SULFUR SINKS AND ORGANIC-CARBON RELATIONSHIPS IN CRETACEOUS ORGANIC-RICH CARBONATES - IMPLICATIONS FOR EVALUATION OF OXYGEN-POOR DEPOSITIONAL-ENVIRONMENTS

被引：51

作者：

BEIN, A ^{[1
]}

ALMOGILABIN, A ^{[1
]}

SASS, E ^{[1
]}

机构：

[1] HEBREW UNIV JERUSALEM,DEPT GEOL,IL-91904 JERUSALEM,ISRAEL

来源：

AMERICAN JOURNAL OF SCIENCE | 1990年 / 290卷 / 08期

关键词：

D O I：

10.2475/ajs.290.8.882

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

A succession of Upper Cretaceous organic-rich carbonates and phosphorites in central Israel was used to study the relationships between sulfur sinks and organic carbon. In these sediments, deposited in oxygen-deficient and iron-poor environments, organic matter is the sink for the H2S obtained from sulfate reduction. The observed relationships between pyrite, organic sulfur, organic S/C ratio, and reduced sulfur isotopic composition provide valuable information on oxygen-poor depositional regimes. -from Authors

引用

页码：882 / 911

页数：30

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