MH1 U6.Store auditorium<\/a>.<\/p>\n[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_4,3_4″ make_equal=”on” _builder_version=”4.27.4″ _module_preset=”default” background_color=”#e0eaff” custom_padding=”20px|10px|20px|10px|false|false” hover_enabled=”0″ custom_css_main_element=”align-items: center;” global_colors_info=”{}” sticky_enabled=”0″][et_pb_column type=”1_4″ _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”]<\/p>\n
09:15 – 09:30<\/p>\n
[\/et_pb_text][\/et_pb_column][et_pb_column type=”3_4″ _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”][et_pb_text content_tablet=”<\/p>\n
Alo\u00efs Rev\u00e9ret
<\/strong>The lost ecosystems of Doggerland as revealed by sedimentary ancient DNA<\/p>\n” content_phone=”<\/p>\n
Alo\u00efs Rev\u00e9ret
<\/strong>The lost ecosystems of Doggerland as revealed by sedimentary ancient DNA<\/p>\n” content_last_edited=”off|desktop” _builder_version=”4.27.4″ _module_preset=”default” hover_enabled=”0″ global_colors_info=”{}” sticky_enabled=”0″]<\/p>\n
Anna Hughes
<\/strong>DATED-2: An updated ice-extent chronology for the Eurasian Ice Sheet Complex, 40-10 ka<\/p>\n[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_4,3_4″ make_equal=”on” _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”20px|10px|20px|10px|false|false” custom_css_main_element=”align-items: center;” global_colors_info=”{}”][et_pb_column type=”1_4″ _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”]<\/p>\n
09:30 – 09:45<\/p>\n
[\/et_pb_text][\/et_pb_column][et_pb_column type=”3_4″ _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”][et_pb_text content_tablet=”<\/p>\n
Inger Greve Alsos (Keynote)
<\/strong>Ecosystem drivers and niche changes inferred from sedimentary ancient DNA<\/p>\n” content_phone=”<\/p>\n
Inger Greve Alsos (Keynote)
<\/strong>Ecosystem drivers and niche changes inferred from sedimentary ancient DNA<\/p>\n” content_last_edited=”off|desktop” _builder_version=”4.27.4″ _module_preset=”default” hover_enabled=”0″ global_colors_info=”{}” sticky_enabled=”0″]<\/p>\n
Lis Allaart
<\/strong>New insights from the southern margin of the Fennoscandian Ice Sheet \u2013 regional mapping of the shallow subsurface in Denmark<\/p>\n[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_4,3_4″ make_equal=”on” _builder_version=”4.27.4″ _module_preset=”default” background_color=”#e0eaff” custom_padding=”20px|10px|20px|10px|false|false” custom_css_main_element=”align-items: center;” global_colors_info=”{}”][et_pb_column type=”1_4″ _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”]<\/p>\n
09:45 – 10:00<\/p>\n
[\/et_pb_text][\/et_pb_column][et_pb_column type=”3_4″ _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”][et_pb_text content_tablet=”<\/p>\n
Alo\u00efs Rev\u00e9ret
<\/strong>The lost ecosystems of Doggerland as revealed by sedimentary ancient DNA<\/p>\n” content_phone=”<\/p>\n
Alo\u00efs Rev\u00e9ret
<\/strong>The lost ecosystems of Doggerland as revealed by sedimentary ancient DNA<\/p>\n” content_last_edited=”off|desktop” _builder_version=”4.27.4″ _module_preset=”default” hover_enabled=”0″ global_colors_info=”{}” sticky_enabled=”0″]<\/p>\n
Daniel Wiberg
<\/strong>Evidence of Weichselian slides and the possibility of future events in the northern Storegga Slide area<\/p>\n[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_4,3_4″ make_equal=”on” _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”20px|10px|20px|10px|false|false” custom_css_main_element=”align-items: center;” global_colors_info=”{}”][et_pb_column type=”1_4″ _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”]<\/p>\n
10:00 – 10:15<\/p>\n
