Also known as Linnania progressus type
Where: Guangdong, China (25.1° N, 114.3° E: paleocoordinates 25.7° N, 109.2° E)
• coordinate based on political unit
• small collection-level geographic resolution
When: Shanghu Formation, Early/Lower Paleocene (66.0 - 61.7 Ma)
• Upper part of the Shanghu Formation
• bed-level stratigraphic resolution
Environment/lithology: terrestrial; lithology not reported
Size class: macrofossils
Collected in 1973; reposited in the IVPP
Primary reference: X.-S. Huang. 2006. A new anagalid (Anagalida, Mammalia) from the Paleocene of Nanxiong basin, Guangdong province. Vertebrata PalAsiatica 44(3):274-277 [P. Mannion/P. Mannion]more details
Purpose of describing collection: taxonomic analysis
PaleoDB collection 139602: authorized by Philip Mannion, entered by Philip Mannion on 14.02.2013
Creative Commons license: CC BY (attribution)
Taxonomic list
| Mammalia | |
Linnania progressus n. sp.
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Dysnoetodon minuta n. gen. n. sp.2 Zhang 1980 tillodont IVPP V5837 (maxilla and associated lower jaw) and V5838 (left m2) - holotype
Huananius youngi n. gen. n. sp.1 Huang and Zheng 1999 pantodont IVPP V11700 - holotype (fragmentary upper right jaw and partial lower right jaw from the same individual)
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