Abstract
A distinctive Shell and Sand Sheet found beneath the marine ponds of Anegada, British Virgin Islands, was formed by a post-1650 AD overwash event, but its origin (tsunami or hurricane) was unclear. This study assesses the taphonomic characters of the shell and large clast material (>2 mm) to determine its provenance and origin. Pond-wide stratigraphic units (Shelly Mud, Shell and Sand Sheet, Mud Cap) were analyzed (12 samples) at four sites in Bumber Well and Red Pond along with eight samples from the Shell and Sand Sheet in a 2-km transect of Bumber Well. Mollusks in the pond muds include Anomalocardia spp. and cerithids with no allochthonous shells from the offshore reef-flat. Results show that the shells and clasts (>2 mm) are derived from the erosion and winnowing of the underlying Shelly Mud of the former marine pond, forming a distinctive sheet-like deposit with Homotrema sand. The Shell and Sand Sheet contains articulated Anomalocardia bivalves and moderate numbers of angular fragments (approximately 35%) that are likely from crab predation. Radiocarbon dates of articulated Anomalocardia specimens from the Shell and Sand Sheet range widely (approximately 4000 years), with shell condition (pristine to variably preserved) showing no correlation with age. The articulated condition of the bivalves with the wide-ranging dates suggests erosion and winnowing of the underlying Shelly Mud but minimal transport of the bivalves. The Shell and Sand Sheet has taphonomic characteristics indicative of a widespread tsunami overwash (sheet-like extent and articulated specimens) but lacks allochthonous reef-flat shells. Reef-flat shell material may not have penetrated the pond, as a tsunami would have to cross the reef-flat and overtop high dunes (2.2 m) hindering transport of larger shell material but allowing the Homotrema sand to penetrate. Processes including hurricane overwash, pond wave action, or tidal channel opening and closure are not favoured interpretations as they would not produce extensive sheet-like deposits. Taphonomic analysis is hampered by the limited (400–500 years BP) depositional history from Anegada’s ponds and the lack of comparative data from other Caribbean locations.
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References
Anderson LC, McBride RA (1996) Taphonomic and paleoenvironmental evidence of Holocene shell-bed genesis and history on the northeastern Gulf of Mexico shelf. Palaios 11:532–549
Atwater BF, ten Brink US, Buckley M, Halley RS, Jaffe BF, López-Venagas AM, Reinhardt EG, Tuttle MP, Watt S, Wei Y (2011) Geomorphic and stratigraphic evidence for an unusual tsunami or storm a few centuries ago at Anegada, British Virgin Islands. Nat Hazards. doi: 10.1007/s11069-010-9622-6
Barkan R, ten Brink US, Lin J (2009) Far field tsunami simulations of the 1755 Lisbon earthquake: implications for tsunami hazard to the US east coast and the Caribbean. Mar Geol 264:109–122. doi:10.1016/j.margeo.2008.10.010
Brett CE (2003) Taphonomy: sedimentological implications of fossil preservation. In: Middleton GV (ed) Encyclopedia of sediments and sedimentary rocks. Springer, Dordrecht, pp 723–729
Brewster-Wingard G, Ishman SE (1999) Historical trends in salinity and substrate in central Florida Bay: a paleoecological reconstruction using modern analogue data. Estuaries 22:369–383
Britton JC, Morton B (1989) Shore Ecology of the Gulf of Mexico. University of Texas Press, Austin
