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- W1606437650 abstract "This chapter explains the geology of the Pitcairn Islands Group with special emphasis on the three carbonate islands of Southern Polynesia. The chapter considers the reefs in the Pitcairn Group to be depauperate because: (1) successful recolonization of coral populations after Quaternary sea-level lows might have been inhibited by long oceanic distances, and (2) water temperatures are low compared to Pacific islands located to the northwest. The Pitcairn Islands are probably the most remote and least- studied group of carbonate islands in the Pacific Ocean. The most recent scientific expeditions have been of short duration: the National Geographic Society-Oceanic Institute Expedition, Operation Raleigh, and the Smithsonian Institution's visit by RV Rambler all lasted only a few days. The Pitcairn Island Group comprises, from west to east, Oeno Atoll, Pitcairn Island, Henderson Island, and Ducie Atoll. Oeno, Henderson, and Ducie are all carbonate islands and support living coral reefs. Pitcairn Island, although supporting a localized carbonate reef (corals growing on rocks) with low diversity and abundance, is not a carbonate island, but a volcanic one." @default.
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- W1606437650 date "2004-01-01" @default.
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- W1606437650 title "Geology of Selected Islands of the Pitcairn Group, Southern Polynesia" @default.
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- W1606437650 doi "https://doi.org/10.1016/s0070-4571(04)80034-7" @default.
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