Welcome to Visited Vertebrata Palasiatica, Today is

Mansancun Micromammal Fauna from the upper part of the Jiaozigou Formation in Linxia Basin, Gansu Province

  • Ban-Yue WANG ,
  • Zhan-Xiang QIU ,
  • Shi-Qi WANG
Expand
  • Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Sciences Beijing 100044

Received date: 2022-07-05

  Online published: 2023-01-12

Abstract

The micromammal fossils collected from the upper part of the Jiaozigou Formation near Mansancun in 2015 are described. The sample consists of 10 species of six previously known genera (Amphechinus, Sinolagomys, Parasminthus, Litodonomys, Heterosminthus and Yindirtemys) belonging to three orders. Of them, four genera (Sinolagomys, Litodonomys, Heterosminthus and Yindirtemys) made their first appearance in the Late Oligocene and Sinolagomys kansuensis and Heterosminthus lanzhouensis are known only in the Late Oligocene. In comparison with the other Late Oligocene mammalian faunas known in China and Mongolia, the above assemblage appears to be contemporaneous with Xiagou, Taben-buluk, Yikebulage faunas and Tieersihabahe assemblages, but slightly younger than the Shargaltein-Tal Fauna in age. The Mansancun Fauna is also younger than the three Late Oligocene biozones recognized recently in Asia. Compared with the Yagou Fauna collected from the lower part of the Jiaozigou Formation, the Mansancun Local Fauna is clearly younger. Consequently, the Yagou Fauna would be early Late Oligocene, while the Mansancun Local Fauna may be considered late Late Oligocene. Thus, as a whole, the Jiaozigou Formation is Late Oligocene in age.

Cite this article

Ban-Yue WANG , Zhan-Xiang QIU , Shi-Qi WANG . Mansancun Micromammal Fauna from the upper part of the Jiaozigou Formation in Linxia Basin, Gansu Province[J]. Vertebrata Palasiatica, 2023 , 61(2) : 123 -141 . DOI: 10.19615/j.cnki.2096-9899.230112

