Vegetation and climate since the last interglacial in the Vienne area (France)
International audience Biomes and climate reconstructions are based on variations of the pollen content of the sediments. Pollen analysis was conducted on sediment deposits sampled at Chantemerle site (Vienne department, France). The pollen diagram covered only the last 7200 years BP. Consequently,...
Published in: | Global and Planetary Change |
---|---|
Main Authors: | , , , , , |
Other Authors: | , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
HAL CCSD
1999
|
Subjects: | |
Online Access: | https://hal.science/halsde-00270431 https://doi.org/10.1016/S0921-8181(98)00054-X |
id |
ftciradhal:oai:HAL:halsde-00270431v1 |
---|---|
record_format |
openpolar |
spelling |
ftciradhal:oai:HAL:halsde-00270431v1 2024-05-19T07:49:39+00:00 Vegetation and climate since the last interglacial in the Vienne area (France) Fauquette, Séverine Guiot, Joel Menut, Marianne de Beaulieu, Jacques-Louis Reille, Maurice Guenet, Pascal Institut Méditerranéen d'Ecologie et de Paléoécologie (IMEP) Université Paul Cézanne - Aix-Marseille 3-Université de Provence - Aix-Marseille 1-Avignon Université (AU)-Centre National de la Recherche Scientifique (CNRS) 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) Centre européen de recherche et d'enseignement des géosciences de l'environnement (CEREGE) Institut de Recherche pour le Développement (IRD)-Institut National de la Recherche Agronomique (INRA)-Aix Marseille Université (AMU)-Collège de France (CdF (institution))-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS) EPLEA Laboratoire de chrono-écologie - CNRS (UMR6565) (LCE) Centre National de la Recherche Scientifique (CNRS)-Université de Franche-Comté (UFC) Université Bourgogne Franche-Comté COMUE (UBFC)-Université Bourgogne Franche-Comté COMUE (UBFC) 1999 https://hal.science/halsde-00270431 https://doi.org/10.1016/S0921-8181(98)00054-X en eng HAL CCSD Elsevier info:eu-repo/semantics/altIdentifier/doi/10.1016/S0921-8181(98)00054-X halsde-00270431 https://hal.science/halsde-00270431 doi:10.1016/S0921-8181(98)00054-X ISSN: 0921-8181 Global and Planetary Change https://hal.science/halsde-00270431 Global and Planetary Change, 1999, 20, pp.1-17. ⟨10.1016/S0921-8181(98)00054-X⟩ Palaeoclimates Biomes Pollen data Last glacial-interglacial cycle Vienne department (France) [SDE.MCG]Environmental Sciences/Global Changes info:eu-repo/semantics/article Journal articles 1999 ftciradhal https://doi.org/10.1016/S0921-8181(98)00054-X 2024-04-25T00:57:21Z International audience Biomes and climate reconstructions are based on variations of the pollen content of the sediments. Pollen analysis was conducted on sediment deposits sampled at Chantemerle site (Vienne department, France). The pollen diagram covered only the last 7200 years BP. Consequently, additional pollen sequences, derived from the European Pollen Database, have been used to provide a first climate and biome reconstruction on a longer period, from the Riss (ca 140 ka BP) to the present-day. These pollen sequences show that the succession of the biomes and of the climate has been similar throughout a large part of France since about 140 000 years BP. However it is noteworthy that near the Atlantic coast, a warmer biome is recorded during the temperate periods: the warm mixed biome. This homogeneity allows us to extrapolate the results obtained from all these sequences to the Vienne region. The climate was warmer and more humid than today, or equivalent, during the Eemian, Saint-Germain I and Saint-Germain II. These periods were characterised by temperate deciduous or mixed forests with warmer episodes of warm mixed forests. On the other hand, climate was colder and dryer than today during the glacial phases (Melisey I, Melisey II, Würm, Late Glacial) which were characterised by cold steppes andror tundra. Article in Journal/Newspaper Tundra CIRAD: HAL (Agricultural Research for Development) Global and Planetary Change 20 1 1 17 |
institution |
Open Polar |
collection |
CIRAD: HAL (Agricultural Research for Development) |
op_collection_id |
ftciradhal |
language |
English |
topic |
Palaeoclimates Biomes Pollen data Last glacial-interglacial cycle Vienne department (France) [SDE.MCG]Environmental Sciences/Global Changes |
spellingShingle |
