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Trace elements, stable isotopes, and clay mineralogy of the Elles II K–T boundary section in Tunisia: indications for sea level fluctuations and primary productivity

Stüben, D, Kramar, U, Berner, Z, Stinnesbeck, W, Keller, G, Adatte, T·2002·Palaeogeography, Palaeoclimatology, Palaeoecology
DOI 10.1016/s0031-0182(01)00401-1
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    “…foraminifera is believed to accurately record N18O variations of the ambient seawater and hence variations of temperature, based on the assumption that planktic foraminifera build their tests in isotopic equilibrium with ambient seawater (Epstein et al., 1953; Shackelton, 1967; Erez and Luz, 1992).”
    Background

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Metadata

Authors
Stüben, D., Kramar, U., Berner, Z., Stinnesbeck, W., Keller, G., & Adatte, T.
Venue
Palaeogeography, Palaeoclimatology, Palaeoecology
Publisher
Elsevier BV
Published
2002-02
Volume
178
Issue
3-4
Pages
321-345
ISSN
0031-0182
DOI
10.1016/s0031-0182(01)00401-1
Cited by
63
References
1
Language
en
Licence
www.elsevier.com/tdm/userlicense/1.0/ (tdm)

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