Climate of the Past
Climate of the Past
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Articles | Volume 12, issue 2
Articles | Volume 12, issue 2
https://doi.org/10.5194/cp-12-429-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/cp-12-429-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
Articles | Volume 12, issue 2
Research article
 | 
24 Feb 2016
Research article |  | 24 Feb 2016

Late Cretaceous (late Campanian–Maastrichtian) sea-surface temperature record of the Boreal Chalk Sea

Nicolas Thibault, Rikke Harlou, Niels H. Schovsbo, Lars Stemmerik, and Finn Surlyk

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Cited articles

Abramovich, S., Keller, G., Stüben, D., and Berner, Z.: Characterization of late Campanian foraminiferal depth habitats and vital activities based on stable isotopes, Palaeogeogr. Palaeoecol., 202, 1–29, 2003.
Anderson, T. F. and Arthur, M. A.: Stable isotopes of oxygen and carbon and their application to sedimentologic and environmental problems, in: Stable isotopes in sedimentary geology, edited by: Arthur, M. A., Anderson, T. F., Kaplan, I. R., Veizer, J., and Land, L. S., SEPM Short Course Notes, 10, 1–151, 1983.
Barrera, E. and Savin, S. M.: Evolution of late Campanian–Maastrichtian marine climates and oceans, in: Evolution of the Cretaceous ocean-climate system, edited by: Barrera, E. and Johnson, C. C., GSA Special Paper, 332, 245–282, 1999.
Bemis, B. E., Spero, H. J., Bijma, J., and Lea, D. W.: Reevaluation of the oxygen isotopic composition of planktonic foraminifera: Experimental results and revised paleotemperature equations, Paleoceanography, 13, 150–160, 1998.
Billups, K. and Schrag, D. P.: Paleotemperatures and ice volume of the past 27 Myr revisited with paired Mg ∕ Ca and 18O ∕ 16O measurements on benthic foraminifera, Paleoceanography, 17, 1003, https://doi.org/10.1029/2000PA000567, 2002.
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We present here for the first time a very high-resolution record of sea-surface temperature changes in the Boreal Chalk Sea for the last 8 million years of the Cretaceous. This record was obtained from 1932 bulk oxygen isotope measurements, and their interpretation into temperature trends is validated by similar trends observed from changes in phytoplankton assemblages.
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