Significance of primate petrosal from Middle Eocene fissure-fillings at Shanghuang, Jiangsu Province, People's Republic of China

An isolated petrosal bone belonging to a diminutive primate is reported from Middle Eocene fissure-fills near Shanghuang (southern Jiangsu Province, People's Republic of China), the type locality of several newly described primates (Eosimias sinensis, a basal anthropoid; Adapoides troglodytes, a basal adapinan; Tarsius eocaenus, a congener of extant tarsiers; and Macrotarsius macrorhysis, the first Asian representative of an otherwise exclusively North American genus). Because of its fragmentary condition and unique combination of characters, the Shanghuang petrosal cannot be assigned unambiguously to any of the Shanghuang primate taxa known from dental remains. However, the possibility that the petrosal represents either an adapid or a tarsiid can be dismissed because it lacks defining basicranial apomorphines of these groups. By contrast, the element does present arterial features consistent with its being haplorhine. Deciding between the likeliest candidates for its allocation—Omomyidae and Eosimiidae—is difficult, in part because it is not known what (or even whether) basicranial characters can be used to distinguish these clades. If the Shanghuang petrosal is that of an cosimiid, as both direct and indirect evidence appears to indicate, the following implications emerge: (1) as long suspected on other grounds, anthropoids share a closer evolutionary history with Omomyidae (and Tarsiiformes) than they do with Adapidae (and Strepsirhini); (2) the specialised basicranial anatomy of extant anthropoids and their immediate cladistic relatives is derived from a primitive precursor whose otic morphology was like that of omomyids in most known respects; (3) the evolution of the defining dental and basicranial apomorphies of extant Anthropoidea has been distinctly mosaic in pattern.     

A new species of horseshoe bat of the genus Rhinolophus from China (Chiroptera: Rhinolophidae)

A new species of the Rhinolophus philippinensis group (Chiroptera: Rhinolophidae) is described from Guangdong, Guangxi, and Jiangxi Provinces in China. Rhinolophus huananus n. sp. is characterized by the horseshoe, as well as by external and cranial characteristics that separate it at the species level from the other members of the philippinensis group. One of the small species of the philippinensis group, R. huananus is intermediate in size between smaller R. siamensis and larger R. macrotis.     

Growth of horseshoe bats (Chiroptera: Rhinolophidae) in temperate continental conditions and the influence of climate

Growth characteristics of three species of horseshoe bats (Rhinolophus ferrumequinum, R. euryale and R. mehelyi) were studied in northern Bulgaria, and measurements of cohorts born there in different years were compared interannually. Bulgarian horseshoe bats are usually born in the first 3 weeks of June and start to leave the roost at an age of about 3 weeks. Young horseshoe bats of all three species had attained more than 95% of the adult dimensions at the time when they started to regularly leave the cave to forage on their own in mid of July. Individually marked juvenile R. ferrumequinum reached adult dimensions in most external wing measurements in the first half of August. Accordingly the pooled measurements of all juveniles did not differ anymore from those of adult bats in the second half of August. The same pattern was found in R. mehelyi and R. euryale.We found a clear relationship between the climatic conditions prevailing in each year and the final size of individuals born respectively in those years. Whereas previous studies have addressed climatic effects only on several bat species along their northern limits of distribution, these data provide the first evidence for an influence of climate on the growth of individuals in the centre of the species’ distributions.     

A new species of Rhinolophus (Chiroptera: Rhinolophidae) from China

A new species of the genus Rhinolophus is described from Yunnan Province, southwestern China. The new taxon belongs to the Rhinolophus "philippinensis-group" and is distinguished by differences in the nose-leaf structures, craniodental characteristics, and bacular features.     

中国大陆菊头蝠科一新纪录——单角菊头蝠(Rhinolophus monoceros Andersen,1905)

During a survey of bat species diversity from July 2008 to February 2009 in Songtao county of Guizhou Province, one specimen of Rhinolophus was collected from Guizhou. It was identified as a Formosan lesser horseshoe bat, based on the following features: small body size, forearm length of 36. 3mm, the greatest length of skull was 15.16 mm, the cells of lancet were shorter and appeared triangular and showed an acute angle, and forward bending, the lancet was shorter and approximately triangular and had a narrow top, the anterior median swellings of the skull were higher and more vertical, the rear of the sagittal crest was thin, the upper molars were shorter and the length of C~1 - M~3 was 5. 36 mm, the width of M~3 M~3 was 5.24 mm. Rhinolophus monoceros, which is new record in Guizhou and the first found on the Chinese mainland, supports Simmons' prediction that Rhinolophus monoceros may occur in the south of China.     

