Contribution of fossil Lagomorpha (Mammalia) to the refinement of the late Miocene–Quaternary palaeobiogeographical setting of Italy

Fossil lagomorphs are very useful palaeogeographical indicators. In the last 15 years, several papers centered on fossil lagomorphs contributed to improve the Italian late Miocene–Quaternary palaeogeographical setting, solving palaeobiogeographical enigmas debated for decades, and providing new, challenging palaeogeographic data. The high number of endemic fossil lagomorphs of Italy is due in part to its complex tectonic history (insular endemisms), and in part to the semi-isolation and the physiography of the Peninsula (continental endemisms). In Italian lagomorphs, a direct causal relationship between dispersal and turnovers is not observed, except for the Toringian. Actually, species replacements are customarily due to archipelago effect (late Miocene), phyletic speciation (Pliocene of Sardinia and Italian mainland) or occur after the extinction of older congeneric species (early Pleistocene).     

The Miocene mammal record of the Vallès-Penedès Basin (Catalonia)

The land mammal record of the Vallès-Penedès Basin (Catalonia, NE Spain) ranges from the early Miocene (Ramblian) to the late Miocene (Turolian), that is from about 20 to 7 Ma. Here we present an updated review of the mammal succession focusing on biochronology as well as on environmental and faunal changes. Based on faunal similarities with central Europe, we interpret this basin as a transitional zone between the forested environments of northern regions and the more arid landscapes of the inner Iberian Peninsula. The quality of the Vallès-Penedès record and its chronostratigraphic control is clearly better for the late Aragonian and the Vallesian (between 12.6–9.0 Ma), especially for small mammals. Therefore, we analyze small mammal diversity dynamics during this interval. Contrary to previous analyses, which found an abrupt extinction event coinciding with the early/late Vallesian boundary (the Vallesian Crisis), our results show that this pattern is due to uneven sampling. Instead, taxonomic richness slowly decreased since the late Vallesian as a result of a series of extinctions that mostly affected forest-dwelling taxa.     

Review of Japanese Cenozoic (Miocene–Modern) Vertebrate Tracks

One hundred and seventy three Cenozoic vertebrate track sites from Miocene to 1600 A.D have been reported in Japan. Three ichnofaunas can be recognized: a perissodactyl and artiodactyl ichnofauna in the Miocene, an artiodactyl and proboscidean ichnofauna in the Plio-Pleistocene, and human ichnofauna from about 900–800 B.C. to about 1400–1600 A.D. Track data indicate that a predominance of large vertebrates in fluvio-lacustrine environment in lowland changed from perissodactyls to proboscidean through Miocene to Plio-Pleistocene, and ancient people then occupied lowlands instead of large animals. Pes length of proboscidean tracks revealed temporal variation, and the relationship between proboscidean body sizes and tracks was observed. The Cenozoic Japanese proboscidean trackways can be distinguished on the basis of trackway width, as narrow- and wide-gauge, but the difference between of those narrow- and wide-gauge trackways probably indicates generic level differences. The Cenozoic Japanese bird tracks can be identified as four types: ?crane (Family Gruidae?), ?heron (Family Ardeidae?), ?stork (Family Ciconiidae?), and ?shorebird tracks.     

New data on the Cricetidae from the Miocene “Terre Rosse” of Gargano (Apulia,Italy)

The Gargano “Terre Rosse” deposits are paleokarst fissure fillings found in the Mesozoic limestone of the Apricena-Poggio Imperiale area. They are an important source of information for evolutionary and paleobiogeographic studies. The Late Miocene-Early Pliocene assemblages found in the Terre Rosse attest the complex history of endemic faunal distribution in a paleoarchipelago. Based on the cricetid samples from six distinct fissures (F15, F21a, F21b, F21c, F1, F9, NBS) stored in the Department of Earth Sciences of the University of Florence, three species of endemic cricetids are described: the small-sized Hattomys beetsi, the middle-sized Hattomys nazarii, and the large-sized Hattomys gargantua. The specimens from fissure F15 are attributed to H. beetsi, those from F21a-b to the transitional form Hattomys beetsi-nazarii, those belonging to NBS are ascribed to H. nazarii, whereas those from F1 and F9 are classified as H. gargantua. F21c is considered contaminated with material from different fissures. In line with previously published results, the analysis confirms that the endemic cricetids underwent a remarkable increase in size through time. The morphological variations show a marked trend towards increasing enamel thickness, but also the tendency of the cusps to assume a carved-in aspect. The variations of the morphological characters confirm that the three species likely belong to the same lineage.     

