Catskill Formation
Age[1]
PeriodDevonian
PrilithologySandstone
OtherlithologySiltstone, shale
NamedforCatskill Mountains, New York
RegionAppalachian Mountains
CountryUnited States
UnderliesRockwell Formation, Huntley Mountain Formation, Pocono Formation, Spechty Kopf Formation
OverliesForeknobs Formation, Lock Haven Formation, Trimmers Rock Formation
ThicknessUp to 10,000 ft (3,000 m)
ExtentPennsylvania, New York (state)

The Devonian Catskill Formation or the Catskill Clastic Wedge is a unit of mostly terrestrial sedimentary rock found in Pennsylvania and New York. Minor marine layers exist in this thick rock unit (up to 10,000 feet (3,000 m)). It is equivalent to the Hampshire Formation of Maryland, West Virginia, and Virginia.

The Catskill is the largest bedrock unit of the Upper Devonian in northeast Pennsylvania and the Catskill region of New York, from which its name is derived. The Pocono Mountains of Pennsylvania are largely underlain by this unit as well. The rocks of the Catskill are a clastic wedge of predominantly red sandstone, indicating a large-scale terrestrial deposition during the Acadian orogeny. Many beds are cyclical in nature, preserving the record of a dynamic environment during its approximately 20 million years of deposition.

The Catskill Formation preserves a highly diverse paleobiota, including many early sarcopterygians (especially tetrapodomorphs), providing important evidence about the evolution of terrestrial vertebrates. The formation also provides important fossils about the evolution of land plants.[2]

Geology

Depositional environment

During the Devonian period, the Catskill Delta was formed by a series of river deltas and otherwise marshy terrain. This terrain was sandwiched between the epicontinental Kaskaskia Sea in central North America and the now-vanished Acadian Mountains. Erosion brought sediment from the mountain westwards into the sea, forming the deltas.

Eventually, the Delta formation was buried and transformed into sandstone, which was then revealed in places when the Catskill and Appalachian Mountains were formed at a later date. This transformation and uncovering is the primary reason why the Catskill Delta is notable in the present. Western Pennsylvania's petroleum was formed as a consequence. This was the first major oil region to be developed.

The Catskill was once considered to be related to the Old Red Sandstone, but in actuality, the two are only coincidentally similar. Both formed at approximately the same time, and under similar conditions: to the north of the Acadian Mountains were the Caledonian Mountains, and a similar region of marsh and river delta formed there.

Glacial erosion

Though both mountain ranges were formed during the Acadian orogeny, the Catskill Mountains, unlike the Appalachian Mountains underwent glacial erosion.[3] Much of what formed the Catskills as they stand today is a result of the Wisconsin glaciation which ended only about 12,000 years ago.[4]

There are many signs of the Glacial period event which carved the current day Catskill Mountains.

These markers include:

Members

Eastern Pennsylvania

Towamensing, Walcksville, Beaverdam Run, Long Run, Packerton, Poplar Gap, Sawmill Run, Berry Run, Clarks Ferry, and Duncannon.

Central Pennsylvania

Irish Valley, Sherman Creek, Buddys Run, Clarks Ferry, and Duncannon.

Paleobiota

Plants

Plantae
NameSpeciesLocalityMaterialNotesImages
TaeniocradaspCatskill Formatiom, Potter County>80 Specimens
BarinophytoncitrulliformeCatskill Formation, Potter County, Pennsylvania>20 specimens
cf. obscurumCatskill Formation, Potter County, Pennsylvania
ssp.Catskill Formation, Potter County, Pennsylvania>100 Specimens
ProtobarinophytonP. pennsylvanicumCatskill Formation, Potter County, Pennsylvania2 Specimens of megasporeThe genus these spore are attached to belong to an early group of land plants from the Silurian.
Rhacophyton
LycopsidaIndeterminateCatskill Formation, Potter County, Pennsylvania8 Specimens
ArchaeopterisA.sspCatskill Formation, Potter County, Pennsylvania>160 SpecimensOne of the earliest known large "tree" like plants to take root

Invertebrates

Protostomes
NameSpeciesLocalityMaterialNotesImages
LingulaspCatskill Formation, Potter County, Pennsylvania1 Specimen
GigantocharinusG.szatmaryiRed Hill Locality, Clinton County, PennsylvainiaHolotype consists of an extremely well preserved exoskeleton and a few impressions.The genus has helped begin bridging the gap between its family's missing record from the Middle Devonian to the Late Carboniferous.[5]
OrsadesmusO.rubecollusRed Hill Locality, Clinton County, PennsylvainiaHolotype is an impression of the exoskeletonThe species was described alongside the Quebec genus Zanclodesmus, forming a new family within the broad flat keeled members of the order Archidesmida.[6]
HallipterusH.excelciorCatskill Formation, Wyoming County, Pennsylvania
AdelophthalmusA.sspCatskill Formation, Potter County, Pennsylvania1 SpecimenIt was described in 2002 by W. E. Stein (2002) as an indeterminate Eurypterid, it was then redescribed as an indeterminate species of Adelophthalmus in 2022 by R. E. Plotnick (2022).[7]

