Geology topics

B. H. Lidz

Publications and source records attributed to B. H. Lidz.

22 records · Page 2Linked to original sources

USGS1989

Diagnostic foraminiferal assemblages of Florida Bay and adjacent shallow waters: a comparison

Ecologic studies of benthic Foraminifera in Florida Bay indicate that 1) the bay is a specialized restricted platform interior environment; 2) its fauna is divisible into 3 subfaunas: nearshore, mudbank, and "lake', 3) substrate, currents, wave intensity, and wave direction affect local distribution but do not alter regional patterns; and 4) faunal assemblages rather than individual species of Foraminifera are diagnostic environmental indicators as many species range over several faunal zones. -from Authors

Bulletin of Marine Science↗

USGS1985

Holocene carbonate sedimentary petrology and facies accumulation, Looe Key National Marine Sanctuary, Florida.

Suggests a greater production of coralline sand (rather than slower Halimeda growth) results from a marked acceleration of bioerosion of abundant dead reefs in the area. -from Authors

Bulletin of Marine Science↗

USGS1984

Oldest (Early Tertiary) subsurface carbonate rocks of St. Croix, USVI, revealed in a turbidite-mudball.

Ranging in age from early Eocene to early Miocene and younger, pelagic foraminifers form the major component of a phenoclastic mudball within a fossiliferous turbidite. The turibidite is part of a more than 12m-thick section of biogenic deposits of middle Miocene age.-from Author

Journal of Foraminiferal Research↗

USGS1977

Topographic control and accumulation rate of some Holocene coral reefs: south Florida and Dry Tortugas

Core drilling and examination of underwater excavation on 6 reef sites in south Florida and Dry Tortugas revealed that underlying topography is the major factor controlling reef morphology. Carbon-14 dating on coral recovered from cores enables calculation of accumulation rates. Accumulation rates were found to range from 0.38 m/1000 years in thin Holocene reefs to as much as 4.85 m/1000 years in thicker buildups. Cementation and alteration of corals were found to be more pronounced in areas of low buildup rates than in areas of rapid accumulation rates. Acropora palmata, generally considered the major reef builder in Florida, was found to be absent in most reefs drilled. At Dry Tortugas, the more than 13-meter thick Holocene reef did not contain A. palmata. The principal reef builders in this outer reef are the same as those which built the Pleistocene Key Largo formation, long considered to be fossilized patch reef complex.

Florida↗