{"id":458,"date":"2025-05-13T11:04:29","date_gmt":"2025-05-13T09:04:29","guid":{"rendered":"https:\/\/site.uit.no\/palaeoarc2025\/?page_id=458"},"modified":"2025-05-23T08:51:14","modified_gmt":"2025-05-23T06:51:14","slug":"posters","status":"publish","type":"page","link":"https:\/\/site.uit.no\/palaeoarc2025\/posters\/","title":{"rendered":"Poster presentations"},"content":{"rendered":"

[et_pb_section fb_built=”1″ _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”][et_pb_row _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”][et_pb_column type=”4_4″ _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”][et_pb_heading title=”Poster Presentations” _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”][\/et_pb_heading][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”]<\/p>\n

The poster session will take place on Tuesday, June 3rd, from 15:30 to 18:00 in the Medicine and Health Studies (MH) building<\/span>. Accepted abstract titles are listed below.<\/p>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_4,3_4″ use_custom_gutter=”on” gutter_width=”1″ make_equal=”on” _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”20px||20px||false|false” global_colors_info=”{}”][et_pb_column type=”1_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Griselda Anglada-Ortiz<\/strong><\/p>\n

[\/et_pb_text][\/et_pb_column][et_pb_column type=”3_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Planktic calcifiers: from living assemblages to proxies in the Arctic Ocean<\/p>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_4,3_4″ use_custom_gutter=”on” gutter_width=”1″ make_equal=”on” _builder_version=”4.27.4″ _module_preset=”default” background_color=”#e0eaff” custom_padding=”20px||20px||false|false” global_colors_info=”{}”][et_pb_column type=”1_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Satu Anttila<\/strong><\/p>\n

[\/et_pb_text][\/et_pb_column][et_pb_column type=”3_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;\t” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Preliminary results of mineralogical and geochemical properties of glaciolacustrine and marine clays related to the Fennoscandian Ice Sheet<\/p>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_4,3_4″ use_custom_gutter=”on” gutter_width=”1″ make_equal=”on” _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”20px||20px||false|false” global_colors_info=”{}”][et_pb_column type=”1_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Alice Carter-Champion<\/strong><\/p>\n

[\/et_pb_text][\/et_pb_column][et_pb_column type=”3_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Climate change and marine diversity in the Arctic: Holocene insights from the Baffin Bay-Labrador Sea region<\/p>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_4,3_4″ use_custom_gutter=”on” gutter_width=”1″ make_equal=”on” _builder_version=”4.27.4″ _module_preset=”default” background_color=”#e0eaff” custom_padding=”20px||20px||false|false” global_colors_info=”{}”][et_pb_column type=”1_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Gregory De Pascale <\/strong><\/p>\n

[\/et_pb_text][\/et_pb_column][et_pb_column type=”3_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;\t” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Seismotectonic Controls on Postglacial Landslides at the Arctic Circle, Troll Peninsula North Iceland<\/p>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_4,3_4″ use_custom_gutter=”on” gutter_width=”1″ make_equal=”on” _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”20px||20px||false|false” global_colors_info=”{}”][et_pb_column type=”1_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Prasadi De Silva<\/strong><\/p>\n

[\/et_pb_text][\/et_pb_column][et_pb_column type=”3_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Sedimentary evidence for the Storegga tsunami expansion: multi-proxy records from the northwestern Barents Sea<\/p>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_4,3_4″ use_custom_gutter=”on” gutter_width=”1″ make_equal=”on” _builder_version=”4.27.4″ _module_preset=”default” background_color=”#e0eaff” custom_padding=”20px||20px||false|false” global_colors_info=”{}”][et_pb_column type=”1_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Caixa Dong<\/strong><\/p>\n

[\/et_pb_text][\/et_pb_column][et_pb_column type=”3_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;\t” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Organic carbon records in the Western Arctic since the Last Deglaciation: sedimentary evidence from the Canada Basin<\/p>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_4,3_4″ use_custom_gutter=”on” gutter_width=”1″ make_equal=”on” _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”20px||20px||false|false” global_colors_info=”{}”][et_pb_column type=”1_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

