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Journal Article

The Genus Strombus (Mollusca: Caenogastropoda: Strombidae) in the Neogene of the Bocas del Toro Area, Panama, with the Description of Three New Species

Bernard Landau, Gijs C. Kronenberg, Gregory S. Herbert, Carlos M. da Silva
Published: 01 March 2011
Journal of Paleontology (2011) 85 (2): 337–352.
DOI: https://doi.org/10.1666/10-047.1
... are a suitable starting point for the revision of the gastropod assemblages from the Neogene of Bocas del Toro. Six species of Strombus are described, three of them new: S. acanthospira n. sp., S. pugiloides , S. gatunensis , S. elegantissimus n. sp., S. vermeiji n. sp. and S . cf. floridanus . Figure 1...
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View PDF for article title, The Genus <span class="search-highlight">Strombus</span> (Mollusca: Caenogastropoda: Strombidae) in the Neogene of the Bocas del Toro Area, Panama, with the Description of Three New Species
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Journal Article

The influence of sponge borings on aragonite-to-calcite inversion in late Pleistocene Strombus gigas from Grand Cayman, British West Indies

Jill Rehman, Brian Jones, T. H. Hagan, M. Coniglio
Published: 01 April 1994
Journal of Sedimentary Research (1994) 64 (2a): 174–179.
DOI: https://doi.org/10.1306/D4267D48-2B26-11D7-8648000102C1865D
...Jill Rehman; Brian Jones; T. H. Hagan; M. Coniglio Abstract Large, robust Strombus gigas lived in a variety of habitats in the Ironshore Lagoon that existed on Grand Cayman during the Late Sangamon highstand, approximately 125,000 years ago. Some well-preserved shells are still entirely aragonitic...
View PDF for article title, The influence of sponge borings on aragonite-to-calcite inversion in late Pleistocene <span class="search-highlight">Strombus</span> gigas from Grand Cayman, British West Indies
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Journal Article

Th/U dating of Strombus bubonius -bearing marine terraces in southeastern Spain

Claude Hillaire-Marcel, Odette Carro, Christiane Causse, José-Luis Goy, Cari Zazo
Journal: Geology
Published: 01 July 1986
Geology (1986) 14 (7): 613–616.
DOI: https://doi.org/10.1130/0091-7613(1986)14<613:TDOSBM>2.0.CO;2
... was demonstrated to yield coherent chronologies in both continental and marine environments. We report on 34 new Th and U isotope measurements on Strombus bubonius and Glycymeris glycymeris fossils from raised marine terraces in the Almeria area, southeastern Spain. The results yield a coherent chronology...
View PDF for article title, Th&#x2F;U dating of <span class="search-highlight">Strombus</span> bubonius -bearing marine terraces in southeastern Spain
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Journal Article

The role of skeletal porosity in aragonite neomorphism-Strombus and Montastrea from the Pleistocene Key Largo Limestone, Florida

Gale D. Martin, Bruce H. Wilkinson, Kyger C. Lohmann
Published: 01 March 1986
Journal of Sedimentary Research (1986) 56 (2): 194–203.
DOI: https://doi.org/10.1306/212F88B9-2B24-11D7-8648000102C1865D
... and Strombus gigas, from the vadose zone of the Pleistocene Key Largo Formation in southern Florida, were examined in order to evaluate the effect of initial skeletal porosity on system closure during neomorphism. Fabrics of replacement calcite in both taxa are similar, consisting of blocky crystals largely...
View PDF for article title, The role of skeletal porosity in aragonite neomorphism-<span class="search-highlight">Strombus</span> and Montastrea from the Pleistocene Key Largo Limestone, Florida
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Figure9. 1–3, Strombus cf. floridanus, NMB H18454, height 54.4 mm, locality PPP 01188 ( = NMB 18373), southeast coast, north of Piedra Roja Point, Cayo Agua Island, Cayo Agua Formation, Zanclean, Early Pliocene; 4–6, Strombus cf. floridanus, NMB H18447, height 65.0 mm, locality NMB 17477, Rio Banano, Costa Rica, Banano Formation, Piacenzian, Pliocene; 7–10, Strombus cf. floridanus. NHMW 2010/0039/0011 (ex BL coll.), height 61.3 mm, Tiburon Point, Cayo Agua Island, Cayo Agua Formation, Zanclean, Pliocene; 11–13, Strombus cf. floridanus, NMB H18446, height 50.0 mm, locality PPP 01735 (NMB 17455), Rio Banano, Quitaria, 2.3 km southwest of bridge, Costa Rica, Banano Formation, Zanclean, Pliocene; 14–16, Strombus floridanusMansfield, 1930. Greg Herbert coll., height 61.3 mm, SMR Quarry, Sarasota Co., Florida, U.S.A., lower Pinecrest Beds, Tamiami Formation (3.5–2.5 Ma), Zanclean, late Pliocene; 17–19, Strombus floridanusMansfield, 1930, Greg Herbert coll., height 80.0 mm, Okeelanta Sugar Co., Florida, U.S.A., Caloosahatchee Formation (2.5–1.8 Ma), lower Pleistocene.

