Did Cooling Oceans Trigger Ordovician Biodiversification? Evidence from Conodont Thermometry

By J. Trotter, I. Williams, C. Barnes, C. Lécuyer, R. Nicoll. Science, 2008

653 citations recorded by the source corpus.

Subfields: Ecology, Geochemistry and Petrology, Paleontology

View Paper: https://www.semanticscholar.org/paper/7ce0483ddec0a935f376d2aee94b29def459a5d7

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In Paleontology

1. G. Shields-Zhou
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Citations in the corpus

• The case for a Neoproterozoic Oxygenation Event: Geochemical evidence and biological consequences (2011, background): “However, any irreversible change in weathering rates will lead to global cooling unless compensated for by higher outgassing and an accelerated global carbon cycle, which may explain why Gondwanan orogenesis, characterized presumably by exceedingly high erosion rates, enhanced marine productivity an”
• A review of the evolution, biostratigraphy, provincialism and diversity of Middle and early Late Triassic conodonts (2016, background): “…of host rocks; oxygen stable isotopes in conodont apatite are an indicator of prevailing oceanic temperature (Joachimski and Buggish 2003; Trotter et al. 2008; Sun et al. 2012; Romano et al. 2013); size may be a parameter for environmental stress (Chen et al. 2013); and latitudinal…”