10.1594/PANGAEA.733897
Anderson, David M
David M
Anderson
0000-0001-9507-6777
Prell, Warren L
Warren L
Prell
Barratt, N J
N J
Barratt
Estimates of sea surface temperatures in the Coral Sea
PANGAEA
1989
Piston corer
RC09
RC10
RC12
V24
Robert Conrad
Vema
Lamont-Doherty Earth Observatory, Columbia University (LDEO)
1965-04-09T00:00:00/1968-05-06T00:00:00
en
Supplementary Publication Series of Datasets
10.1029/PA004i006p00615
22 datasets
application/zip
Creative Commons Attribution 3.0 Unported
The CLIMAP [1981] reconstruction of the Coral Sea found relatively little cooling (2°C) in the low latitudes (10°S) but a warming off Australia at about 25°S. The small low-latitude changes are of interest because terrestrial pollen and snowline data from the New Guinea highlands imply that surface temperatures may have been 6° to 9°C colder at the last glacial maximum (LGM). The purpose of this paper is to evaluate these conclusions on the basis of additional core sites, new oxygen isotope stratigraphy, and new sea surface temperature (SST) estimates using the modern analog technique (MAT). In the northern Coral Sea, planktonic foraminifer assemblages consist of tropical-subtropical species that show little change over the past 20 kyr. Quantitative estimates of SST using the modern analog technique (MAT) confirm the CLIMAP [1981] conclusion that little or no temperature change occurred in this tropical region at the LGM, thus reinforcing the conflict with terrestrial evidence. In the southern region (25°S), two cores indicate that foraminifer faunas became more subtropical at the LGM. The MAT estimates for the LGM are 3° to 4°C colder than modern, producing a steeper thermal gradient in the southern Coral Sea. These data remove the warm SST anomaly along the eastern coast of Australia and indicate that during the LGM, cool high- latitude waters were displaced northward along the coast of Australia into the southern Coral Sea.
Supplement to: Anderson, David M; Prell, Warren L; Barratt, N J (1989): Estimates of sea surface temperature in the Coral Sea at the last glacial Maximum. Paleoceanography, 4(6), 615-627
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