Yorktown Formation

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Typesedimentary
Sub-unitsSunken Meadow Member, Rushmere Member, Morgarts Beach Member, Moore House Member, Tunnels Mill Member
Yorktown Formation
Stratigraphic range: Early to Middle Pliocene, 4.8–3.15 Ma
Outcrop of the Yorktown Formation at Carters Grove Bluffs along the James River
Typesedimentary
Unit ofChesapeake Group
Sub-unitsSunken Meadow Member, Rushmere Member, Morgarts Beach Member, Moore House Member, Tunnels Mill Member
UnderliesCroatan Formation
OverliesEastover Formation, Pungo River Formation
Lithology
PrimarySandstone, claystone
Othershells
Location
RegionAtlantic Coastal Plain of North America
ExtentMaryland, Virginia, North Carolina, South Carolina
Type section
Named forYorktown, Virginia
Named byClark and Miller, 1906[1]

The Yorktown Formation is a mapped bedrock unit in the Coastal Plain of Maryland, Virginia, North Carolina and South Carolina. It is overconsolidated and highly fossiliferous.

Stratigraphy

The Yorktown is composed largely of overconsolidated sand and clay with abundant calcareous shells, primarily bivalves.

The Yorktown unconformably overlies the Miocene Eastover Formation, and conformably underlies the Pliocene Croatan Formation.[2]

The Yorktown was divided into members by Ward and Blackwelder (1980). These are in ascending order: Sunken Meadow Member, Rushmere Member, Morgarts Beach Member, and Moore House Member.[3] The uppermost Tunnels Mill Member is recognized in Maryland only.

Notable exposures

Aurora mine

The most diverse paleobiota of the Yorktown Formation has been recovered from the Aurora mine of Beaufort County, North Carolina, where it overlies the intensively-mined Pungo River Formation. As with the Pungo River Formation, this locality has become a prime target for fossil collecting, and some of the most notable fossils from both formations are displayed at the Aurora Fossil Museum.[5] Foraminiferal analyses suggests that this locality belongs the Early Pliocene-aged Sunken Meadow Member.[6] The Yorktown fauna at the Aurora mine is far more diverse than the Pungo River fauna from the same locality, as the Pungo River sediments are mechanically processed for their phosphorite, while the Yorktown sediments are discarded and are thus in better condition for study.[7] This locality was likely deposited in a bay, with older sediments being deposited at a depth of 80 to 100 metres (260 to 330 ft) underwater, while younger sediments were deposited at a depth of 30 metres (98 ft) underwater.[8]

Clear differences are seen in the paleoichthyofauna of the Pungo River Formation and the overlying Yorktown Formation at the Aurora mine, with the Pungo River fauna representing almost exclusively warm-water taxa, while the Yorktown fauna preserves both warm and cooler-water taxa. These fossils provide important evidence for the significant cooling of ocean temperatures between the Miocene and Pliocene. However, the invertebrate fauna from both time periods appears to have cool-temperate affinities.[9]

Age

Hazel (1971) revised the age of the Yorktown from Miocene to Late Miocene to Early Pliocene using ostracod biostratigraphy.[10] The age was revised by Gibson (1983) to extend into the Middle Pliocene based on foraminifera.[11] Further biostratigraphic work with ostracods and foraminifera was completed by Cronin (1991), which also summarized previous investigations.[12] More recently, Spivey (2025) dated the Sunken Meadow Member to the Zanclean stage, about 4.8 to 3.8 million years ago,[6] while Dowsett et al (2001) dated the Rushmere and Morgarts Beach Members to the early-mid Piacenzian stage, about 3.3 to 3.15 million years ago. The deposition of these latter two members is thought to be linked to a marine transgression caused by the mid-Piacenzian warm period.[13]

Fossils

Vertebrate paleobiota

References

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