Please use this identifier to cite or link to this item: https://apo.ansto.gov.au/dspace/handle/10238/6326
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dc.contributor.authorMcGregor, HV-
dc.contributor.authorWoodroffe, CD-
dc.contributor.authorFischer, MJ-
dc.contributor.authorGagan, MK-
dc.contributor.authorFink, D-
dc.date.accessioned2015-10-14T01:24:42Z-
dc.date.available2015-10-14T01:24:42Z-
dc.date.issued2013-08-01-
dc.identifier.citationMcGregor, H. V., Woodroffe, C. D., Fischer, M., Gagan, M. K., & Fink, D. (2013). Coral microatoll reconstructions of El Niño-Southern Oscillation: New windows on seasonal and interannual processes. PAGES news 21(2), 52-53. doi:10.22498/pages.21.2.52en_AU
dc.identifier.govdoc6159-
dc.identifier.issn1811-1602-
dc.identifier.urihttps://doi.org/10.22498/pages.21.2.52en_AU
dc.identifier.urihttp://apo.ansto.gov.au/dspace/handle/10238/6326-
dc.description.abstractPorites corals are the most commonly used genus for reconstructing El Niño- Southern Oscillation (ENSO). This hermatypic coral is found in all tropical reef environments(Veron 2000) with a variety of growth forms. Climate reconstructions of a century or more have been obtained from the most common, dome-shaped Porites growth form, whereby the colonies, beginning from the substrate, grow outward and upward towards the ocean surface(Knutson et al. 1972). Domed structures, however, are not the only Porites growth form. © 2013, Authors.en_AU
dc.language.isoenen_AU
dc.publisherPAGES Past Global Changesen_AU
dc.subjectCoralsen_AU
dc.subjectSouthern oscillationen_AU
dc.subjectSeasonsen_AU
dc.subjectWindowsen_AU
dc.subjectDomed structuresen_AU
dc.subjectClimatesen_AU
dc.titleCoral microatoll reconstructions of El Niño-southern oscillation: new windows on seasonal and interannual processesen_AU
dc.typeJournal Articleen_AU
dc.date.statistics2015-10-09-
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