Paleocene-Early Eocene planktic foraminifera of the Farafra Oasis, Egypt

被引：8

作者：

Haggag, Mona A. ^{[1
]}

Strougo, Amin ^{[1
]}

Luterbacher, Hanspeter ^{[2
]}

Wielandt, Ulrike ^{[3
]}

机构：

[1] Ain Shams Univ, Fac Sci, Dept Geol, Cairo 11566, Egypt

[2] Museo Geol Seminario Barcelona, E-08007 Barcelona, Spain

[3] Landesamt Geol Rohstoffe & Bergbau Baden Wurttemb, D-79104 Freiburg, Germany

来源：

NEUES JAHRBUCH FUR GEOLOGIE UND PALAONTOLOGIE-ABHANDLUNGEN | 2010年 / 256卷 / 02期

关键词：

Foraminifera; biostratigraphy; biozonation; Paleogene; Egypt; PALAEOCENE/EOCENE BOUNDARY; THERMAL MAXIMUM; BIOSTRATIGRAPHY; SECTION; TURNOVER; ZONATION;

D O I：

10.1127/0077-7749/2010/0041

中图分类号：

Q91 [古生物学];

学科分类号：

0709 ; 070903 ;

摘要：

During the Paleocene and Early Eocene, three main events affected the stratigraphic distribution of the planktic foraminifera in the area of the Farafra Oasis. The first one at the K/Pg boundary is characterized by a stratigraphic gap corresponding to most of the lower Paleocene. The second event starts in the upper part of the Praemurica uncinata Zone (P2) and extends into the Globanomalina pseudomenardii Zone (P4a). It is marked again by a stratigraphic gap corresponding to most of the Middle Paleocene or to numerous short diastems. The third event is the widespread "velascoensis-event". All three events are also reflected by the intensive reworking of older faunas.

引用

页码：161 / 182

页数：22

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