A reassessment of the age of the Cockburn Island Formation, northern Antarctic Peninsula, and its palaeoclimatic implications

被引:28
作者
Jonkers, HA
Kelley, SP
机构
[1] British Antarctic Survey, NERC, Cambridge CB3 0ET, England
[2] Open Univ, Dept Earth Sci, Milton Keynes MK7 6AA, Bucks, England
关键词
Antarctica; Pliocene; palaeoclimatology; 40Ar-39Ar; diatoms;
D O I
10.1144/gsjgs.155.5.0737
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
New constraints on the age of the Cockburn Island Formation, northern Antarctic Peninsula, resulting from whole rock laser-stepped heated 40Ar-39Ar dating of associated basalt and palaeomagnetic re-calibration of the ranges of the formation's fossil diatom taxa, suggest that interglacial conditions existed around 3 million years ago. The refined age of the deposit supports continent-wide Late Pliocene warming in Antarctica, and makes more likely the occurrence of extensive marine incursions in East Antarctica at that time.
引用
收藏
页码:737 / 740
页数:4
相关论文
共 33 条
[1]  
Andersson J.Gunnar, 1906, Upsala Bull Geol Inst, V7
[2]  
BALDAUF JG, 1991, P OC DRILL PROGR SCI, V0119
[3]   GEOCHRONOLOGICAL EVIDENCE SUPPORTING ANTARCTIC DEGLACIATION 3 MILLION YEARS AGO [J].
BARRETT, PJ ;
ADAMS, CJ ;
MCINTOSH, WC ;
SWISHER, CC ;
WILSON, GS .
NATURE, 1992, 359 (6398) :816-818
[4]  
Berggren W.A., 1995, GEOCHRONOLOGY TIME S, V54, P129
[5]  
Burckle LH, 1996, GEOLOGY, V24, P235, DOI 10.1130/0091-7613(1996)024<0235:PPDIPA>2.3.CO
[6]  
2
[7]   IMPLICATIONS OF A PLIOCENE STAND OF NOTHOFAGUS (SOUTHERN BEECH) WITHIN 500-KILOMETERS OF THE SOUTH-POLE [J].
BURCKLE, LH ;
POKRAS, EM .
ANTARCTIC SCIENCE, 1991, 3 (04) :389-403
[8]  
Denton G.H., 1993, GEOGR ANN, V75A, P155, DOI DOI 10.2307/521200
[9]  
DENTON GH, 1984, GEOLOGY, V12, P263, DOI 10.1130/0091-7613(1984)12<263:LTHOTA>2.0.CO
[10]  
2