Arvicolidae (Rodentia) from the Pliocene of Tollo de Chiclana (Granada, SE Spain)

Several new fossiliferous Pliocene localities have been identified in the continental deposits of the area of Tollo de Chiclana (Guadix Basin, SE Spain), that have yielded a rich rodent and insectivore fauna. In this paper, we study the Arvicolidae from these localities. Remains adscribed to the genera Dolomys, Mimomys and Kislangia have been found, which are very interesting from a biostratigraphical point of view.     

Psychochaetetes (Varioparietes) lucentius nov. sp. (Cnidaria,chaetetida) du Tortonien superieur de la Sierra del Gorda (Nord d'Elche,province d'Alicante,Espagne)

The occurence of Ptychochaetetes (Varioparietes) lucentius nov. sp. in the Upper Tortonian from Sierra del Gorda(North of Elche, Spain) lets to hope the discovery of younger organisms.     

Human talus bones from the Middle Pleistocene site of Sima de los Huesos (Sierra de Atapuerca,Burgos, Spain)

Here we present and describe comparatively 25 talus bones from the Middle Pleistocene site of the Sima de los Huesos (SH) (Sierra de Atapuerca, Burgos, Spain). These tali belong to 14 individuals (11 adult and three immature). Although variation among Middle and Late Pleistocene tali tends to be subtle, this study has identified unique morphological characteristics of the SH tali. They are vertically shorter than those of Late Pleistocene Homo sapiens, and show a shorter head and a broader lateral malleolar facet than all of the samples. Moreover, a few shared characters with Neanderthals are consistent with the hypothesis that the SH population and Neanderthals are sister groups. These shared characters are a broad lateral malleolar facet, a trochlear height intermediate between modern humans and Late Pleistocene H. sapiens, and a short middle calcaneal facet. It has been possible to propose sex assignment for the SH tali based on their size. Stature estimates based on these fossils give a mean stature of 174.4 cm for males and 161.9 cm for females, similar to that obtained based on the long bones from this same site.     

Le Silurien et le Dévonien basal dans le Nord de la province de Seville (Espagne)

In the studied area, on the southern slope(«Ossa-Morena Zone) of the Sierra Morena (Spain) the Silurian and earliest Devonian (Lochkovian = approximately Gedinnian) consist of about 130 m of black, argillaceous, largely euxinic graptolitic slates, which, by the intermezzo of the dark «Limestones with Orthoceras and Scyphocrinus (late Ludlow and Pridolian), are divided into two inequal units, namely the Lower and Upper Graptolitic Slates. The occurence of 21 Graptolite zones and horizons was established, starting off with the basal Llandovery (A. acuminatus zone) and ending up with the Upper Lochkovian (M. hercynicas zone). This condensed tripartite graptolitic sequence, both lithologically and faunally, compares closely with the typical development of the Palaeotethys, as known from Thuringia, Carnic Alps, Sardinia and Northwest Africa. Certain graptolite species and details of the graptolitic succession (for instance across the Wenlock-Ludlow junction) that were hitherto known only or essentially from Thuringia, are recognized also in southern Spain.     

Integrated archaeobotanical research into vegetation management and land use in El Llano de la Horca (Santorcaz, Madrid, central Spain)

This paper presents an integrated archaeobotanical analysis carried out at the site known as “El Llano de la Horca”, a Bronze and Late Iron Age (3rd–1st century b.c.) Carpetanian settlement in central Spain (3600?±?80 b.p.). Pollen and spore analysis indicates an open landscape dominated by the herb taxa Asteraceae, Chenopodiaceae and Poaceae with an important representation of Glomus. The combination of pollen and charcoal studies also reveals the presence of Pinus sylvestris-nigra, P. pinaster-pinea, Juniperus thurifera, Quercus faginea, Q. ilex and Q. suber as the main trees used. Occurrences of Alnus, Corylus, Fraxinus and Juglans suggest the existence of water courses nearby. The archaeobotanical data is correlated with the geographical setting and archaeological context. The evolution of settlement patterns in central Spain, as well as the economy of other Carpetanian sites, is also considered to evaluate how this territory was managed for its vegetational resources since the Bronze Age (BA). Changes are expected as a consequence of different socio-economic factors at this site, especially when the settlement became an important Carpetanian oppidum. The combined results demonstrate a subsistence system based on cereal agriculture, in which naked wheat was dominant, together with some hulled barley and some erratic occurrences of hulled wheat. Furthermore, livestock breeding and metalwork activities seem to have resulted in a significant loss of woodland in order to clear land for crop fields and cattle grazing to cope with the needs of the growing Carpetanian community.     

New data on Mio-Pliocene Sciuridae (Rodentia,Mammalia) from southern Spain

Sciurids are very scarce in the fossil record, especially in the basins of southern Spain. The aim of this paper is to review the Sciuridae record in these basins. The Granada and Guadix basins have yielded specimens of Xerini and Pteromyinae, which represent the largest collection of fossil Sciuridae in southern Spain from the Middle Turolian to the Upper Ruscinian. The new discoveries change the currently known geographical and temporal range of some taxons, since we find the oldest evidence of Pliopetaurista pliocaenica in localities from the Late Turolian and of Heteroxerus mariatheresae in a locality of the Middle Turolian. Furthermore, we record the first evidence of Atlantoxerus margaritae in southern Spain.     

