Title of article :
A Late Glacial–Early Holocene multiproxy record from the eastern Fram Strait, Polar North Atlantic
Author/Authors :
Aagaard-Sّrensen، نويسنده , , S. and Husum، نويسنده , , Helen K. and Werner-Washburne، نويسنده , , K. and Spielhagen، نويسنده , , R.F. and Hald، نويسنده , , M. and Marchitto، نويسنده , , T.M.، نويسنده ,
Issue Information :
روزنامه با شماره پیاپی سال 2014
Pages :
12
From page :
15
To page :
26
Abstract :
The paleoceanographic development of the eastern Fram Strait during the transition from the cold Late Glacial and into the warm Early Holocene was elucidated via a multiproxy study of a marine sediment record retrieved at the western Svalbard slope. The multiproxy study includes analyses of planktic foraminiferal fauna, bulk sediment grain size and CaCO3 content in addition to Mg/Ca ratios and stable isotopes (δ13C and δ18O) measured on the planktic foraminifer Neogloboquadrina pachyderma. Furthermore paleosubsurface water temperatures were reconstructed via Mg/Ca ratios (sSSTMg/Ca) and transfer functions (sSSTTransfer) enabling comparison between the two proxies within a single record. The age model was constrained by four accelerator mass spectrometry (AMS) 14C dates. 4,000 to 10,300 cal yr B.P. N. pachyderma dominated the planktic fauna and cold polar sea surface conditions existed. The period was characterized by extensive sea ice cover, iceberg transport and low subsea surface temperatures (sSSTTransfer ~ 2.1 °C; sSSTMg/Ca ~ 3.5 °C) resulting in restricted primary production. Atlantic Water inflow was reduced compared to the present-day and likely existed as a subsurface current. At ca. 10,300 cal yr B.P. Atlantic Water inflow increased and the Arctic Front retreated north-westward resulting in increased primary productivity, higher foraminiferal fluxes and a reduction in sea ice cover and iceberg transport. The fauna rapidly became dominated by the subpolar planktic foraminifer Turborotalita quinqueloba and summer sSSTTransfer increased by ~ 3.5 °C. Concurrently, the sSSTMg/Ca recorded by N. pachyderma rose only ~ 0.5 °C. From ca. 10,300 to 8600 cal yr B.P. the average sSSTMg/Ca and sSSTTransfer were ~ 4.0 °C and ~ 5.5 °C, respectively. The relatively modest change in sSSTMg/Ca compared to sSSTTransfer can probably be tied to a change of the main habitat depth and/or shift in the calcification season for N. pachyderma during this period.
Keywords :
Polar North Atlantic , Planktic foraminifera , sub-sea surface temperature reconstruction , transfer functions , Trace elements , stable isotopes , Late Glacial/Holocene transition , Fram Strait
Journal title :
Marine Geology
Serial Year :
2014
Journal title :
Marine Geology
Record number :
2258846
Link To Document :
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