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Late Maastrichtian paleoclimatic and paleoceanographic changes inferred from Sr/Ca ratio and stable isotopes
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“The Elles section in Tunisia is composed of marls, silty marls, shales, and clay stones deposited in 100- to 150-m paleodepth on the continental shelf of the Tethys seaway (12, 87, 88).”
From Earth orbital rhythms links timing of Deccan trap volcanism phases and global climate change (2025) · cites this paper as [87]
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Keller, G., Mateo, P., Monkenbusch, J., Thibault, N., Punekar, J., Spangenberg, J. E., Abramovich, S., Ashckenazi-Polivoda, S., Schoene, B., Eddy, M. P., et al. (2020) · Global and Planetary Change · doi:10.1016/j.gloplacha.2020.103312 · Cited by 130
Self-citationSprain, C. J., Renne, P. R., Wilson, G. P., & Clemens, W. A. (2015) · Geological Society of America Bulletin · doi:10.1130/b31076.1 · Cited by 103
Earth orbital rhythms links timing of Deccan trap volcanism phases and global climate change
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Metadata
- Authors
- Stüben, D., Kramar, U., Berner, Z. A., Meudt, M., Keller, G., Abramovich, S., Adatte, T., Hambach, U., & Stinnesbeck, W.
- Venue
- Palaeogeography, Palaeoclimatology, Palaeoecology
- Publisher
- Elsevier BV
- Published
- 2003-10
- Volume
- 199
- Issue
- 1-2
- Pages
- 107-127
- ISSN
- 0031-0182
- Cited by
- 37
- References
- 0
- Language
- en
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