Variability of the terrestrial ecosystems and climate along a glacial-interglacial cycle.
International audience During the last 130 millennia, several climatic changes of various amplitudes and lengths have influenced the continental biosphere. The records available for several continents agree to show that the Interglacial climate (Eemian and Holocene) was less variable and contrasted...
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ftinsu:oai:HAL:hal-01457705v1 2023-12-17T10:46:34+01:00 Variability of the terrestrial ecosystems and climate along a glacial-interglacial cycle. Guiot, Joel Cheddadi, R 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) 2004-06 https://hal.science/hal-01457705 https://doi.org/10.1016/j.crte.2003.12.020 en eng HAL CCSD Elsevier info:eu-repo/semantics/altIdentifier/doi/10.1016/j.crte.2003.12.020 hal-01457705 https://hal.science/hal-01457705 doi:10.1016/j.crte.2003.12.020 Comptes Rendus Géoscience https://hal.science/hal-01457705 Comptes Rendus Géoscience, 2004, 336 (7-8), pp.667-675. ⟨10.1016/j.crte.2003.12.020⟩ [SDE.MCG]Environmental Sciences/Global Changes info:eu-repo/semantics/article Journal articles 2004 ftinsu https://doi.org/10.1016/j.crte.2003.12.020 2023-11-22T17:49:29Z International audience During the last 130 millennia, several climatic changes of various amplitudes and lengths have influenced the continental biosphere. The records available for several continents agree to show that the Interglacial climate (Eemian and Holocene) was less variable and contrasted than the Glacial climate. These changes are mainly related to changes of insolation suffered by Earth during its orbital revolution. Vegetation and hydrological changes of the North Atlantic Ocean can have strong feedbacks on the atmosphere, generating more abrupt and shorter climatic changes, also recorded by bio-indicators. The climatic changes observed on most of the continents using pollen data and other fossil remains are reviewed and analysed in function of possible forcing. In conclusion, we show how joined use of past data and vegetation models can enlighten on current global changes. (C) 2004 Academie des sciences. Publie par Elsevier SAS. Tous droits reserves. Article in Journal/Newspaper North Atlantic Institut national des sciences de l'Univers: HAL-INSU Comptes Rendus Geoscience 336 7-8 667 675 |
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Open Polar |
collection |
Institut national des sciences de l'Univers: HAL-INSU |
op_collection_id |
ftinsu |
language |
English |
topic |
[SDE.MCG]Environmental Sciences/Global Changes |
spellingShingle |
[SDE.MCG]Environmental Sciences/Global Changes Guiot, Joel Cheddadi, R Variability of the terrestrial ecosystems and climate along a glacial-interglacial cycle. |
topic_facet |
[SDE.MCG]Environmental Sciences/Global Changes |
description |
International audience During the last 130 millennia, several climatic changes of various amplitudes and lengths have influenced the continental biosphere. The records available for several continents agree to show that the Interglacial climate (Eemian and Holocene) was less variable and contrasted than the Glacial climate. These changes are mainly related to changes of insolation suffered by Earth during its orbital revolution. Vegetation and hydrological changes of the North Atlantic Ocean can have strong feedbacks on the atmosphere, generating more abrupt and shorter climatic changes, also recorded by bio-indicators. The climatic changes observed on most of the continents using pollen data and other fossil remains are reviewed and analysed in function of possible forcing. In conclusion, we show how joined use of past data and vegetation models can enlighten on current global changes. (C) 2004 Academie des sciences. Publie par Elsevier SAS. Tous droits reserves. |
author2 |
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) |
format |
Article in Journal/Newspaper |
author |
Guiot, Joel Cheddadi, R |
author_facet |
Guiot, Joel Cheddadi, R |
author_sort |
Guiot, Joel |
title |
Variability of the terrestrial ecosystems and climate along a glacial-interglacial cycle. |
title_short |
Variability of the terrestrial ecosystems and climate along a glacial-interglacial cycle. |
title_full |
Variability of the terrestrial ecosystems and climate along a glacial-interglacial cycle. |
title_fullStr |
Variability of the terrestrial ecosystems and climate along a glacial-interglacial cycle. |
title_full_unstemmed |
Variability of the terrestrial ecosystems and climate along a glacial-interglacial cycle. |
title_sort |
variability of the terrestrial ecosystems and climate along a glacial-interglacial cycle. |
publisher |
HAL CCSD |
publishDate |
2004 |
url |
https://hal.science/hal-01457705 https://doi.org/10.1016/j.crte.2003.12.020 |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_source |
Comptes Rendus Géoscience https://hal.science/hal-01457705 Comptes Rendus Géoscience, 2004, 336 (7-8), pp.667-675. ⟨10.1016/j.crte.2003.12.020⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1016/j.crte.2003.12.020 hal-01457705 https://hal.science/hal-01457705 doi:10.1016/j.crte.2003.12.020 |
op_doi |
https://doi.org/10.1016/j.crte.2003.12.020 |
container_title |
Comptes Rendus Geoscience |
container_volume |
336 |
container_issue |
7-8 |
container_start_page |
667 |
op_container_end_page |
675 |
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1785570081919467520 |