V\u00e5rin Tr\u00e6lvik Eilertsen<\/strong><\/p>\n

[\/et_pb_text][\/et_pb_column][et_pb_column type=”3_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Depositional environments in the Kong Karls Trough and Erik Eriksenstredet in the northern Barents Sea, from the last glacial to the present<\/p>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_4,3_4″ use_custom_gutter=”on” gutter_width=”1″ make_equal=”on” _builder_version=”4.27.4″ _module_preset=”default” background_color=”#e0eaff” custom_padding=”20px||20px||false|false” global_colors_info=”{}”][et_pb_column type=”1_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Lena Friedrich<\/strong><\/p>\n

[\/et_pb_text][\/et_pb_column][et_pb_column type=”3_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;\t” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Speleothem Fluid Inclusions as Proxies for Miocene Palaeoprecipitation and Palaeotemperature in Eastern North Greenland<\/p>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_4,3_4″ use_custom_gutter=”on” gutter_width=”1″ make_equal=”on” _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”20px||20px||false|false” global_colors_info=”{}”][et_pb_column type=”1_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Christine T\u00f8mmervik Kollsg\u00e5rd<\/strong><\/p>\n

[\/et_pb_text][\/et_pb_column][et_pb_column type=”3_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Sand migration in the southern part of the Norwegian North Sea<\/p>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_4,3_4″ use_custom_gutter=”on” gutter_width=”1″ make_equal=”on” _builder_version=”4.27.4″ _module_preset=”default” background_color=”#e0eaff” custom_padding=”20px||20px||false|false” global_colors_info=”{}”][et_pb_column type=”1_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Julie Lattaud<\/strong><\/p>\n

[\/et_pb_text][\/et_pb_column][et_pb_column type=”3_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;\t” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Boreal forest fires recorded in 3000 yr Arctic delta sediments<\/p>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_4,3_4″ use_custom_gutter=”on” gutter_width=”1″ make_equal=”on” _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”20px||20px||false|false” global_colors_info=”{}”][et_pb_column type=”1_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Christine Lockwood-Ireland<\/strong><\/p>\n

[\/et_pb_text][\/et_pb_column][et_pb_column type=”3_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Suppressed Nordic Seas convection and bottom water warmings during Greenland stadials: driving mechanisms<\/p>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_4,3_4″ use_custom_gutter=”on” gutter_width=”1″ make_equal=”on” _builder_version=”4.27.4″ _module_preset=”default” background_color=”#e0eaff” custom_padding=”20px||20px||false|false” global_colors_info=”{}”][et_pb_column type=”1_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Gregor Luetzenburg<\/strong><\/p>\n

[\/et_pb_text][\/et_pb_column][et_pb_column type=”3_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;\t” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Greenland\u2019s Holocene Deglacial Marine Limit and Relative Sea Level Changes Decoded<\/p>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_4,3_4″ use_custom_gutter=”on” gutter_width=”1″ make_equal=”on” _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”20px||20px||false|false” global_colors_info=”{}”][et_pb_column type=”1_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Andrew Martin<\/strong><\/p>\n

[\/et_pb_text][\/et_pb_column][et_pb_column type=”3_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

The Holocene Arctic Biodiversity Map and database: systematically mapping and harnessing palaeo-data for use in Arctic biodiversity assessments<\/p>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_4,3_4″ use_custom_gutter=”on” gutter_width=”1″ make_equal=”on” _builder_version=”4.27.4″ _module_preset=”default” background_color=”#e0eaff” custom_padding=”20px||20px||false|false” global_colors_info=”{}”][et_pb_column type=”1_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Katarzyna Melaniuk<\/strong><\/p>\n

[\/et_pb_text][\/et_pb_column][et_pb_column type=”3_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;\t” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Currents of Change: Unveiling the 150,000-Year Variability of the East Greenland Current.<\/p>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_4,3_4″ use_custom_gutter=”on” gutter_width=”1″ make_equal=”on” _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”20px||20px||false|false” global_colors_info=”{}”][et_pb_column type=”1_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Matthias Nyfeler<\/strong><\/p>\n

[\/et_pb_text][\/et_pb_column][et_pb_column type=”3_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Weichselian deglaciation of And\u00f8ya, North Norway<\/p>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_4,3_4″ use_custom_gutter=”on” gutter_width=”1″ make_equal=”on” _builder_version=”4.27.4″ _module_preset=”default” background_color=”#e0eaff” custom_padding=”20px||20px||false|false” global_colors_info=”{}”][et_pb_column type=”1_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Rachel Oien<\/strong><\/p>\n

