Synchronous tropical South China Sea SST change and Greenland warming during deglaciation

被引：177

作者：

Kienast, M ^{[1
]}

Steinke, S

Stattegger, K

Calvert, SE

机构：

[1] Univ British Columbia, Vancouver, BC V6T 1Z4, Canada

[2] Univ Kiel, Inst Geowissensch, Kiel, Germany

来源：

SCIENCE | 2001年 / 291卷 / 5511期

关键词：

D O I：

10.1126/science.1057131

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：

The tropical ocean plays a major role in global climate, It is therefore crucial to establish the precise phase between tropical and high-latitude climate variability during past abrupt climate events in order to gain insight into the mechanisms of global climate change. Here we present alkenone sea surface temperature (SST) records from the tropical South China Sea that show an abrupt temperature increase of at least 1 degreesC at the end of the Last glacial period. Within the recognized dating uncertainties, this SST increase is synchronous with the Bolling warming observed at 14.6 thousand years ago in the Greenland Ice Sheet Project 2 ice core.

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页码：2132 / 2134

页数：3

相关论文

共 28 条

[1] THE OXYGEN-ISOTOPE COMPOSITION OF TROPICAL OCEAN SURFACE-WATER DURING THE LAST DEGLACIATION [J].

ANDERSON, DM ;

THUNELL, RC .

QUATERNARY SCIENCE REVIEWS, 1993, 12 (06) :465-473

[2] Hydrological impact of Heinrich events in the subtropical northeast Atlantic [J].

Bard, E ;

Rostek, F ;

Turon, JL ;

Gendreau, S .

SCIENCE, 2000, 289 (5483) :1321-1324

[3] Interhemispheric synchrony of the last deglaciation inferred from alkenone palaeothermometry [J].

Bard, E ;

Rostek, F ;

Sonzogni, C .

NATURE, 1997, 385 (6618) :707-710

[4] CORRECTION OF ACCELERATOR MASS SPECTROMETRY C-14 AGES MEASURED IN PLANKTONIC FORAMINIFERA: PALEOCEANOGRAPHIC IMPLICATIONS [J].

Bard, Edouard .

PALEOCEANOGRAPHY, 1988, 3 (06) :635-645

[5] LONG-TERM VARIATIONS OF CALORIC INSOLATION RESULTING FROM EARTHS ORBITAL ELEMENTS [J].

BERGER, AL .

QUATERNARY RESEARCH, 1978, 9 (02) :139-167

[6] Dansgaard-Oeschger and heinrich event imprints in Alboran Sea paleotemperatures [J].

Cacho, I ;

Grimalt, JO ;

Pelejero, C ;

Canals, M ;

Sierro, FJ ;

Flores, JA ;

Shackleton, N .

PALEOCEANOGRAPHY, 1999, 14 (06) :698-705

[7] Planktonic foraminiferal and alkenone records of the last deglaciation from the Eastern Arabian Sea [J].

Cayre, O ;

Bard, E .

QUATERNARY RESEARCH, 1999, 52 (03) :337-342

[8] Biomarker temperature estimates for modern and last glacial surface waters of the California Current system between 33 degrees and 42 degrees N [J].

Doose, H ;

Prahl, FG ;

Lyle, MW .

PALEOCEANOGRAPHY, 1997, 12 (04) :615-622

[9] HOW FAST DID THE OCEAN - ATMOSPHERE SYSTEM RUN DURING THE LAST DEGLACIATION [J].

DUPLESSY, JC ;

BARD, E ;

ARNOLD, M ;

SHACKLETON, NJ ;

DUPRAT, J ;

LABEYRIE, L .

EARTH AND PLANETARY SCIENCE LETTERS, 1991, 103 (1-4) :27-40

[10] Rapid flooding of the Sunda Shelf: A late-glacial sea-level record [J].

Hanebuth, T ;

Stattegger, K ;

Grootes, PM .

SCIENCE, 2000, 288 (5468) :1033-1035