Timing of the Ethiopian flood basalt event and implications for plume birth and global change

被引:520
作者
Hofmann, C
Courtillot, V
Feraud, G
Rochette, P
Yirgu, G
Ketefo, E
Pik, R
机构
[1] INST PHYS GLOBE, F-75252 PARIS 05, FRANCE
[2] UNIV NICE, CNRS, UMR GEOSCI AZUR, F-06108 NICE 2, FRANCE
[3] UNIV AIX MARSEILLE 3, CEREGE, F-13545 AIX EN PROVENCE 4, FRANCE
[4] UNIV ADDIS ABABA, DEPT GEOL & GEOPHYS, ADDIS ABABA, ETHIOPIA
关键词
D O I
10.1038/39853
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
Continental flood basalts are often considered as fossil evidence of mantle plume heads impinging on the lithosphere(1,2) and have been related to continental breakup(3-5). Many of these flood basalts erupted within a short time span-of the order of 1 Myr- and were apparently synchronous with crises in global climate and with mass extinctions(6). Here we present geochronological (40Ar/39Ar) and magnetostratigraphic results for the Ethiopian traps, one of the last remaining flood basalts for which few such data were available. The bulk of the traps, which have been inferred to mark the appearance of the Ethiopian-Afar plume head at the Earth's surface, erupted approximately 30 Myr ago, over a period df 1 Myr or less. This was about the time of a change to a colder and drier global climate, a major continental ice-sheet advance in Antarctica, the largest Tertiary sea-level drop and significant extinctions.
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页码:838 / 841
页数:4
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