Víctor Sauqué

Bone Accumulation by Leopards in the Late Pleistocene in the Moncayo Massif (Zaragoza, NE Spain)

Eating habits of Panthera pardus are well known. When there are caves in its territory, prey accumulates inside them. This helps to prevent its kill from being stolen by other predators like hyenas. Although the leopard is an accumulator of bones in caves, few studies have been conducted on existing lairs. There are, however, examples of fossil vertebrate sites whose main collecting agent is the leopard. During the Late Pleistocene, the leopard was a common carnivore in European faunal associations. Here we present a new locality of Quaternary mammals with a scarce human presence, the cave of Los Rincones (province of Zaragoza, Spain); we show the leopard to be the main accumulator of the bones in the cave, while there are no interactions between humans and leopards. For this purpose, a taphonomic analysis is performed on different bone-layers of the cave.

A Late Pleistocene (MIS3) ungulate mammal assemblage (Los Rincones, Zaragoza, Spain) in the Eurosiberian–Mediterranean boundary

The Late Pleistocene archaeo-palaeontological sites in the Iberian Peninsula are located mainly on the coasts. Here, we present for the first time a palaeoenvironmental proxy for Upper Pleistocene locality (Marine Isotope Stage 3 MIS3) that is in the interior peninsular, in the Moncayo massif (Zaragoza). This is actually the boundary between Mediterranean and Eurosiberian climatic regions. This study is based in the site ungulates: Capra pyrenaica, which is larger in size than the current and fossil Capra from the Mediterranean area of the Iberian Peninsula. The horses have a small size, which is similar to that of the horses from Fontainhas and Casares. Significantly lesser in the number of specimens are the roe deer, the southern chamois and the auroch. The study and comparison of the faunal assemblage of the locality of Los Rincones with other sites of the Iberian MIS3 show a cluster of sites in the southern Peninsular, though separated, due to the abundance of Capra pyrenaica. The association of Los Rincones is similar to the southern peninsular sites such as Nerja, Gorham Cave, Cova Beneito and Zafarraya. The ungulate assemblage of Los Rincones represents a landscape with temperate climate, presence of steppe and patches of forest, similar to the current landscape surrounding the cavity today.

Carnivores from Los Rincones, a leopard den in the highest mountain of the Iberian range (Moncayo, Zaragoza, Spain)

Carnivores are a common element in Pleistocene fossil assemblages. However, they are not so abundant in terms of the numbers of remains. Here, we present a palaeontological study of the carnivores from the Late Pleistocene (MIS 3) of Los Rincones (Spain), one of the few deposits accumulated by leopards. One hundred and ten leopard remains have been recovered. This carnivore is not the only inhabitant of the cave, and 175 remains belonging to Ursus arctos have also been recovered, making it one of the sites with the greatest number of brown bear remains in the Iberian Peninsula. The large number of leopard remains has allowed us to make a detailed morphological and biometrical study that has enabled us to classify the remains within the subspecies Panthera pardus spelaea. The European Ice Age leopard inhabited Europe during Upper Pleistocene and it presents some similarities with Panthera uncia. A study of the scarce remains of Canis lupus indicates that this was similar in size to Canis lupus maximus; the scarcity of the remains prevents us from assigning our remains to this subspecies. A study of the brown bear remains indicates that it is similar to other populations in the north of the Iberian Peninsula with this chronology.

Avian remains from the Upper Pleistocene (MIS3) site of Aguilón P-7, south of the Ebro River, Spain

Aves are represented by abundant fossil remains in Quaternary sites. Birds are well adapted to the environment they inhabit, so they make very good paleoenvironmental indicators for Quaternary sites. Here we analyse the avian remains from the Late Pleistocene (probably MIS3) site of Aguilón P-7 (AGP-7). The Pleistocene sediments fill up a shallow cave, which is located in the Zaragozan part of the Iberian Range, 55 km south of the city of Zaragoza. We have for the first time provided a taxonomic and taphonomic study of the avian assemblage of AGP-7, as well as a preliminary paleoenvironmental analysis based on these data. Nine avian taxa have been identified: Galliformes indet., Lagopus sp., Aquila chrysaetos, Gyps fulvus, Passeridae indet., Anthus sp., Prunella modularis,Sturnus cf. unicolor and Corvus monedula. The taphonomic analysis did not provide conclusive information. However, it suggests an accumulation of uneaten food remains by diurnal birds of prey. The identified taxa currently inhabit the Iberian Peninsula, populating woodland environments with rocky areas. They are found in areas with an oceanic climate, in contrast to the Mediterranean climate that now prevails in Aguilón.