[\/et_pb_text][\/et_pb_column][et_pb_column type=”3_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;\t” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Reconstructing Peripheral Glacier Persistence during Holocene Climate Transitions, Lofoten and Sortland, Norway<\/p>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_4,3_4″ use_custom_gutter=”on” gutter_width=”1″ make_equal=”on” _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”20px||20px||false|false” global_colors_info=”{}”][et_pb_column type=”1_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Henry Patton<\/strong><\/p>\n

[\/et_pb_text][\/et_pb_column][et_pb_column type=”3_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Quaternary landscape development of the Eurasian Arctic<\/p>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_4,3_4″ use_custom_gutter=”on” gutter_width=”1″ make_equal=”on” _builder_version=”4.27.4″ _module_preset=”default” background_color=”#e0eaff” custom_padding=”20px||20px||false|false” global_colors_info=”{}”][et_pb_column type=”1_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Ma\u00eflys Picard<\/strong><\/p>\n

[\/et_pb_text][\/et_pb_column][et_pb_column type=”3_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;\t” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Reconstituting rising anoxia using molecular paleoecology – an Arctic and local case study<\/p>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_4,3_4″ use_custom_gutter=”on” gutter_width=”1″ make_equal=”on” _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”20px||20px||false|false” global_colors_info=”{}”][et_pb_column type=”1_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Elena Popova<\/strong><\/p>\n

[\/et_pb_text][\/et_pb_column][et_pb_column type=”3_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Magnetostratigraphy of Pliocene-Quaternary sediments across the Mendeleev Ridge, the Podvodnikov Basin, and the Lomonosov Ridge (Central Arctic Ocean)<\/p>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_4,3_4″ use_custom_gutter=”on” gutter_width=”1″ make_equal=”on” _builder_version=”4.27.4″ _module_preset=”default” background_color=”#e0eaff” custom_padding=”20px||20px||false|false” global_colors_info=”{}”][et_pb_column type=”1_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Jakob Reif<\/strong><\/p>\n

[\/et_pb_text][\/et_pb_column][et_pb_column type=”3_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;\t” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Constraining the timing and spatial extent of the Troms\u00f8-Lyngen stage in Troms, Northern Norway, using threshold lakes<\/p>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_4,3_4″ use_custom_gutter=”on” gutter_width=”1″ make_equal=”on” _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”20px||20px||false|false” global_colors_info=”{}”][et_pb_column type=”1_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Mat\u011bj Roman<\/strong><\/p>\n

[\/et_pb_text][\/et_pb_column][et_pb_column type=”3_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Multi-proxy Holocene lacustrine sedimentary records from\u00a0S\u00f8r-Varanger, bridging the Arctic tree-line ecocline<\/p>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_4,3_4″ use_custom_gutter=”on” gutter_width=”1″ make_equal=”on” _builder_version=”4.27.4″ _module_preset=”default” background_color=”#e0eaff” custom_padding=”20px||20px||false|false” global_colors_info=”{}”][et_pb_column type=”1_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Paulina Romel<\/strong><\/p>\n

[\/et_pb_text][\/et_pb_column][et_pb_column type=”3_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;\t” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Early Holocene marine ecosystem changes in the western Canadian Arctic Archipelago based on foraminiferal analysis \u2013 preliminary results<\/p>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_4,3_4″ use_custom_gutter=”on” gutter_width=”1″ make_equal=”on” _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”20px||20px||false|false” global_colors_info=”{}”][et_pb_column type=”1_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Astrid Rosenberg Hansen<\/strong><\/p>\n

[\/et_pb_text][\/et_pb_column][et_pb_column type=”3_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]Constraining the timing of the Last Glacial Maximum in Greenland using inverse modelling of in situ 14<\/sup>C measurements[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_4,3_4″ use_custom_gutter=”on” gutter_width=”1″ make_equal=”on” _builder_version=”4.27.4″ _module_preset=”default” background_color=”#e0eaff” custom_padding=”20px||20px||false|false” global_colors_info=”{}”][et_pb_column type=”1_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Abhinav Roy<\/strong><\/p>\n