Placoderms

Placoderms of the Catskill Formation
GenusSpeciesPresenceMaterialNotesImages
BothriolepisB. sp.Mansfield, Tioga County, PennsylvaniaAbundant material, including mass mortality of hatchlings.[8]A bothriolepidid. Species unknown, though sometimes referred to as B. nitida.[9]
GroenlandaspisG. pennsylvanica[9]A groenlandaspidid.
PhyllolepisP. rossimontinaA phyllolepidid.
P. thomsoni[10]Articulated skeleton.
TurrisaspisT. elektor[9]A groenlandaspidid.

Acanthodians

Acanthodians of the Catskill Formation
GenusSpeciesPresenceMaterialNotesImages
GyracanthusG. cf. sherwoodi[9]A gyracanthid.

Chondrichthyans

Chondrichthyans of the Catskill Formation
GenusSpeciesPresenceMaterialNotesImages
AgeleodusA. pectinatusRed Hill Locality, Clinton County, PennsylvainiaTeethA holocephalan of uncertain affinities.
CtenacanthusC. sp.A ctenacanthiform elasmobranch.[9]

Actinopterygians

Actinopterygians of the Catskill Formation
GenusSpeciesPresenceMaterialNotesImages
LimnomisL. delaneyiRed Hill, Clinton County, PennsylvaniaHolotype is a compressed skull.An early ray-finned fish.[11]

Sarcopterygians

Sarcopterygians of the Catskill Formation
GenusSpeciesPresenceMaterialNotesImages
ApatorhynchusA. opistheretmusApatorhynchus-type locality, Tioga County, PennsylvaniaHolotype is a partial skull, 1 specimen.A lungfish of uncertain affinities.[12]
DensignathusD. roweiA stegocephalian tetrapodomorph.[13]
EusthenodonE. bourdoni[14]A tristichopterid tetrapodomorph.
E. leganihanne[15]
HyneriaH. lindaeRed Hill Site, Clinton County, PennsylvainiaHolotype is a disarticulated skull and 3D body fossil.A tristichopterid tetrapodomorph.
HynerpetonH. bassettiA stegocephalian tetrapodomorph.[16]
LanglieriaL. radiataA tristichopterid tetrapodomorph. Originally identified as Holoptychius.[17]
L. smalingi[18]Irish Valley Member
MegalichthysM. mullisoniA megalichthyid tetrapodomorph.[19]
SauripterusS. tayloriSherman Creek Locality, Lycoming County, PennsylvainiaThe Holotype is an articulated limb and 3 scales, there are 3 individuals.A rhizodontid tetrapodomorph.[20]
SoederberghiaS. groenlandicaCatskill Formation, Lycoming County, PennsylvaniaA rhynchodipterid lungfish.[12]
SterropterygionS. brandeiAn indeterminate osteolepiform tetrapodomorph.[19]

