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Ordovician-Silurian Boundary Extinction and Its Relationship to Iridium and carbon Isotope Anomalies
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作者 Wang Xiaofeng Chai Zhifang Yichang Institute of Geology and Minieral Resources, Chinese Academy of Geological Sciences, Yichang. Hubei Institute of High Energy, Academia Sinica, Beijing Liu Linqun 《Acta Geologica Sinica(English Edition)》 SCIE CAS CSCD 1990年第1期81-92,共12页
The abundance distributions of more than 40 elements in the No. 502 Ordovician-Silurian (O/S) bounda-ry section at Fenxiang, Yichang have been studied by RNAA and INAA. The results show that in the bounda-ry bed, ther... The abundance distributions of more than 40 elements in the No. 502 Ordovician-Silurian (O/S) bounda-ry section at Fenxiang, Yichang have been studied by RNAA and INAA. The results show that in the bounda-ry bed, there is a distinctive Ir anomaly because the Ir concentration abruptly increases to 0.64 ppb.Furthermore, the Ir is positively correlated in abundance variation with some siderophile and sulphophile ele-ments. In the same bed of the O/S boundary section at Huanghuachang, Yichang, there is also a δ^(13)C excur-sion. These geochemical signs support the hypothesis that the terminal Ordovician mass extinction was proba-bly related to extraterrestrial event, and provide new evidence for defining the O/S boundary between theHirnantia-Kinnella and G. persculptus Zones. 展开更多
关键词 Ordovician-Silurian Boundary Extinction and Its Relationship to iridium and carbon Isotope Anomalies Chen Wang
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Some Evidence for a Possible Extraterrestrial Event at/near Permian-Triassic Boundary 被引量:2
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作者 Xu Daoyi Institute of Geology, China Seismological Bureau, Beijing 100029 《Journal of China University of Geosciences》 SCIE CSCD 2002年第2期151-156,共6页
A selection of evidence, including a carbon isotopic excursion, iridium anomaly, fullerenes (C 60 and C 70 ) with trapped noble gases, microspherules and shocked quartz, is discussed in this paper. All the ev... A selection of evidence, including a carbon isotopic excursion, iridium anomaly, fullerenes (C 60 and C 70 ) with trapped noble gases, microspherules and shocked quartz, is discussed in this paper. All the evidence in hand favors the hypothesis that the PTB event was probably related to an extraterrestrial cause, and the impact would lead to great physical change, including large volcanic eruptions on the earth's surface. The ET markers for the CTB event could be considered only as an example, and cannot be taken as a unique standard of an ET event. 展开更多
关键词 Permian Triassic boundary extraterrestrial event iridium anomaly carbon isotopic excursion.
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What happened at Precambrian-Cambrian boundary
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作者 Weijia Zhang1a Xiaodong Zou1b Hangjie Yu2 Yang Lei1a(1a.Department ofPhysics and Astronomy, PekingUniversity, Beijing 100871 1b.Research Institute of Paleontology, Peking University, Beijing 100871 2.School of Physics, Sun Yat-sen University, Zhuhai, Guangdong 510275) 《科技风》 2010年第11期267-,共1页
The Precambrian-Cambrian boundary represents one of the most puzzling and intriguing transitions in Earth history. One of the former hypotheses put forward an evolutional mechanism after a bolide impact, which is stil... The Precambrian-Cambrian boundary represents one of the most puzzling and intriguing transitions in Earth history. One of the former hypotheses put forward an evolutional mechanism after a bolide impact, which is still uncertain. Anyhow, biological and geological studies seem to be favorable to an impact. Three most important elements were discovered and thus shed light upon the issue. 展开更多
关键词 Impact crater iridium anomaly negative C13 excursion
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