Abstract
The Bermuda islands and shallow platform lie on the top of an extinct Meso-Cenozoic volcano. The islands and the Bermuda Platform were created by reef building corals, vermetid snails and calcareous algae that colonized the eroding seamount. Coral reefs even played a significant role in the settlement of Bermuda and now human impacts of the well-populated islands are important to the ongoing health of the reefs and coral communities. The economic underpinnings of Bermuda – financial services and tourism, along with limited agriculture and small fisheries have created a society that has a moderate impact on the reefs and has a significant and direct economic interest in maintaining a healthy marine environment. Throughout the history of Bermuda, the distribution of coral reefs, and coral communities on the Platform have been determined by the interactions of several environmental factors. Pleistocene formations underlie many modern reefs and there is evidence of submerged reef tracts at depths below 60 m, all around the Bermuda Pedestal. The positions of these formations correspond to stable sea level positions attained during glacial and interglacial periods. Today, there is great variability in the marine environment on the Platform, with the most extreme conditions occurring in inshore waters. The most extensive reefs are developed around the shallow rim of the Platform and, seaward from this, down a gradually descending slope to about 50–60 m depth. Algal-vermetid cup reefs are particularly abundant in Bermuda. On the Platform, seagrass and calcareous green algae beds are closely associated spatially and ecologically with coral reefs, forming unique communities; these are widespread across the lagoon and larger inshore water bodies.
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References
Andersson J, Mackenzie FT (2011) Ocean acidification: setting the record straight. Biogeosci Discuss 8:6161–6190
Badgley BD, Lipschultz F, Sebens KP (2006) Nitrate uptake by the reef coral Diploria strigosa: effects of concentration, waterflow and irradiance. Mar Biol 149:327–338
Barnes JA, von Bodungen B (1978) The Bermuda marine environment, vol II. Bermuda Biological Station for Research, special publication no. 17. Bermuda Biological Station, St Georges
Bates NR, Amat A, Andersson AJ (2010) Feedbacks and responses of coral calcification of the Bermuda reef system to seasonal changes in biological processes and ocean acidification. Biogeosciences 7:2509–2530
Beck JW, Recy J, Taylor F, Edwards RL, Cabioch G (1997) Abrupt changes in early Holocene tropical sea surface temperature derived from coral records. Nature 385:705–707
Bermuda Census (2010) Department of Statistics, Bermuda Government, 2010 Census of population and housing preliminary results. Hamilton, Pembroke Parish
Boyer JN, Briceno HO (2010) Water quality monitoring program for Bermuda’s coastal resources. Tech Rept Southeast Environ Res Centre, Florida International University, Miami. http://serc.fiu.edu/wqmnetwork/Bermuda/home.html
Brand S (ed) (2009) Hurricane havens handbook. Naval Research Laboratory, Monterey. www.nrlmry.navy.mil?∼cannon/tr8203nc/0start.htm
Cairns SD (1979) The deep-water Scleractinia of the Caribbean and adjacent waters. Stud Fauna Curaçao. 57:1–341
Calder DR (2000) Assemblages of hydroids Cnidaria) from the three seamounts near Bermuda in the western North Atlantic. Deep-Sea Res I 47:1125–1139
Cook CB, Dodge RE, Smith SR (1994) Fifty years of impacts on coral reefs in Bermuda. In: Ginsburg RN (ed) Proceedings on global aspects of coral reefs: health, hazards, and history, Rosenstiel School of Marine and Atmospheric Science, University of Miami, Miami, pp160–166
Crowley TJ (2000) CLIMAP SSTs re-visited. Clim Dynam 16:241–255