Origin of Spanish invasion by the zebra mussel, Dreissena polymorpha (Pallas, 1771) revealed by amplified fragment length polymorphism (AFLP) fingerprinting

The zebra mussel, Dreissena polymorpha is an aquatic nuisance invasive species originally native to the Ponto-Caspian region where it is found in lakes and delta areas of large rivers draining into the Black and Caspian seas. The dispersal of D. polymorpha began at the end of the 18th century, at a time when shipping trade become increasingly important and many canals were built for linking different navigable river systems in Europe. Over the past 200 years, zebra mussels spread to most of the lakes, rivers and waterways in Europe by a combination of natural and anthropogenic dispersal mechanisms. D. polymorpha invaded Spain around 2001, being found for the first time in the Riba-roja reservoir at the lower part of the Ebro River, North-East Spain. The relatively late invasion of Spain was most likely caused by the presence of the Pyrenees, which isolated the Iberian Peninsula from the rest of the European continent, and acted as a barrier to the dispersal of D. polymorpha. In recent studies, molecular genetic methods have successfully been used to determine phylo-geographic relationships, which may reflect invasion corridors and can help retrace source populations. Zebra mussels from populations in Great Britain, The Netherlands, Belgium, France, Germany, Spain, Italy, Romania and North America were analyzed using PCR based amplified fragment length polymorphism (AFLP)-fingerprinting to determine the source population of D. polymorpha in Spain. The phylogenetic analyses and pair-wise genetic distances revealed that the recent invasion of zebra mussels in Spain is most likely from France.     

Restauration d’un fémur fossile humain du site de la Sima de los Huesos (Atapuerca, Espagne)

A fossil human femur of Homo heidelbergensis from the site of the Sima de los Huesos (Atapuerca, Spain) was reconstructed from two main proximal and distal portions and numerous smaller fragments from the diaphysis. The use of an evaporative process to separate the bone fragments during their restoration represents an innovative approach in restoring paleontological materials and the intervention has resulted in the reconstruction of a complete femur. To avoid excessive manipulation of the reconstructed femur, a mold (negative) and cast (positive) were made of the restored specimen. This case study provides general protocols which can be widely applied to the restoration of paleontological materials from the moment of their excavation until they are deposited in a research center.     

New foot remains from the Gran Dolina-TD6 Early Pleistocene site (Sierra de Atapuerca, Burgos, Spain)

This paper presents and describes new foot fossils from the species Homo antecessor, found in level TD6 of the site of Gran Dolina (Sierra de Atapuerca, Burgos, Spain). These new fossils consist of an almost complete left talus (ATD6-95) and the proximal three-quarters of a right fourth metatarsal (ATD6-124). The talus ATD6-95 is tentatively assigned to Hominin 10 of the TD6 sample, an adult male specimen with which the second metatarsal ATD6-70+107 (already published) is also tentatively associated. Analysis of these fossils and other postcranial remains has made possible to estimate a stature similar to those of the specimens from the Middle Pleistocene site of Sima de los Huesos (Sierra de Atapuerca, Burgos, Spain). The morphology of the TD6 metatarsals does not differ significantly from that of modern humans, Neanderthals and the specimens from Sima de los Huesos. Talus ATD6-95, however, differs from the rest of the comparative samples in being long and high, having a long and wide trochlea, and displaying a proportionally short neck.     

First record ofBorelis melo andDendritina sp. in the Messinian of SE Spain (Cabo de Gata, Province Almeria)

Borelis melo andDendritina sp. occur in Messinian carbonates of the Cabo de Gata near Almeria. This is the first record of these larger benthic foraminifera from Messinian deposits in SE Spain. Two foraminiferal assemblages are differentiated: firstly, aBorelis- Dendritina assemblage which occurs on reef flanks, and secondly a lagoonal monospecificDendritina fauna.     

Description of the male of Potamocypris villosa (Jurine, 1820) (Crustacea,Ostracoda)

A bisexual population of Potamocypris villosa, found in Lago de Encina, a mesotrophic lake in the Cantabrian mountains, NW Spain, is the first certain record of the male of this species. Valves and soft parts are described. Males of Potamocypris-species lack a furca although a rudimentary furca is always present in females. The same applies to species of related genera, such as Tanganyikacypridopsis and Plesiocypridopsis. Some remarks on the position of the genus Potamocypris in the Cyprinopsinae are presented.     

