Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
6350094 | Palaeogeography, Palaeoclimatology, Palaeoecology | 2014 | 25 Pages |
Abstract
The depositional cycle containing the studied carbonate deposits represents a warmer phase than the preceding glacially influenced Asselian to early Sakmarian interval and the subsequent cool phase of the “mid” Artinskian that is followed by significant warming during the late Artinskian-early Kungurian. The timing of cooler and warmer intervals in the west Australian basins seems out-of-phase with the eastern Australian succession, but this may be a problem of chronostratigraphic miscorrelation due to endemic faunas and palynofloras.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Earth-Surface Processes
Authors
David W. Haig, Eujay McCartain, Arthur J. Mory, Gilsel Borges, Vladimir I. Davydov, Matthew Dixon, Andrej Ernst, Stefan Groflin, Eckart HÃ¥kansson, Myra Keep, Zelia Dos Santos, G.R. Shi, Jacinto Soares,