Amphibians and squamate reptiles from the latest early Pleistocene of Cueva Victoria (Murcia, southeastern Spain, SW Mediterranean): Paleobiogeographic and paleoclimatic implications

The karstic filling of Cueva Victoria in southeastern Spain, dated from the latest early Pleistocene (ca. 1.1 Ma), is famous for providing primate fossil remains (Theropithecus) of typical African origin, in the general controversy on the antiquity of the first hominid settlements in Western Europe and their possible entrance into Europe through the Strait of Gibraltar. Cueva Victoria has also furnished the following fauna of anurans and squamate reptiles: cf. Pelodytes sp. (Pelodytidae), Bufo cf. B. bufo (Bufonidae), Blanus cinereus (Blanidae), Tarentola sp. (Geckonidae), Chalcides cf. Ch. bedriagai (Scincidae), Timon cf. T. lepidus and indeterminate small lacertids (Lacertidae), Natrix maura, Coronella girondica, Rhinechis scalaris and Malpolon cf. M. monspessulanus (Colubridae). This faunal association seems to suggest a mean annual temperature slightly fresher than nowadays (approximately 1°C less than at present in the area), with cooler winters but warmer summers and above all higher mean annual precipitations (+ 400 mm). The landscape may correspond to an open forest environment of a Mediterranean type, with some still water points

Catálogo de los micromamíferos (Rodentia, Eulipotyphla, Chiroptera) del Cuaternario Superior Ibérico del Museu de Geologia de Barcelona, Spain

The present catalogue represents an attempt to list Middle–Upper Pleistocene and Holocene micromammal material deposited in the Museu de Geologia de Barcelona, coming from 12 Iberian Peninsula localities (ten from Catalonia, one from Castilla y León and one from Andalucia). It permits to observe changes in species geographical distribution as Iberomys cabrerae, Microtus oeconomus, Hystrix cristata or Citellus sp. with regard to their present location. By this way, we can observe the existence during the Middle–Upper Pleistocene of some today extinct species such as Pliomys lenki or Allocricetus bursae. Key words: Middle-Upper Pleistocene, Holocene, Micromammals, Palaeobiogeography, Museo de Geologia de Barcelona, Spain.En este trabajo se presenta una lista del material de micromamíferos del Pleistoceno Medio-Superior y Holoceno depositado en el Museo de Geología de Barcelona, perteneciente a 12 yacimientos de la Península Ibérica (diez de Cataluña, uno de Castilla y León y uno de Andalucía). Este listado nos permite observar cambios en la distribución de especies como Iberomys cabrerae, Microtus oeconomus, Hystrix cristata o Citellus sp. respecto a su actual situación geográfica. Así mismo, nos permite vislumbrar la existencia durante el Pleistoceno Medio–Superior de algunas especies actualmente extintas, como Pliomys lenki y Allocricetus bursae. Palabras clave: Pleistoceno Medio-Superior, Holoceno, Micromamíferos, Paleobiogeografía, Museu de Geologia de Barcelona, España

Biochronological data for the Early Pleistocene site of Quibas (SE Spain) inferred from rodents assemblage

In this paper, the rodent fauna from the Early Pleistocene of Gruta1 (Quibas karstic complex, Murcia, SE Spain) is described. The assemblage includes one arvicoline (Allophaiomys sp.), two murines (Apodemus ex gr. mystacinus-epimelas, Castillomys rivas) and one glirid (Eliomys quercinus). The rodent assemblage indicates an age very close to the age of Fuente Nueva 3 and Barranco León 5 in the Guadix-Baza Basin, and Sima del Elefante in the Atapuerca karstic complex, between ca. 1.2-1.4My.

The Upper Oligocene of Montgat (Catalan Coastal Ranges, Spain): New age constrains to the western Mediterranean Basin opening

