古脊椎动物学报
古脊椎動物學報
고척추동물학보
VERTEBRATA PALASIATICA
2010年
4期
328-335
,共8页
Mary R.DAWSON%李传夔%齐陶
Mary R.DAWSON%李傳夔%齊陶
Mary R.DAWSON%리전기%제도
亚洲%始新世%啮齿目%硅藻鼠科%双脊齿型颊齿
亞洲%始新世%齧齒目%硅藻鼠科%雙脊齒型頰齒
아주%시신세%교치목%규조서과%쌍척치형협치
Asia%Eocene%Rodentia%Diatomyidae%bilophodont cheek teeth
亚洲特有的啮齿类硅藻鼠科自渐新世以来分布于东亚和南亚.现生硅藻鼠类的分布只限于老挝的喀斯特地区.就目前所知,这些具有豪猪型头骨一松鼠型下颌的啮齿类的颊齿都是不同程度的横向双脊齿.时代最早的硅藻鼠类产于巴基斯坦渐新世地层中,其颊齿的双脊齿构造上仍保留齿尖残迹,基本符合双脊齿型牙齿结构.至渐新世末期,硅藻鼠科的牙齿出现分化.中新世及以后硅藻鼠类的化石记录相对较少.分子生物学证据将硅藻鼠类归入Ctenohystrica,这种归属也从始新世梳趾鼠类的臼齿形态上得到一定的支持.除此之外,有关硅藻鼠类的起源问题几乎一无所知.亚洲中始新世的Hydentomys臼齿表现出轻微的双脊型,然而其他方面却与硅藻鼠类不同.另一个具双脊齿的啃齿类Dolosimus(新属)产于江苏中始新世,其具有更为发育的双脊齿,特别是臼齿型下牙.新属的不完整记录及其形态不能解决如下问题:它是否与后来出现的像硅藻鼠类和跃兔类这些具有明显双脊齿型颊齿的啮齿类有亲缘关系,或者只是这种形态发育中没有留下后继者的早期试验品.
亞洲特有的齧齒類硅藻鼠科自漸新世以來分佈于東亞和南亞.現生硅藻鼠類的分佈隻限于老撾的喀斯特地區.就目前所知,這些具有豪豬型頭骨一鬆鼠型下頜的齧齒類的頰齒都是不同程度的橫嚮雙脊齒.時代最早的硅藻鼠類產于巴基斯坦漸新世地層中,其頰齒的雙脊齒構造上仍保留齒尖殘跡,基本符閤雙脊齒型牙齒結構.至漸新世末期,硅藻鼠科的牙齒齣現分化.中新世及以後硅藻鼠類的化石記錄相對較少.分子生物學證據將硅藻鼠類歸入Ctenohystrica,這種歸屬也從始新世梳趾鼠類的臼齒形態上得到一定的支持.除此之外,有關硅藻鼠類的起源問題幾乎一無所知.亞洲中始新世的Hydentomys臼齒錶現齣輕微的雙脊型,然而其他方麵卻與硅藻鼠類不同.另一箇具雙脊齒的啃齒類Dolosimus(新屬)產于江囌中始新世,其具有更為髮育的雙脊齒,特彆是臼齒型下牙.新屬的不完整記錄及其形態不能解決如下問題:它是否與後來齣現的像硅藻鼠類和躍兔類這些具有明顯雙脊齒型頰齒的齧齒類有親緣關繫,或者隻是這種形態髮育中沒有留下後繼者的早期試驗品.
아주특유적교치류규조서과자점신세이래분포우동아화남아.현생규조서류적분포지한우로과적객사특지구.취목전소지,저사구유호저형두골일송서형하합적교치류적협치도시불동정도적횡향쌍척치.시대최조적규조서류산우파기사탄점신세지층중,기협치적쌍척치구조상잉보류치첨잔적,기본부합쌍척치형아치결구.지점신세말기,규조서과적아치출현분화.중신세급이후규조서류적화석기록상대교소.분자생물학증거장규조서류귀입Ctenohystrica,저충귀속야종시신세소지서류적구치형태상득도일정적지지.제차지외,유관규조서류적기원문제궤호일무소지.아주중시신세적Hydentomys구치표현출경미적쌍척형,연이기타방면각여규조서류불동.령일개구쌍척치적습치류Dolosimus(신속)산우강소중시신세,기구유경위발육적쌍척치,특별시구치형하아.신속적불완정기록급기형태불능해결여하문제:타시부여후래출현적상규조서류화약토류저사구유명현쌍척치형협치적교치류유친연관계,혹자지시저충형태발육중몰유류하후계자적조기시험품.
The Asian endemic rodent family Diatomyidae is known to have inhabited eastern and southern Asia since the Oligocene.Its current distribution is limited to karstic regions of Laos.So far as known these hystricomorphous-sciurognathous rodents have some degree of transverse bilophodonty of the cheek teeth.The earliest recognized diatomyids,which are from the Oligocene of Pakistan,retain some traces of cusps on the cheek teeth,overlying the basically bilophodont tooth structure.By the end of the Oligocene there is some dental diversity within the family.Miocene and later diatomyids are relatively rare in the fossil record.Molecular evidence unites the diatomyids in the Ctenohystrica,an assignment that receives some support from the molar morphology of Eocene ctenodactyloids.Other than this connection.little is clear regarding the origin of the diatomyids.The middle Eocene Asian Hydentomys exhibits a slight degree of bilophodonty,but is otherwise unlike diatomyids.Another taxon of bilophodont rodent,Dolosimus n.gen.from the middle Eocene of Jiangsu Province,has still more precocious development of bilophodonty,especially in the lower molariform teeth.The incomplete record of this new taxon as well as its morphology cannot answer the question of whether this taxon is allied to such later appearing,strongly bilophodont rodents as diatomyids and pedetids,or is an early experiment of this striking morphological development that left no successors.