Influence of Atlantic Ocean thermohaline circulation on Northwest African climate during the Holocene/Late Pleistocene: Inferences from geochemical analysis, plant wax stable hydrogen (dD) and carbon (d13C) isotopic composition.

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dc.contributor.authorBAQLOUL Asmae
dc.date.accessioned2019-07-11T14:14:32Z
dc.date.accessioned2025-05-21T09:03:33Z
dc.date.available2019-07-11T14:14:32Z
dc.date.issued2019-07-11
dc.date.registred2019
dc.description.cedCEDOC IBN ZOHR
dc.description.collaboratorBOUCHAOU LHOUSSAINE
dc.description.laboratoryGéosciences et Géo-environnement
dc.identifier.urihttps://otrohati.imist.ma/handle/123456789/59145
dc.titleInfluence of Atlantic Ocean thermohaline circulation on Northwest African climate during the Holocene/Late Pleistocene: Inferences from geochemical analysis, plant wax stable hydrogen (dD) and carbon (d13C) isotopic composition.

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