[\/et_pb_text][\/et_pb_column][et_pb_column type=”3_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;\t” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Recent Foraminiferal Assemblages and Environmental Change in Krossfjorden, Svalbard<\/p>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_4,3_4″ use_custom_gutter=”on” gutter_width=”1″ make_equal=”on” _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”20px||20px||false|false” global_colors_info=”{}”][et_pb_column type=”1_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Mathia Sabino<\/strong><\/p>\n

[\/et_pb_text][\/et_pb_column][et_pb_column type=”3_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Insights from long chain diols on organic matter remobilization from collapsing Arctic permafrost<\/p>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_4,3_4″ use_custom_gutter=”on” gutter_width=”1″ make_equal=”on” _builder_version=”4.27.4″ _module_preset=”default” background_color=”#e0eaff” custom_padding=”20px||20px||false|false” global_colors_info=”{}”][et_pb_column type=”1_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Rujian Wang<\/strong><\/p>\n

[\/et_pb_text][\/et_pb_column][et_pb_column type=”3_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;\t” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” hover_enabled=”0″ global_colors_info=”{}” sticky_enabled=”0″]<\/p>\n

Sea ice history in the Western Arctic Ocean over the past 600 ka: reconstruction based on foraminifera and ostracod indicators<\/p>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_4,3_4″ use_custom_gutter=”on” gutter_width=”1″ make_equal=”on” _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”20px||20px||false|false” global_colors_info=”{}”][et_pb_column type=”1_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Anita W\u0142odarczyk<\/strong><\/p>\n

[\/et_pb_text][\/et_pb_column][et_pb_column type=”3_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Spatial Variability of Foraminiferal Assemblages in Surface Sediments of the Northwest Passage, Canadian Arctic<\/p>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_4,3_4″ use_custom_gutter=”on” gutter_width=”1″ make_equal=”on” _builder_version=”4.27.4″ _module_preset=”default” background_color=”#e0eaff” custom_padding=”20px||20px||false|false” global_colors_info=”{}”][et_pb_column type=”1_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Wenshen Xiao<\/strong><\/p>\n

[\/et_pb_text][\/et_pb_column][et_pb_column type=”3_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;\t” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Paleomagnetism and Rock Magnetism in Quaternary Arctic Ocean sediments: implications on Stratigraphy and Environmental reconstructions<\/p>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_4,3_4″ use_custom_gutter=”on” gutter_width=”1″ make_equal=”on” _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”20px||20px||false|false” global_colors_info=”{}”][et_pb_column type=”1_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Xiaotong Xiao<\/strong><\/p>\n

[\/et_pb_text][\/et_pb_column][et_pb_column type=”3_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Centennial sea-ice variability influencing organic carbon sources in the Western Arctic Ocean<\/span><\/p>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_4,3_4″ use_custom_gutter=”on” gutter_width=”1″ make_equal=”on” _builder_version=”4.27.4″ _module_preset=”default” background_color=”#e0eaff” custom_padding=”20px||20px||false|false” global_colors_info=”{}”][et_pb_column type=”1_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px|3px|10px|false|false” global_colors_info=”{}”]<\/p>\n

Defang You<\/strong><\/p>\n

[\/et_pb_text][\/et_pb_column][et_pb_column type=”3_4″ _builder_version=”4.27.4″ _module_preset=”default” custom_css_main_element=”margin: auto;\t” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”|10px||10px|false|false” global_colors_info=”{}”]<\/p>\n

Mediterranean Overflow Water contributed to subsurface warming preceding Heinrich Events<\/p>\n

[\/et_pb_text][\/et_pb_column][\/et_pb_row][\/et_pb_section]<\/p>\n","protected":false},"excerpt":{"rendered":"