Buckley M, Wei Y, Jaffe J, Watt S (2011) Estimated velocities and inferred cause of overwash that emplaced inland fields of boulders and cobbles at Anegada, British Virgin Islands. Nat Hazards
Dattilo BF, Brett CE, Tsujita CJ, Fairhurst R (2008) Sediment supply versus storm winnowing in the development of muddy and shelly interbeds from the Upper Ordovician of the Cincinnati region, USA. Can J Earth Sci 45:243
Davies DJ, Powell EN, Stanton RJ Jr (1989) Taphonomic signature as a function of environmental process: shells and shell beds in a hurricane-influenced inlet on the Texas coast. Palaeogeogr Palaeoclimatol Palaeoecol 72:317–356
Dix GR, Patterson RT, Parks LE (1999) Marine saline ponds as sedimentary archives of late Holocene climate and sea-level variation along a carbonate platform margin; Lee stocking island, Bahamas. Palaeogeogr Palaeoclimatol Palaeoecol 150:223–246
Donato SV, Reinhardt EG, Boyce JI, Rothaus R, Vosmer T (2008) Identifying tsunami deposits using bivalve shell taphonomy. Geology 36:199–202
Donato SV, Reinhardt EG, Boyce JI, Pilarczyk JE, Jupp BP (2009) Particle-size distribution of inferred tsunami deposits in sur lagoon, sultanate of Oman. Mar Geol 257:54–64
Donnelly JP (2005) Evidence of past intense tropical cyclones from backbarrier salt pond sediments: A case study from Isla de Culebrita, Puerto Rico, USA. J Coast Res I42:201–210
Dunn GE (1961) The hurricane season of 1960. Mon Weather Rev 89:99–108
Dunne RP, Brown BE (1979) Some aspects of the ecology of reefs surrounding Anegada, British Virgin Islands. Atoll research bulletin 236. The Smithsonian Institution, Washington, p 80
Emery KO, Stevenson RE, Hedgpeth JW (1957) Estuaries and lagoons. In: Hedgpeth JW (ed) Geological Society of America memoir 67: treatise on marine ecology and paleoecology. Geol Soc of Am, Boulder, pp 73–750
Flessa KW, Cutler AH, Meldahl KH (1993) Time and taphonomy: quantitative estimates of time-averaging and stratigraphic disorder in a shallow marine habitat. Paleobiology 19:266–286
Goff J, McFadgen BG, Chagué-Goff C (2004) Sedimentary differences between the 2002 Easter storm and the 15th-century Okoropunga tsunami, southeastern North Island, New Zealand. Mar Geol 204:235–250
Goodman-Tchernov BN, Dey HW, Reinhardt EG, McCoy F, Mart Y (2009) Tsunami waves generated by the Santorini eruption reached Eastern Mediterranean shores. Geology 37:943–946
Grindlay NR, Mann P, Dolan JF, van Gestel J (2005) Neotectonics and subsidence of the northern Puerto Rico—Virgin Islands margin in response to the oblique subduction of high-standing ridges. Geol Soc Am Spec Publ 385:31–60
Horsfield WT (1975) Quaternary vertical movements in the Greater Antilles. Geol Soc Am Bull 86:933–938
Howard J (1970) Reconnaissance geology of Anegada Island. Caribbean Research Institute, St. Thomas, p 18
Hughen KA, Baillie MGL, Bard E, Beck JW, Bertrand CJH, Blackwell PG, Buck CE, Burr GS, Cutler KB, Damon PE, Edwards RL, Fairbanks RG, Friedrich M, Guilderson TP, Kromer B, McCormac G, Manning S, Ramsey CB, Reimer PJ, Reimer RW, Remmele S, Southon JR, Stuiver M, Talamo S, Taylor FW, van der Plicht J, Weyhenmeyer CE (2004) Marine04 marine radiocarbon age calibration, 0–26 cal kyr BP; IntCal04; calibration. Radiocarbon 46:1059–1086
Jarecki L, Walkey M (2006) Variable hydrology and salinity of salt ponds in the British Virgin Islands. Saline systems 2. doi: 10.1186/1746-1448-2-2
