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Download Download Journal of Coastal Research Fort Lauderdale The Pliocene Reefs of Miami: Their Geomorphological Significance in the Evolution of the Atlantic Coastal Ridge, Southeastern Florida, U. S.A1 Edward J. Petuch Department of Geology Florida Atlantic University Boca Raton, Florida :i3431 ABSTRACT _ PETUCH, E.•I., 1986. The Pliocene reefs of Miami: their geomorphological significance in the evolu­ tion ofthe Atlantic Coastal Ridge, southeasern Florida, U.S.A. Journal of Coastal Research. 2(4),391­ 408. Fort Lauderdale, ISSN 0749-0208. ~',"" Construction excavations in western Metropolitan Miami (Metropolitan Dade County), " Florida have recently dredged up coral reefdeposits from depths ofonly 15-20 m below the •.. Atlantic Coastal Ridge. Based upon index fossils, these richly fossiliferous sediments are • ••• • referrable to the Buckingham Formation (~"PinecrestBeds or Formation" of Olsson) and ~ are dated as early Pliocene. A distinctive Pliocene coral fauna was present, including -- ....-...- ~ e Diploria sarasotana Weisbord, Septastrea marylandica (Conrad), Septastrea crassa (Holmes), -2 Porites furcula Lamarck, and the hydrocoralMillepora alcicomin Linnaeus, and over three hun­ --+ *• dred species ofmollusks alongwith several species ofechinoids and crustaceans(collected as fragments). Although being more biohermal in form. the Pliocene reef system under Miami appeared to have distinct zonation, with evidence of four ecological zones being collected at the sampling sites. These zones included the high-energy. reefcrest Millepora­ Trochita Zone (Zone I), the reef platform lJip[oria-Gorgonian Zone (Zone 2), the back reef Porites-Septastrea Zone (Zone 3), and a lagoonal Thalaesio- Turritella Zone (Zone 4) to the west of the reef tract. Based upon both the extent of the Atlantic Coastal Ridge and the implied faunal zonation of the reefs, it is conjectured that the Pliocene reef tract produced the original topographic high along the southeasterncoast ofFlorida. This was latercovered by a crust of oolitic limestone and sand in the late Pleistocene to produce the Atlantic Coastal Ridge. Similar Pliocene reeftracts are known from southwestern and southern Florida. and these linked with the eastern reef tract to form an atoll-like structure around a central. lagoon-like basin. The southern part of this basin infilled with carbonate sediments. and during subaerial exposure in the early Pleistocene, produced the Tamiami Formation. Together, the atoll-like Pliocene reeftracts and the central lagoon-like basin laid down the geomorphological framework for the formation of the Everglades in the Holocene. The Everglades is now seen to be reef-controlled. Fourteen new gastropod species. all index fossils for the reeffacies ofthe Buckingham Formation, and a new genus ofhard substrate muricid gastropods, are proposed. ADDITIONAL INDEX WORDS: Atlantic Coastal Ridge. Buckingham Formation, coral reef, Ecergludvs. Florida, index fossil, Pliocene, Tamiami Formation. INTRODUCTION sits on top of an anomolous oolitic limestone-capped topographic high referred to as the Atlantic Coastal Recent dredgings and excavations for artificial Ridge (Figure I), the uncovering of this deeper sub­ lakes and housing projects in western Metropolitan surface material offered the first large-scale detailed Miami (Metropolitan Dade County), Florida, have look at what lies below Miami. uncovered the first large quantities of deeper sub­ In 1955, GARDNER (in PARKER, etal.) described a surface sediments from that area. UntiI1980-1983, Pliocene molluscan fauna taken from 20-50 m much of this area was still the swampy Eastern depths in wells that were drilled near the site repor­ Everglades and its subsurface geology was poorly ted in this paper. Based upon index fossils, she cor­ known. Because a large part of Metropolitan Miami related this fauna with the Pliocene Duplin Forma­ 18.5006 received 24 January. /986: accepted in recision 211 Feb­ tion of North Carolina. The Floridian equivalent of ruary 1986. this well-known Carolinian formation has since been 392 Petuch referred to the BuckinghamFormationof MANSFIELD MEEDER (1979) described similar-appearing (1939) (="Pinecrest Beds or Formation" of OLSSON, Buckingham-aged reef material taken in quarries 1968, andin OLSSON and PETIT, 1964. Fora discus­ along the southwestern coast of Florida, from Naples sion of this nomenclatural change, see PETUCH, in north to Estero. Although faunistically similar to press*). Some of the key Buckingham-Duplin index the eastern Floridian reef tract, this western reef fossils taken from below western Metropolitan complex contained a richer coral fauna, with over Miami included Urosalpinx suffolkensis Gardner, forty species of hermatypes. Among these were the Cancellaria