The poster session will take place on Tuesday, June 3rd, from 15:30 to 18:00 in the Medicine and Health Studies (MH) building. Accepted abstract titles are listed below.Griselda Anglada-OrtizPlanktic calcifiers: from living assemblages to proxies in the Arctic OceanSatu AnttilaPreliminary results of mineralogical and geochemical properties of glaciolacustrine and marine clays related to the Fennoscandian […]<\/p>\n","protected":false},"author":123625,"featured_media":0,"parent":0,"menu_order":0,"comment_status":"closed","ping_status":"closed","template":"","meta":{"_et_pb_use_builder":"on","_et_pb_old_content":"","_et_gb_content_width":"","footnotes":""},"class_list":["post-458","page","type-page","status-publish","hentry"],"yoast_head":"\nPoster presentations - PalaeoArc 2025<\/title>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/site.uit.no\/palaeoarc2025\/posters\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Poster presentations - PalaeoArc 2025\" \/>\n<meta property=\"og:description\" content=\"The poster session will take place on Tuesday, June 3rd, from 15:30 to 18:00 in the Medicine and Health Studies (MH) building. Accepted abstract titles are listed below.Griselda Anglada-OrtizPlanktic calcifiers: from living assemblages to proxies in the Arctic OceanSatu AnttilaPreliminary results of mineralogical and geochemical properties of glaciolacustrine and marine clays related to the Fennoscandian […]\" \/>\n<meta property=\"og:url\" content=\"https:\/\/site.uit.no\/palaeoarc2025\/posters\/\" \/>\n<meta property=\"og:site_name\" content=\"PalaeoArc 2025\" \/>\n<meta property=\"article:modified_time\" content=\"2025-05-23T06:51:14+00:00\" \/>\n<meta property=\"og:image\" content=\"https:\/\/site.uit.no\/palaeoarc2025\/wp-content\/uploads\/sites\/517\/2024\/10\/Tromso-scaled.jpg\" \/>\n\t<meta property=\"og:image:width\" content=\"2560\" \/>\n\t<meta property=\"og:image:height\" content=\"1210\" \/>\n\t<meta property=\"og:image:type\" content=\"image\/jpeg\" \/>\n<meta name=\"twitter:card\" content=\"summary_large_image\" \/>\n<meta name=\"twitter:site\" content=\"@PalaeoArc\" \/>\n<meta name=\"twitter:label1\" content=\"Est. reading time\" \/>\n\t<meta name=\"twitter:data1\" content=\"20 minutes\" \/>\n<script type=\"application\/ld+json\" class=\"yoast-schema-graph\">{\"@context\":\"https:\\\/\\\/schema.org\",\"@graph\":[{\"@type\":\"WebPage\",\"@id\":\"https:\\\/\\\/site.uit.no\\\/palaeoarc2025\\\/posters\\\/\",\"url\":\"https:\\\/\\\/site.uit.no\\\/palaeoarc2025\\\/posters\\\/\",\"name\":\"Poster presentations - PalaeoArc 2025\",\"isPartOf\":{\"@id\":\"https:\\\/\\\/site.uit.no\\\/palaeoarc2025\\\/#website\"},\"datePublished\":\"2025-05-13T09:04:29+00:00\",\"dateModified\":\"2025-05-23T06:51:14+00:00\",\"breadcrumb\":{\"@id\":\"https:\\\/\\\/site.uit.no\\\/palaeoarc2025\\\/posters\\\/#breadcrumb\"},\"inLanguage\":\"en-US\",\"potentialAction\":[{\"@type\":\"ReadAction\",\"target\":[\"https:\\\/\\\/site.uit.no\\\/palaeoarc2025\\\/posters\\\/\"]}]},{\"@type\":\"BreadcrumbList\",\"@id\":\"https:\\\/\\\/site.uit.no\\\/palaeoarc2025\\\/posters\\\/#breadcrumb\",\"itemListElement\":[{\"@type\":\"ListItem\",\"position\":1,\"name\":\"Home\",\"item\":\"https:\\\/\\\/site.uit.no\\\/palaeoarc2025\\\/\"},{\"@type\":\"ListItem\",\"position\":2,\"name\":\"Poster presentations\"}]},{\"@type\":\"WebSite\",\"@id\":\"https:\\\/\\\/site.uit.no\\\/palaeoarc2025\\\/#website\",\"url\":\"https:\\\/\\\/site.uit.no\\\/palaeoarc2025\\\/\",\"name\":\"PalaeoArc 2025\",\"description\":\"\",\"potentialAction\":[{\"@type\":\"SearchAction\",\"target\":{\"@type\":\"EntryPoint\",\"urlTemplate\":\"https:\\\/\\\/site.uit.no\\\/palaeoarc2025\\\/?s={search_term_string}\"},\"query-input\":{\"@type\":\"PropertyValueSpecification\",\"valueRequired\":true,\"valueName\":\"search_term_string\"}}],\"inLanguage\":\"en-US\"}]}<\/script>\n<!