174 lines
22 KiB
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174 lines
22 KiB
XML
<document id="9FAE3A7742B5558134A33D292FAF474E" ID-DOI="10.1206/0003-0090(2003)279<0586:c>2.0.co;2" ID-ISSN="0003-0090" IM.bibliography_approvedBy="felipe" IM.illustrations_approvedBy="felipe" IM.materialsCitations_approvedBy="felipe" IM.metadata_approvedBy="felipe" IM.taxonomicNames_approvedBy="felipe" IM.treatments_approvedBy="felipe" checkinTime="1721328380972" checkinUser="felipe" docAuthor="ZHUDING, QIU & CHUANKUEI, LI" docDate="2003" docId="03A7D5505877A335FF7B9C12FE5FFD6F" docLanguage="en" docName="BulAmeMusNatHis.2003.B279a22.586-602.pdf" docOrigin="Bulletin of the American Museum of Natural History 279" docSource="http://dx.doi.org/10.1206/0003-0090(2003)279<0586:c>2.0.co;2" docStyle="DocumentStyle:25EFC9A7B3A675566A5530656FFE3DF4.2:BulAmeMusNatHis.2000-2010.chapters" docStyleId="25EFC9A7B3A675566A5530656FFE3DF4" docStyleName="BulAmeMusNatHis.2000-2010.chapters" docStyleVersion="1" docTitle="Protalactaga major CHINESE NEOGENE RODENT FAUNAS" docType="treatment" docVersion="1" lastPageNumber="590" masterDocId="FF9EAD285875A331FFFD9E71FFF9FFFF" masterDocTitle="Chapter 22: Rodents from the Chinese Neogene: Biogeographic Relationships with Europe and North America" masterLastPageNumber="602" masterPageNumber="586" pageNumber="588" updateTime="1721671559394" updateUser="felipe" zenodo-license-document="CC-BY-4.0">
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<mods:title id="752FDBDF944A7A440585E82F321A12B0">Chapter 22: Rodents from the Chinese Neogene: Biogeographic Relationships with Europe and North America</mods:title>
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<mods:namePart id="6353A08908613BD6EFFFE5E73A354465">ZHUDING, QIU</mods:namePart>
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<mods:namePart id="AAA78C9CB201F65F60356301A223E2B5">CHUANKUEI, LI</mods:namePart>
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<mods:title id="DB16A5785B77442A803AD0432C9934E0">Bulletin of the American Museum of Natural History</mods:title>
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<mods:date id="D7CE7AD66C33CEAED10CF0D48E68143F">2003</mods:date>
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<mods:number id="EEA56BEF21E09F59ED5A5ADD004CCD47">2003-11-30</mods:number>
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<mods:number id="F9513BF747046F72283856D8FCE20081">279</mods:number>
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<mods:classification id="3521DE48D3810E02B9A81BBD0632608B">journal article</mods:classification>
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<mods:identifier id="F07980EB1FC6B7F002065D986CFF412D" type="DOI">10.1206/0003-0090(2003)279<0586:c>2.0.co;2</mods:identifier>
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<mods:identifier id="16645939C51ABCF54D5499BEB5569C3E" type="ISSN">0003-0090</mods:identifier>
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<treatment id="03A7D5505877A335FF7B9C12FE5FFD6F" LSID="urn:lsid:plazi:treatment:03A7D5505877A335FF7B9C12FE5FFD6F" httpUri="http://treatment.plazi.org/id/03A7D5505877A335FF7B9C12FE5FFD6F" lastPageId="4" lastPageNumber="590" pageId="2" pageNumber="588">
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<subSubSection id="C31437CD5877A333FF7B9C12FEA7FB61" pageId="2" pageNumber="588" type="nomenclature">
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<paragraph id="8BB164465877A333FF7B9C12FE45FD68" blockId="2.[134,640,611,663]" pageId="2" pageNumber="588">
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<heading id="D0F9D32A5877A333FF7B9C12FE45FD68" centered="true" fontSize="10" level="2" pageId="2" pageNumber="588" reason="4">
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<taxonomicName id="4C0E1FC55877A333FF7B9C12FE45FD68" authority="CHINESE NEOGENE RODENT FAUNAS" authorityName="CHINESE NEOGENE RODENT FAUNAS" class="Mammalia" family="Dipodidae" genus="Protalactaga" higherTaxonomySource="GBIF" kingdom="Animalia" order="Rodentia" pageId="2" pageNumber="588" phylum="Chordata" rank="species" species="major">MAJOR CHINESE NEOGENE RODENT FAUNAS</taxonomicName>
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</heading>
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</paragraph>
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<paragraph id="8BB164465877A333FF659CC3FEA7FB61" blockId="2.[123,652,690,1741]" pageId="2" pageNumber="588">
