Provenance of freshwater pulses in the Gulf of Mexico during the last deglaciation

International audience During the last deglaciation, the decaying Laurentide Ice Sheet (LIS) delivered huge volumes of meltwater toward the Gulf of Mexico. The present investigation of clay mineralogy and grain-size characteristics of terrigenous sediments deposited in the Orca Basin (Gulf of Mexico...

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Published in:Quaternary Research
Main Authors: Sionneau, Thomas, Bout-Roumazeilles, Viviane, Flower, Benjamin, P, Bory, A., Tribovillard, N., Kissel, Catherine, van Vliet-Lanoë, Brigitte, Montero Serrano, J.C, C, Flower, B.P., Montero Serrano, J.C.
Other Authors: Géosystèmes - UMR 8157, Université de Lille, Sciences et Technologies-Centre National de la Recherche Scientifique (CNRS), University of South Florida Tampa (USF), Lamont-Doherty Earth Observatory (LDEO), Columbia University New York, Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)), Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA), Climat et Magnétisme (CLIMAG), Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)), Domaines Océaniques (LDO), Institut national des sciences de l'Univers (INSU - CNRS)-Université de Brest (UBO)-Observatoire des Sciences de l'Univers-Institut d'écologie et environnement-Centre National de la Recherche Scientifique (CNRS)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2010
Subjects:
Online Access:https://insu.hal.science/insu-00564117
https://doi.org/10.1016/j.yqres.2010.07.002
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institution Open Polar
collection Institut national des sciences de l'Univers: HAL-INSU
op_collection_id ftinsu
language English
topic Mississippi River
Deglaciation
Meltwater pulse
Laurentide Ice Sheet
Clay minerals
Orca Basin
[SDU.STU.MI]Sciences of the Universe [physics]/Earth Sciences/Mineralogy
[SDU.STU.HY]Sciences of the Universe [physics]/Earth Sciences/Hydrology
[SDE.MCG]Environmental Sciences/Global Changes
spellingShingle Mississippi River
Deglaciation
Meltwater pulse
Laurentide Ice Sheet
Clay minerals
Orca Basin
[SDU.STU.MI]Sciences of the Universe [physics]/Earth Sciences/Mineralogy
[SDU.STU.HY]Sciences of the Universe [physics]/Earth Sciences/Hydrology
[SDE.MCG]Environmental Sciences/Global Changes
Sionneau, Thomas
Bout-Roumazeilles, Viviane
Flower, Benjamin, P
Bory, A.
Tribovillard, N.
Kissel, Catherine
van Vliet-Lanoë, Brigitte
Montero Serrano, J.C, C
Flower, B.P.
Montero Serrano, J.C.
Provenance of freshwater pulses in the Gulf of Mexico during the last deglaciation
topic_facet Mississippi River
Deglaciation
Meltwater pulse
Laurentide Ice Sheet
Clay minerals
Orca Basin
[SDU.STU.MI]Sciences of the Universe [physics]/Earth Sciences/Mineralogy
[SDU.STU.HY]Sciences of the Universe [physics]/Earth Sciences/Hydrology
[SDE.MCG]Environmental Sciences/Global Changes
description International audience During the last deglaciation, the decaying Laurentide Ice Sheet (LIS) delivered huge volumes of meltwater toward the Gulf of Mexico. The present investigation of clay mineralogy and grain-size characteristics of terrigenous sediments deposited in the Orca Basin (Gulf of Mexico) offers a unique opportunity to link the marine record of these meltwater floods with the reconstructed continental glacial history and the modeled drainage patterns. Five peculiar sedimentary levels, characterized by high smectite content and low CaCO3 content, were identified and occurred simultaneously with major meltwater floods. According to recently published clay mineral distribution maps for North America, these results help to pinpoint the southwestern margin of the LIS as a main contributor to most of the meltwater discharges. In addition, the peculiar mineralogical composition (illite and chlorite-rich) of the sediments characterizing the meltwater episode associated with Heinrich event 1 suggests a provenance from the Great Lakes area, supporting the interpretation of destabilization of the LIS southeastern margin during this event. Decreased terrigenous contribution associated with changing provenance of sediments after 12.9 cal ka BP suggests strong modifications of the continental hydrography in relation to Lake Agassiz history and changes in the morphology of Mississippi delta due to rising sea level.
author2 Géosystèmes - UMR 8157
Université de Lille, Sciences et Technologies-Centre National de la Recherche Scientifique (CNRS)
University of South Florida Tampa (USF)
Lamont-Doherty Earth Observatory (LDEO)
Columbia University New York
Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE)
Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA))
Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)
Climat et Magnétisme (CLIMAG)
Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA))
Domaines Océaniques (LDO)
Institut national des sciences de l'Univers (INSU - CNRS)-Université de Brest (UBO)-Observatoire des Sciences de l'Univers-Institut d'écologie et environnement-Centre National de la Recherche Scientifique (CNRS)
format Article in Journal/Newspaper
author Sionneau, Thomas
Bout-Roumazeilles, Viviane
Flower, Benjamin, P
Bory, A.
Tribovillard, N.
Kissel, Catherine
van Vliet-Lanoë, Brigitte
Montero Serrano, J.C, C
Flower, B.P.
