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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 | 122 |
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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 | 1 | 3 | 3 | 0 | 12 | 1 |
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SCOPUS1342937X-2015-28-2-SID84936933679-p1.pdf | 17 |
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