Analytical Chemistry","url":"https://www.academia.edu/Documents/in/Analytical_Chemistry?f_ri=400","nofollow":false},{"id":13397,"name":"Forensic Medicine","url":"https://www.academia.edu/Documents/in/Forensic_Medicine?f_ri=400","nofollow":false},{"id":16137,"name":"Food Chemistry","url":"https://www.academia.edu/Documents/in/Food_Chemistry?f_ri=400","nofollow":false},{"id":28235,"name":"Multidisciplinary","url":"https://www.academia.edu/Documents/in/Multidisciplinary?f_ri=400"},{"id":37306,"name":"Quality Control","url":"https://www.academia.edu/Documents/in/Quality_Control?f_ri=400"},{"id":47884,"name":"Biological Sciences","url":"https://www.academia.edu/Documents/in/Biological_Sciences?f_ri=400"},{"id":64568,"name":"Humans","url":"https://www.academia.edu/Documents/in/Humans?f_ri=400"},{"id":80465,"name":"Liquid Liquid Extraction","url":"https://www.academia.edu/Documents/in/Liquid_Liquid_Extraction?f_ri=400"},{"id":83426,"name":"Solid Phase Extraction","url":"https://www.academia.edu/Documents/in/Solid_Phase_Extraction?f_ri=400"},{"id":83996,"name":"Hair","url":"https://www.academia.edu/Documents/in/Hair?f_ri=400"},{"id":98925,"name":"Female","url":"https://www.academia.edu/Documents/in/Female?f_ri=400"},{"id":99234,"name":"Animals","url":"https://www.academia.edu/Documents/in/Animals?f_ri=400"},{"id":100292,"name":"Methamphetamine","url":"https://www.academia.edu/Documents/in/Methamphetamine?f_ri=400"},{"id":111545,"name":"Male","url":"https://www.academia.edu/Documents/in/Male?f_ri=400"},{"id":121705,"name":"Ethanol","url":"https://www.academia.edu/Documents/in/Ethanol?f_ri=400"},{"id":121706,"name":"Amphetamine","url":"https://www.academia.edu/Documents/in/Amphetamine?f_ri=400"},{"id":156594,"name":"Sequential Extraction","url":"https://www.academia.edu/Documents/in/Sequential_Extraction?f_ri=400"},{"id":166448,"name":"Gas Chromatography","url":"https://www.academia.edu/Documents/in/Gas_Chromatography?f_ri=400"},{"id":201241,"name":"Affinity chromatography","url":"https://www.academia.edu/Documents/in/Affinity_chromatography?f_ri=400"},{"id":260118,"name":"CHEMICAL SCIENCES","url":"https://www.academia.edu/Documents/in/CHEMICAL_SCIENCES?f_ri=400"},{"id":289271,"name":"Aged","url":"https://www.academia.edu/Documents/in/Aged?f_ri=400"},{"id":295155,"name":"Middle Aged","url":"https://www.academia.edu/Documents/in/Middle_Aged?f_ri=400"},{"id":326380,"name":"Liquid Chromatography / Electrospray Ionization Mass Spectrometry","url":"https://www.academia.edu/Documents/in/Liquid_Chromatography_Electrospray_Ionization_Mass_Spectrometry?f_ri=400"},{"id":375054,"name":"Rats","url":"https://www.academia.edu/Documents/in/Rats?f_ri=400"},{"id":382075,"name":"Adult","url":"https://www.academia.edu/Documents/in/Adult?f_ri=400"},{"id":391252,"name":"Room 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biology","url":"https://www.academia.edu/Documents/in/Biochemistry_and_cell_biology?f_ri=400"},{"id":1758881,"name":"Analytical Sciences","url":"https://www.academia.edu/Documents/in/Analytical_Sciences?f_ri=400"},{"id":1826013,"name":"Mass Spectrometer","url":"https://www.academia.edu/Documents/in/Mass_Spectrometer?f_ri=400"}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_28851339" data-work_id="28851339" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/28851339/Shorebird_abundance_and_species_diversity_in_natural_intertidal_and_non_tidal_anthropogenic_wetlands_of_the_Colorado_River_Delta_Mexico">Shorebird abundance and species diversity in natural intertidal and non-tidal anthropogenic wetlands of the Colorado River Delta, Mexico</a></div></div><div class="u-pb4x u-mt3x"></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/28851339" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="2dc4b7c13157309f2758a6182dc09fdb" rel="nofollow" data-download="{"attachment_id":49271661,"asset_id":28851339,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" 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Hinojosa-Huerta","profile_url":"https://cornell.academia.edu/OsvelHinojosaHuerta?f_ri=400","photo":"https://0.academia-photos.com/3384091/1141469/1429963/s65_osvel.huerta.jpg"}</script></span></span></li><li class="js-paper-rank-work_28851339 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="28851339"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 28851339, container: ".js-paper-rank-work_28851339", }); });</script></li><li class="js-percentile-work_28851339 InlineList-item InlineList-item--bordered hidden u-tcGrayDark"><span class="percentile-widget hidden"><span class="u-mr2x percentile-widget" style="display: none">•</span><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 28851339; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = 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data-has-card-for-ri="400" href="https://www.academia.edu/Documents/in/Earth_Sciences">Earth Sciences</a>, <script data-card-contents-for-ri="400" type="text/json">{"id":400,"name":"Earth Sciences","url":"https://www.academia.edu/Documents/in/Earth_Sciences?f_ri=400","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="58054" href="https://www.academia.edu/Documents/in/Environmental_Sciences">Environmental Sciences</a><script data-card-contents-for-ri="58054" type="text/json">{"id":58054,"name":"Environmental Sciences","url":"https://www.academia.edu/Documents/in/Environmental_Sciences?f_ri=400","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=28851339]'), work: {"id":28851339,"title":"Shorebird abundance and species diversity in natural intertidal and non-tidal anthropogenic wetlands of the Colorado River Delta, Mexico","created_at":"2016-10-01T10:56:20.207-07:00","url":"https://www.academia.edu/28851339/Shorebird_abundance_and_species_diversity_in_natural_intertidal_and_non_tidal_anthropogenic_wetlands_of_the_Colorado_River_Delta_Mexico?f_ri=400","dom_id":"work_28851339","summary":null,"downloadable_attachments":[{"id":49271661,"asset_id":28851339,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":3384091,"first_name":"Osvel","last_name":"Hinojosa-Huerta","domain_name":"cornell","page_name":"OsvelHinojosaHuerta","display_name":"Osvel Hinojosa-Huerta","profile_url":"https://cornell.academia.edu/OsvelHinojosaHuerta?f_ri=400","photo":"https://0.academia-photos.com/3384091/1141469/1429963/s65_osvel.huerta.jpg"}],"research_interests":[{"id":48,"name":"Engineering","url":"https://www.academia.edu/Documents/in/Engineering?f_ri=400","nofollow":false},{"id":79,"name":"Ecological Engineering","url":"https://www.academia.edu/Documents/in/Ecological_Engineering?f_ri=400","nofollow":false},{"id":400,"name":"Earth Sciences","url":"https://www.academia.edu/Documents/in/Earth_Sciences?f_ri=400","nofollow":false},{"id":58054,"name":"Environmental Sciences","url":"https://www.academia.edu/Documents/in/Environmental_Sciences?f_ri=400","nofollow":false}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_66400725" data-work_id="66400725" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/66400725/Extensive_genetic_population_structure_in_the_Indo_West_Pacific_spot_tail_shark_Carcharhinus_sorrah">Extensive genetic population structure in the Indo–West Pacific spot-tail shark, Carcharhinus sorrah</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest"><div class="summarized">Carcharhinus sorrah (Mülle and Henle, 1839) is a coastal pelagic shark of the tropical and subtropical Indo–West Pacific, reaching 1.6 m total length. The species is widely harvested in line, net, and trawl fisheries over tropical... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_66400725" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">Carcharhinus sorrah (Mülle and Henle, 1839) is a coastal pelagic shark of the tropical and subtropical Indo–West Pacific, reaching 1.6 m total length. The species is widely harvested in line, net, and trawl fisheries over tropical continental shelves. We investigated mtDNA genetic differentiation in C. sorrah across the majority of the species&#39; range, and examined the importance of six major historical and contemporary biogeographic features in shaping population genetic structure in this species. The present study includes dense sampling for a shark species across the Indo–West Pacific, with 349 specimens sampled from 21 collection locations from the northwestern Indian Ocean, Southeast Asia, New Caledonia, and to southerly distribution limits in Australia. Based on 469 base pairs of the control region, we found extensive genetic population structure, with allopatric lineages confined to Australia, New Caledonia, and the remaining surveyed area. Significant genetic subdivisions...</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/66400725" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="416cc2656656a47d029cb0a3458cd090" rel="nofollow" data-download="{"attachment_id":77606360,"asset_id":66400725,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/77606360/download_file?st=MTczMjM2NjYxNyw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="7582180" href="https://independent.academia.edu/DareenAlmojil">Dareen Almojil</a><script data-card-contents-for-user="7582180" type="text/json">{"id":7582180,"first_name":"Dareen","last_name":"Almojil","domain_name":"independent","page_name":"DareenAlmojil","display_name":"Dareen Almojil","profile_url":"https://independent.academia.edu/DareenAlmojil?f_ri=400","photo":"https://0.academia-photos.com/7582180/4052190/4727597/s65_dareen.almojil.jpg"}</script></span></span></li><li class="js-paper-rank-work_66400725 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="66400725"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 66400725, container: ".js-paper-rank-work_66400725", }); 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The species is widely harvested in line, net, and trawl fisheries over tropical continental shelves. We investigated mtDNA genetic differentiation in C. sorrah across the majority of the species\u0026#39; range, and examined the importance of six major historical and contemporary biogeographic features in shaping population genetic structure in this species. The present study includes dense sampling for a shark species across the Indo–West Pacific, with 349 specimens sampled from 21 collection locations from the northwestern Indian Ocean, Southeast Asia, New Caledonia, and to southerly distribution limits in Australia. Based on 469 base pairs of the control region, we found extensive genetic population structure, with allopatric lineages confined to Australia, New Caledonia, and the remaining surveyed area. Significant genetic subdivisions...","downloadable_attachments":[{"id":77606360,"asset_id":66400725,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":7582180,"first_name":"Dareen","last_name":"Almojil","domain_name":"independent","page_name":"DareenAlmojil","display_name":"Dareen Almojil","profile_url":"https://independent.academia.edu/DareenAlmojil?f_ri=400","photo":"https://0.academia-photos.com/7582180/4052190/4727597/s65_dareen.almojil.jpg"}],"research_interests":[{"id":400,"name":"Earth Sciences","url":"https://www.academia.edu/Documents/in/Earth_Sciences?f_ri=400","nofollow":false},{"id":7710,"name":"Biology","url":"https://www.academia.edu/Documents/in/Biology?f_ri=400","nofollow":false},{"id":47884,"name":"Biological Sciences","url":"https://www.academia.edu/Documents/in/Biological_Sciences?f_ri=400","nofollow":false},{"id":58054,"name":"Environmental Sciences","url":"https://www.academia.edu/Documents/in/Environmental_Sciences?f_ri=400","nofollow":false}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_8861845" data-work_id="8861845" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/8861845/DURABILITY_PROPERTIES_OF_STABILIZED_EARTH_BLOCKS">DURABILITY PROPERTIES OF STABILIZED EARTH BLOCKS</a></div></div><div class="u-pb4x u-mt3x"></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/8861845" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="f108724db150fd70c1c0d3e774795f89" rel="nofollow" data-download="{"attachment_id":35197911,"asset_id":8861845,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/35197911/download_file?st=MTczMjM2NjYxNyw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="19387901" href="https://upm-es.academia.edu/webtierra">web tierra</a><script data-card-contents-for-user="19387901" type="text/json">{"id":19387901,"first_name":"web","last_name":"tierra","domain_name":"upm-es","page_name":"webtierra","display_name":"web tierra","profile_url":"https://upm-es.academia.edu/webtierra?f_ri=400","photo":"/images/s65_no_pic.png"}</script></span></span></li><li class="js-paper-rank-work_8861845 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="8861845"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 8861845, container: ".js-paper-rank-work_8861845", }); 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In this paper, the structure and composition of benthic, drifting and marginal macroinvertebrate... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_5247709" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">Aquatic macroinvertebrates living in anastomosing lowland rivers use different habitats and respond differently to the hydrological regime. In this paper, the structure and composition of benthic, drifting and marginal macroinvertebrate assemblages are analyzed in the lowland river Ctalamochita (Córdoba, Argentina). The assemblages were studied in an annual cycle; a comparison among the composition of benthos, drift and marginal fauna was carried out; and size structure of the assemblages was characterized. Samples were obtained from two sites: a rural and an urban site. In total 73 taxa of aquatic macroinvertebrates were collected. Benthos was characterized by Chironomidae and Oligochaeta; marginal fauna was mainly constituted by Coleoptera, Heteroptera, Decapoda, the Trichoptera Nectopsyche sp., Ephemeroptera and Odonata. Drifting assemblage was composed by macroinvertebrates from local and remote upstream benthos, and from the marginal zone. Marginal fauna diversity was higher than benthos and drift. Total biomass of the assemblages pooled together was relatively equitably among size classes. Larger size classes consisted of organisms from the marginal zone whereas the smallest ones were composed by benthic and drifting organisms. In the study area there is habitat partitioning in the lateral dimension of the river. Marginal fauna was more diverse due to the asymmetry of transport and deposit processes, which generate a heterogeneous habitat in the bankside. The relation between fine substrate and high current velocity determines an unstable habitat in the central channel, which makes colonization by benthic macroinvertebrates difficult.