Neogene–Quaternary Mammalian Paleobiogeography of the Indian Subcontinent: An appraisal

A biostratigraphic evaluation of the Indian subcontinent Neogene–Quaternary mammal genera at 1 Ma intervals reveals a strong correlation between faunal turnovers (first and last appearances and immigrations), diversity and major tectonic and climate-induced sea level and vegetation changes at 23–22, 20–18, 17–16, 15–14, 11–10, 9–8, 3–2 and 1–0 Ma. The Early Miocene collision of Afro-Arabian and Eurasian Plates, followed by the Middle Miocene Climate Optima and the presence of evergreen rainforests, most likely facilitated the dispersals into and out of the subcontinent from the west along the coast and included African proboscideans, primates, creodonts, thryonomyid rodents and Asian chalicotheres, rhinos, suids, anthracotheres, carnivores and muroid rodents. The Late Miocene and Early Pleistocene cooler and drier conditions, the spread of grasslands and sea level drops may have influenced the exchange of African monkeys, Eurasian carnivores, bovids, equids, camelid, and South Asian suids, leporids and murids. Immigrations from the east (East and SE Asia) occurred mostly during the Miocene and involved primarily small mammals.     

Plio-pleistocene mammals from Gidhniya village Western Nepal

Recently collected vertebrate fossils from the Himalayanfoothills of western Nepal comprise the first diverse Plio-Pleistocene mammal assemblage known from Nepal. Specimens representing Stegodon insignis, Elephas planifrons, Equus sivalensis, Hexaprotodon sivalensis, Cervus sp., and two taxa of bovids are present in this collection from Gidhniya Village. The Gidhniya assemblage is biostratigraphically correlated with the «Pinjor fauna of India and Pakistan; it is between 1.5 and 2.9 million years old.     

Siwalik synopsis: A long stratigraphic sequence for the Later Cenozoic of South Asia

The Tertiary sediments of northern Pakistan are an exceptional record of terrestrial sedimentation and represent most of Neogene time. Foremost is the Siwalik Group of the Potwar Plateau, for which multiple, superposed fossil levels span ∼18–6 Ma. Well-developed magnetostratigraphic control provides secure dating so that Siwalik fossil horizons may be interpolated into a time scale with resolution to 100,000 years. We describe the geographic setting of the Potwar, give an overview of the temporal distribution of faunas, and discuss changes in paleohabitat and paleoecology with coinciding faunal change, as seen from the Siwalik viewpoint. The long Siwalik biostratigraphy of many successive assemblages with its resolved time scale may be compared directly with other well-dated sequences. Immigrant arrival and timing of faunal change may be traced. The basins of the Iberian Peninsula show somewhat different timing of introduction of hipparionine horses, and faunal turnover in the Siwaliks clearly precedes the Vallesian crisis in Spain. In contrast to the increasingly seasonal precipitation of the late Miocene Potwar, the paleohabitat of coeval North China appears to have been moist and equable, with high diversity faunas. Continued development and comparison of resolved Neogene records allow increasing resolution of the patterns of faunal change on regional to global levels.     

A new genus (Chardinomys) of murid rodent (Mammalia,Rodentia) from the neogene of China,and comments on its biogeography

Three murid specimens from the late Neogene ofChina are described, one as the new taxon Chardinomys, which is most closely related to Orientalomys. The Orientalomys-Chardinomys complex was widely distributed over the Palearctic region during the late Neogene. Cf. Rattus occurring with the Orientalomys-Chardinomys complex in China suggests South Asian influence in the eastern Palearctic during the late Neogene.     

Biogeography and chronology of the Eurasian extinct rhinoceros Stephanorhinus etruscus (Mammalia,Rhinocerotidae)

Stephanorhinus etruscus is one of the most abundantly recorded and better known Eurasian Early Pleistocene rhinoceroses. Nevertheless, the first and last appearances of this species, as well as its paleogeographic distribution, are controversial and debated in literature. S. etruscus is documented since the latest Pliocene in Spain (Las Higueruelas), Italy (Montopoli and Castelnuovo di Barardenga), France (Perrier–Les Étouaires) and Romania (Iar??–Cariera Veche). During the Early Pleistocene, S. etruscus occurred in several Spanish, French and Italian localities, as well as in The Netherlands (e.g., Tegelen), Germany (e.g., Thiede), Greece (e.g., Aivaliki) and Israel (e.g., Ubeidiya). The last appearance of S. etruscus in Eurasia is debatable. Etruscan rhino populations survived till the Jaramillo subchrone (around 1.1 Ma) in France (Bois-de-Riquet), Romania (Betfia XII) and Hungary (Osztramos 2 and 8), and close to the early–middle Pleistocene transition in Spain (Cueva Victoria, Huéscar 1, Atapuerca TD4, TD6 and TD8), and Italy (Monte delle Piche).     

