Palynological evidence for prolonged cooling along the Tunisian continental shelf following the K–Pg boundary impact (Q63971648)

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Palynological evidence for prolonged cooling along the Tunisian continental shelf following the K–Pg boundary impact
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    Palynological evidence for prolonged cooling along the Tunisian continental shelf following the K–Pg boundary impact (English)
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    Jan Smit
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    May 2015
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    426
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    216-228
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