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Carbon isotope fractionation during decomposition of organic matter in soils and paleosols: Implications for paleoecological interpretations of paleosols

✍ Scribed by Jonathan G. Wynn


Book ID
116819525
Publisher
Elsevier Science
Year
2007
Tongue
English
Weight
503 KB
Volume
251
Category
Article
ISSN
0031-0182

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Carbon isotopic fractionations in plant materials and those occurring during decomposition have direct implications in studies of short-and longer-term soil organic matter dynamics. Thus the products of decomposition, the evolved CO 2 and the newly formed soil organic matter, may vary in their 13 C