Definition and introduction
The British Overseas Territory of Bermuda , a crescent-shaped chain of about 150 islands, lies in the north-west Atlantic Ocean at 32°20′N and 64°45′W, about 1,500 km south of Halifax, NS. The regional setting and geological foundation of Bermuda’s coral reefs are summarized in Logan (1992). Physiographically, Bermuda is an atoll , in that a peripheral annular reef tract and islands form a mostly submerged 26- by 52-km ellipse around a shallow central lagoon (Figure 1). The 20 m isobath separates this shallow platform from the fore-reef slope , with slopes of the latter rarely exceeding 10° seawards. The islands form the only emergent part of the Bermuda Seamount arising from 4,000 m depth and comprise a thin Pleistocene–Holocene carbonate sequence capping volcanic rocks below. The antecedent topography of this carbonate platform, formed from alternating periods of sediment movement and subaerial erosion...
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Bibliography
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Online sites (URLs)
Bermuda Reef Ecosystem Assessment and Mapping Programme (BREAM): http://www.bermudabream.org
Bermuda Zoological Society’s aerial mosaic of Bermuda’s reef platform, hosted by LookBermuda: http://www.lookbermuda.com/PhotoMap/800x600.html
Marine Environmental Program (MEP) at Bermuda Institute of Ocean Sciences (BIOS): http://www.bios-mep.info
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Logan, A., Murdoch, T. (2011). Bermuda. In: Hopley, D. (eds) Encyclopedia of Modern Coral Reefs. Encyclopedia of Earth Sciences Series. Springer, Dordrecht. https://doi.org/10.1007/978-90-481-2639-2_46
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DOI: https://doi.org/10.1007/978-90-481-2639-2_46
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