{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2026,6,16]],"date-time":"2026-06-16T21:56:32Z","timestamp":1781646992449,"version":"3.54.5"},"reference-count":74,"publisher":"SEPM Society for Sedimentary Geology","isbn-type":[{"value":"1565760778","type":"print"},{"value":"9781565761926","type":"electronic"}],"content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":[],"published-print":{"date-parts":[[2001]]},"abstract":"<jats:title>Abstract:<\/jats:title>\n                  <jats:p>Two continuous core borings 8.5 km apart on the leeward margin of Great Bahama Bank provided a special opportunity to interpret the depositional history during the Late Pliocene and Pleistocene. The upper ca. 200 m of the borings presented in this paper show seaward progradation of the margin with overall shallowing. At the base of this succession are skeletal grainstones and packstones that accumulated on the proximal slope of the margin. These are succeeded by thick intervals of reefal and coral-bearing deposits that in turn are capped by nonskeletal grainstones similar to the modern sediments in the interior of the Bahama Banks.<\/jats:p>\n                  <jats:p>Reefal and coral-bearing limestones produce about half of the leeward progradation. In both borings, the major episodes of coral growth began on unconsolidated sediments and show indications of upward shallowing according to the interpretations of Budd and Manfrino (this volume). In Clino, the seaward boring, the major episode of reef growth was terminated by deposition of fine-grained sediment mixed with coral floatstone; in Unda, the bankward boring, reef demise was the result of subaerial exposure.<\/jats:p>\n                  <jats:p>In Unda, the post-reefal deposits, termed the layered cap, are largely a succession of packstones and grainstones of peloids and skeletal debris, which are interpreted as platform-top accumulations similar to those of the Holocene. Thirteen discontinuity horizons, which are distinct breaks in sedimentation and have numerous features indicative of subaerial exposure, are used to divide this interval into sea -level flooding events (rising sea level and highstands) and periods of exposure (falling sea level and lowstands) during the Pleistocene and Late Pliocene.<\/jats:p>\n                  <jats:p>In Clino, above the major episodes of reef development, corals and skeletal grainstones and packstones continued to be the major component of aggradation. Nonskeletal packstones and grainstones from the platform interior are present only in the uppermost 20 m. Ten discontinuity horizons, which indicate falling sea level and sea-level lowstands, are identified in the Late Pleistocene.<\/jats:p>\n                  <jats:p>Two magnetostratigraphic datums provide the primary dating for this upper succession (McNeill et al., this volume). Three factors show that reef development occurred first in Unda during a period of relative rise of sea level: (1) correlating the top of the Olduvai between the two borings, (2) coral assemblages, and (3) interpretations of depositional environments. Coral assemblages in Unda include Pliocene species, whereas those in Ciino are largely Pleistocene to recent (Budd and Manfrino, this volume). A drop in sea level produced a downshift of major reef growth of some tens of meters (and as much as 100 m) to Clino. Another relative rise of sea level allowed for reefal aggradation. This offlap succession of reefal deposits confirms the pre-drilling model of margin evolution developed from seismic stratigraphy (Eberli and Ginsburg, 1989). The downshift in reef development during the Late Pliocene have been coincident with the onset of Northern Hemisphere ice accumulation as inferred from the deep-sea isotope record.<\/jats:p>\n                  <jats:p>These results confirm and expand on the role of reefs and sea-level fluctuations in the architecture of Great Bahama Bank. Reefs make a major contribution to leeward progradation, a circumstance that adds support to considering the Neogene Bank an atoll-Like structure. It is estimated that the margin shifted seaward some 10 km in approximately two million years. This episodic progradation was controlled by a hierarchy of sea-level fluctuations during the Late Pliocene and Pleistocene. Major episodes of sea-level rise allowed for aggrading reef development; higher-frequency cycles of sea-level fluctuation in the Pleistocene are recorded in the alternations of subaerial exposure and accumulation of coral-bearing limestones in Clino and the nonskeletal grainstones and packstones of Unda. The ten alternations in the Upper Pleistocene (above the Brunhes\/Matnyama boundary) interval matches the number of sea-level oscillations (glacial and interglacial stages) inferred from the oxygen isotope record in the deep sea.<\/jats:p>","DOI":"10.2110\/pec.01.70.0017","type":"book-chapter","created":{"date-parts":[[2010,11,22]],"date-time":"2010-11-22T14:37:34Z","timestamp":1290436654000},"page":"17-39","source":"Crossref","is-referenced-by-count":11,"title":["Pliocene to Pleistocene Depositional History of the Upper Platform Margin"],"prefix":"10.2110","author":[{"given":"Carrie","family":"Manfrino","sequence":"first","affiliation":[{"name":"Rosenstiel School of Marine and Atmospheric Science, University of Miami, 4600 Rickenbacker Cswy., Miami, Florida 33149, U.S.A. Current address: Kean University, Department of Geology, Union, New Jersey 07893, U.S.A., ckievman@turbo.kean.edu"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"Robert N.","family":"Ginsburg","sequence":"additional","affiliation":[{"name":"Rosenstiel School of Marine and Atmospheric Science, University of Miami, 4600 Rickenbacker Cswy., Miami, Florida 33149, U.S.A."}],"role":[{"vocabulary":"crossref","role":"author"}]}],"member":"860","reference":[{"key":"2026061617232117300_ch02r1","doi-asserted-by":"crossref","first-page":"203","DOI":"10.2110\/pec.89.44.0203","article-title":"Sedimentary and tectonic controls on the development of an early Mississippian carbonate ramp, Sacramento Mountains area, New Mexico","volume-title":"Controls on Carbonate Platform and Basin Development: 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