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Chinese Science Bulletin 2003年第7期48卷 691-695页

作者： wang banyue & QIU Zhanxiang Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences, Beijing 100044, China Institute of Vertebrate Paleontology and Paleoanthropology Chinese Academy of Sciences Beijing 100044 China

Aepyosciurinae, a new subfamily of Sciuridae, were found at the base of the early Pleistocene loess deposits in Dongxiang County, Gansu Province. Its unilaterally hyp-sodont and lophodont cheek teeth are unique among the sciurids so far known all over the world. Certain degree of similarity can be observed between the cheek teeth of the new subfamily and the Anomalurinae living in tropical and subtropical forests in central and western Africa. Aepyosci-uris orientalis gen. et sp. nov. might have lived in montaneous woodland or grassland and lived on harder leaves, barks, or even grass. This tends to show that the northeastern border area of the Tibetan Plateau had been lifted considerably high in early Pleistocene (ca. 2 Ma), with drier climate, becoming a suitable habitat for Aepyosciurus orientalis.

关键词：西藏高原松鼠亚科啮齿目哺乳纲早更新世黄土沉积物古动物分类学

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A NEW MIDDLE TERTIARY MAMMALIAN LOCALITY FROM SUNITEZUOQI, NEI MONGOL

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古脊椎动物学报(中英文） 1996年第4期 303-304页

作者： MENG Jin wang banyue BAI Zhiqiang(Department of vertebrate Paleontology, the American Museum of NaturaI History New York 10024)(Institute of Vertebate Paleontology and Paleoanthropology, Chinese Academy of Sciences Beijing 100044(Department of Geology

A new middle Tertiary locality from the Bai-yin-bau-li-dau commune,Su-ni -te -zuo-qi (County) of Nei Mongol (Inner Mongolia), was discovered duringthe course of 1:50000 geological mapping in the field seasons of 1992-... 详细信息

关键词： Nei Mongol Late Oligocene-Early Miocene mammals

DISTYLOMYIDAE FAM. NOV. (?CTENODACTYLOIDEA, RODENTIA) FROM NEI MONGOL, CHINA

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古脊椎动物学报 1988年第1期 45-49页

作者： wang banyue Institute of Vertebrate Paleontology and Paleoanthropology, Academia Sinica

IntroductionA pair of rodent lower jaws believed belonging to one and the same individual were collected by the present author from Upper Oligocene Yikebulage Formation in Qianlishan district,Ih Ju League(=Yih Ju Meng),Nei Mongol,in 1978 The affinity searching of the lower jaws has really been a brain-racking one. At first glance I was struck by the similarity between

关键词： Nei Mongol Upper Oligocene Middle Miocene Ctenodactyloidea Distylomyidae

DISCOVERY OF CRICETIDS (RODENTIA, MAMMALIA) FROM MIDDLE OLIGOCENE OF NEI MONGOL, CHINA

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古脊椎动物学报 1987年第3期 195-198页

作者： wang banyue lnstitute Vertebrate Paleontology and Paleoanthropology, Academia Sinica

The Cricetidae, a group of small rodents presently extremely flourishing all over the world, were already widely distributed in Holarctic in Oligocene. Although abundant Oligocene cricetids have been found in North America and Europe, their occurrence in Asia has been restricted so far mainly to the Hsanda Gol Formation. In China no middle Oligocene cricetids had been encountered until 1977 and 1978, when the author succeeded in finding some cricetids from Saint Jacques, Nei Mongol, China. Those cricetid are described in this paper.

关键词： Nei Mongol Middle Oligocene Cricetidae

DISCOVERY OF APLODONTIDAE (RODENTIA, MAMMALIA) FROM MIDDLE OLIGOCENE OF NEI MONGOL, CHINA

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古脊椎动物学报 1987年第1期 41-45页

作者： wang banyue Institute of Vertebrate Paleontology and Paleoanthropology, Academia Sinica

Today only a single species of the aplodontid rodents still survives in the humid region of western North America, but in the Oligocene time the family was widespread over the Northern Hemisphere. Fossils of the Oligocene aplodontids so far have been mainly found in North America and Europe. Their occurrence in Asia is scarce. Only a few examples are known from Kazakhstan, USSR, and Mongolia. No record was known in China until 1977, when some fossil aplodontids were collected from the Middle Oligocene in Nei Mongol.

关键词： Nei Mongol Middle Oligocene Aplodontidae

ON THE SYSTEMATIC POSITION OF PROSCIURUS LOHICULUS

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古脊椎动物学报(中英文） 1986年第4期 291-294页

作者： wang banyue Institute of Vertebrate Paleontology and Paleoanthropology, Academia Sinica

The species Prosciurus lohiculus was erected by Matthew & Granger (1923), based on an upper jaw from Hsanda Gol Formation (Middle Oligocene), Mongolia. Later, Argyropulo (1939) described a lower jaw from the upper Oligocene of Kazakhstan, USSR, which was identified as Prosciurus sp. (lohiculus). Stehlin & Schaub (1951, p. 278) thought that the Kazakhstan lower jaw described by Argyropulo should belong to Plesispermophilus, leaving the holotype of P. lohiculus from Hsanda Gol Formation still in Prosciurus. Wood (1962, p. 236) transferred P. lohiculus into Plesispermophilus on the assumption that the Kazakhstan lower jaw belongs to the same form as the holotype from Hsanda Gol. Wood’s opinion was followed by Mellett (1968, p. 6) and Shevyreva (1976, p. 22). Meanwhile, Kowalski (1974, p. 153) described several lower jaws, new material from the type locality, and believed they belongs to Prosciurus lohiculus and came to the conclusion that the Kazakhstan lower jaw was morphologically quite different from those he found in Tatal Gol, and hence could not belong to the species in question. Schmidt-Kittler and Vianey-Liaud (1979; p. 73) agreed with Kowalski and gave further evidence that the upper teeth of true Plesispermophilus was also different from those of P. lohiculus and that the lower jaw from Kazakhstan might well be of Plesispermophilus. Irrespective of these disagreements, all the authors consented to include P. lohiculus in Prosciurinae (Aplodontidae).

