Zobrazeno 1 - 4
of 4
pro vyhledávání: '"F. J. Rodríguez-Tovar"'
Autor:
V. Smith, S. Warny, K. Grice, B. Schaefer, M. T. Whalen, J. Vellekoop, E. Chenot, S. P. S. Gulick, I. Arenillas, J. A. Arz, T. Bauersachs, T. Bralower, F. Demory, J. Gattacceca, H. Jones, J. Lofi, C. M. Lowery, J. Morgan, N. B. Nuñez Otaño, J. M. K. O'Keefe, K. O'Malley, F. J. Rodríguez-Tovar, L. Schwark
Publikováno v:
Climate of the Past, Vol 16, Pp 1889-1899 (2020)
Thermal stress on the biosphere during the extreme warmth of the Paleocene–Eocene Thermal Maximum (PETM) was most severe at low latitudes, with sea surface temperatures at some localities exceeding the 35 ∘C at which marine organisms experience
Externí odkaz:
https://doaj.org/article/79129e6f5ea74a49992d7c386eced3ac
Autor:
Bettina Schaefer, Kliti Grice, S. L. Lyons, Si Athena Chen, G. Turner‐Walker, Timothy J. Bralower, Sonia M. Tikoo, Kenneth A. Farley, Cornelia Rasmussen, Christopher M. Lowery, Vivi Vajda, Axel Wittmann, Heather L. Jones, Joshua M. Garber, Elizabeth Hajek, J. L. Gray, Charles S. Cockell, Sean P. S. Gulick, Joanna Morgan, David A. Kring, Katherine H. Freeman, Peter J. Heaney, Marco J. L. Coolen, Natalia Artemieva, J. Carte, Benjamin H. Passey, Michael T. Whalen, James C Zachos, Steven Goderis, F. J. Rodríguez Tovar, Elizabeth C Sibert, Julie Cosmidis, M. Gonzalez, Jan Smit, M. S. Fantle
An expanded sedimentary section provides an opportunity to elucidate conditions in the nascent Chicxulub crater during the hours to millennia after the Cretaceous‐Paleogene (K‐Pg) boundary impact. The sediments were deposited by tsunami followed
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7cd6a27abdda4555cb268e7de6cbbc3f
https://resolver.caltech.edu/CaltechAUTHORS:20201125-070002260
https://resolver.caltech.edu/CaltechAUTHORS:20201125-070002260
Publikováno v:
Geobiology. 7:533-543
Biotic recovery after the Cretaceous-Palaeogene (K-Pg) impact is one unsolved question concerning this mass extinction event. To evaluate the incidence of the K-Pg event on biota, and the subsequent recovery, a recent environmental disaster has been
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::03e5fd1dd6004f5f5c6d505d8e366cb0
https://doi.org/10.1111/j.1472-4669.2009.00213.x
https://doi.org/10.1111/j.1472-4669.2009.00213.x
Autor:
T. J. Bralower, J. Cosmidis, M. S. Fantle, C. M. Lowery, B. H. Passey, S. P. S. Gulick, J. V. Morgan, V. Vajda, M. T. Whalen, A. Wittmann, N. Artemieva, K. Farley, S. Goderis, E. Hajek, P. J. Heaney, D. A. Kring, S. L. Lyons, C. Rasmussen, E. Sibert, F. J. Rodríguez Tovar, G. Turner‐Walker, J. C. Zachos, J. Carte, S. A. Chen, C. Cockell, M. Coolen, K. H. Freeman, J. Garber, M. Gonzalez, J. L. Gray, K. Grice, H. L. Jones, B. Schaefer, J. Smit, S. M. Tikoo
Publikováno v:
AGU Advances, Vol 1, Iss 4, Pp n/a-n/a (2020)
Abstract An expanded sedimentary section provides an opportunity to elucidate conditions in the nascent Chicxulub crater during the hours to millennia after the Cretaceous‐Paleogene (K‐Pg) boundary impact. The sediments were deposited by tsunami
Externí odkaz:
https://doaj.org/article/e259b8506e96472ea80398ad2d61c1c2