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Discovery of shallow-marine biofacies conodonts in a bioherm within the Carboniferous-Permian transition in the Omolon Massif, NE Russia near the North paleo-pole: Correlation with a warming spike in the southern hemisphere | 100 |
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Discovery of shallow-marine biofacies conodonts in a bioherm within the Carboniferous-Permian transition in the Omolon Massif, NE Russia near the North paleo-pole: Correlation with a warming spike in the southern hemisphere | 0 | 0 | 5 | 5 | 2 | 0 | 0 |
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