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...
Published in: | Quaternary Research |
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Main Authors: | , , , , , , , , , |
Other Authors: | , , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
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HAL CCSD
2010
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Online Access: | https://insu.hal.science/insu-00564117 https://doi.org/10.1016/j.yqres.2010.07.002 |
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ftinsu:oai:HAL:insu-00564117v1 |
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openpolar |
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 |
_version_ |
1797584894442864640 |
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 |