skip to main content
OSTI.GOV title logo U.S. Department of Energy
Office of Scientific and Technical Information

Title: Transgressive Holocene sequence recorded in Steinhatchee estuarine sediments: Western peninsular Florida

Conference · · Geological Society of America, Abstracts with Programs; (United States)
OSTI ID:7060235
; ; ;  [1];  [2]
  1. Florida Geological Survey, Tallahassee, FL (United States)
  2. Florida State Univ., Tallahassee, FL (United States). Geology Dept.

The flat regional topography of peninsular Florida's Gulf Coast reflects the shallow dip of the underlying carbonate platform. As a result of this low gradient, wave energy is generally low and sedimentation within the Steinhatchee Estuary is dominated by river- and tidal-hydrodynamics. Carbonate dissolution has caused the Eocene-aged limestone surface to be highly irregular. The transgressive sequence unconformably overlying this karstic surface is comprised of clastics, from upriver and offshore, and organics produced by reefal and salt-marsh communities. Sequences deposited in karstic lows are up to 7 meters (m) thick. More typical sequences are 3 m thick, or less. The oldest unlithified marsh strata include dolosilt or carbonate rubble with clay and wood fragments. This clayey rubble-zone is overlain by subaerially deposited reddish-brown clayey sands and organic sands (including buried trees) which are in turn overlain by black, organic-rich, peaty, wetland deposits. These marsh sequences are primarily sand, which fines upwards. Silt-sized (and smaller) clastics and organic components increase up-sequence at similar rates. Thin sequences (.3--.5 m) of shelly organic-rich sand occur in current submarine environments. Thicker submarine sequences (up to 7 m) of similar material occur in present or relic oyster bars. Although a basal clayey rubble-zone may be present, subaerial and/or wetlands facies are not observed in offshore sediments. Erosion of these facies as sea level rose may have resulted from insufficient sediment supply to maintain the beach profile and/or from down-cutting by tidal currents.

OSTI ID:
7060235
Report Number(s):
CONF-9404221-; CODEN: GAAPBC
Journal Information:
Geological Society of America, Abstracts with Programs; (United States), Vol. 26:4; Conference: 43. annual meeting of the Southeastern Section of the Geological Society of America, Blacksburg, VA (United States), 7-8 Apr 1994; ISSN 0016-7592
Country of Publication:
United States
Language:
English

Similar Records

Depositional environments of Schuler Formation (Cotton Valley Sands), Upshur County, Texas
Conference · Tue Mar 01 00:00:00 EST 1983 · Am. Assoc. Pet. Geol., Bull.; (United States) · OSTI ID:7060235

Depositional sequence evolution as a result of tectonism, basin subsidence, and sea level change, Turonian to Santonian, west-central Utah
Conference · Fri Aug 01 00:00:00 EDT 1986 · Am. Assoc. Pet. Geol., Bull.; (United States) · OSTI ID:7060235

Depositional environments and facies analysis of the Cherokee Group in west-central Kansas
Conference · Fri Mar 01 00:00:00 EST 1991 · AAPG Bulletin (American Association of Petroleum Geologists); (United States) · OSTI ID:7060235