[\/et_pb_text][\/et_pb_column][et_pb_column type=”3_4″ _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”][et_pb_text content_tablet=”<\/p>\n
Bishnu Timilsina
<\/strong>Taxon-Specific Marker Improves Bryophyte Taxonomic Resolution and Paleo-Vegetation Reconstruction<\/p>\n” content_phone=”<\/p>\n
Bishnu Timilsina
<\/strong>Taxon-Specific Marker Improves Bryophyte Taxonomic Resolution and Paleo-Vegetation Reconstruction<\/p>\n” content_last_edited=”off|desktop” _builder_version=”4.27.4″ _module_preset=”default” hover_enabled=”0″ global_colors_info=”{}” sticky_enabled=”0″]<\/p>\n
Bartosz Kurjanski
<\/strong>The role of shallow banks and marine ice domes in marine- based ice sheet deglaciation<\/p>\n[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row _builder_version=”4.27.4″ _module_preset=”default” background_color=”#fffcea” border_width_top=”1px” border_width_bottom=”1px” global_colors_info=”{}”][et_pb_column type=”4_4″ _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”]<\/p>\n
COFFEE BREAK<\/strong><\/p>\n[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_4,3_4″ make_equal=”on” _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”20px|10px|20px|10px|false|false” custom_css_main_element=”align-items: center;” global_colors_info=”{}”][et_pb_column type=”1_4″ _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” hover_enabled=”0″ global_colors_info=”{}” sticky_enabled=”0″]<\/p>\n
10:45 – 11:00<\/p>\n
[\/et_pb_text][\/et_pb_column][et_pb_column type=”3_4″ _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”][et_pb_text content_tablet=”<\/p>\n
Bishnu Timilsina
<\/strong>Taxon-Specific Marker Improves Bryophyte Taxonomic Resolution and Paleo-Vegetation Reconstruction<\/p>\n” content_phone=”<\/p>\n
Bishnu Timilsina
<\/strong>Taxon-Specific Marker Improves Bryophyte Taxonomic Resolution and Paleo-Vegetation Reconstruction<\/p>\n” content_last_edited=”off|desktop” _builder_version=”4.27.4″ _module_preset=”default” hover_enabled=”0″ global_colors_info=”{}” sticky_enabled=”0″]<\/p>\n
Jutta Wollenburg
<\/strong>Arctic stratigraphy – problems with micropaleontological approaches<\/p>\n[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_4,3_4″ make_equal=”on” _builder_version=”4.27.4″ _module_preset=”default” background_color=”#e0eaff” custom_padding=”20px|10px|20px|10px|false|false” custom_css_main_element=”align-items: center;” global_colors_info=”{}”][et_pb_column type=”1_4″ _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”]<\/p>\n
11:00 – 11:15<\/p>\n
[\/et_pb_text][\/et_pb_column][et_pb_column type=”3_4″ _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”][et_pb_text content_tablet=”<\/p>\n
Lisbeth Lyngkj\u00e6r Pedersen
<\/strong>Late Pleistocene and Holocene landscape evolution at Ilimanaq, central West Greenland<\/p>\n” content_phone=”<\/p>\n
Lisbeth Lyngkj\u00e6r Pedersen
<\/strong>Late Pleistocene and Holocene landscape evolution at Ilimanaq, central West Greenland<\/p>\n” content_last_edited=”off|desktop” _builder_version=”4.27.4″ _module_preset=”default” hover_enabled=”0″ global_colors_info=”{}” sticky_enabled=”0″]<\/p>\n
Laura Bronzo
<\/strong>Calcareous nannofossil assemblages as a proxy for paleoclimatic and paleoceanographic reconstruction over the past 24 ky along the West Spitsbergen margin<\/p>\n[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_4,3_4″ make_equal=”on” _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”20px|10px|20px|10px|false|false” custom_css_main_element=”align-items: center;” global_colors_info=”{}”][et_pb_column type=”1_4″ _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”]<\/p>\n
11:15 – 11:30<\/p>\n
