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Bermont Formation

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Figure1—Collecting localities in the Bermont Formation (Lower Pleistocene) at the Palm Beach Aggregate Quarry and Holey Land Canal in southern Florida
Published: 01 May 2010
Figure 1 —Collecting localities in the Bermont Formation (Lower Pleistocene) at the Palm Beach Aggregate Quarry and Holey Land Canal in southern Florida
Journal Article
Journal: PALAIOS
Published: 01 March 2007
PALAIOS (2007) 22 (2): 166–173.
... of the environmental context. The interaction of Chione elevata with its epibionts and gastropod predators in two shallow marine facies from the Pleistocene of Florida, corresponding to the Bermont and the overlying Fort Thompson Formations, were examined. Fort Thompson samples exhibit roughly an order of magnitude...
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Published: 01 March 2007
TABLE 2 —Spatial distribution of boreholes on C. elevata valves. Fort Thompson Formation = FTT; Bermont Formation = BER
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Published: 01 March 2007
TABLE 1 —Total counts of fragmental, complete, measured, and mean shell length for samples of C. elevata valves. Fort Thompson Formation = FTT; Bermont Formation = BER
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FIGURE 6—Bivariate scatter plot and least square regression lines of shell length versus outer borehole diameter for bored C. elevata valves from the two facies. Fort Thompson Formation = FTT; Bermont Formation = BER; OBD = outer borehole diameter
Published: 01 March 2007
FIGURE 6 —Bivariate scatter plot and least square regression lines of shell length versus outer borehole diameter for bored C. elevata valves from the two facies. Fort Thompson Formation = FTT; Bermont Formation = BER; OBD = outer borehole diameter
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Figure2—Crepidula maculosa from the early Pleistocene Bermont Formation, Okeechobee County, Florida. 1–5, Brooded young collected from within aperture of parent shell, UF 111877. Scale bar = 500 μm.
Published: 01 February 2004
Figure 2 — Crepidula maculosa from the early Pleistocene Bermont Formation, Okeechobee County, Florida. 1–5, Brooded young collected from within aperture of parent shell, UF 111877. Scale bar = 500 μm.
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Published: 01 March 2007
TABLE 3 —Count, mean valve length, and difference between mean valve lengths for bored and unbored specimens and boring frequency of C. elevata within each sample. Significant differences indicated by * (t-test) or # (Mann-Whitney U). Fort Thompson Formation = FTT; Bermont Formation = BER
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FIGURE 1. Three views of a typical flat-based colony of Manicina areolata (PBA, UF148043) collected from the lower Bermont Formation, southern Florida. A) Oral surface. B) Lateral view. C) Basal surface. Scale in C is for all three views.
Published: 01 January 2010
FIGURE 1. Three views of a typical flat-based colony of Manicina areolata (PBA, UF148043) collected from the lower Bermont Formation, southern Florida. A) Oral surface. B) Lateral view. C) Basal surface. Scale in C is for all three views.
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FIGURE 1—Distribution of samples from the Caloosa Shell outcrop. Paleoecological analysis (Daley, 2001) revealed two distinct assemblages that correspond to two formations. The predominantly epifaunal (seagrass) community of the Bermont Formation is shown as open triangles; the predominantly infaunal community of the Fort Thompson Formation is shown as filled, inverted triangles. A mixed zone approximately 1 m thick marks the contact between formations
Published: 01 March 2007
FIGURE 1 —Distribution of samples from the Caloosa Shell outcrop. Paleoecological analysis ( Daley, 2001 ) revealed two distinct assemblages that correspond to two formations. The predominantly epifaunal (seagrass) community of the Bermont Formation is shown as open triangles; the predominantly
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Figure1—Crepidula maculosaConrad, 1846 from the early Pleistocene Bermont Formation of Okeechobee County, Florida. 1, Parent CrepidulaLamarck, 1799 shell in life position on columella of OlivaBruguiére, 1789 host gastropod, UF 111876; 2, apertural view of parent shell; 3, apical view of parent shell; 4, lateral view of parent shell; 5, top-down view of parent shell, showing close fit of parent shell to host shell. Length of parent shell along long axis, 30.0 mm; length of parent shell perpendicular to long axis, 16.1 mm. Length of host shell, 60.0 mm; length of host shell perpendicular to long axis, 23.5 mm.
