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Autor:
Anna C Mudd, Kira E Murray, Nicholas E. Bader, Kirsten P. Nicolaysen, Ricardo Lopez-Maldonado
Publikováno v:
Geoderma. :195-205
The high-resolution marine isotope climate record indicates pronounced global cooling during the Langhian (16–13.8 Ma), beginning with the warm middle Miocene climatic optimum and ending with significant Antarctic ice sheet expansion and the transi