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Neogene rodent localities are centered largely in northern and northwestern
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<collectingCountry id="F31924D65877A333FDC39CBEFD7FFD19" box="[574,646,719,742]" name="China" pageId="2" pageNumber="588">China</collectingCountry>
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, scattered in southwestern areas and the area between the Yangtze River and the Huai Riv er, but so far not known in southeastern and northeastern parts of
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<collectingCountry id="F31924D65877A333FE7E9D35FE35FCA4" box="[387,460,836,859]" name="China" pageId="2" pageNumber="588">China</collectingCountry>
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. A set of local rodent faunas in central
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<collectingRegion id="49CAAAA45877A333FE629D13FDAEFC86" box="[415,599,866,889]" country="China" name="Nei Mongol" pageId="2" pageNumber="588">Inner Mongolia</collectingRegion>
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and the middle part of the Yellow River valley characterize very well the history of Chinese Neogene rodents in North
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<collectingCountry id="F31924D65877A333FE359DCBFDE8FC2E" box="[456,529,954,977]" name="China" pageId="2" pageNumber="588">China</collectingCountry>
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. The best representative and highly significant Neogene local faunas are the Suosuoquan fauna, Xiejia fauna, Sihong fauna, Tunggur fauna, Amuwusu fauna, Shihuiba fauna of Lufeng, Yushe faunas, Ertemte fauna, Wenwanggou faunas of Lingtai, Bilike fauna, Daodi fauna, and Wushan fauna.
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</paragraph>
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</subSubSection>
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<subSubSection id="C31437CD5877A335FF659AD5FE5FFD6F" lastPageId="4" lastPageNumber="590" pageId="2" pageNumber="588" type="description">
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<paragraph id="8BB164465877A333FF659AD5FD8AFA76" blockId="2.[123,652,690,1741]" pageId="2" pageNumber="588">
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The Suosuoquan fauna has been variously considered late Oligocene (
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<bibRefCitation id="EF9F19B75877A333FE479AB3FD7BFB26" author="Tong, Y. S. & S. H. Zheng & Z. D. Qiu" box="[442,642,1218,1241]" pageId="2" pageNumber="588" pagination="290 - 314" refId="ref9406" refString="Tong, Y. S., S. H. Zheng, and Z. D. Qiu. 1995. Cenozoic mammal ages of China. Vertebrata PalAsiatica 33 (4): 290 - 314. [In Chinese with English summary]" type="journal article" year="1995">Tong et al., 1995</bibRefCitation>
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) and early Miocene (
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<bibRefCitation id="EF9F19B75877A333FE969AAEFDA8FB09" author="Qiu, Z. X. & Z. D. Qiu" box="[363,593,1247,1270]" pageId="2" pageNumber="588" pagination="41 - 70" refId="ref8990" refString="Qiu, Z. X., and Z. D. Qiu. 1995. Chronological sequence and subdivision of Chinese Neogene mammalian faunas. Palaeogeography, Palaeoclimatology, Palaeoecology 116: 41 - 70." type="journal article" year="1995">Qiu and Qiu, 1995</bibRefCitation>
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;
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<bibRefCitation id="EF9F19B75877A333FDA29AAEFEFAFAEC" author="Qiu, Z. X. & W. Y. Wu & Z. D. Qiu" pageId="2" pageNumber="588" pagination="443 - 455" refId="ref9027" refString="Qiu, Z. X., W. Y. Wu, and Z. D. Qiu. 1999. Miocene mammal faunal sequence of China: Palaeozoogeography and Eurasian relationships. In G. E. Rossner and K. Heissig (editors), The Miocene land mammals of Europe: 443 - 455. Munich: Pfeil Verlag." type="book chapter" year="1999">Qiu et al., 1999</bibRefCitation>
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). It is here referred to the earliest Neogene fauna of
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<collectingCountry id="F31924D65877A333FEAE9B6BFE61FACE" box="[339,408,1306,1329]" name="China" pageId="2" pageNumber="588">China</collectingCountry>
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because the nine rodents associated with other mammals are derived species of the genera present in latest Oligocene faunas, such as at Tabenbuluk.
