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pro vyhledávání: '"Aris Lempotesis-Davies"'
Autor:
Lauren K. O’Connor, Emily Dearing Crampton-Flood, Rhodri M. Jerrett, Gregory D. Price, B. David A. Naafs, Richard D. Pancost, Paul McCormack, Aris Lempotesis-Davies, Bart E. van Dongen, Sabine K. Lengger
Publikováno v:
Geology. 51:486-490
The Cretaceous-Paleogene (K-Pg) boundary marks one of the five major mass extinctions of the Phanerozoic. The ways in which the climate system responded to a bolide impact and extensive volcanism at this time over different time scales are highly deb
Autor:
Lauren O'Connor, Emily Crampton-Flood, Rhodri Jerrett, Gregory Price, B. David A. Naafs, Richard Pancost, Paul McCormack, Aris Lempotesis-Davies, Bart van Dongen, Sabine Lengger
The Cretaceous-Paleogene (K-Pg) boundary marks one of the five major mass extinctions of the Phanerozoic. How the climate system responded to a bolide impact and extensive volcanism at this time over different timescales is highly debated. Here we us
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d565190815828957bf7546bbe7dd62cc
https://doi.org/10.31223/x5qh2v
https://doi.org/10.31223/x5qh2v
Autor:
David Naafs, Rhodri M. Jerrett, Bart E. van Dongen, Richard D. Pancost, Paul McCormack, Aris Lempotesis-Davies, Gregory D. Price, Emily Dearing Crampton-Flood, Sabine K. Lengger
The Cretaceous-Paleogene (K-Pg) boundary marks one of the five major mass extinctions of the Phanerozoic. A bolide impact and flood basalt volcanism compete as triggers for the extinction, but their relative roles remain contentious. This is in part
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::94320acb335592bb4cf9fefc9d92831b
https://doi.org/10.5194/egusphere-egu21-12647
https://doi.org/10.5194/egusphere-egu21-12647