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A M Lorrey

Biographic Data

ID4130306
NAMEA M Lorrey
GIVEN NAMESA M
FAMILY NAMELorrey
SIGNATURELORREY A M
AFFILIATIONSNational Institute of Water and Atmospheric Research
ORCID0000-0002-3923-3181
VERIFIEDYes
TOTAL WORKS2
TOTAL CITATIONS5
AUTHOR COUNT2
EDITOR COUNT0
FIRST PUBLICATION YEAR2016
LATEST PUBLICATION YEAR2020
H-INDEX1
  • Late Quaternary Climate Variability and Change from Aotearoa New Zealand Speleothems: Progress in Age Modelling, Oxygen Isotope Master Record Construction and Proxy-Model Comparisons

    Open Access•A M Lorrey, Peter W Williams et al.•ARTICLE•Quaternary•2020

    We re-evaluated speleothem isotope series from Aotearoa New Zealand that were recently contributed to the Speleothem Isotopes Synthesis and AnaLysis (SISAL) database. COnstructing Proxy Records from Age Models (COPRA) software was used to produce Bayesian age models for those speleothems. The new age modelling helped us examine Late Quaternary temporal coverage for the national speleothem network, and also supported our exploration of three diffe…

  • Timing, magnitude and effects of late Holocene sea level drawdown on island habitability, Aitutaki, Cook Islands

    Open Access•M S Allen, Alex E Morrison et al.•ARTICLE•Archaeology in Oceania/Archæology…•2016•Cited by: 5•References: 32

    Geologist Bill Dickinson argued that prior to late Holocene sea level fall, in many Pacific island settings low‐lying islands were awash, shallow nearshore environments were restricted and human settlement was constrained or sometimes impossible. Stable coastlines and islets of modern configuration only developed after the “cross‐over date”, when declining high‐tide levels fell below mid‐Holocene low‐tide levels, a regionally variable process. We…

  • Timing, magnitude and effects of late Holocene sea level drawdown on island habitability, Aitutaki, Cook Islands

    Open Access•M S Allen, Alex E Morrison et al.•ARTICLE•Archaeology in Oceania/Archæology…•2016•Cited by: 5•References: 32

    Geologist Bill Dickinson argued that prior to late Holocene sea level fall, in many Pacific island settings low‐lying islands were awash, shallow nearshore environments were restricted and human settlement was constrained or sometimes impossible. Stable coastlines and islets of modern configuration only developed after the “cross‐over date”, when declining high‐tide levels fell below mid‐Holocene low‐tide levels, a regionally variable process. We…

  • Timing, magnitude and effects of late Holocene sea level drawdown on island habitability, Aitutaki, Cook Islands

    Open Access•M S Allen, Alex E Morrison et al.•ARTICLE•Archaeology in Oceania/Archæology…•2016•Cited by: 5•References: 32

    Geologist Bill Dickinson argued that prior to late Holocene sea level fall, in many Pacific island settings low‐lying islands were awash, shallow nearshore environments were restricted and human settlement was constrained or sometimes impossible. Stable coastlines and islets of modern configuration only developed after the “cross‐over date”, when declining high‐tide levels fell below mid‐Holocene low‐tide levels, a regionally variable process. We…

  • Late Quaternary Climate Variability and Change from Aotearoa New Zealand Speleothems: Progress in Age Modelling, Oxygen Isotope Master Record Construction and Proxy-Model Comparisons

    Open Access•A M Lorrey, Peter W Williams et al.•ARTICLE•Quaternary•2020

    We re-evaluated speleothem isotope series from Aotearoa New Zealand that were recently contributed to the Speleothem Isotopes Synthesis and AnaLysis (SISAL) database. COnstructing Proxy Records from Age Models (COPRA) software was used to produce Bayesian age models for those speleothems. The new age modelling helped us examine Late Quaternary temporal coverage for the national speleothem network, and also supported our exploration of three diffe…

Archaeology (2 works) · Geography (2 works) · Geology (2 works) · Geology and Paleoclimatology Research (2 works) · Holocene (2 works) · Oceanography (2 works) · Physical geography (2 works) · Cave (1 works) · Climate change (1 works) · Climate model (1 works)

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