CONSTRAINTS ON THE AGE AND DURATION OF THE LAST INTERGLACIAL PERIOD AND ON SEA-LEVEL VARIATIONS

被引：106
作者：
LAMBECK, K [1 ]
NAKADA, M [1 ]
机构：
[1] KUMAMOTO UNIV,FAC SCI,DEPT GEOL,KUMAMOTO 860,JAPAN
来源：
NATURE | 1992年 / 357卷 / 6374期
关键词：
D O I：
10.1038/357125a0
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 relation between height and age of shorelines formed during the last interglacial period, as revealed by coral reefs, cannot be related directly to changes in ocean volume because of the effect of isostatic uplift in response to changes in ice-sheet loading. Sea-level changes at sites near the melting ice sheet, such as Bermuda and the Caribbean islands, differ from those along the Australian margin. Modelling of these differences constrains the times of onset and termination of the last interglacial, which are at variance with those deduced from oxygen-isotope studies of deep-sea cores.
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页码：125 / 128
页数：4
相关论文
共 33 条
[1]  
[Anonymous], URANIUM SERIES DISEQ
[2]  
BARD E, 1990, NATURE, V346, P456, DOI 10.1038/346456a0
[3]  
BENDER ML, 1979, GEOL SOC AM BULL, V90, P577, DOI 10.1130/0016-7606(1979)90<577:UDOTPR>2.0.CO
[4]  
2
[5]  
CHEN JH, 1991, GEOL SOC AM BULL, V103, P81
[6]  
Cronin T.M, 1983, QUATERNARY SCI REV, V1, P177
[7]  
DANSGAARD W, 1981, BOREAS, V10, P219
[8]  
DETTRICK RS, 1986, J GEOPHYS RES, V91, P3701
[9]   PLEISTOCENE SEA LEVELS FROM RAISED CORAL REEFS OF HAITI [J].
DODGE, RE ;
FAIRBANKS, RG ;
BENNINGER, LK ;
MAURRASSE, F .
SCIENCE, 1983, 219 (4591) :1423-1425
[10]  
FLOHN H, 1984, PALAEOCLIMATIC RES M, P17
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