References

[1] Aymard A, 1850. Concernant les restes de mammiferes fossils recueillis dans le calcaire miocène des environs du Puy. Ann Soc Agric Puy, 14: 104-114
[2] Bohlin B, 1937. Oberoligoz?ne S?ugetiere aus dem Shargaltein-Tal (Western Kansu). Palaeont Sin, New Ser C, 3: 1-66
[3] Bohlin B, 1942. The fossil mammals from the Tertiary deposit of Taben-buluk, westetn Kansu. Part I: Insectivora and Lagomorpha. Palaeont Sin, New Ser C, 8: 1-113
[4] Bohlin B, 1946. The fossil mammals from the Tertiary deposit of Taben-buluk, western Kansu, Part II: Simplicidentata, Carnivora, Artiodactyla, Perissodactyla, and Primates. Palaeont Sin, New Ser C, 8(b): 1-259
[5] Bowdich T E, 1821. An Analysis of the Natural Classifications of Mammalia for the Use of Students and Travelers. Paris: J Smith. 1-115
[6] Brandt J F, 1855. Beitr?ge zur n?hern Kenntniss der S?ugethiere Russland’s. Mém Acad Imp Sci St Pétersbourg, Ser 6, 9: 1-375
[7] Butler P M, 1948. On the evolution of the skull and teeth in the Erinaceidae, with special reference to fossil material in the British Museum. Proc Zool Soc London, 118: 446-500
[8] Coues E, 1875. Some account, critical, descriptive, and historical, of Zapus hudsonius. Bull US Geol Geogr Surv Terr (F V Hayden), Ser 2, 1(5): 253-262
[9] Daxner-H?ck G, Badamgarav D, 2007. 1. Geological and stratigraphic setting. In Daxner-H?ck ed. Oligocene-Miocene Vertebrate from the Valley of Lakes (Central Mongolia): Morphology, Phylogenetic and Stratigraphic Implications. Ann Naturhist Mus Wien, 108A: 1-24
[10] Daxner-H?ck G, Badamgarav D, Erbajeva M, 2010. Oligocene stratigraphy based on a sediment-basalt association in Central Mongolia (Taatsiin Gol and Taatsiin Tsagaan Nuur area, Valley of Lakes): review of a Mongolian-Austrian Project. Vert PalAsiat, 48(4): 348-366
[11] Daxner-H?ck G, Badamgarav D, Maridet O, 2014. Dipodidae (Rodentia, Mammalia) from the Oligocene and Early Miocene of Mongolia. Ann Naturhist Mus Wien, Ser A, 116: 131-214
[12] Daxner-H?ck G, Badamgarav D, Barsbold R et al., 2017. Oligocene stratigraphy across the Eocene and Miocene boundaries in the Valley of Lakes (Mongolia). Palaeobio Palaeoenv, 97(1): 111-218
[13] Deng T, Wang X M, Ni X J et al., 2004. Cenozoic stratigraphic sequence of the Linxia Basin in Gansu, China and its evidence from mammal fossils. Vert PalAsiat, 42(1): 45-66
[14] Deng T, Qiu Z X, Wang B Y et al., 2013. 9. Late Cenozoic biostratigraphy of the Linxia Basin, Northwestern China. In: Wang X M, Flynn L J, Fortelius M eds. Fossil Mammals of Asia. New York: Columbia University Press. 243-273
[15] Deng T, Lu X K, Wang S Q et al., 2021. An Oligocene giant rhino provides insights into Paraceratherium evolution. Commun Biol, doi: 10.1038/s42003-021-02170-6
[16] Erbajeva M, Daxner-H?ck G, 2014. The most prominent Lagomorpha from the Oligocene and Early Miocene of Mongolia. Ann Naturhist Mus Wien, Ser A, 116: 215-245
[17] Fang X M, Wang J Y, Zhang W L et al., 2016. Tectonosedimentary evolution model of an intracontinental flexural (foreland) basin for paleoclimatic research. Glob Planet Change, 145: 78-97
[18] Fischer von Waldheim G, 1814. Zoognosia tabulis synopticis illustrata. Vol. 3. Moscow: Nicolai Sergeidis Vsevolozsky. 1-730
[19] Gervais F L P, 1853. Description ostéologique de l’Anomalurus et remarques sur la classification naturelle des rogeurs. Ann Sci Nat Zool, Paris, Ser 3, 20: 238-246
[20] Gomes Rodrigues H, Marivaux L, Vianey-Liaud M, 2012. The Cricetidae (Rodentia, Mammalia) from the Ulantatal area (Inner Mongolia, China): new data concerning the evolution of Asian cricetids during the Oligocene. J Asian Earth Sci, 56: 160-179
[21] Gomes Rodrigues H, Marivaux L, Vianey-Liaud M, 2014. Rodent paleocommunities from the Oligocene of Ulantatal (Inner Mongolia, China). Palaeovertebrata, 38(1): 1-11
[22] Huang X S, 1987. Fossil ochotonids from the Middle Oligocene of Ulantatal, Nei Mongol. Vert PalAsiat, 25(4): 260-282
[23] Huang X S, 1992. Zapodidae (Rodentia, Mammalia) from the Middle Oligocene of Ulantatal, Nei Mongol. Vert PalAsiat, 30(4): 249-286
[24] Kimura Y, 2010. New material of dipodid rodents (Dipodidae, Rodentia) from the Early Miocene of Gashunyinadege, Nei Mongol, China. J Vert Paleont, 30(6): 1860-1873
[25] Li C K, 1965. Eocene leporids of North China. Vert PalAsiat, 9(1): 23-36
[26] Li C K, Qiu Z D, 1980. Early Miocene mammalian fossils of Xining Basin, Qinghai. Vert PalAsiat, 18(3): 198-214
[27] Li C K, Zhang Z Q, 2019. Order Lagomopha Brandt, 1855. In: Li C K, Zhang Z Q eds. Palaeovertebrata Sinica, Vol III, Fasc 4. Beijing: Science Press. 34-144
