Causes of oxic-anoxic changes in Cretaceous marine environments and their implications for Earth systems-An introduction

被引：20

作者：

Wagreich, Michael ^{[1
]}

Hu, Xiumian ^{[2
]}

Sageman, Brad ^{[3
]}

机构：

[1] Univ Vienna, Dept Geodynam & Sedimentol, A-1090 Vienna, Austria

[2] Nanjing Univ, Sch Earth Sci & Engn, State Key Lab Mineral Deposits Res, Nanjing 210093, Peoples R China

[3] Northwestern Univ, Dept Earth & Planetary Sci, Evanston, IL 60208 USA

来源：

SEDIMENTARY GEOLOGY | 2011年 / 235卷 / 1-2期

关键词：

Oxic-anoxic changes; Cretaceous; Palaeoclimate; OCEANIC RED BEDS; CARBON; RECORD; CORBS; ICE;

D O I：

10.1016/j.sedgeo.2010.10.012

中图分类号：

P5 [地质学];

学科分类号：

0709 ; 081803 ;

摘要：

This special issue originated from a session at the 33th International Geological Congress, Oslo, Norway, in August 2008: Causes of oxic-anoxic changes in Cretaceous marine and non-marine environments and their implications for Earth systems (IGCP 463 and 555), convened by Chengshan Wang, Michael Wagreich, and Bradley Sageman. The session aimed at bringing together contributions that shed light on the anoxic to oxic changes in the world oceans during the Cretaceous, including discussion on consequences for today's global change. (C) 2010 Elsevier B.V. All rights reserved.

引用

页码：1 / 4

页数：4

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