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</paragraph>
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<paragraph id="8BB164465877A333FF659BFEFDC5F9A8" blockId="2.[123,652,690,1741]" pageId="2" pageNumber="588">
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The Xiejia fauna well represents the early Miocene in northwestern
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<collectingCountry id="F31924D65877A333FE589BDDFE14FA3C" box="[421,493,1452,1475]" name="China" pageId="2" pageNumber="588">China</collectingCountry>
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, and contains survivors of endemic Oligocene forms, but with definitely advanced species characters (
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<bibRefCitation id="EF9F19B75877A333FF7E9874FE9BF9E3" author="Li, C. K. & Z. D. Qiu" box="[131,354,1541,1564]" pageId="2" pageNumber="588" pagination="198 - 214" refId="ref8083" refString="Li, C. K., and Z. D. Qiu. 1980. Early Miocene mammalian fossils of Xining basin, Qinghai. Vertebrata PalAsiatica 18 (2): 198 - 214. [In Chinese with English summary]" type="journal article" year="1980">Li and Qiu, 1980</bibRefCitation>
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). The species of
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<taxonomicName id="4C0E1FC55877A333FDC19874FF2EF9C5" class="Mammalia" family="Dipodidae" genus="Parasminthus" higherTaxonomySource="GBIF" kingdom="Animalia" order="Rodentia" pageId="2" pageNumber="588" phylum="Chordata" rank="genus">
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<emphasis id="B97AB8545877A333FDC19874FF2EF9C5" italics="true" pageId="2" pageNumber="588">Parasminthus</emphasis>
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</taxonomicName>
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in this fauna shows more derived morphology than that of Suosuoquan.
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</paragraph>
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<paragraph id="8BB164465877A333FF65982FFC6EFE56" blockId="2.[123,652,690,1741]" lastBlockId="2.[699,1228,193,1741]" pageId="2" pageNumber="588">
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The Sihong (Xiacaowan or Hsiatsaowan) fauna, consisting of 17 species of rodents from the Songlinzhuang, Zhengji, and Shuanggou sites, represents the very few early Miocene assemblages of eastern
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<collectingCountry id="F31924D65877A333FBA69EB0FB59FF27" box="[1115,1184,193,216]" name="China" pageId="2" pageNumber="588">China</collectingCountry>
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(
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<bibRefCitation id="EF9F19B75877A333FB4D9EB0FCBDFF09" author="Li, C. K. & Y. P. Lin & Y. M. Gu & L. H. Hou & W. Y. Wu & Z. D. Qiu" pageId="2" pageNumber="588" pagination="313 - 317" refId="ref7999" refString="Li, C. K., Y. P. Lin, Y. M. Gu, L. H. Hou, W. Y. Wu, and Z. D. Qiu. 1983. The Aragonian vertebrate fauna of Xiacaowan, Jiangsu - 1. A brief introduction to the fossil localities and preliminary report to the new material. Vertebrata PalAsiatica 21 (4): 313 - 317. [In Chinese with English summary]" type="journal article" year="1983">Li et al., 1983</bibRefCitation>
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). It is composed of quite a number of rodents and other mammals either particular to the present Palearctic region or distributed over the Oriental region and tropical/ subtropical areas today. The fauna is closely related to the early Miocene Li Mae Long fauna of
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<collectingCountry id="F31924D65877A333FCDA9FE3FC6BFE56" box="[807,914,402,425]" name="Thailand" pageId="2" pageNumber="588">Thailand</collectingCountry>
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.
