Early Holocene vegetation development on islands of proglacial Lake Ojibway in northwestern Québec

International audience At the beginning of the Holocene, the Laurentide Ice Sheet was progressively melting and liberating eastern Canadian landscapes. Meltwater accumulated at the glacier front, forming the proglacial Lake Ojibway, which covered western Québec and eastern Ontario for approximately...

Full description

Bibliographic Details
Main Authors: Vogel, Marianne, Asselin, Hugo, Ali, Adam, A, Latapy, Cécile, Leclercq, Sabrina, Bergeron, Yves, Joannin, Sébastien
Other Authors: Institut des Sciences de l'Evolution de Montpellier (UMR ISEM), Centre de Coopération Internationale en Recherche Agronomique pour le Développement (Cirad)-École Pratique des Hautes Études (EPHE), Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Université de Montpellier (UM)-Institut de recherche pour le développement IRD : UR226-Centre National de la Recherche Scientifique (CNRS), Université du Québec en Abitibi-Témiscamingue (UQAT), Centre d'étude de la forêt (CEF), Université de Sherbrooke (UdeS)-Université Laval Québec (ULaval)-McGill University = Université McGill Montréal, Canada -Université du Québec à Chicoutimi (UQAC)-Université de Montréal (UdeM)-Université Téluq (TELUQ)-Université du Québec en Abitibi-Témiscamingue (UQAT)-Université du Québec à Rimouski (UQAR)-Concordia University Montreal -Université du Québec à Montréal = University of Québec in Montréal (UQAM)-Université du Québec en Outaouais (UQO), Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-Institut de recherche pour le développement IRD : UR226-Centre National de la Recherche Scientifique (CNRS)-Université de Montpellier (UM)
Format: Conference Object
Language:English
Published: HAL CCSD 2023
Subjects:
Online Access:https://hal.science/hal-04168498
Description
Summary:International audience At the beginning of the Holocene, the Laurentide Ice Sheet was progressively melting and liberating eastern Canadian landscapes. Meltwater accumulated at the glacier front, forming the proglacial Lake Ojibway, which covered western Québec and eastern Ontario for approximately 2,000 years before flushing into James Bay around 8,200 years ago. Paleoecological vegetation dynamics reconstructions of sites covered by Lake Ojibway showed that spruce forests were established from the onset, whereas sites south of the southern extent of Lake Ojibway first went through a steppe period before being afforested. One possible explanation for this rapid postglacial forest establishment in western Québec is that islands present on Lake Ojibway (paleo-islands) were colonized by forests before the drainage of the proglacial lake, hence acting as migration outposts. However, this hypothesis had not yet been tested with empirical data. We studied sediments from two small lakes located on paleo-islands (current hilltops) of Lake Ojibway to reconstruct vegetation development and diversity at the local (macro-remains) and regional (pollen) scales. Afforestation occurred between 9,900 and 9,600 years before present on the paleo-islands and was followed by a transition from open woodlands to denser forests around 9,200 years ago. Pinus banksiana, Picea mariana and Betula papyrifera were thus established on the islands almost 1,000 years before the drainage of Lake Ojibway. We also used diversity indicators and charcoal particles counting to better understand and characterize the vegetation and fire dynamics. Diversity indicators showed opposite trends for macro-remains and pollen, indicating local diversification and regional homogenization of the vegetation, supporting the boreal-mixed wood establishment around 9,200 years ago. Charcoal particles combined with the Charcoal Size Distribution (CSD) method reveal that local fires occurred on the paleo-islands and seemed to trigger the vegetation diversification ...