An alternative age model for the Paleocene-Eocene thermal maximum using extraterrestrial 3He

被引:139
作者
Farley, KA [1 ]
Eltgroth, SF [1 ]
机构
[1] CALTECH, Div Geol & Planetary Sci, Pasadena, CA 91125 USA
基金
美国国家科学基金会;
关键词
D O I
10.1016/S0012-821X(03)00017-7
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
A continuous age model for the brief climate excursion at the Paleocene-Eocene boundary has been constructed by assuming a constant flux of extraterrestrial He-3 (He-3(ET)) to the seafloor. (HeET)-He-3 measurements from ODP Site 690 provide quantitative evidence for the rapid onset ( < few kyr) and short duration ( < 120 kyr) of global warming and of the associated disturbance to the Earth's surficial carbon budget at this time. These observations support astronomically calibrated age models indicating extremely rapid release of isotopically light carbon, possibly from seafloor methane hydrate, as' the proximal cause of the event. However, the He-3(ET) technique indicates a previously unrecognized and extreme increase in sedimentation rate coincident with the return of climate proxies to pre-event values. The He-3(ET)-based age model thus suggests a far more rapid recovery from the climatic perturbation than previously proposed or predicted on the basis of the modern carbon cycle, and so may indicate additional or accelerated mechanisms of carbon removal from the ocean-atmosphere system during this period. He-3(ET) was also measured at ODP Site 1051 to test the validity of the Site 690 chronology. Comparison of these data sets seems to require removal of several tens of kyr of sediment within the climatic excursion at Site 1051, an observation consistent with sediment structures and previous age modeling efforts. The Site 1051 age model shows a similar to30 kyr period in which climate proxies return toward pre-event values, after which they remain invariant for similar to80 kyr. If this rise represents the recovery interval identified at Site 690, then the 3 HeET-based age models of the two sites are in good agreement. However, alternative interpretations are possible, and work on less disrupted sites is required to evaluate the reliability of the proposed new chronology of the climate excursion. Regardless of these details, this work shows that the 3HeET technique can provide useful independent evidence for the development and testing of astronomically calibrated age models. (C) 2003 Elsevier Science B.V. All rights reserved.
引用
收藏
页码:135 / 148
页数:14
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