Active Plum Run Quarry section, (9.0 m height, Peebles Dolomite), Adams Co., Ohi: Sheinwoodian, Ohio

List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Conodonta - Panderodontida - Panderodontidae
Panderodus unicostatus (Branson and Mehl 1933)
1 element
Conodonta - Ozarkodinida
Ozarkodina confluens (Rhodes 1953)
2 elements
see common names

Geography
Country:United States State/province:Ohio County:Adams
Coordinates: 39.0° North, 83.4° West (view map)
Paleocoordinates:28.3° South, 51.2° West
Basis of coordinate:stated in text
Time
Period: Silurian Epoch: Wenlock
Stage: Sheinwoodian 10 m.y. bin: Silurian 2
*International age/stage:Sheinwood
Key time interval: Sheinwoodian Zone:  Ozarkodina? crassa
Age range of interval: 433.4 - 430.5 m.y. ago
* legacy (obsolete) database fields
Stratigraphy
Formation:Peebles Dolomite Local bed:83MK3, 9.0 m
Lithology and environment
Primary lithology: dolomite
Environment:shallow subtidal indet.
Geology comments: Vuggy, according to strat column. Fossiliferous. Pervasive dolomitization, difficulty in determining original carbonate textures. No (almost) qtz. silt. Probably skeletal packstones. Abundant skeletal material only in lower Peebles beds, corresponds with rapid increase in upper beds of gypsum crystals. Poor preservation of conodonts in Peebles indicates most or all are allocthonous. Very shallow, high energy water, increasing salinity.
Taphonomy
Modes of preservation:body
Collection methods and comments
Reason for describing collection:biostratigraphic analysis
Taxonomic list comments:Conodonts only. Author does indicate there are other taxa present.
Metadata
Database number:1163
Authorizer:J. Alroy Enterer:M. Sommers
Modifier:J. Alroy Research group:marine invertebrate
Created:1999-03-16 18:06:18 Last modified:2006-09-14 19:58:14
Access level:the public Released:2000-11-20 13:53:11
Creative Commons license:CC BY
Reference information

Primary reference:

35. M. A. Kleffner. 1990. Wenlockian (Silurian) conodont biostratigraphy, depositional environments, and depositional history along the eastern flank of the Cincinnati Arch in southern Ohio. Journal of Paleontology 64(2):319-328 [J. Alroy/M. Sommers/J. Alroy]