Deep-water changes: the near-synchronous disappearance of a group of benthic foraminifera from the Late Miocene Mediterranean

Palaeogeography, Palaeoclimatology, Palaeoecology - Tập 152 - Trang 259-281 - 1999
T.J. Kouwenhoven1, M.-S. Seidenkrantz2, G.J. van der Zwaan1,3
1Department of Geology, Utrecht University, P.O. Box 80021, 3508 TA Utrecht, The Netherlands
2Department of Earth Sciences, University of Aarhus, C.F. Møllers Allé, DK-8000 Århus-C, Denmark
3Department of Biogeology, University of Nijmegen, Toernooiveld 1, 6525 ED Nijmegen, The Netherlands

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