Jack N. Carter , Caroline E.J. Hasler , Anthony J. Fuentes , Andrew J. Tholt , Leah E. Morgan , Paul R. Renne
{"title":"Bayesian calibration of the 40K decay scheme with implications for 40K-based geochronology","authors":"Jack N. Carter , Caroline E.J. Hasler , Anthony J. Fuentes , Andrew J. Tholt , Leah E. Morgan , Paul R. Renne","doi":"10.1016/j.gca.2025.03.024","DOIUrl":null,"url":null,"abstract":"<div><div>The K/Ar and <sup>40</sup>Ar/<sup>39</sup>Ar geochronometers are based on the naturally occurring radionuclide <sup>40</sup>K. Their precision and accuracy are limited by uncertainties on the <sup>40</sup>K decay constants and, in the case of the <sup>40</sup>Ar/<sup>39</sup>Ar geochronometer, the isotopic composition of neutron fluence monitors. To address these limitations, we introduce a Bayesian calibration of the <sup>40</sup>K decay scheme. We formulate robust priors for all model parameters including partial <sup>40</sup>K decay constants, <sup>238</sup>U and <sup>235</sup>U decay constants, and age offset parameters to account for phenomena that can perturb apparent U-Pb and <sup>40</sup>Ar/<sup>39</sup>Ar ages. We then harness a set of complementary <sup>40</sup>Ar/<sup>39</sup>Ar, <sup>238</sup>U/<sup>206</sup>Pb, and <sup>235</sup>U/<sup>207</sup>Pb data from well- characterized geological samples with ages from 1.919 ka to 2000 Ma to derive Bayesian estimates of the <sup>40</sup>K decay constants. Posterior values for the partial <sup>40</sup>K decay constants are <span><math><mrow><msub><mi>λ</mi><msup><mrow><mi>β</mi></mrow><mo>-</mo></msup></msub></mrow></math></span>= (4.9252 <span><math><mrow><mo>±</mo></mrow></math></span> 0.0054) <span><math><mrow><mo>×</mo></mrow></math></span> 10<sup>−10</sup> yr<sup>−1</sup>, <span><math><mrow><msub><mi>λ</mi><msup><mrow><mi>β</mi></mrow><mo>+</mo></msup></msub></mrow></math></span> = (5.6658 <span><math><mrow><mo>±</mo></mrow></math></span> 0.1543) <span><math><mrow><mo>×</mo></mrow></math></span> 10<sup>−15</sup> yr<sup>−1</sup>, <span><math><mrow><msub><mi>λ</mi><msup><mrow><mi>EC</mi></mrow><mrow><mo>∗</mo></mrow></msup></msub></mrow></math></span> = (5.7404 <span><math><mrow><mo>±</mo></mrow></math></span> 0.0053) <span><math><mrow><mo>×</mo></mrow></math></span> 10<sup>−11</sup> yr<sup>−1</sup>, and <span><math><mrow><msub><mi>λ</mi><msub><mrow><mi>EC</mi></mrow><mn>0</mn></msub></msub></mrow></math></span>= (4.9060 <span><math><mrow><mo>±</mo></mrow></math></span> 0.2942) <span><math><mrow><mo>×</mo></mrow></math></span> 10<sup>−13</sup> yr<sup>−1</sup> (uncertainties reported at the 68 % (1<span><math><mrow><mi>σ</mi></mrow></math></span>) credible interval). These combine to a total <sup>40</sup>K decay constant <span><math><mrow><msub><mi>λ</mi><mrow><mi>tot</mi></mrow></msub></mrow></math></span>= (5.5042 <span><math><mrow><mo>±</mo></mrow></math></span> 0.0054) <span><math><mrow><mo>×</mo></mrow></math></span> 10<sup>−10</sup> yr<sup>−1</sup>. Model estimates of the <sup>238</sup>U and <sup>235</sup>U decay constants are statistically indistinguishable from those reported by <span><span>Jaffey et al. (1971)</span></span>. Posterior values of the <sup>40</sup>K decay constants and the <sup>40</sup>Ar*/<sup>40</sup>K isotopic composition of Fish Canyon sanidine (FCs) define a K/Ar FCs age of 28.183 <span><math><mrow><mo>±</mo></mrow></math></span> 