U-Pb Ages from the Neoproterozoic Doushantuo Formation, China

By D. Condon, Maoyan Zhu, S. Bowring, Wei Wang, A. Yang, Yu-gan Jin. Science, 2005

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View Paper: https://www.semanticscholar.org/paper/88bdc9d5e020f5fcf1972ba3d64d47f9bdf5a96c

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Citations in the corpus

FOSSIL CALIBRATIONS FOR THE ARTHROPOD TREE OF LIFE (2016, background): “None of these Lagerstatten, least of all the Lantian, preserves anything that could possibly be interpreted as even a total group eumetazoan and on this basis we define our soft maximum constraint at 635.5 Ma ± 0.6 Myr (Condon et al., 2005) and, thus, 636.1 Ma.”
Tempo and mode of early animal evolution: inferences from rocks, Hox, and molecular clocks (2005, background): “…whether the Gaskiers and related units in the Avalonian-Cadomian volcanic arc (Thompson and Bowring 2000) correlate with the Marinoan ice age, or if they instead represent a younger glaciation of merely regional extent (see Myrow and Kaufman 1999; Evans 2000; Xiao et al. 2004; Condon et al. 2005).”
The case for a Neoproterozoic Oxygenation Event: Geochemical evidence and biological consequences (2011, background): “If the Shuram-Wonoka δ13C anomaly represents the exhaustion of this pool, its culmination, at ca. 551 Ma (Condon et al., 2005), could correspond to a rise in atmospheric oxygen just before the late Ediacaran– Cambrian emergence of modern animal phyla.”
Poriferan paraphyly and its implications for Precambrian palaeobiology (2007, background): “Chemostratigraphic correlations with other sections worldwide suggest that the Shuram event likely occurred prior to 551 Ma (Condon et al. 2005), while detrital zircons from Oman date it younger than 610 Ma (Le Guerroue et al. 2006a).”
Pulsed oxidation and biological evolution in the Ediacaran Doushantuo Formation (2008, background): “Second, the remarkably stable 13Corg values decoupled from variable 13Ccarb values in Doushantuo member II, representing 50 million years if EN2 is of Gaskiers age (11) or 30 million years if we accept the 599 4 Ma age from the upper Doushantuo (33), is strong evidence for a large, isotopically buff”
Birth and early evolution of metazoans (2014, background): “Since the landmark work by Bowring et al. (1993), a large number of respectable ages have been added also in South China (e.g. Condon et al., 2005; P. Liu et al., 2009; Xiao and Laflamme, 2009; Sawaki et al., 2010; Liu et al., 2013; Zhu et al., 2013; Tahata et al., 2013; Okada et al., 2014-in this…”
The Laurentian record of Neoproterozoic glaciation, tectonism, and eukaryotic evolution in Death Valley, California (2013, background): “…(ca. 717–662 Ma; Bowring et al., 2007; Macdonald et al., 2010b; Zhou et al., 2004) glacial deposits and late Cryogenian “Marinoan” (ca. 635 Ma; Condon et al., 2005; Hoffmann et al., 2004) glacial deposits are present in the Kingston Peak Formation on the west side of Death Valley, in the…”