Please use this identifier to cite or link to this item: https://apo.ansto.gov.au/dspace/handle/10238/5868
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dc.contributor.authorMcGregor, HV-
dc.contributor.authorFischer, MJ-
dc.contributor.authorGagan, MK-
dc.contributor.authorFink, D-
dc.contributor.authorPhipps, SJ-
dc.contributor.authorWong, HKY-
dc.contributor.authorWoodroffe, CD-
dc.date.accessioned2014-09-17T05:30:01Z-
dc.date.available2014-09-17T05:30:01Z-
dc.date.issued2013-09-05-
dc.identifier.citationMcGregor, H.V., Fischer, M.J., Gagan, M.K., Fink, D., Phipps, S.J., Wong, H., & Woodroffe, C.D. (2013). A weak El Niño/Southern Oscillation with delayed seasonal growth around 4,300 years ago. Nature Geoscience, 6(11), 949-953. doi:10.1038/ngeo1936en_AU
dc.identifier.govdoc5226-
dc.identifier.issn1752-0894-
dc.identifier.urihttp://dx.doi.org/doi:10.1038/ngeo1936en_AU
dc.identifier.urihttp://apo.ansto.gov.au/dspace/handle/10238/5868-
dc.description.abstractPalaeoclimate records indicate lower El Niño/Southern Oscillation (ENSO) variance during the middle Holocene compared with today, but the mechanisms leading to this muted variability are not clear. A 175-year oxygen isotope record from a Porites coral microatoll in the NINO3.4 region records persistently reduced ENSO variance about 4,300 years ago, and season-specific analyses of the record suggest that insolation played an important role in this change.© 2013, Nature Publishing Group.en_AU
dc.language.isoenen_AU
dc.publisherNature Publishing Groupen_AU
dc.subjectSouthern Oscillationen_AU
dc.subjectSeasonal variationsen_AU
dc.subjectGrowthen_AU
dc.subjectClimatesen_AU
dc.subjectVariationsen_AU
dc.subjectIsotopesen_AU
dc.titleA weak El Niño/Southern Oscillation with delayed seasonal growth around 4,300 years agoen_AU
dc.typeJournal Articleen_AU
dc.date.statistics2013-09-17-
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