-- \/ Yoast SEO plugin. -->","yoast_head_json":{"title":"Poster presentations - PalaeoArc 2025","robots":{"index":"index","follow":"follow","max-snippet":"max-snippet:-1","max-image-preview":"max-image-preview:large","max-video-preview":"max-video-preview:-1"},"canonical":"https:\/\/site.uit.no\/palaeoarc2025\/posters\/","og_locale":"en_US","og_type":"article","og_title":"Poster presentations - PalaeoArc 2025","og_description":"The poster session will take place on Tuesday, June 3rd, from 15:30 to 18:00 in the Medicine and Health Studies (MH) building. Accepted abstract titles are listed below.Griselda Anglada-OrtizPlanktic calcifiers: from living assemblages to proxies in the Arctic OceanSatu AnttilaPreliminary results of mineralogical and geochemical properties of glaciolacustrine and marine clays related to the Fennoscandian […]","og_url":"https:\/\/site.uit.no\/palaeoarc2025\/posters\/","og_site_name":"PalaeoArc 2025","article_modified_time":"2025-05-23T06:51:14+00:00","og_image":[{"width":2560,"height":1210,"url":"https:\/\/site.uit.no\/palaeoarc2025\/wp-content\/uploads\/sites\/517\/2024\/10\/Tromso-scaled.jpg","type":"image\/jpeg"}],"twitter_card":"summary_large_image","twitter_site":"@PalaeoArc","twitter_misc":{"Est. reading time":"20 minutes"},"schema":{"@context":"https:\/\/schema.org","@graph":[{"@type":"WebPage","@id":"https:\/\/site.uit.no\/palaeoarc2025\/posters\/","url":"https:\/\/site.uit.no\/palaeoarc2025\/posters\/","name":"Poster presentations - PalaeoArc 2025","isPartOf":{"@id":"https:\/\/site.uit.no\/palaeoarc2025\/#website"},"datePublished":"2025-05-13T09:04:29+00:00","dateModified":"2025-05-23T06:51:14+00:00","breadcrumb":{"@id":"https:\/\/site.uit.no\/palaeoarc2025\/posters\/#breadcrumb"},"inLanguage":"en-US","potentialAction":[{"@type":"ReadAction","target":["https:\/\/site.uit.no\/palaeoarc2025\/posters\/"]}]},{"@type":"BreadcrumbList","@id":"https:\/\/site.uit.no\/palaeoarc2025\/posters\/#breadcrumb","itemListElement":[{"@type":"ListItem","position":1,"name":"Home","item":"https:\/\/site.uit.no\/palaeoarc2025\/"},{"@type":"ListItem","position":2,"name":"Poster presentations"}]},{"@type":"WebSite","@id":"https:\/\/site.uit.no\/palaeoarc2025\/#website","url":"https:\/\/site.uit.no\/palaeoarc2025\/","name":"PalaeoArc 2025","description":"","potentialAction":[{"@type":"SearchAction","target":{"@type":"EntryPoint","urlTemplate":"https:\/\/site.uit.no\/palaeoarc2025\/?s={search_term_string}"},"query-input":{"@type":"PropertyValueSpecification","valueRequired":true,"valueName":"search_term_string"}}],"inLanguage":"en-US"}]}},"_links":{"self":[{"href":"https:\/\/site.uit.no\/palaeoarc2025\/wp-json\/wp\/v2\/pages\/458","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/site.uit.no\/palaeoarc2025\/wp-json\/wp\/v2\/pages"}],"about":[{"href":"https:\/\/site.uit.no\/palaeoarc2025\/wp-json\/wp\/v2\/types\/page"}],"author":[{"embeddable":true,"href":"https:\/\/site.uit.no\/palaeoarc2025\/wp-json\/wp\/v2\/users\/123625"}],"replies":[{"embeddable":true,"href":"https:\/\/site.uit.no\/palaeoarc2025\/wp-json\/wp\/v2\/comments?post=458"}],"version-history":[{"count":2,"href":"https:\/\/site.uit.no\/palaeoarc2025\/wp-json\/wp\/v2\/pages\/458\/revisions"}],"predecessor-version":[{"id":546,"href":"https:\/\/site.uit.no\/palaeoarc2025\/wp-json\/wp\/v2\/pages\/458\/revisions\/546"}],"wp:attachment":[{"href":"https:\/\/site.uit.no\/palaeoarc2025\/wp-json\/wp\/v2\/media?parent=458"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}