[\/et_pb_text][\/et_pb_column][et_pb_column type=”3_4″ _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”][et_pb_text content_tablet=”<\/p>\n
Astrid Lys\u00e5
<\/strong>Lateglacial and Holocene glacier variations in Jan Mayen, Norway; a story involving climate and volcanism<\/p>\n” content_phone=”<\/p>\n
Astrid Lys\u00e5
<\/strong>Lateglacial and Holocene glacier variations in Jan Mayen, Norway; a story involving climate and volcanism<\/p>\n” content_last_edited=”off|desktop” _builder_version=”4.27.4″ _module_preset=”default” hover_enabled=”0″ global_colors_info=”{}” sticky_enabled=”0″]<\/p>\n
Robert Spielhagen
<\/strong>Arctic Ocean freshwater export and its relation to AMOC over the last two glacial cycles<\/p>\n[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_4,3_4″ make_equal=”on” _builder_version=”4.27.4″ _module_preset=”default” background_color=”#e0eaff” custom_padding=”20px|10px|20px|10px|false|false” custom_css_main_element=”align-items: center;” global_colors_info=”{}”][et_pb_column type=”1_4″ _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”]<\/p>\n
11:30 – 11:45<\/p>\n
[\/et_pb_text][\/et_pb_column][et_pb_column type=”3_4″ _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”][et_pb_text content_tablet=”<\/p>\n
Wesley Farnsworth
<\/strong>Refining the age of Iceland\u00b4s Saksunarvatn Ash: new constraints on the G10ka Series<\/p>\n” content_phone=”<\/p>\n
Wesley Farnsworth
<\/strong>Refining the age of Iceland\u00b4s Saksunarvatn Ash: new constraints on the G10ka Series<\/p>\n” content_last_edited=”off|desktop” _builder_version=”4.27.4″ _module_preset=”default” hover_enabled=”0″ global_colors_info=”{}” sticky_enabled=”0″]<\/p>\n
Agathe Ollive
<\/strong>Possible controls of the authigenic 10<\/sup>Be\/9<\/sup>Be ratio in surface sediments of the Arctic Ocean<\/p>\n[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row _builder_version=”4.27.4″ _module_preset=”default” background_color=”#fffcea” border_width_top=”1px” border_width_bottom=”1px” global_colors_info=”{}”][et_pb_column type=”4_4″ _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”]<\/p>\n
LUNCH
In the Lysg\u00e5rden<\/span><\/strong><\/p>\n[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_4,3_4″ make_equal=”on” _builder_version=”4.27.4″ _module_preset=”default” background_color=”#e0eaff” custom_padding=”20px|10px|20px|10px|false|false” custom_css_main_element=”align-items: center;” global_colors_info=”{}”][et_pb_column type=”1_4″ _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”]<\/p>\n
12:45 – 13:15<\/p>\n
[\/et_pb_text][\/et_pb_column][et_pb_column type=”3_4″ _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”][et_pb_text content_tablet=”<\/p>\n
Fredrik H\u00f8gass
<\/strong>A watery ice sheet demise: Formation and drainage of ice-dammed lakes in southern Norway during the Early Holocene<\/p>\n” content_phone=”<\/p>\n
Fredrik H\u00f8gass
<\/strong>A watery ice sheet demise: Formation and drainage of ice-dammed lakes in southern Norway during the Early Holocene<\/p>\n” content_last_edited=”off|desktop” _builder_version=”4.27.4″ _module_preset=”default” hover_enabled=”0″ global_colors_info=”{}” sticky_enabled=”0″]<\/p>\n
Simon Belt (Keynote)
<\/strong>Arctic sea surface temperatures<\/p>\n[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_4,3_4″ make_equal=”on” _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”20px|10px|20px|10px|false|false” custom_css_main_element=”align-items: center;” global_colors_info=”{}”][et_pb_column type=”1_4″ _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”]<\/p>\n
13:15 – 13:30<\/p>\n