The Oligocene deposits of Montgat are integrated in a small outcrop made up of Cenozoic and Mesozoic rocks located in the Garraf-Montnegre horst, close to the major Barcelona fault. The Oligocene of Montgat consists of detrital sediments of continental origin mainly deposited in alluvial fan environments; these deposits are folded and affected by thrusts and strike-slip faults. They can be divided in two lithostratigraphic units separated by a minor southwest-directed thrust: (i) the Turó de Montgat Unit composed of litharenites and lithorudites with high contents of quartz, feldspar, plutonic and limestone rock fragments; and (ii) the Pla de la Concòrdia Unit composed of calcilitharenites and calcilithorudites with high contents of dolosparite and dolomicrite rock fragments. The petrological composition of both units indicates that sediments were derived from the erosion of Triassic (Buntsandstein, Muschelkalk and Keuper facies), Jurassic and Lower Cretaceous rocks (Barremian to Aptian in age). Stratigraphic and petrological data suggest that these units correspond to two coalescent alluvial fans with a source area located northwestwards in the adjoining Collserola and Montnegre inner areas. Micromammal fossils (Archaeomys sp.) found in a mudstone layer of the Pla de la Concòrdia Unit assign a Chattian age (Late Oligocene) to the studied materials. Thus, the Montgat deposits are the youngest dated deposits affected by the contractional deformation that led to the development of the Catalan Intraplate Chain. Taking into account that the oldest syn-rift deposits in the Catalan Coastal Ranges are Aquitanian in age, this allows to precise that the change from a compressive to an extensional regime in this area took place during latest Oligocene-earliest Aquitanian times. This age indicates that the onset of crustal extension related to the opening of the western Mediterranean Basin started in southern France during latest Eocene-early Oligocene and propagated southwestward, affecting the Catalan Coastal Ranges and the northeastern part of the Valencia trough during the latest Chattian-earliest Aquitanian times

A new key locality for the Pliocene vertebrate record of Europe : the Camp dels Ninots maar (NE Spain)

A new Pliocene Konservat-Lagerstätte in north-eastern Spain is described here for the first time. It is referred to as Camp dels Ninots. The particular geological conditions of the site, which correspond to lacustrine sedimentation in a maar, made it ideal for the preservation of fossils. At present, five large mammal skeletons in anatomical connection have been recovered: three individuals of Alephis tigneresi, one of Stephanorhinus jeanvireti and one of Tapirus arvernenis, as well as isolated remains. A minimum of five individuals of the chelonian Mauremys leprosa have been recovered, some of them in anatomical connection. The rodent Apodemus atavus, the amphibians cf. Pleurodeles sp., Lissotriton aff. helveticus and Pelophylax cf. perezi and freshwater fishes (Leuciscus ?) complete the vertebrate assemblage uncovered up to the present time. The coexistence of Stephanorhinus jeanvireti and Alephis tigneresi suggests an age of about 3.2Ma for the Camp dels Ninots, near the MN15-MN16 transition. The Camp del Ninots fossil record enables one to extend the biogeographic range of some vertebrate taxa, such as Stephanorhinus jeanvireti, Tapirus arvernensis or Mauremys leprosa to the Iberian Peninsula. Taphonomic evidences of the skeletal remains indicates minimal (if any) weathering. Deposition at the lake bottom seems to have taken place in oxygen depleted layers. In this way, Camp dels Ninots is comparable to other remarkable maar sites such as Messel, the Eocene site situated in Germany

El barranc de la Boella de la Canonja (Tarragonès) revisitat en la intervenció arqueològica preventiva de l'any 2007

El barranc de la Boella de la Canonja és un jaciment descobert en el primer terç del segle XX. Cinquanta anys després de la seva descoberta, la publicació d'aquest jaciment pels senyors R. Capdevila i S. Vilaseca va permetre actualitzar l'escàs coneixement de la bioestratigrafia del quaternari del Camp de Tarragona (Vilaseca, 1973). Tal com assenyala el mateix S. Vilaseca, la presència de fòssils de mamífers en el barranc va ser donada a conèixer per J. R. Bataller en la memòria explicativa del segon mapa geològic del full 473 de l'IGME corresponent a Tarragona (Bataller, 1935). El mateix S. Vilaseca apunta altres descobertes de mamífers ressenyades en el Camp de Tarragona, com la nota de Faura i Sans sobre un fragment de molar de proboscidi que Harlé determinaria com Elephas meridionalis el mateix any (Faura i Sans, 1920; Harlé, 1920). Aquesta resta va ser enviada per A. Romaní, aleshores director del Museu Balaguer de Vilanova i la Geltrú, a qui li van fer arribar des d'unes pedreres del Port de Tarragona. Els treballs geològics de M. Faura i Sans, J.R. Bataller i S. Vilaseca durant el primer quart del segle XX protagonitzaren el desenvolupament de la geologia, la paleontologia i la prehistòria en el marc del Servei del Mapa de la Mancomunitat de Catalunya

Expedición ANTARTIC'86 : Resultados científicos

Segundo Symposium Español de Estudios Antárticos, celebrado del 13 asl 15 de julio de 1987 en Madrid.-- 20 pages, 10 figures, 2 tablesPeer reviewe

Vanadium, PCB's in mussels from pillar Amposta oil platform

Peer reviewe