</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/5247709" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="62eca77780a6b96a1e2eb7934b9172ff" rel="nofollow" data-download="{"attachment_id":49383714,"asset_id":5247709,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/49383714/download_file?st=MTczMjM2NjYxNyw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="560209" href="https://unrc.academia.edu/MariaCorigliano">Maria Corigliano</a><script data-card-contents-for-user="560209" type="text/json">{"id":560209,"first_name":"Maria","last_name":"Corigliano","domain_name":"unrc","page_name":"MariaCorigliano","display_name":"Maria Corigliano","profile_url":"https://unrc.academia.edu/MariaCorigliano?f_ri=400","photo":"https://0.academia-photos.com/560209/201195/234595/s65_maria.corigliano.jpg"}</script></span></span></li><li class="js-paper-rank-work_5247709 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="5247709"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 5247709, container: ".js-paper-rank-work_5247709", }); 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$(".js-view-count[data-work-id=5247709]").text(description); $(".js-view-count-work_5247709").attr('title', description).tooltip(); }); });</script></span><script>$(function() { $(".js-view-count-work_5247709").removeClass('hidden') })</script></div></li><li class="InlineList-item u-positionRelative" style="max-width: 250px"><div class="u-positionAbsolute" data-has-card-for-ri-list="5247709"><i class="fa fa-tag InlineList-item-icon u-positionRelative"></i>  <a class="InlineList-item-text u-positionRelative">6</a>  </div><span class="InlineList-item-text u-textTruncate u-pl9x"><a class="InlineList-item-text" data-has-card-for-ri="400" href="https://www.academia.edu/Documents/in/Earth_Sciences">Earth Sciences</a>, <script data-card-contents-for-ri="400" type="text/json">{"id":400,"name":"Earth Sciences","url":"https://www.academia.edu/Documents/in/Earth_Sciences?f_ri=400","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="47884" href="https://www.academia.edu/Documents/in/Biological_Sciences">Biological Sciences</a>, <script data-card-contents-for-ri="47884" type="text/json">{"id":47884,"name":"Biological Sciences","url":"https://www.academia.edu/Documents/in/Biological_Sciences?f_ri=400","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="58054" href="https://www.academia.edu/Documents/in/Environmental_Sciences">Environmental Sciences</a>, <script data-card-contents-for-ri="58054" type="text/json">{"id":58054,"name":"Environmental Sciences","url":"https://www.academia.edu/Documents/in/Environmental_Sciences?f_ri=400","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="146915" href="https://www.academia.edu/Documents/in/Chironomidae">Chironomidae</a><script data-card-contents-for-ri="146915" type="text/json">{"id":146915,"name":"Chironomidae","url":"https://www.academia.edu/Documents/in/Chironomidae?f_ri=400","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=5247709]'), work: {"id":5247709,"title":"Benthic, Drifting and Marginal Macroinvertebrate Assemblages in a Lowland River: Temporal and Spatial Variations and Size Structure","created_at":"2013-11-27T21:03:05.905-08:00","url":"https://www.academia.edu/5247709/Benthic_Drifting_and_Marginal_Macroinvertebrate_Assemblages_in_a_Lowland_River_Temporal_and_Spatial_Variations_and_Size_Structure?f_ri=400","dom_id":"work_5247709","summary":"Aquatic macroinvertebrates living in anastomosing lowland rivers use different habitats and respond differently to the hydrological regime. In this paper, the structure and composition of benthic, drifting and marginal macroinvertebrate assemblages are analyzed in the lowland river Ctalamochita (Córdoba, Argentina). The assemblages were studied in an annual cycle; a comparison among the composition of benthos, drift and marginal fauna was carried out; and size structure of the assemblages was characterized. Samples were obtained from two sites: a rural and an urban site. In total 73 taxa of aquatic macroinvertebrates were collected. Benthos was characterized by Chironomidae and Oligochaeta; marginal fauna was mainly constituted by Coleoptera, Heteroptera, Decapoda, the Trichoptera Nectopsyche sp., Ephemeroptera and Odonata. Drifting assemblage was composed by macroinvertebrates from local and remote upstream benthos, and from the marginal zone. Marginal fauna diversity was higher than benthos and drift. Total biomass of the assemblages pooled together was relatively equitably among size classes. Larger size classes consisted of organisms from the marginal zone whereas the smallest ones were composed by benthic and drifting organisms. In the study area there is habitat partitioning in the lateral dimension of the river. Marginal fauna was more diverse due to the asymmetry of transport and deposit processes, which generate a heterogeneous habitat in the bankside. The relation between fine substrate and high current velocity determines an unstable habitat in the central channel, which makes colonization by benthic macroinvertebrates difficult.","downloadable_attachments":[{"id":49383714,"asset_id":5247709,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":560209,"first_name":"Maria","last_name":"Corigliano","domain_name":"unrc","page_name":"MariaCorigliano","display_name":"Maria Corigliano","profile_url":"https://unrc.academia.edu/MariaCorigliano?f_ri=400","photo":"https://0.academia-photos.com/560209/201195/234595/s65_maria.corigliano.jpg"}],"research_interests":[{"id":400,"name":"Earth Sciences","url":"https://www.academia.edu/Documents/in/Earth_Sciences?f_ri=400","nofollow":false},{"id":47884,"name":"Biological Sciences","url":"https://www.academia.edu/Documents/in/Biological_Sciences?f_ri=400","nofollow":false},{"id":58054,"name":"Environmental 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Crowley","profile_url":"https://tcd.academia.edu/QCrowley?f_ri=400","photo":"/images/s65_no_pic.png"}],"research_interests":[{"id":400,"name":"Earth Sciences","url":"https://www.academia.edu/Documents/in/Earth_Sciences?f_ri=400","nofollow":false},{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology?f_ri=400","nofollow":false}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_23748672" data-work_id="23748672" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/23748672/Palaeoproterozoic_to_Neoproterozoic_growth_and_evolution_of_the_eastern_Congo_Craton_Its_role_in_the_Rodinia_puzzle">Palaeoproterozoic