[\/et_pb_text][\/et_pb_column][et_pb_column type=”3_4″ _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”][et_pb_text content_tablet=”<\/p>\n
Carl R\u00e9gnell (Keynote)
<\/strong>Dead in the water \u2013 the final demise of the Scandinavian Ice Sheet<\/p>\n” content_phone=”<\/p>\n
Carl R\u00e9gnell (Keynote)
<\/strong>Dead in the water \u2013 the final demise of the Scandinavian Ice Sheet<\/p>\n” content_last_edited=”off|desktop” _builder_version=”4.27.4″ _module_preset=”default” hover_enabled=”0″ global_colors_info=”{}” sticky_enabled=”0″]<\/p>\n
Henning Bauch
<\/strong>Atlantic-driven development of Arctic temperature regimes: The case of MIS 11<\/p>\n[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_4,3_4″ make_equal=”on” _builder_version=”4.27.4″ _module_preset=”default” background_color=”#e0eaff” custom_padding=”20px|10px|20px|10px|false|false” custom_css_main_element=”align-items: center;” global_colors_info=”{}”][et_pb_column type=”1_4″ _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”]<\/p>\n
13:30 – 13:45<\/p>\n
[\/et_pb_text][\/et_pb_column][et_pb_column type=”3_4″ _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”][et_pb_text content_tablet=”<\/p>\n
Fredrik H\u00f8gass
<\/strong>A watery ice sheet demise: Formation and drainage of ice-dammed lakes in southern Norway during the Early Holocene<\/p>\n” content_phone=”<\/p>\n
Fredrik H\u00f8gass
<\/strong>A watery ice sheet demise: Formation and drainage of ice-dammed lakes in southern Norway during the Early Holocene<\/p>\n” content_last_edited=”off|desktop” _builder_version=”4.27.4″ _module_preset=”default” hover_enabled=”0″ global_colors_info=”{}” sticky_enabled=”0″]<\/p>\n
Monika Mikler
<\/strong>Sea ice and ice sheet dynamics in southeastern Baffin Bay from Late MIS 3 to Early Holocene: a high-resolution biomarker study<\/p>\n[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row _builder_version=”4.27.4″ _module_preset=”default” background_color=”#fffcea” border_width_top=”1px” border_width_bottom=”1px” global_colors_info=”{}”][et_pb_column type=”4_4″ _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”]<\/p>\n
COFFEE BREAK<\/strong><\/p>\n[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_4,3_4″ make_equal=”on” _builder_version=”4.27.4″ _module_preset=”default” background_color=”#e0eaff” custom_padding=”20px|10px|20px|10px|false|false” custom_css_main_element=”align-items: center;” global_colors_info=”{}”][et_pb_column type=”1_4″ _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”]<\/p>\n
14:15 – 14:30<\/p>\n
[\/et_pb_text][\/et_pb_column][et_pb_column type=”3_4″ _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”][et_pb_text content_tablet=”<\/p>\n
Henrik Rasmussen
<\/strong>The Early-Mid Holocene Tapes Transgression along a mid-outer fjord transect in Troms, northern Norway<\/p>\n” content_phone=”<\/p>\n
Henrik Rasmussen
<\/strong>The Early-Mid Holocene Tapes Transgression along a mid-outer fjord transect in Troms, northern Norway<\/p>\n” content_last_edited=”off|desktop” _builder_version=”4.27.4″ _module_preset=”default” hover_enabled=”0″ global_colors_info=”{}” sticky_enabled=”0″]<\/p>\n
Subhadip Mukherjee
<\/strong>Identifying sedimentary facies using X-Ray CT, XRF, Paleomagnetic and Parasound to associate two sediment cores from Central Baffin Bay<\/p>\n[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_4,3_4″ make_equal=”on” _builder_version=”4.27.4″ _module_preset=”default” custom_padding=”20px|10px|20px|10px|false|false” custom_css_main_element=”align-items: center;” global_colors_info=”{}”][et_pb_column type=”1_4″ _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”]<\/p>\n
14:30 – 14:45<\/p>\n