Fossil record and dynamics of Late Miocene small mammal faunas of the Vienna Basin and adjacent basins,Austria

The Late Miocene small mammal assemblages of the hinterland of Lake Pannon in Austrian Basins are represented by 99 species-level taxa and 30,400 specimens. The fossil-bearing localities can be grouped into eight intervals spanning about three million years from the Early Vallesian to the Middle Turolian. Each time slice is characterised by the occurrence and/or dominance of certain species. The retreat of Lake Pannon is reflected by a distinct diversification. This pattern may be a regional signal due to increasing habitat availability but may also be taphonomically biased due to a rather poor Earliest Vallesian record. Nevertheless, the overall community structure is quite stable throughout the Vallesian and no indication of a Vallesian Crisis can be detected. Instead, a moderate turnover occurs with the onset of the Turolian, reflected by the increasing abundance of xerophilic taxa.     

Potamotrygon marinae n. sp., a new species of freshwater stingrays from French Guiana (Myliobatiformes, Potamotrygonidae)

Six specimens of freshwater stingrays from the French Guiana belonging to the genus Potamotrygon [S.W. Garman, On the pelvis and external sexual organs of selachians, with special reference to the new genera Potamotrygon and Disceus, Proc. Bost. Soc. nat. Hist. 19 (1877) 197-215], do not present characters that are typically shown by species to which they have been attributed. Five belong to a new species here named Potamotrygon marinae n. sp. This species is differentiated from the others by the feebly development of the prepelvic process, the development of the postorbital process as an enlarged blade, the unsegmented angular cartilage, the dorsal surface coloration composed of wide circular patches themselves formed by smaller pale patches, the almost dark coloration of the ventral surface tessellated with pale patches, and the small sized spiny tubercles situated in the middorsal region, before the caudal sting.     

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.     

First mammal species identified from the Upper Cretaceous of the Rusca Montană Basin (Transylvania,Romania)

Multituberculate mammals are scarce in the Late Cretaceous of Europe, being recorded exclusively from the Maastrichtian terrestrial deposits of the Ha?eg and Transylvanian basins, in Romania. Moreover, they all belong to the endemic and primitive cimolodontan family Kogaionidae. Here, we report multituberculate teeth originating from the Maastrichtian fluviatile sediments of the Rusca Montan? Basin (Occidental Carpathians, Poiana Rusc? Mountains). This is the westernmost occurrence of these Cretaceous mammals in Romania. These teeth are assigned to Barbatodon oardaensis, the smallest Cretaceous kogaionid species. This study presents the first occurrence of this species outside the Metaliferi sedimentary area (southwestern Transylvania, Romania). The distribution of Romanian Maastrichtian kogaionids is also discussed.     

Lithostratigraphic context of Oligocene mammalian faunas from Ulantatal,Nei Mongol,China

The Ulantatal area is well-known for its extraordinarily rich Oligocene mammalian fossils. The Ulantatal fauna was originally considered to be the representative fauna for the Chinese Land mammalian Age, Ulantatalian. However, the abundant fossils collected in the 1980s lack coordinates and/or detailed stratigraphic levels, and have been lumped together as either single, coeval fauna or grouped into three units. This lack of stratigraphic information hampers more precise biostratigraphic division and correlation of the faunas. Here we present a complete lithostratigraphic profile of the Ulantatal Formation with new fossil localities calibrated into the profile. Lithologically, the sequence shows a rather uniform pattern characterized by interbedded reddish to yellowish brown claystones and siltstones, with minor fine-grained sandstones. Preliminary biostratigraphic analysis shows that the Ulantatal Formation covers most of the Oligocene, and offers a long sequence and successive fossil records for understanding the evolution of mammal faunas after the critical Eocene/Oligocene transition.     

