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Geology; June 2004; v. 32; no. 6; p. 529-532; DOI: 10.1130/G20439.1
© 2004 Geological Society of America
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Records of post–Cretaceous-Tertiary boundary millennial-scale cooling from the western Tethys: A smoking gun for the impact-winter hypothesis?

Simone Galeotti1, Henk Brinkhuis2 and Matthew Huber3

1 Istituto di Geologia and Centro di Geobiologia–Università di Urbino, Località Crocicchia, 61029 Urbino, Italy
2 Laboratory of Palaeobotany and Palynology, Utrecht University, Budapestlaan 4, 3584 CD Utrecht, Netherlands
3 Earth and Atmospheric Sciences Department, Purdue University, 1397 Civil Engineering Building, West Lafayette, Indiana 47906, USA

The record of both dinoflagellate cysts and benthic foraminifera across the Cretaceous-Tertiary boundary at El Kef, Tunisia, reveals a brief expansion of the Boreal bioprovince into the western Tethys, suggesting that an ~2 k.y. cooling occurred during the earliest Danian. We show that this prolonged cooling phase is consistent with the oceanographic response to an impact winter.

Key Words: K-T boundary • foraminifera • dinoflagellates • extraterrestrial impact • cooling




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