Published: 01 February 2004
Figure 1 — Crepidula maculosa Conrad, 1846 from the early Pleistocene Bermont Formation of Okeechobee County, Florida. 1, Parent Crepidula Lamarck, 1799 shell in life position on columella of Oliva Bruguiére, 1789 host gastropod, UF 111876; 2, apertural view of parent shell; 3
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Figure3—Numeric labels for arrows indicate illustrated character and character state respectively (see Appendix). 1–7, Tenuicorbula tenuis, Recent, Colombia, PRI 25916a, 1, 3, 4, right valve, length 22.0 mm, ×2.5, ×3.6, ×2.6 respectively, 2, 5–7, left valve, length 20.7 mm, ×13, ×2.7, ×2.6, ×3.3 respectively; 8–10, 12, Juliacorbula scutata, Pleistocene Bermont Formation, Florida, UF 83290, 8, 12, left valve, length 10.3 mm, ×5.6, 9–10, right valve, length 10.1 mm, ×5.8, ×5.6 respectively; 11, 13, 15, 16,Cuneocorbula biangulata, Eocene Paris Basin, France, USNM 326895, 11, 15, left valve, length 6.9 mm, ×7.8, 13, 16, right valve, length 9.4 mm, ×5.8; 14, 17–20,Varicorbula gibba, Recent, Ireland, UF 17610, 14, 18, right valve, length 16.3 mm, ×3.1, ×3 respectively, 17, 19, 20, left valve, length 15.0 mm, ×3.1, ×3.3, ×9 respectively
Published: 01 November 2003
, ×2.6, ×3.3 respectively; 8–10, 12 , Juliacorbula scutata , Pleistocene Bermont Formation, Florida, UF 83290, 8, 12, left valve, length 10.3 mm, ×5.6, 9–10, right valve, length 10.1 mm, ×5.8, ×5.6 respectively; 11, 13, 15, 16, Cuneocorbula biangulata , Eocene Paris Basin, France, USNM 326895
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Figure1—1–4, Thais brevicula n. sp., 1–2, holotype, height 22.9 mm, NMB H 18253; 3–4, paratype, height 15.4 mm, NMB H 18254. 5–7, Stramonita bifida n. sp., holotype, height, 113 mm NMB H 18255; 8–13, Stramonita haemastoma; 8–10, Anse bernard, Dakar, Senegal, height 75.3 mm, Vermeij collection; 11–13, Miami Rock Pit, Dade County, Florida, Bermont Formation, height 72.1 mm, Vermeij collection. 14–16, Stramonita canaliculata, Turkey Point, Florida, 71.9 mm, Vermeij collection. 17–19, Stramonita floridana, Kingston Harbour, Jamaica, height 49.4 mm, Vermeij collection. 20–25, Stramonita biserialis; 20–22, Piedra Blanca, Nayarit, Mexico, height 40.8 mm, Vermeij collection; 23–25, Playa Venado, Panamá, height 35.6 mm, Vermeij collection. 26–28, Stramonita semiplicata n. sp., holotype, 35.5 mm, NMB H 18257. 29–31, Stramonita bicarinata, Southwest Bay, Ascension Island, height 52.0 mm, Vermeij collection
Published: 01 May 2001
collection; 11–13, Miami Rock Pit, Dade County, Florida, Bermont Formation, height 72.1 mm, Vermeij collection. 14–16, Stramonita canaliculata, Turkey Point, Florida, 71.9 mm, Vermeij collection. 17–19, Stramonita floridana, Kingston Harbour, Jamaica, height 49.4 mm, Vermeij collection. 20–25
Journal Article
Published: 07 April 2025
Journal of Sedimentary Research (2025) 95 (2): 367–382.
..., Caloosahatchee, Bermont, and Fort Thompson formations). Bulk sediment samples collected from 22 horizons were used to broadly characterize stratigraphic variations in lithology and faunal content. Predation intensity was estimated from drill-hole frequency among populations of the bivalve Chione spp. While all...
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Journal Article
Published: 01 February 2004
Journal of Paleontology (2004) 78 (2): 424–429.
...Figure 2 — Crepidula maculosa from the early Pleistocene Bermont Formation, Okeechobee County, Florida. 1–5, Brooded young collected from within aperture of parent shell, UF 111877. Scale bar = 500 μm. ...
FIGURES
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Grain-size fractions of bulk sediment samples. Labels indicate resistant beds and formations (TAM, Tamiami; CA, Caloosahatchee; BM, Bermont; FT, Fort Thompson). A) Eastern sections (FSE, FSE2). B) Western section (FSW).
Published: 07 April 2025
Fig. 4. Grain-size fractions of bulk sediment samples. Labels indicate resistant beds and formations (TAM, Tamiami; CA, Caloosahatchee; BM, Bermont; FT, Fort Thompson). A) Eastern sections (FSE, FSE2). B) Western section (FSW).
Journal Article
Published: 01 May 2010
Journal of Paleontology (2010) 84 (3): 505–517.
...Figure 1 —Collecting localities in the Bermont Formation (Lower Pleistocene) at the Palm Beach Aggregate Quarry and Holey Land Canal in southern Florida ...
FIGURES | View All (14)
Journal Article
Journal: PALAIOS
Published: 01 January 2010
PALAIOS (2010) 25 (6): 400–414.
...FIGURE 1. Three views of a typical flat-based colony of Manicina areolata (PBA, UF148043) collected from the lower Bermont Formation, southern Florida. A) Oral surface. B) Lateral view. C) Basal surface. Scale in C is for all three views. ...
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FIGURE 3—Size-frequency distribution, medians, means, and 95% confidence intervals for whole C. elevata valve lengths in the Bermont and Fort Thompson Formations
Published: 01 March 2007
FIGURE 3 —Size-frequency distribution, medians, means, and 95% confidence intervals for whole C. elevata valve lengths in the Bermont and Fort Thompson Formations
Journal Article
Journal: Paleobiology
Published: 01 January 2005
Paleobiology (2005) 31 (4): 624–642.
..., Caloosahatchee Formation, including bed 1 at Sarasota; and (4) early Pleistocene, Loxahatchee Member, Bermont Formation. I considered Caloosahatchee time to be latest Pliocene (1.8 Ma) ( Akers 1972 ; Bender 1973 ; Stanley 1986 ; Jones et al. 1991 ; Campbell 1993 ), and not early Pleistocene ( Cronin 1990...
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Journal Article
Published: 01 September 2014
Journal of Paleontology (2014) 88 (5): 851–894.
... formation, Tenmile crek 02, Florida U.S.A; UF53535, Richardson Rd. Shell Pit 01B, Florida, U.S.A; UF47715, 49626 Macasphalt Shell Pit, Florida, U.S.A.; UF51907, 27564 Bermont Formation, Leisey Shell Pit, Florida, U.S.A.; LSUMG-I9314, E Destin FL. U.S.A. (Gulf of Mexico); MHNMC IB88, 11°19′86″ Lat., 74°5′ 28...
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