A partial skeleton of Prodeinotherium bavaricum (Proboscidea, Mammalia) from the Middle Miocene of Unterzolling (Upper Freshwater Molasse, Germany)

Here, a partial skeleton of Prodeinotherium bavaricum from Unterzolling (Southern Germany) is documented. The following elements are preserved and described for the first time: cervical vertebrae 1-2 and 5-7, the first thoracic vertebra, one lumbar vertebra, trapezium, metacarpals 1-5, tibia, calcaneus, endo- and mesocuneiform, cuboid, the fourth metatarsal, and some phalanges. Comparisons with the skeletons of P. bavaricum from Franzensbad (Czech Republic) and Deinotherium giganteum from Eserovo (Bulgaria) show osteological differences that are described and discussed.     

Late Miocene Proboscidea (Mammalia) from Macedonia and Samos Island, Greece: preliminary results

The abundant Late Miocene proboscidean remains of Greece have never been studied in detail and compared with those of Eurasia in order to determine their taxonomy and their biostratigraphical and palaeoecological significance. The first results of such study are given in this article. During the past decades, several new proboscidean specimens have been added to the old collections, significantly enriching the available material. The Axios Valley (Macedonia, Greece) proboscidean fossils belong mainly to two species of Choerolophodon: C. anatolicus of early Vallesian age and C. pentelici of late Vallesian–Turolian age. Deinotherium giganteum is rare and recognized only in the late Vallesian locality Ravin de la Pluie of Axios Valley. A zygodont form has also been identified in the Turolian of Axios Valley, attributed to “Mammut” sp. The Late Miocene localities of Nikiti (Macedonia, Greece) revealed several remains of C. pentelici, which are similar to the Turolian ones of Axios Valley. The Samos proboscidean collection includes C. pentelici, “Tetralophodon” atticus, “Mammut” sp. and Deinotherium gigantissimum. The taxonomy of the Late Miocene peri-Mediterranean Choerolophodon is given, and the biostratigraphy and palaeoecology of the Greek Late Miocene proboscideans are discussed.     

Cranial and dental remains of Deinotherium bozasi (Mammalia: Proboscidea) from East Rudolf, Kenya

A skull, three immature mandibles and a number of isolated teeth belonging to Deinotherium bozasi have been collected from Plio-Pleistocene sediments to the east of Lake Rudolf, Kenya. D. bozasi is the youngest representative of the family Deinotheriidae and the skull is the most complete yet found of this taxon. The East Rudolf specimens are contrasted with comparable specimens of Prodeinotherium hobleyi from East and North Africa and of Deinotherium giganteum from Europe. The size and morphology of the cranial vault of the East Rudolf skull confirms allocation to the genus Deinotherium but other dental and cranial evidence confirms taxonomic differentiation from D. giganteum and direct descent from P. hobleyi. Although the postcranial elements of D. bozasi are poorly known it is considered unlikely that this species developed the cursorial adaptations of D. giganteum. The extinction of D. bozasi is attributable to major changes in ecologic conditions towards the end of the early Pleistocene.     

Evolution of feeding mechanisms in the family Deinotheriidae (Mammalia: Proboscidea)

The fossil record of the extinct family Deinotheriidae is restricted to Neogene and early Quaternary faunas of the Old World. The family is assigned to the Order Proboscidae but the nature of its relationship to other proboscidean families is still uncertain. Deinotheres are rendered unique by the retention of a single pair of lower tusks and by the morphology of the cheekteeth.
The earliest recorded deinotheres exhibiteo morphological adaptations for a proboscis. In terms of length and prehensibility, the proboscises of the early deinotheres were more tapir-like than elephantine. Later representatives had larger and more powerful but not necessarily longer proboscises.
It is unlikely that the tusks were used for digging and the most probable functions were for stripping vegetation, for providing a source of purchase for the proboscis, and in providing a means of recognition of the individual.
The cheek teeth were deployed in two distinct functional batteries: an anterior crushing battery and a posterior shearing battery. The anterior molar acted initially as part of the shearing battery but, on becoming worn, subscribed to the crushing function of the anterior battery.
Deinotheres were shearing browsers and replaced barytheres in the African Paleogene faunas. Evolutionary trends in the known representatives afford some indication of the nature of pre-Miocene adaptations.     