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</paragraph>
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<paragraph id="8BB164465877A333FD259FC1FB90FD2B" blockId="2.[699,1228,193,1741]" pageId="2" pageNumber="588">
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The Third Central Asiatic Expedition organized by the American Museum of Natural History initially investigated the Tunggur fauna. The site was recollected by Chinese paleontologists in 1986, who recovered 21 rodent taxa to be added to the socalled
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<taxonomicName id="4C0E1FC55877A333FB649C37FCD7FD85" authorityName="Borissiak" authorityYear="1928" class="Mammalia" family="Gomphotheriidae" genus="Platybelodon" higherTaxonomySource="GBIF" kingdom="Animalia" order="Proboscidea" pageId="2" pageNumber="588" phylum="Chordata" rank="genus">
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<emphasis id="B97AB8545877A333FB649C37FCD7FD85" italics="true" pageId="2" pageNumber="588">Platybelodon</emphasis>
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</taxonomicName>
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fauna. This is the most diverse and abundant middle Miocene fauna known in
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<collectingCountry id="F31924D65877A333FD469CEEFCF9FD49" box="[699,768,671,694]" name="China" pageId="2" pageNumber="588">China</collectingCountry>
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and all of Asia (
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<bibRefCitation id="EF9F19B75877A333FC259CEEFB81FD49" author="Stirton, R. A." box="[984,1144,671,694]" pageId="2" pageNumber="588" pagination="1 - 4" refId="ref9179" refString="Stirton, R. A. 1934. A new species of Amblycastor from the Platybelodon beds, Tung Gur Formation of Mongolia. American Museum Novitates 694: 1 - 4." type="journal article" year="1934">Stirton, 1934</bibRefCitation>
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,
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<bibRefCitation id="EF9F19B75877A333FB749CEEFB3EFD49" author="Stirton, R. A." box="[1161,1223,671,694]" pageId="2" pageNumber="588" pagination="391 - 458" refId="ref9212" refString="Stirton, R. A. 1935. A review of the Tertiary beavers. University of California Publications, Geological Sciences 23 (13): 391 - 458." type="journal article" year="1935">1935</bibRefCitation>
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;
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<bibRefCitation id="EF9F19B75877A333FD469CCCFCB6FD2B" author="Wood, A. E." box="[699,847,701,724]" pageId="2" pageNumber="588" pagination="1 - 7" refId="ref9610" refString="Wood, A. E. 1936. Two new rodents from the Miocene of Mongolia. American Museum Novitates 865: 1 - 7." type="journal article" year="1936">Wood, 1936</bibRefCitation>
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;
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<bibRefCitation id="EF9F19B75877A333FCA09CCCFC3FFD2B" author="Li, C. K." box="[861,966,701,724]" pageId="2" pageNumber="588" pagination="240 - 243" refId="ref7922" refString="Li, C. K. 1963. A new species of Monosaulax from Tung Gur Miocene, Inner Mongolia. Vertebrata PalAsiatica 7 (3): 240 - 243. [In Chinese with English summary]" type="journal article" year="1963">Li, 1963</bibRefCitation>
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;
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<bibRefCitation id="EF9F19B75877A333FC299CCCFBA4FD2B" author="Qiu, Z. D." box="[980,1117,701,724]" pageId="2" pageNumber="588" refId="ref8518" refString="Qiu, Z. D. 1996 a. Middle Miocene micromammalian fauna from Tunggur, Nei Mongol. Beijing: Science Press. [In Chinese with English summary]" type="book" year="1996">Qiu, 1996a</bibRefCitation>
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).
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</paragraph>
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<paragraph id="8BB164465877A333FD259CAAFC4BFC96" blockId="2.[699,1228,193,1741]" pageId="2" pageNumber="588">
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The Amuwusu fauna (19 taxa) contains either Tunggurian relict forms or very primitive Baodean elements (
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<bibRefCitation id="EF9F19B75877A333FC029D67FD00FCB4" author="Qiu, Z. D. & X. M. Wang" pageId="2" pageNumber="588" pagination="120 - 139" refId="ref8882" refString="Qiu, Z. D., and X. M. Wang. 1999. Small mammal faunas and their ages in Miocene of central Nei Mongol (Inner Mongolia). Vertebrata PalAsiatica 37 (2): 120 - 139. [In Chinese with English summary]" type="journal article" year="1999">Qiu and Wang, 1999</bibRefCitation>
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), and is considered an earliest late Miocene fauna in
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<collectingCountry id="F31924D65877A333FC989D23FC57FC96" box="[869,942,850,873]" name="China" pageId="2" pageNumber="588">China</collectingCountry>
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.
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</paragraph>
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<paragraph id="8BB164465877A333FD259D01FB32FBC5" blockId="2.[699,1228,193,1741]" pageId="2" pageNumber="588">
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The Shihuiba fauna from the Lufeng hominoid locality, including 19 species of rodents, is the best represented late Miocene fauna in South
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<collectingCountry id="F31924D65877A333FC8F9DBBFC42FC1E" box="[882,955,970,993]" name="China" pageId="2" pageNumber="588">China</collectingCountry>
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. It exhibits a quite different composition from that of the contemporary faunas of North
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<collectingCountry id="F31924D65877A333FC199A74FBD0FBE3" box="[996,1065,1029,1052]" name="China" pageId="2" pageNumber="588">China</collectingCountry>
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and is obviously Oriental in character (
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<bibRefCitation id="EF9F19B75877A333FBFE9A52FB46FBC5" author="Qiu, Z. D. & D. F. Han & G. Q. Qi & Y. F. Lin" box="[1027,1215,1059,1082]" pageId="2" pageNumber="588" pagination="13 - 32" refId="ref8585" refString="Qiu, Z. D., D. F. Han, G. Q. Qi, and Y. F. Lin. 1985. A preliminary report on a micromammalian assemblage from the hominoid locality of Lufeng, Yunnan. Acta Anthropologica Sinica, 4 (1): 13 - 32. [In Chinese with English summary]" type="journal article" year="1985">Qiu et al., 1985</bibRefCitation>
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).