[28] Lopatin A V, Zazhigin V S, 2000. The history of Dipodoidea (Rodentia, Mammalia) in the Miocene of Asia: 2. Zapodidae. Paleont J, 34(4): 449-454
[29] Matthew W D, Granger W, 1924. Nine insectivores and ruminants from the Tertiary of Mongolia, with remarks on the correlation. Am Mus Novit, 105: 1-7
[30] Meng J, Ye J, Wu W Y et al., 2006. A recommended boundary stratotype section for Xiejian Stage from northern Junggar Basin: implications to related bio-chronostratigraphy and environmental changes. Vert PalAsiat, 44(3): 205-236
[31] Qiu Z D, 1996. Middle Miocene Micromammalian Fauna from Tunggur, Nei Mongol. Beijing: Science Press. 1-216
[32] Qiu Z D, Li Q, 2016. Neogene rodents from central Nei Mongol, China. Palaeont Sin, New Ser C, 30: 1-485
[33] Qiu Z D, Tong Y S, 2015. Order Eulipotyphla Waddell, Okada et Hasegawa, 1999. In: Li C K, Qiu Z D eds. Palaeovertebrata Sinica, Vol III, Fasc 3. Beijing: Science Press. 1-140
[34] Qiu Z D, Wang B Y, 2019. Family Dipodidae Fischer von Waldheim, 1817. In: Li C K, Qiu Z D eds. Palaeovertebrata Sinica, Vol III, Fasc 5(1). Beijing: Science Press. 242-326
[35] Qiu Z X, Xie J Y, Yan D F, 1990. Discovery of some Early Miocene mammalian fossils from Dongxiang, Gansu. Vert PalAsiat, 28(1): 9-24
[36] Qiu Z X, Wang B Y, Deng T, 2004a. Indricotheres (Perissodactyla, Mammalia) from Oligocene of Linxia Basin, Gansu, China. Vert PalAsiat, 42(3): 177-192
[37] Qiu Z X, Wang B Y, Deng T, 2004b. Mammal fossils from Yagou, Linxia Basin, Gansu, and related stratigraphic problems. Vert PalAsiat, 42(4): 276-296
[38] Savinov P R, 1970. Jerboas (Rodentia, Mammalia) from the Neogene of Kazakhstan. In: Material on Evolution of Terrestrial Vertebrates. Otd Obshch Biol: Akad Nauk USSR. 97-134
[39] Schaub S, 1930. Fossile Sicistinae. Eclogae Geol Helv, 23(2): 616-637
[40] Sulimski A, 1969. On some Oligocene insectivore remains from Mongolia. Palaeont Pol, 21: 53-70
[41] Thomas O, 1897. On the genera of rodents: an attempt to bring up to date the current arrangement of the order. Proc Zool Soc London, 1012-1028
[42] Vianey-Liaud M, Schmidt-Kittler N, Marivaux L, 2006. The Ctenodactylidae (Rodentia) from the Oligocene of Ulantatal (Inner Mongolia, China). Palaeovertebrata, 34(3-4): 111-206
[43] Waddell P J, Okada N, Hasgawa M, 1999. Towards resolving the interordinal relationships of placental mammals. Syst Biol, 48: 1-5
[44] Wang B Y, 1991. Discovery of Yindirtemys (Ctenodactylidae, Rodentia, Mammalia) from Late Oligocene of Nei Mongol, China. Vert PalAsiat, 29(4): 296-302
[45] Wang B Y, 1997a. Chronological sequence and subdivision of Chinese Oligocene mammalian fauna. J Stratigr, 21(3): 183-191
[46] Wang B Y, 1997b. The Mid-Tertiary Ctenodactylidae (Rodentia, Mammalia) of Eastern and Central Asia. Bull Am Mus Nat Hist, 234: 1-88
[47] Wang B Y, 2003. Dipodidae (Rodentia, Mammalia) from the mid-Tertiary deposits in Danghe Area, Gansu, China. Vert PalAsiat, 41(2): 89-103
[48] Wang B Y, 2019. Family Ctenodactylidae Gervais, 1853. In: Li C K, Qiu Z D eds. Palaeovertebrata Sinica, Vol. III, Fasc 5(1). Beijing: Science Press. 388-436
[49] Wang B Y, Qiu Z X, 2000a. Dipodidae (Rodentia Mammalia) from the Lower Member of Xianshuihe Formation in Lanzhou Basin, Gansu, China. Vert PalAsiat, 38(1): 10-35
[50] Wang B Y, Qiu Z X, 2000b. Micromammal fossils from red mudstone of Lower Member of Xianshuihe Formation in Lanzhou Basin, Gansu, China. Vert PalAsiat, 38(4): 255-273
[51] Wang B Y, Qiu Z X, in press. Micromammal fossils from the lower part of the Jiaozigou Formation in Yagou area of Linxia Basin, Gansu Province. Palaeogeogr, Palaeoclimatol, Palaeoecol
[52] Wasiljeff J, Zhang Z Q, 2022. Stratigraphical significance of Ulantatal sequence (Nei Mongol, China) in refining the latest Eocene and Oligocene terrestrial regional stages. Vert PalAsiat, 60(1): 42-53
[53] Wasiljeff J, Kaakinen A, Salminen J M et al., 2020. Magnetostratigraphic constraint on the fossiliferous Ulantatal sequence in Inner Mongolia, China: implications for Asian aridification and faunal turnover before the Eocene-Oligocene boundary. Earth Planet Sci Lett, 535: 116125, doi: 10.1016/j.epsl.2020.116125
[54] Zhang Z Q, Liu Y, Wang L H et al., 2016. Lithostratigraphic context of Oligocene Mammalian faunas from Ulantatal, Nei Mongol, China. C R Palevol, 15(7): 903-910
[55] Ziegler R, Dahlmann T, Storch G, 2007. 4. Marsupialia, Erinaceomorpha and Soricomorpha (Mammalia). In: Daxner-H?ck G ed.ed. Oligocene-Miocene Vertebrates from the Valley of Lakes (Central Mongolia): Morphology, Phylogenetic and Stratigraphic Implications. Ann Naturhist Mus Wien, 108A: 53-164
Outlines

/