Where: Japan (33.6° N, 130.3° E: paleocoordinates 40.0° N, 126.2° E)
• coordinate based on nearby landmark
• outcrop-level geographic resolution
When: Meinohama Group, Rupelian (33.9 - 28.1 Ma)
• The Meinohama Sandstone (or Formation, or Group) is correlative with the Kishima Group and the lowest part of the Ashiya Group. The Ashiya Group corresponds to Zones P21-"N4" of Blow's scale of planktonic foraminifera (Saito & Okada, 1984; Tsuchi et al., 1987) and Zones CP18-CP19b of calcareous nannoplankton (Okada & Bukry, 1980). The fission track age of the bottom of the Yamaga Formation is about 32 Ma (Ozaki & Hamasaki, 1991). Okada (1992) showed that the Yamaga and Sakamizu Formations were assigned to Zone CP19a (latest Rupelian-early Chattian) of calcareous nannoplankton. Miyachi & Sakai (1991) obtained fission track ages of 33.9 Ma for the Sari Formation, the second-lowest in the Kishima Group, consistent with nannoplankton biostratigraphy suggesting a CP16a zone for the underlying Kishima Formation (Okada, 1992). Together, the evidence suggests a Rupelian age for the Meinohama Group.
• group of beds-level stratigraphic resolution
Environment/lithology: coastal; lithified sandstone
Size class: macrofossils
Collected by T. Sumitomo, H. Yabe, T. Nagao
Primary reference: T. Nagao. 1926. Aturia yokoyamai, nov. nom., from the Palaeogene of Kyushu. Science Reports of the Tohoku Imperial University, 2nd Series, Geology 9:29-32 [M. Clapham/M. Clapham]more details
Purpose of describing collection: taxonomic analysis
PaleoDB collection 179888: authorized by Matthew Clapham, entered by Matthew Clapham on 03.07.2016, edited by Mark Uhen
Creative Commons license: CC BY (attribution)
Taxonomic list
Cephalopoda | |
Aturia yokoyamai Nagao 1926 nautiloid | |
Bivalvia | |
Parapholas satoi n. sp.
Parapholas satoi n. sp. Nagao 1928 clam |