Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
4749755 | Palaeoworld | 2013 | 22 Pages |
Abstract
The isotopic age of the Little Port Complex is reported to be of the Middle Cambrian [508 and 505 (â2+3) Ma]. According to a previous radiolarian study on the red chert of the Complex, the fauna was assigned to the basal Tremadoc based on co-occurring conodonts. However, a recently recovered index fossil conodont from the Complex, Oepikodus evae, indicates that the fauna belongs to the O. evae conodont zone. The common three dominant species, as mentioned above, which make up more than 95% of the total individuals in the Little Port Complex and the strata assigned to O. evae conodont zone and Pendeograptus fruticosus graptolite zone of the Cow Head Group suggest that the two faunas are coeval in the lower Arenig.
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Physical Sciences and Engineering
Earth and Planetary Sciences
Palaeontology
Authors
Mun-Zu Won, William J. Iams,