Postglacial vegetation migration facilitated by outposts on proglacial lake islands in eastern North America

Postglacial vegetation colonization that followed ice retreat and proglacial lakes drainage in north-eastern America occurred rapidly, more rapidly than expected based on the modern dispersal capacities of boreal mixedwood trees. Paleo-islands from proglacial Lake Ojibway in Québec (Canada) were aff...

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Main Authors: Marianne F.S. Vogel, Adam A. Ali, Sébastien Joannin, Yves Bergeron, Hugo Asselin
Format: Article
Language:English
Published: Elsevier 2024-01-01
Series:Quaternary Science Advances
Subjects:
Online Access:http://www.sciencedirect.com/science/article/pii/S2666033424000029
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author Marianne F.S. Vogel
Adam A. Ali
Sébastien Joannin
Yves Bergeron
Hugo Asselin
author_facet Marianne F.S. Vogel
Adam A. Ali
Sébastien Joannin
Yves Bergeron
Hugo Asselin
author_sort Marianne F.S. Vogel
collection DOAJ
description Postglacial vegetation colonization that followed ice retreat and proglacial lakes drainage in north-eastern America occurred rapidly, more rapidly than expected based on the modern dispersal capacities of boreal mixedwood trees. Paleo-islands from proglacial Lake Ojibway in Québec (Canada) were afforested early, before the final drainage of the lake. We hypothesized that these paleo-islands could have acted as outposts of migration and thus, could explain the rapid afforestation of lowlands observed. To determine if postglacial colonization occurred as a south-north front from the southern margin of Lake Ojibway or if islands acted as migration outposts, we estimated the date of first arrival of the main taxa of the current boreal mixedwood forest. We studied southern sites never covered by proglacial Lake Ojibway, sites that were islands within Lake Ojibway, and northern lowland sites that were liberated after the final drainage of proglacial Lake Ojibway. Taxa arrival was estimated as a sharp rise of the pollen percentage or as the occurrence of macro-remains within the sediments of small lakes dated with radiocarbon. Then we compared migration scenarios where colonization occurred gradually from south to north from the southern margin of proglacial Lake Ojibway and where paleo-islands of Lake Ojibway were first colonized through long-distance dispersal, thus becoming sources of seeds readily available to colonize lowland sites after the final drainage of Lake Ojibway. Finally, we compared the migration rates from the scenarios with the current mean dispersal capacities of the studied taxa. The migration rates estimated without taking the paleo-islands into account are too slow to explain the rapid afforestation observed following the final drainage of proglacial Lake Ojibway. Only the migration rates estimated from the scenarios with paleo-islands were comparable to the current mean dispersal capacity of the boreal mixedwood taxa. Thus, paleo-islands acted as stepping stones during postglacial migration, which explains why the lowlands were rapidly colonized. Larger paleo-islands and those located closer to the southern margin of the proglacial Lake were colonized first, in line with the theory of island biogeography.
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spelling doaj.art-26fce965bd844175a25ce31bbb97a5972024-03-08T05:19:29ZengElsevierQuaternary Science Advances2666-03342024-01-0113100164Postglacial vegetation migration facilitated by outposts on proglacial lake islands in eastern North AmericaMarianne F.S. Vogel0Adam A. Ali1Sébastien Joannin2Yves Bergeron3Hugo Asselin4Institut de Recherche sur Les Forêts, Université du Québec en Abitibi-Témiscamingue, Rouyn-Noranda, Québec, Canada; ISEM, Université de Montpellier, CNRS, IRD, Montpellier, France; Corresponding author. 445, boulevard de l’Université, J9X5E4, Rouyn-Noranda, Québec, Canada.ISEM, Université de Montpellier, CNRS, IRD, Montpellier, FranceISEM, Université de Montpellier, CNRS, IRD, Montpellier, FranceInstitut de Recherche sur Les Forêts, Université du Québec en Abitibi-Témiscamingue, Rouyn-Noranda, Québec, Canada; Département des Sciences Biologiques, Université du Québec à Montréal, Montréal, Québec, CanadaÉcole d’Études Autochtones, Université du Québec en Abitibi-Témiscamingue, Rouyn-Noranda, Québec, CanadaPostglacial vegetation colonization that followed ice retreat and proglacial lakes drainage in north-eastern America occurred rapidly, more rapidly than expected based on the modern dispersal capacities of boreal mixedwood trees. Paleo-islands from proglacial Lake Ojibway in Québec (Canada) were afforested early, before the final drainage of the lake. We hypothesized that these paleo-islands could have acted as outposts of migration and thus, could explain the rapid afforestation of lowlands observed. To determine if postglacial colonization occurred as a south-north front from the southern margin of Lake Ojibway or if islands acted as migration outposts, we estimated the date of first arrival of the main taxa of the current boreal mixedwood forest. We studied southern sites never covered by proglacial Lake Ojibway, sites that were islands within Lake Ojibway, and northern lowland sites that were liberated after the final drainage of proglacial Lake Ojibway. Taxa arrival was estimated as a sharp rise of the pollen percentage or as the occurrence of macro-remains within the sediments of small lakes dated with radiocarbon. Then we compared migration scenarios where colonization occurred gradually from south to north from the southern margin of proglacial Lake Ojibway and where paleo-islands of Lake Ojibway were first colonized through long-distance dispersal, thus becoming sources of seeds readily available to colonize lowland sites after the final drainage of Lake Ojibway. Finally, we compared the migration rates from the scenarios with the current mean dispersal capacities of the studied taxa. The migration rates estimated without taking the paleo-islands into account are too slow to explain the rapid afforestation observed following the final drainage of proglacial Lake Ojibway. Only the migration rates estimated from the scenarios with paleo-islands were comparable to the current mean dispersal capacity of the boreal mixedwood taxa. Thus, paleo-islands acted as stepping stones during postglacial migration, which explains why the lowlands were rapidly colonized. Larger paleo-islands and those located closer to the southern margin of the proglacial Lake were colonized first, in line with the theory of island biogeography.http://www.sciencedirect.com/science/article/pii/S2666033424000029AfforestationLong-distance dispersalMigration outpostPostglacial colonizationProglacial lakeTheory of island biogeography
spellingShingle Marianne F.S. Vogel
Adam A. Ali
Sébastien Joannin
Yves Bergeron
Hugo Asselin
Postglacial vegetation migration facilitated by outposts on proglacial lake islands in eastern North America
Quaternary Science Advances
Afforestation
Long-distance dispersal
Migration outpost
Postglacial colonization
Proglacial lake
Theory of island biogeography
title Postglacial vegetation migration facilitated by outposts on proglacial lake islands in eastern North America
title_full Postglacial vegetation migration facilitated by outposts on proglacial lake islands in eastern North America
title_fullStr Postglacial vegetation migration facilitated by outposts on proglacial lake islands in eastern North America
title_full_unstemmed Postglacial vegetation migration facilitated by outposts on proglacial lake islands in eastern North America
title_short Postglacial vegetation migration facilitated by outposts on proglacial lake islands in eastern North America
title_sort postglacial vegetation migration facilitated by outposts on proglacial lake islands in eastern north america
topic Afforestation
Long-distance dispersal
Migration outpost
Postglacial colonization
Proglacial lake
Theory of island biogeography
url http://www.sciencedirect.com/science/article/pii/S2666033424000029
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