Trilobite extinctions, facies changes and the ROECE carbon isotope excursion at the Cambrian Series 2 - 3 boundary, Great Basin, western USA

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Faggetter, LE; Wignall, PB; Pruss, SB; Newton, RJ; Sun, YD; Crowley, SF;
(2017)
  • Publisher: Elsevier

The mass extinction of the olenellid trilobites occurred around the Cambrian Series 2 - Series 3 boundary. Like many other crises, it coincided with a negative carbon isotope excursion but the associated palaeoenvironmental changes remain unclear. To investigate the cau... View more
  • References (49)
    49 references, page 1 of 5

    Adams, R.D., Grotzinger, J. P. (1996). Lateral continuity of facies and parasequences in Middle Cambrian platform carbonates, Carrara Formation, southeastern California, USA. Journal of Sedimentary Resesearch, 66(6), 1079-1090.

    Banner, J.L., Hanson, G. N. (1990). Calculation of simultaneous isotopic and trace element variations during water-rock interaction with applications to carbonate diagenesis. Geochim. Cosmo. Acta 54(11), 3123-3137.

    Bond, D.P.G., Grasby, S.E. (2016). On the causes of mass extinctions. Palaeogeography, Palaeoclimatology, Palaeoecology. (In this issue).

    Bond, D.P.G, Wignall, P.B. (2010). Pyrite framboid study of marine Permian-Triassic boundary sections: a complex anoxic event and its relationship to contemporaneous mass extinction. Geological Society of America Bulletin, 122(7-8), 1265-1279.

    Bond, G. C., and Kominz, M. A. (1984). Construction of tectonic subsidence curves for the early Paleozoic miogeocline, southern Canadian Rocky Mountains: Implications for subsidence mechanisms, age of breakup, and crustal thinning. Geological Society of America Bulletin, 95(2), 155-173.

    Boucot, A. J. (1990). Phanerozoic extinctions: How similar are they to each other? In Extinction Events in Earth History (pp. 5-30). Springer Berlin Heidelberg.

    Brand, U., Veizer, J. (1981). Chemical diagenesis of a multicomponent carbonate system-2: stable isotopes. Journal of Sedimentary Petrology, 51(3), 987-997.

    Cochran, J. K., Kallenberg, K., Landman, N. H., Harries, P. J., Weinreb, D., Turekian, K. K., Cobban, W. A. (2010). Effect of diagenesis on the Sr, O, and C isotope composition of late Cretaceous mollusks from the Western Interior Seaway of North America. American Journal of Science, 310(2), 69-88.

    Cornwall, H. R., Kleinhampl, F. J. (1961). Geology of the Bare Mountain Quadrangle, Nevada. USGS Report No. 157.

    Corsetti, F. A., and Hagadorn, J. W. (2000). Precambrian-Cambrian transition: Death Valley, United States. Geology, 28(4), 299-302.

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