Zobrazeno 1 - 4
of 4
pro vyhledávání: '"L. J. LeVay"'
Autor:
E. J. Screaton, M. E. Torres, B. Dugan, K. U. Heeschen, J. J. Mountjoy, C. Ayres, P. S. Rose, I. A. Pecher, P. M. Barnes, L. J. LeVay
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 21, Iss 6, Pp n/a-n/a (2020)
Abstract Screaton et al. (2019, https://doi.org/10.1029/2019GC008603) examined the role of sedimentation, sea level, and bottom water temperature (BWT) changes due to glaciation as drivers for the downward migration of the base of gas hydrate stabili
Externí odkaz:
https://doaj.org/article/94b49a0fd03045fb988381b97cc921f0
Autor:
A. Sluijs, L. van Roij, G. J. Harrington, S. Schouten, J. A. Sessa, L. J. LeVay, G.-J. Reichart, C. P. Slomp
Publikováno v:
Climate of the Past, Vol 10, Iss 4, Pp 1421-1439 (2014)
The Paleocene–Eocene Thermal Maximum (PETM, ~ 56 Ma) was a ~ 200 kyr episode of global warming, associated with massive injections of 13C-depleted carbon into the ocean–atmosphere system. Although climate change during the PETM is relatively well
Externí odkaz:
https://doaj.org/article/bfcbf45135334b30b29e398f0b9dd1a0
Autor:
Caroline P. Slomp, Appy Sluijs, Jocelyn A. Sessa, L. J. LeVay, Stefan Schouten, Gert-Jan Reichart, L. van Roij, Guy J. Harrington
The Paleocene/Eocene Thermal Maximum (PETM, ~56 Ma) was a ~200 kyr episode of global warming, associated with massive injections of 13C-depleted carbon into the ocean-atmosphere system. Although climate change during the PETM is relatively well const
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0963f7d697c5831e777ae4bac63cfba2
https://doi.org/10.5194/cpd-9-6459-2013
https://doi.org/10.5194/cpd-9-6459-2013
