Jg. Sha et Ja. Grantmackie, LATE PERMIAN TO MIOCENE BIVALVE ASSEMBLAGES FROM HOHXIL, QINGHAI-XIZANG PLATEAU, CHINA, Journal of the Royal Society of New Zealand, 26(4), 1996, pp. 429-455
Nine fossil bivalve assemblages have been recognized in the Hohxil des
ert area of western Qinghai, China: Wuchiapingian Netschajewia jiangsu
ensis assemblage, Smithian - Spathian Bakevellia costata - Leptochondr
ia virgalensis - Entolium microtis assemblage, Carnian Halobia austria
ca - Halobia yunnanensis - Halobia convexa assemblage, Norian Halobia
yandongensis - Halobia aff. dilatata assemblage, Carnian-Norian Trigon
odus carniolicus - Unionites? rhomboidalis assemblage, Bathonian Kimme
ridgian Radulopecten pamirensis - Protocardia stricklandi assemblage,
Late Jurassic Pseudolimea - Opis assemblage, Early Cretaceous Eokorean
aia qinghaiensis assemblage, and Miocene Sphaerium nitidum assemblage.
The marine bivalves, except for the cosmopolitan Halobia, are Tethyan
and characterised mainly the northern margin of the Tethys. Non-marin
e taxa are restricted Asian forms. These assemblages are very signific
ant in studying the biostratigraphy, paleobiogeography and tectonic hi
story of the Qinghai - Xizang Plateau. In the Early Cretaceous marine
connections were broken and the area has experienced since then only t
errestrial conditions.