Marc Furió

Biochronological, taphonomical, and paleoenvironmental background of the fossil great ape Pierolapithecus catalaunicus (Primates, Hominidae)

The Late Aragonian (late middle Miocene) stratigraphic sequence of Abocador de Can Mata (ACM) from Els Hostalets de Pierola (Vallès-Penedès Basin, Catalonia, Spain), rich in fossil vertebrate localities, provides a unique opportunity to study the evolution of western Eurasian hominoids. Among these sites, Barranc de Can Vila 1 (BCV1) recently delivered a well-preserved hominoid partial skeleton of a new genus and species, Pierolapithecus catalaunicus. On the basis of the small-mammal fauna recovered at BCV1, we infer an early MN 7+8 age, between 12.5 and 12Ma, for this site. The spatial distribution of macromammal fossils, the relative abundances of skeletal elements, and their state of preservation suggest that different agents were involved in the accumulation of the P. catalaunicus individual and the remaining taxa. Carnivore marks occur on some bones of the P. catalunicus skeleton, documenting the action of predators and/or scavengers in this case. In contrast, carnivore marks are extremely rare on other macromammal remains, which seem to be derived from adjacent alluvial-fan plain areas. The small-mammal fauna from BCV1 and the large-mammal fauna from the ACM series, indicate the presence of considerably humid and warm forest environments. The compositions of the small-mammal fauna from BCV1 and from other Late Aragonian sites from the Vallès-Penedès area are similar to those from France and central Europe. The former are clearly distinct from those of Iberian inner basins, where the environment appears to have been drier, thus precluding the dispersal of hominoids into that area.

EVOLUTIONARY HISTORY OF THE AFRICAN SORICID MYOSOREX (INSECTIVORA, MAMMALIA) OUT OF AFRICA

Abstract The species Myosorex meini Jammot, 1977 was a nomen nudum because it was named in an unpublished dissertation. The species is here revised using the new material found in the Late Pliocene fissure infillings of Almenara-Casablanca 1 and 4 (province of Castelló, East of Spain) and from the Tollo de Chiclana localities 1B, 3, 10, and 10B in the Guadix Basin (province of Granada, Southeastern Spain). A new diagnosis is given with some differential characters to identify the species within the family. The species definitively belongs to the genus Myosorex. A definitive new allocation for the genus into the subfamily Crocidosoricinae is proposed as an alternative to the classical assignment to the Crocidurinae. This is justified by available data coming from different fields of research, such as genetics, reproductive biology, morphology, and paleontology. Within the Crocidosoricinae, the tribe Myosoricini Kretzoi, 1965 is resurrected, and two other ones, the Crocidosoricini and the Oligosoricini, are redefined. From the paleobiogeographical point of view, the occurrence of the African genus Myosorex constitutes a new striking evidence of the faunal exchange between Eurasia and Africa that took place during the Messinian Salinity Crisis.

The Paleobiology of the Extinct Venomous Shrew Beremendia (Soricidae, Insectivora, Mammalia) in Relation to the Geology and Paleoenvironment of Dmanisi (Early Pleistocene, Georgia)

ABSTRACT The uses of toxic substances in the animal kingdom are usually explained as adaptations to reach bigger prey—venom, or to defend from the attack of predators—poison. This is a quite simplistic explanation of the reality, which offers other, less evident, uses for the possession of these compounds. In the present work, we analyze the characters of Beremendia Kormos, 1934, an extinct Eurasian genus of shrews, which was recently said to have been venomous. The envenomation apparatus of these shrews was correlated with its uncommonly large size, justifying a possible adaptation to hunt big prey. Examining its dental characters, we do reassess the venomous nature of the species included in this genus, but we deduce that the diet of Beremendia was highly specialized in coleopterans and gastropods instead of large animals. The use of venom in shrews feeding on non-struggling prey can be reliably explained as a mechanism to subdue the prey without killing them before the real time of consumption. The induction of victims into a comatose-state permits their hoarding for a longer time in a better state of preservation than if they were dead, thus diminishing the risk of starvation. Such strategy provides important benefits to their users under irregular conditions, because the effects of environmental unpredictability are consequently reduced. This interpretation of Beremendia is supported by the ethology of some extant shrews, and correlated at local scale with the geological context of Dmanisi, and at global scale with the Plio-Pleistocene climatic trends.

