Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Carlos Lancis"'
Publikováno v:
RUA. Repositorio Institucional de la Universidad de Alicante
Universidad de Alicante (UA)
Universidad de Alicante (UA)
Sediment samples from Ocean Drilling Program (ODP) Sites 999 and 1237 in the Caribbean Sea and Eastern Pacific Ocean were studied to monitor the evolution of ceratoliths from 7.4 Ma to 6 Ma. Orthorhabdus rugosus shows high variability at the end of t
Autor:
Carlos Lancis, Hugo Corbí, Jaume Dinarès-Turell, Jesús M. Soria, Jose Enrique Tent-Manclus, Alice Giannetti
Publikováno v:
RUA. Repositorio Institucional de la Universidad de Alicante
Universidad de Alicante (UA)
Universidad de Alicante (UA)
A composite stratigraphic section ranging from the Messinian to the Pliocene, recording the most important phases of the Messinian Salinity Crisis, is represented in the San Miguel de Salinas area (Bajo Segura basin, SE Spain). Detailed magnetostrati
Autor:
César Viseras, Hugo Corbí, Jesús M. Soria, José-Antonio Pina, Fernando García-García, Carlos Lancis, Jose Enrique Tent-Manclus
Publikováno v:
Geobios. 45:249-263
The marine stratigraphic record of the Granada Basin (central Betic Cordillera, Spain) is composed of three Late Miocene genetic units deposited in different sea-level contexts (from base to top): Unit I (sea-level rise), Unit II (high sea-level), an
Autor:
Jaume Dinarès-Turell, Carlos Lancis, Antonio Estévez, Hugo Corbí, José-Enrique Tent-Manclús, Jesús-Esteban Caracuel, J. M. Soria, Alfonso Yébenes
Publikováno v:
Geobios. 43:201-217
The Fortuna Basin is an example of a marginal Mediterranean basin with evaporitic sedimentation during the Late Tortonian and Messinian. This basin shows an early restriction event before the main Messinian Salinity Crisis (MSC) that allows the Torto
Autor:
Jesús M. Soria, Antonio Estévez, Jaume Dinarès-Turell, Alfonso Yébenes, Carlos Lancis, Jesús E. Caracuel, Jose Enrique Tent-Manclus
Publikováno v:
Comptes Rendus Geoscience. 340:474-481
The Neogene Fortuna and Bajo Segura basins are located on the northeastern end of the Trans-Alboran Shear Zone (TASZ), on the eastern Betic cordillera. The stratigraphic study of the infilling of these basins has shown two major sedimentary discontin
Autor:
Carlos Lancis, Jesús E. Caracuel, Jesús M. Soria, Alfonso Yébenes, Jaume Dinarès-Turell, Jose Enrique Tent-Manclus, Hugo Corbí, César Viseras
Publikováno v:
Sedimentary Geology. 203:267-288
The analysis of the Messinian and Pliocene stratigraphy of the southern Bajo Segura Basin (Betic Cordillera, Spain) has revealed three highstand sedimentary phases (Messinian I, Messinian II, and Pliocene) bounded by two lowstand erosional surfaces (
Autor:
Carlos Lancis, José-Abel Flores
Publikováno v:
Micropaleontology. 52:477-481
Here we describe Reticulofenestra cisnerosii nov. sp. a rounded species of “Reticulofenestrid” with a well defined stratigraphic distribution in the Mediterranean Neogene. The first occurrence of this new taxa is placed in the middle part of subc