欢迎访问《古脊椎动物学报》官方网站,今天是

内蒙古二连盆地沙拉木伦期啮齿类动物群研究

  • 李琪 ,
  • 李茜
展开
  • 1 云南大学生命科学学院脊椎动物演化研究中心 昆明 650500
    2 中国科学院古脊椎动物与古人类研究所,中国科学院脊椎动物演化与人类起源重点实验室 北京 100044
    3 中国科学院生物演化与环境卓越创新中心 北京 100044

收稿日期: 2022-09-15

  网络出版日期: 2022-11-23

基金资助

国家自然科学基金(42072023);中国科学院战略性先导科技专项(XDB26000000);中国科学院战略性先导科技专项(XDA20070203);中国科学院古生物化石发掘与修理专项资助

The Sharamurunian rodent fauna in the Erlian Basin, Nei Mongol, China

  • Qi LI ,
  • Qian LI
Expand
  • 1 Centre for Vertebrate Evolutionary Biology, Yunnan University Kunming 650500
    2 Key Laboratory of Vertebrate Evolution and Human Origins of Chinese Academy of Sciences, Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences Beijing 100044
    3 CAS center for Excellence in Life and Paleoenviroment Beijing 100044

Received date: 2022-09-15

  Online published: 2022-11-23

摘要

内蒙古二连盆地乌拉乌苏地区是亚洲哺乳动物分期中沙拉木伦期哺乳动物群的发现地和经典产地。在以往的研究中鲜少有关于这一地区啮齿类化石的报道。近来,在该地区沙拉木伦组下部地层中发现大量的啮齿类化石,经详细的形态学研究,它们被归入1超科4科7属9种,包括梳趾鼠超科的Yuomys cavioides, Gobiomys neimongolensis, G. exiguus以及G. asiaticus; 跳鼠科Allosminthus uniconjugatusPrimisminthus shanghenus; 仓鼠科Pappocricetodon rencunensis; 壮鼠科Hulgana cf. H. ertnia和圆柱齿鼠科Proardynomys ulausuensis。乌拉乌苏沙拉木伦组下部与额尔登敖包“下红层”的啮齿类组合具有高度相似性,两者共同构成了二连盆地沙拉木伦期啮齿类动物群。综合二连盆地乌拉乌苏地点沙拉木伦组下部以及额尔登敖包剖面“下红层”的啮齿类化石,运用最小个体数的方法对二连盆地沙拉木伦期啮齿类动物群的组分和特征进行了分析,结果显示梳趾鼠类最具优势,跳鼠类和仓鼠类次之。通过物种多样性分析,二连盆地古近纪啮齿类动物群呈现出早中始新世以梳趾鼠类为主导类群到晚始新世以仓鼠、跳鼠类为主导类群的转变。内蒙古二连盆地和山西垣曲盆地沙拉木伦期啮齿类动物群的特征存在差异,很可能是由两个动物群所处不同的区域环境所造成的。

本文引用格式

李琪 , 李茜 . 内蒙古二连盆地沙拉木伦期啮齿类动物群研究[J]. 古脊椎动物学报, 2023 , 61(1) : 43 -70 . DOI: 10.19615/j.cnki.2096-9899.221123

Abstract

New middle Eocene rodent fossils discovered from the lower part of the Shara Murun Formation of Ula Usu, Erlian Basin, Nei Mongol, China, the classical locality of Sharamurunian mammalian fauna, were identified as 9 separate species (the ctenodactyloids Yuomys cavioides, Gobiomys neimongolensis, G. exiguus, and G. asiaticus, the dipodids Allosminthus uniconjugatus and Primisminthus shanghenus, the cricetid Pappocricetodon rencunensis, the ischyromyid Hulgana cf. H. ertnia, and the cylindrodontid Proardynomys ulausuensis) belonging to 7 genera, 4 families, and 1 superfamily of Rodentia. The Ula Usu rodent assemblage shares a high degree of similarity with that from the “Lower Red” beds of the Erden Obo, and they both represent the typical Sharamurunian rodent assemblages found in northern China. The Sharamurunian rodent fauna in the Erlian Basin is analyzed by the minimum number of individuals based on the rodent materials from the lower part of the Shara Murun Formation in the Ula Usu and the “Lower Red” beds of the Erden Obo. In the Sharamurunian rodent fauna of the Erlian Basin, ctenodactyloids are the most dominant elements, and dipodids and cricetids follow next in prevalence. By analyzing the evolution of the rodent species richness in the Erlian Basin, the rodent faunas show a transformation from a ctenodactyloid dominant assemblage to a cricetid-dipodid dominant one in chronological order. The Sharamurunian rodent fauna from the Erlian Basin differs from that of the Yuanqu Basin and the differences in the rodent assemblages may be a response to the differences between the regional environments.