tabulata Gardner and Aldrich, Calophos characteristic reef- building genera Stylophora, (Dorsanum of authors) plicatile (Bose), Con­ Acropora, Goniopora, Diploria; Dichocoenia, Sider­ traconus adversarius (Conrad), Sconsia hodgii astrea, Agaricia, andMontastrea. To the east of the (Conrad), and Siphocypraea carolinensis (Conrad). west coast reef tract, MEEDER(1980) later encoun­ Among the extensive list of invertebrate species tered a lagoonal, soft- bottom, solitary coral fauna, given by Gardner, there were several taxa that also characterized by the generaPlacocyathus, Manicina, indicated coral reef or hard bottom, shallow water Antillia, Antillophylia, andFlabellum. In containing environments. These included the gastropods Cru­ Placocyathus, this lagoonal assemblage was similar cibulum multilineatum (Conrad), Trossulasalpinx to the lagoonal assemblage found along the western trossulus (Conrad) new genus, Coralliophila sp., side of the Miami reeftract, which will be discussed and Cerithium leonensis Mansfield, the encrusting later in this paper. bivalvePseudochama striata (Emmons), along with echinoid spines, large barnacles, and small coral fragments. The Buckingham Formation has subse­ quently been radiometrically dated (as the "Pine­ crestFormation") at3.7 millionyears BP (BENDER, 1972), making it the chronological equivalentof the Duplin Formation. Since August, 1983, draglines used in construct­ ing artificial lakes have broughtup large amounts of highly fossiliferous sediments at several sites near SW 146 th Avenue and Bird Road in Greater Miami, all from depths of approximately 15-20 m. While visiting four of these sites, I found that the marly sediments contained a pure and species-rich as­ semblage of Buckingham-Duplin marine inverteb­ rates. This assemblage was similar to that previ­ ously described by Gardner, but contained greater numbers of corals and coralliophilous mollusks. Commonly found at Bird Road were the reef corals EVERGLADES Diploria, Montastrea, Septastrea, and Porites, and NATIONAL these, along with the Duplin-Buckingham gas­ PARK tropod index fossils, give strong evidence for the existence of a Pliocene reef complex in the shallow subsurface of southeastern Florida. For a descrip­ tion of the stratigraphy of this site, see PETUCH (in press). The discovery of the Bird Road construc­ Figure I. Location and extent of the Atlantic Coastal Ridge tion sites also allowed the first detailed look at the (stippled areas) in Dade County, Florida. A Pliocene reef tract shallowly underlies the stippled areas, and represents the south­ structure of the eastern Floridian Pliocene reef tract eastern corner of an atoll-like structure. and gave a possible explanation for the regional topographic high that rises above the rest of the southeastern end of the Floridian Platform. Specimens of Pliocene, Buckingham-aged coral reef index fossils have also been taken farther 'The name Pinecrest Formation is a stratigraphic homonyn of the northward under the Atlantic Coastal Ridge at West Pinecrest Formation of the Triassic of Pinecrest Ridge. Red Butte Creek. Utah, proposed in 1929 (see Keroher, 1966), and cannot he Palm Beach and Boca Raton (SWAYZE and MILLER, used, again, for the Floridian formation. 1984) (designated as reefal limestones and shells), .Iournal of Coastal Research. VoL 2, No.4, 1986 Pliocene ReefR of Miami 393 Figure2. Schematic diagram showingthe possihle configurationof the Floridian atoll-feature during its maximumdevelopment in the Pliocene. Black areas denote land above mean sea level, stippled areas denote coral reefs; contour shows depth in meters below mean Pliocenesea level.Pliocene coral reef index fORRilR have been collected, in wellcores and dredging operations, at Bird Road, Miami(B), KromeAvenue,Miami(K)(GARDNER, 1955),Pinecrest (PC) (OLSSON and PETIT, 1964; OLSSON, 1967),MulePen Quarry,Naples (M) and Estero (E) (MEEDER, 1979, 1980), Buckingham (BU) (MANSFIELD, 1939), Olga (0) (MANSFIELD, 19:19), Fisheating Creek (F), and Brighton(BR) (OLSSON and PETIT, 1964; OLSSON, 1967), and West Palm Beach (P) (SWAYZE and MILLF:R, 1984). and in Broward County (CAUSERAS, USGS, per­ reeftract and the eastern reeftract underthe Atlan­ sonal communication). This evidence indicates that tic Coastal Ridge, these other reeftracts complete the Pliocene reef system of southeastern Florida the picture and demonstrate the existence ofa ring­ formed a relatively continuous tract running from like configuration of coral reefs in southern Florida Palm Beach southward to Miami and possibly during the Pliocene (Figure 2). southern Dade County. Pliocene coral reef index Somewhat overshadowed by the finding of an fossils, primarily mollusks, have also been taken eastern Floridian Pliocene reef fauna, but still of from
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