Beatriz Bádenas

Universidad de Zaragoza

Author Statistics

Papers

Citation

H-Index

i-10 index

Research Trends

Author Order

Document Type

Co-Authors

Marcos Aurell

Universidad de Zaragoza

110

José Ignacio Canudo

Universidad de Zaragoza

Idoia Rosales

Instituto Geológico y Minero de España

José Manuel Gasca

Universidad de Salamanca

G. San Miguel

Total (France)

Cristina Sequero

Universidad Complutense de Madrid

Miguel Moreno‐Azanza

Universidad de Zaragoza

Diego Castanera

Universidad de Zaragoza

Ana R. Soria

Universidad de Zaragoza

Eduardo Puértolas‐Pascual

Museu da Lourinhã

Cooperative Institutions

Universidad de Zaragoza

Universidad Complutense de Madrid

Instituto de Geociencias

Instituto Geológico y Minero de España

Consejo Superior de Investigaciones Científicas

Universitat de Barcelona

Universidad de Jaén

Universidad de Oviedo

University of the Basque Country

Universidad de Granada

Author Statistics

Papers

Citation

H-Index

i-10 index

Research Field

Facies architecture of a microbial–siliceous sponge-dominated carbonate platform: the Bajocian of Moscardón (Middle Jurassic, Spain)

Geological Society London Special Publications (2015)

Marcos Aurell Beatriz Bádenas

Abstract Extensive facies analysis of the outcrops located near Moscardón (Iberian basin, NE Spain) resulted in a precise reconstruction of the facies architecture of a Bajocian (Middle Jurassic) carbonate platform. Different types of microbialites occurred in the transitional area between the shallow and relatively deep carbonate platform domains, located above and below wave base level, respectively. The most significant volume of the micorbialites is found in the platform slope, located below wave base level, in a depth range of around 30–50 m. In the lower slope, during stages of rapid accommodation gain, the vertical aggradation of individual stratiform building blocks results in the formation of up to 25 m-thick microbial–siliceous sponge buildups. During stages of sea-level highstand the individual building blocks are dominated by lateral (down-slope) progradational accretion, resulting in flatter, lens-shaped buildups. The transition between the upper slope and the shallow platform area is characterized by microbial-encrusted intraclastic–bioclastic packstones. Microbial crust development helped to stabilize the seafloor, allowing the eventual accumulation and preservation of the sand-sized grains above wave base.

Sponge

Carbonate platform

10.1144/sp418.1

Cite

Citations (11)

Ricla eventites (Upper Jurassic) revisited; surface storm waves vs. internal waves

Beatriz Bádenas Luis Pomar Marcos Aurell Michele Morsilli

Source

Cite

Citations (1)

Factors Controlling Oncoid Distribution in the Inner Areas of a Late Kimmeridgian Carbonate Ramp (Northeast Spain)

Advances in Science, Technology & Innovation/Advances in science, technology & innovation (2019)

Cristina Sequero Beatriz Bádenas Marcos Aurell

Micrite

Sedimentation

Carbonate platform

10.1007/978-3-030-01452-0_41

Cite

Citations (2)

Fracture distribution along an Upper Jurassic carbonate ramp, NE Spain

Marine and Petroleum Geology (2015)

L.M. Kleipool John J. G. Reijmer N. Hardebol Giovanni Bertotti Marcos Aurell

Outcrop

Siliciclastic

Marl

10.1016/j.marpetgeo.2015.11.017

Cite

Citations (6)

Evaluation of pinnacle reef distribution at shallow subsurface using integrated geophysical methods: A case study from the upper Kimmeridgian (Spain)

Marine and Petroleum Geology (2016)

Óscar Pueyo Anchuela G. San Miguel Beatriz Bádenas Marcos Aurell

Ground-Penetrating Radar

Outcrop

10.1016/j.marpetgeo.2016.05.027

Cite

Citations (1)

The Tetrapod Fossil Record from the Uppermost Maastrichtian of the Ibero-Armorican Island: An Integrative Review Based on the Outcrops of the Western Tremp Syncline (Aragón, Huesca Province, NE Spain)

Geosciences (2021)

Manuel Pérez-Pueyo Penélope Cruzado‐Caballero Miguel Moreno‐Azanza Bernat Vila Diego Castanera

The South-Pyrenean Basin (northeastern Spain) has yielded a rich and diverse record of Upper Cretaceous (uppermost Campanian−uppermost Maastrichtian) vertebrate fossils, including the remains of some of the last European dinosaurs prior to the Cretaceous-Paleogene (K-Pg) extinction event. In this work, we update and characterize the vertebrate fossil record of the Arén Sandstone and Tremp formations in the Western Tremp Syncline, which is located in the Aragonese area of the Southern Pyrenees. The transitional and continental successions of these sedimentary units are dated to the late Maastrichtian, and exploration of their outcrops has led to the discovery of numerous fossil remains (bones, eggshells, and tracks) of dinosaurs, including hadrosauroids, sauropods, and theropods, along with other tetrapods such as crocodylomorphs, testudines, pterosaurs, squamates, and amphibians. In particular, this fossil record contains some of the youngest lambeosaurine hadrosaurids (Arenysaurus and Blasisaurus) and Mesozoic crocodylomorphs (Arenysuchus and Agaresuchus subjuniperus) in Europe, complementing the lower Maastrichtian fossil sites of the Eastern Tremp Syncline. In addition, faunal comparison with the fossil record of Hațeg island reveals the great change in the dinosaur assemblages resulting from the arrival of lambeosaurine hadrosaurids on the Ibero-Armorican island, whereas those on Haţeg remained stable. In the light of its paleontological richness, its stratigraphic continuity, and its calibration within the last few hundred thousand years of the Cretaceous, the Western Tremp Syncline is one of the best places in Europe to study the latest vertebrate assemblages of the European Archipelago before the end-Cretaceous mass extinction.

Syncline

Outcrop

Sauropoda

10.3390/geosciences11040162

Cite

Citations (13)

La unidad Almonacid de la Cuba en el sector de Obón-Castel de Cabra (Teruel)

Ana Pilar Bordonaba Beatriz Bádenas Marcos Aurell

The results o f a sedimentological analysis o f the Carixlan (lower Pliensbachian) o f the northern Iberian Chain (Obon-Castel de Cabra area, Teruel province) are presented in this work. Detailed facies analysis in the Almonacid Unit allowed the paleoenvironmental reconstruction of the carbonate platform developed in the northern part of the Iberian basin. Shall ower areas, located around the Castel de Cabra, were dominated by crinoids, corals and calcareous algae. They were deposited in the transition area between inner and mid ramp environments. In the midramp settings, located to the North (Obon), the facies consists o f marls and bioclastic limestones (mudstone to wackstone), that contain interbedded storm levels (tempestites).

Marl

Source

Cite

Citations (2)

Timing of sea level, tectonics and climate events during the uppermost Oxfordian (Planula zone) on the Iberian ramp (northeast Spain)

Palaeogeography Palaeoclimatology Palaeoecology (2014)

Claude Colombié Fabienne Giraud J. Schnyder Annette E. Götz Mekki Boussaha

Siliciclastic

Palynofacies

Sequence Stratigraphy

Diachronous

10.1016/j.palaeo.2014.07.014