Palaeoclimates Biomes Pollen data Last glacial-interglacial cycle Vienne department (France) [SDE.MCG]Environmental Sciences/Global Changes Fauquette, Séverine Guiot, Joel Menut, Marianne de Beaulieu, Jacques-Louis Reille, Maurice Guenet, Pascal Vegetation and climate since the last interglacial in the Vienne area (France) |
topic_facet |
Palaeoclimates Biomes Pollen data Last glacial-interglacial cycle Vienne department (France) [SDE.MCG]Environmental Sciences/Global Changes |
description |
International audience Biomes and climate reconstructions are based on variations of the pollen content of the sediments. Pollen analysis was conducted on sediment deposits sampled at Chantemerle site (Vienne department, France). The pollen diagram covered only the last 7200 years BP. Consequently, additional pollen sequences, derived from the European Pollen Database, have been used to provide a first climate and biome reconstruction on a longer period, from the Riss (ca 140 ka BP) to the present-day. These pollen sequences show that the succession of the biomes and of the climate has been similar throughout a large part of France since about 140 000 years BP. However it is noteworthy that near the Atlantic coast, a warmer biome is recorded during the temperate periods: the warm mixed biome. This homogeneity allows us to extrapolate the results obtained from all these sequences to the Vienne region. The climate was warmer and more humid than today, or equivalent, during the Eemian, Saint-Germain I and Saint-Germain II. These periods were characterised by temperate deciduous or mixed forests with warmer episodes of warm mixed forests. On the other hand, climate was colder and dryer than today during the glacial phases (Melisey I, Melisey II, Würm, Late Glacial) which were characterised by cold steppes andror tundra. |
author2 |
Institut Méditerranéen d'Ecologie et de Paléoécologie (IMEP) Université Paul Cézanne - Aix-Marseille 3-Université de Provence - Aix-Marseille 1-Avignon Université (AU)-Centre National de la Recherche Scientifique (CNRS) 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) Centre européen de recherche et d'enseignement des géosciences de l'environnement (CEREGE) Institut de Recherche pour le Développement (IRD)-Institut National de la Recherche Agronomique (INRA)-Aix Marseille Université (AMU)-Collège de France (CdF (institution))-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS) EPLEA Laboratoire de chrono-écologie - CNRS (UMR6565) (LCE) Centre National de la Recherche Scientifique (CNRS)-Université de Franche-Comté (UFC) Université Bourgogne Franche-Comté COMUE (UBFC)-Université Bourgogne Franche-Comté COMUE (UBFC) |
format |
Article in Journal/Newspaper |
author |
Fauquette, Séverine Guiot, Joel Menut, Marianne de Beaulieu, Jacques-Louis Reille, Maurice Guenet, Pascal |
author_facet |
Fauquette, Séverine Guiot, Joel Menut, Marianne de Beaulieu, Jacques-Louis Reille, Maurice Guenet, Pascal |
author_sort |
Fauquette, Séverine |
title |
Vegetation and climate since the last interglacial in the Vienne area (France) |
title_short |
Vegetation and climate since the last interglacial in the Vienne area (France) |
title_full |
Vegetation and climate since the last interglacial in the Vienne area (France) |
title_fullStr |
Vegetation and climate since the last interglacial in the Vienne area (France) |
title_full_unstemmed |
Vegetation and climate since the last interglacial in the Vienne area (France) |
title_sort |
vegetation and climate since the last interglacial in the vienne area (france) |
publisher |
HAL CCSD |
publishDate |
1999 |
url |
https://hal.science/halsde-00270431 https://doi.org/10.1016/S0921-8181(98)00054-X |
genre |
Tundra |
genre_facet |
Tundra |
op_source |
ISSN: 0921-8181 Global and Planetary Change https://hal.science/halsde-00270431 Global and Planetary Change, 1999, 20, pp.1-17. ⟨10.1016/S0921-8181(98)00054-X⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1016/S0921-8181(98)00054-X halsde-00270431 https://hal.science/halsde-00270431 doi:10.1016/S0921-8181(98)00054-X |
op_doi |
https://doi.org/10.1016/S0921-8181(98)00054-X |
container_title |
Global and Planetary Change |
container_volume |
20 |
container_issue |
1 |
container_start_page |
1 |
op_container_end_page |
17 |
_version_ |
1799468176853958656 |