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dc.contributor.authorGehrels, Maria J.
dc.contributor.authorLowe, David J.
dc.contributor.authorHazell, Zoë J.
dc.contributor.authorNewnham, Rewi M.
dc.date.accessioned2008-08-07T02:50:21Z
dc.date.available2008-08-07T02:50:21Z
dc.date.issued2006-02
dc.identifier.citationGehrels, M.J., Lowe, D.J., Hazell, Z.J. & Newnham, R.M. (2006). A continuous 5300-yr Holocene cryptotephrostratigraphic record from northern New Zealand and implications for tephrochronology and volcanic-hazard assessment. The Holocene 16(2), 173-187.en_US
dc.identifier.issn1477-0911
dc.identifier.urihttps://hdl.handle.net/10289/927
dc.description.abstractA continuous 5280 calendar (cal.) yr long cryptotephrostratigraphic record of a peat core from northern New Zealand demonstrates that cryptotephra studies can enhance conventional tephra records by extending the known distribution of ash fall and enabling re-assessment of volcanic hazards. A systematic sampling strategy was used to locate peaks in glass-shard concentrations and to determine loci of individual geochemical populations, and a palynological method involving spiking samples with Lycopodium spores was adapted to facilitate accurate counting of glass-shard concentrations. Using glass shard major element compositions, and a core chronology based on eight AMS 14C ages and two visible macroscopic tephra layers, Taupo Tephra (Unit Y) (1688-1748 cal. BP) and Tuhua Tephra (6800-7230 cal. BP) (2cr-age ranges), four cryptotephras were correlated with known eruptions: Whakaipo (Unit V) (2743-2782 cal. BP), Stent (Unit Q) (4240-4510 cal. BP), and Unit K (4970-5290 cal. BP), erupted from Taupo Volcanic Centre, and Whakatane Tephra (5470-5600 cal. BP) erupted from Okataina Volcanic Centre. Mixed glass populations were found in the core, most likely an artefact of post-depositional remobilization of shards vertically (both up and down) in the peat or on its surface by wind, or a result of closely spaced eruption events, or a combination of these. A secondary glass population identified within the macroscopic Taupo Tephra was tentatively attributed to either an earlier phase within that eruption or to mixing with a slightly older Taupo-derived eruptive or (less likely) a currently unknown Okataina-derived eruptive. These results indicate that, in the absence of continuous cryptotephrostratigraphic analysis, a peak in shard concentrations may not in itself be indicative of the ‘true’ stratigraphic (ie, isochronous) level of a tephra layer. For cryptotephra studies of peat cores, we recommend (1) using a detailed sampling strategy for the analysis of distal tephra-derived glass to detect and account for any mixed populations and possible vertical spread of glass shards through the peat, and (2) analysing more shards from larger samples to help ‘capture’ sparsely represented cryptic andesitic tephra deposits.en_US
dc.language.isoen
dc.publisherHodder Arnold Journalsen_NZ
dc.subjectcrytotephraen_US
dc.subjecttephraen_US
dc.subjecttephrochronologyen_US
dc.subjectglass countsen_US
dc.subjectvolcanic hazardsen_US
dc.subject14C datingen_US
dc.subjectisochronsen_US
dc.subjectpeat coresen_US
dc.subjectNorth Islanden_US
dc.subjectKopouatai bogen_US
dc.subjectHoloceneen_US
dc.subjectNew Zealanden_US
dc.titleA continuous 5300-yr Holocene cryptotephrostratigraphic record from northern New Zealand and implications for tephrochronology and volcanic-hazard assessment.en_US
dc.typeJournal Articleen_US
dc.identifier.doi10.1191/0959683606hl918rpen_US
dc.relation.isPartOfThe Holoceneen_NZ
pubs.begin-page173en_NZ
pubs.elements-id31636
pubs.end-page187en_NZ
pubs.issue2en_NZ
pubs.volume16en_NZ


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