Montero Serrano, J.C.
author_facet Sionneau, Thomas
Bout-Roumazeilles, Viviane
Flower, Benjamin, P
Bory, A.
Tribovillard, N.
Kissel, Catherine
van Vliet-Lanoë, Brigitte
Montero Serrano, J.C, C
Flower, B.P.
Montero Serrano, J.C.
author_sort Sionneau, Thomas
title Provenance of freshwater pulses in the Gulf of Mexico during the last deglaciation
title_short Provenance of freshwater pulses in the Gulf of Mexico during the last deglaciation
title_full Provenance of freshwater pulses in the Gulf of Mexico during the last deglaciation
title_fullStr Provenance of freshwater pulses in the Gulf of Mexico during the last deglaciation
title_full_unstemmed Provenance of freshwater pulses in the Gulf of Mexico during the last deglaciation
title_sort provenance of freshwater pulses in the gulf of mexico during the last deglaciation
publisher HAL CCSD
publishDate 2010
url https://insu.hal.science/insu-00564117
https://doi.org/10.1016/j.yqres.2010.07.002
genre Ice Sheet
Orca
genre_facet Ice Sheet
Orca
op_source ISSN: 0033-5894
EISSN: 1096-0287
Quaternary Research
https://insu.hal.science/insu-00564117
Quaternary Research, 2010, 74 (2), pp.235-245. ⟨10.1016/j.yqres.2010.07.002⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1016/j.yqres.2010.07.002
insu-00564117
https://insu.hal.science/insu-00564117
doi:10.1016/j.yqres.2010.07.002
op_doi https://doi.org/10.1016/j.yqres.2010.07.002
container_title Quaternary Research
container_volume 74
container_issue 2
container_start_page 235
op_container_end_page 245
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spelling ftinsu:oai:HAL:insu-00564117v1 2024-04-28T08:24:53+00:00 Provenance of freshwater pulses in the Gulf of Mexico during the last deglaciation Sionneau, Thomas Bout-Roumazeilles, Viviane Flower, Benjamin, P Bory, A. Tribovillard, N. Kissel, Catherine van Vliet-Lanoë, Brigitte Montero Serrano, J.C, C Flower, B.P. Montero Serrano, J.C. Géosystèmes - UMR 8157 Université de Lille, Sciences et Technologies-Centre National de la Recherche Scientifique (CNRS) University of South Florida Tampa (USF) Lamont-Doherty Earth Observatory (LDEO) Columbia University New York Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA) Climat et Magnétisme (CLIMAG) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) Domaines Océaniques (LDO) Institut national des sciences de l'Univers (INSU - CNRS)-Université de Brest (UBO)-Observatoire des Sciences de l'Univers-Institut d'écologie et environnement-Centre National de la Recherche Scientifique (CNRS) 2010-09-23 https://insu.hal.science/insu-00564117 https://doi.org/10.1016/j.yqres.2010.07.002 en eng HAL CCSD Elsevier info:eu-repo/semantics/altIdentifier/doi/10.1016/j.yqres.2010.07.002 insu-00564117 https://insu.hal.science/insu-00564117 doi:10.1016/j.yqres.2010.07.002 ISSN: 0033-5894 EISSN: 1096-0287 Quaternary Research https://insu.hal.science/insu-00564117 Quaternary Research, 2010, 74 (2), pp.235-245. ⟨10.1016/j.yqres.2010.07.002⟩ Mississippi River Deglaciation Meltwater pulse Laurentide Ice Sheet Clay minerals Orca Basin [SDU.STU.MI]Sciences of the Universe [physics]/Earth Sciences/Mineralogy [SDU.STU.HY]Sciences of the Universe [physics]/Earth Sciences/Hydrology [SDE.MCG]Environmental Sciences/Global Changes info:eu-repo/semantics/article Journal articles 2010 ftinsu https://doi.org/10.1016/j.yqres.2010.07.002 2024-04-05T00:25:18Z International audience During the last deglaciation, the decaying Laurentide Ice Sheet (LIS) delivered huge volumes of meltwater toward the Gulf of Mexico. The present investigation of clay mineralogy and grain-size characteristics of terrigenous sediments deposited in the Orca Basin (Gulf of Mexico) offers a unique opportunity to link the marine record of these meltwater floods with the reconstructed continental glacial history and the modeled drainage patterns. Five peculiar sedimentary levels, characterized by high smectite content and low CaCO3 content, were identified and occurred simultaneously with major meltwater floods. According to recently published clay mineral distribution maps for North America, these results help to pinpoint the southwestern margin of the LIS as a main contributor to most of the meltwater discharges. In addition, the peculiar mineralogical composition (illite and chlorite-rich) of the sediments characterizing the meltwater episode associated with Heinrich event 1 suggests a provenance from the Great Lakes area, supporting the interpretation of destabilization of the LIS southeastern margin during this event. Decreased terrigenous contribution associated with changing provenance of sediments after 12.9 cal ka BP suggests strong modifications of the continental hydrography in relation to Lake Agassiz history and changes in the morphology of Mississippi delta due to rising sea level. Article in Journal/Newspaper Ice Sheet Orca Institut national des sciences de l'Univers: HAL-INSU Quaternary Research 74 2 235 245