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December 01, 1989
Upper Ordovician tempestites from Swatara Gap, Pennsylvania; depositional processes affecting the sediments and paleoecology of the fossil faunas
David Lehman
;
David Lehman
Univ. Rochester, Dep. Geol. Sci., Rochester, NY, United States
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John K. Pope
John K. Pope
Miami Univ. at Oxford, OH, United States
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PALAIOS (1989) 4 (6): 553–564.
Article history
first online:
03 Mar 2017
Citation
David Lehman, John K. Pope; Upper Ordovician tempestites from Swatara Gap, Pennsylvania; depositional processes affecting the sediments and paleoecology of the fossil faunas. PALAIOS 1989;; 4 (6): 553–564. doi: https://doi.org/10.2307/3514745
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Index Terms/Descriptors
- Arthropoda
- Articulata
- benthic taxa
- biogenic structures
- Brachiopoda
- clastic rocks
- claystone
- communities
- deposition
- diversity
- faunal studies
- Invertebrata
- Lebanon County Pennsylvania
- lithofacies
- mudstone
- Ordovician
- paleoecology
- paleoenvironment
- Paleozoic
- Pennsylvania
- Reedsville Formation
- sedimentary rocks
- sedimentary structures
- sediments
- shallow-water environment
- siltstone
- Sowerbyella
- storm environment
- stratigraphy
- Strophomenida
- taphonomy
- tempestite
- Trilobita
- Trilobitomorpha
- United States
- Upper Ordovician
- Isotelus gigas
- Rafinesquina
- Gravicalymene
- Swatara Gap
- Thaerodonta
- Cryptolithus bellulus
- Laptaena
- Triarthus becki
Latitude & Longitude
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