Climate- and gateway-driven cooling of Late Eocene to earliest Oligocene sea surface temperatures in the North Sea Basin
Author:
Funder
the Netherlands Earth System Science Center
Det Frie Forskningsråd
Publisher
Springer Science and Business Media LLC
Subject
Multidisciplinary
Link
http://www.nature.com/articles/s41598-019-41013-7.pdf
Reference95 articles.
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2. Galeotti, S. et al. Antarctic Ice Sheet variability across the Eocene-Oligocene boundary climate transition. Science 352, 76–80 (2016).
3. Miller, K. G., Wright, J. D. & Fairbanks, R. G. Unlocking the Ice House: Oligocene-Miocene oxygen isotopes, eustasy, and margin erosion. J. Geophys. Res. Solid Earth 96, 6829–6848 (1991).
4. Miller, K. G. et al. Eocene-Oligocene global climate and sea-level changes: St. Stephens Quarry, Alabama. Bull. Geol. Soc. Am. 120, 34–53 (2008).
5. Zachos, J. C., Quinn, T. M. & Salamy, K. A. High-resolution (104 years) deep-sea foraminiferal stable isotope records of the Eocene-Oligocene climate transition. Paleoceanography 11, 251–266 (1996).
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