First porcupine fossils (Mammalia,Rodentia) from the late Miocene of NW Iran,with notes on late Miocene–Pliocene dispersal of porcupines

This paper describes the first fossil porcupine remains from Iran. Four upper cheek teeth and two fragmentary lower incisors present sufficient characters for identification as Hystrix aryanensis, a species previously known from the late Miocene locality of Molayan (Afghanistan) estimated at ca. 7–8 Ma. The dental features of porcupines are discussed to show their systematic value and highlight evolutionary trends in late Miocene and Pliocene porcupines. This study also discusses the dispersal history of fossil porcupines in relation to paleobiogeographic provinces and environmental changes during late Miocene to late Pliocene time.     

Carnivore Trackways from the Miocene Site of Salinas de Añana (Alava,Spain)

A fossil tracksite of Lower Miocene age discovered near Salinas de Añana, Alava (Spain), has rendered an exceptionally well-preserved assemblage of vertebrate ichnites. The site shows a high proportion of carnivore tracks (3 out of 5 mammal ichnospecies) and a high number of individual trackways (15), some including over 50 consecutive footprints. The carnivore ichnites are classified as Felipeda lynxi Panin & Avram, 1962 Panin, M. and Avram, B. 1962. Noi urme de vertebrate in Miocenul Subcarpatilor Rominesti. Studii Cercet Geologia, 13: 521–525.  [Google Scholar], Felipeda parvula ichnosp. nov. and Canipeda longigriffa Panin & Avram, 1962 Panin, M. and Avram, B. 1962. Noi urme de vertebrate in Miocenul Subcarpatilor Rominesti. Studii Cercet Geologia, 13: 521–525.  [Google Scholar], and they are attributed to a felid, an undetermined small aeluroid, and a herpestid, respectively. The long trackways allow determination of gaits, which include lateral sequence walks and diagonal sequence trots, and of speed, which ranges from 0.4 to 1.4 m/s. Froude numbers range between 0.1 and 0.8, agreeing with gait interpretations and speed calculations. The felid trackways provide the first known evidence of group traveling in fossil cats. The herpestid footprints show modern-grade adaptations for terrestrial locomotion and digging.     

Snake fauna (Reptilia: Serpentes) from the Early/Middle Miocene of Sandelzhausen and Rothenstein 13 (Germany)

The Early/Middle Miocene (European Land Mammal Zone MN5) localities of Sandelzhausen and Rothenstein 13 in southern Germany have yielded remains of about 13 ophidian taxa: Eoanilius sp. (Aniliidae), Bavarioboa ultima (Boidae), “Coluber” sp., ?Telescopus sp., Natrix sp., cf. Natrix sp., cf. “Neonatrix” sp., unidentified “colubrines” and “natricines” (Colubridae), Naja sp., an unidentified elapid (Elapidae), Vipera sp. (“Oriental viper”), Vipera sp. (“aspis complex”) (Viperidae). Both faunas document a transitional phase from those reported from several late Early and Middle Miocene sites of Central and Western Europe. The climates of Sandelzhausen and Rothenstein 13, as indicated by ophidian fossils, were warm, although not tropical or subtropical.     

Palaeoecological implications of the sympatric distribution of two species of Machairodus (Felidae,Machairodontinae, Homotherini) in the Late Miocene of Los Valles de Fuentidueña (Segovia,Spain)

In this paper, we study a sample of cranial, mandibular and dental remains of two species of the machairodontine felid genus Machairodus from the Early Vallesian (MN 9, around 10 Ma) site of Los Valles de Fuentidueña (Segovia, Spain): the tiger-sized Machairodus aphanistus, and the smaller and more primitive M. alberdiae; a species which is only known from this site. The fossils of these two sympatric populations are compared with the most abundant samples of M. aphanistus from the Late Vallesian (MN 10), younger sites of Batallones-1 and Batallones-3 (Torrejón de Velasco, Madrid, Spain). The results support the specific separation of M. alberdiae from M. aphanistus based on several differences in teeth size and proportions. Besides this, we observed differences among the analysed samples of M. aphanistus, indicating a differentiation between the older and more primitive form from Los Valles de Fuentidueña, and the younger and more derived one from the two Batallones sites. These differences fit well with the morphological evolution of this lineage towards the more derived Turolian Amphimachairodus giganteus. Finally, a relatively structured, patched habitat, combining the presence of open landscapes with shrubby and wooded areas, is inferred to explain the sympatric distribution of these two large machairodontines in Los Valles de Fuentidueña.     

