Pleistocene foxes (Vulpes,Canidae, Carnivora) from the Taurida Cave,Crimea

Doklady Biological Sciences - A mandible fragment and four isolated teeth of the fossil foxes, Vulpes alopecoides (Del Campana, 1913), Vulpes cf. vulpes (Linnaeus, 1758) and Vulpes sp., are...     

Early Pleistocene Lynx issiodorensis (Felidae,Carnivora) from the Taurida Cave,Crimea

Doklady Biological Sciences - The cranial and mandibular remains of two adult individuals of Lynx issiodorensis (Croizet et Jobert, 1828) are described from the Early Pleistocene locality of the...     

Early Pleistocene Spiral-Horned Antelopes (Artiodactyla,Bovidae) from the Taurida Cave (Crimea,Russia)

Paleontological Journal - The article describes fossil remains of two spiral-horned antelope species Gazellospira torticornis (Aymard, 1854) and Pontoceros ambiguus Vereschagin, Alexejeva, David et...     

Megantereon adroveri from the Early Pleistocene of Taurida Cave,Crimea, and the European Lineage of Dirk-toothed Cats

Recent field surveys performed in the newly-discovered Taurida Cave (Crimea, Russia, Late Villafranchian, 1.8–1.5 Ma) enabled us to unearth dentognathic remains of the dirk-toothed cat Megantereon. Here we describe in detail the recovered remains further comparing it anatomically and biometrically with coeval Eurasian and African sites. The performed analysis suggests the inclusion of the Taurida remains in the hypodigm of the Villafranchain European species Megantereon adroveri, a medium-sized saber-toothed cat poorly known in Europe as a consequence of the scarcity and fragmentary nature of the known remains. Our results and the putative transitional characters displayed by the Taurida specimen support the idea put forward by previous authors of a continuous European lineage of dirk-toothed cats.

     

The Large Porcupine Hystrix refossa (Rodentia,Hystricidae) from the Early Pleistocene Taurida Locality in Crimea

Doklady Biological Sciences - The remains of large porcupines (an incomplete skull, cranial and mandibular fragments, isolated teeth and postcranial bones) from the Early Pleistocene Taurida cave...     

Early Pleistocene White-toothed Shrew Crocidura kornfeldi (Lipotyphla,Soricidae) from Crimea

Doklady Biological Sciences - The remains of the white-toothed shrew Crocidura kornfeldi Kormos, 1934 (one skull fragment with almost complete dentition, the fragmental rostral part of a skull with...     

Mammalian Carnivore Coprolites from the Sopas Formation (Upper Pleistocene,Lujanian Stage), Uruguay

Continental tetrapod coprolites from Uruguay are described for the first time. These remains come from the Piedra Pintada locality (Artigas Department), northern Uruguay, where the Sopas Formation crops out (Upper Pleistocene, Lujanian Stage). It was possible to identify several attributes indicative of a coprolitic origin, such as anisopolar shape, extrusion marks, pointed ends, sutures, gas bubbles, and inclusions. These specimens are assigned to carnivorous mammals, probably large felids, based on morphological attributes and inclusions of rodent bones and teeth.     

湖北郧西白龙洞古人类遗址的大额牛化石

牛亚科动物在中国第四纪古人类遗址中十分常见,但其分类和鉴定仍存在诸多问题。南方洞穴动物群经常仅有单个牙齿保存,所以南方更新世洞穴遗址中牛亚科动物化石鉴别问题更为突出。湖北郧西白龙洞古人类遗址出土的大型牛亚科动物化石,不仅有大量单个牙齿,还有残破颅骨、角心、下颌骨及头后骨骼。白龙洞的牛亚科动物角心粗短、横截面呈背腹略扁的椭圆形;额骨上的角间隆突发育且呈拱形;顶骨从颅顶退出;枕面较圆且高;角后颅骨收缩强烈使得枕骨上部变窄,颞窝明显凹进;下颌角大于90°,下颌支向后倾斜;下颌p2的结构复杂程度介于水牛Bubalus和黄牛Bos(Bos)taurus之间。依据上述特征,可将白龙洞的大型牛亚科动物化石归入大额牛Bos(Bibos)gaurus。白龙洞是我国出土大额牛化石最为丰富的古人类遗址,为区分南方洞穴出土的牛亚科动物化石提供了重要材料。     

