Carbon Isotope Geochemistry and 14C Ages of Microbial Mats from the Gavish Sabkha and the Solar Lake View Full Text


Ontology type: schema:Chapter     


Chapter Info

DATE

1985

AUTHORS

Manfred Schidlowski , Udo Matzigkeit , W. G. Mook , Wolfgang E. Krumbein

ABSTRACT

Photosynthetic organisms incorporate carbon with a marked though variable bias in favor of the light carbon isotope (12C) which ultimately derives from a kinetic fractionation effect imposed on the principal assimilatory pathways (see Vogel 1980, O’Leary 1981). As a result, average organic matter is enriched by about 20–30‰ in 12C as compared to oceanic bicarbonate and carbonate, the quantitatively most abundant inorganic carbon species in our environment (Schidlowski 1982, 1983). More... »

PAGES

381-401

Book

TITLE

Hypersaline Ecosystems

ISBN

978-3-642-70292-1
978-3-642-70290-7

Identifiers

URI

http://scigraph.springernature.com/pub.10.1007/978-3-642-70290-7_22

DOI

http://dx.doi.org/10.1007/978-3-642-70290-7_22

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1022513477


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