The beaver (Mammalia,Castoridae) from the Miocene of Sandelzhausen (southern Germany)

The Early/Middle Miocene boundary locality Sandelzhausen (MN5, southern Germany) yielded three beaver teeth: one lower incisor fragment and two strongly worn upper premolars, a right and a left one. The latter are so similar in wear, height, size, and enamel pattern that they probably represent one individual. Although the teeth have been referred to Chalicomys jaegeri Kaup, 1832 (e.g., Hugueney 1999, Fahlbusch 2003), it seems more likely that they belong to Steneofiber depereti Mayet, 1908. However, the assignment of the present material to either one of these species is difficult, because in the advanced wear stage some diagnostic characteristics cannot be assessed. As to ecological implications for the locality Sandelzhausen the taxonomic identity of these two beaver species may not be important. Both are known from riverine, lacustrine or swamp sediments, and it can be assumed that they usually lived in close vicinity to water. Thus, the presence of beaver remains supports the presence of water at Sandelzhausen. However, the teeth might have an allochthonous origin from creeks of the rising Alps.      

The South American Gomphotheres (Mammalia, Proboscidea, Gomphotheriidae): Taxonomy, Phylogeny, and Biogeography

The taxonomic history of South American Gomphotheriidae is very complex and controversial. Three species are currently recognized: Amahuacatherium peruvium, Cuvieronius hyodon, and Notiomastodon platensis. The former is a late Miocene gomphothere whose validity has been questioned by several authors. The other two, C. hyodon and N. platensis, are Quaternary taxa in South America, and they have distinct biogeographic patterns: Andean and lowland distributions, respectively. South American gomphotheres became extinct at the end of the Pleistocene. We conducted a phylogenetic analysis of Proboscidea including the South American Quaternary gomphotheres, which resulted in two most parsimonious trees. Our results support a paraphyletic Gomphotheriidae and a monophyletic South American gomphothere lineage: C. hyodon and N. platensis. The late Miocene gomphothere record in Peru, Amahuacatherium peruvium, seems to be a crucial part of the biogeography and evolution of the South American gomphotheres.     

Mitochondrial cytochrome b of the Lyakhov mammoth (Proboscidea,Mammalia): new data and phylogenetic analyses of Elephantidae

The phylogenetic relationships between recent Elephantidae (Proboscidea, Mammalia), that is to say extant elephants (Asian and African) and extinct woolly mammoth, have remained unclear to date. The prevailing morphological scheme (mammoth grouped with Asian elephant) is either supported or questioned by the molecular results. Recently, the monophyly of woolly mammoths on mitochondrial grounds has been demonstrated (Thomas, et al., 2000), but it conflicts with previous studies (Barriel et al., 1999; Derenko et al., 1997). Here, we report the partial sequencing of two mitochondrial genes: 128 bp of 12S rDNA and 561 bp of cytochrome b for the Lyakhov mammoth, a 49,000-year-old Siberian individual. We use the most comprehensive sample of mammoth (11 sequences) to determine whether the sequences achieved by former studies were congruent or not. The monophyly of a major subset of mammoths sequences (including ours) is recovered. Such a result is assumed to be a good criterion for ascertaining the origin of ancient DNA. Our sequence is incongruent with that of Yang et al. (1996), though obtained for the same individual. As far as the latter sequence is concerned, a contamination by non-identified exogenous DNA is suspected. The robustness and reliability of the sister group relation between Mammuthus primigenius and Loxodonta africana are examined: down-weighting saturated substitutions has no impact on the topology; analyzing data partitions proves that the support of this clade can be assigned to the most conservative phylogenetic signal; insufficient taxonomic and/or characters sampling contributed to former discordant conclusions. We therefore assume the monophyly of "real mammoth sequences" and the (Mammuthus, Loxodonta) clade.     

