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1 Istituto di Geologia and Centro di GeobiologiaUniversità 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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