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Variability in the δ13C of lower Palaeozoic palynomorphs: implications for the interpretation of ancient marine sediments

✍ Scribed by Christophe Lécuyer; Florentin Paris


Book ID
117073443
Publisher
Elsevier Science
Year
1997
Tongue
English
Weight
435 KB
Volume
138
Category
Article
ISSN
0009-2541

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The carbon-isotopic composition (y 13 C) of bulk carbonates, obtained from a transect of sites drilled through platform and periplatform sediments of Holocene to Early Miocene age, has been compared to ascertain whether changes in the y 13 C can be correlated between sediments of equivalent ages and