参考文献

[1] Bai B, Wang Y Q, Li Q et al., 2018. Biostratigraphy and diversity of Paleogene Perissodactyls from the Erlian Basin of Inner Mongolia, China. Am Mus Novit, 3914: 1-60
[2] Berkey C P, Granger W, 1923. Later sediments of the desert basins of central Mongolia. Am Mus Novit, 77: 1-16
[3] Berkey C P, Morris F K, 1927. Geology of Mongolia—a reconnaissance report based on the investigations of the years 1922-1923. In: Natural History of Central Asia. Vol II. New York: American Museum of Natural History. 1-475
[4] Burke J J, 1935. Pseudocylindrodon, a new rodent genus from the Pipestone Springs Oligocene of Montana. Ann Carnegie Mus, 25: 1-4
[5] Burke J J, 1936. Ardynomys and Desmatolagus in the North American Oligocene. Ann Carnegie Mus, 25: 135-154
[6] Chow M C, Rozhdestvensky A K, 1960. Exploration in Inner Mongolia - a preliminary account of the 1959 field work of the Sino-Soviet Paleontological Expedition (SSPE). Vert PalAsiat, 4: 1-10
[7] Dashzeveg D, Meng J, 1998. A new Eocene cylindrodont rodent (Mammalia, Rodentia) from the eastern Gobi of Mongolia. Am Mus Novit, 3253: 1-18
[8] Dawson M R, 1968. Oligocene rodents (Mammalia) from East Mesa, Inner Mongolia. Am Mus Novit, 2324: 1-12
[9] Daxner-H?ck G, 2001. New Zapodids (Rodentia) from Oligocene-Miocene deposits in Mongolia. Part 1. Senckenbergiana lethaea, 81: 351-389
[10] Daxner-H?ck G, Badamgarav D, Maridet O, 2014. Dipodidae (Rodentia, Mammalia) from the Oligocene and Early Miocene of Mongolia. Ann Naturh Mus Wien, Ser A, 116: 131-214
[11] Douglass E, 1901. Fossil Mammalia of the White River Beds of Montana. Trans Am Philos Soc, Philadelphia, 20: 237-279
[12] Emry R J, Tyutkova L A, Lucas S G et al., 1998. Rodents of the Middle Eocene Shinzhaly Fauna of eastern Kazakatan. J Vert Paleont, 18: 218-227
[13] Fostowicz-Frelik ?, Li C K, Meng J et al., 2012. New Gobiolagus (Mammalia: Lagomorpha) from the Middle Eocene of Erden Obo (Nei Mongol, China). Vert PalAsiat, 50: 219-236
[14] Fostowicz-Frelik ?, Li C K, Mao F Y et al., 2015. A large mimotonid from the Middle Eocene of China sheds light on the evolution of lagomorphs and their kin. Sci Rep, 9394: 1-9, doi: 10.1038/srep09394
[15] Gong H, Li Q, Ni X J, 2021. New species of Yuomys (Rodentia, Ctenodactyloidea) from the upper Eocene of eastern Ningxia, China. J Vert Paleont, doi: 10.1080/02724634.2021.1938099
[16] Granger W, 1925. Records of fossils, Mongolia 1925. Third Central Asiatic Expeditions (Field Notes). New York: American Museum of Natural History. 1-76
[17] Granger W, Berkey C P, 1922. Discovery of Cretaceous and older Tertiary strata in Mongolia. Am Mus Novit, 42: 1-7
[18] Huang X S, Zhang J N, 1990. First record of Early Tertiary mammals from southern Yunnan. Vert PalAsiat, 28: 296-303
[19] Jin J H, Liao W B, Wang B S et al., 2003. Global change in Cenozoic and evolution of flora in China. Guihaia, 23: 217-225
[20] Li C K, 1975. Yuomys, a new ischyromyid rodent genus from the Upper Eocene of North China. Vert PalAsiat, 13: 58-70
[21] Li C K, Ting S Y, 1983. The Paleogene mammals of China. Bull Carnegie Mus Nat Hist, 21: 1-93
[22] Li Q, 2012. Middle Eocene Cricetids (Rodentia, Mammalia) from the Erlian Basin, Nei Mongol, China. Vert PalAsiat, 50: 360-364
