Miocene to Pliocene vegetation and climate estimates in the Iberian Peninsula from pollen data
International audience Pollen analysis of Miocene and Pliocene sediments from the Iberian Peninsula shows a progressive reduction in plant diversity through time caused by the disappearance of thermophilous and high-water requirement plants. In addition, an increase in warm–temperate (mesothermic),...
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Online Access: | https://hal.archives-ouvertes.fr/halsde-00542381 https://doi.org/10.1016/j.revpalbo.2009.08.001 |
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ftunivnantes:oai:HAL:halsde-00542381v1 2023-05-15T13:53:06+02:00 Miocene to Pliocene vegetation and climate estimates in the Iberian Peninsula from pollen data Jiménez-Moreno, Gonzalo Fauquette, Séverine Suc, Jean-Pierre Departamento de Estratigrafia y paleontologia Université de grenade 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) PaleoEnvironnements et PaleobioSphere (PEPS) Université Claude Bernard Lyon 1 (UCBL) Université de Lyon-Université de Lyon-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS) 2010 https://hal.archives-ouvertes.fr/halsde-00542381 https://doi.org/10.1016/j.revpalbo.2009.08.001 en eng HAL CCSD Elsevier info:eu-repo/semantics/altIdentifier/doi/10.1016/j.revpalbo.2009.08.001 halsde-00542381 https://hal.archives-ouvertes.fr/halsde-00542381 doi:10.1016/j.revpalbo.2009.08.001 ISSN: 0034-6667 Review of Palaeobotany and Palynology https://hal.archives-ouvertes.fr/halsde-00542381 Review of Palaeobotany and Palynology, Elsevier, 2010, 162, pp.403-415. ⟨10.1016/j.revpalbo.2009.08.001⟩ Miocene Pliocene Iberian Peninsula pollen vegetation climate change [SDE.MCG]Environmental Sciences/Global Changes info:eu-repo/semantics/article Journal articles 2010 ftunivnantes https://doi.org/10.1016/j.revpalbo.2009.08.001 2022-10-04T22:59:58Z International audience Pollen analysis of Miocene and Pliocene sediments from the Iberian Peninsula shows a progressive reduction in plant diversity through time caused by the disappearance of thermophilous and high-water requirement plants. In addition, an increase in warm–temperate (mesothermic), seasonal-adapted “Mediterranean” taxa, high-elevation conifers and herbs (mainly Artemisia) occurred during the Middle and LateMiocene and Pliocene. This has mainly been interpreted as a response of the vegetation to global and regional processes, including climate cooling related to the development of the East Antarctic Ice Sheet and then the onset of the Arctic Ice Sheet, uplift of regional mountains related to the Alpine uplift and the progressive movement of Eurasia towards northern latitudes as a result of the northwards subduction of Africa. The development of steppe-like vegetation in southern Iberia is ancient and probably started during the Oligocene. The onset of a contrasted seasonality in temperature during the Mid-Pliocene superimposed on the pre-existing seasonality in precipitation, the annual length of which increased southward. The Mediterranean climatic rhythm (summer drought) began about 3.4Ma and caused the individualization of modern Mediterranean ecosystems. Quaternary-type Mediterranean climatic fluctuations started at 2.6Ma (Gelasian) resulting in repeated steppe vs. forest alternations. A latitudinal climatic gradient between the southern and the northern parts of the Iberian Peninsula existed since the Middle Miocene. Article in Journal/Newspaper Antarc* Antarctic Arctic Climate change Ice Sheet Université de Nantes: HAL-UNIV-NANTES Antarctic Arctic East Antarctic Ice Sheet Review of Palaeobotany and Palynology 162 3 403 415 |
institution |
Open Polar |
collection |
Université de Nantes: HAL-UNIV-NANTES |
op_collection_id |
ftunivnantes |
language |
English |
topic |
Miocene Pliocene Iberian Peninsula pollen vegetation climate change [SDE.MCG]Environmental Sciences/Global Changes |
spellingShingle |
Miocene Pliocene Iberian Peninsula pollen vegetation climate change [SDE.MCG]Environmental Sciences/Global Changes Jiménez-Moreno, Gonzalo Fauquette, Séverine Suc, Jean-Pierre Miocene to Pliocene vegetation and climate estimates in the Iberian Peninsula from pollen data |
