Heti Formation F 11 (Eocene of China)

Also known as 5310, Hoti-Tsun, Hedicun, Anwo, Locality 11

Where: Shanxi, China (35.0° N, 111.8° E: paleocoordinates 36.0° N, 105.8° E)

• coordinate stated in text

• outcrop-level geographic resolution

When: Rencun Member (Heti Formation), Sharamurunian (56.0 - 37.7 Ma)

• the Hedi Formation is now known as the Heti Formation and is Sharamurunian; this locality is in the Rencun Member (Beard and Wang 2004)

Environment/lithology: terrestrial

• Yuanqu basin

Size class: macrofossils

Collection methods: bulk,

Primary reference: C. Young. 1937. An early Tertiary vertebrate fauna from Yuanchü. Bulletin of the geological society of China 17(3-4):413-438 [J. Alroy/S. Kuemmell/S. Kuemmell]more details

Purpose of describing collection: taxonomic analysis

PaleoDB collection 42196: authorized by John Alroy, entered by Susanna Kümmell on 26.07.2004

Creative Commons license: CC BY (attribution)

Taxonomic list

Show authors, comments, and common names
Mammalia
 Artiodactyla - Helohyidae
Gobiohyus yuanchuensis n. sp.
Gobiohyus yuanchuensis n. sp. Young 1937 even-toed ungulate
originally it is written: yuanchüensis
 Artiodactyla - Anthracotheriidae
Anthracosenex ambiguus
Anthracosenex ambiguus Zdansky 1930 anthracothere
 Perissodactyla - Deperetellidae
"Diplolophodon major n. sp." = Bahinolophus birmanicus
"Diplolophodon major n. sp." = Bahinolophus birmanicus Pilgrim 1925 odd-toed ungulate