Abstract Details
(2020) The Fate of Organic Fermentation Products in Carbonate Sediments
Hutchinson T, Leung PM, Callahan D, Kessler A, Wong WW, Greening C & Cook P
https://doi.org/10.46427/gold2020.1120
The author has not provided any additional details.
10c: Room 2, Saturday 27th June 07:12 - 07:15
Tess Hutchinson
View all 2 abstracts at Goldschmidt2020
View abstracts at 2 conferences in series
Pok Man Leung
Damien Callahan
Adam J. Kessler View all 4 abstracts at Goldschmidt2020
Wei Wen Wong View all 2 abstracts at Goldschmidt2020 View abstracts at 4 conferences in series
Chris Greening View all 5 abstracts at Goldschmidt2020 View abstracts at 2 conferences in series
Perran L. M. Cook View all 3 abstracts at Goldschmidt2020
Pok Man Leung
Damien Callahan
Adam J. Kessler View all 4 abstracts at Goldschmidt2020
Wei Wen Wong View all 2 abstracts at Goldschmidt2020 View abstracts at 4 conferences in series
Chris Greening View all 5 abstracts at Goldschmidt2020 View abstracts at 2 conferences in series
Perran L. M. Cook View all 3 abstracts at Goldschmidt2020
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 David J. Burdige on Thursday 25th June 18:19
Is the build-up of H2 that you see in short term incubations or do you see it in sediment profiles? The reason I ask is that the hydrogen eventually has to go somewhere to be oxidized (even of it escapes the sediments). The same would have to be true for these organic compounds you suggest are produced and stored by the bacteria, unless of course they simply accumulate in the sediments. Good talk and I'll go look for your paper as many of the answers may actually be there. David Burdige
Is the build-up of H2 that you see in short term incubations or do you see it in sediment profiles? The reason I ask is that the hydrogen eventually has to go somewhere to be oxidized (even of it escapes the sediments). The same would have to be true for these organic compounds you suggest are produced and stored by the bacteria, unless of course they simply accumulate in the sediments. Good talk and I'll go look for your paper as many of the answers may actually be there. David Burdige
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