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</paragraph>
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<paragraph id="8BB164465877A333FD259A30FCB6FA9A" blockId="2.[699,1228,193,1741]" pageId="2" pageNumber="588">
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The Ertemte fauna was first discovered in 1919 and studied by Schlosser in 1924. Recollection in 1980 added a rodent fauna with up to 32 forms and made it the richest fauna among the numerous late Miocene rodent assemblages in North
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<collectingCountry id="F31924D65877A333FC4D9AA7FC0CFB12" box="[944,1013,1238,1261]" name="China" pageId="2" pageNumber="588">China</collectingCountry>
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(
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<bibRefCitation id="EF9F19B75877A333FBF59AA7FB3EFB12" author="Schlosser, M." box="[1032,1223,1238,1261]" pageId="2" pageNumber="588" pagination="1 - 119" refId="ref9156" refString="Schlosser, M. 1924. Tertiary vertebrates from Mongolia. Palaeontologia Sinica C 1 (1): 1 - 119." type="journal article" year="1924">Schlosser, 1924</bibRefCitation>
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;
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<bibRefCitation id="EF9F19B75877A333FD469A85FC34FAF4" author="Fahlbusch, V., Z. D. & G. Storch" box="[699,973,1268,1291]" pageId="2" pageNumber="588" pagination="205 - 224" refId="ref7430" refString="Fahlbusch, V., Z. D. Qiu, and G. Storch. 1983. Neogene mammalian faunas of Ertemte and Harr Obo in Nei Mongol, China. Report on fieldwork in 1980 and preliminary results. Scientia Sinica 26 (2): 205 - 224." type="journal article" year="1983">Fahlbusch et al., 1983</bibRefCitation>
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). It reflects a typical temperate steppe or forest–grassland environment, like that of the present day Palearctic province.
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</paragraph>
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<paragraph id="8BB164465877A333FD259B1DFCAFF96E" blockId="2.[699,1228,193,1741]" pageId="2" pageNumber="588">
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The Yushe faunas (containing Mahui, Gaozhuang, Mazegou, and Haiyan assemblages) and Wenwanggou fauna, spanning from about 6–7 Ma to 2 Ma, have long composites of successive rodents and magnetostratigraphic control (
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<bibRefCitation id="EF9F19B75877A333FC2C9873FB96F9E6" author="Flynn, L. J." box="[977,1135,1538,1561]" pageId="2" pageNumber="588" pagination="95 - 101" refId="ref7482" refString="Flynn, L. J. 1993. A new bamboo rat from the late Miocene of Yushe basin. Vertebrata PalAsiatica 31 (2): 95 - 101. [In Chinese with English summary]" type="journal article" year="1993">Flynn, 1993</bibRefCitation>
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, 1997;
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<bibRefCitation id="EF9F19B75877A333FD469851FC6DF9C8" author="Flynn, L. J. & Z. X. Qiu & N. D. Opdyke & R. H. Tedford" box="[699,916,1568,1591]" pageId="2" pageNumber="588" pagination="365 - 373" refId="ref7612" refString="Flynn, L. J., Z. X. Qiu, N. D. Opdyke, and R. H. Tedford. 1995. Ages of key fossil assemblages in the late Neogene terrestrial record of northern China. In W. Berggren, D. Kent, M. - P. Aubry, and J. Hardenbol (editors), Geochronology, time scales, and global stratigraphic correlation. Society for Economic Paleontology and Mineralogy Special Publication 54: 365 - 373." type="journal article" year="1995">Flynn et al., 1995</bibRefCitation>
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, 1997;
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<bibRefCitation id="EF9F19B75877A333FC0D9851FD03F9AA" author="Zheng, S. H. & Z. Q. Zhang" pageId="2" pageNumber="588" pagination="58 - 71" refId="ref10314" refString="Zheng, S. H., and Z. Q. Zhang. 2000. Late Miocene-Early Pleistocene micromammals from Wenwanggou of Lingtai, Gansu, China. Vertebrata PalAsiatica 38 (1): 58 - 71. [In Chinese with English summary]" type="journal article" year="2000">Zheng and Zhang, 2000</bibRefCitation>
|
||
). They have the potential to provide a key reference for the late Neogene faunas of North
|
||
<collectingCountry id="F31924D65877A333FCF5980BFCA8F96E" box="[776,849,1658,1681]" name="China" pageId="2" pageNumber="588">China</collectingCountry>
|
||
.