[23] Li Q, 2016. Eocene fossil rodent assemblages from the Erlian Basin (Inner Mongolia, China): biochronological implications. Palaeoworld, 25: 95-103
[24] Li Q, 2017. Eocene ctenodactyloid rodent assemblages and diversification from Erden Obo, Nei Mongol, China. Hist Biol, 31: 813-823
[25] Li Q, 2018. Additional cricetid and dipodid rodent material from the Erden Obo section, Erlian Basin (Nei Mongol, China) and its biochronological implications. Palaeoworld, 27: 490-505
[26] Li Q, 2020. New late Eocene cylindrodontid rodents from the Erlian Basin (Nei Mongol, China). Palaeobio Palaeoenv, 100: 1083-1094
[27] Li Q, 2021. Additional tsaganomyid, cylindrodontid and ctenodactyloid rodent materials from the Erden Obo section, Erlian Basin (Nei Mongol, China). Vert PalAsiat, 59: 1-17
[28] Li Q, Meng J, 2015. New ctenodactyloid rodents from the Erlian Basin, Nei Mongol, China, and the phylogenetic relationships of Eocene Asian ctenodactyloids. Am Mus Novit, 3828: 1-58
[29] Li Q, Meng J, Wang Y Q, 2016. New cricetid rodents from strata near the Eocene-Oligocene boundary in Erden Obo Section (Nei Mongol, China). PloS One, 11: 1-17
[30] Li Q, Gong Y X, Wang Y Q, 2017. New dipodid rodents from the Late Eocene of Erden Obo (Nei Mongol, China). Hist Biol, 29: 692-703
[31] Li Q, Wang Y Q, Mao F Y et al., 2019. A new Eocene cylindrodontid rodent from the Erlian Basin (Nei Mongol, China) and its implications for phylogeny and biochronology. J Vert Paleont, 39: e1680990, doi: 10.1080/02724634.2019.1680990
[32] Luterbacher H P, Ali J R, Brinkhuis H et al., 2004. The Paleogene Period. In: Gradstein F M, Ogg J G, Smith A eds. A Geological Time Scale 2004. Cambridge: Cambridge University Press. 384-408
[33] Matthew W D, Granger W, 1925. New creodonts and rodents from the Ardyn Obo Formation of Mongolia. Am Mus Novit, 193: 1-7
[34] Matthew W D, Granger W, 1926. Two new perissodactyls from the Arshanto Eocene of Mongolia. Am Mus Novit, 208: 1-5
[35] Meng J, Ye J, Huang X S, 1999. Eocene mammals from the Bayan Ulan of Nei Mongol (Inner Mongolia) and comments on related straigraphy. Vert PalAsiat, 37: 165-174
[36] Romer A S, 1966. Vertebrate Paleontology. Chicago and London: University of Chicago Press. 1-467
[37] Rose K D, 1981. The Clarkforkian land-mammal age and mammalian faunal composition across the Paleocene-Eocene boundary. Pap Palaeontol, 26: 1-197
[38] Shi R L, 1989. Late Eocene mammalian fauna of Huangzhuang, Qufu, Shandong. Vert PalAsiat, 27: 87-102
[39] Tong Y S, 1992. Pappocricetodon, a pre-Oligocene cricetid genus (Rodentia) from central China. Vert PalAsiat, 30: 1-16
[40] Tong Y S, 1997. Middle Eocene small mammals from Liguanqiao Basin of Henan Province and Yuanqu Basin of Shanxi Province, Central China. Palaeon Sin, New Ser C, 26: 1-256
[41] Tong Y S, Zheng S H, Qiu Z D, 1995. Cenozoic mammal ages of China. Vert PalAsiat, 33: 290-314
[42] Speijer R P, P?like H, Hollis C J et al., 2020. The Paleogene Period. In: Gradstein F M, Ogg J G, Schmitz M D et al. eds. Geologic Time Scale 2020. Oxford: Elsevier BV. 1087-1140