Chromosome painting among Proboscidea, Hyracoidea and Sirenia: support for Paenungulata (Afrotheria, Mammalia) but not Tethytheria

Despite marked improvements in the interpretation of systematic relationships within Eutheria, particular nodes, including Paenungulata (Hyracoidea, Sirenia and Proboscidea), remain ambiguous. The combination of a rapid radiation, a deep divergence and an extensive morphological diversification has resulted in a limited phylogenetic signal confounding resolution within this clade both at the morphological and nucleotide levels. Cross-species chromosome painting was used to delineate regions of homology between Loxodonta africana (2n=56), Procavia capensis (2n=54), Trichechus manatus latirostris (2n=48) and an outgroup taxon, the aardvark (Orycteropus afer, 2n=20). Changes specific to each lineage were identified and although the presence of a minimum of 11 synapomorphies confirmed the monophyly of Paenungulata, no change characterizing intrapaenungulate relationships was evident. The reconstruction of an ancestral paenungulate karyotype and the estimation of rates of chromosomal evolution indicate a reduced rate of genomic repatterning following the paenungulate radiation. In comparison to data available for other mammalian taxa, the paenungulate rate of chromosomal evolution is slow to moderate. As a consequence, the absence of a chromosomal character uniting two paenungulates (at the level of resolution characterized in this study) may be due to a reduced rate of chromosomal change relative to the length of time separating successive divergence events.     

Skeleton of the giant deer Megaloceros giganteus giganteus (Blumenbach, 1803) (Mammalia,Artiodactyla) from the Irtysh Region near Pavlodar

An almost complete skeleton of the giant deer Megaloceros giganteus giganteus (Blumenbach, 1803) from the Dzhambul locality on the Irtysh River (Pavlodar Region, Kazakhstan) is described. About 80% of bones are intact, including the skull with well-preserved antlers. At present, the skeleton is mounted in the Pavlodar Local History Regional Museum. Comparative analysis of giant deer skulls varying in age from the southeastern West Siberian Plain has revealed stable characters distinguishing Middle and Late Neopleistocene specimens. These characteristics are considered to be of subspecies rank, allowing the identification of Megaloceros giganteus ruffi Nehring and Megaloceros giganteus giganteus (Blumenbach.) Changes in absolute and relative dimensions of the dentition and facial skull length are most indicative with reference to evolution.     

On the phylogenetic position of monotremes (Mammalia,Monotremata)

Henosferida from the Middle-Upper Jurassic of Western Gondwana is the most probable sister group for monotremes. They share the derived pretribosphenic structure of lower molars combined with the presumably absent protocone on the upper molars and the plesiomorphic retention of postdentary bones and pseudangular process of the lower jaw. In addition, the two groups share the dental formula with three molars and the position of the Meckel’s groove, which passes ventral to the mandibular foramen. In the course of subsequent evolution, monotremes acquired the mammalian middle ear with three auditory ossicles independently of therian mammals and multituberculates. Jurassic Laurasian Shuotheriidae are probably a sister group of the Gondwanian clade Henosferida + Monotremata. The Jurassic shuotheriid Pseudotribos shows a great plesiomorphic similarity to monotremes in the structure of the pectoral girdle, with a large interclavicle immovably connected to the clavicle. In the lineages leading to therian mammals and multituberculates, the pectoral girdle changed probably independently and in parallel in connection with the establishment of the parasagittal posture of the forelimbs (reduction of the interclavicle, mobile articulation of the interclavicle with clavicle, reduction of the procoracoid, and development of a supraspinous fossa of the scapula) and formation of the mammalian middle ear with three auditory ossicles.     

A new species of Proboscidea (Martyniaceae) from Mexico

Proboscidea diversifolia is described, the type being from Michoacan. The species, which appears most similar toP. triloba (Cham. & Schlecht.) Decne., is apparently restricted to the vicinity of Apatzingan.     

