Climatically controlled sediment deposition patterns in a high alpine lake (Lake Anterne, French Alps)
Poster International audience Lake Anterne is a small (ca. 0.11 km2, 13.2 m max. water depth) high-alpine lake located at 2061 m asl in the French Alps. Through its location mainly influenced by low-pressure systems bringing moisture from the North Atlantic this site represents a highly sensitive lo...
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fttriple:oai:gotriple.eu:10670/1.o4jkja 2023-05-15T17:35:19+02:00 Climatically controlled sediment deposition patterns in a high alpine lake (Lake Anterne, French Alps) Enters, Dirk Giguet-Covex, Charline Arnaud, Fabien Chapron, Emmanuel Environnements, Dynamiques et Territoires de la Montagne (EDYTEM) Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS) Geological Institute ETH Zürich Department of Earth Sciences Swiss Federal Institute of Technology - ETH Zürich (D-ERDW) Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology Zürich (ETH Zürich)- Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology Zürich (ETH Zürich) Vienne, Austria 2007-04-01 https://hal.archives-ouvertes.fr/hal-00195678 en eng HAL CCSD hal-00195678 10670/1.o4jkja https://hal.archives-ouvertes.fr/hal-00195678 undefined Hyper Article en Ligne - Sciences de l'Homme et de la Société Geophysical Research Abstracts EGU 4th general assembly EGU 4th general assembly, Apr 2007, Vienne, Austria. pp.9025 geo envir Conference Output https://vocabularies.coar-repositories.org/resource_types/c_c94f/ 2007 fttriple 2023-01-22T18:35:49Z Poster International audience Lake Anterne is a small (ca. 0.11 km2, 13.2 m max. water depth) high-alpine lake located at 2061 m asl in the French Alps. Through its location mainly influenced by low-pressure systems bringing moisture from the North Atlantic this site represents a highly sensitive location to identify climate changes at high alpine regions of the NW Alps. Ongoing research of the geomorphological processes in the catchment suggests that the sediment supply into the lake is mainly controlled by snowmelt in late spring and early summer, while in winter the lake is frozen and only fine-grained particles settle down. The laminated silts and clays observed in sediment cores of the deepest part of Lake Anterne reflect this annual pattern and possibly represent clastic varves thus allowing a precise dating of the sediment record. This assumption is supported through previously made comparisons between the 210-Pb and 137-Cs dating results and laminae counting made directly on a sediment core. However, subannual rhythmites which are attributed to summer rainfall events with increased fluvial sediment delivery appear to be intercalated within the varves. A higher accuracy of laminae counts as well as a better understanding of sedimentation processes is archived through the study of large format thin sections as well as high resolution grain size analysis and XRF scanning. These analyses show different facies types which can be related to annual sedimentation patterns, turbidite deposits related to rainstorm events and layers deposited through failures of the delta fronts triggered by earthquakes. Lake monitoring using temperature data loggers and sediment traps will give further insights into the external (climatic) factors controlling sediment deposition and will allow the identification climatic changes in the laminated sediment record. Other/Unknown Material North Atlantic Unknown Alpine Lake ENVELOPE(-129.182,-129.182,55.529,55.529) |
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language |
English |
topic |
geo envir |
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geo envir Enters, Dirk Giguet-Covex, Charline Arnaud, Fabien Chapron, Emmanuel Climatically controlled sediment deposition patterns in a high alpine lake (Lake Anterne, French Alps) |
topic_facet |
geo envir |
description |
Poster International audience Lake Anterne is a small (ca. 0.11 km2, 13.2 m max. water depth) high-alpine lake located at 2061 m asl in the French Alps. Through its location mainly influenced by low-pressure systems bringing moisture from the North Atlantic this site represents a highly sensitive location to identify climate changes at high alpine regions of the NW Alps. Ongoing research of the geomorphological processes in the catchment suggests that the sediment supply into the lake is mainly controlled by snowmelt in late spring and early summer, while in winter the lake is frozen and only fine-grained particles settle down. The laminated silts and clays observed in sediment cores of the deepest part of Lake Anterne reflect this annual pattern and possibly represent clastic varves thus allowing a precise dating of the sediment record. This assumption is supported through previously made comparisons between the 210-Pb and 137-Cs dating results and laminae counting made directly on a sediment core. However, subannual rhythmites which are attributed to summer rainfall events with increased fluvial sediment delivery appear to be intercalated within the varves. A higher accuracy of laminae counts as well as a better understanding of sedimentation processes is archived through the study of large format thin sections as well as high resolution grain size analysis and XRF scanning. These analyses show different facies types which can be related to annual sedimentation patterns, turbidite deposits related to rainstorm events and layers deposited through failures of the delta fronts triggered by earthquakes. Lake monitoring using temperature data loggers and sediment traps will give further insights into the external (climatic) factors controlling sediment deposition and will allow the identification climatic changes in the laminated sediment record. |
author2 |
Environnements, Dynamiques et Territoires de la Montagne (EDYTEM) Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS) Geological Institute ETH Zürich Department of Earth Sciences Swiss Federal Institute of Technology - ETH Zürich (D-ERDW) Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology Zürich (ETH Zürich)- Eidgenössische Technische Hochschule - Swiss Federal Institute of Technology Zürich (ETH Zürich) |
format |
Other/Unknown Material |
author |
Enters, Dirk Giguet-Covex, Charline Arnaud, Fabien Chapron, Emmanuel |
author_facet |
Enters, Dirk Giguet-Covex, Charline Arnaud, Fabien Chapron, Emmanuel |
author_sort |
Enters, Dirk |
title |
Climatically controlled sediment deposition patterns in a high alpine lake (Lake Anterne, French Alps) |
title_short |
Climatically controlled sediment deposition patterns in a high alpine lake (Lake Anterne, French Alps) |
title_full |
Climatically controlled sediment deposition patterns in a high alpine lake (Lake Anterne, French Alps) |
title_fullStr |
Climatically controlled sediment deposition patterns in a high alpine lake (Lake Anterne, French Alps) |
title_full_unstemmed |
Climatically controlled sediment deposition patterns in a high alpine lake (Lake Anterne, French Alps) |
title_sort |
climatically controlled sediment deposition patterns in a high alpine lake (lake anterne, french alps) |
publisher |
HAL CCSD |
publishDate |
2007 |
url |
https://hal.archives-ouvertes.fr/hal-00195678 |
op_coverage |
Vienne, Austria |
long_lat |
ENVELOPE(-129.182,-129.182,55.529,55.529) |
geographic |
Alpine Lake |
geographic_facet |
Alpine Lake |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
Hyper Article en Ligne - Sciences de l'Homme et de la Société Geophysical Research Abstracts EGU 4th general assembly EGU 4th general assembly, Apr 2007, Vienne, Austria. pp.9025 |
op_relation |
hal-00195678 10670/1.o4jkja https://hal.archives-ouvertes.fr/hal-00195678 |
op_rights |
undefined |
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1766134445186744320 |