Where: Tibet, China (31.5° N, 79.8° E: paleocoordinates 29.4° N, 80.4° E)
• coordinate based on nearby landmark
• small collection-level geographic resolution
When: Zanda Formation, MN 14 (4.9 - 4.2 Ma)
• said to be "early Pliocene (~4.4 Ma)" (presumably based on paleomagnetic stratigraphy), i.e., MN 14
• group of beds-level stratigraphic resolution
Environment/lithology: "floodplain"; sandy siltstone and claystone
Size class: macrofossils
Reposited in the IVPP
Primary reference: T. Deng, X. Wang, M. Fortelius, Q. Li, Y. Wang, Z. J. Tseng, G. T. Takeuchi, J. E. Saylor, L. K. Säilä and G. Xie. 2011. Out of Tibet: Pliocene woolly rhino suggests high-plateau origin of Ice Age megaherbivores. Science 333:1285-1288 [J. Alroy/J. Alroy/J. Alroy]more details
Purpose of describing collection: taxonomic analysis
PaleoDB collection 115623: authorized by John Alroy, entered by John Alroy on 02.09.2011
Creative Commons license: CC BY (attribution)
Taxonomic list
unclassified | |
Mammalia | |
Prosiphneus cf. eriksoni rodent | |
Cricetidae "n. gen." Fischer von Waldheim 1817 rodent
Nannocricetus sp. Schaub 1934 rodent | |
Trischizolagus cf. dumitrescuae Radulesco and Samson 1967 rabbit | |
Ochotona "sp. 3" Link 1795 pika | |
Soricidae indet. Fischer 1814 shrew | |
Bovidae "gen. B" Gray 1821 antelope
Bovidae "gen. A" Gray 1821 antelope | |
Mustela sp. Linnaeus 1758 weasel | |
Panthera (Uncia) "n. sp." Oken 1816 cat | |
Vulpes "n. sp." Frisch 1775 fox |