High-frequency climate fluctuations over the last deglaciation in the Alboran Sea, Western Mediterranean: Evidence from calcareous plankton assemblages

作者: Pietro Bazzicalupo , Patrizia Maiorano , Angela Girone , Maria Marino , Nathalie Combourieu-Nebout

DOI: 10.1016/J.PALAEO.2018.06.042

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摘要: Abstract A high resolution study, with a centennial scale resolution, has been performed on the calcareous plankton assemblage (coccolithophores and planktonic foraminifera) at Ocean Drilling Program Site 976, Alboran Sea (Western Mediterranean), focusing interval between 20 9 ka, in order to reconstruct changes surface subsurface water dynamics productivity. The biotic proxies integrate extremely detailed (multi-decadal scale) geochemical data set pollen record already available core, thus providing complete paleoenvironmental/paleoceanographic reconstruction. results highlight sensitivity of recording stadial/interstadial phases higher-frequency climatic events, that produced sea features. Wind-induced upwelling river discharge during Last Glacial Period favored nutrient availability moderate During Heinrich Stadial 1 (HS1), arrival cold fresher waters from iceberg melting North Atlantic, significantly hampered productivity, its lowest values whole investigated interval. Calcareous behavior supports hypothesis HS1 is composite event, marked by three phases: HS1a characterized coldest SST, polar Atlantic inflow into basin first step toward dry climate continent; HS1b enhanced freshwater drought land, HS1c indicating reduced influx. Bolling-Allerod (BA) interstadial sees highest rate productivity entire accompanies deposition Organic Rich Layer 1; BA coccolithophore also marks higher frequency hydrographic conditions, apparently relation Greenland Interstadial I (GI-I) variability. Younger Dryas (YD) refunding although not as severe HS1, detrital input drier conditions land. Holocene onset records amelioration both marine continental environment, BA. rapid shifts sensitive taxa support each phases-subphases complex pattern forced strong interaction ice-sheet instability, meltwater entering Gibraltar Strait, westerlies moisture availability, clearly impacting over temperature, land masses.

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