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High eustatic sea level during the middle Pliocene: Evidence from the southeastern U. S. Atlantic Coastal Plain

Journal Article · · Geology; (USA)
;  [1]
  1. Geological Survey, Reston, VA (USA)
The middle Pliocene, {approximately}3.5-2.5 Ma, was a period of global warmth preceding the growth of major Northern Hemisphere ice sheets. The authors report on eustatic sea level for the middle Pliocene based on microspaleontologic study of marine deposits of the Duplin Formation of South Carolina and North Carolina. The Duplin was deposited during a middle Pliocene marine transgression that formed the Orangeburg scarp, a prominent wave-cut geomorphic paleoshoreline of the southeastern U.S. Atlantic Coastal Plain. They concluded that (1) the scarp in South Carolina was formed mostly during the middle Pliocene (3.5-3.0 Ma), (2) eustatic sea level was about 35 {plus minus} 18 m higher than modern sea level (the scarp has been uplifted about 50-65 m since the middle Pliocene), and (3) ocean-water temperatures along eastern North America were warmer when the scarp was formed that they are at present.
OSTI ID:
6314486
Journal Information:
Geology; (USA), Journal Name: Geology; (USA) Vol. 18:5; ISSN GLGYB; ISSN 0091-7613
Country of Publication:
United States
Language:
English