New hyaenodonta (Mammalia) from the middle Eocene of Myanmar

The middle Eocene Pondaung Formation in Myanmar has yielded a rich mammalian fauna including several Primate taxa. Hyaenodonta are known by the genera Kyawdawia, Yarshea, Orienspterodon, and two other indeterminate taxa. We describe here new material of Kyawdawia, including some morphological details, a new species of the hypercarnivorous genus Propterodon and an indeterminate species, different from those described earlier in Myanmar, and characterized by a reduction of m3 and would belong to a third lineage with the same evolutionary trend as Galecyon and the Limnocyoninae. The hyainailourines (Orienspterodon) and hyaenodontines (Propterodon) are recorded for the first time in Southeast Asia and these subfamilies appeared in quasi the same time in Europe illustrating probably a profound change in the carnivorous fauna among Laurasia.     

Phylogeography of the Japanese greater horseshoe bat Rhinolophus nippon (Mammalia: Chiroptera) in Northeast Asia: New insight into the monophyly of the Japanese populations

The Japanese greater horseshoe bat (Rhinolophus nippon) is distributed widely in East Asia. Within the species, R. nippon in Northeast Asia is regarded as the lineage that diverged most recently. However, the monophyly of the Japanese populations is unclear due to insufficient data about phylogenetic relationship of the western Japanese populations. To test the monophyly of the Japanese populations of R. nippon, we sampled R. nippon from western Japan and performed a phylogeographic analysis based on mitochondrial DNA cytochrome b and the D‐loop. The Northeast Asian lineage consisted of three main clades in eastern Japan (clade I), western Japan (clade II), and the continent as well as the Kumamoto population in westernmost Japan (clade III). The results of this study do not support the monophyly of the Japanese population. The findings suggest the “reverse colonization” of R. nippon from the Japanese Archipelago to the Eurasian continent, and provide important insight into the role of the island system in creation and supply of diversity to the continent.     

New primate hind limb elements from the middle Eocene of China

The continued washing, sorting, and identification of middle Eocene (45 Mya) primates from the Shanghuang fissure-fillings (Jiangsu Province, China) have produced additional hind limb elements. All are isolated elements. The strepsirhine hind limb elements include a first metatarsal and a talus, which are appropriate in size and morphology to pertain to Adapoides troglodytes. Adapoides is interpreted as a quadrupedal-climbing (nonleaping) primate with similarities to living lorises and the fossil primate Adapis. The haplorhine hind limb elements are estimated to span a range of adult body sizes from tiny (17 g) to small (200 g). Included among the new sample of haplorhine hind limb specimens is the smallest primate talus reported thus far. These new postcranial specimens expand our understanding of early haplorhine hind limb anatomy and demonstrate additional similarities between Shanghuang eosimiids and other anthropoids.     

New notharctine (primates,adapiformes) skull from the Uintan (middle Eocene) of San Diego County,California

A new genus and species of notharctine primate, Hesperolemur actius, is described from Uintan (middle Eocene) aged rocks of San Diego County, California. Hesperolemur differs from all previously described adapiforms in having the anterior third of the ectotympanic anulus fused to the internal lateral wall of the auditory bulla. In this feature Hesperolemur superficially resembles extant cheirogaleids. Hesperolemur also differs from previously known adapiforms in lacking bony canals that transmit the internal carotid artery through the tympanic cavity. Hesperolemur, like the later occurring North American cercamoniine Mahgarita stevensi, appears to have lacked a stapedial artery. Evidence from newly discovered skulls of Notharctus and Smilodectes, along with Hesperolemur, Mahgarita, and Adapis, indicates that the tympanic arterial circulatory pattern of these adapiforms is characterized by stapedial arteries that are smaller than promontory arteries, a feature shared with extant tarsiers and anthropoids and one of the characteristics often used to support the existence of a haplorhine-strepsirhine dichotomy among extant primates. The existence of such a dichotomy among Eocene primates is not supported by any compelling evidence. Hesperolemur is the latest occurring notharctine primate known from North America and is the only notharctine represented among a relatively diverse primate fauna from southern California. The coastal lowlands of southern California presumably served as a refuge area for primates during the middle and later Eocene as climates deteriorated in the continental interior. Hesperolemur probably was an immigrant taxon that entered California from either the northern (Wyoming/Utah) or southern (New Mexico) western interior during the middle Eocene © 1995 Wiley-Liss, Inc.     