关键词： Asia Oligocene CyIindrodontidae Aplodontidae

FOSSIL VERTEBRATES FROM THE MIOCENE OF NORTHERN KIANGSU

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古脊椎动物学报(中英文） 1964年第4期 348-354页

作者： CHOW MINCHEN wang banyue Institute of Vertebrate Paleontology and Paleoanthropology, Academia Sinica

In this paper some vertebrate fossils collected from the Miocene at Puchen,Nan-king and at Hsiachaohwan,Shihung County,both in northern Kiangsu,are described;and the age of the localities as well as that of the “Hsiachaohwan fauna”are *** Puchen faunaThe fossils were found when siliceous sands were quarryed from a small hill at Pu-chen,a town in the Nanking district,some 8 kilometers on the northern bank of the

关键词：脊椎动物周明镇 FOSSIL VERTEBRATES FROM THE MIOCENE OF NORTHERN KIANGSU 中新世第三纪原大伴月

DISCOVERY OF TWO MID-TERTIARY MAMMALIAN FAUNAS FROM HAIYUAN, NINGXIA, CHINA

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古脊椎动物学报(中英文） 1994年第4期 294-296页

作者： wang banyue (Institute of Vertebrate Paleontology and Paleoanthropolopy, Acodemia Sinica, Beijing, 100044)Yan Zhiqiang,Lu Yanjun,Chen Guoxin (Ningxia Geological and Mineral Prospecting Institution, Yinchuan, 750004)

In Haiyuan County of south Ningxia red beds are well developed. They were noticed early in this century and discussed several times since then. They were first referred to the Eocene (Andersson, 1923; Hsieh, 1923, 1925), but later called Pliocene Kuyuan (=Guyuan) series and Ssukoutze (=Sikouzi) series (Yuan, 1925). Then they were variously allocated as Eocene Kuyuan Formation, Tertiary Kansu (=Gansu) Formation, or subdivided into Paleogene Kuyuan Formation and Neogene Kansu ***, mainly based on lithology, they have been subdivided into Eocene (Sikouzi Formation), Oligocene, early Middle Miocene (Hongliugou Formation), and later Middle Miocene (Ganghegou Formation). The Oligocene in the Ningxia area is also considered to include Early Oligocene, Middle Oligocene (Qingshuiying Formation),and Later Oligocene (Hejiakouzi Formation). However, in the Haiyuan area the geological ages of these subdivisions remain uncertain, and the Oligocene is not subdivided because of lack of mammal fossils and other data that can help determine geological age.

关键词： Haiyuan, Ningxia Early Miocene Middle Oligocene Mammalia

The Shanghuang Mammalian Fauna, Middle Eocene of Jiangsu:History of Discovery and Significance

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古脊椎动物学报(中英文） 1996年第3期 209-214页

作者： Qi Tao K. Christopher Beard wang banyue Mary R. Dawson Guo Jianwei Li Chuankui(Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences Beijing 100044)(Section of Vertebrate Paleontology, Carnegie Museam of Natural Histo

A Paleogene mammalian fauna, here named the Shanghuang fauna, was discov ered near the village of Shanghuang, close to Liyang City, Jiangsu Province, China (Fig.1). At present, rouglily sixty species of fossil mammals have been recognied in the Shanghuang fauna. Many of these mammal taxa are new to science, and others represent new occurrences for the Eocene of China. Particularly well represented in the Shanghuang fauna are micromammals (including marsupials, insectivores, rodents,lagomorphs, primates, and bats) that have seldom if ever been found in other Eocene Asian localities. Biostratigraphic correlations suggest that the Shanghuang fauna repre sents the Irdinmanhan and early Sharamurunian Land Mammal Ages and is likely to be about 45 million years old. Ongoing study of the Shanghuang manunal fauna promlses to shed new insight into the phylogeny and historical biogeography of numer ous higherlevel mammalian taxa. Here, we provide a history of field activities at Shanghuang and an overview of mammalian diversity at Shanghuang.

关键词： Jiangsu Middle Eocene Shanghuang Mammalian Fauna

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双柱鼠科一新属在新疆的发现

古脊椎动物学报 1989年第1期27卷 28-36页

作者：王伴月齐陶中国科学院古脊椎动物与古人类研究所

本文记述了产自新疆准噶尔盆地上渐新统的双柱鼠科一新属——原双柱鼠属(Prodistylo-mys)。它具有一些较原始的特点,但代表不同于Distylomys的另一分支。它的颊齿是由下后方斜向前上方生长的。

关键词：新疆准噶尔盆地上渐新统梳趾鼠超科双柱鼠科

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