to Neoproterozoic growth and evolution of the eastern Congo Craton: Its role in the Rodinia puzzle</a></div></div><div class="u-pb4x u-mt3x"></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/23748672" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="d14ef64cf78435547db048312294c6f5" rel="nofollow" data-download="{"attachment_id":44186421,"asset_id":23748672,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/44186421/download_file?st=MTczMjM2NjYxOCw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="45239226" href="https://curtinedu.academia.edu/BertDeWaele">Bert De Waele</a><script data-card-contents-for-user="45239226" type="text/json">{"id":45239226,"first_name":"Bert","last_name":"De Waele","domain_name":"curtinedu","page_name":"BertDeWaele","display_name":"Bert De Waele","profile_url":"https://curtinedu.academia.edu/BertDeWaele?f_ri=400","photo":"https://0.academia-photos.com/45239226/12007059/13377162/s65_bert.waele.jpg"}</script></span></span></li><li class="js-paper-rank-work_23748672 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="23748672"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 23748672, container: ".js-paper-rank-work_23748672", }); 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$(".js-view-count[data-work-id=23748672]").text(description); $(".js-view-count-work_23748672").attr('title', description).tooltip(); }); });</script></span><script>$(function() { $(".js-view-count-work_23748672").removeClass('hidden') })</script></div></li><li class="InlineList-item u-positionRelative" style="max-width: 250px"><div class="u-positionAbsolute" data-has-card-for-ri-list="23748672"><i class="fa fa-tag InlineList-item-icon u-positionRelative"></i>  <a class="InlineList-item-text u-positionRelative">3</a>  </div><span class="InlineList-item-text u-textTruncate u-pl9x"><a class="InlineList-item-text" data-has-card-for-ri="400" href="https://www.academia.edu/Documents/in/Earth_Sciences">Earth Sciences</a>, <script data-card-contents-for-ri="400" type="text/json">{"id":400,"name":"Earth Sciences","url":"https://www.academia.edu/Documents/in/Earth_Sciences?f_ri=400","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="78114" href="https://www.academia.edu/Documents/in/Precambrian">Precambrian</a>, <script data-card-contents-for-ri="78114" type="text/json">{"id":78114,"name":"Precambrian","url":"https://www.academia.edu/Documents/in/Precambrian?f_ri=400","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="1139408" href="https://www.academia.edu/Documents/in/South_Atlantic">South Atlantic</a><script data-card-contents-for-ri="1139408" type="text/json">{"id":1139408,"name":"South Atlantic","url":"https://www.academia.edu/Documents/in/South_Atlantic?f_ri=400","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=23748672]'), work: {"id":23748672,"title":"Palaeoproterozoic to Neoproterozoic growth and evolution of the eastern Congo Craton: Its role in the Rodinia puzzle","created_at":"2016-03-28T20:43:09.209-07:00","url":"https://www.academia.edu/23748672/Palaeoproterozoic_to_Neoproterozoic_growth_and_evolution_of_the_eastern_Congo_Craton_Its_role_in_the_Rodinia_puzzle?f_ri=400","dom_id":"work_23748672","summary":null,"downloadable_attachments":[{"id":44186421,"asset_id":23748672,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":45239226,"first_name":"Bert","last_name":"De Waele","domain_name":"curtinedu","page_name":"BertDeWaele","display_name":"Bert De Waele","profile_url":"https://curtinedu.academia.edu/BertDeWaele?f_ri=400","photo":"https://0.academia-photos.com/45239226/12007059/13377162/s65_bert.waele.jpg"}],"research_interests":[{"id":400,"name":"Earth Sciences","url":"https://www.academia.edu/Documents/in/Earth_Sciences?f_ri=400","nofollow":false},{"id":78114,"name":"Precambrian","url":"https://www.academia.edu/Documents/in/Precambrian?f_ri=400","nofollow":false},{"id":1139408,"name":"South Atlantic","url":"https://www.academia.edu/Documents/in/South_Atlantic?f_ri=400","nofollow":false}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_23180102" data-work_id="23180102" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/23180102/Map_Folio_70_Early_Devonian_Emsian_402_3_Ma_">Map Folio 70 Early Devonian (Emsian, 402.3 Ma)</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest"><div class="summarized">This map folio should be referenced as: Scotese, C.R., 2013. Map Folio 70 Early Devonian (Emsian, 402.3 Ma), PALEOMAP PaleoAtlas for ArcGIS, volume 4, Late Paleozoic Paleogeographic, Paleoclimatic and Plate Tectonic Reconstructions,... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_23180102" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">This map folio should be referenced as:<br />Scotese, C.R., 2013. Map Folio 70 Early Devonian (Emsian, 402.3 Ma), PALEOMAP PaleoAtlas for ArcGIS, volume 4, Late Paleozoic Paleogeographic, Paleoclimatic and Plate Tectonic Reconstructions, PALEOMAP Project, Evanston, IL.<br /><br />Introduction<br />These maps (rectilinear projection) are from the PALEOMAP PaleoAtlas for ArcGIS (Scotese, 2013a-f).  This is a digital atlas of plate tectonic, paleogeographic, and paleoclimatic reconstructions designed for use with the GIS software, ArcMap (ESRI).  Table 1 lists the various types of maps that comprise the PALEOMAP PaleoAtlas.  The maps included in this folio are highlighted in bold text (Table 1).<br />The last map in each folio is a rectilinear graticule that can be overlain on the maps to provide a geographic reference frame.  A rectilinear projection was used because it can be easily georeferenced in ArcMap and transformed into a variety of other map projections.  The rectilinear map projection can also be directly “wrapped” onto a spherical projection, like the oneused by Google Earth. A set of Google Earth paleoglobes has made from the maps in this folio. These Google Earth paleoglobes can be downloaded at: <a href="http://www.globalgeology.com" rel="nofollow">www.globalgeology.com</a>.  <br />If the map you need is missing, or if there doesn’t seem to be a map folio for the exact time interval of interest, please contact me (<a href="mailto:cscotese@gmail.com" rel="nofollow">cscotese@gmail.com</a>). Table 2 lists all the time intervals that comprise the PALEOMAP PaleoAtlas for ArcGIS. The PaleoAtlas contains one map for every stage in the Phanerozoic, as well as 6 maps for the late Precambrian.  Eventually, Map Folios, like this one, will be published for every time interval in the PALEOMAP PaleoAtlas.  The following section is a brief description of the maps that makeup the Map Folio.