Los mamíferos insulares del Mioceno medio y superior de Menorca (islas Baleares, Mediterráneo occidental)

The insular mammals from the karstic deposits of Punta Nati-2 and the marine beds of es Cul de sa Ferrada, placed in the northwest coast of Minorca (Balearic islands, Spain, western Mediterranean) are described in this work. One of the mammals (only present in Punta Nati-2) is a new glirid species, Margaritamys adroveri, closely related with Margaritamys llulli Mein and Adrover, 1982 and Pseudodryomys granatensis Agustí, 1993, from the middle Miocene of Santa Margalida and Sant Llorenç (Mallorca) and Murchas (Granada), respectively. M. adroveri shows more derived characters than P. granatensis and is more archaic than M. llulli, the size being similar to P. granatensis. The ochotonid present in Minorca is very similar to Gymnesicolagus gelaberti Mein and Adrover, 1982 from Mallorca. In the two minorcan deposits were recovered the first mandibles of this ochotonid, characterized by their big size. The medium weight (estimated from the length of the lower row) for G. aff. gelaberti is 5.4 kg, very similar to that some extant leporids like Lepus alleni Mearns, 1890 or Lepus arcticus Ross, 1819 and higher than any other living ochotonid. Doubtless, the big size of G. aff. gelaberti is a consequence of insular evolution, but not the short diastema, a primitive character shared with continental ochotonids and insular leporids. The discovery of a mandible in the marine beds of es Cul de sa Ferrada permits to place G. aff. gelaberti in the lower Tortonian, which represents the youngest record for this species with respect the faunal associations of Mallorca and Granada, Langhian-Serravalian in age (middle-upper Miocene). The fauna from Punta Nati-2 may represent an endemic association or a faunal group closely related to the fauna of Mallorca and Granada, but in an older context. The age of Gymnesicolagus and the presence of a similar fauna in Mallorca and Minorca suggest a connection between both islands during the Serravalian and the existence of an emerged area in Minorca after the Tortonian transgression.     

Late Paleozoic faunal, climatic, and geographic changes in the Baoshan block as a Gondwana-derived continental fragment in southwest China

The Carboniferous and Permian of the Baoshan block consist of three major depositional sequences: a Lower Carboniferous carbonate sequence, a Lower Permian siliciclastic sequence, and a Middle Permian carbonate sequence. These three sequences were interrupted by two major regressive events: first, the Namurian Uplift ranging in age from Serpukovian to Gzhelian, and second, the Post-Sakmarian Regression occurring probably at Artinskian time in the Baoshan block, although the precise time interval of the latter event is still unclear. The Baoshan block is characterized by warm-water, highly diverse and abundant faunas during the Early Carboniferous, by cold-water and low diversity faunas during the Early Permian, and by possibly warm-water but low diversity faunas during the Middle Permian. The Sweetognathus bucaramangus conodont fauna constrains the upper boundary of the diamictite-bearing siliciclastic deposits (Dingjiazhai Formation) to the Sakmarian to early Artinskian, as well as the eruption of the rifting basalts (Woniusi Formation) to, at least, the post-early Artinskian. Paleozoogeographically, affiliation of the faunas in the Baoshan block changed from Eurasian in the Early Carboniferous, to Peri-Gondwanan in the Early Permian, and to Marginal Cathaysian/Cimmerian in the Middle Permian. Cimmerian blocks have more or less comparable geohistory to one another in the Carboniferous and Permian. During the Middle Permian, the eastern Cimmerian blocks such as Sibumasu (s.s), Baoshan, and Tengchong are not far from the palaeoequator, but apparently more distant than the western Cimmerian blocks based on the presence or absence of some index taxa such as the fusulinaceans Eopolydiexodina and Neoschwagerina, and the corals Thomasiphyllum and Wentzellophyllum persicum.     

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.     

Comparative Ant Faunas between Seonyudo and Seven Other Islands of West Sea in Korea

ABSTRACT This paper is intended as an investigation of the biogeographic characteristics of ant faunas of the eight islands in West Sea of South Korea, using quantitative genetic analyses. The faunal similarity is examined using the Nomura-Simpson's Coefficient (NSC). The obtained NSC value matrix was examined by a cluster analysis using UPGMA method. The MSC-values between the seven areas investigated range from 0.500 (Deokjeokdo Hongdo) to 0.909 (Wonsando-Hongdo). In these islands including Seonyudo, the NSC -values range from 0.571 (Deokjeokdo) to 0.778 (Bigeumdo). The cluster analysis using the similarity index (NSC) showed that eight islands were divided into two groups at the level of 41%. It was shown that Wonsando and Bigeumdo were closer (Similarity = 83%) than those between others. Deokjeokdo and Bigeumdo were remote (Similarity = 41%) from each conspecific population. That is, the species composition of Bigeumdo (Similarity = 70%) was similar to that of the Seonyudo, while that of Deokjeokdo (Similarity = 41%) was different from that.