TY - JOUR
T1 - Revisiting the age of the Fish Canyon sanidine dating standard
AU - Kuiper, Klaudia F.
AU - Toorenburgh, Zoë
AU - Wotzlaw, Jörn Frederik
AU - Zeeden, Christian
AU - Sierro, Francisco J.
AU - Davies, Joshua H.F.L.
AU - Sahy, Diana
AU - Condon, Daniel J.
AU - Hilgen, Frederik J.
N1 - Publisher Copyright:
© 2025 The Authors
PY - 2026/1/15
Y1 - 2026/1/15
N2 - In 2008, Kuiper and others published an astronomically calibrated age of 28.201 ± 0.046 Ma for the Fish Canyon sanidine (FCs), the most widely used standard in Ar/Ar dating. This age was incorporated in GTS2012 and GTS2020, but has been challenged by later studies that used various approaches, leading again to a ∼ 1.5 % age scattering. This uncertainty hampers the construction of a uniform and coherent time scale that is key to modern high-resolution, multi-disciplinary studies in Earth history. To solve this ongoing uncertainty, we present 1) a visual and statistical re-examination of the astronomical tuning on which the FCs age of 28.201 Ma is based and 2) new single crystal U/Pb ID-TIMS zircon ages of the astronomically calibrated Faneromeni A1 ash bed and the Fish Canyon Tuff (FCT). Our results corroborate the initial tuning and invalidate astronomical and U/Pb based FCs age calibrations, which are much younger or older. The preferred astronomical calibration seems to converge to a slightly younger age of 28.171–28.176 Ma. This is in good agreement with our new Bayesian zircon eruption age of 28.171 + 0.039/− 0.044 Ma for the FCT and the recently published Bayesian calibration of the 40 K decay scheme with a coupled FCs age of 28.183 ± 0.070 Ma. Importantly, the astronomical and U/Pb-based calibrations now yield similar ages, implying mutual agreement between the three main dating methods to construct our time scale. However, by contrast, the Cretaceous/Paleogene (K/Pg) boundary, which represents a critical triple point for the intercalibration, now produces divergent ages. In summary, much progress has been made in solving the critical issue of the age of the FCs dating standard. For the moment, we either recommend the continued use of the astronomically calibrated age of 28.201 ± 0.046 Ma or, preferentially, a slightly younger age of 28.171–28.176 Ma. We further endorse investigation in a community-based effort where new data and improved methodologies may lead to further insight into fundamental properties and potentially a definitive age not only for the FCs dating standard, but importantly also for the K/Pg boundary.
AB - In 2008, Kuiper and others published an astronomically calibrated age of 28.201 ± 0.046 Ma for the Fish Canyon sanidine (FCs), the most widely used standard in Ar/Ar dating. This age was incorporated in GTS2012 and GTS2020, but has been challenged by later studies that used various approaches, leading again to a ∼ 1.5 % age scattering. This uncertainty hampers the construction of a uniform and coherent time scale that is key to modern high-resolution, multi-disciplinary studies in Earth history. To solve this ongoing uncertainty, we present 1) a visual and statistical re-examination of the astronomical tuning on which the FCs age of 28.201 Ma is based and 2) new single crystal U/Pb ID-TIMS zircon ages of the astronomically calibrated Faneromeni A1 ash bed and the Fish Canyon Tuff (FCT). Our results corroborate the initial tuning and invalidate astronomical and U/Pb based FCs age calibrations, which are much younger or older. The preferred astronomical calibration seems to converge to a slightly younger age of 28.171–28.176 Ma. This is in good agreement with our new Bayesian zircon eruption age of 28.171 + 0.039/− 0.044 Ma for the FCT and the recently published Bayesian calibration of the 40 K decay scheme with a coupled FCs age of 28.183 ± 0.070 Ma. Importantly, the astronomical and U/Pb-based calibrations now yield similar ages, implying mutual agreement between the three main dating methods to construct our time scale. However, by contrast, the Cretaceous/Paleogene (K/Pg) boundary, which represents a critical triple point for the intercalibration, now produces divergent ages. In summary, much progress has been made in solving the critical issue of the age of the FCs dating standard. For the moment, we either recommend the continued use of the astronomically calibrated age of 28.201 ± 0.046 Ma or, preferentially, a slightly younger age of 28.171–28.176 Ma. We further endorse investigation in a community-based effort where new data and improved methodologies may lead to further insight into fundamental properties and potentially a definitive age not only for the FCs dating standard, but importantly also for the K/Pg boundary.
KW - Ar/Ar dating
KW - Astronomical dating
KW - Fish Canyon sanidine
KW - Fish Canyon Tuff
KW - Geological time scale
KW - U/Pb dating
UR - https://www.scopus.com/pages/publications/105021625819
UR - https://www.scopus.com/inward/citedby.url?scp=105021625819&partnerID=8YFLogxK
U2 - 10.1016/j.palaeo.2025.113421
DO - 10.1016/j.palaeo.2025.113421
M3 - Article
AN - SCOPUS:105021625819
SN - 0031-0182
VL - 682
SP - 1
EP - 14
JO - Palaeogeography, Palaeoclimatology, Palaeoecology
JF - Palaeogeography, Palaeoclimatology, Palaeoecology
M1 - 113421
ER -