Prominatherium dalmatinum from the late Eocene of Grancona (Vicenza,NE Italy). The oldest terrestrial mammal of the Italian peninsula

So far, the oldest terrestrial mammal associations in Italy dates to the beginning of the Oligocene, with Anthracotheriidae being the most represented taxon. Sites from northern Italy yielded remains of the genus Anthracotherium that spread from Asia to western Europe after the Grande Coupure. A finding at Grancona, which is Priabonian in age, implies that Anthracotheriidae family reached the Italian Peninsula before the Eocene–Oligocene boundary. Thus, the dispersal of this family in northern Italy is anterior than previously believed. The fossil consists of a poorly preserved right hemi-maxilla with well-preserved P4 and M3. The shape and the size of the teeth are not compatible with the genus Anthracotherium. On the contrary, the closer affinities with the Croatian species Prominatherium dalmatinum suggest a connection between the Balkan area and the Italian peninsula and a possible new way of dispersal for this family.     

Armored dinosaurs(Ornithischia: Ankylosauria)) from the Middle and Upper Jurassic of England

Hitherto the earliest positive record of ankylosaurs(armored dinosaurs) has been from beds well up in the Lower Cretaceous; in fact, however, specimens referable to the ankylosaurian family Nodosauridae are present in the Middle and Upper Jurassic of England: from the Middle Callovian [partial mandible Sarcolestes leedsiLydekker]], the Upper Oxfordian [femur Cryptodraco eumerus (Seeley)), maxilla Priodontognathus phillipsii (Seeley))], and the Upper Tithonian [caudal vertebra, tooth]. The Tithonian tooth and those of Priodontognathus are large and similar to those of the nodosaurids Priconodon and Sauropelta (Lower Cretaceous, U.S.A.). The incomplete mandible of Sarcolestes is similar to that of Sauropelta with a dermal scute fused to the lateral surface, and a tooth row extending to the anterior end of the jaw; an unusual feature is the caniniform first tooth. The quadrupedal ankylosaurs and stegosaurs probably represent separate evolutionary lines that extend back at least into the Lower Jurassic, and both lines probably evolved from ornithopod dinosaurs that were bipedal. Nodosaurid ankylosaurs occur in Europe from the Middle Jurassic to Late Cretaceous and probably reached North America via a filter route in the early Cretaceous.     

Cold-climate rodent indicators for the Late Pleistocene of Central Iberia: New data from the Buena Pinta Cave (Pinilla del Valle,Madrid Region,Spain)

In the Iberian Peninsula, the Late Pleistocene record of small mammal indicators of cold climates is largely restricted to two sets of sites at the eastern and western ends of the Pyrenees. Some assemblages from other sites at the Peninsular centre have, however, recently yielded such taxa. This work describes the remains of three such rodent species from the Buena Pinta Cave, a site in the Sierra de Guadarrama mountains in the Spanish Central System. Excavation campaigns in the cave have taken place every summer since 2003. Thermoluminescence analyses of sediments from levels 2–5 of the site suggest an age corresponding to the middle of the Late Pleistocene, within Marine Isotope Stage 4 or the beginning of Marine Isotope Stage 3. Sieve-washing and picking out of the small fossils contained in the sediments of levels 2–5 yielded several thousand small mammal teeth and other remains, dominated by Microtus arvalis. Smaller numbers of remains belonging to other rodents typical of cold climates were also identified, such as Microtus oeconomus, Microtus gregalis and Chionomys nivalis. Thus, the small mammal record of the Buena Pinta Cave shows that rodent indicators of cold climates reached the centre of the Iberian Peninsula during the mid-Late Pleistocene, i.e., well before the Last Glacial Maximum. These findings represent one of the southernmost Pleistocene records for M. oeconomus in Europe, and the most southerly for M. gregalis.     

A numerical simulation for the dynamics of the sexual phase of monogonont rotifera

A numerical simulation for the dynamics of a model that describes the sexual phase of Monogonont Rotifera reproduction is presented. The simulation is carried out by means of a numerical method based on the integration along the characteristic curves. The numerical experiments cover two basic situations: the existence of an asymptotic stable equilibrium state and the existence of an stable periodic solution. Our results are in agreement with the theoretical analysis made by Calsina and Ripoll (J. Math. Biol. 45 (2002) 22).     

Le paléoplancton des Grès de Landévennec (Gedinnien de la rade de Brest — Finistère) étude biostratigraphique

In the Gedinnian Landévennec Sandstones Formation(Rade de Brest, Finistère, Massif Armoricain), rich and well-preserved assemblages of organic-walled microplancton were observed. In the Lanvéoc section, worked out bed after bed, fifty-five species of this organic-walled microphytoplancton of uncertain algal affinity and Prasinophyceae are described. Four genera and fifteen species are new in this total. The assemblage shows many relationship to others gedinnian microplancton from Europa. Africa and United States of America.