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Extinction patterns, δ18 O trends, and magnetostratigraphy from a southern high-latitude Cretaceous–Paleogene section: Links with Deccan volcanism
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“We find evidence of climate change at the onset of Deccan volcanism and again at the KPB that align with two previously identified pulses of extinction10, indicating the complete end-Cretaceous extinction at this site is due to the combined effects of the volcanic and meteorite kill mechanisms.”
From End-Cretaceous extinction in Antarctica linked to both Deccan volcanism and meteorite impact via climate change (2016) · cites this paper as [10]
In the citing paper
“Species extinction at Seymour Island occurred in two statistically distinguishable pulses10, one at the KPg boundary and another one 40 m below, calculated to be at 66.23 Ma in this age model (Fig. 1a).”
From End-Cretaceous extinction in Antarctica linked to both Deccan volcanism and meteorite impact via climate change (2016) · cites this paper as [10]
Citations
Cites
Equilibrium and nonequilibrium oxygen isotope effects in synthetic carbonates
Kim, S.-T., & O'Neil, J. R. (1997) · Geochimica et Cosmochimica Acta · doi:10.1016/s0016-7037(97)00169-5 · Cited by 2,558 · cited 2×
“Paleotemperature estimates were made following the procedures of Kim et al. (2007b) and Kim and O'Neil (1997) for aragonite and calcite respectively.”
BackgroundMethodAn Overview of Biomineralization Processes and the Problem of the Vital Effect
Weiner, S. (2003) · Reviews in Mineralogy and Geochemistry · doi:10.2113/0540001 · Cited by 1,022
Kim, S.-T., O’Neil, J. R., Hillaire-Marcel, C., & Mucci, A. (2007) · Geochimica et Cosmochimica Acta · doi:10.1016/j.gca.2007.04.019 · Cited by 532 · cited 3×
“Paleotemperature estimates were made following the procedures of Kim et al. (2007b) and Kim and O'Neil (1997) for aragonite and calcite respectively.”
BackgroundMethodPhosphoric acid fractionation factors for calcite and aragonite between 25 and 75 °C: Revisited
Kim, S.-T., Mucci, A., & Taylor, B. E. (2007) · Chemical Geology · doi:10.1016/j.chemgeo.2007.08.005 · Cited by 374 · cited 3×
“Paleotemperature estimates were made following the procedures of Kim et al. (2007b) and Kim and O'Neil (1997) for aragonite and calcite respectively.”
BackgroundMethod
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Cited by
The eruptive tempo of Deccan volcanism in relation to the Cretaceous-Paleogene boundary
Sprain, C. J., Renne, P. R., Vanderkluysen, L., Pande, K., Self, S., & Mittal, T. (2019) · Science · doi:10.1126/science.aav1446 · Cited by 395
Petersen, S. V., Dutton, A., & Lohmann, K. C. (2016) · Nature Communications · doi:10.1038/ncomms12079 · Cited by 210
Sprain, C. J., Renne, P. R., Wilson, G. P., & Clemens, W. A. (2015) · Geological Society of America Bulletin · doi:10.1130/b31076.1 · Cited by 103
Metadata
- Authors
- Tobin, T. S., Ward, P. D., Steig, E. J., Olivero, E. B., Hilburn, I. A., Mitchell, R. N., Diamond, M. R., Raub, T. D., & Kirschvink, J. L.
- Venue
- Palaeogeography, Palaeoclimatology, Palaeoecology
- Publisher
- Elsevier BV
- Published
- 2012-09
- Volume
- 350-352
- Pages
- 180-188
- ISSN
- 0031-0182
- Cited by
- 108
- References
- 4
- Language
- en
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- Tobin, T. S., Ward, P. D., Steig, E. J., Olivero, E. B., Hilburn, I. A., Mitchell, R. N., Diamond, M. R., Raub, T. D., & Kirschvink, J. L. (2012). Extinction patterns, δ18 O trends, and magnetostratigraphy from a southern high-latitude Cretaceous–Paleogene section: Links with Deccan volcanism. Palaeogeography, Palaeoclimatology, Palaeoecology. https://doi.org/10.1016/j.palaeo.2012.06.029