References

  1. ^ https://www.researchgate.net/publication/288606271_Dating_the_earliest_tetrapods_A_catskill_palynological_problem_in_Pennsylvania
  2. ^ Broussard, David R.; Trop, Jeffrey M.; Benowitz, Jeff A.; Daeschler, Edward B.; Chamberlain, John A.; Chamberlain, Rebecca B. (2018-12-15). "Depositional setting, taphonomy and geochronology of new fossil sites in the Catskill Formation (Upper Devonian) of north-central Pennsylvania, USA, including a new early tetrapod fossil". Palaeogeography, Palaeoclimatology, Palaeoecology. 511: 168–187. Bibcode:2018PPP...511..168B. doi:10.1016/j.palaeo.2018.07.033. ISSN 0031-0182
  3. ^ Rich, John Lyon (1906). "Local Glaciation in the Catskill Mountains". The Journal of Geology. 14 (2): 113–121. Bibcode:1906JG.....14..113R. doi:10.1086/621285. JSTOR 30055593. S2CID 129029014
  4. ^ Titus, Robert (1996). The Catskills in the Ice Age. Flieschmanns, New York: Purple Mountain Press. pp. 14–29. ISBN 978-0-935796-77-3.
  5. ^ Shear, William A. (2000). "GIGANTOCHARINUS SZATMARYI, A NEW TRIGONOTARBID ARACHNID FROM THE LATE DEVONIAN OF NORTH AMERICA (CHELICERATA, ARACHNIDA, TRIGONOTARBIDA)". Journal of Paleontology. 74: 25–31. doi:10.1666/0022-3360(2000)074<0025:GSANTA>2.0.CO;2
  6. ^ Wilson, Heather M.; Daeschler, Edward B.; Desbiens, Sylvain (2005). "New Flat-Backed Archipolypodan Millipedes from the Upper Devonian of North America". Journal of Paleontology. 79 (4): 738–744. doi:10.1666/0022-3360(2005)079[0738:NFAMFT2.0.CO;2]
  7. ^ Plotnick, Roy E. & Lamsdell, James C. (2023). "Eurypterids from the Price Formation of Virginia: First Eurypterids from the Mississippian of North America". Journal of Paleontology. 97 (1): 167-171. doi:10.1017/jpa.2022.84
  8. ^ Downs, Jason P.; Criswell, Katharine E.; Daeschler, Edward B. (2011). "Mass Mortality of Juvenile Antiarchs ( Bothriolepis sp.) from the Catskill Formation (Upper Devonian, Famennian Stage), Tioga County, Pennsylvania". Proceedings of the Academy of Natural Sciences of Philadelphia. 161 (1): 191–203. Bibcode:2011PANSP.161..191D. doi:10.1635/053.161.0111. ISSN 0097-3157
  9. ^ Daeschler, Edward B. & Cressler, Walter L., III (2011-01-01), "Late Devonian paleontology and paleoenvironments at Red Hill and other fossil sites in the Catskill Formation of north-central Pennsylvania", From the Shield to the Sea: Geological Field Trips from the 2011 Joint Meeting of the GSA Northeastern and North-Central Sections. Vol. 20, Ruffolo, Richard M. (ed.), Geological Society of America, p. 0, doi:10.1130/2011.0020(01). ISBN 978-0-8137-0020-5, retrieved 2025-04-15
  10. ^ Long, John A. & Daeschler, Edward B. (2013). "First Articulated Phyllolepid Placoderm from North America, with Comments on Phyllolepid Systematics". Proceedings of the Academy of Natural Sciences of Philadelphia. 162 (1): 33–46. Bibcode:2013PANSP.162...33L. doi:10.1635/053.162.0103. ISSN 0097-3157
  11. ^ Daeschler, Edward B. (2000). "An Early Actinopterygian Fish from the Catskill Formation (Late Devonian, Famennian) in Pennsylvania, U.S.A.". Proceedings of the Academy of Natural Sciences of Philadelphia. 150: 181–192. ISSN 0097-3157. JSTOR 4065069
  12. ^ Friedman, Matt & Daeschler, Edward B. (2006). "Late Devonian (famennian) Lungfishes from the Catskill Formation of Pennsylvania, Usa". Palaeontology. 49 (6): 1167–1183. Bibcode:2006Palgy..49.1167F. doi:10.1111/j.1475-4983.2006.00594.x. ISSN 1475-4983
  13. ^ Daeschler, E.B. (2000). "Early tetrapod jaws from the Late Devonian of Pennsylvania, USA". Journal of Paleontology. 74 (2): 301–308. Bibcode:2000JPal...74..301D. doi:10.1666/0022-3360(2000)074<0301:etjftl>2.0.co;2. S2CID 131194763
  14. ^ Downs, Jason P.; Barbosa, Jeremy; Daeschler, Edward B. (2021-05-04). "A new species of Eusthenodon (Sarcopterygii, Tristichopteridae) from the Upper Devonian (Famennian) of Pennsylvania, U.S.A., and a review of Eusthenodon taxonomy". Journal of Vertebrate Paleontology. 41 (3). Bibcode:2021JVPal..41E6197D. doi:10.1080/02724634.2021.1976197. ISSN 0272-4634
  15. ^ Downs, Jason P.; Osatchuck, Madison M.; Goodchild, Owen A.; Daeschler, Edward B. (2022-11-25). "Second species of Eusthenodon (Tristichopteridae, Sarcopterygii) from the Upper Devonian (Famennian) Catskill Formation of Pennsylvania, U.S.A., and a review of global Eusthenodon occurrence". Journal of Vertebrate Paleontology. 42 (5). Bibcode:2022JVPal..42E1627D. doi:10.1080/02724634.2023.2201627. ISSN 0272-4634
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  20. ^ T.A. Stewart,J.B. Lemberg,N.K. Taft,I. Yoo,E.B. Daeschler,& N.H. Shubin, Fin ray patterns at the fin-to-limb transition, Proc. Natl. Acad. Sci. U.S.A. 117 (3) 1612-1620,(2020). Marcus C. Davis, Shubin, N., & Daeschler, E. B. (2004). A New Specimen of Sauripterus taylori (Sarcopterygii, Osteichthyes) from the Famennian Catskill Formation of North America. Journal of Vertebrate Paleontology, 24(1), 26–40.