Publications des scientifiques de l'IRD

Gasse F., Vidal L., Van Campo E., Demory F., Develle A. L., Tachikawa K., Elias A., Bard E., Garcia M., Sonzogni C., Thouveny Nicolas. (2015). Hydroclimatic changes in northern Levant over the past 400,000 years. Quaternary Science Reviews, 111, p. 1-8. ISSN 0277-3791.

Titre du document
Hydroclimatic changes in northern Levant over the past 400,000 years
Année de publication
2015
Type de document
Article référencé dans le Web of Science WOS:000353431100001
Auteurs
Gasse F., Vidal L., Van Campo E., Demory F., Develle A. L., Tachikawa K., Elias A., Bard E., Garcia M., Sonzogni C., Thouveny Nicolas
Source
Quaternary Science Reviews, 2015, 111, p. 1-8 ISSN 0277-3791
The Levant, a transition zone between the temperate Mediterranean domain and subtropical deserts, is a key area to study the latitudinal migrations of zonal climatic belts in response to glacial-interglacial conditions. The region underwent large climatic shifts during the Late Quaternary, with dramatic impacts on water resources and human populations. This paper presents the unique long-term hydroclimatic record (ca. 400 ka) from Northern Levant, derived from a sediment core taken from a small tectonic basin of northern Lebanon, the currently wettest area of the Levant. Combined biotic (pollen, biologic aquatic remains) and abiotic proxies (sediment properties, carbonate oxygen isotopes) reveal relatively high water availability during interglacials and generally drier glacials periods during the past four climate cycles. These general trends are in line with pollen records from southeastern and near east Mediterranean areas, but differ from some paleohydrological records from the southern Levant. Southward migrations of the rain-bearing mid-latitude westerlies during glacial periods and regional land topography are likely to explain the observed regional climate signatures. In addition, distinctive climate signatures of the successive wetter/drier intervals reflect interactions between global forcing (insolation, atmospheric greenhouse gas concentration), eastern Mediterranean Sea surface conditions intimately linked to North Atlantic climate and to ice-sheet and sea-ice extent at high northern latitudes, land topography, and local hydrogeological processes. Our record brings new benchmarks for understanding the spatial heterogeneity of eastern Mediterranean responses to global climate changes.
Plan de classement
Sciences du milieu [021] ; Hydrologie [062] ; Géologie et formations superficielles [064]
Description Géographique
ZONE MEDITERRANEENNE
Localisation
Fonds IRD
Identifiant IRD
PAR00013075
Contact