Zobrazeno 1 - 10
of 56
pro vyhledávání: '"Victoriano Pujalte"'
Autor:
Julio Aguirre, Juan C. Braga, Victoriano Pujalte, Xabier Orue-Etxebarria, Edward Salazar-Ortiz, Daniel Rincón-Martínez, Manuel Abad, Fernando Pérez-Valera
Publikováno v:
Diversity, Vol 12, Iss 3, p 117 (2020)
During the greenhouse conditions prevailing in the early−middle Eocene, larger benthic foraminifers (LBF) spread out on carbonate platforms worldwide while rhodolith beds were scarcely represented. This reduction in rhodolith beds coincided with a
Externí odkaz:
https://doaj.org/article/8b1748e8b3874ca7baf2dea03c508516
Autor:
Simonetta Monechi, Birger Schmitz, Xabier Orue-Etxebarria, Francisco J. Rodríguez-Tovar, Victoriano Pujalte, Silvia Ortiz
Publikováno v:
Global and Planetary Change. 178:153-167
An expanded record (~14 m)of the Paleocene–Eocene Thermal Maximum (PETM), a transient period of extreme global warming that occurred ~56 million years ago, has been found based on calcareous nannofossil and foraminifera stratigraphy in the deep mar
Autor:
Xabier Orue-Etxebarria, Victoriano Pujalte, Julio Aguirre, Manuel Abad, Juan C. Braga, Edward A. Salazar-Ortiz, Daniel Rincón-Martínez, Fernando Pérez-Valera
Publikováno v:
Addi. Archivo Digital para la Docencia y la Investigación
instname
Diversity
Volume 12
Issue 3
Diversity, Vol 12, Iss 3, p 117 (2020)
Universidad de Cantabria (UC)
RUA. Repositorio Institucional de la Universidad de Alicante
Universidad de Alicante (UA)
Digibug. Repositorio Institucional de la Universidad de Granada
instname
Diversity
Volume 12
Issue 3
Diversity, Vol 12, Iss 3, p 117 (2020)
Universidad de Cantabria (UC)
RUA. Repositorio Institucional de la Universidad de Alicante
Universidad de Alicante (UA)
Digibug. Repositorio Institucional de la Universidad de Granada
During the greenhouse conditions prevailing in the early&ndash
middle Eocene, larger benthic foraminifers (LBF) spread out on carbonate platforms worldwide while rhodolith beds were scarcely represented. This reduction in rhodolith beds coincide
middle Eocene, larger benthic foraminifers (LBF) spread out on carbonate platforms worldwide while rhodolith beds were scarcely represented. This reduction in rhodolith beds coincide
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::26552849db125ec959ed266d204b3e54
http://hdl.handle.net/10810/42600
http://hdl.handle.net/10810/42600
Publikováno v:
AAPG Bulletin. 101:563-570
The Danian carbonates exposed in the Urbasa–Andia plateau (western Pyrenees, North Spain) provide the opportunity to examine at different scales the facies types and architecture of a greenhouse ramp to rimmed shelf from the slope to coralgal reefa
Autor:
Bastiaan C. J. van den Berg, Ángel Salazar, Josep Maria Salvany, José N. Pérez-Asensio, Francisco Javier Sierro, M.P. Mata, Birger Schmitz, Daniel García-Castellanos, Pedro P. Cunha, Antonio Barnolas, Santiago Ledesma, Jorge Civis, Victoriano Pujalte, Juan C. Larrasoaña
Publikováno v:
Digital.CSIC. Repositorio Institucional del CSIC
instname
The Geology of Iberia: A Geodynamic Approach ISBN: 9783030111892
UPCommons. Portal del coneixement obert de la UPC
Universitat Politècnica de Catalunya (UPC)
Recercat. Dipósit de la Recerca de Catalunya
instname
The Geology of Iberia: A Geodynamic Approach ISBN: 9783030111892
UPCommons. Portal del coneixement obert de la UPC
Universitat Politècnica de Catalunya (UPC)
Recercat. Dipósit de la Recerca de Catalunya
This chapter deals with the two Alpine Foreland Basins of the Iberian Peninsula. The first part of the chapter refers to the South Pyrenean Foreland Basin and its westward prolongation, the Basque–Cantabrian Paleogene Basin. It includes: (1) the in
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3b2e666dfe0b9d269e941615137c1b1a
http://hdl.handle.net/10261/202737
http://hdl.handle.net/10261/202737
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology. 459:453-470
The La Pardina Formation is a siliciclastic-dominated unit up to 26 m thick intercalated within a 300 m thick Danian–lower Ilerdian succession of shallow marine carbonates in the southern Pyrenees. The unit is composed of four interdigitated facies
Autor:
F. Caballero, Estibaliz Apellaniz, Birger Schmitz, Simonetta Monechi, Silvia Ortiz, Francisco J. Rodríguez-Tovar, Xabier Orue-Etxebarria, Victoriano Pujalte
Publikováno v:
Spanish Journal of Palaeontology, Vol 32, Iss 1, Pp 185-206 (2020)
Research interest in the early Paleogene was greatly enhanced after the recognition of several short-lived warming events in that period (hyperthermals), considered ancient analogues of the ongoing warming of the Earth climate. In the Caravaca and Al
Publikováno v:
Climate of the Past, Vol 11, Iss 12, Pp 1653-1672 (2015)
The Paleocene–Eocene thermal maximum (PETM) is represented in numerous shallow and deep marine sections of the south–central and western Pyrenees by a 2–4 m thick unit (locally up to 20 m) of clays or marly clays intercalated within a carbonate
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d964457917e01830878fe6192fa71dc9
https://www.clim-past.net/11/1653/2015/
https://www.clim-past.net/11/1653/2015/