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Plio-Pleistocene Indonesian Throughflow Variability Drove Eastern Indian Ocean Sea Surface Temperatures

Smith, Rebecca A. (författare)
Univ Massachusetts, Dept Geosci, Amherst, MA 01003 USA.
Castaneda, Isla S. (författare)
Univ Massachusetts, Dept Geosci, Amherst, MA 01003 USA.
Groeneveld, Jeroen (författare)
Helmholtz Ctr Polar & Marine Res, Alfred Wegener Inst, Potsdam, Germany.
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De Vleeschouwer, David (författare)
Univ Bremen, MARUM Ctr Marine & Environm Sci, Bremen, Germany.
Henderiks, Jorijntje (författare)
Uppsala universitet,Paleobiologi
Christensen, Beth A. (författare)
Rowan Univ, Dept Environm Sci, Glassboro, NJ USA.
Renema, Willem (författare)
Natl Nat Hist Museum, Leiden, Netherlands.
Auer, Gerald (författare)
Karl Franzens Univ Graz, Inst Earth Sci, Graz, Austria.
Bogus, Kara (författare)
Univ Exeter, Camborne Sch Mines, Penryn, Cornwall, England.;Texas A&M Univ, Int Ocean Discovery Program, College Stn, TX USA.
Gallagher, Stephen J. (författare)
Univ Melbourne, Sch Earth Sci, Melbourne, Vic, Australia.
Fulthorpe, Craig S. (författare)
Univ Texas Austin, Inst Geophys, Jackson Sch Geosci, Austin, TX USA.
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Univ Massachusetts, Dept Geosci, Amherst, MA 01003 USA Helmholtz Ctr Polar & Marine Res, Alfred Wegener Inst, Potsdam, Germany. (creator_code:org_t)
American Geophysical Union (AGU), 2020
2020
Engelska.
Ingår i: PALEOCEANOGRAPHY AND PALEOCLIMATOLOGY. - : American Geophysical Union (AGU). - 2572-4517 .- 2572-4525. ; 35:10
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
Stäng  
  • Ocean gateways facilitate circulation between ocean basins, thereby impacting global climate. The Indonesian Gateway transports water from the Pacific to the Indian Ocean via the Indonesian Throughflow (ITF) and drives the strength and intensity of the modern Leeuwin Current, which carries warm equatorial waters along the western coast of Australia to higher latitudes. Therefore, ITF dynamics are a vital component of global thermohaline circulation. Plio-Pleistocene changes in ITF behavior and Leeuwin Current intensity remain poorly constrained due to a lack of sedimentary records from regions under its influence. Here, organic geochemical proxies are used to reconstruct sea surface temperatures on the northwest Australian shelf at IODP Site U1463, downstream of the ITF outlet and under the influence of the Leeuwin Current. Our records, based on TEX86 and the long-chain diol index, provide insight into past ITF variability (3.5-1.5 Ma) and confirm that sea surface temperature exerted a control on Australian continental hydroclimate. A significant TEX86 cooling of similar to 5 degrees C occurs within the mid-Pliocene Warm Period (3.3-3.1 Ma) suggesting that this interval was characterized by SST fluctuations at Site U1463. A major feature of both the TEX86 and long-chain diol index records is a strong cooling from similar to 1.7 to 1.5 Ma. We suggest that this event reflects a reduction in Leeuwin Current intensity due to a major step in ongoing ITF constriction, accompanied by a switch from South to North Pacific source waters entering the ITF inlet. Our new data suggest that an additional ITF constriction event may have occurred in the Pleistocene.

Ämnesord

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Klimatforskning (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Climate Research (hsv//eng)

Nyckelord

TEX86
LDI
Indonesian Throughflow
sea surface temperature
Pliocene
Pleistocene

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