0.017 Ma (1<span><math><mrow><mi>σ</mi></mrow></math></span>). Significantly, Bayesian calibrated <sup>40</sup>Ar/<sup>39</sup>Ar ages align with astronomically tuned ages throughout the Cenozoic and with <sup>238</sup>U/<sup>206</sup>Pb and <sup>235</sup>U/<sup>207</sup>Pb ages in the Mesozoic, Paleozoic, and Proterozoic, as well as having comparable precision to the <sup>238</sup>U/<sup>206</sup>Pb method. Thus, Bayesian calibration of the <sup>40</sup>K decay scheme and the K/Ar age of FCs reconciles the <sup>40</sup>Ar/<sup>39</sup>Ar, U-Pb, and astronomical chronometers.</div></div>","PeriodicalId":327,"journal":{"name":"Geochimica et Cosmochimica Acta","volume":"397 ","pages":"Pages 149-163"},"PeriodicalIF":4.5000,"publicationDate":"2025-03-24","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Geochimica et Cosmochimica Acta","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0016703725001620","RegionNum":1,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
引用次数: 0
Abstract
The K/Ar and 40Ar/39Ar geochronometers are based on the naturally occurring radionuclide 40K. Their precision and accuracy are limited by uncertainties on the 40K decay constants and, in the case of the 40Ar/39Ar geochronometer, the isotopic composition of neutron fluence monitors. To address these limitations, we introduce a Bayesian calibration of the 40K decay scheme. We formulate robust priors for all model parameters including partial 40K decay constants, 238U and 235U decay constants, and age offset parameters to account for phenomena that can perturb apparent U-Pb and 40Ar/39Ar ages. We then harness a set of complementary 40Ar/39Ar, 238U/206Pb, and 235U/207Pb data from well- characterized geological samples with ages from 1.919 ka to 2000 Ma to derive Bayesian estimates of the 40K decay constants. Posterior values for the partial 40K decay constants are = (4.9252 0.0054) 10−10 yr−1, = (5.6658 0.1543) 10−15 yr−1, = (5.7404 0.0053) 10−11 yr−1, and = (4.9060 0.2942) 10−13 yr−1 (uncertainties reported at the 68 % (1) credible interval). These combine to a total 40K decay constant = (5.5042 0.0054) 10−10 yr−1. Model estimates of the 238U and 235U decay constants are statistically indistinguishable from those reported by Jaffey et al. (1971). Posterior values of the 40K decay constants and the 40Ar*/40K isotopic composition of Fish Canyon sanidine (FCs) define a K/Ar FCs age of 28.183 0.017 Ma (1). Significantly, Bayesian calibrated 40Ar/39Ar ages align with astronomically tuned ages throughout the Cenozoic and with 238U/206Pb and 235U/207Pb ages in the Mesozoic, Paleozoic, and Proterozoic, as well as having comparable precision to the 238U/206Pb method. Thus, Bayesian calibration of the 40K decay scheme and the K/Ar age of FCs reconciles the 40Ar/39Ar, U-Pb, and astronomical chronometers.
期刊介绍:
Geochimica et Cosmochimica Acta publishes research papers in a wide range of subjects in terrestrial geochemistry, meteoritics, and planetary geochemistry. The scope of the journal includes:
1). Physical chemistry of gases, aqueous solutions, glasses, and crystalline solids
2). Igneous and metamorphic petrology
3). Chemical processes in the atmosphere, hydrosphere, biosphere, and lithosphere of the Earth
4). Organic geochemistry
5). Isotope geochemistry
6). Meteoritics and meteorite impacts
7). Lunar science; and
8). Planetary geochemistry.