Figure 9 . 1–3, Strombus cf. floridanus , NMB H18454, height 54.4 mm, l...

Published: 01 March 2011
Figure 9 . 1–3, Strombus cf. floridanus , NMB H18454, height 54.4 mm, locality PPP 01188 ( = NMB 18373), southeast coast, north of Piedra Roja Point, Cayo Agua Island, Cayo Agua Formation, Zanclean, Early Pliocene; 4–6, Strombus cf. floridanus , NMB H18447, height 65.0 mm, locality NMB 17477
Image
Figure4. 1–5, Strombus acanthospira n. sp., holotype, NMB H18372, height 61.2 mm, locality PPP 02247 ( = NMB 18744), Ground Creek, about 400 m NNE of PJ2282, first tributary NE from yard of boat-house, Isla Colon, Ground Creek Unit, Calabrian, Pleistocene; 6, 7, Strombus acanthospira n. sp., paratype 1, NMB H18459, height 54.8 mm, locality PPP 02247 ( = NMB 18744), Ground Creek, about 400 m NNE of PJ2282, first tributary NE from yard of boat-house, Isla Colon, Ground Creek Unit, Calabrian, Pleistocene; 8, 9, Strombus acanthospira n. sp., NHMW 2010/0039/0001, height 75.8 mm, Las Lomas, Puerto Limon, Costa Rica, Moin Formation, Pleistocene, Gelasian-Calabrian; 10–13, Strombus pugiloidesGuppy, 1873, lectotype USNM 115477, height 56.3 mm, Bowden Formation, Pliocene-?Pleistocene, Jamaica; 14–16, Strombus pugiloidesGuppy, 1873, paralectotype 1, USNM 542241, height 56.8 mm, Bowden Formation, Pliocene-?Pleistocene, Jamaica.

Figure 4 . 1–5, Strombus acanthospira n. sp., holotype, NMB H18372, heig...

Published: 01 March 2011
Figure 4 . 1–5, Strombus acanthospira n. sp., holotype, NMB H18372, height 61.2 mm, locality PPP 02247 ( = NMB 18744), Ground Creek, about 400 m NNE of PJ2282, first tributary NE from yard of boat-house, Isla Colon, Ground Creek Unit, Calabrian, Pleistocene; 6, 7, Strombus acanthospira n. sp
Image
Figure8. 1–3, Strombus vermeiji n. sp., holotype, NHMW 2010/0039/0008 (ex BL coll.), height 55.3 mm, Area C, Escudo de Veraguas Island, lower part of the Escudo de Veraguas Formation, Piacenzian, Pliocene; 4, 5, Strombus vermeiji n. sp., paratype, NHMW 2010/0039/0009 (ex BL coll.), height 49.3 mm, Area C, Escudo de Veraguas Island, lower part of the Escudo de Veraguas Formation, Piacenzian, Pliocene; 6, Strombus elegantissimus n. sp., holotype, NMB H18451, height 62.1 mm, locality PPP 02172 ( = NMB 18671) Area A, Escudo de Veraguas Island, northwest coast, small island about 600m W of 2207, “Cerro Antoine,” upper part of the Escudo de Veraguas Formation, Gelasian, Pleistocene, detail of spire sculpture;7, Strombus pugiloidesGuppy, 1873, NHMW 2010/0039/0010 (ex BL coll.), height 53.2 mm, Area C, Escudo de Veraguas Island, lower part of the Escudo de Veraguas Formation, Piacenzian, Pliocene, detail of spire sculpture; 8, Strombus gatunensisToula, 1909, NMB H18452, height 54.2 mm, locality PPP 01967 ( = NMB 18772), Nispero Point, Cayo Agua Island, Cayo Agua Formation, Zanclean, Pliocene, detail of spire sculpture; 9, Strombus vermeiji n. sp., holotype, NHMW 2010/0039/0008 (ex BL coll.), height 55.3 mm, Area C, Escudo de Veraguas Island, lower part of the Escudo de Veraguas Formation, Piacenzian, Pliocene, detail of spire sculpture.

