ALL TOGETHER NOW: AN INTERNATIONAL PALYNOLOGICAL TEAM DOCUMENTS VEGETATION AND CLIMATE CHANGES DURING THE LAST 500 KYR AT LAKE OHRID (SE EUROPE)
Autor: | Bertini, A., Sadori, L., Nathalie Combourieu-Nebout, Donders, T. H., Kouli, K., Koutsodendris, A., Joannin, S., Masi, A., Mercuri, A. M., Panagiotopoulos, K., Peyron, O., Sinopoli, G., Torri, P., Zanchetta, G., Francke, A., Wagner, B. |
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Přispěvatelé: | Herrada, Anthony, Dipartimento di Scienze della Terra [Firenze] (DST), Università degli Studi di Firenze = University of Florence (UniFI), Università degli Studi di Roma 'La Sapienza' = Sapienza University [Rome] (UNIROMA), Histoire naturelle de l'Homme préhistorique (HNHP), Muséum national d'Histoire naturelle (MNHN)-Université de Perpignan Via Domitia (UPVD)-Centre National de la Recherche Scientifique (CNRS), Utrecht University [Utrecht], Faculty of Geology and Geoenvironment [Athens], National and Kapodistrian University of Athens (NKUA), Heidelberg University, 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), Università degli Studi di Modena e Reggio Emilia = University of Modena and Reggio Emilia (UNIMORE), University of Cologne, Dipartimento di Scienze della Terra [Pisa], University of Pisa - Università di Pisa, Palaeo-ecologie, Coastal dynamics, Fluvial systems and Global change |
Jazyk: | angličtina |
Rok vydání: | 2016 |
Předmět: |
earth-surface processes
geology Balkan peninsula climate flora Lake Ohrid pleistocene pollen vegetation archeology (arts and humanities) paleontology Palaeontology [SDE.MCG]Environmental Sciences/Global Changes Climate Flora Pleistocene Pollen Vegetation Geology [SDE.MCG] Environmental Sciences/Global Changes [SDV.EE.BIO] Life Sciences [q-bio]/Ecology environment/Bioclimatology Archaeology Lake Ohrid pollen flora vegetation climate Pleistocene Balkan peninsula [SDU.STU.PG] Sciences of the Universe [physics]/Earth Sciences/Paleontology [SDV.EE.BIO]Life Sciences [q-bio]/Ecology environment/Bioclimatology [SDU.STU.PG]Sciences of the Universe [physics]/Earth Sciences/Paleontology Earth-Surface Processes |
Zdroj: | Scopus-Elsevier Alpine and Mediterranean Quaternary Alpine and Mediterranean Quaternary, 2016, 29 (2), pp.201-210 |
ISSN: | 2279-7327 2279-7335 |
Popis: | International audience; Lake Ohrid (Balkan peninsula) is the oldest European extant lake and one of the deepest and largest. Such a unique, terrestrial natural archive is especially relevant for both paleoenvironmental and paleoclimatic reconstructions but also for genetic studies. In the frame of the International Continental Scientific Drilling Program (ICDP), a deep drilling campaign was carried out within the scope of the Scientific Collaboration on Past Speciation Conditions in Lake Ohrid (SCOPSCO) project in 2013. Here, we present the summary of palynological analyses carried out in the upper 200 m of the overall 569 m long DEEP site sediment succession from the central part of the lake. These studies, performed by an international palynological team, document the main floristic, vegetation and climate changes during the last ca 500 kyr, at a millennial-scale resolution (~1.6 kyr). The continuous sediment infill permitted to trace multiple non-forested/ forested phases as a response to Glacial/Interglacial cycles as well as to sub-Milankovitch climate changes. The pollen record, corresponding with marine isotope stages MIS 13 to MIS 1, points to a progressive change from cooler and wetter to warmer and drier interglacials. New palynological studies are underway to reconstruct vegetational and climatic conditions over older intervals as well as to obtain high resolution data for some key intervals such as MIS 5-6, MIS 11-12, MIS 35-42. The complete record of changes in flora composition and vegetation during both glacials and interglacials will furnish indispensable insights for understanding the role of refugia, ecosystem resilience and maintenance of terrestrial biodiversity in the Mediterranean area. |
Databáze: | OpenAIRE |
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