topic_facet |
Miocene Pliocene Iberian Peninsula pollen vegetation climate change [SDE.MCG]Environmental Sciences/Global Changes |
description |
International audience Pollen analysis of Miocene and Pliocene sediments from the Iberian Peninsula shows a progressive reduction in plant diversity through time caused by the disappearance of thermophilous and high-water requirement plants. In addition, an increase in warm–temperate (mesothermic), seasonal-adapted “Mediterranean” taxa, high-elevation conifers and herbs (mainly Artemisia) occurred during the Middle and LateMiocene and Pliocene. This has mainly been interpreted as a response of the vegetation to global and regional processes, including climate cooling related to the development of the East Antarctic Ice Sheet and then the onset of the Arctic Ice Sheet, uplift of regional mountains related to the Alpine uplift and the progressive movement of Eurasia towards northern latitudes as a result of the northwards subduction of Africa. The development of steppe-like vegetation in southern Iberia is ancient and probably started during the Oligocene. The onset of a contrasted seasonality in temperature during the Mid-Pliocene superimposed on the pre-existing seasonality in precipitation, the annual length of which increased southward. The Mediterranean climatic rhythm (summer drought) began about 3.4Ma and caused the individualization of modern Mediterranean ecosystems. Quaternary-type Mediterranean climatic fluctuations started at 2.6Ma (Gelasian) resulting in repeated steppe vs. forest alternations. A latitudinal climatic gradient between the southern and the northern parts of the Iberian Peninsula existed since the Middle Miocene. |
author2 |
Departamento de Estratigrafia y paleontologia Université de grenade 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) PaleoEnvironnements et PaleobioSphere (PEPS) Université Claude Bernard Lyon 1 (UCBL) Université de Lyon-Université de Lyon-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS) |
format |
Article in Journal/Newspaper |
author |
Jiménez-Moreno, Gonzalo Fauquette, Séverine Suc, Jean-Pierre |
author_facet |
Jiménez-Moreno, Gonzalo Fauquette, Séverine Suc, Jean-Pierre |
author_sort |
Jiménez-Moreno, Gonzalo |
title |
Miocene to Pliocene vegetation and climate estimates in the Iberian Peninsula from pollen data |
title_short |
Miocene to Pliocene vegetation and climate estimates in the Iberian Peninsula from pollen data |
title_full |
Miocene to Pliocene vegetation and climate estimates in the Iberian Peninsula from pollen data |
title_fullStr |
Miocene to Pliocene vegetation and climate estimates in the Iberian Peninsula from pollen data |
title_full_unstemmed |
Miocene to Pliocene vegetation and climate estimates in the Iberian Peninsula from pollen data |
title_sort |
miocene to pliocene vegetation and climate estimates in the iberian peninsula from pollen data |
publisher |
HAL CCSD |
publishDate |
2010 |
url |
https://hal.archives-ouvertes.fr/halsde-00542381 https://doi.org/10.1016/j.revpalbo.2009.08.001 |
geographic |
Antarctic Arctic East Antarctic Ice Sheet |
geographic_facet |
Antarctic Arctic East Antarctic Ice Sheet |
genre |
Antarc* Antarctic Arctic Climate change Ice Sheet |
genre_facet |
Antarc* Antarctic Arctic Climate change Ice Sheet |
op_source |
ISSN: 0034-6667 Review of Palaeobotany and Palynology https://hal.archives-ouvertes.fr/halsde-00542381 Review of Palaeobotany and Palynology, Elsevier, 2010, 162, pp.403-415. ⟨10.1016/j.revpalbo.2009.08.001⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1016/j.revpalbo.2009.08.001 halsde-00542381 https://hal.archives-ouvertes.fr/halsde-00542381 doi:10.1016/j.revpalbo.2009.08.001 |
op_doi |
https://doi.org/10.1016/j.revpalbo.2009.08.001 |
container_title |
Review of Palaeobotany and Palynology |
container_volume |
162 |
container_issue |
3 |
container_start_page |
403 |
op_container_end_page |
415 |
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1766258058208477184 |