PYRITE - ITS RAPID FORMATION IN A SALT-MARSH AND ITS IMPORTANCE IN ECOSYSTEM METABOLISM

被引：256

作者：

HOWARTH, RW

机构：

来源：

SCIENCE | 1979年 / 203卷 / 4375期

关键词：

D O I：

10.1126/science.203.4375.49

中图分类号：

O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];

学科分类号：

07 ; 0710 ; 09 ;

摘要：

Pyrite formation in salt-marsh peat occurs more rapidly than is generally thought for any natural system. Pyrite is the major end product of sulfate reduction, and sulfate reduction is the major form of respiration in the salt-marsh ecosystem. When the rapid formation of pyrite is ignored, the rates of sulfate reduction and ecosystem respiration may be grossly underestimated. Copyright © 1978 AAAS.

引用

页码：49 / 51

页数：3

共 14 条

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