</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/23180102" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="34c2e3c4bbad24a2de4cb0a05036f79e" rel="nofollow" data-download="{"attachment_id":43665977,"asset_id":23180102,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/43665977/download_file?st=MTczMjM2NjYxOCw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="21510336" href="https://uta.academia.edu/ChristopherScotese">Christopher Scotese</a><script data-card-contents-for-user="21510336" type="text/json">{"id":21510336,"first_name":"Christopher","last_name":"Scotese","domain_name":"uta","page_name":"ChristopherScotese","display_name":"Christopher Scotese","profile_url":"https://uta.academia.edu/ChristopherScotese?f_ri=400","photo":"https://0.academia-photos.com/21510336/5916564/6717945/s65_christopher.scotese.jpg_oh_ae484ccc511c6f7c218a12ce7ab55104_oe_55181a85___gda___1424411645_ce1ec2f4e41562d45bd92df483d11bf8"}</script></span></span></li><li class="js-paper-rank-work_23180102 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="23180102"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 23180102, container: ".js-paper-rank-work_23180102", }); 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$(".js-view-count[data-work-id=23180102]").text(description); $(".js-view-count-work_23180102").attr('title', description).tooltip(); }); });</script></span><script>$(function() { $(".js-view-count-work_23180102").removeClass('hidden') })</script></div></li><li class="InlineList-item u-positionRelative" style="max-width: 250px"><div class="u-positionAbsolute" data-has-card-for-ri-list="23180102"><i class="fa fa-tag InlineList-item-icon u-positionRelative"></i>  <a class="InlineList-item-text u-positionRelative">18</a>  </div><span class="InlineList-item-text u-textTruncate u-pl10x"><a class="InlineList-item-text" data-has-card-for-ri="400" href="https://www.academia.edu/Documents/in/Earth_Sciences">Earth Sciences</a>, <script data-card-contents-for-ri="400" type="text/json">{"id":400,"name":"Earth Sciences","url":"https://www.academia.edu/Documents/in/Earth_Sciences?f_ri=400","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="406" href="https://www.academia.edu/Documents/in/Geology">Geology</a>, <script data-card-contents-for-ri="406" type="text/json">{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology?f_ri=400","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="417" href="https://www.academia.edu/Documents/in/Paleontology">Paleontology</a>, <script data-card-contents-for-ri="417" type="text/json">{"id":417,"name":"Paleontology","url":"https://www.academia.edu/Documents/in/Paleontology?f_ri=400","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="2119" href="https://www.academia.edu/Documents/in/Paleomagnetism">Paleomagnetism</a><script data-card-contents-for-ri="2119" type="text/json">{"id":2119,"name":"Paleomagnetism","url":"https://www.academia.edu/Documents/in/Paleomagnetism?f_ri=400","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=23180102]'), work: {"id":23180102,"title":"Map Folio 70 Early Devonian (Emsian, 402.3 Ma)","created_at":"2016-03-12T13:55:45.991-08:00","url":"https://www.academia.edu/23180102/Map_Folio_70_Early_Devonian_Emsian_402_3_Ma_?f_ri=400","dom_id":"work_23180102","summary":"This map folio should be referenced as:\nScotese, C.R., 2013. Map Folio 70 Early Devonian (Emsian, 402.3 Ma), PALEOMAP PaleoAtlas for ArcGIS, volume 4, Late Paleozoic Paleogeographic, Paleoclimatic and Plate Tectonic Reconstructions, PALEOMAP Project, Evanston, IL.\n\nIntroduction\nThese maps (rectilinear projection) are from the PALEOMAP PaleoAtlas for ArcGIS (Scotese, 2013a-f). This is a digital atlas of plate tectonic, paleogeographic, and paleoclimatic reconstructions designed for use with the GIS software, ArcMap (ESRI). Table 1 lists the various types of maps that comprise the PALEOMAP PaleoAtlas. The maps included in this folio are highlighted in bold text (Table 1).\nThe last map in each folio is a rectilinear graticule that can be overlain on the maps to provide a geographic reference frame. A rectilinear projection was used because it can be easily georeferenced in ArcMap and transformed into a variety of other map projections. The rectilinear map projection can also be directly “wrapped” onto a spherical projection, like the oneused by Google Earth. A set of Google Earth paleoglobes has made from the maps in this folio. These Google Earth paleoglobes can be downloaded at: www.globalgeology.com. \nIf the map you need is missing, or if there doesn’t seem to be a map folio for the exact time interval of interest, please contact me (cscotese@gmail.com). Table 2 lists all the time intervals that comprise the PALEOMAP PaleoAtlas for ArcGIS. The PaleoAtlas contains one map for every stage in the Phanerozoic, as well as 6 maps for the late Precambrian. Eventually, Map Folios, like this one, will be published for every time interval in the PALEOMAP PaleoAtlas. The following section is a brief description of the maps that makeup the Map Folio.\n","downloadable_attachments":[{"id":43665977,"asset_id":23180102,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":21510336,"first_name":"Christopher","last_name":"Scotese","domain_name":"uta","page_name":"ChristopherScotese","display_name":"Christopher Scotese","profile_url":"https://uta.academia.edu/ChristopherScotese?f_ri=400","photo":"https://0.academia-photos.com/21510336/5916564/6717945/s65_christopher.scotese.jpg_oh_ae484ccc511c6f7c218a12ce7ab55104_oe_55181a85___gda___1424411645_ce1ec2f4e41562d45bd92df483d11bf8"}],"research_interests":[{"id":400,"name":"Earth 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design and “natural” disasters</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest"><div class="summarized">This article analyzes the processes of risk visualization characterizing disaster risk reduction policies and, in particular, the digital artifacts the international world of disaster management uses in an effort to view threats to the... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_31225596" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">This article analyzes the processes of risk visualization characterizing disaster risk reduction policies and, in particular, the digital artifacts the international world of disaster management uses in an effort to view threats to the planet and render them open to human experience. The purpose of these artifacts is to foster experiences that grant both quantitative shape and social form to the nature of global risks. Tangible Earth, the first interactive digital globe, is the most sophisticated of these artifacts in that it strives to gather a wide, varied audience of humans and enroll them in co-producing the risks affecting the Earth. This process of delving into experiences of the globe as mediated by digital equipment mobilizes diverse ontologies: there is a “naturalist ontology” that represents nature as independent of the social sphere, as a force that remains insurgent and unpredictable despite efforts to quantitatively capture it through earth-monitoring instruments and probabilistic calculations, and there is also an “analogist ontology” in which nature is cast as indistinguishable from the social sphere on the grounds that both human and non-human collectives share the same propensity for resilience.