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dc.contributor.authorAlloway, Brent V.
dc.contributor.authorLowe, David J.
dc.contributor.authorBarrell, David J.A.
dc.contributor.authorNewnham, Rewi M.
dc.contributor.authorAlmond, Peter C.
dc.contributor.authorAugustinus, Paul Christian
dc.contributor.authorBertler, Nancy A.N.
dc.contributor.authorCarter, Lionel
dc.contributor.authorLitchfield, Nicola J.
dc.contributor.authorMcGlone, Matt S.
dc.contributor.authorShulmeister, Jamie
dc.contributor.authorVandergoes, Marcus J.
dc.contributor.authorWilliams, Paul W.
dc.contributor.authorNZ-INTIMATE members
dc.date.accessioned2008-08-07T00:09:32Z
dc.date.available2008-08-07T00:09:32Z
dc.date.issued2007-01
dc.identifier.citationAlloway, B.V., Lowe, D.J., Barrell, D.J.A., Newnham, R.M.., Almond, P.C., Augustinus, P.C., Bertler, N.A., Carter, L., Litchfield, N.J., McGlone, M.S., Shulmeister, J., Vandergoes, M.J., Williams, P.W. & NZ-INTIMATE members. (2007). Towards a climate event stratigraphy for New Zealand over the past 30,000 years (NZ-INTIMATE project). Journal of Quaternary Science 22(1), 9-35.en_US
dc.identifier.issn1099-1417
dc.identifier.urihttps://hdl.handle.net/10289/924
dc.description.abstractIt is widely recognised that the acquisition of high-resolution palaeoclimate records from southern mid-latitude sites is essential for establishing a coherent picture of inter-hemispheric climate change and for better understanding of the role of Antarctic climate dynamics in the global climate system. New Zealand is considered to be a sensitive monitor of climate change because it is one of a few sizeable landmasses in the Southern Hemisphere westerly circulation zone, a critical transition zone between subtropical and Antarctic influences. New Zealand has mountainous axial ranges that amplify the climate signals and, consequently, the environmental gradients are highly sensitive to subtle changes in atmospheric and oceanic conditions. Since 1995, INTIMATE has, through a series of international workshops, sought ways to improve procedures for establishing the precise ages of climate events, and to correlate them with high precision, for the last 30 000 calendar years. The NZ-INTIMATE project commenced in late 2003, and has involved virtually the entire New Zealand palaeoclimate community. Its aim is to develop an event stratigraphy for the New Zealand region over the past 30 000 years, and to reconcile these events against the established climatostratigraphy of the last glacial cycle which has largely been developed from Northern Hemisphere records (e.g. Last Glacial Maximum (LGM), Termination I, Younger Dryas). An initial outcome of NZ-INTIMATE has been the identification of a series of well-dated, high-resolution onshore and offshore proxy records from a variety of latitudes and elevations on a common calendar timescale from 30 000 cal. yr BP to the present day. High-resolution records for the last glacial coldest period (LGCP) (including the LGM sensu stricto) and last glacial-interglacial transition (LGIT) from Auckland maars, Kaipo and Otamangakau wetlands on eastern and central North Island, marine core MD97-2121 east of southern North Island, speleothems on northwest South Island, Okarito wetland on southwestern South Island, are presented. Discontinuous (fragmentary) records comprising compilations of glacial sequences, fluvial sequences, loess accumulation, and aeolian quartz accumulation in an andesitic terrain are described. Comparisons with ice-core records from Antarctica (EPICA Dome C) and Greenland (GISP2) are discussed. A major advantage immediately evident from these records apart from the speleothem record, is that they are linked precisely by one or more tephra layers. Based on these New Zealand terrestrial and marine records, a reasonably coherent, regionally applicable, sequence of climatically linked stratigraphic events over the past 30 000 cal. yr is emerging. Three major climate events are recognised: (1) LGCP beginning at ca. 28 000 cal. yr BP, ending at Termination I, ca. 18 000 cal. yr BP, and including a warmer and more variable phase between ca. 27 000 and 21 000 cal. yr BP, (2) LGIT between ca. 18 000 and 11 600 cal. yr BP, including a Lateglacial warm period from ca. 14 800 to 13 500 cal. yr BP and a Lateglacial climate reversal between ca. 13 500 and 11 600 cal. yr BP, and (3) Holocene interglacial conditions, with two phases of greatest warmth between ca. 11 600 and 10 800 cal. yr BP and from ca. 6 800 to 6 500 cal. yr BP. Some key boundaries coincide with volcanic tephras.en_US
dc.language.isoen
dc.sourceQuaternary International, v167-168 (Supplement)en_NZ
dc.subjectLast glacial coldest perioden_US
dc.subjectLast Glacial Maximumen_US
dc.subjectAntarctic Cold Reversalen_US
dc.subjectTermination Ien_US
dc.subjectpalaeoclimateen_US
dc.subjectvegetationen_US
dc.subjectdatingen_US
dc.subjecttephraen_US
dc.subjecttephrochronologyen_US
dc.subjectmarine coreen_US
dc.subjectforaminiferaen_US
dc.subjectpollenen_US
dc.subjectspeleothemsen_US
dc.subjectglacial sequencesen_US
dc.subjectriver terracesen_US
dc.subjectloessen_US
dc.subjectaeolian quartzen_US
dc.subjectNew Zealanden_US
dc.titleTowards a climate event stratigraphy for New Zealand over the past 30,000 years (NZ-INTIMATE project)en_US
dc.typeJournal Articleen_US
dc.identifier.doi10.1002/jqs.1079en_US
pubs.begin-page9en_NZ
pubs.elements-id17265
pubs.end-page35en_NZ
pubs.finish-date2007-08-03en_NZ
pubs.start-date2007-07-28en_NZ


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