Geodiversitas | |
Pliocene suids from Musaitu and Dermenji, Moldova: implications for understanding the origin of African Kolpochoerus Van Hoepen & Van Hoepen, 1932 | |
Théodor Obada1  Martin Pickford1  | |
关键词: Moldova; Pliocene; Suidae; Dasychoerus; Kolpochoerus; Evolution; Palaeobiogeography; Moldavie; Pliocène; Suidae; Dasychoerus; Kolpochoerus; évolution; Paléobiogéographie; | |
DOI : 10.5252/g2016n1a5 | |
学科分类:生物科学(综合) | |
来源: Museum National d Histoire Naturelle | |
【 摘 要 】
EarlyPliocenesuidsofEuropearegenerallyrareandpoorlypreserved,butsomeexceptionalfossilshavebeenfoundatRoussillon,France,Villafrancad'Asti,Italy,andKvabebi,Georgia.WeheredescribeandinterpretanalmostcompleteskullofasmallsuidfromMusaituandamandiblefragmentfromDermenji,Moldova,whichaddpreciousinformationtothedatabaseconcerningthesesmallEuropeanPliocenesuids,hereattributedtoDasychoerusarvernensis(Croizetamp;Jobert,1828).TheMoldovanfossilsprovideanimportantbiogeographiclinkbetweentheWesternEuropeanandAsianPlio-Pleistocenesuines.TheMusaituskull,inparticular,showstheelongatedsnout,enlargedcanineflanges,pneumatisedzygomaticarchandlowslungincisorrowcharacteristicofthegenusDasychoerusGray,1873.ThisspeciesisimportantbecauseitrepresentsthegroupfromwhichtheAfricanKolpochoerusVanHoepenamp;VanHoepen,1932lineageprobablyemerged.Thelattergroupisusefulforbiochronologybecause,havingarrivedinAfrica,whereithasbeencalledKolpochoerusdeheinzeliniBrunetamp;White,2001(infactajuniorsynonymofDasychoerusarvernensis)itevolvedrapidlyindimensionsanddentalmorphology.DuringthePliocenethegenusDasychoerus,alreadyadaptedtotropicalandsub-tropicalclimates,waswidespreadinmid-latitudeEurasiaandAfrica,butwhenmuchofmid-latitudeEurasiabecameborealduringthePlio-Pleistocene,therangeofDasychoerusshrankequatorwards,givingwaytoboreallyadaptedSusscrofaLinnaeus,1758overmuchofitsformerterritory,leavingadisjunctdistributionofitsdescendantsinAfrica(HylochoerusThomas,1904,possiblyPotamochoerusGray,1854)andthetropicalislandsoftheFarEast(Dasychoerus).
【 授权许可】
Unknown
【 预 览 】
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RO201912090770180ZK.pdf | 4603KB | download |