</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/31225596" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="66c2928524a615b9922df3654676ecec" rel="nofollow" data-download="{"attachment_id":51792943,"asset_id":31225596,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/51792943/download_file?st=MTczMjM2NjYxOCw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="4651717" href="https://unict.academia.edu/MaraBenadusi">Mara Benadusi</a><script data-card-contents-for-user="4651717" type="text/json">{"id":4651717,"first_name":"Mara","last_name":"Benadusi","domain_name":"unict","page_name":"MaraBenadusi","display_name":"Mara Benadusi","profile_url":"https://unict.academia.edu/MaraBenadusi?f_ri=400","photo":"https://0.academia-photos.com/4651717/1951404/16241036/s65_mara.benadusi.jpg"}</script></span></span></li><li class="js-paper-rank-work_31225596 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="31225596"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 31225596, container: ".js-paper-rank-work_31225596", }); 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This process of delving into experiences of the globe as mediated by digital equipment mobilizes diverse ontologies: there is a “naturalist ontology” that represents nature as independent of the social sphere, as a force that remains insurgent and unpredictable despite efforts to quantitatively capture it through earth-monitoring instruments and probabilistic calculations, and there is also an “analogist ontology” in which nature is cast as indistinguishable from the social sphere on the grounds that both human and non-human collectives share the same propensity for resilience.","downloadable_attachments":[{"id":51792943,"asset_id":31225596,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":4651717,"first_name":"Mara","last_name":"Benadusi","domain_name":"unict","page_name":"MaraBenadusi","display_name":"Mara 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Anthropology","url":"https://www.academia.edu/Documents/in/Environmental_Anthropology?f_ri=400"},{"id":92179,"name":"Anthropology of Disasters","url":"https://www.academia.edu/Documents/in/Anthropology_of_Disasters?f_ri=400"},{"id":126587,"name":"Disaster Culture","url":"https://www.academia.edu/Documents/in/Disaster_Culture?f_ri=400"},{"id":965327,"name":"Natural Disasters Reduction","url":"https://www.academia.edu/Documents/in/Natural_Disasters_Reduction?f_ri=400"}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_40374350" data-work_id="40374350" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" 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work_20811342" data-work_id="20811342" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/20811342/ANCIENT_INDIAN_FLYING_MACHINES_vymnika_shastra_">ANCIENT INDIAN FLYING MACHINES (vymnika shastra)</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest"><div class="summarized">It is a precious knowledge of ancient india. this script was originally composed by mahrshi BHARADWAJA, the great indian sage around 5000 BC ,it content english transtation of some of its sanskrit stotras and shlokas.before wright... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_20811342" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">It is a precious knowledge of ancient india. this script was originally composed by mahrshi BHARADWAJA, the great indian sage around 5000 BC  ,it content english transtation of some of its sanskrit stotras and shlokas.before wright brothers first aircraft was made by dr Talpade was an Indian scholar who is said to have constructed and flown an unmanned airplane in 1895 with reference of this ancient hindu sanskrit manuscript .</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/20811342" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="ad57fb8dd9d160969d6c2f23c6da412c" rel="nofollow" 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data-has-card-for-ri="5769" href="https://www.academia.edu/Documents/in/Mass_Spectrometry">Mass Spectrometry</a>, <script data-card-contents-for-ri="5769" type="text/json">{"id":5769,"name":"Mass Spectrometry","url":"https://www.academia.edu/Documents/in/Mass_Spectrometry?f_ri=400","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="118582" href="https://www.academia.edu/Documents/in/Physical_sciences">Physical sciences</a>, <script data-card-contents-for-ri="118582" type="text/json">{"id":118582,"name":"Physical sciences","url":"https://www.academia.edu/Documents/in/Physical_sciences?f_ri=400","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="309434" href="https://www.academia.edu/Documents/in/Solar_System">Solar System</a><script data-card-contents-for-ri="309434" type="text/json">{"id":309434,"name":"Solar 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u-pv7x u-mb0x js-work-card work_12583504" data-work_id="12583504" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/12583504/A_review_of_palaeoclimates_and_palaeoenvironments_in_the_Levant_and_Eastern_Mediterranean_from_25_000_to_5000_years_BP_setting_the_environmental_background_for_the_evolution_of_human_civilisation">A review of palaeoclimates and palaeoenvironments in the Levant and Eastern Mediterranean from 25,000 to 5000 years BP: setting the environmental background for the evolution of human civilisation</a></div></div><div class="u-pb4x u-mt3x"></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/12583504" 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})();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_13363632" data-work_id="13363632" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/13363632/Simulation_of_hybrid_forest_tree_breeding_strategies">Simulation of hybrid forest tree breeding strategies</a></div></div><div class="u-pb4x u-mt3x"></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/13363632" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" 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data-has-card-for-user="32581772" href="https://scionresearch.academia.edu/HeidiDungey">Heidi Dungey</a><script data-card-contents-for-user="32581772" type="text/json">{"id":32581772,"first_name":"Heidi","last_name":"Dungey","domain_name":"scionresearch","page_name":"HeidiDungey","display_name":"Heidi Dungey","profile_url":"https://scionresearch.academia.edu/HeidiDungey?f_ri=400","photo":"/images/s65_no_pic.png"}</script></span></span></li><li class="js-paper-rank-work_13363632 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="13363632"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 13363632, container: ".js-paper-rank-work_13363632", }); });</script></li><li class="js-percentile-work_13363632 InlineList-item InlineList-item--bordered hidden u-tcGrayDark"><span class="percentile-widget hidden"><span class="u-mr2x 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Sciences</a><script data-card-contents-for-ri="58054" type="text/json">{"id":58054,"name":"Environmental Sciences","url":"https://www.academia.edu/Documents/in/Environmental_Sciences?f_ri=400","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=13363632]'), work: {"id":13363632,"title":"Simulation of hybrid forest tree breeding strategies","created_at":"2015-06-27T15:15:22.130-07:00","url":"https://www.academia.edu/13363632/Simulation_of_hybrid_forest_tree_breeding_strategies?f_ri=400","dom_id":"work_13363632","summary":null,"downloadable_attachments":[{"id":45430751,"asset_id":13363632,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":32581772,"first_name":"Heidi","last_name":"Dungey","domain_name":"scionresearch","page_name":"HeidiDungey","display_name":"Heidi Dungey","profile_url":"https://scionresearch.academia.edu/HeidiDungey?f_ri=400","photo":"/images/s65_no_pic.png"}],"research_interests":[{"id":400,"name":"Earth Sciences","url":"https://www.academia.edu/Documents/in/Earth_Sciences?f_ri=400","nofollow":false},{"id":58054,"name":"Environmental Sciences","url":"https://www.academia.edu/Documents/in/Environmental_Sciences?f_ri=400","nofollow":false}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_80045689" data-work_id="80045689" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/80045689/Quando_il_mondo_scal%C3%B2_il_Sublime">Quando il mondo scalò il Sublime</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest"><div class="summarized">In the 19th century, a unique combination of scientific, social, political and cultural factors attracted crowds of visitors from all over the world to the Dolomite Mountains. This phenomenon had its epicenter in Fiemme Valley and in the... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_80045689" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">In the 19th century, a unique combination of scientific, social, political and cultural factors attracted crowds of visitors from all over the world to the Dolomite Mountains. This phenomenon had its epicenter in Fiemme Valley and in the town of Predazzo, where Michele Giacomelli and his family hosted a great number of these travelers in their hotel: the Nave d’Oro. <br />This book features a critical edition of the first manuscript volume of the guestbook of the hotel, the Memoriale (1820–1875): a document where countless characters intertwined their lives, jobs, works, and passions. A stratification of social and cultural contexts, languages and events which make this manuscript a precious source for understanding a crucial chapter in Italian and European history.</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/80045689" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="b4510f335f652ec5389a11f8b1a30fc0" rel="nofollow" data-download="{"attachment_id":86557762,"asset_id":80045689,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/86557762/download_file?st=MTczMjM2NjYxOCw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="972141" href="https://unive.academia.edu/FrancescoLuzzini">Francesco Luzzini</a><script data-card-contents-for-user="972141" type="text/json">{"id":972141,"first_name":"Francesco","last_name":"Luzzini","domain_name":"unive","page_name":"FrancescoLuzzini","display_name":"Francesco Luzzini","profile_url":"https://unive.academia.edu/FrancescoLuzzini?f_ri=400","photo":"https://0.academia-photos.com/972141/354109/149888785/s65_francesco.luzzini.jpg"}</script></span></span></li><li class="js-paper-rank-work_80045689 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="80045689"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 80045689, container: ".js-paper-rank-work_80045689", }); 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This phenomenon had its epicenter in Fiemme Valley and in the town of Predazzo, where Michele Giacomelli and his family hosted a great number of these travelers in their hotel: the Nave d’Oro.\r\nThis book features a critical edition of the first manuscript volume of the guestbook of the hotel, the Memoriale (1820–1875): a document where countless characters intertwined their lives, jobs, works, and passions. A stratification of social and cultural contexts, languages and events which make this manuscript a precious source for understanding a crucial chapter in Italian and European history.","downloadable_attachments":[{"id":86557762,"asset_id":80045689,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":972141,"first_name":"Francesco","last_name":"Luzzini","domain_name":"unive","page_name":"FrancescoLuzzini","display_name":"Francesco Luzzini","profile_url":"https://unive.academia.edu/FrancescoLuzzini?f_ri=400","photo":"https://0.academia-photos.com/972141/354109/149888785/s65_francesco.luzzini.jpg"}],"research_interests":[{"id":131,"name":"European History","url":"https://www.academia.edu/Documents/in/European_History?f_ri=400","nofollow":false},{"id":400,"name":"Earth 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class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="6546466" href="https://independent.academia.edu/victorlukhele">victor lukhele</a><script data-card-contents-for-user="6546466" type="text/json">{"id":6546466,"first_name":"victor","last_name":"lukhele","domain_name":"independent","page_name":"victorlukhele","display_name":"victor lukhele","profile_url":"https://independent.academia.edu/victorlukhele?f_ri=400","photo":"/images/s65_no_pic.png"}</script></span></span></li><li class="js-paper-rank-work_4964144 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="4964144"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 4964144, container: 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})();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_33326937" data-work_id="33326937" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/33326937/The_Earth_isnt_flat_but_much_bigger_than_we_are_told_update_04_06_17_">The Earth isn't flat but much bigger than we are told (update 04 06 17)</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest"><div class="summarized">The Earth isn't flat, but much bigger than we are told. The earth is a part of something much bigger. Therefore, it seems flat, but that's because of the scale. There are many continents, and 33 of them were camouflaged through our... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_33326937" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">The Earth isn't flat, but much bigger than we are told. The earth is a part of something much bigger. Therefore, it seems flat, but that's because of the scale. There are many continents, and 33 of them were camouflaged through our classic earth model, by bending them inward through Antarctica. This is where the term 'hollow earth' comes from.