Zobrazeno 1 - 10
of 265
pro vyhledávání: '"Gerta Keller"'
Autor:
Ulrich Heimhofer, Nina Wucherpfennig, Thierry Adatte, Stefan Schouten, Elke Schneebeli-Hermann, Silvia Gardin, Gerta Keller, Sarah Kentsch, Ariane Kujau
Publikováno v:
Nature Communications, Vol 9, Iss 1, Pp 1-8 (2018)
The Cretaceous Oceanic Anoxic Event 2 represents one of the warmest episodes in the last 250 million years. Here, the authors present spore-pollen data and temperature estimates (TEX86) across an expanded stratigraphic section illustrating the dynami
Externí odkaz:
https://doaj.org/article/9efac2e5ce8a4374bd1a057b40a0e0dc
The extensively studied Cretaceous-Palaeogene (K-Pg) boundary mass extinction of planktic foraminifera (~66 Ma) has been linked with two catastrophic triggers: the Chicxulub impact (Gulf of Mexico) and Deccan volcanism (India). All the studies of the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6e4c5d1175438c1a4b4e5c7a18346f4b
https://doi.org/10.5194/egusphere-egu23-14240
https://doi.org/10.5194/egusphere-egu23-14240
Major volcanic eruptions like the Deccan have long been invoked as causes of global mass extinctions. Deccan volcanism erupted ~ 600,000 km3 over the span of ~ 700 ka contemporaneously with the end-Cretaceous mass extinction. It has been difficult to
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d9a5e8eb043023845ec7b81eaac7688e
https://doi.org/10.5194/egusphere-egu23-16993
https://doi.org/10.5194/egusphere-egu23-16993
Autor:
Thierry Adatte, Marcel Regelous, Hassan Khozyem, Jorge E. Spangenberg, Gerta Keller, Uygar Karabeyoglu, Blair Schoene, Syed F.R. Khadri
Mercury (Hg) and more recently tellurium (Te) are indicator of large-scale volcanism in marine sediments and provide new insights into relative timing between biological and environmental changes, mass extinctions and delayed recovery. Several studie
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8f293f1180cab835f653cc6e43ac0449
https://doi.org/10.5194/egusphere-egu23-11057
https://doi.org/10.5194/egusphere-egu23-11057
Discovery of impact glass in deep water at El Penon, NE Mexico, revealed a 2m thick impact spherule deposit during excavation of an 8m thick late Maastrichtian sequence [1]. The impact spherules are pristine and undisturbed in the late Maastrichtian.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d7b117037bbae4d52704a1f53686e4e6
https://doi.org/10.5194/egusphere-egu23-17344
https://doi.org/10.5194/egusphere-egu23-17344
Large Igneous Provinces (LIPs) have been widely studied over the past decades due to their likely link to mass extinction events. Previous work involving U-Pb zircon dating of the Deccan lava flows indicates that the main phase-2 began 250 Ka before
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cdd63c05d8d7ed8cc5e80a8bf4c09388
https://doi.org/10.31223/x50t0p
https://doi.org/10.31223/x50t0p
Publikováno v:
The Phanerozoic Geology and Natural Resources of Egypt ISBN: 9783030956363
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9992e4644aad50f01579506ada50cd2d
https://doi.org/10.1007/978-3-030-95637-0_12
https://doi.org/10.1007/978-3-030-95637-0_12
Autor:
Paula Mateo, Jorge E. Spangenberg, Maya Chaudhary, Madan L. Nagori, Gerta Keller, Thierry Adatte, B. C. Jaiprakash, A. Nallapa Reddy
Publikováno v:
Gondwana Research. 94:73-86
We report the Narmada Seaway began in India during the largest global sea-level transgression and Oceanic Anoxic Event 2 (OAE2) δ13C excursion during the late Cenomanian to early Turonian. The transgression progressed eastward during the Turonian-Co
Massive volcanic eruptions of the Deccan coincided with the end-Cretaceous mass extinction. Precisely dating when the most intense eruptions occurred is challenging because the resolution of geochronological techniques does not yet resolve events sho
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::33870e53e2ccc83afa9e72bf5624afbf
https://doi.org/10.5194/egusphere-egu22-6736
https://doi.org/10.5194/egusphere-egu22-6736