Dodge RS, Vaisnys JR (1977) Coral populations and growth patterns: responses to sedimentation and turbidity associated with dredging. J Mar Res 35:715–730
Dodge RE, Logan A, Antonius A (1982) Quantitative reef assessment studies in Bermuda: a comparison of methods and preliminary results. Bull Mar Sci 32:745–760
Dryer S, Logan A (1978) Holocene reefs and sediments of Castle Harbour, Bermuda. J Mar Res 36:399–425
Ellison JC (1993) Mangrove retreat with rising sea-level, Bermuda. Estuar Coast Shelf Sci 37:75–87
Flood VS, Pitt JM, Smith SR (2005) Historical and ecological analysis of coral communities in Castle Harbour (Bermuda) after more than a century of environmental perturbation. Mar Pollut Bull 51:545–557
Focke JW, Gebelein CD (1978) Marine lithification of reef rock and rhodolites at a fore-reef slope locality (−50m) off Bermuda. Geol Mijnbouw 52:163–171
Fricke H, Meischner D (1985) Depth limits of Bermudan scleractinian corals: a submersible survey. Mar Biol 88:175–187
Gees RA, Medioli F (1970) A continuous seismic survey of the Bermuda Platform, part I: Castle Harbour. Marit Sed 6:21–25
Gordon AL, Guilivi CF (2008) Sea surface salinity trends: over fifty years within the subtropical North Atlantic. Oceanography 21:21–29
Guilderson TP, Fairbanks RG, Rubenstone JL (1994) Tropical temperature variations since 20,000 years ago: modulating interhemispheric climate change. Science 263:663–665
Hayward WB (1924) Bermuda past and present. Dodd Mead & Company, New York
Hearty PJ (2002) Revision of the late Pleistocene stratigraphy of Bermuda. Sed Geol 153:1–21
Hearty PJ, Kaufman DS (2000) Whole-rock aminostratigraphy and Quaternary sea-level history of the Bahamas. Quat Res 54:163–173
Hearty PJ, Olson SL (2011) Preservation of trace fossils and molds of terrestrial biota by intense storms in mid–last interglacial (MIS 5c) dunes on Bermuda, with a model for development of hydrological conduits. Palaios 26:394–405
Hearty PJ, Hollin JT, Neumann AC, O’Leary MJ, McCulloch M (2007) Global sea-level fluctuations during the last interglaciation (MIS 5e). Quat Sci Rev 26:2090–2112
Iliffe TM, Kvitek R, Blasco S, Blasco K, Covill R (2011) Search for Bermuda’s deep water caves. Hydrobiologia 677:157–168. doi:10.1007/s10750-011-0883-1
Jickells TD, Knap AH, Smith SR (1986) Trace metals and nutrient fluxes through the Bermuda inshore waters. Rapp P V Reun Cons Int Expl Mer 186:251–262
Jones RJ, Parsons R, Watkinson E, Kendall D (2010) Sewage contamination of a densely populated coral ‘atoll’ (Bermuda). Environ Monit Assess. doi:10.1007/s10661-010-1738-3
Kuhn G, Torunski H, Meischner D (1981) Reef growth and lagoon development on the Bermuda carbonate platform recorded by seismic reflection profiling and deep vibration coring. In: Proceedings of the fourth international coral reef symposium, Marine Sciences Centre, University of the Phillippines, Manila vol 1, p 597
Lapointe BE, O’Connell J (1989) Nutrient-enhanced growth of Cladophora prolifera in Harrington Sound, Bermuda: eutrophication of a confined, phosphorus-limited marine ecosystem. Estuar Coast Shelf Sci 28:347–360
Locarnini RA, Mishonov AV, Antonov JI, Boyer TP, Garcia HE (2006) In: Levitus S (ed) World ocean atlas 2005, volume 1: temperature, vol 61, NOAA Atlas NESDIS. US Government Printing Office, Washington, DC
Logan A (1988) Holocene reefs of Bermuda, vol XI, Sedimenta. Rosenstiel School of Marine and Atmospheric Science, University of Miami, Miami
Logan A (1992) Reefs. In: Thomas MLH, Logan A (eds) A guide to the ecology of shoreline and shallow-water marine communities of Bermuda, Bermuda Biological Station for Research special publication no. 30. Wm. C. Brown, Dubuque, pp 31–68
Logan A (1998) The high-latitude coral reefs of Bermuda: characteristics and comparisons. In: Viera Rodriguez MA, Haroun R (eds) Proceedings of the second symposium of fauna and flora of the Atlantic Islands, Las Palmas de Gran Canaria, 1996, Bol Mus Municipal do Funchal, Las Palmas, suppl. 5, pp 187–197
