Late Quaternary vegetation and climate of SE Europe -NW Asia according to pollen records in three offshore cores from the Black and Marmara seas

International audience High-resolution pollen analyses were performed on two cores from the western Black Sea and one core from the Marmara Sea, covering the Late Glacial-Holocene transition using 14C chronology. Particular effort was invested in the botanical identification of pollen grains thereby...

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Published in:Palaeobiodiversity and Palaeoenvironments
Main Authors: Popescu, Speranta-Maria, Jiménez-Moreno, Gonzalo, Klotz, Stefan, Lericolais, Gilles, Guichard, François, Çağatay, M, Giosan, Liviu, Calleja, Michel, Fauquette, Séverine, Suc, Jean-Pierre
Other Authors: GeoBioStratData.Consulting, Rillieux la Pape, France, Departamento de Estratigrafia y paleontologia, Université de grenade, Karl-Eberhardt Universität Tübingen, Institut Français de Recherche pour l'Exploitation de la Mer - Brest (IFREMER Centre de Bretagne), Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER), Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ), Faculty of Mining, Istanbul, Geology and Geophysics Department, Woods Hole Oceanographic Institution, Woods Hole, MA, USA, Institut national d’études supérieures agronomiques de Montpellier (Montpellier SupAgro), Institut des Sciences de l'Evolution de Montpellier (UMR ISEM), École pratique des hautes études (EPHE), Université Paris sciences et lettres (PSL)-Université Paris sciences et lettres (PSL)-Université de Montpellier (UM)-Centre de Coopération Internationale en Recherche Agronomique pour le Développement (Cirad)-Centre National de la Recherche Scientifique (CNRS)-Institut de recherche pour le développement IRD : UR226, Institut des Sciences de la Terre de Paris (iSTeP), Centre National de la Recherche Scientifique (CNRS)-Sorbonne Université (SU)-Institut national des sciences de l'Univers (INSU - CNRS)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2020
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Online Access:https://doi.org/10.1007/s12549-020-00464-x
https://hal.archives-ouvertes.fr/hal-02957446/file/Popescu%20et%20al.,%20in%20press,%20Palaeobiodiversity%20and%20Palaeoenvironments.pdf
https://hal.archives-ouvertes.fr/hal-02957446
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Summary:International audience High-resolution pollen analyses were performed on two cores from the western Black Sea and one core from the Marmara Sea, covering the Late Glacial-Holocene transition using 14C chronology. Particular effort was invested in the botanical identification of pollen grains thereby significantly improving our knowledge of regional flora. When interpreted with respect to modern vegetation, pollen records revealed all the major changes caused by climatic fluctuations over the last 20,000 years. The results of this study provide evidence for the occurrence of relict thermophilous-hygrophilous trees (papillate Cupressaceae, Carya, Liquidambar, Zelkova) in certain refugia up to the Holocene. Vegetation dynamics is specified for some taxa (e.g. Cupressus–Juniperus, Fagus, Cedrus) and some ecosystems (e.g. mesophilous forests, Mediterranean sclerophyllous populations, steppes). Pollen data enabled palaeoclimatic reconstructions which were compared with available estimates in the region. The use of a powerful pollen ratio between ‘thermophilous and steppe taxa’ led to fruitful climatostratigraphic relationships with the oxygen isotope curve from the NGRIP core. The Younger Dryas and cooling at 8.2 ka are among the most obvious climatic phases identified in the three cores studied here.