Late Pleistocene leopards as a bone accumulator: taphonomic results from S’Espasa cave and other Iberian key sites

Abstract The Pleistocene faunal accumulations documented in caves have commonly been attributed to the activity of humans or carnivores. According to the palaeontological and archaeological literature, cave hyena (Crocuta spelaea) was the main known bone accumulator in karstic environments. However, in recent times, the role of leopards as bone accumulators has been revealed, and recent research has identified this behaviour in the Iberian Pleistocene. Moreover, there are other caves where leopard could have been claimed as an accumulator such as S’Espasa. In this work we present its taphonomic study. This cave was compared with the actualistic studies of leopards. Besides, the site of S’Espasa was compared with the other leopard dens in the Iberian Peninsula. These sites present faunal assemblages composed mainly by leopard (Panthera pardus) and Iberian wild goat (Capra pyrenaica), the bones of this ungulate present a similar pattern of bone modification by carnivores, skeletal survival rate, and bone breakage. These features indicate that goats could have been accumulated by leopards. With the data from this work and the previous ones, we try to establish a pattern that will help in the future to identify other accumulations created by this big cat.

Pleistocene cave hyenas in the Iberian Peninsula: new insights from Los Aprendices cave (Moncayo, Zaragoza)

A new Pleistocene paleontological site, Los Aprendices, located in the northwestern part of the Iberian Peninsula in the area of the Moncayo (Zaragoza) is presented. The layer with fossil remains has been dated by amino acid racemization to 143.8 ± 38.9 ka (earliest Late Pleistocene or latest Middle Pleistocene). Five mammal species have been identified in the assemblage: Crocuta spelaea (Goldfuss, 1823) Capra pyrenaica (Schinz, 1838), Lagomorpha indet, Arvicolidae indet and Galemys pyrenaicus (Geoffroy, 1811). The remains of C. spelaea represent a mostly complete skeleton in anatomical semi-connection. The hyena specimen represents the most complete skeleton ever recovered in Iberia and one of the most complete remains in Europe. It has been compared anatomically and biometrically with both European cave hyenas and extant spotted hyenas. In addition, a taphonomic study has been carried out in order to understand the origin and preservation of these exceptional remains. The results suggest rapid burial with few scavenging modifications putatively produced by a medium sized carnivore. A review of the Pleistocene Iberian record of Crocuta spp. has been carried out, enabling us to establish one of the earliest records of C. spelaea in the recently discovered Los Aprendices cave, and also showing that the most extensive geographical distribution of this species occurred during the Late Pleistocene (MIS4- 2).

Cranial Biometrics of the Iberian Myotis myotis/Myotis blythii Complex: New Data for Studying the Fossil Record

The Myotis myotis/M. blythii species complex, spread across the Western Palearctic, is a problematic group for which the taxonomy of the species is not yet satisfactorily resolved. The Iberian Peninsula played a key role in its evolutionary history as a Pleistocene refuge and as the starting point for the eastward expansion of M. myotis in the early Holocene, while M. blythii reached the Iberian Peninsula only during the middle Holocene. The study of Iberian populations and particularly of the Iberian fossil record is of high interest in this regard. However, there are few data available on the biometry of the skulls and teeth of Iberian populations (which differ somewhat in size from those of other regions of Europe and Asia) or tools for the identification of fragmentary cranial remains. Much of the Quaternary Iberian record of large Myotis remains unassigned. Here, we contribute to the task of determining fragmentary cranial remains by providing new cranial and dental biometric data from extant Iberian populations, predictive models for isolated upper molar identification, and a set of indices that allow quantitative evaluation of the differences in anatomical traits (in skull and molars) between the two species.