The complete mitochondrial genome of the greater horseshoe bat subspecies, Rhinolophus ferrumequinum korai (Chiroptera: Rhinolophidae)

The total length of the mitogenome of Rhinolophus ferrumequinum korai is 16,839?bp with a total base composition of 31.8% A, 25.4% T, 28.7% C, and 14.0% G. The mitogenome consists of 13 protein-coding genes, 2 rRNA (12S and 16S RNA) genes, 22 tRNA genes, and 1 control region.     

广东五种菊头蝠的核型分析

本用蝙蝠的新鲜肺组织和尾椎进行组织培养,然后在光学显微镜下计数30个染色体分散良好的中期分裂相细胞,并进行摄影、剪贴和测量。分析了广东地区5种菊头蝠的核型,即小菊头蝠的核型为2n=62,FN=60;角菊头蝠的核型为2n=62,FN=60;中菊头蝠的核型为2n=62,FN=60;大耳菊头蝠的核型为2n=62,FN=60;中华(栗黄)菊头蝠的核型为2n=36,FN=60。大耳菊头蝠的核型为首次报道。角菊头蝠和中菊头蝠的核型与前人报道的结果基本相同。中华(栗黄)菊头蝠的核型(2n=36)与张维道报道的鲁氏菊头蝠相同,而与印度和斯里兰卡产R．rouxii的核型2n=56迥异。最后对东亚地区菊头蝠多样性进行了探讨。     

Approaches to the identification of ectoparasite complexes of bats (Chiroptera: Vespertilionidae,Miniopteridae, Rhinolophidae,Molossidae) in the Palaearctic

The first attempt at identifying the faunal complexes of ectoparasites of Palaearctic bats is presented. Several approaches are used to estimate the distribution and dynamics of parasitocenoses of different host taxa in both latitudinal and meridional directions. Our analysis shows that the arid temperate zone is characterized by the highest number of species and the greatest taxonomic richness of bat ectoparasites in the Palaearctic. The results obtained reflect the phylogeography of the Palaearctic bat families and tribes.     

Development of 19 polymorphic microsatellite loci for the intermediate horseshoe bat, Rhinolophus affinis (Rhinolophidae, Chiroptera)

The intermediate horseshoe bat (Rhinolophus affinis) is a widespread species in Southeast Asia. We developed 19 novel microsatellite loci from an enriched genomic library of the bat, and tested their polymorphism using a single population from Guangdong province, southern China. The number of alleles ranged from 3 to 15 per locus with the expected and observed heterozygosity ranging from 0.397 to 0.920 and 0.280–0.926, respectively. Three markers significantly deviated from the Hardy-Weinberg expectations after Bonferroni correction and no linkage disequilibrium was detected in any of loci. These microsatellite loci will be useful in studying the phylogeography of this species.     

A new basal tapiromorph (Perissodactyla, Mammalia) from the middle Eocene of Myanmar

A new genus and species of tapiromorph, Skopaiolophus burmese nov. gen., nov. sp., is described from the middle Eocene Pondaung Formation in central Myanmar. This small form displays a striking selenolophodont morphology associated with a mixture of primitive “condylarthran” dental characters and derived tapiromorph features. Skopaiolophus is here tentatively referred to a group of Asian tapiromorphs unknown so far. The occurrence of such a form in Pondaung suggests that primitive tapiromorphs might have persisted in southeast Asia until the late middle Eocene while they became extinct elsewhere in both Eurasia and North America.     

