Nearshore zone +1, Villanow Quadrangle, Dug Gap Road: Caradoc, Georgia

List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
Rhynchonellata - Rhynchonellida - Ancistrorhynchidae
Ancistrorhyncha costata Ulrich and Cooper 1942
Ulrich & Cooper
Rhynchonellata - Rhynchonellida - Orthorhynchulidae
Orthorhynchula linneyi (James 1881)
James
Rhynchonellata - Rhynchonellida - Rhynchotrematidae
Rhynchotrema minnesotensis
Sandeson
Rhynchotrema increbescens (Hall 1847)
Hall
Rhynchonellata - Rhynchonellida - Camarotoechiidae
Camarotoechia sp. Hall and Clarke 1893
Rhynchonellata - Atrypida - Anazygidae
Zygospira recurvirostris (Hall 1847)
recombined as Anazyga recurvirostra
Hall
Strophomenata - Strophomenida - Sowerbyellidae
Sowerbyella sp. Jones 1928
see common names

Geography
Country:United States State/province:Georgia County:Whitfield
Coordinates: 34.7° North, 85.0° West (view map)
Paleocoordinates:29.5° South, 66.0° West
Basis of coordinate:estimated from map
Geographic resolution:small collection
Time
Period:Ordovician Epoch:Late/Upper Ordovician
10 m.y. bin:Ordovician 4-5
*Period:Middle Ordovician - Late/Upper Ordovician
Key time interval:Caradoc
Age range of interval:458.40000 - 449.60000 m.y. ago
* legacy (obsolete) database fields
Stratigraphy
Stratigraphy comments: No information given.
Lithology and environment
Primary lithology:red,yellow siltstone
Secondary lithology:yellow sandstone
Includes fossils?Y
Lithology description: \"The upper one-fourth of the zone is composed of red to yellow siltstone with an occasional mottled bed showing purplish splotches. A fine-grained, buff-colored sandstone occurs about 45 feet below the top of the zone. The middle part of the zone is composed of red siltstone. The lower half of the zone is composed of red and yellow alternating beds of thinly laminated siltstone. About 5 feet above the base occurs a fossil horizon containing both identifiable and unidentifiable fragments of brachiopods and bryozoa. The lowest member of the zone is a bed of medium-grained yellowish sandstone about 2 to 4 feet thick. In some sections small pebbles randomly scattered through it give it a loose conglomeratic texture."
Environment:shallow subtidal indet.
Taphonomy
Size of fossils:macrofossils
Collection methods and comments
Collection excludes:difficult macrofossils
Collection methods:field collection
Reason for describing collection:biostratigraphic analysis
Metadata
Database number:32457
Authorizer:S. Holland Enterer:T. Hanson
Modifier:S. Holland Research group:marine invertebrate
Created:2003-07-01 14:05:31 Last modified:2004-10-20 09:27:39
Access level:the public Released:2003-07-01 14:05:31
Creative Commons license:CC BY
Reference information

Primary reference:

8741. A. T. Allen and J. G. Lester. 1957. Zonation of the Middle and Upper Ordovician strata in northwestern Georgia. Georgia State Division of Conservation, the Geological Survey Bulletin 66:1-104 [S. Holland/T. Hanson/T. Hanson]