Author Type

Graduate Student

Date of Award

1999

Document Type

Thesis

Publication Status

Version of Record

Submission Date

October 2026

Thesis/Dissertation Advisor [Chair]

Finkl, Charles W.

Abstract

The southern Florida peninsula has experienced numerous oscillations of sealevel during the Quaternary Period. Lithologic and stratigraphic interpretation of geologic borings collected in the region suggest five separate marine transgressions separated by periods of prolonged exposure. Subdivision of the marine units was through the recognition of lithologic changes and the identification of paleosols. Paleosols generally signify periods of subaerial exposure suggesting a hiatus between similar shallow water siliciclastic and carbonate marine deposits. Amino acid racemization on mollusk shells collected from the upper three units confirm the stratigraphic subdivision and suggest high sealevel stands and associated marine depositional events during oxygen isotope stage 5E (125,000 years BP), stage 7 (210,000 years BP) and stage 9 (300,000 years BP).

Extent

164 p.

Comments

Thesis (M.S.)--Florida Atlantic University, 1999.|Thesis (M.S.)--Florida Atlantic University, 1999.

Identifier

FADT15649

Format

pdf

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