[\/et_pb_text][\/et_pb_column][et_pb_column type=”3_4″ _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”][et_pb_text content_tablet=”<\/p>\n
Gabriella Koltai
<\/strong>A Late Miocene temperature record from eastern North Greenland speleothems<\/p>\n” content_phone=”<\/p>\n
Gabriella Koltai
<\/strong>A Late Miocene temperature record from eastern North Greenland speleothems<\/p>\n” content_last_edited=”off|desktop” _builder_version=”4.27.4″ _module_preset=”default” hover_enabled=”0″ global_colors_info=”{}” sticky_enabled=”0″]<\/p>\n
Blanda Matzenbacher
<\/strong>Holocene Reconstruction of C.H. Ostenfeld Glacier based on Sediment Stratigraphy in Victoria Fjord<\/p>\n[\/et_pb_text][\/et_pb_column][\/et_pb_row][et_pb_row column_structure=”1_4,3_4″ make_equal=”on” _builder_version=”4.27.4″ _module_preset=”default” background_color=”#e0eaff” custom_padding=”10px|10px|10px|10px|false|false” custom_css_main_element=”align-items: center;” global_colors_info=”{}”][et_pb_column type=”1_4″ _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”][et_pb_text _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”]<\/p>\n
14:45 – 15:15<\/p>\n
[\/et_pb_text][\/et_pb_column][et_pb_column type=”3_4″ _builder_version=”4.27.4″ _module_preset=”default” global_colors_info=”{}”][et_pb_text content_tablet=”<\/p>\n
Poster session<\/b><\/p>\n
” content_phone=”<\/p>\n
Poster session<\/b><\/p>\n
” content_last_edited=”off|desktop” _builder_version=”4.27.4″ _module_preset=”default” hover_enabled=”0″ global_colors_info=”{}” content__hover_enabled=”off|desktop” sticky_enabled=”0″]<\/p>\n
Concluding remarks, best student presentation awards, and the way forward with the new research network<\/b><\/p>\n
[\/et_pb_text][\/et_pb_column][\/et_pb_row][\/et_pb_section]<\/p>\n","protected":false},"excerpt":{"rendered":"
Medicine and Health Studies (MH) building.\u00a0Find us in MH1 U6.Store auditorium.09:15 – 09:30Anna HughesDATED-2: An updated ice-extent chronology for the Eurasian Ice Sheet Complex, 40-10 ka09:30 – 09:45Lis AllaartNew insights from the southern margin of the Fennoscandian Ice Sheet \u2013 regional mapping of the shallow subsurface in Denmark09:45 – 10:00Daniel WibergEvidence of Weichselian slides and […]<\/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-470","page","type-page","status-publish","hentry"],"yoast_head":"\n
Scientific schedule - Thursday 5th - 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\/thursday\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Scientific schedule - Thursday 5th - PalaeoArc 2025\" \/>\n<meta property=\"og:description\" content=\"Medicine and Health Studies (MH) building.\u00a0Find us in MH1 U6.Store auditorium.09:15 - 09:30Anna HughesDATED-2: An updated ice-extent chronology for the Eurasian Ice Sheet Complex, 40-10 ka09:30 - 09:45Lis AllaartNew insights from the southern margin of the Fennoscandian Ice Sheet \u2013 regional mapping of the shallow subsurface in Denmark09:45 - 10:00Daniel WibergEvidence of Weichselian slides and […]\" \/>\n<meta property=\"og:url\" content=\"https:\/\/site.uit.no\/palaeoarc2025\/thursday\/\" \/>\n<meta property=\"og:site_name\" content=\"PalaeoArc 2025\" \/>\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=\"12 minutes\" \/>\n<script type=\"application\/ld+json\" class=\"yoast-schema-graph\">{\"@context\":\"https:\\\/\\\/schema.org\",\"@graph\":[{\"@type\":\"WebPage\",\"@id\":\"https:\\\/\\\/site.uit.no\\\/palaeoarc2025\\\/thursday\\\/\",\"url\":\"https:\\\/\\\/site.uit.no\\\/palaeoarc2025\\\/thursday\\\/\",\"name\":\"Scientific schedule - 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