The early Mesozoic radiation of dinoflagellates

Dinoflagellates are a major component of the marine microplankton and, from fossil evidence, appear to have been so for the past 200 million years. In contrast, the pre-Triassic record contains only equivocal occurrences of dinoflagellates, despite the fact that comparative ultrastructural and molec...

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Veröffentlicht in:Paleobiology 1996, Vol.22 (3), p.329-338
Hauptverfasser: Fensome, R. A., MacRae, R. A., Moldowan, J. M., Taylor, F. J. R., Williams, G. L.
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Sprache:eng
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Zusammenfassung:Dinoflagellates are a major component of the marine microplankton and, from fossil evidence, appear to have been so for the past 200 million years. In contrast, the pre-Triassic record contains only equivocal occurrences of dinoflagellates, despite the fact that comparative ultrastructural and molecular phylogenetic evidence indicates a Precambrian origin for the lineage. Thus, it has often been assumed that the dearth of Paleozoic fossil dinoflagellates was due to a lack of preservation or recognition and that the relatively sudden appearance of dinoflagellates in the Mesozoic is an artifact of the record. However, new evidence from a detailed analysis of the fossil record and from the biogeochemical record indicates that dinoflagellates did indeed undergo a major evolutionary radiation in the early Mesozoic.
ISSN:0094-8373
1938-5331
DOI:10.1017/S0094837300016316