Compositional changes in deglacial red mud event beds off the Laurentian Channel reveal source mixing, grain-size partitioning and ice retreat
International audience Between 22 and 17 cal ka BP, five large meltwater events from within the Laurentian Channel Ice Stream deposited mud beds meters thick across a large area of the Laurentian Fan and adjacent continental slopes. This study determines the sources of these event beds and relates t...
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Online Access: | https://hal.science/hal-02181009 https://doi.org/10.1016/j.quascirev.2019.04.031 |
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ftuniversailles:oai:HAL:hal-02181009v1 2024-04-28T08:25:03+00:00 Compositional changes in deglacial red mud event beds off the Laurentian Channel reveal source mixing, grain-size partitioning and ice retreat Leng, Wei von Dobeneck, Tilo Just, Janna Govin, Aline St-Onge, Guillaume Piper, David J.W. Center for Marine Environmental Sciences Bremen (MARUM) Universität Bremen Bedford Institute of Oceanography 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)) Institut des Sciences de la MER de Rimouski (ISMER) Université du Québec à Rimouski (UQAR) 2019 https://hal.science/hal-02181009 https://doi.org/10.1016/j.quascirev.2019.04.031 en eng HAL CCSD Elsevier info:eu-repo/semantics/altIdentifier/doi/10.1016/j.quascirev.2019.04.031 hal-02181009 https://hal.science/hal-02181009 doi:10.1016/j.quascirev.2019.04.031 ISSN: 0277-3791 EISSN: 1873-457X Quaternary Science Reviews https://hal.science/hal-02181009 Quaternary Science Reviews, 2019, 215, pp.98-115. ⟨10.1016/j.quascirev.2019.04.031⟩ Quaternary Sedimentology-marine cores North Atlantic Paleoceanography Gulf of St. Lawrence Laurentian Channel Ice Stream Subglacial outburst floods Environmental Magnetism Major element analysis Provenance study [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology info:eu-repo/semantics/article Journal articles 2019 ftuniversailles https://doi.org/10.1016/j.quascirev.2019.04.031 2024-04-04T17:38:15Z International audience Between 22 and 17 cal ka BP, five large meltwater events from within the Laurentian Channel Ice Stream deposited mud beds meters thick across a large area of the Laurentian Fan and adjacent continental slopes. This study determines the sources of these event beds and relates them to the glaciological evolution of the retreating Laurentian Ice Stream. We analyzed major element and magnetic mineral contents of these event beds and compare them with a new collection of 80 source reference samples from the Gulf of St. Lawrence area. Element ratios suggest a steady compositional change from older to younger outburst event beds, while element-specific offsets from reference sample compositions indicate grain-size and mineral/element partitioning during suspension transport. Their magnetic properties place event beds on the source mixing trend of four reference samples groups, which represent two magnetite-rich sources (Canadian Shield and/or Southern Newfoundland) and two hematite-rich sources (Appalachian red beds). Using a deterministic linear source mixing model based on IRM 100mT , HIRM and Ca%, we find that the earlier two outburst events had higher contributions from granitic and calcareous sources than the later three events. Combining materials, timing and scenarios of the outburst events with ice-sheet retreat and ice-stream dynamics, we argue that the subglacial sediment depocenter of the earlier two event beds was located in the lower Laurentian Channel while that of the later three events was upstream from Cabot Strait. Article in Journal/Newspaper Ice Sheet Newfoundland North Atlantic Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQ Quaternary Science Reviews 215 98 115 |
institution |
Open Polar |
collection |
Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQ |
op_collection_id |
ftuniversailles |
language |
English |
topic |
Quaternary Sedimentology-marine cores North Atlantic Paleoceanography Gulf of St. Lawrence Laurentian Channel Ice Stream Subglacial outburst floods Environmental Magnetism Major element analysis Provenance study [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology |
spellingShingle |
