T. Qi et Kc. Beard, LATE EOCENE SIVALADAPID PRIMATE FROM GUANGXI-ZHUANG AUTONOMOUS REGION, PEOPLES-REPUBLIC-OF-CHINA, Journal of Human Evolution, 35(3), 1998, pp. 211-220
A new genus and species of Sivaladapidae is described from the late Eo
cene Gongkang Formation, Yongle Basin, western Guangxi Zhuang Autonomo
us Region, southern China. Guangxilemur tongi, new genus and species,
shows a combination of traits that occur separately in earlier and mor
e primitive Asian adapiforms (Hoanghonius and Rencunius) and in Miocen
e sivaladapines (Sivaladapis and Sinoadapis). Phylogenetic analysis of
dental characters suggests that Guangxilemur is closely related to th
e Miocene sivaladapine clade. Miocene sivaladapines were the latest su
rviving members of a broad radiation of Eocene adapiforms in Asia that
included Hoanghonius, Rencunius, and Wailekia in addition to Guangxil
emur. European Periconodon may also be specially related to this prima
rily Asian clade, but current anatomical data are insufficient to test
this possibility adequately. Sivaladapine adapiforms and tarsiid tars
iiforms maintained relictual distributions in southern and/or southeas
tern Asia far beyond the extirpation of their closest relatives on oth
er Holarctic continents near the Eocene-Oligocene boundary. This tempo
ral persistence was mediated by Asian paleogeography, which allowed vi
rtually continuous access to tropical refugia during a middle Cenozoic
interval of climatic deterioration that coincided with the extinction
of adapiforms and tarsiiforms in Europe and North America. (C) 1998 A
cademic Press.