Where: Marshall Islands (11.4° N, 162.4° E: paleocoordinates 4.0° N, 176.0° W)
When: Priabonian (38.0 - 33.9 Ma)
• Late Eocene, Tertiary b. Cole (1957, p. 749) places the top of the Eocene at 2,780 feet on the basis of the first appearance of a diagnostic smaller Foraminifera, Pseudochrysalidina. Todd and Low (1960, p. 807) place the top of the Eocene at 2,770 feet. The writer accepts 2,780 feet as the top because of the appearance of a different lithology. Chips that appear at this depth show strong solution features, such as molds, which indicate that a solution unconformity separates the rocks of Eocene and Miocene age, just as the Miocene e sediments are separated from younger rocks by a similar but better developed unconformity.
• group of beds-level stratigraphic resolution
Environment/lithology: perireef or subreef; lithified limestone
Size class: macrofossils
Reposited in the USNM
Collection methods: core
Primary reference: P. M. Kier. 1964. Fossil echinoids from the Marshall Islands. United States Geological Survey Professional Paper 260-GG:1121-1126 [M. Clapham/M. Clapham]more details
Purpose of describing collection: taxonomic analysis
PaleoDB collection 195885: authorized by Matthew Clapham, entered by Matthew Clapham on 29.08.2018
Creative Commons license: CC BY (attribution)
Taxonomic list
Echinoidea | |
Echinocyamus petalus Kier 1964 sand dollar |