Pachycrocuta (hyaenids) from the Pliocene of east Africa

Hyaenas belonging to the genusPachycrocuta were the largest hyaenas known. They had a wide distribution in the Plio-Pleistocene, having been found throughout Eurasia and in South Africa. The genus has been reported several times from east Africa, but these finds have been poorly documented. I here describe newly identified specimens ofPachycrocuta from the Turkana Basin, Kenya. It is concluded that although there are certain differences between east and South African specimens, these are of a nature that can be explained by individual variation, and therefore all African specimens are assigned to the Eurasian speciesPachycrocuta brevirostris. The migration patterns of the species are discussed and although these are still equivocal, I speculate that the species originated in Asia and migrated from there to Africa ca. 3.5 Ma and to Europe ca. 1.6 Ma.     

Microbial Biomineralization in Biotic Crusts from a Pleistocene Marine Cave (NW Sicily,Italy)

Biotic crusts occurring in the Early Pleistocene Rumena Cave, in NW Sicily, have been analyzed from a geomicrobiological point of view. The crusts consist largely of scleractinians and of subordinate bryozoans and serpuloideans, all typical of submarine cave biota. Encrustations document a blind cave in a shadowed setting, or possibly below the fair weather swell zone. Autochthonous and, subordinately, detrital fractions were observed within the skeletal framework of biotic crusts. The syndepositional lithified fraction occurs mainly as very fine-grained laminations. Clotted peloidal and aphanitic (structureless) textures occur in the micrites as well. Autochthonous micrite is always associated with a significant amount of organic matter remains. In caves from the Plemmirio area in SE Sicily, the autochthonous microbial micrite, occurring in the bioconstructions, contains bacterial lipid biomarkers, including abundant compounds derived from sulfate-reducing bacteria. It is likely that a similar microbial mediation was involved in the formation of the autochthonous micrite present in the biotic crusts of the Rumena Cave.     

Ancient Mitochondrial DNA Analyses of Ascaris Eggs Discovered in Coprolites from Joseon Tomb

Analysis of ancient DNA (aDNA) extracted from Ascaris is very important for understanding the phylogenetic lineage of the parasite species. When aDNAs obtained from a Joseon tomb (SN2-19-1) coprolite in which Ascaris eggs were identified were amplified with primers for cytochrome b (cyt b) and 18S small subunit ribosomal RNA (18S rRNA) gene, the outcome exhibited Ascaris specific amplicon bands. By cloning, sequencing, and analysis of the amplified DNA, we obtained information valuable for comprehending genetic lineage of Ascaris prevalent among pre-modern Joseon peoples.     

贵州兴义中三叠世拉丁期兴义动物群粪化石

粪化石是重要的遗迹化石,其内含物信息可为讨论生物行为、生理、相互关系、古环境等提供重要证据,进而对恢复和重建地质历史时期的生态系统等有重要意义。本文首次报道了贵州省兴义市泥麦古剖面中三叠世拉丁期兴义动物群化石层第35自然层的7种不同形态的粪化石。通过观察粪化石的内含物情况,发现其主要由贵州龙骨骼和鱼鳞组成,极少含有无脊椎动物碎片,表明粪化石来源于非壳食性的肉食性动物。依据粪化石的尺寸、缺少螺旋结构及相对较小的内含物碎片等信息,排除动物源是无脊椎动物、大型肉食性鱼类及大型鱼龙类的可能。结合兴义动物群下部化石组合海生爬行类实体化石的信息,进一步推断所研究粪化石的动物源应为非鱼龙的海生爬行动物,很可能是幻龙类、鸥龙类或海龙类。本文报道的7种形态的粪化石显示该下部化石层中的海生爬行动物之间至少存在1级营养等级的差异,这为恢复和重建中三叠世拉丁期海洋生态系统提供了重要依据。另外微生物的参与及泥质含量较高的厌氧环境使得该层的粪化石保存完好。     

