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While it is tempting to use all available geochronological data in compilations irrespective of decay scheme and precision, caution is urged. B., 2004, U-Pb zircon age constraints on late Neoproterozoic glaciation in Tasmania: Geology, v. The ID-TIMS approach can yield single grain U-Pb dates with a precision of better than about 0.1 percent; however, it is a time consuming and expensive approach.

Correlation of its distinctive cap sequence coupled with high–precision U-Pb (zircon) ages from Namibia (within the glacial Ghaub Formation) and Southern China (within the cap carbonate to the Nantuo tillite) indicate synchronous termination of the Marinoan glaciation at about 635 Ma (See photo). D., 2003, High-precision U-Pb zircon geochronology and the stratigraphic record: Zircon, v. M., and Selby, D., 2004, Constraints on the timing of Marinoan "Snowball Earth" glaciation by Re-187-Os-187 dating of a Neoproterozoic, post-glacial black shale in Western Canada: Earth And Planetary Science Letters, v. L., 2000, Age of Neoproterozoic bilatarian body and trace fossils, White Sea, Russia: Implications for metazoan evolution: Science, v. U-Pb zircon age from the base of the Ediacaran Doushantuo Formation in the Yangtze Gorges, South China: constraint on the age of Marinoan glaciation. During the Ediacaran Period the short-lived Gaskiers glaciation occurred about at 582 Ma and the oldest known Ediacaran fossils first appear within 4 Ma of deglaciation. H., Telouk, P., Frei, R., and Baker, J., 2002, New Lu-Hf and Pb-Pb age constraints on the earliest animal fossils: Earth And Planetary Science Letters, v. When all well-dated sequences containing Ediacaran fossils are considered in the context of global chemostratigraphic correlation schemes, a number of major conclusions can be drawn.

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