Zobrazeno 1 - 10
of 12
pro vyhledávání: '"Victor M. Giraldo-Gómez"'
Autor:
Tomáš Kočí, Mathias Mueller, M. Aleksandra Bitner, Simon Schneider, Manfred Jäger, Gerald Auer, Victor M. Giraldo-Gómez, Andrzej Pisera, John S. Buckeridge, René Hoffmann, Kevin Stevens
Publikováno v:
Geobios. 59:1-28
Marly sediments of the early Messinian Abad Member of the Turre Formation from the northeastern sector of the Carboneras-Nijar Basin (southern Spain) have yielded a rich fossil assemblage, of which 60 taxa are documented herein. Besides nannoflora an
Autor:
G. Gambacorta, Janet Rethemeyer, Victor M. Giraldo-Gómez, Cinzia Bottini, Sebastian Steinig, Alexander Farnsworth, Daniel J. Lunt, Onoriode Esegbue, Elisabetta Erba, Thomas Wagner, Wolf Dummann, Peter Hofmann, Liyenne Cavalheiro, Stefano Torricelli, Sascha Flögel
Publikováno v:
Nature Communications, Vol 12, Iss 1, Pp 1-11 (2021)
Cavalheiro, L, Wagner, T, Steinig, S, Bottini, C, Dummann, W, Esegbue, O, Gambacorta, G, Giraldo-Gómez, V, Farnsworth, A, Flögel, S, Hofmann, P, Lunt, D J, Rethemeyer, J, Torricelli, S & Erba, E 2021, ' Impact of global cooling on Early Cretaceous high pCO 2 world during the Weissert Event ', Nature Communications, vol. 12, no. 1, 5411 . https://doi.org/10.1038/s41467-021-25706-0
Cavalheiro, L, Wagner, T, Steinig, S, Bottini, C, Dummann, W, Esegbue, O, Gambacorta, G, Giraldo-Gómez, V, Farnsworth, A, Flögel, S, Hofmann, P, Lunt, D J, Rethemeyer, J, Torricelli, S & Erba, E 2021, ' Impact of global cooling on Early Cretaceous high pCO 2 world during the Weissert Event ', Nature Communications, vol. 12, no. 1, 5411 . https://doi.org/10.1038/s41467-021-25706-0
The Weissert Event ~133 million years ago marked a profound global cooling that punctuated the Early Cretaceous greenhouse. We present modelling, high-resolution bulk organic carbon isotopes and chronostratigraphically calibrated sea surface temperat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7d4e1cd51a9e965d8c559cf2ed5adcee
http://publikationen.ub.uni-frankfurt.de/files/64575/container.zip
http://publikationen.ub.uni-frankfurt.de/files/64575/container.zip
The Cretaceous was punctuated by interludes of widespread deposition of organic-rich sediments (black shales) in the oceans and epicontinental seas, named Oceanic Anoxic Events (OAE)s, representing major alterations in the global carbon budget. The e
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7237ba337eeaf5cfca3ff5665f3d46a4
https://doi.org/10.5194/egusphere-egu21-8045
https://doi.org/10.5194/egusphere-egu21-8045
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology. 588:110803
Autor:
Victor M. Giraldo-Gómez, Maria Rose Petrizzo, Cinzia Bottini, Carla Möller, Thomas Wagner, Liyenne Cavalheiro, Onoriode Esegbue, Gabriele Gambacorta, Elisabetta Erba
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology. 587:110795
Publikováno v:
Cretaceous Research. 91:1-13
This study is based on Maastrichtian and Danian oil shales of a cored well located in the Jafr Basin in central Jordan. Studied sedimentary rocks consist of alternations of monotonous bituminous marls, phosphatized marls, occasional dolomite, black c
Publikováno v:
Journal of African Earth Sciences. 143:134-144
Organic matter (OM) rich marls were deposited in several intrashelf basins in Jordan (e.g. Yarmouk Basin, Lajjun Basin, Azraq-Hamza Basin, Jafr Basin, Eshidiyya Basin) on the southeastern Tethyan margin during the Maastrichtian to middle Eocene . Fac
Benthic Foraminifera and Geochemistry Across the Paleocene–eocene Thermal Maximum Interval in Jordan
Publikováno v:
Journal of Foraminiferal Research. 48:100-120
© 2018 Cushman Foundation. All rights reserved. This study presents benthic foraminiferal data from two sedimentary successions across the Paleocene-Eocene Thermal Maximum (PETM) from Jordan. Calcareous nannofossil biozones NP9a, NP9b, and NP10 of l
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology. 485:723-739
Core OS-28 located in central Jordan offers an expanded record of calcareous nannofossils and benthic foraminifera for the early Eocene of the southern Tethys. The oil shale succession of the studied interval covers calcareous nannofossil biozones NP