Figure 8 . 1–3, Strombus vermeiji n. sp., holotype, NHMW 2010/0039/0008 ...

Published: 01 March 2011
Figure 8 . 1–3, Strombus vermeiji n. sp., holotype, NHMW 2010/0039/0008 (ex BL coll.), height 55.3 mm, Area C, Escudo de Veraguas Island, lower part of the Escudo de Veraguas Formation, Piacenzian, Pliocene; 4, 5, Strombus vermeiji n. sp., paratype, NHMW 2010/0039/0009 (ex BL coll.), height
Image
Figure5. 1–4, Strombus pugiloidesGuppy, 1873, paralectotype 2, USNM 542242, height 56.2 mm, Bowden Formation, Pliocene-?Pleistocene, Jamaica; 5–7, Strombus pugiloidesGuppy, 1873, NHMW 2010/0039/0002 (ex BL coll.), height 52.3 mm, Area C, Escudo de Veraguas Island, lower part of the Escudo de Veraguas Formation, Piacenzian, Pliocene, specimen with sharp knobs on shoulder of last whorl; 8–10, Strombus pugiloidesGuppy, 1873, NHMW 2010/0039/0003 (ex BL coll.), height 52.5 mm, Area C, Escudo de Veraguas Island, lower part of the Escudo de Veraguas Formation, Piacenzian, Pliocene, specimen with sharp knobs on shoulder only on abapical half of last whorl; 11–13, Strombus pugiloidesGuppy, 1873, NHMW 2010/0039/0004 (ex BL coll.), height 54.0 mm, Area C, Escudo de Veraguas Island, lower part of the Escudo de Veraguas Formation, Piacenzian, Pliocene, specimen with smooth last whorl; 14, 15, Strombus pugiloidesGuppy, 1873 (SPINEY), NHMW 2010/0039/0005 (ex BL coll.), height 52.2 mm, Area C, Escudo de Veraguas Island, lower part of the Escudo de Veraguas Formation, Piacenzian, Pliocene.

Figure 5 . 1–4, Strombus pugiloides Guppy, 1873 , paralectotype 2, USNM ...

Published: 01 March 2011
Figure 5 . 1–4, Strombus pugiloides Guppy, 1873 , paralectotype 2, USNM 542242, height 56.2 mm, Bowden Formation, Pliocene-?Pleistocene, Jamaica; 5–7, Strombus pugiloides Guppy, 1873 , NHMW 2010/0039/0002 (ex BL coll.), height 52.3 mm, Area C, Escudo de Veraguas Island, lower part
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FIGURE 5—Strombus and Telescopium shells present on tethered arrays by sample date (1994, 1995, 1999) along the AA transect. Shells collected in 1994 were deployed for one year; in 1995, for two years, and in 1999, for six years. For all sample dates and depths (except for 15 and 30 m in 1999) frequencies were computed for n = 4 shells each, Strombus or Telescopium. For 15-m and 30-m sites in 1999, frequencies were computed for n = 8 shells each as both replicates were combined for Strombus and Telescopium (refer to Appendix 1 for raw data)

FIGURE 5 — Strombus and Telescopium shells present on tethered arrays by...

