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- W2018649478 abstract "Abstract Palaeontological data from the Permian‐Triassic Bulla section, northern Italy, demonstrate a rapid extinction at this site. This occurs after a negative carbonate carbon‐isotope (δ 13 C carb ) shift, consistent with two other northern Italian sites (Val Badia and Tesero). However, conclusion goes against recent reporting that the extinction occurs before the δ 13 C carb shift. We agree that the shift occurs after the extinction at Jameson Land, east Greenland (a high latitude palaeolocation). However, all other sections show the shift before, or coincident with, the extinction. We suggest that the simplest explanation is a coeval shift in carbonate carbon‐isotope shifts, and it follows that the extinction was not. This suggests that the end‐Permian extinction crept from region to region. It also suggests that the marine extinction occurred first in high northern latitudes." @default.
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- W2018649478 date "2008-07-21" @default.
- W2018649478 modified "2023-09-30" @default.
- W2018649478 title "A carbon-isotopic study of an end-Permian mass-extinction horizon, Bulla, northern Italy: a negative δ<sup>13</sup>C shift prior to the marine extinction" @default.
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- W2018649478 doi "https://doi.org/10.1111/j.1365-3121.2008.00813.x" @default.
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