Developing tree-ring chronologies from New Zealand matai (Prumnopitys taxifolia) and miro (Prumnopitys ferruginea) for archaeological dating: Progress and problems
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Boswijk, Gretel
[1
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Loader, Neil J.
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Swansea Univ, Dept Geog, Swansea, W Glam, WalesUniv Auckland, Sch Environm, Auckland, New Zealand
Loader, Neil J.
[2
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Young, Giles H. F.
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Swansea Univ, Dept Geog, Swansea, W Glam, Wales
Nat Resources Finland LUKE, Helsinki, FinlandUniv Auckland, Sch Environm, Auckland, New Zealand
Young, Giles H. F.
[2
,3
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Hogg, Alan
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Univ Waikato, Radiocarbon Dating Lab, Hamilton, New ZealandUniv Auckland, Sch Environm, Auckland, New Zealand
Hogg, Alan
[4
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[1] Univ Auckland, Sch Environm, Auckland, New Zealand
[2] Swansea Univ, Dept Geog, Swansea, W Glam, Wales
[3] Nat Resources Finland LUKE, Helsinki, Finland
[4] Univ Waikato, Radiocarbon Dating Lab, Hamilton, New Zealand
This paper describes attempts to develop tree-ring chronologies from New Zealand matai (Prumnopitys taxifolia) and miro (Prumnopitys ferruginea). These tree species have been recovered from Ma over bar ori archaeological contexts, including as objects such as canoes and palisade posts. Dendrochronology offers the potential to establish accurate and precise calendar dates for wooden objects but relies on cultural use of species that are also suitable for tree-ring analysis, and the availability of calendar-dated reference chronologies for crossdating wood of unknown age. We used archived cross-section and core samples from seven sites in central North Island, and nineteen core samples collected in 2019 from matai and miro trees at Pureora Forest Park for our analysis. Some of these samples came from long lived trees, with ring counts indicating ages up to 800 years old. We found that both matai and miro exhibit considerable variability in ring clarity and ring width. They also have ring anomalies affecting the reliability of ring-width series. Miro was very challenging, and no tree sequences were built for this species. Tree-ring sequences were built for several matai samples but no secure inter-tree matches were identified. Further analysis of matai samples is required to establish reliable tree ring patterns for inter-tree and intersite crossmatching.
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Swansea Univ Prifysgol Abertawe, Dept Geog, Swansea, WalesSwansea Univ Prifysgol Abertawe, Dept Geog, Swansea, Wales
Loader, Neil J.
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Boswijk, Gretel
Young, Giles H. F.
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Swansea Univ Prifysgol Abertawe, Dept Geog, Swansea, Wales
Nat Resources Finland LUKE, Helsinki, FinlandSwansea Univ Prifysgol Abertawe, Dept Geog, Swansea, Wales
Young, Giles H. F.
Hogg, Alan G.
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Univ Waikato Te Whare Wananga O Waikato, Sch Sci, Hamilton, New ZealandSwansea Univ Prifysgol Abertawe, Dept Geog, Swansea, Wales
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Univ New S Wales, Sch Biol Earth & Environm Sci, Climate Change Res Ctr, Sydney, NSW 2052, AustraliaUniv New S Wales, Sch Biol Earth & Environm Sci, Climate Change Res Ctr, Sydney, NSW 2052, Australia
Palmer, J. G.
Turney, C. S. M.
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Univ New S Wales, Sch Biol Earth & Environm Sci, Climate Change Res Ctr, Sydney, NSW 2052, AustraliaUniv New S Wales, Sch Biol Earth & Environm Sci, Climate Change Res Ctr, Sydney, NSW 2052, Australia
Turney, C. S. M.
Hogg, A. G.
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Univ Waikato, Waikato Radiocarbon Dating Lab, Hamilton, New ZealandUniv New S Wales, Sch Biol Earth & Environm Sci, Climate Change Res Ctr, Sydney, NSW 2052, Australia
Hogg, A. G.
Lorrey, A. M.
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Natl Inst Water & Atmospher Res, Auckland 1010, New ZealandUniv New S Wales, Sch Biol Earth & Environm Sci, Climate Change Res Ctr, Sydney, NSW 2052, Australia
Lorrey, A. M.
Jones, R. J.
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Univ Exeter, Dept Geog, Exeter EX4 4RJ, Devon, EnglandUniv New S Wales, Sch Biol Earth & Environm Sci, Climate Change Res Ctr, Sydney, NSW 2052, Australia