Please use this identifier to cite or link to this item: https://hdl.handle.net/11017/115

Age Structure of the Fantome Island Fringing Reef


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dc.date.accessioned2012-05-24T07:58:14Zen
dc.date.available2012-05-24T07:58:14Zen
dc.date.copyright1985en
dc.date.issued1985en-US
dc.identifier.urihttp://hdl.handle.net/11017/115en
dc.description.abstractRadiocarbon age dating of three high recovery cores from the leeward fringing reef of Fantome Island (Palm Isles, Central Great Barrier Reef), indicate the reef began forming about 6,000 years BP,. The reef has formed by progradation of a hard bottom, reef top unit over soft reef slope deposits. Progradation has averaged lm/lO years over the past 5,000 years. Management of such fringing reefs will need to focus on preserving the soft reef slope deposits (to prevent erosion and undercutting) as well as maintaining a favourable environment for coral growth.en
dc.language.isoenen
dc.publisherGreat Barrier Reef Marine Park Authorityen
dc.relation.ispartofseriesTechnical memorandum TM-6en
dc.relation.ispartofseriesTechnical memorandum series-
dc.subjectCoral reef and islandsen
dc.titleAge Structure of the Fantome Island Fringing Reefen
dc.typeReporten
dc.subject.asfaProgradationen
dc.subject.asfaManagementen
dc.subject.asfaRadiocarbon datingen
dc.subject.asfaFringing reefsen
dc.format.pages26en
dc.contributor.corpauthorGreat Barrier Reef Marine Park Authorityen
dc.subject.apaisScientific researchen
dc.subject.apaisReefsen
dc.publisher.placeTownsvilleen
dc.relation.connectiontogbrmpaGBRMPA published this itemen
dc.subject.categoryProcessesen
dc.subject.categoryResearchen
dc.subject.themeManaging Multiple Useen
dc.subject.themeReef Ecosystems and Speciesen
dc.subject.locationReef-wideen
dc.keywordsFantome Island reefen
dc.keywordsAge structureen
dc.keywordsRadiocarbon datingen
dc.keywordsFringing reefsen
dc.keywordsManagementen
Appears in Collections:Management

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