Eby Pit upper bench coal site 2: Desmoinesian, Indiana
List of taxa
Where & when
Geology
Taphonomy & methods
Metadata & references
Taxonomic list
unclassified
|
|||||||
Synchysidendron resinosum
|
0.25 grid-count | ||||||
Lycopodiopsida
- Isoetales
|
|||||||
Paralycopodites brevifolius
|
35.79 grid-count | ||||||
unclassified
|
|||||||
Medullosa spp.
|
44.89 grid-count | ||||||
Equisetopsida
- Sphenophyllales
|
|||||||
Sphenophyllum plurifoliatum
|
3.95 grid-count | ||||||
Pinopsida
|
|||||||
Pennsylvanioxylon nauertianum
|
0.06 grid-count | ||||||
Coenopteridales
|
|||||||
Stelastellara parvula
Baxter 1965
|
0.06 grid-count | ||||||
Polypodiopsida
- Equisetales
- Calamitaceae
|
|||||||
Calamodendron americanum
|
3.2 grid-count | ||||||
Polypodiopsida
- Marattiales
- Marattiaceae
|
|||||||
Psaronius spp.
|
9.23 grid-count | ||||||
Lepidodendrales
- Lepidodendraceae
|
|||||||
Lepidodendraceae indet.
|
1.19 grid-count | ||||||
Lepidophloios hallii
|
1.31 grid-count | ||||||
see common names |
Geography
Country: | United States | State/province: | Indiana | County: | Warrick County |
Coordinates: | 38.2° North, 87.3° West (view map) | ||||
Paleocoordinates: | 8.0° South, 24.3° West | ||||
Basis of coordinate: | based on nearby landmark | ||||
Geographic resolution: | small collection |
Time
Period: | Carboniferous | Epoch: | Pennsylvanian |
10 m.y. bin: | Carboniferous 4-5 | ||
*Period: | Late/Upper Carboniferous | *Local age/stage: | Late/Upper Desmoinesian |
Key time interval: | Desmoinesian | ||
Age range of interval: | 312.70000 - 305.90000 m.y. ago | ||
* legacy (obsolete) database fields |
Stratigraphy
Formation: | Carbondale | Member: | Springfield Coal | ||
Stratigraphic resolution: | bed | ||||
Stratigraphy comments: Eby Pit of the Peabody Coal Company Lynnville Mine.
Equivalent to late Westphalian D. |
Lithology and environment
Primary lithology: | coal ball |
Secondary lithology: | "shale" |
Includes fossils? | Y |
Lithology description: Coal balls; The upper bench of the Springfield Coal, continuous wiht the main coal bed at the edge of the split, is present over most of the Folsomville Member and varies widely in character. In some sections it appears as a normally brightly-banded bituminous coal. In other areas, it appears as a clastic-rich coal or organic shale and in some cases, the clastic-rich layers may be intermixed iwth more coaly layers or grade upward into a normally bright-banded coal. | |
Environment: | mire/swamp |
Taphonomy
Modes of preservation: | permineralized |
Lagerst�tten type: | conservation |
Size of fossils: | macrofossils |
Preservation of anatomical detail: | excellent |
Temporal resolution: | snapshot |
Spatial resolution: | parautochthonous |
Collection methods and comments
Collection methods: | selective quarrying,peel or thin section,field collection |
Rock censused: | 2366 cm2 (area) |
Reason for describing collection: | paleoecologic analysis |
Metadata
Also known as: | UI 26792-26823 | ||
Database number: | 11042 | ||
Authorizer: | H. Sims | Enterer: | H. Lindon, S. Ostrowski |
Modifier: | H. Lindon | Research group: | paleobotany |
Created: | 2001-07-09 11:35:12 | Last modified: | 2002-06-27 10:12:58 |
Access level: | the public | Released: | 2001-07-09 11:35:12 |
Creative Commons license: | CC BY |
Reference information
Primary reference:
4066. | T. L. Phillips and W.A. DiMichele. 1998. A Transect through a Clastic-swamp to Peat-swamp Ecotene in the Springfield Coal, Middle Pennsylvanian Age of Indiana, USA. Palaios 13:113-128 [H. Sims/H. Sims/H. Sims] |