Jones B, Hunter IG (1992) Very large boulders on the coast of Grand Cayman: the effects of giant waves on rocky coastlines. J Coast Res 8:763–774
Kidwell SM, Best MMR, Kaufman DS (2005) Taphonomic trade-offs in tropical marine death assemblages: Differential time averaging, shell loss, and probable bias in siliciclastic vs. carbonate facies. Geology 33:729–732
Liu K, Fearn ML (2000) Reconstruction of prehistoric landfall frequencies of catastrophic hurricanes in northwestern Florida from lake sediment records. Quat Res 54:238–245
López AM, Stein S, Dixon T, Sella G, Calais E, Jansma P, Weber J, LaFemina P (2006) Is there a northern Lesser Antilles forearc block? Geophys Res Lett 33. doi: 10.1029/2005GL025293
Martin AJ, Henderson SW (2003) When does a taphocoenose become a biocoenose? A storm-generated inland molluscan assemblage, San Salvador Island, Bahamas. Abstracts with programs. Geol Soc Am 35(1):64
Massari F, D’Alessandro A, Davaud E (2009) A coquinoid tsunamite from the Pliocene of Salento (SE Italy). Sediment Geol 221:7
McCabe JM, Niemi TM (2008) The 2004 Hurricane Frances overwash deposition indeposition in Salt Pond, San Salvador, the Bahamas. In: Park LE, Freile D (eds) The 13th Symposium on the geology of the Bahamas and other carbonate regions. Gerace Research Centre, San Salvador, pp 25–42
Meldahl KH, Cutler AH (1992) Neotectonics and taphonomy: pleistocene molluscan shell accumulations in the northern Gulf of California. Palaois 7:187–197
Mikkelsen PM, Bieler R (2007) Seashells of southern Florida: living marine mollusks of the Florida Keys and adjacent regions: bivalves. Princeton University Press, Princeton, NJ
Millás JC, Pardue L (1968) Hurricanes of the Caribbean and adjacent regions, 1492–1800. Academy of the Arts and Sciences of the Americas, Miami
Miller AI, Parsons KM, Cummins H, Boardman MR, Greenstein BJ, Jacobs DK (1992) Effect of hurricane hugo on molluscan skeletal distributions, Salt River Bay, St. Croix, US Virgin Islands. Geology 20:23–26
Morales JA, Borrego J, San Miguel EG, López-González N, Carro B (2008) Sedimentary record of recent tsunamis in the Huelva estuary (southwestern Spain). Quat Sci Rev 27:734–746
Morton RA, Gelfenbaum G, Jaffe BE (2007) Physical criteria for distinguishing sandy tsunami and storm deposits using modern examples. Sediment Geol 200:184–207
O’Loughlin KF, Lander JF (2003) Caribbean tsunamis; a 500-year history from 1498–1998. Kluwer Academic, Dordrecht, p 263
Parker RH (1959) Macro-invertebrate assemblages of central Texas coastal bays and Laguna Madre. Am Assoc Pet Geol Bull 43:2100–2166
Parks LE, Siewers FD, Metzger TM, Sipahioglu SM (2009) After the hurricane hits: recovery and response to large storm events in a tropical saline lake, San Salvador Island, Bahamas. Quat Int 195:98–105
Parsons-Hubbard K (2005) Molluscan taphofacies in recent carbonate reef/lagoon systems and their application to sub-fossil samples from reef cores. Palaios 20:175–191
Pickering VW (1983) Early history of the British Virgin Islands: from Columbus to emancipation. Falcon Publications International, New York
Pilarczyk JE, Reinhardt EG (2011) Homotrema rubrum (Lamarck) taphonomy as an overwash indicator in marine ponds from Anegada, British Virgin Islands. Nat Hazards. doi:10.1007/s11069-010-9706-3
Read RH (1964) Ecology and environmental physiology of some Puerto Rican bivalve molluscs and a comparison with boreal forms Carib. J Sci 4:459–465