Published: 01 April 2002
FIGURE 5 — Strombus and Telescopium shells present on tethered arrays by sample date (1994, 1995, 1999) along the AA transect. Shells collected in 1994 were deployed for one year; in 1995, for two years, and in 1999, for six years. For all sample dates and depths (except for 15 and 30 m in 1999
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Figure6. 1–3, Strombus gatunensisToula, 1909, NMB H18455, height 63.3 mm, locality PPP 00348 ( = NMB 17829), unnamed promontory between Tiburon &amp; Piedra Roja Points, West side, Cayo Agua Island, Cayo Agua Formation, Zanclean, Pliocene; 4–6, Strombus gatunensisToula, 1909, H18452, height 54.2 mm, locality PPP 01967 ( = NMB 18772), Nispero Point, Cayo Agua Island, Cayo Agua Formation, Zanclean, Pliocene, specimen showing horizontal chevron color pattern; 7–9, Strombus gatunensisToula, 1909, NMB H18453, height 71.8 mm, locality PPP 01203 ( = NMB 18374), east coast, south of Norte Point, Cayo Agua Island, Cayo Agua Formation, Zanclean, Pliocene, specimen with broad last whorl; 10–12, Strombus gatunensisToula, 1909, NMB H18448, height 68.0 mm, locality PPP 01735 ( = NMB 17455), Rio Banano, Quitaria, 2.3km southwest of bridge, Costa Rica, Banano Formation, Piacenzian, Pliocene, specimen with broad last whorl.

Figure 6 . 1–3, Strombus gatunensis Toula, 1909 , NMB H18455, height 63....

Published: 01 March 2011
Figure 6 . 1–3, Strombus gatunensis Toula, 1909 , NMB H18455, height 63.3 mm, locality PPP 00348 ( = NMB 17829), unnamed promontory between Tiburon & Piedra Roja Points, West side, Cayo Agua Island, Cayo Agua Formation, Zanclean, Pliocene; 4–6, Strombus gatunensis Toula, 1909 , H18452
Image
Figure7. 1–3, Strombus gatunensisToula, 1909, holotype, NHMW 1933/18/185, height 43.0 mm (specimen figured by Toula, 1909, pl. 25, fig. 7), Gatun Formation, Gatun, Panama, Pliocene; 4–6, Strombus elegantissimus n. sp., holotype, NMB H18451, height 62.1 mm, locality PPP 02172 ( = NMB 18671), Area A, Escudo de Veraguas Island, northwest coast, small island about 600m W of 2207, “Cerro Antoine,” upper part of the Escudo de Veraguas Formation, Gelasian, Pleistocene, 7–9, Strombus elegantissimus n. sp., paratype 1, NMB H18450, height 62.7 mm, locality PPP 00178 ( = NMB 17626), Area A, Escudo de Veraguas Island, Long Bay Point, about 20m east of CJ87-10-06, upper part of the Escudo de Veraguas Formation, Gelasian, Pleistocene; 10–12, Strombus elegantissimus n. sp., paratype 2, NHMW 2010/0039/0006 (ex BL coll.), height 65.5 mm, Area A, Escudo de Veraguas Island, upper part of the Escudo de Veraguas Formation, Gelasian, Pleistocene.

Figure 7 . 1–3, Strombus gatunensis Toula, 1909 , holotype, NHMW 1933/18...