Magnetostratigraphy of the Ouarzazate Basin: Implications for the timing of deformation and mountain building in the High Atlas Mountains of Morocco.

Two magnetostratigraphic profiles (450 samples) have been carried out to constrain the age of synorogenic formations in the southern foreland of the High Atlas of Morocco. The Amekchoud profile covers the Aït Ouglif and Aït Kandoula alluvial formations that form the bulk of the Ouarzazate basin fill, indicating an age between the upper Langhian and the Messinian (Miocene). Data obtained in the previously unexplored Hadida formation profile covers the oldest terms of the foreland basin succession, but the low quality of the magnetic record only allows proposing a tentative age between the middle Lutetian and an undetermined middle to late Eocene. The correlation of the Amekchoud profile is based on the recognition of the long C5n chron (Tortonian) in the middle part of the section studied and a new vertebrate locality of upper Tortonian age found in the upper part. These results indicate a discontinuous record of foreland basin development in the southern Atlas domain from mid Eocene to late Miocene times, punctuated by an intermediate large hiatus of 20-25 ma (late Eocene to mid Miocene). Thrusting in the Sub-Atlas frontal thrust belt began before the Aït Ouglif and Kandoula formations, probably during the Oligocene, and extends up to recent times. The alternation of periods of deposition with others of no sedimentary record, which does not coincide with specific tectonic events, results probably from the interference of orogenic deformation and the mantle-related thermal uplift events that have been described for the Moroccan Atlas.

New Data on Paenelimnoecus from the Middle Miocene of Spain Support the Shrew Subfamily Allosoricinae

Limnoecus truyolsi was long considered an enigmatic shrew. Additional material from the Calatayud-Montalbán Basin (Spain) shows it to be referable to the genus Paenelimnoecus. The species represents an intermediate form between P. micromorphus and P. crouzeli. This lineage confirms the separate development of the “soricine” p4, and thus supports the Allosoricinae as a separate subfamily.

Chronological and environmental context of the first hominin dispersal into Western Europe: The case of Barranco León (Guadix-Baza Basin, SE Spain)

The early Pleistocene site of Barranco León (Guadix-Baza Basin, SE Spain), dated to 1.4 Ma (millions of years ago), records the oldest hominin occurrence in Western Europe, as evidenced by the discovery of one tooth and thousands of Mode 1 stone tools. In this paper a detailed analysis of the microvertebrate content of the D1 and D2 units from this site is presented. The early Pleistocene in the Guadix-Baza Basin is characterized by a sharp climatic deterioration, which possibly impeded the settlement of this region by the early hominin population from the southern Caucasus. Shortly afterwards, when the climatic conditions were again favorable, a hominin presence is suddenly evidenced at the units D1 and D2 of Barranco León. According to the microvertebrate analysis of these units, the mean annual temperature at the time of deposition was significantly higher than 13 °C, with prevalent humid conditions. However, although most of the species were inhabitants of water edges, an open landscape was present in the vicinity of the lake. The data reported here clearly support the idea that the early hominin occupation of Europe was strongly constrained by climatic and environmental conditions, rather than by physiography or cultural factors.

