Abstract Details
(2020) Stable Sr Isotopes of the Middle-Late Permian Carbonate: Its Implication for Driving Ocean Sr Budget Change
Kani T, Isozaki Y, Misawa K, Ishikawa A & Yoneda S
https://doi.org/10.46427/gold2020.1247
The author has not provided any additional details.
14j: Plenary Hall, Tuesday 23rd June 08:39 - 08:42
Tomomi Kani
View abstracts at 8 conferences in series
Yukio Isozaki View abstracts at 8 conferences in series
Keiji Misawa View abstracts at 5 conferences in series
Akira Ishikawa View all 6 abstracts at Goldschmidt2020 View abstracts at 17 conferences in series
Shigekazu Yoneda View all 4 abstracts at Goldschmidt2020 View abstracts at 15 conferences in series
Yukio Isozaki View abstracts at 8 conferences in series
Keiji Misawa View abstracts at 5 conferences in series
Akira Ishikawa View all 6 abstracts at Goldschmidt2020 View abstracts at 17 conferences in series
Shigekazu Yoneda View all 4 abstracts at Goldschmidt2020 View abstracts at 15 conferences in series
Listed below are questions that have been submitted by the community that the author will try and cover in their presentation. To submit a question, ensure you are signed in to the website. Authors or session conveners approve questions before they are displayed here.
Submitted by Mingsong Li on Tuesday 23rd June 06:17
Hi Tomomi, there is a temporal link between the Emeishan large igneous province (SW China) and the end-Guadalupian mass extinction. What's the role of the LIP magmatism in your model? Thanks.
Hi, Mingsong Li , Thank you for the question. The temporally minor decline in Wuchiapingian might relate to a LIP activity. Some minor fluctuations in the Phanerozoic 87Sr/86Sr curve may reflect pulses of less radiogenic Sr input related with emplacements of LIPs.
Hi Tomomi, there is a temporal link between the Emeishan large igneous province (SW China) and the end-Guadalupian mass extinction. What's the role of the LIP magmatism in your model? Thanks.
Hi, Mingsong Li , Thank you for the question. The temporally minor decline in Wuchiapingian might relate to a LIP activity. Some minor fluctuations in the Phanerozoic 87Sr/86Sr curve may reflect pulses of less radiogenic Sr input related with emplacements of LIPs.
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