Published: 01 March 2011
Figure 7 . 1–3, Strombus gatunensis Toula, 1909 , holotype, NHMW 1933/18/185, height 43.0 mm (specimen figured by Toula, 1909 , pl. 25, fig. 7), Gatun Formation, Gatun, Panama, Pliocene; 4–6, Strombus elegantissimus n. sp., holotype, NMB H18451, height 62.1 mm, locality PPP 02172 ( = NMB
Image
Figure2—StrombusLinnaeus, 1758 and HemichenopusSteinmann and Wilckens, 1908. 1–3, Strombus (Austrombus) medinae (Philippi, 1887), late Miocene, central Chile. 1, Lost holotype (from Philippi, 1887), height 90 mm. 2, 3, Neotype SGO.PI.5964, height 73.7 mm. 4, 5, 9, Hemichenopus araucanus (Philippi, 1887), ?Eocene, south-central Chile. 4, Syntype SGO.PI.4504, height 19 mm. 5, Syntype SGO.PI.4504 (on backside of sample). 9, Syntype SGO.PI.763, height 19 mm. 6–8, Hemichenopus zelandicus (Marshall, 1919), Middle Eocene, New Zealand. Hypotype TM 5131, height 25 mm

Figure 2 — Strombus Linnaeus, 1758 and Hemichenopus Steinmann and Wilc...

Published: 01 November 2005
Figure 2 — Strombus Linnaeus, 1758 and Hemichenopus Steinmann and Wilckens, 1908 . 1–3, Strombus ( Austrombus ) medinae ( Philippi, 1887 ), late Miocene, central Chile. 1, Lost holotype (from Philippi, 1887 ), height 90 mm. 2, 3, Neotype SGO.PI.5964, height 73.7 mm. 4, 5, 9
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FIGURE 4—Tethered shell array with empty shells of Strombus and Telescopium, weight, and square float to facilitate array recovery

FIGURE 4 —Tethered shell array with empty shells of Strombus and Telesco...

Published: 01 April 2002
FIGURE 4 —Tethered shell array with empty shells of Strombus and Telescopium , weight, and square float to facilitate array recovery
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FIGURE 7—Selected Strombus from the tethered experimental arrays. (A) Tethered Strombus in good condition, AA transect, 1994, 88-m depth, shell height 56.05 mm. (B) Outer lip fragment, AA transect, 1995, 15-m depth, 38.72 mm length. (C) Outer lip fragment, AA transect, 1995, 30-m depth, 40.26 mm length. (D) Putative stomatopod damage, AA transect, 1995, 30-m depth, shell height 56.74 mm

FIGURE 7 —Selected Strombus from the tethered experimental arrays. (A) Te...

Published: 01 April 2002
FIGURE 7 —Selected Strombus from the tethered experimental arrays. (A) Tethered Strombus in good condition, AA transect, 1994, 88-m depth, shell height 56.05 mm. (B) Outer lip fragment, AA transect, 1995, 15-m depth, 38.72 mm length. (C) Outer lip fragment, AA transect, 1995, 30-m depth, 40.26
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FIGURE 9—Strombus and Telescopium shells present on tethered arrays by sample date (1995, 1996) along the BA transect. Shells collected in 1995 were deployed for one year; in 1996, for two years. Samples were not collected in 1999 for the BA transect. All replicates were collected for all sites below 30 m and graphed separately because the replicates were affected differentially by predation (see especially the 30-m S site where all shells were preyed on, in contrast to the 30-m N site, which had at least half the shells retained on the arrays). For the 15-m site, only one replicate was collected. For all sample dates, replicates, and depths, frequencies were computed for n = 4 shells each, Strombus or Telescopium (refer to Appendix 2 for raw data)

FIGURE 9 — Strombus and Telescopium shells present on tethered arrays by...

Published: 01 April 2002
FIGURE 9 — Strombus and Telescopium shells present on tethered arrays by sample date (1995, 1996) along the BA transect. Shells collected in 1995 were deployed for one year; in 1996, for two years. Samples were not collected in 1999 for the BA transect. All replicates were collected for all
Image
FIGURE 10—Peeled or sheared Strombus from slope depths, BA transect. (A) Peeled aperture, 183-m depth, shell height, 43.35 mm. (B) Outer lip fragment, 195-m depth, 37.68 mm

FIGURE 10 —Peeled or sheared Strombus from slope depths, BA transect. (A)...

Published: 01 April 2002
FIGURE 10 —Peeled or sheared Strombus from slope depths, BA transect. (A) Peeled aperture, 183-m depth, shell height, 43.35 mm. (B) Outer lip fragment, 195-m depth, 37.68 mm
Image
—Fragment of Strombus shell and specimen of reef rock (on right) showing evidence of burrowing organisms.

