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

Author:

Faggetter Luke E.,Wignall Paul B.,Pruss Sara B.,Newton Robert J.,Sun Yadong,Crowley Stephen F.

Publisher

Elsevier BV

Subject

Paleontology,Earth-Surface Processes,Ecology, Evolution, Behavior and Systematics,Oceanography

Reference65 articles.

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2. Lateral continuity of facies and parasequences in Middle Cambrian platform carbonates, Carrara Formation, southeastern California, USA;Adams;J. Sediment. Res.,1996

3. Calculation of simultaneous isotopic and trace element variations during water-rock interaction with applications to carbonate diagenesis;Banner;Geochim. Cosmochim. Acta,1990

4. On the causes of mass extinctions;Bond;Palaeogeogr. Palaeoclimatol. Palaeoecol.,2017

5. Construction of tectonic subsidence curves for the early Paleozoic miogeocline, southern Canadian Rocky Mountains: implications for subsidence mechanisms, age of breakup, and crustal thinning;Bond;Geol. Soc. Am. Bull.,1984

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