</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/33326937" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="13e01dcbe76cc923eb5259728695a76f" rel="nofollow" data-download="{"attachment_id":53388235,"asset_id":33326937,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/53388235/download_file?st=MTczMjM2NjYxOCw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="16005828" href="https://ulg.academia.edu/DavidVanderper">David Vanderper</a><script data-card-contents-for-user="16005828" type="text/json">{"id":16005828,"first_name":"David","last_name":"Vanderper","domain_name":"ulg","page_name":"DavidVanderper","display_name":"David Vanderper","profile_url":"https://ulg.academia.edu/DavidVanderper?f_ri=400","photo":"https://0.academia-photos.com/16005828/4341433/19170987/s65_david.vanderper.jpg"}</script></span></span></li><li class="js-paper-rank-work_33326937 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="33326937"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 33326937, container: ".js-paper-rank-work_33326937", }); 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The earth is a part of something much bigger. Therefore, it seems flat, but that's because of the scale. There are many continents, and 33 of them were camouflaged through our classic earth model, by bending them inward through Antarctica. This is where the term 'hollow earth' comes from.","downloadable_attachments":[{"id":53388235,"asset_id":33326937,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":16005828,"first_name":"David","last_name":"Vanderper","domain_name":"ulg","page_name":"DavidVanderper","display_name":"David Vanderper","profile_url":"https://ulg.academia.edu/DavidVanderper?f_ri=400","photo":"https://0.academia-photos.com/16005828/4341433/19170987/s65_david.vanderper.jpg"}],"research_interests":[{"id":128,"name":"History","url":"https://www.academia.edu/Documents/in/History?f_ri=400","nofollow":false},{"id":280,"name":"Cartography","url":"https://www.academia.edu/Documents/in/Cartography?f_ri=400","nofollow":false},{"id":400,"name":"Earth Sciences","url":"https://www.academia.edu/Documents/in/Earth_Sciences?f_ri=400","nofollow":false},{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology?f_ri=400","nofollow":false},{"id":6756,"name":"Conspiracy Theories","url":"https://www.academia.edu/Documents/in/Conspiracy_Theories?f_ri=400"},{"id":28442,"name":"Matrix Theory","url":"https://www.academia.edu/Documents/in/Matrix_Theory?f_ri=400"},{"id":54534,"name":"Humanity","url":"https://www.academia.edu/Documents/in/Humanity?f_ri=400"},{"id":57487,"name":"Antarctica","url":"https://www.academia.edu/Documents/in/Antarctica?f_ri=400"},{"id":229775,"name":"Old Maps","url":"https://www.academia.edu/Documents/in/Old_Maps?f_ri=400"},{"id":453325,"name":"Nazis","url":"https://www.academia.edu/Documents/in/Nazis?f_ri=400"},{"id":812440,"name":"NWO","url":"https://www.academia.edu/Documents/in/NWO?f_ri=400"},{"id":1649422,"name":"Admiral Byrd","url":"https://www.academia.edu/Documents/in/Admiral_Byrd?f_ri=400"}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_74337573" data-work_id="74337573" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/74337573/Distinguishing_wild_from_cultivated_agarwood_Aquilaria_spp_using_direct_analysis_in_real_time_and_time_of_flight_mass_spectrometry">Distinguishing wild from cultivated agarwood ( Aquilaria spp.) using direct analysis in real time and time of-flight mass spectrometry</a></div></div><div class="u-pb4x u-mt3x"></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/74337573" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="dc9f549b27a9f3a2e264d20104a1c2cd" rel="nofollow" data-download="{"attachment_id":82525493,"asset_id":74337573,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/82525493/download_file?st=MTczMjM2NjYxOCw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="25321912" href="https://utah.academia.edu/CadyLancaster">Cady Lancaster</a><script data-card-contents-for-user="25321912" type="text/json">{"id":25321912,"first_name":"Cady","last_name":"Lancaster","domain_name":"utah","page_name":"CadyLancaster","display_name":"Cady Lancaster","profile_url":"https://utah.academia.edu/CadyLancaster?f_ri=400","photo":"https://0.academia-photos.com/25321912/20668909/20256215/s65_cady.lancaster.jpg"}</script></span></span></li><li class="js-paper-rank-work_74337573 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="74337573"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 74337573, container: ".js-paper-rank-work_74337573", }); 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Part I: Coerced to Cooperate with the Negative Aliens</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest"><div class="summarized">Over the course of years, and as of more recently, many followers-friends of the author have been asking questions with reference to the Melchizedeks and their role in humanity-Earth Ascension. Below, you will find a sample of such... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_43760869" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">Over the course of years, and as of more recently, many followers-friends of the author have been asking questions with reference to the Melchizedeks and their role in humanity-Earth Ascension. Below, you will find a sample of such questions posted to the author as of more recently, and the response to some of these questions, which were also later posted as slides for the benefit of the all. Herein, via the publication of this paper, you will find a more detailed response to such questions and concerns pertaining to the coerced role of fallen Melchizedeks with reference to cooperating with the negative aliens.</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/43760869" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="94b0d1945f50b97b74db0551d9178cb9" rel="nofollow" data-download="{"attachment_id":101445600,"asset_id":43760869,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/101445600/download_file?st=MTczMjM2NjYxOCw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="49852223" href="https://independent.academia.edu/MohsenPaulSarfarazi">Mohsen Paul Sarfarazi</a><script data-card-contents-for-user="49852223" type="text/json">{"id":49852223,"first_name":"Mohsen Paul","last_name":"Sarfarazi","domain_name":"independent","page_name":"MohsenPaulSarfarazi","display_name":"Mohsen Paul Sarfarazi","profile_url":"https://independent.academia.edu/MohsenPaulSarfarazi?f_ri=400","photo":"https://0.academia-photos.com/49852223/14993974/15735910/s65_mohsen_paul.sarfarazi.jpg"}</script></span></span></li><li class="js-paper-rank-work_43760869 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="43760869"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 43760869, container: ".js-paper-rank-work_43760869", }); 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Part I: Coerced to Cooperate with the Negative Aliens","created_at":"2020-08-01T09:13:09.720-07:00","url":"https://www.academia.edu/43760869/Who_are_the_Fallen_Melchizedeks_Part_I_Coerced_to_Cooperate_with_the_Negative_Aliens?f_ri=400","dom_id":"work_43760869","summary":"Over the course of years, and as of more recently, many followers-friends of the author have been asking questions with reference to the Melchizedeks and their role in humanity-Earth Ascension. Below, you will find a sample of such questions posted to the author as of more recently, and the response to some of these questions, which were also later posted as slides for the benefit of the all. 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