|
||
</paragraph>
|
||
<paragraph id="8BB164465877A335FD2598E9FF3FFEEC" blockId="2.[699,1228,193,1741]" lastBlockId="4.[123,652,193,656]" lastPageId="4" lastPageNumber="590" pageId="2" pageNumber="588">
|
||
The Bilike fauna, containing 30 rodents, shows strong similarities with the Ertemte fauna and represents, on the whole, a sort of modernized Ertemte fauna (
|
||
<bibRefCitation id="EF9F19B75871A335FE379EAFFF43FEEC" author="Qiu, Z. D. & G. Storch" pageId="4" pageNumber="590" pagination="173 - 229" refId="ref8794" refString="Qiu, Z. D., and G. Storch. 2000. The early Pliocene micromammalian fauna of Bilike, Inner Mongolia, China (Mammalia: Lipotyphla, Chiroptera, Rodentia, Lagomorpha. Senckenbergiana Lethaea 80 (1): 173 - 229." type="journal article" year="2000">Qiu and Storch, 2000</bibRefCitation>
|
||
).
|
||
</paragraph>
|
||
<caption id="DF7134CE5876A332FF6B982DFB50F98E" box="[150,1193,1628,1649]" pageId="3" pageNumber="589" startId="3.[150,188,1628,1649]" targetBox="[187,1166,189,1607]" targetPageId="3" targetType="figure">
|
||
<paragraph id="8BB164465876A332FF6B982DFB50F98E" blockId="3.[150,1193,1628,1649]" box="[150,1193,1628,1649]" pageId="3" pageNumber="589">Fig. 22.2. Correlation of Chinese Neogene biochrons with those of Europe and North America.</paragraph>
|
||
</caption>
|
||
<paragraph id="8BB164465871A335FF659F68FEF0FE5A" blockId="4.[123,652,193,656]" pageId="4" pageNumber="590">
|
||
The Daodi fauna is a younger Neogene assemblage with 13 wellrepresented rodents and one of the best records of a late Pliocene small mammal community in North
|
||
<collectingCountry id="F31924D65871A335FDBB9F00FD72FE77" box="[582,651,369,392]" name="China" pageId="4" pageNumber="590">China</collectingCountry>
|
||
(
|
||
<bibRefCitation id="EF9F19B75871A335FF7E9FFFFF04FE5A" author="Cai, B. Q." box="[131,253,398,421]" pageId="4" pageNumber="590" pagination="124 - 136" refId="ref7099" refString="Cai, B. Q. 1987. A preliminary report on the late Pliocene micromammalian fauna from Yangyuan and Yuxian, Hebei. Vertebrata PalAsiatica 25 (2): 124 - 136. [In Chinese with English summary]" type="journal article" year="1987">Cai, 1987</bibRefCitation>
|
||
).
|
||
</paragraph>
|
||
<paragraph id="8BB164465871A335FF659FDDFE5FFD6F" blockId="4.[123,652,193,656]" pageId="4" pageNumber="590">
|
||
The Wushan fauna from cave deposits of Central
|
||
<collectingCountry id="F31924D65871A335FF269FB8FED9FE1F" box="[219,288,457,480]" name="China" pageId="4" pageNumber="590">China</collectingCountry>
|
||
consists of 30 rodents. It was considered Pleistocene in age by Zheng in 1993. The assemblage represents the youngest Neogene fauna, that is, late Pliocene rather than Pleistocene in age, if the age interpretation of 2 Ma for the locality is correct (
|
||
<bibRefCitation id="EF9F19B75871A335FF7E9C08FE60FD6F" author="Huang, W. P. & Q. R. Fang" box="[131,409,633,656]" pageId="4" pageNumber="590" refId="ref7746" refString="Huang, W. P., and Q. R. Fang. 1991. The ruins of Wushan Man. Beijing: China Ocean Press, 229 pp. [In Chinese with English summary]" type="book" year="1991">Huang and Fang, 1991</bibRefCitation>
|
||
).
|
||
</paragraph>
|
||
</subSubSection>
|
||
</treatment>
|
||
</document> |