Lower Ovetian (Lower Cambrian) trilobites and biostratigraphy of the Pedroche Formation (Sierra de Córdoba, southern Spain)

The low Lower Cambrian rocks from the Sierra de Córdoba, which consist of well exposed mixed facies and abundant fossil assemblages showing long stratigraphic ranges throughout the Pedroche Formation, represent one of the best successions of this age in Europe. The fossil assemblages include diverse Ovetian archaeocyaths, trilobites, small shelly fossils, calcimicrobia, trace fossils and stromatolites. Trilobites are still poorly known, and thus they are the main objective of this work. The trilobites studied originate from three sections. At the Arroyo de Pedroche 1 section, cf. Bigotinella and Bigotinabivallata are replaced towards the top by Lemdadellalinaresae, Lemdadellaperejoni sp. nov. and, finally, by Eoredlichia cf. ovetensis. At the Arroyo de Pedroche 2 section, Lemdadellalinaresae is replaced by Lemdadellaperejoni sp. nov. and Eoredlichia cf. ovetensis, while at the Puente de Hierro section Lemdadellalinaresae, L. aff. linaresae and Serraniaverae occur together. These new biostratigraphic data confirm that the Pedroche Formation, originally defined as a repetitive sequence of four members, contains only two members. The new trilobite discoveries permit the first tentative correlation between the Ovetian of southern Spain and Lower Cambrian strata from the High Atlas (Morocco), Siberia, Antarctica and Carteret (France).     

Considérations paléobiogéographiques sur les Streptelasmatina (Coelenterata,Rugosa) solitaires du Dévonien des monts Cantabriques (NW de l'Espagne)

The study of numerous fossil solitary forms ofStreptelasmatina (Coelenterata, Rugosa) and some ones belonging to different suborders from the Devonian of the Cantabrian Mountains (NW Spain), shows the importance of such organisms concerning the relations among the major faunal provinces during the Devonian time.The analysis of the Devonian Rugose coral fauna(from Emsian to Frasnian) lets to establish the paleobiogeographical relations of the Cantabrian genera. Particularly, during the Lower Devonian (Emsian) the relationships between the Eastern of North America and Spain would be closer than it was supposed until now.The evidence on the world distribution of thestudied forms suggest possible migration roads.     

Endocranial traits of the Sima de los Huesos (Atapuerca,Spain) and Petralona (Chalkidiki,Greece) Middle Pleistocene ursids. Phylogenetic and biochronological implications

A complete cranium of Ursus deningeri from Petralona (Chalkidiki, Greece) covered by a thick carbonate crust has been virtually liberated through CT scan and 3D image reconstruction, and compared with a specimen from the Sima de los Huesos, Sierra de Atapuerca (Spain) Middle Pleistocene site. X-ray computed tomography allowed for the identification of previously unrecognized and phylogenetically relevant traits. Analysis of these traits and an additional series of classically defined traits demonstrate the near identity of these specimens, thereby, confirming an early stage of the speloid “(cave bear)” condition. The replicate luminescence ages obtained for the SH deposit provide a combined minimum age estimate of 427 ± 12 ka for the underlying fossils. Based on a series of primitive and derived morphological features of these two crania, a similar age is here proposed for the Petralona and SH U. deningeri.     

The chronostratigraphic position of the Camping Francas section(Neogene of Tarragona,Spain)

The presence of Cirsotrema (s.s.) pumiceum (BROCCHI) and Chlamys (Manupecten) pesfelis (LINNE) in the section of Camping Francás (Province of Tarragona, Spain) suggests that the age of the deposits be changed from the upper Miocene (Tortonian) to the Pliocene. The change is of particular significance as the site is one of the classic localities of Pectinidae of the Neogene in North East Spain, and is type locality of Pecten (Flabellipecten) constisulcatus ALMERA & BOFILL.     

Notes on the genus Polycoccum (Ascomycota,Dacampiaceae) in Spain,with a key to the species

Comments on and a key to the 13 Polycoccum species known in Spain are presented, including synopses of their world distributions. Amongst these is P. rubellianae sp. nov., a lichenicolous fungus growing on thalli of Caloplaca rubelliana in eastern Spain (Valencia). It has relatively small ascomata, the lower part pale brown, and also small ascospores which are coarsely verrucose and have a thick gelatinous sheath when young. The new species is associated with a Phoma-like anamorph. The identity and systematic position of P. opulentum requires further study as the name has been applied to different species, and the occurrence of P. marmoratum in Spain is in need of confirmation. The Spanish record of P. arnoldii on Lecania cyrtella probably refers to another yet undescribed species.     

New Pseudaelurus and Styriofelis remains (Carnivora: Felidae) from the Middle Miocene of Abocador de Can Mata (Vallès-Penedès Basin)

New remains of felid jaws and teeth are described from several localities of the local stratigraphic series of Abocador de Can Mata (ca. 11.9 to 11.6 Ma, Middle Miocene; Vallès-Penedès Basin, Catalonia, Spain). Three different taxa are identified: Styriofelis turnauensis, Pseudaelurus romieviensis and Pseudaelurus quadridentatus. The described remains of P. romieviensis enable extending considerably the chronological range of this species in the Iberian Peninsula, in agreement with its record in the rest of Europe. Moreover, it is shown for the first time that P. romieviensis may possess a p2. The presence of this tooth therefore does not constitue a valid diagnostic feature to distinguish P. romieviensis from P. quadridentatus.