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Modelling δ13C and δ18O in the solution layer on stalagmite surfaces

✍ Scribed by Denis Scholz; Christian Mühlinghaus; Augusto Mangini

Book ID
116503867
Publisher
Elsevier Science
Year
2009
Tongue
English
Weight
689 KB
Volume
73
Category
Article
ISSN
0016-7037

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**Abstract** Positive shifts in global seawater δ^13^C~DIC~ are related to changes in the ratio of organic relative to inorganic carbon burial in oceanic basins, whereas factors such as climatic cooling and the accumulation of polar ice are known to cause positive shifts in δ^18^O. Here, an alternat