Quaternary Sedimentology-marine cores North Atlantic Paleoceanography Gulf of St. Lawrence Laurentian Channel Ice Stream Subglacial outburst floods Environmental Magnetism Major element analysis Provenance study [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology Leng, Wei von Dobeneck, Tilo Just, Janna Govin, Aline St-Onge, Guillaume Piper, David J.W. Compositional changes in deglacial red mud event beds off the Laurentian Channel reveal source mixing, grain-size partitioning and ice retreat |
topic_facet |
Quaternary Sedimentology-marine cores North Atlantic Paleoceanography Gulf of St. Lawrence Laurentian Channel Ice Stream Subglacial outburst floods Environmental Magnetism Major element analysis Provenance study [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology |
description |
International audience Between 22 and 17 cal ka BP, five large meltwater events from within the Laurentian Channel Ice Stream deposited mud beds meters thick across a large area of the Laurentian Fan and adjacent continental slopes. This study determines the sources of these event beds and relates them to the glaciological evolution of the retreating Laurentian Ice Stream. We analyzed major element and magnetic mineral contents of these event beds and compare them with a new collection of 80 source reference samples from the Gulf of St. Lawrence area. Element ratios suggest a steady compositional change from older to younger outburst event beds, while element-specific offsets from reference sample compositions indicate grain-size and mineral/element partitioning during suspension transport. Their magnetic properties place event beds on the source mixing trend of four reference samples groups, which represent two magnetite-rich sources (Canadian Shield and/or Southern Newfoundland) and two hematite-rich sources (Appalachian red beds). Using a deterministic linear source mixing model based on IRM 100mT , HIRM and Ca%, we find that the earlier two outburst events had higher contributions from granitic and calcareous sources than the later three events. Combining materials, timing and scenarios of the outburst events with ice-sheet retreat and ice-stream dynamics, we argue that the subglacial sediment depocenter of the earlier two event beds was located in the lower Laurentian Channel while that of the later three events was upstream from Cabot Strait. |
author2 |
Center for Marine Environmental Sciences Bremen (MARUM) Universität Bremen Bedford Institute of Oceanography 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)) Institut des Sciences de la MER de Rimouski (ISMER) Université du Québec à Rimouski (UQAR) |
format |
Article in Journal/Newspaper |
author |
Leng, Wei von Dobeneck, Tilo Just, Janna Govin, Aline St-Onge, Guillaume Piper, David J.W. |
author_facet |
Leng, Wei von Dobeneck, Tilo Just, Janna Govin, Aline St-Onge, Guillaume Piper, David J.W. |
author_sort |
Leng, Wei |
title |
Compositional changes in deglacial red mud event beds off the Laurentian Channel reveal source mixing, grain-size partitioning and ice retreat |
title_short |
Compositional changes in deglacial red mud event beds off the Laurentian Channel reveal source mixing, grain-size partitioning and ice retreat |
title_full |
Compositional changes in deglacial red mud event beds off the Laurentian Channel reveal source mixing, grain-size partitioning and ice retreat |
title_fullStr |
Compositional changes in deglacial red mud event beds off the Laurentian Channel reveal source mixing, grain-size partitioning and ice retreat |
title_full_unstemmed |
Compositional changes in deglacial red mud event beds off the Laurentian Channel reveal source mixing, grain-size partitioning and ice retreat |
title_sort |
compositional changes in deglacial red mud event beds off the laurentian channel reveal source mixing, grain-size partitioning and ice retreat |
publisher |
HAL CCSD |
publishDate |
2019 |
url |
https://hal.science/hal-02181009 https://doi.org/10.1016/j.quascirev.2019.04.031 |
genre |
Ice Sheet Newfoundland North Atlantic |
genre_facet |
Ice Sheet Newfoundland North Atlantic |
op_source |
ISSN: 0277-3791 EISSN: 1873-457X Quaternary Science Reviews https://hal.science/hal-02181009 Quaternary Science Reviews, 2019, 215, pp.98-115. ⟨10.1016/j.quascirev.2019.04.031⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1016/j.quascirev.2019.04.031 hal-02181009 https://hal.science/hal-02181009 doi:10.1016/j.quascirev.2019.04.031 |
op_doi |
https://doi.org/10.1016/j.quascirev.2019.04.031 |
container_title |
Quaternary Science Reviews |
container_volume |
215 |
container_start_page |
98 |
op_container_end_page |
115 |
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