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Volumn 280, Issue 5371, 1998, Pages 1922-1925

Post-cambrian trilobite diversity and evolutionary Faunas

Author keywords

[No Author keywords available]

Indexed keywords

ORDOVICIAN; TRILOBITE;

EID: 0032546820     PISSN: 00368075     EISSN: None     Source Type: Journal    
DOI: 10.1126/science.280.5371.1922     Document Type: Article
Times cited : (100)

References (44)
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    • note
    • The full database will be published elsewhere; a current version is available from the senior author on request.
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    • note
    • We used North American Ordovician series, but the globally correlative Nemograptus gracilis Zone is included in the Mohawk, instead of its traditional assignment to the upper Whiterock. This revision is based on the recent recommendations of the Sub-commission on Ordovician Stratigraphy and results in more satisfactory sampling intervals. At the series level of resolution, there are few examples of Lazarus taxa (taxa occurring earlier and later than, but not within, a given sampling interval); where such sampling gaps occurred, genera were scored as present.
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    • note
    • Principal components analysis of the data set confirmed the division into two major faunas. The groupings are so robust that the use of alternative similarity indices will not significantly alter the result.
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    • note
    • A single family, Harpetidae, falls outside the two major clusters. The generic taxonomy of this group is in need of revision.
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    • note
    • We define the Silurian Fauna as Whiterock Fauna families in which at least one lineage survived the end-Ordovician extinction and subsequently diversified, thus excluding two minor relict distributions, Pterygometopidae and Raphiophoridae, in each of which a single low-diversity lineage extended into the Silurian but became extinct during the period.
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    • note
    • We thank G. D. Edgecombe, J. J. Sepkoski Jr., and A. B. Smith for comments on the manuscript. Preparation of this study was funded by Natural Environment Research Council (UK) grant GR3/09654 and by Natural Sciences and Engineering Research Council (Canada) grant 41197.


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