TY - JOUR
T1 - Multi-method dating comparison for mid-pleistocene Rangitawa Tephra, New Zealand
AU - Pillans, Brad
AU - Kohn, Barry P.
AU - Berger, Glenn
AU - Froggatt, Paul
AU - Duller, Geoff
AU - Alloway, Brent
AU - Hesse, Paul
PY - 1996
Y1 - 1996
N2 - The Rangitawa Tephra, a widespread mid-Pleistocene marker in the New Zealand region, is dated by fission-track, thermoluminescence (TL), infrared stimulated luminescence (IRSL). K/Ar and single crystal laser fusion (SCLF)40Ar/39Ar methods, as well as by matching to the astronomical timescale via oxygen isotope stratigraphy in deep sea cores. Fifty one independent numerical age estimates for Rangitawa Tephra range from 173 to 456 ka. However, only 15 of these results are considered to be reliable; five zircon fission-track results, four isothermal plateau fission-track (ITPFT) age estimates on glass shards, four SCLF40Ar/39Ar results, and two astronomically calibrated age estimates from deep sea cores. The weighted mean of the nine reliable fission-track age determination is 345±12 ka, in excellent agreement with the weighted mean of 340+7 ka for the two reliable astronomically calibrated age estimates. The weighted mean of the four reliable 40Ar/39Ar results (302±18 ka) is significantly younger, and further Ar/Ar dating is recommended to investigate this difference. Since the TL and IRSL dating methods are experimental for sediments beyond 200 ka, we have excluded these from the group of reliable age results. TL and IRSL results on dunesand appear to e systematically younger than TL results on loess, and loess results depend upon analytical procedures.
AB - The Rangitawa Tephra, a widespread mid-Pleistocene marker in the New Zealand region, is dated by fission-track, thermoluminescence (TL), infrared stimulated luminescence (IRSL). K/Ar and single crystal laser fusion (SCLF)40Ar/39Ar methods, as well as by matching to the astronomical timescale via oxygen isotope stratigraphy in deep sea cores. Fifty one independent numerical age estimates for Rangitawa Tephra range from 173 to 456 ka. However, only 15 of these results are considered to be reliable; five zircon fission-track results, four isothermal plateau fission-track (ITPFT) age estimates on glass shards, four SCLF40Ar/39Ar results, and two astronomically calibrated age estimates from deep sea cores. The weighted mean of the nine reliable fission-track age determination is 345±12 ka, in excellent agreement with the weighted mean of 340+7 ka for the two reliable astronomically calibrated age estimates. The weighted mean of the four reliable 40Ar/39Ar results (302±18 ka) is significantly younger, and further Ar/Ar dating is recommended to investigate this difference. Since the TL and IRSL dating methods are experimental for sediments beyond 200 ka, we have excluded these from the group of reliable age results. TL and IRSL results on dunesand appear to e systematically younger than TL results on loess, and loess results depend upon analytical procedures.
UR - http://www.scopus.com/inward/record.url?scp=0030303158&partnerID=8YFLogxK
U2 - 10.1016/0277-3791(96)00035-2
DO - 10.1016/0277-3791(96)00035-2
M3 - Article
AN - SCOPUS:0030303158
VL - 15
SP - 641
EP - 653
JO - Quaternary Science Reviews
JF - Quaternary Science Reviews
SN - 0277-3791
IS - 7
ER -