Rodents and insectivores from the hominoid-bearing site of Can Feu (Vallès-Penedès Basin, Catalonia, Spain)

ISAAC CASANOVAS-VILAR,*,1 MARC FURIÓ,1 DAVID M. ALBA,1 SALVADOR MOYÀ-SOLÀ,2 and JOSEP MANEL MÉNDEZ1; 1Institut Català de Paleontologia Miquel Crusafont, Universitat Autònoma de Barcelona, Edifici ICP, Campus de la UAB s/n, 08193 Cerdanyola del Vallès, Barcelona, Spain, isaac.casanovas@icp.cat; marc.furio@icp.cat david.alba@icp.cat manuel.mendez@icp.cat; 2ICREA at Institut Català de Paleontologia Miquel Crusafont and Unitat d’Antropologia Biològica (Dept. BABVE), Universitat Autònoma de Barcelona, Edifici ICP, Campus de la UAB s/n, 08193 Cerdanyola del Vallès, Barcelona, Spain, salvador.moya@icp.cat

Multispectral and colour imaging systems for the detection of small vertebrate fossils: A preliminary study

The process of separating small vertebrate fossils from sediment is a monotonous exercise, usually carried out manually and mainly based on morphological features. The large amount of time and personnel required results in the high economic costs associated with this antiquated technique. In this study we test the potential of colour and multispectral imaging for the detection of small vertebrate fossils to facilitate their separation from sediment. This technique is based on the analysis of the spectral and fluorescence characteristics of fossils. Specifically, a multispectral system with a charge-coupled device (CCD) camera attached to a liquid crystal tunable filter and a digital colour camera was used in combination with daylight and ultraviolet light sources. The results show that the reflectance of bones, teeth and sediment are usually different at longer wavelengths, and that fluorescence rates also differ in the bluegreen region. Unfortunately, samples from different paleontological sites present different patterns, hindering the standardization of a method that discriminates microfossils from sediments. However, the combination of colour and multispectral imaging systems with recent advances in laser-stimulated fluorescence in fossils could constitute an optimal solution for an efficient sorting process of small vertebrate remains within geological samples.

The use of the species concept in paleontology. Comment on "Nesiotites rafelinensis sp. nov., the earliest shrew (Mammalia, Soricidae) from the Balearic Islands, Spain" by Rofes et al., 2012

The earliest representative of Nesiotites from Caló d’en Rafelino (Mallorca) has been recently described as a new species (Nesiotites rafelinensis) based on a single hemimandible with p4-m3. A thorough inspection of large collections of different species of Nesiotites from the Balearic Islands reveals wide intraspecific morphological variation within these Plio-Pleistocene shrews. Six out of seven diagnostic characters of N. rafelinensis fall within the variability of the oldest species previously known, N. ponsi. We thus conclude that no traits sufficiently support the definition of a new species, and in our opinion this material should be better referred to N. ponsi or to a closely related form (N. aff. ponsi / N. cf. ponsi). Marc Furió . Institut Català de Paleontologia M. Crusafont, Edifici ICP, Universitat Autònoma de Barcelona, Cerdanyola del Vallès, 08193, Barcelona, Spain. marc.furio@icp.cat Guillem Pons-Monjo. Institut Català de Paleontologia M. Crusafont, Edifici ICP, Universitat Autònoma de Barcelona, Cerdanyola del Vallès, 08193, Barcelona, Spain. guillem.pons@icp.cat

Rodents and insectivores from the late Miocene of Romerales (Fortuna Basin, Southern Spain)

Abstract The Neogene Fortuna Basin (Murcia Region, SE Spain) is rich in microvertebrate sites. Its continental sections include localities extended from the middle Turolian (MN12) to the early Ruscinian (MN14). However, there are few works dealing with the taxonomy of these fossil assemblages. In this paper we provide a complete taxonomic study of the rodents and insectivores from three levels (ROM-2B, ROM-2C and ROM-3A) within the Romerales section. We infer a late Turolian age (late Messinian) for these levels, among which the richest and most diverse level is ROM-C, including at least 11 different taxa. In addition, the paleoecological analysis of these fossil assemblages suggests the dominance of open herbaceous meadows under temperate climate during the formation of these sites, with a slight decrease in temperature and humidity from ROM-2B to ROM-2C.