Literature DB >> 17792783

Oxygen-18 composition of oceanic sulfate.

R M Llyod.   

Abstract

Comparison of experimental data with analyses of oceanic sulfate indicates that oceanic sulfate is not in oxygen isotope equilibrium with ocean water. Preliminary experiments suggest that the turnover of sulfate in the sulfur cycle is too rapid to allow equilibrium to be established. If this is so, the sulfur cycle must exert a significant influence on the oxygen balance of the oceanatmosphere system.

Entities:  

Year:  1967        PMID： 17792783     DOI： 10.1126/science.156.3779.1228

Source DB:  PubMed          Journal:  Science        ISSN： 0036-8075            Impact factor:   47.728


  3 in total

1.  Flourishing ocean drives the end-Permian marine mass extinction.

Authors:  Martin Schobben; Alan Stebbins; Abbas Ghaderi; Harald Strauss; Dieter Korn; Christoph Korte
Journal:  Proc Natl Acad Sci U S A       Date:  2015-08-03       Impact factor: 11.205

2.  δ34S and δ18O of dissolved sulfate as biotic tracer of biogeochemical influences on arsenic mobilization in groundwater in the Hetao Plain, Inner Mongolia, China.

Authors:  M D Li; Y X Wang; P Li; Y M Deng; X J Xie
Journal:  Ecotoxicology       Date:  2014-08-23       Impact factor: 2.823

3.  Placing an upper limit on cryptic marine sulphur cycling.

Authors:  D T Johnston; B C Gill; A Masterson; E Beirne; K L Casciotti; A N Knapp; W Berelson
Journal:  Nature       Date:  2014-09-07       Impact factor: 49.962
  3 in total

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