—Fragment of Strombus shell and specimen of reef rock (on right) showing ...

Published: 01 May 1962
Fig. 12. —Fragment of Strombus shell and specimen of reef rock (on right) showing evidence of burrowing organisms.
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APPENDIX 1  Type of biological taphonomic damage of experimentally deployed...

Published: 01 April 2002
= South site. Each tethered array had four Strombus and four Telescopium deployed; for 1999, two replicates were examined for a total of eight Strombus and eight Telescopium
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Disposition, morphology, and possible functions of the opercula in different gastropod taxa across the Phanerozoic. (1) Early Ordovician Teiichispira: 1. Teiichispira argentina (Kayser, 1876); 2. Teiichispira teresae n. sp.; 3. Unguiculate operculum of Teiichispira teresae n. sp.; (2) Early Ordovician Ceratopea: 1, 2. Ceratopea unguis Yochelson and Bridge, 1957, life association of the shell and unguiculate operculum (taken from Rohr et al., 2004); (3) Holocene Strombus: 1. Strombus pugilis Linnaeus, 1758 (taken from the www.marinespecies.org); 2. unguiculate operculum Strombus pugilis (taken from Simone, 2005); (4) Late Triassic/Late Jurassic Neritimorpha: 1. Late Triassic Fedaiella neritacea (Münster, 1841) with the low multispiral operculum in place (taken from Bandel, 2007); 2. Late Jurassic Neritopsis subvaricosa Brösamlen, 1909, operculum with an adaxial projection (taken from Kaim and Sztajner, 2005); 3. Middle Jurassic Neridomus sp. with the paucispiral operculum in place (taken from Bandel, 2008); 4. Recent Smaragdia Issel, 1869, with the paucispiral operculum in place showing close resemblance to the Jurassic Neridomus (taken from Bandel, 2008); 5. paucispiral operculum of the recent Neritina corona (Linnaeus, 1758) (taken from Bandel, 2008). Note that the characterization of the unguiculate, low-multispiral, and paucispiral opercula shown in the bottom of the figure were extracted and modified from Simone (2020).

Disposition, morphology, and possible functions of the opercula in differen...

Published: 01 May 2023
. sp.; ( 2 ) Early Ordovician Ceratopea : 1, 2. Ceratopea unguis Yochelson and Bridge, 1957 , life association of the shell and unguiculate operculum (taken from Rohr et al., 2004 ); ( 3 ) Holocene Strombus : 1. Strombus pugilis Linnaeus, 1758 (taken from the www.marinespecies.org ); 2
Journal Article

CENOZOIC STROMBIDAE, APORRHAIDAE, AND STRUTHIOLARIIDAE (GASTROPODA: STROMBOIDEA) FROM CHILE: THEIR SIGNIFICANCE TO THE INTERPRETATION OF SOUTHEAST PACIFIC BIOGEOGRAPHY AND CLIMATE

SVEN N. NIELSEN
Published: 01 November 2005
Journal of Paleontology (2005) 79 (6): 1120–1130.
DOI: https://doi.org/10.1666/0022-3360(2005)079[1120:CSAASG]2.0.CO;2
...Figure 2 — Strombus Linnaeus, 1758 and Hemichenopus Steinmann and Wilckens, 1908 . 1–3, Strombus ( Austrombus ) medinae ( Philippi, 1887 ), late Miocene, central Chile. 1, Lost holotype (from Philippi, 1887 ), height 90 mm. 2, 3, Neotype SGO.PI.5964, height 73.7 mm. 4, 5, 9...
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View PDF for article title, CENOZOIC STROMBIDAE, APORRHAIDAE, AND STRUTHIOLARIIDAE (GASTROPODA: STROMBOIDEA) FROM CHILE: THEIR SIGNIFICANCE TO THE INTERPRETATION OF SOUTHEAST PACIFIC BIOGEOGRAPHY AND CLIMATE
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