Logan A, Murdoch TJT (2011) Bermuda. In: Hopley D (ed) Encyclopedia of modern coral reefs. Springer, Dordrecht, pp 118–123
Logan A, Mathers SM, Thomas MLH (1984) Sessile invertebrate coelobite communities from reefs of Bermuda: species composition and distribution. Coral Reefs 2:205–213
Logan A, Yang L, Tomascik T (1994) Linear skeletal extension rates in two species of Diploria from high-latitude reefs of Bermuda. Coral Reefs 13:225–230
Marine Environmental Program (2007) Annual report: 2006 to 2007. Annual report submitted by the Bermuda Institute of Ocean Sciences to the Bermuda Department of Environmental Protection, Ministry of Environment and Sport. Bermuda Aquarium, Museum, and Zoo Pub #2230
McGillicuddy DJ, Anderson LA, Bates NR, Bibby T, Buesseler KO, Carlson CA, Davis CS, Ewart C, Falkowski PG, Goldthwait SA, Hansell DA, Jenkins WJ, Johnson R, Kosnyrev VK, Ledwell JR, Li QP, Siegel DA, Steinberg DK (2007) Eddy/wind interactions stimulate extraordinary mid-ocean plankton blooms. Science 316:1021–1026
McGlathery KJ (1995) Nutrient and grazing influences on a subtropical seagrass community. Mar Ecol Prog Ser 122:239–252
Meischner D, Meischner U (1977) Bermuda south shore reef morphology – a preliminary report In: Taylor DL (ed) Proceedings of the third international coral reef symposium, Rosenstiel School of Marine and Atmospheric Science, University of Miami, Miami, vol 2, pp 243–250
Montoya M, Crowley TJ, von Storch H (1998) Temperatures at the last interglacial simulated by a coupled ocean atmosphere model. Palaeo Oceanogr 13:170–177
Moore HB, Moore DM (1946) Preglacial history of Bermuda. Bull Geol Soc Am 57:207–222
Morris BF, Barnes J, Brown IF, Markham JC (1977) The Bermuda marine environment, vol I. Bermuda Biological Station for Research, special publication no. 15. Bermuda Biological Station for Research, St Georges
Muhs DR, Simmons KR, Steinke B (2002) Timing and warmth of the last interglacial period: new U-series evidence from Hawaii and Bermuda and a new fossil compilation for North America. Quat Sci Rev 21:1355–1383
Murdoch TJT (2007) A functional group approach for predicting the composition of hard coral assemblages in Florida and Bermuda. Ph.D. thesis, University of South Alabama, Mobile
Murdoch TJT, Glasspool AF, Outerbridge M, Ward J, Manuel S, Nash A, Coates KA, Pitt J, Fourqurean JW, Barnes PAG, Vierros M, Holzer K, Smith SR (2007) Large-scale decline in offshore seagrass meadows in Bermuda. Mar Ecol Prog Ser 339:123–130
NASA (2010) Surface meteorology and solar energy. A renewable energy resource web site (release 6.0), Stackhouse PW Jr, Whitlock CH, Kusterer JM (Administrators). http://eosweb.larc.nasa.gov/sse/
Neumann CJ, Cry GW, Caso EL, Jarvinen BR (1985) Tropical cyclones of the North Atlantic Ocean, 1871–1980. National Climatic Center, Asheville
NOAA (2012) Tides and currents. http://www.tidesandcurrents.noaa.gov/geo.shtml?location=2695540
Olson SL, Hearty PJ (2009) A sustained +21 m sea-level highstand during MIS 11 (400 ka): direct fossil and sedimentary evidence from Bermuda. Quat Sci Rev 28:271–285
Olson SL, Hearty PJ, Pregill GK (2006) Geological constraints on evolution and survival in endemic reptiles on Bermuda. J Herp 40:394–398
Pirazzoli PA (1987) Recent sea-level changes in the North Atlantic. In: Scott DB, Pirazzoli PA, Honig CA (eds) Later Quarternary sea-level correlation and applications. Kluwer, Boston, pp 153–167
Pirsson LV (1914a) Geology of Bermuda Island: the igneous platform. Am J Sci 38:189–206
Pirsson LV (1914b) Geology of Bermuda Island: petrology of the lavas. Am J Sci 38:331–344