Characterization of 14 polymorphic microsatellite loci for the lesser horseshoe bat,Rhinolophus hipposideros (Rhinolophidae,Chiroptera)

Fourteen polymorphic microsatellites isolated in the lesser horseshoe bat, Rhinolophus hipposideros, are described. A subset of eight loci successfully coamplified in a multiplex polymerase chain reaction (PCR), and allowed to confirm that expected heterozygosity was relatively high for the eight loci (0.56–0.83). This set of eight microsatellites indeed permits to build genetic tags that distinguish all individuals in colonies consisting of up to more than 1000 individuals.     

New dipodid rodents from the Late Eocene of Erden Obo (Nei Mongol,China)

New dipodid occurrences (Heosminthus nomogenesis sp. nov., Sinosminthus sp., Allosminthus cf. A. majusculus, Allosminthus ernos and Allosminthus cf. A. diconjugatus) are reported from the ‘Upper Red’ beds of the Erden Obo section in Nei Mongol, China. Heosminthus nomogenesis is similar to Heosminthus primiveris from the Caijiachong Formation, and it is more primitive than Heosminthus chimidae of the Mongolian biozone A. Allosminthus cf. A. majusculus has a more variable mesolophid and metalophid in m1-2. Based on the dipodid assemblage, the age of the ‘Upper Red’ of the Erden Obo section is late Eocene and correlative to the Ergilian. Based on the comparison of their morphological characters, we recognize some differences between the stem dipodoids and muroids.     

A new anthropoid from the latest middle Eocene of Pondaung, central Myanmar

A new genus and species of medium-sized fossil primate, Myanmarpithecus yarshensis, is described from the lastest middle Eocene sediments of Pondaung, central Myanmar (Burma). The specimens consist of right maxillary fragments with P(4)-M(3)and a left mandibular corpus with C-P(3)and M(2-3). To date, three purported anthropoids have been discovered from the Pondaung Formation: Pondaungia and Amphipithecus (Amphipithecidae) and Bahinia (Eosimiidae). Myanmarpithecus differs from these other Pondaung primates in having cingular hypocones on upper molars and in lacking paraconids on M(2-3). Although Myanmarpithecus resembles some utahiin omomyines in superficial aspects of the morphology of M(2-3)(i.e., mesiodistally compressed molar trigonid and enamel crenulation), the morphological analysis of upper molars and lower premolars indicates that it is neither an omomyoid nor an adapoid but is more derived than fossil prosimians (such as adapoids, omomyoids, and tarsiers) and more anthropoid-like. On the other hand, it is more primitive (prosimian-like) than early anthropoids from the late Eocene/early Oligocene of the Fayum, Egypt. Myanmarpithecus is likely to be an early, primitive anthropoid ("protoanthropoid").     

Squamate reptiles from the middle Eocene of Lissieu (France). A landmark in the middle Eocene of Europe

In Europe, faunas of squamates (lizards and snakes) from the middle Eocene are very poorly known, with the exception of those from the level MP 16 (latest middle Eocene). From the MP 11-MP 15 interval, squamates were previously reported only from Messel (MP 11, earliest middle Eocene) and from the untere and obere Mittelkohle of Geiseltal (MP 12 and MP 13 respectively) in Germany. The present report describes the middle Eocene assemblage of squamates from Lissieu (France), the first fauna reported from the level MP 14. Whereas fossils from Messel and Geiseltal are mostly articulated skeletons, fossils from Lissieu are represented by disarticulated bones; such fossils may be more easily compared to those from other Cenozoic localities, in which bones are almost always disarticulated. The fauna from Lissieu is more diverse than those from the Geiseltal sites and approximately as diverse as that from Messel as they are presently known; it is comprised of 17 distinct taxa. These taxa cannot be all identified to the species or genus level. They belong to iguanids, gekkonids, lacertids, anguids, thecoglossan platynotans, ophidians incertaesedis, boids, ?tropidophiines, “tropidophiids” incertaesedis, booids incertaesedis, and perhaps russellophiids. The fauna includes several new taxa but only a presumed tropidophiine snake may be named on the basis of the available material. The fauna from Lissieu is a mixture of taxa restricted to the middle Eocene and taxa known from older or younger levels. Taxa shared by Lissieu and the few other localities from the middle Eocene of Europe are rare. This fauna from Lissieu represents a stratigraphical landmark for the middle Eocene.