- Sponsor Seminars
These are scheduled events to help delegates test out the tools and platform we will be using for the Q&A and other events at the conference.
Our workshop program provides training and teaching in topics across geochemistry and related fields. We are currently liaising with the workshop organisers to ascertain if any workshops can become virtual. Any updates will be added to this page.
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Evidence of Early and Late Diagenesis of Sediments from Past Habitable Environments in Gale Crater, Mars: A Mastcam Multispectral Perpsective
Rudolph A, Haber J, Horgan B, Bennett K, Fox V, Seeger C, Rice M, Johnson J, Bell Iii J, Jacob S & Rampe E
Rudolph A, Haber J, Horgan B, Bennett K, Fox V, Seeger C, Rice M, Johnson J, Bell Iii J, Jacob S & Rampe E (2020) Goldschmidt Abstracts, 2020 2239
The author has not provided any additional details.
01b: Room 1, View in program
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.
Several of the potential analogs seemed very divergent. How do you reconcile a buried soil/paleosol within a fluviolacustrine system?
Thanks for your question! A paleosol would indicate a period of low lake levels and exposure of sediments, in terrestrial lacustrine sequences you see paleosols when the shoreline moves inward. So the clay-rich sediments in Glen Torridon may have formed through the weathering of lacustrine sediments as the shoreline of the fluviolacustrine system fluctuated and because of that the clay-rich region we see today could represent a clay-rich soil horizon/paleosol.
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