U-Pb geochronology and global context of the Charnian Supergroup, UK: Constraints on the age of key Ediacaran fossil assemblages

Author:

Noble Stephen R.,Condon Daniel J.,Carney John N.,Wilby Philip R.,Pharaoh Timothy C.,Ford Trevor D.

Publisher

Geological Society of America

Subject

Geology

Reference101 articles.

1. Growth and Ecology of a Multi-branched Ediacaran Rangeomorph from the Mistaken Point Assemblage, Newfoundland

2. Benus A.P. , 1988, Sedimentological context of a deep-water Ediacaran fauna (Mistaken Point, Avalon zone, eastern Newfoundland), in Landing E. Narbonne G.M. Myrow P. , eds., Trace Fossils, Small Shelly Fossils and the Precambrian-Cambrian Boundary: New York State Museum and Geological Survey Bulletin 463, p. 8–9.

3. Bland B.H. Goldring R. , 1995, Teichichnus Seilacher 1955 and other trace fossils (Cambrian?) from the Charnian of central England: Neues Jahrbuch für Geologie und Palaeontologie, v. 195, p. 5–23.

4. Bowring S. Myrow P. Landing E. Ramezani J. , 2003, Geochronological constraints on terminal Neoproterozoic events and the rise of metazoans: Geophysical Research Abstracts, v. 5, no. 13, p. 219.

5. Boynton H.E. , 1978, Fossils from the Precambrian of Charnwood Forest, Leicestershire: Mercian Geologist, v. 6, p. 291–296.

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