Harvey Site - D: Bartonian, Louisiana

List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
unclassified
Pilicatula filamentosa
1 individual
Pilicatula filamentosa concentrica
Polyplacophora - Chitonida - Chitonidae
Chiton sp. Linnaeus 1758
1 individual
Scaphopoda - Dentaliida - Dentaliidae
Dentalium minutistriatum Gabb 1850
5 individuals
Gastropoda - Turritellidae
Turritella dutexata Harris 1895
2 individuals
[entered as Turritella detexata]
Gastropoda - Neogastropoda - Olividae
Ancilla staminea Conrad 1832
2 individuals
Ancilla staminea punctulifera
Gastropoda - Neogastropoda - Fasciolariidae
Latirus moorei Gabb 1860
1 individual
Gastropoda - Neogastropoda - Volutidae
Athleta petrosus (Conrad 1833)
14 individuals
recombined as Athleta petrosa
Gastropoda - Neogastropoda - Marginellidae
Marginella (Dentimargo) constrictoides
1 individual
Gastropoda - Neogastropoda - Turridae
Coronia margaritosa
1 individual
spelled with current rank as Gemmula (Coronia)
Gastropoda - Heterostropha - Architectonicidae
Architectonica sp. Röding 1798
1 individual
Gastropoda - Solariellidae
Solariella tricostata Conrad 1833
1 individual
Gastropoda - Opisthobranchia - Retusidae
Retusa (Cylichnina) galba (Conrad 1833)
3 individuals
Bivalvia - Nuculida - Nuculidae
Nucula (Nucula) mauricensis (Harris 1919)
38 individuals
Bivalvia - Pholadida - Corbulidae
Caestocorbula fossata
24 individuals
Bivalvia - Cardiida - Veneridae
Callista (Callista) perovata (Conrad 1833)
37 individuals
Callista (Callista) perovata lisbone
Bivalvia - Carditida - Crassatellidae
Crassatella texalta Harris 1895
1 individual
Bivalvia - Carditida - Carditidae
Venericardia (Rotundicardia) rotunda (Lea 1833)
15 individuals
Venericardia (Venericor) sp. Stewart 1930
1 individual
Bivalvia - Pectinida - Pectinidae
Eburneopecten sp. (Conrad 1865)
86 individuals
Bivalvia - Ostreida - Ostreidae
Cubitostrea sellaeformis (Conrad 1832)
21 individuals
Bivalvia - Arcida - Arcidae
Barbatia (Cucullaearca) ludoviciana
1 individual
Bivalvia - Arcida - Glycymerididae
Glycymeris trigonella (Conrad 1833)
18 individuals
original and current combination Pectunculus trigonella
Gymnolaemata - Cheilostomata - Lepraliellidae
Holoporella granulosa
3 individuals
synonym of Celleporaria
Gymnolaemata - Cheilostomata - Lunulitidae
Lunulites sp. Lamarck 1816
4 individuals
Thecostraca - Calanticomorpha - Calanticidae
Euscalpellum eocenense (Meyer 1885)
1 individual
Anthozoa - Scleractinia - Dendrophylliidae
Balanophyllia sp. Wood 1844
2 individuals
Endopachys lonsdalei Vaughan 1900
5 individuals
Anthozoa - Scleractinia - Flabellidae
Flabellum cuneiforme (Lonsdale 1845)
1 individual
Flabellum cuneiforme pachyphyllum
see common names

Geography
Country:United States State/province:Louisiana County:Jackson
Coordinates: 32.3° North, 92.7° West (view map)
Paleocoordinates:33.4° North, 83.8° West
Basis of coordinate:based on nearby landmark
Time
Period:Paleogene Epoch:Eocene
Stage:Bartonian 10 m.y. bin:Cenozoic 3
Key time interval:Bartonian
Age range of interval:41.20000 - 37.71000 m.y. ago
Stratigraphy
Geological group:Claiborne Formation:Cook Mountain
Stratigraphic resolution:bed
Stratigraphy comments: "Three samples from the site were strontium dated forty-five million years old"
Ivany - Cook Mt is Bartonian
Lithology and environment
Primary lithology:gray,red unlithified sandy claystone
Includes fossils?Y
Lithology description: "2'9" Gray and Reddish Orange Variegated Sandy Clay"
Environment:marginal marine indet. Tectonic setting:passive margin
Glacial or sequence phase:transgressive
Geology comments: "The Clairborn Group is composed of a transgressive sequence including the Cane River, Sparta, Cook Mountain, and Cockfield (Rainwater, 1982). Cockfield fluvial deposits are also present in this area. The Cook Mountain Formation was deposited during the latter part of the Clairborne stage of the Tejas sequence. It shows a transgression with the influence from the Mississippi and possibly a Ouachita source (McCarley, 1981). The Laramide and Mexican Cordilleran orogens contributed large amounts of sediment to the Gulf throughout the Eocene (Frazier and Schwimmer, 1987)."
Taphonomy
Modes of preservation:body
Size of fossils:macrofossils,mesofossils
Articulated whole bodies:some
Disassociated major elements:some
Temporal resolution:time-averaged
Spatial resolution:autochthonous
Collection methods and comments
Collection methods:bulk,sieve,field collection
Rock censused:14 kg
Reason for describing collection:paleoecologic analysis
Collection method comments: "Horizontal bulk samples were collected, disaggregated, sieved, and counted. Forty pounds of substrate were removed from a four inch horizontal layer near each lithological boundary ...These bulk samples were dried and a thirty pound sub-sample was boiled in Quaternary O solution until they disaggregated. The disaggregated sub-samples were sieved through USGS #10 and #14 sieves."
Taxonomic list comments:"To obtain a minimum number of species, bivalve valves were counted and divided by two. A valve was counted if more than one-half of the shell remained or if a majority of the cardinal processes and one-third of the shell remained. Whole gastropods and recognizable spires were counted. For scaphopods the toal length of the species pieces was divided by the average length of the species. Remains of bryozoan colonies were counted as an individual. Solitary corals were counted as one organism if more than one-half of the theca remained.
...
A type collection was established from surface samples and identifed using Dockery (1980) and MacNeil and Dockery (1984). This collection was confirmed by David T. Dockery of the Mississippi Office of Geology."
Metadata
Database number:44410
Authorizer:L. Ivany Enterer:P. Wall
Modifier:U. Smith Research group:GCP,marine invertebrate
Created:2004-09-09 12:46:19 Last modified:2010-10-10 19:52:54
Access level:the public Released:2004-09-09 12:46:19
Creative Commons license:CC BY
Reference information

Primary reference:

11665. G. Zumwalt, J. Pratt, and J. Moncrief. 1995. Marine Macro-Invertebrate Paleoenvirionmental Interpretation of the Harvey Site (Cook Mountain, Eocene) in North-Central Louisiana. Mississippi Geology 16(1):12-21 [L. Ivany/P. Wall/P. Wall]