Abstract Details
(2020) Deciphering the Early Triassic Paleocean Using Stable Oxygen Isotopes in Conodont Bioapatite
Luz Z, Leu M, Edward O, Baumgartner LP, Bucher H & Vennemann T
https://doi.org/10.46427/gold2020.1665
The author has not provided any additional details.
14b: Plenary Hall, Monday 22nd June 22:48 - 22:51
Zoneibe Augusto Silva Luz
View all 3 abstracts at Goldschmidt2020
Marc Leu
Oluwaseun Edward View all 3 abstracts at Goldschmidt2020
Lukas P. Baumgartner View all 4 abstracts at Goldschmidt2020 View abstracts at 4 conferences in series
Hugo Bucher View all 3 abstracts at Goldschmidt2020 View abstracts at 7 conferences in series
Torsten Vennemann View all 5 abstracts at Goldschmidt2020 View abstracts at 6 conferences in series
Marc Leu
Oluwaseun Edward View all 3 abstracts at Goldschmidt2020
Lukas P. Baumgartner View all 4 abstracts at Goldschmidt2020 View abstracts at 4 conferences in series
Hugo Bucher View all 3 abstracts at Goldschmidt2020 View abstracts at 7 conferences in series
Torsten Vennemann View all 5 abstracts at Goldschmidt2020 View abstracts at 6 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 Georgina Lukoczki on Monday 22nd June 19:36
We have seen that rock-buffered diagenesis may result in apparent, rather than actual d18Ofluid values when calculated from clumped isotope data. My understanding is that you used d18Owater from clumped isotope measurements on brachiopods from the same layers and plugged these values into the phosphate-water fractionation equation. How did you ensure that the d18Owater values truly reflect the real seawater composition?
We have seen that rock-buffered diagenesis may result in apparent, rather than actual d18Ofluid values when calculated from clumped isotope data. My understanding is that you used d18Owater from clumped isotope measurements on brachiopods from the same layers and plugged these values into the phosphate-water fractionation equation. How did you ensure that the d18Owater values truly reflect the real seawater composition?
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