Reid HF, Taber S (1920) The Virgin Islands earthquakes of 1867–1868. Bull Seismol Soc Am 10:9–30
Reimer PJ, Baillie MGL, Bard E, Bayliss A, Beck JW, Bertrand CJH, Blackwell PG, Buck CE, Burr GS, Cutler KB, Damon PE, Edwards RL, Fairbanks RG, Friedrich M, Guilderson TP, Hogg AG, Hughen KA, Kromer B, McCormac G, Manning S, Ramsey CB, Reimer RW, Remmele S, Southon JR, Stuiver M, Talamo S, Taylor FW, van der Plicht J, Weyhenmeyer CE (2004) IntCal04 terrestrial radiocarbon age calibration, 0–26 cal kyr BP; IntCal04; calibration. Radiocarbon 46:1029–1058
Reinhardt EG, Goodman BN, Boyce JI, Lopez G, van Hengstum P, Rink WJ, Mart Y, Raban A (2006) The tsunami of 13 December A.D. 115 and the destruction of Herod the Great’s harbor at Caesarea Maritima, Israel. Geology 34:1061–1064
Simms AR, Aryal N, Yokoyama Y, Matsuzaki H, Dewitt R (2009) Insights on a proposed Mid-Holocene highstand along the northwestern Gulf of Mexico from the evolution of small coastal ponds. J Sed Res 79:757–772
Tanner JG, Shedlock KM (2004) Seismic hazard maps of Mexico, the Caribbean, and central and south America. Tectonophysics 390:159
ten Brink US, Danforth WW, Polloni CF, Andrews B, Llanes P, Smith S, Parker E, Uozumi T (2004) New seafloor map of the Puerto Rico trench helps assess earthquake and tsunami hazards. EOS Trans Am Geophys Union 85:349
Toscano MA, Macintyre IG (2003) Corrected western Atlantic sea-level curve for the last 11,000 years based on calibrated 14C dates from Acropora palmata framework and intertidal mangrove peat. Coral Reefs 22:257–270
Warmke GL, Abbott RT (1961) Caribbean Seashells; a guide to the marine mollusks of Puerto Rico and other West Indian Islands, Bermuda and the Lower Florida Keys. Livingston Pub. Co, Narnerth, Pennsylvania
Watt S, Buckley ME, Jaffe BE (2011) Inland fields of dispersed cobbles and boulders as evidence for a tsunami on Anegada. Nat Hazards
Wei Y, ten Brink US, Atwater BF (2010) Modeling of tsunamis and hurricanes as causes of the catastrophic overwash of Anegada, British Virgin Islands, between 1650 and 1800: Abstract OS42B-03 presented at 2010 Fall meeting, American Geophysical Union, San Francisco, Calif., 13–17 December 2010
Zahibo N (2003) The 1867 Virgin Island tsunami; observations and modeling. Oceanol Acta 26:609–621
Zuschin M, Stachowitsch M, Stanton RJ Jr (2003) Patterns and processes of shell fragmentation in modern and ancient marine environments. Earth-Sci Rev 63:33–82
Acknowledgments
The government of the British Virgin Islands provided access to Anegada’s salt ponds, use of airphotos, and guidance from its specialists in disaster management, surveying, and natural science. Among them, we especially thank Cynthia Rolli, Rondell Smith, Shannon Gore, and Dylan Penn. Lianna Jarecki shared her comprehensive knowledge of Anegada’s salt ponds, and Alejandra Rodriguez assisted with field work. Brian Atwater provided comments on early drafts of the manuscript. The work was supported in part by the Nuclear Regulatory Commission under its project N6480, a tsunami-hazard assessment for the eastern United States and NSERC Discovery grant to ER.
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Reinhardt, E.G., Pilarczyk, J. & Brown, A. Probable tsunami origin for a Shell and Sand Sheet from marine ponds on Anegada, British Virgin Islands. Nat Hazards 63, 101–117 (2012). https://doi.org/10.1007/s11069-011-9730-y
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DOI: https://doi.org/10.1007/s11069-011-9730-y