Feeding preferences of <Emphasis Type="Italic">Gomphotherium subtapiroideum</Emphasis> (Proboscidea,Mammalia) from the Miocene of Sandelzhausen (Northern Alpine Foreland Basin,southern Germany) through life and geological time: evidence from dental microwear analysis

The objective of this study is to estimate changes in feeding preferences of the proboscidean species Gomphotherium subtapiroideum (Schlesinger 1917) by means of dental microwear analyses. The dietary changes are first evaluated through the ontogeny of this species, between juveniles and adults, and are then studied through geological time, from early Middle Miocene (MN5) to middle Late Miocene (MN8–9) localities of the German Molasse Basin. The microwear patterns of juvenile and adult individuals of G. subtapiroideum from Sandelzhausen (MN5) differ merely by the variable “length of scratches”, emphasizing longer jaw movements during mastication in adults. The microwear signatures of G. subtapiroideum do not vary significantly between the two geological time periods studied, but reflect mixed feeding preferences in both cases. These results imply that, despite an important environmental change at that time (drying and opening), the ecology of G. subtapiroideum and, especially, its feeding habits were not affected. Its dental microwear pattern is then compared with those of other species of Proboscidea from the Middle-Late Miocene of Germany, namely Deinotherium giganteum and Gomphotherium steinheimense.     

The status of Mastodon angustidens pygmaeus Depéret, 1897 (Proboscidea,Mammalia): The contribution of X-ray tomography

The status of Mastodon angustidens pygmaeus Depéret, 1897 is discussed on the basis of an examination of the holotype (a broken lower molar) with tomography using X-rays, and on a review of the previous taxonomic hypotheses. The conclusion is that the holotype is a possible supernumerary post-m3 molar that may be that of a tetralophodont gomphothere. “M. angustidens pygmaeus” is then a nomen dubium that should only be used in relation to the holotype.     

On the phylogeny and zoogeography of the leptarctines (Carnivora,Mammalia)

A restudy of the skull and mandible ofLeptarctus neimenguensis Zhai from the Middle Miocene of China and the preparation of its auditory region led to the recognition of new features. The most important among them is the presence of a small suprameatal fossa partly hidden in the bony mastoid process corresponding to the structure described inPlesiogale andParagale (Schmidt-Kittler 1981) and representing the most primitive type of the mustelid middle ear. A detailed comparison of the dentition revealed thatTrocharion albanense Major from the European Miocene is closely related toLeptarctus so that is has to be included in the leptarctines. On the basis of special synapomorphies, the Mustelidae can be devided in two (holo-) monophyletic subunits of the next lower level: The first group is represented by the leptarctines (includingTrocharion), whereas the second group comprises all Recent mustelids and its forerunners. The splitting of these groups must have taken place still before the end of the Oligocene. On various grounds it is argued the leptarctines are of Eurasian origin.     

Caprinae (Bovidae,Artiodactyla, Mammalia) from the Neogene of Mongolia

Gobiocerus mongolicus Sokolov, 1952, Turcocerus kekemaidengensis Ye Jie et al., 1999; and Hypsodontus sp. were recorded in Miocene deposits of the Valley of Lakes (MN4-MN8) and Oioceros atropatenes (Rodler et Weithofer, 1890) occurred in the Mio-Pliocene (MN11-MN20) of northwestern Mongolia. Gobiocerus, Turcocerus, and Hypsodontus represent the same evolutionary lineage. Thus, Caprinae existed in Central Asia in the Early Miocene. They diverged from the Bovidae at the Oligocene-Miocene boundary. The presence of early bovids in this region suggests that this group could have appeared in Central Asia.     

Bats (Chiroptera, Mammalia) from Middle Miocene karstic fissure fillings of Petersbuch near Eichstätt, Southern Franconian Alb (Bavaria)

The bats from the karstic fissure fill sites Petersbuch 6, 10, 18, 31, 35 and 48 include 14 species, four of which are new. All samples are numerically dominated by rhinolophids, especially by Rhinolophus delphinensis. The rich samples from Petersbuch 6-18 are striking in their high species diversity (seven species each). Myotis bavaricus nov. sp. is characterised by a series of plesiomorphous characters, while Myotis reductus nov. sp. is more derived. A special trait of Submyotodon petersbuchensis nov. gen. nov. sp. is the coexistence of nyctalodont and (sub-) myotodont molars in one dentary. Miniopterus rummeli nov. sp. is characterised by its large size, a high coronoid process and its widely spaced lower premolars. Composition and origin of the chiropteran faunas are discussed. They are interpreted as an accumulation of bats that perished in the cave or rock crevice and to a negligible extent as remains of owl pellets. The stratigraphic correlation of the faunas, based on rodents, is late Middle Miocene (MN 7/8). This study is based on several thousand specimens.