Finds of Ruminants and New Data on the Stratigraphy of the Late Miocene Locality of Fortep’yanka 2 (Northwest Caucasus,Adygea Republic)

Paleontological Journal - New finds of fossil remains of ruminants of genera Euprox Stehlin, 1928 (Dicrocerini, Muntiacinae, Cervidae) and Protragocerus Depéret, 1887 (Boselaphini, Bovinae,...     

First record of fossil angiosperm wood (Ulmoxylon,Ulmaceae) from the famous locality of Bı́lina (Czech Republic,Early Miocene)

A fossil angiosperm wood is described for the first time from the famous Early Miocene locality of Bı́lina. It represents a fossil elm wood, attributed to Ulmoxylon marchesonii Biondi. The fossil wood can be compared to extant North American soft elms, also to Ulmus macrocarpa Hance and U. parvifolia Jacq. from China or to the European common elm U. carpinifolia Gled. The wood together with fossil leaves/fruits of Ulmus pyramidalis Goeppert forms a single natural fossil species that lived in the Bı́lina area during the Early Miocene. The influence of two types of preservation, permineralised and xylitic, on the same wood species is also discussed. To cite this article: J. Sakala, C. R. Palevol 1 (2002) 161–166.     

The late Miocene mammals from the Konservat-Lagerstätte of Saint-Bauzile (Ardèche,France)

Diatomite deposits of Saint-Bauzile near Privas (Ardèche) in southern France have been known since more than two centuries for abundant and extremely well-preserved fossils of plants and animals. The radiometric dating brackets fossil-bearing horizons between 7.2 and 7.6 Ma, which is consistent with the biochronologic age given by fossil mammals, which are characteristics of the late MN11 zone, i.e. the second part of the late Miocene. The main interest of this site for mammals is that they are preserved almost “in the flesh”, as entire skeletons with bones in their anatomical connection, and often with skin and fur charred and forming a halo around the body. In this work, we studied the remains of a lagomorph, two rodents, an equid, a suid, a bovid and a rhino. The mode of preservation of mammals as entire bodies suggests sudden death and rapid burial of individuals.     

Qurliqnoria (Bovidae,Mammalia) from the Upper Miocene of Çorakyerler (Central Anatolia,Turkey) and its biogeographic implications

New bovid material from the Upper Miocene site of Çorakyerler (Çankırı basin, Anatolia, Turkey) is described and compared here. The described taxon is identified as a representative of the stem caprine genus Qurliqnoria, previously known from the peri-Tibetan area exclusively. The stronger horn-core divergence, weaker anterior keel, smoother horn-core surface, stronger lateral horn-core curvature, stronger and thicker interfrontal suture, less flexed and less pneumatized frontals, and smaller supraorbital foramina differentiate the Çorakyerler Qurliqnoria from the type and only known species of the genus, Q. cheni from China, and demand the erection of a new species, Qurliqnoria chorakensis n. sp. A review of other late Miocene bovid records allows the recognition of Qurliqnoria in Sinap Tepe (Turkey) and Platania (Greece), suggesting a westward propagation of the genus during the Vallesian.     

