Also known as IGPS loco no. So-13
Where: Shinozuka, Japan (34.7° N, 139.0° E: paleocoordinates 35.2° N, 138.4° E)
• coordinate stated in text
• outcrop-level geographic resolution
When: Harada Formation (Shirahama Group), Piacenzian (3.6 - 2.6 Ma)
• The nannofossil assemblage from the Harada Formation in the upper part of this group is characterized by the occurrence of Pseudoemiliania cf. lacunosa, without Reticulofenestra pseudoumbilica and Gephyrocapsa spp. (Okada, 1987). According to Blow (1969) and Okada and Bukry (1980), this group belongs to zones N19 and CN12 (early Piacenzian), according to Akimoto et al. (2012). Utagawa et al. (2015) dated andesite in the underlying Suzaki Formation at 3.62 +/- 0.16 Ma by K-Ar.
• group of beds-level stratigraphic resolution
Environment/lithology: poorly lithified, tuffaceous, calcareous sandstone
Size class: macrofossils
Primary reference: K. M. Hatai. 1940. The Cenozoic Brachiopoda of Japan. Science Reports, Tohoku Imperial University, Series 2 20:1-413 [M. Clapham/M. Clapham]more details
Purpose of describing collection: taxonomic analysis
PaleoDB collection 190824: authorized by Matthew Clapham, entered by Matthew Clapham on 18.12.2017, edited by Mark Uhen
Creative Commons license: CC BY (attribution)
Taxonomic list
Echinoidea | |
Pseudocentrotus stenoporus n. sp.
Pseudocentrotus stenoporus n. sp. Nisiyama 1966 sea urchin | |
Rhynchonellata | |
Jolonica (Kamoica) iduensis Hatai 1936 | |
Terebratulina sirahamensis n. sp., Terebratulina iduensis n. sp.
Terebratulina sirahamensis n. sp. Hatai 1940
Terebratulina iduensis n. sp. Hatai 1936 |