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climate ch... [1]
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Palynological evidence for prolonged cooling along the Tunisian continental shelf following the K-Pg boundary impact [期刊论文]
Palaeogeography, Palaeoclimatology, Palaeoecology, 2015-01-01, 426
Vellekoop J.;  Smit J.;  van de Schootbrugge B.;  Weijers J.W.H.;  Galeotti S.;  Sinninghe Damsté J.S.;  Brinkhuis H.
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