2022
DOI: 10.1016/j.jsames.2022.103730
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Statistic biostratigraphy and paleoecology of tropical Upper Cretaceous dinoflagellate cysts

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Cited by 7 publications
(2 citation statements)
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“…For instance, in geologic time intervals of global climate cooling, warm-loving plankton species have diachronous last occurrences which are progressively later at lower latitudes. A good example is the modern occurrence in the western Pacific warm pool of Dapsilidinium pastielsii, a species that was long thought to be extinct in the Pliocene (Head et al, 1989). This example serves as an indicator that asynchronous biostratigraphic events could actually be the result of paleoceanographic or paleoecologic influences, rather than just biostratigraphic error.…”
mentioning
confidence: 99%
“…For instance, in geologic time intervals of global climate cooling, warm-loving plankton species have diachronous last occurrences which are progressively later at lower latitudes. A good example is the modern occurrence in the western Pacific warm pool of Dapsilidinium pastielsii, a species that was long thought to be extinct in the Pliocene (Head et al, 1989). This example serves as an indicator that asynchronous biostratigraphic events could actually be the result of paleoceanographic or paleoecologic influences, rather than just biostratigraphic error.…”
mentioning
confidence: 99%
“…For instance, in geologic time intervals of global climate cooling, warm-loving plankton species have diachronous last occurrences which are progressively later at lower latitudes. A good example is the modern occurrence in the western Pacific warm pool of Dapsilidinium pastielsii, a species that was long thought to be extinct in the Pliocene (Head et al, 1989). This example serves as an indicator that asynchronous biostratigraphic events could actually be the result of paleoceanographic or paleoecologic influences, rather than just biostratigraphic error.…”
mentioning
confidence: 99%