Precht WF, Miller SL (2007) Ecological shifts along the Florida reef tract. In: Aronson RB (ed) Geological approaches to coral reef ecology. Springer, New York, pp 237–312
Prognon F, Cojan I, Kindler P, Thiry M, Demange M (2011) Mineralogical evidence for a local volcanic origin of the parent material of Bermuda Quaternary paleosols. Quat Res 75:256–266
Seamount Biogeosciences Network (2012) Seamount catalogue. Earthref.org/SC/
Seigel DA, McGillicuddy DJ Jr, Fields EA (1999) Mesoscale eddies, satellite altimetry, and new production in the Sargasso Sea. J Geophys Res 104:13,359–13,379
Siegel DA, Michaels AF, Sorensen JC, O’Brien MC, Hammer MA (1995) Seasonal variability of light availability and utilization in the Sargasso Sea. J Geophys Res 100:8695–8713
Simmons JAK, Johnson R (1993) Measurements of coastal currents at Tynes Bay and the North Lagoon, Bermuda. Bermuda Biological Station for Research, St Georges
Simmons JAK, Lyons WB (1994) The ground water flux of nitrogen and phosphorus to Bermuda’s coastal waters. Water Res Bull 306:983–991
Smith Warner International (2004) Bermuda coastal erosion vulnerability assessment report. Submitted to the Government of Bermuda, Ministry of the Environment
Spalding M, Fos H, Allen G, Davidson N, Ferdaña Z, Finlayson M, Halpern BS, Jorge MA, Lomgana A, Lourie SA, Martin KD, McManus E, Molnar J, Recchia CA, Robertson J (2007) Marine ecoregions of the world: a bioregionalization of coastal and shelf areas. Bioscience 57:573–583
Stanley DJ, Swift DJP (1968) Bermuda’s reef front platform – bathymetry and significance. Mar Geol 6:479–500
State of the Environment Report (2005) Ministry of the Environment Bermuda government. Hamilton, Pembroke Parish
Steinberg DK, Carlson CA, Bates NR, Johnson RJ, Michaels AF, Knap AH (2001) Overview of the US JGOFS Bermuda Atlantic Time-series Study (BATS): a decade-scale look at ocean biology and biogeochemistry. Deep-Sea Res II 48:1405–1447
Thacker WC, Sindlinger L (2007) Estimating salinity to complement observed temperature: 2 Northwestern Atlantic. J Mar Sci 65:249–267
Thomas MLH, Stevens J (1991) Communities of constructional lips and cup reef rims in Bermuda. Coral Reef 9:225–230
Trend-Staid M, Prell WL (2002) Sea surface temperature at the last glacial maximum: a reconstruction using the modern analog technique. Paleoceanography 17:1065–1083
Upchurch SB (1970) Sedimentation on the Bermuda Platform. U.S. Army Corps of Engineers, U.S. Lake Survey Research Report, RR 2–2, Detroit
Vacher HL, Rowe MP (1997) Geology and hydrogeology of Bermuda. In: Vacher HL, Quinn T (eds) Geology and hydrogeology of carbonate islands, 54 Developments in sedimentology. Elsevier, Amsterdam, pp 35–90
Vogt PR (1979) Volcano height and paleo-plate thickness. In: Tucholke BE, Vogt PR (eds) Initial reports of the deep sea drilling project, vol 43. US Government Printing Office, Washington, DC, pp 877–878
Vogt PR, Jung W-Y (2007) Origin of the Bermuda volcanoes and Bermuda Rise: history, observations, models, and puzzles. In: Foulger GR, Jurdy DM (eds) Plates, plumes, and planetary processes, Geological Society America special paper no. 430. Geological Society of America, Boulder
von Bodungen B, Jickells TD, Smith SR, Ward JAD, Hillier GB (1982) The Bermuda marine environment vol III: final report of the Bermuda inshore waters investigation. Bermuda Biological Station for Research special publication no. 19. St Georges, Bermuda
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Coates, K.A., Fourqurean, J.W., Kenworthy, W.J., Logan, A., Manuel, S.A., Smith, S.R. (2013). Introduction to Bermuda: Geology, Oceanography and Climate. In: Sheppard, C. (eds) Coral Reefs of the United Kingdom Overseas Territories. Coral Reefs of the World, vol 4. Springer, Dordrecht. https://doi.org/10.1007/978-94-007-5965-7_10
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