Restructuring outer neritic foraminiferal assemblages in the aftermath of the Paleocene-Eocene thermal maximum

被引：10
|
作者：
Stassen, Peter [1 ]
Thomas, Ellen [2 ,3 ]
Speijer, Robert. P. [1 ]
机构：
[1] Katholieke Univ Leuven, Dept Earth & Environm Sci, B-3001 Louvain, Belgium
[2] Yale Univ, Dept Geol & Geophys, New Haven, CT 06520 USA
[3] Wesleyan Univ, Dept Earth & Environm Sci, Middletown, CT 06459 USA
来源：
JOURNAL OF MICROPALAEONTOLOGY | 2012年 / 31卷
基金：
美国国家科学基金会;
关键词：
Paleocene-Eocene thermal maximum; benthic foraminifera; neritic; stratigraphy; DABABIYA; EGYPT; BOUNDARY; SECTION;
D O I：
10.1144/0262-821X11-026
中图分类号：
Q91 [古生物学];
学科分类号：
0709 ; 070903 ;
摘要：
Deep-sea benthic foraminiferal faunas underwent severe extinction during the Paleocene-Eocene thermal maximum (PETM), but less is known about neritic environments. Through taxonomical analysis we document for the first time that recovery of neritic benthic assemblages after the PETM followed a similar pattern in shelf regions in New Jersey (USA) and Egypt. J. Micropalaeontol. 31(1): 89-93, February 2012.
引用
收藏
页码：89 / 93
页数：5
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