Mandibular remains of Procardiomys martinoi Pascual, 1961 (Hystricognathi,Cavioidea) from the Arroyo Chasicó Formation (early late Miocene) of Argentina: anatomy and the phylogenetic position of the genus within Caviidae

Hydrochoerinae is a clade of caviomorph rodents broadly distributed in South America, which includes the maximum body size recorded among extant rodent taxa. The most basal forms of this group are an assemblage of small to medium body size extinct taxa with a plesiomorphic dentition, traditionally clustered in the group cardiomyines. One of the oldest known cardiomyine is Procardiomys martinoi (Chasicoan South American Land Mammal Age SALMA; early late Miocene), which was known only from the holotype, a fragmentary palate with the left and right molar series. New mandibular remains from the Arroyo Chasicó Formation (Chasicoan SALMA) are described and identified here as belonging to P. martinoi because they share a unique combination of characters (as well matching in size) with the upper dentition of the holotype. These materials help in critically reviewing the taxonomic identification of the mandibular remains previously assigned to Procardiomys and allow testing the phylogenetic affinities of this taxon within Caviidae. P. martinoi is depicted as one of the most basal forms of Hydrochoerinae, placed basally on the lineage leading to extant capybaras after the split between the common ancestor of Kerodon and Hydrochoerus.

http://zoobank.org/F60356E0-CB8E-48C2-BF86-429E347A9579     

New remains of Dorcatherium crassum (Artiodactyla: Tragulidae) from the Early Miocene (MN4) of Els Casots (Subirats,Vallès-Penedès Basin)

New tragulid dental remains from the late Early Miocene (16.5–16.3 Ma, MN4) locality of Els Casots (Vallès-Penedès Basin, Catalonia, Spain) are described. This sample fits well, both in size and occlusal morphology, with the material of Dorcatherium crassum from the type locality (Sansan, France; MN6). We therefore attribute the tragulid from Els Casots to this species, also in agreement with its known chronostratigraphic range throughout Europe (MN4–MN6) and the previous records of this species from other MN4 localities of the Vallès-Penedès Basin. The described remains – which include the postcanine lower deciduous and permanent dentition, as well as several upper cheek teeth – constitute the most complete sample of D. crassum from the Iberian Peninsula. The presence of this species at Els Casots is consistent with the lacustrine depositional environment inferred from sedimentological evidence and associated fauna, and further confirms the nearby presence of densely forested environments with a humid climate with low seasonality.     

Early Late Miocene insectivores (Eulipotyphla,Mammalia) from the Cañada section (Province of Zaragoza,east Central Spain)

Vallesian (early Late Miocene) strata from the recently introduced Cañada section (province of Zaragoza, east Central Spain) have yielded fairly large insectivore assemblages. These show that, after the generally dry Aragonian, the Vallesian gave rise to more humid conditions that were favourable to insectivores, both in number of taxa, and in overall number of specimens. The assemblage of Cañada 8 (Biozone H) is dominated by shrews, whereas the assemblage of Cañada 10 (uppermost Biozone H) contains the oldest record of Desmanella in the area. This seems to signify a bioevent in which after millions of years of absence, talpids return to the area. In addition to the Vallesian assemblages, a small Turolian insectivore fauna has been recovered. On the basis of the rodents, Cañada 12 was assigned to Biozone L, and the insectivore assemblage is very similar to the assemblages from the Teruel basin of that zone. This implies that the discovery of Postpalerinaceus in Cañada 12 is the youngest published record of this large spiny hedgehog.     

Palaeoenvironmental analysis of scleractinian reef corals from the Oligo–Miocene Qom Formation in the Vartun section (northeastern Esfahan,central Iran)

This paper presents a review of palaeoenvironmental reconstructions of scleractinian corals from the Oligo–Miocene Qom Formation in northeastern Esfahan, central Iran. A total of nine genera and four species of colonial corals are identified, including Platycoenia iranica, Goniopora sp., Porites sp., Tarbellastraea reussiana, Solenastrea sp., Favites neglecta, Leptoria sp., Hydnophora cf. pulchra, Hydnophora sp., and Madracis (?) sp. These corals, all parts of massive colonies, are indicative of a reefal environment, with the main constituents, including Leptoria and Hydnophora, possessing massive meandroid, massive hydnophoroid and massive mushroom- to dome-shaped hydnophoroid colonies. The corals identified here are generally indicative of the upper photic zone and shallow water depths of less than 20 m. In the reefal environment, these corals built a wave-resistant and rigid carbonate framework in the form of a reef-front zone encapsulated by environmental conditions including low sedimentation rates and high wave energy. The occurrence of Goniopora and Porites with distinct calicles reflects clearer waters in the external part of the reefal environment.