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Journal ArticleDOI

The use of chromium reduction in the analysis of reduced inorganic sulfur in sediments and shales

TLDR
In this article, a chromium reduction method was used for the determination of reduced inorganic sulfur compounds (pyrite + elemental sulfur + acid volatile monosulfides) in modern sediments and shales.
About
This article is published in Chemical Geology.The article was published on 1986-01-30. It has received 1268 citations till now. The article focuses on the topics: Sulfur & Chromium.

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Carbon-sulfur-iron systematics of the uppermost deep-water sediments of the Black Sea

TL;DR: In this article, carbon-sulfur relationships (evaluated on a calcium carbonate-free basis to avoid spurious correlations resulting from dilution effects) demonstrate that organic carbon and pyrite-S are essentially decoupled.
Journal ArticleDOI

An emerging picture of Neoproterozoic ocean chemistry: Insights from the Chuar Group, Grand Canyon, USA

TL;DR: In this article, a detailed analysis of the > 742 million year old Chuar Group reveals a marine basin dominated by anoxic and ferrous iron-rich bottom waters punctuated, late in the basin's development, by an intrusion of sulfide-rich (euxinic) conditions.
Journal ArticleDOI

Sulfate-reducing bacteria and their activities in cyanobacterial mats of Solar Lake (Sinai, Egypt)

TL;DR: In this article, the sulfate reducing bacteria within the surface layer of the hypersaline cyanobacterial mat of Solar Lake (Sinai, Egypt) were investigated with combined microbiological, molecular, and biogeochemical approaches.
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Changes in Type II Kerogen Density as a Function of Maturity: Evidence from the Kimmeridge Clay Formation

TL;DR: In this paper, the authors purified 26 samples of the Kimmeridge Clay Formation over the full range of maturities pertinent to petroleum generation, and found that most samples comprised >90% amorphous organic matter (AOM).
References
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Journal ArticleDOI

Sedimentary pyrite formation: An update

TL;DR: In this article, it was shown that organic matter appears to be the major control on pyrite formation in normal (non-euxinic) terrigenous marine sediments where dissolved sulfate and iron minerals are abundant.
Book

Textbook of quantitative inorganic analysis

TL;DR: Textbook of quantitative inorganic analysis as discussed by the authors, Textbook of qualitative and quantitative analysis of inorganic properties, textbook of quantitatively analytically-inorganic analysis, as discussed by the authors.
Journal ArticleDOI

The Sulfur Cycle

TL;DR: The authors' model of the sulfur cycle can draw some conclusions that man is now contributing about one half as much as nature to the total atmospheric burden of sulfur compounds, but by A.D. 2000 he will be contributing about as much, and in the Northern Hemisphere alone he is more than matching nature.
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Pyrite: Its Rapid Formation in a Salt Marsh and Its Importance In Ecosystem Metabolism

TL;DR: Pyrite formation in salt-marsh peat occurs more rapidly than is generally thought for any natural system, and the rates of sulfate reduction and ecosystem respiration may be grossly underestimated.
Book

Rock and mineral analysis

TL;DR: In this paper, the authors provide an up-to-date treatment of the problems associated with the analysis of geological materials, including the requesite steps from selection of the sample and choice of elements to the facilities needed, preparation of sample, methods for the determination of individual constituens and reporting of the results of the analysis.