Revised onset age of magnetochron M0r: Chronostratigraphic and geologic implications

التفاصيل البيبلوغرافية
العنوان: Revised onset age of magnetochron M0r: Chronostratigraphic and geologic implications
المؤلفون: Youjuan Li, Huafeng Qin, Brian R. Jicha, Magdalena H. Huyskens, Corey J. Wall, Robin B. Trayler, Qing-Zhu Yin, Mark Schmitz, Yongxin Pan, Chenglong Deng, Brad S. Singer, Huaiyu He, Rixiang Zhu
المصدر: Geology. 51:565-570
بيانات النشر: Geological Society of America, 2023.
سنة النشر: 2023
مصطلحات موضوعية: Geology
الوصف: The timing of the onset of magnetochron M0r and its duration are disputed, reflecting both a limited set of radioisotopic dates and uncertain magnetostratigraphic correlations. We present a chronostratigraphic framework for a reversed polarity interval based on two chronometers (40Ar/39Ar, U-Pb) and newly published paleomagnetic data from the Qingshan Group, Jiaolai Basin, China. Bayesian modeling of U-Pb zircon and 40Ar/39Ar sanidine dates suggests a minimum duration of 540 ± 37 k.y. (95% credible interval) for the reversed polarity interval. These findings are compatible with an astrochronologic age model for M-sequence seafloor magnetic anomalies, indicating that the reversely magnetized sediments correspond to magnetochron M0r rather than the shorter chron “M-1r.” Integration of U-Pb and 40Ar/39Ar ages constrains the onset of M0r to 120.29 ± 0.09 Ma, which is ~1 m.y. younger than that inferred in the current geologic time scale (GTS 2020). This finding also implies that the Cretaceous normal superchron (CNS) began at 119.70 ± 0.12 Ma and that the average seafloor spreading rate during the CNS was ~3.5% higher than that inferred from GTS 2020. It also suggests that oceanic anoxic event 1a began at 119.40 ± 0.12 Ma, thereby providing an updated chronologic basis for exploring the primary trigger of this carbon cycle perturbation.
تدمد: 1943-2682
0091-7613
DOI: 10.1130/g50873.1
URL الوصول: https://explore.openaire.eu/search/publication?articleId=doi_________::41b04ff2884214a36da67fe99494fabc
https://doi.org/10.1130/g50873.1
رقم الانضمام: edsair.doi...........41b04ff2884214a36da67fe99494fabc
قاعدة البيانات: OpenAIRE
الوصف
تدمد:19432682
00917613
DOI:10.1130/g50873.1