COOLING OF TROPICAL BRAZIL (5-DEGREES-C) DURING THE LAST GLACIAL MAXIMUM

被引:438
作者
STUTE, M
FORSTER, M
FRISCHKORN, H
SEREJO, A
CLARK, JF
SCHLOSSER, P
BROECKER, WS
BONANI, G
机构
[1] UNIV FED CEARA, BR-60450 FORTALEZA, CEARA, BRAZIL
[2] COLUMBIA UNIV, DEPT GEOL SCI, NEW YORK, NY 10027 USA
[3] ETH ZURICH, INST MITTELENERGIEPHYS, CH-8093 ZURICH, SWITZERLAND
关键词
D O I
10.1126/science.269.5222.379
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
A 30,000-year paleotemperature record derived from noble gases dissolved in carbon-14-dated ground water indicates that the climate in lowland Brazil (Piaui Province, 7 degrees S, 41.5 degrees W; altitude, 400 meters) was 5.4 degrees +/- 0.6 degrees C cooler during the last glacial maximum than today. This result suggests a rather uniform cooling of the Americas between 40 degrees S and 40 degrees N. A 5.4 degrees C cooling of tropical South America is consistent with pollen records, snow line reconstructions, and strontium/calcium ratios and delta(18)O coral records but is inconsistent with the sea-surface temperature reconstruction of CLIMAP (Climate: Long-Range Investigation. Mapping and Prediction). On the basis of these results, it appears that the tropical Americas are characterized by a temperature sensitivity comparable to that found in higher latitudes.
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页码:379 / 383
页数:5
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