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

页码：89 / 93

页数：5

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