Miocene ants (Hymenoptera,Formicidae) from Crimea

Ant imprints, new and previously known, from Middle Miocene deposits near Kerch (Crimean Peninsula, Russia) are described or redescribed. A new Myrmicinae species, Solenopsis atavinus sp. nov., is described based on a wingless female. A winged female similar to the earlier described Dolichoderus tauricus Dlussky, 1981 is found: due to the excellent preservation of this specimen, the new specimen and the holotype of D. tauricus are redescribed and can be reclassified as Ponerites tauricus (Dlussky, 1981), comb. nov. Oecophylla taurica sp. nov. is described based on a partly preserved imprint of a female thorax with a forewing, the venation of which allows it to be positively identified as a weaver ant. Two other species are transferred from the formal genus Camponotites to Oecophylla based on forewing venation: O. kraussei (Dlussky et Rasnitsyn, 1999), comb. nov. (Early Eocene, United States) and O. macroptera (Dlussky, 1981), comb. nov. (Middle Miocene, Stavropol, Russia). One of the studied forewing imprints is similar in venation to Paraphaenogaster microphthalmus Dlussky, 1981, described from the Middle Miocene of Vishnevaya Balka (Stavropol province, Russia) and so is attributed to this species. Dolichoderus tavridus sp. nov. is described based on a forewing.     

广西崇左三合大洞的早更新世反刍类

系统记述了广西崇左三合大洞巨猿动物群中的反刍类:湖麂(Muntiacus lacustris)、凤岐祖鹿(?)相似种(Cervavitus? cf.C.fenqii)、云南黑鹿(Cervus(R.)yunnanensis)、广西巨羊(Megalovis guangxiensis)、山羊亚科属种未定(Caprinae gen.et sp.indet.)和大额牛未定种(Bos(Bibos)sp.)。与其他相关的早更新世动物群中的反刍类相比, 它们与柳城巨猿洞和田东么会洞的最相似。三合大洞的反刍类在组合上反映早更新世的时代特征及湿热的森林-草丛生态环境。这种环境非常适宜诸如巨猿这类高等灵长类的栖息。     

Vegetation reconstruction on the basis of pollen in Late Pleistocene hyena coprolites from San Teodoro Cave (Sicily, Italy)

Vegetation reconstruction based on pollen from coprolites of extinct spotted hyena (Crocuta crocuta spelaea, Goldfuss 1832) recovered from excavations carried out in 1998 at San Teodoro Cave (Sicily, Italy) supports previous indications of pre-Late Glacial conditions. Eight of the twelve coprolites analysed contained well-preserved pollen grains. There is a general similarity between the pollen contents from the coprolites but they show variability. They suggest a main vegetation type dominated by steppic taxa (Poaceae, Artemisia, Ephedra, Chenopodiaceae and Asteraceae) but also including arboreal taxa (Pinus and Cupressaceae). Low percentages of pollen of mesophilous woody taxa (Quercus, Betula, Abies, Alnus, Pistacia, among others) are noticeable, suggesting the existence of nearby refugia for temperate and Mediterranean vegetation. A reconstruction of the landscape, using the coprolite pollen record and other pollen records from Sicily and south Italy, shows the predominance, during the pre-Late Glacial, of a wooded steppe biome, with elements representing a variety of local environmental conditions.     

The Crocuta crocuta spelaea (Goldfuss 1823) population and its prey from the Late Pleistocene Teufelskammer Cave hyena den besides the famous Paleolithic Neandertal Cave (NRW,NW Germany)

Remains from at least seven individuals of the Late Pleistocene Ice Age spotted hyena Crocuta crocuta spelaea (Goldfuss, 1823) from the Teufelskammer Cave in the Neandertal valley (North Rhine-Westphalia, northwest Germany) are described. The small cave was a well-frequented hyena den of the Early to Middle Late Pleistocene which was only 100 m from the famous small Feldhofer Cave, where the first Neandertal human skeleton was found. The high amount of hyena bone material (37%) and its strongly chewed and incomplete prey remains of the mixed mammoth steppe and boreal forest megafauna prove one more of 11 recently known hyena den caves in the Rhenish Massif. Hyenas and cave bears have used the cave, but Neandertal humans lived possibly not at the same time in the same valley. Although hyenas occupied mainly the smaller caves such as the Teufelskammer Cave, humans preferred large portal cave entrances such as in the Neandertal valley with the Small Feldhofer Cave.