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X. Crosta

2022

How does the Southern Ocean palaeoenvironment during Marine Isotope Stage 5e compare to the modern?
M. Chadwick, C. Allen, L.C. Sime, X. Crosta, C.-D. Hillenbrand
Marine Micropaleontology 170

2009

Constraints on the magnitude and patterns of ocean cooling at the Last Glacial Maximum
Claire Waelbroeck, A Paul, Michal Kucera, Rosell-Mel\ e, M Weinelt, R Schneider, A. Mix, A Abelmann, L. Armand, E. Bard, S. Barker, T.T. Barrows, H. Benway, I. Cacho, M.-T. Chen, Ian Croudace, X. Crosta, A. de Vernal, T. Dokken, J. Duprat, H. Elderfield, F. Eynaud, R. Gersonde, A. Hayes, M. Henry, C. Hillaire-Marcel, C.-C. Huang, E. Jansen, S. Juggins, N. Kallel, T. Kiefer, M. Kienast, L. Labeyrie, H. Leclaire, L. Londeix, S. Mangin, J. Matthiessen, F. Marret, M. Meland, A.E. Morey, S. Mulitza, U. Pflaumann, N.G. Pisias, T. Radi, A. Rochon, Eelco Rohling, L. Sbaffi, C. Schäfer-Neth, S. Solignac, H. Spero, K. Tachikawa, J.-L Turon
Nature Geoscience 2

BOSCORF

The British Ocean Sediment Core Research Facility is based at the Southampton site of the National Oceanography Centre and is Britain’s national deep-sea core repository

boscorf@noc.ac.uk

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