[43] Vandenberghe N, Hilgen F L, Speijer R P, 2012. The Paleogene Period. In: Gradstein F M, Ogg J G, Schmitz M D et al. eds. The Geologic Time Scale 2012. Oxford: Elsevier BV. 855-922
[44] Wang B Y, 1985. Zapodidae (Rodentia, Mammalia) from the Lower Oligocene of Qujing, Yunnan, China. Mainzer geowiss Mitt, 14: 354-367
[45] Wang B Y, 1997a. The Mid-Tertiary Ctenodactylidae (Rodentia, Mammalia) of eastern and central Asia. Bull Am Mus Nat Hist, 234: 1-88
[46] Wang B Y, 1997b. Chronological sequence and subdivision of Chinese Oligocene mammalian faunas. J Stratigr, 21: 183-191
[47] Wang B Y, 2001. Eocene ctenodactyloids (Rodentia, Mammalia) from Nei Mongol, China. Vert PalAsiat, 39: 98-114
[48] Wang B Y, 2007. Late Eocene cricetids (Rodentia, Mammalia) from Nei Mongol, China. Vert PalAsiat, 45: 195-212
[49] Wang B Y, 2008. Additional rodent material from Houldjin Formation of Erenhot, Nei Mongol, China. Vert PalAsiat, 46: 21-30
[50] Wang B Y, 2017. Discovery of Yuomys from Altun Shan, Xinjiang, China. Vert PalAsiat, 5: 227-232
[51] Wang B Y, 2019a. “Cylindrodontidae”. In: Qiu Z X, Li C K eds. Palaeovertebrata Sinica, VIII, Basal Synapsids and Mammals, Fascicle 5, Glires II: Rodentia I. Beijing: Science Press. 449-478
[52] Wang B Y, 2019b. “Gobiomyidae”. In: Qiu Z X, Li C K eds. Palaeovertebrata Sinica, VIII, Basal Synapsids and Mammals, Fascicle 5, Glires II: Rodentia I. Beijing: Science Press. 436-440
[53] Wang B Y, Dawson M R, 1994. A primitive cricetid (Mammalia: Rodentia) from the Middle Eocene of Jiangsu Province, China. Ann Carnegie Mus, 63: 239-256
[54] Wang B Y, Zhou S Q, 1982. Late Eocene mammals from Pingchangguan Basin, Henan. Vert PalAsiat, 20: 203-215
[55] Wang B Y, Wu W Y, Qiu Z D, 2020. “Cricetidae”. In: Qiu Z X, Li C K, Zheng S H et al. eds. Palaeovertebrata Sinica VIII, Basal Synapsids and Mammals, Fascicle 5, Glires II: Rodentia II. Beijing: Science Press. 10-151
[56] Wang J W, 1978. Fossil Amynodontidae and Ischyromyidae of Tongbo, Henan. Vert PalAsiat, 16: 22-29
[57] Wang Y Q, Meng J, Ni X J et al., 2007. Major events of Paleogene mammal radiation in China. Geol J, 42: 415-430
[58] Wang Y Q, Meng J, Christopher K B et al., 2010. Early Paleogene stratigraphic sequences, mammalian evolution and its response to environmental changes in Erlian Basin, Inner Mongolia, China. Sci China Earth Sci, 53: 1918-1926
[59] Wang Y Q, Meng J, Jin X, 2012. Comments on Paleogene localities and stratigraphy in the Erlian Basin, Nei Mongol, China. Vert PalAsiat, 50: 181-203
[60] Wang Y Q, Li Q, Bai B et al., 2019. Paleogene integrative stratigraphy and timescale of China. Sci China Earth Sci, 62: 287-309
[61] Wood A E, 1970. The Early Oligocene rodent Ardynomys (Family Cylindrodontidae) from Mongolia and Montana. Am Mus Novit, 2418: 1-18
[62] Woodburne J M, 1987. Mammal ages, stages, and zones. In: Woodburne M O ed. Cenozoic Mammals of North America: Geochronology and Biostratigraphy. Berkeley: University of California Press. 18-23
[63] Ye J, 1983. Mammalian fauna from the Late Eocene of Ulan Shiren Area, Inner Mongolia. Vert PalAsiat, 21: 109-118
[64] Zdansky O, 1930. Die altterti?ren S?ugetiere Chinas nebst stratigraphischen Bemerkungen. Palaeont Sin, New Ser C, 6: 1-87
文章导航

/