THE OSTRACODAL RESPONSE TO THE CENOMANIAN-TURONIAN BOUNDARY EVENT AT WESTBURY (WILTSHIRE, UK)

被引：0
|
作者：
Vaziri, M. R. [1 ]
机构：
[1] Shahid Bahonar Univ, Fac Sci, Dept Geol, Kerman, Iran
来源：
IRANIAN JOURNAL OF SCIENCE AND TECHNOLOGY TRANSACTION A-SCIENCE | 2009年 / 33卷 / A1期
关键词：
Extinction; ostracods; stable isotopes; Cenomanian-Turonian boundary;
D O I：
暂无
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：
A detailed study of Ostracoda changes against the stable isotopes of carbon and oxygen across the Cenomanian-Turonian boundary mass extinction has been fully documented in one section, the South of England. This section comprises the uppermost Cenomanian to lowermost Turonian strata. The comparison between the results obtained in this research and two rival models for the Cenomanian-Turonian boundary mass extinction, famine and high productivity, have been carried out. Low oxygen level has been proposed as the main cause of the Cenomanian-Turonian boundary mass extinction.
引用
收藏
页码：109 / 119
页数：11
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