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U-Pb sensitive high-resolution ion microprobe ages from the Doushantuo Formation in south China: Constraints on late Neoproterozoic glaciations

¹ School of Earth Sciences and Resources, China University of Geosciences, Beijing 100083, China, and Beijing SHRIMP Center, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China
² Department of Geoscience, University of Nevada, Las Vegas, Nevada 89154, USA
³ Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China
⁴ Beijing SHRIMP Center, Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China
⁵ Department of Earth Sciences, University of California, Riverside, California 92521, USA
⁶ Lamont-Doherty Earth Observatory of Columbia University, Palisades, New York 10964, USA

Two distinctive volcanic ash beds were found in the terminal Proterozoic Doushantuo Formation in south China. The lower ash bed, 2.5 m above the cap carbonate at the base of the Doushantuo, yields a U-Pb zircon age of 621 ± 7 Ma, providing the closest upper limit for a correlative of the Marinoan glaciation. The upper ash bed, near the Doushantuo-Dengying boundary, yields a U-Pb zircon age of 555.2 ± 6.1 Ma, providing for the first time a direct age determination for a prominent negative ¹³C excursion (–5) above the Marinoan glacial level. This excursion, if interpreted to be of glacial origin, is much younger than the Gaskiers Formation (ca. 580 Ma) in Newfoundland, and perhaps the fifth or sixth such level in the Neoproterozoic. That interpretation, however, is not supported by the proliferation of organisms within strata encompassing the negative ¹³C excursion in south China and globally, by the lack of a ca. 555 Ma glacial record, and by the absence of stratigraphic evidence for sea-level change. The data call for alternative paleoceanographic models for the origin of Neoproterozoic ¹³C excursions not clearly related to glaciation.

Key Words: U-Pb • SHRIMP geochronology • Neoproterozoic glaciation • cap carbonates • south China

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