Sample II8P13L202, Shenjiawan, Changma, Yumen City (Cretaceous of China)

Where: Gansu, China (39.9° N, 96.8° E: paleocoordinates 39.5° N, 98.5° E)

• coordinate estimated from map

• outcrop-level geographic resolution

When: Chijinpu Formation, Early/Lower Aptian (121.4 - 122.5 Ma)

• The combined biostratigraphic and numerical age data suggest that the Changma Basin began accumulating sediment no older than Hauterivian (based on pollen records), is older than the Coniacian (based on the crosscutting dykes), but is likely Barremian to Aptian based on the similarities to the Jehol biota (Suarez et al., 2013)

Environment/lithology: lacustrine; lithified, brown, yellow mudstone

• The formation is 591 m in thickness and composed of yellow – brown coarse clastic sediment interbedded with some siltstone and mudstone.

Size classes: macrofossils, mesofossils

Preservation: mold/impression

Collection methods: Repository: Tianjin Institute of Geology and Mineral Resources

Primary reference: Y. C. Hong. 1982. Mesozoic Fossil Insects of Jiuquan Basin in Gansu Province 1-187 [M. Clapham/M. Clapham]more details

Purpose of describing collection: taxonomic analysis

PaleoDB collection 155044: authorized by Matthew Clapham, entered by Matthew Clapham on 27.03.2014

Creative Commons license: CC BY (attribution)

Taxonomic list

Insecta
 Coleoptera -
Mesotricupes lineatus n. gen. n. sp., Synodus changmaensis n. gen. n. sp.
Mesotricupes lineatus n. gen. n. sp. Hong 1982 beetle
Kj1165-1
Synodus changmaensis n. gen. n. sp. Hong 1982 beetle
Kj1161