Where: Japan (32.7° N, 129.8° E: paleocoordinates 38.0° N, 124.3° E)
• coordinate estimated from map
• small collection-level geographic resolution
When: Okinoshima Formation, Bartonian (41.3 - 38.0 Ma)
• Lower to middle part of the Okinoshima Formation. According to foraminiferal and molluscan biostratigraphy, the formation is assigned in age to the Auverisian to the Bartonian (Upper Eocene). The Okinoshima Formation falls within calcareous nannofossil Subzones CP14a–CP15b of Okada and Bukry (1980) and planktic foraminiferal Zones E10–E13 of Berggren and Pearson (2005), dating to the middle Eocene. The Okinoshima Formation including calcareous nannofossils such as Reticulofenestra umbilica and Discoaster barbadiensis, indicating Zones CP14–CP15 and planktic foraminifer, Acarinina primitiva, representing Zone P14 or older (Yamaguchi et al. 2004). These biozones of planktic microfossils assign the Okinoshima Formation to 43.5–39.0 Ma (Yamaguchi & Kamiya, 2007).
• bed-level stratigraphic resolution
Environment/lithology: offshore; lithified, fine-grained, glauconitic sandstone
Size class: macrofossils
Collected by K. Tanabe
• Repository: Department of Earth Sciences, Ehime University
Primary reference: K. Tanabe and N. Chiba. 1983. A new species of Deltoidonautilus (Cephalopoda) from the upper Eocene of western Kyushu. Venus (Japanese Journal of Malacology) 42:248-258 [M. Clapham/M. Clapham]more details
Purpose of describing collection: taxonomic analysis
PaleoDB collection 179880: authorized by Matthew Clapham, entered by Matthew Clapham on 03.07.2016
Creative Commons license: CC BY (attribution)
Taxonomic list
Cephalopoda | |
Deltoidonautilus okinoshimensis n. sp. Tanabe and Chiba 1983 nautiloid |