Data for "Demystifying Diagenesis: The Future of Diagenetic Inquiry in the Geosciences"

Diagenesis encompasses all physical, chemical, mineralogical changes that a sediment, rock, molecule, or mineral undergoes following deposition. Because the time that geologic materials spend in the diagenetic realm is substantial relative to the time spent in the formational environment, there is potential for primary materials to be altered diagenetically. Despite its importance, diagenesis is a difficult and complicated topic to discuss. In this contribution, we demonstrate the use of a range of quantitative tools, from mixing equations to reactive transport models, in order to facilitate diagenesis discussions. We consider simple models of CaCO3 recrystallization and dolomitization, highlight key controls on diagenetic trajectories, present a compilation of partition coefficients for CaCO3 and clays, and discuss model illustrations of the diagenetic generation/modification, of carbon, calcium, and lithium isotopic records in the marine sedimentary section.

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Work Title Data for "Demystifying Diagenesis: The Future of Diagenetic Inquiry in the Geosciences"
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Open Access
Creators
  1. Matthew Fantle
  2. Max Lloyd
Keyword
  1. Ocean Drilling Program
  2. Carbon isotopes
  3. Calcium isotopes
  4. Magnesium isotopes
  5. Reactive transport model
  6. Mixing equations
  7. Carbonate authigenesis
  8. Clay authigenesis
  9. Partition coefficients
License In Copyright (Rights Reserved)
Work Type Part Of Book
Acknowledgments
  1. This research refers to analyses of samples and data provided by the Ocean Drilling Program (ODP) and International Ocean Drilling Program (IODP). M.S.F. thanks Ben Davis Barnes for informal discussions, during one of which he used the words ‘demystifying diagenesis’ that struck a chord. M.S.F. is also grateful to Ben Davis Barnes for coding up the first version of the depositional carbonate recrystallization code that is used in this chapter and for sharing some of the digital art used in Figs. 1 and 3. M.S.F. also profusely thanks Carl Steefel, Jenny Druhan, Sergi Molins Rafa, and Nicole Fernandez for all of their patience, as well as their invaluable help with CrunchTope. M.K.L. acknowledges innumerable helpful discussions with M. Ingalls. The authors thank Editor Matthew Kohn for the invitation to write this chapter; we also appreciate the reviews of Ed Tipper and John Higgins.
Publication Date 2024
Related URLs
Deposited June 26, 2023

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Version 1
published

  • Created
  • Updated
  • Updated Acknowledgments Show Changes
    Acknowledgments
    • M.S.F. thanks B. Davis Barnes for informal discussions, during one of which he used the words ‘demystifying diagenesis’ that struck a chord. M.S.F. is also grateful to B. Davis Barnes for coding up the first version of the carbonate recrystallization code that is used in this chapter and for sharing some of the digital art that is used to create Fig. 1b. M.K.L. acknowledges innumerable helpful discussions with M. Ingalls.
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    • Elsevier
    Related URLs
    • https://exchange.iseesystems.com/directory?_csrf=&query=fantle&name=on&description=on&keywords=on&sims=on&models=on&diagrams=on&bundles=on&limit=40&fromAuthor=
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    • https://rightsstatements.org/page/InC/1.0/
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    • https://exchange.iseesystems.com/directory?_csrf=&query=fantle&name=on&description=on&keywords=on&sims=on&models=on&diagrams=on&bundles=on&limit=40&fromAuthor=
    • https://exchange.iseesystems.com/public/matthewfantle/fantle-and-lloyd-2023-carbonate-recrystallization-model
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  • Updated Acknowledgments Show Changes
    Acknowledgments
    • M.S.F. thanks B. Davis Barnes for informal discussions, during one of which he used the words ‘demystifying diagenesis’ that struck a chord. M.S.F. is also grateful to B. Davis Barnes for coding up the first version of the carbonate recrystallization code that is used in this chapter and for sharing some of the digital art that is used to create Fig. 1b. M.K.L. acknowledges innumerable helpful discussions with M. Ingalls.
    • M.S.F. thanks B. Davis Barnes for informal discussions, during one of which he used the words ‘demystifying diagenesis’ that struck a chord. M.S.F. is also grateful to B. Davis Barnes for coding up the first version of the carbonate recrystallization code that is used in this chapter and for sharing some of the digital art that is used to create Fig. 1. M.K.L. acknowledges innumerable helpful discussions with M. Ingalls.
  • Updated Acknowledgments Show Changes
    Acknowledgments
    • M.S.F. thanks B. Davis Barnes for informal discussions, during one of which he used the words ‘demystifying diagenesis’ that struck a chord. M.S.F. is also grateful to B. Davis Barnes for coding up the first version of the carbonate recrystallization code that is used in this chapter and for sharing some of the digital art that is used to create Fig. 1. M.K.L. acknowledges innumerable helpful discussions with M. Ingalls.
    • This research refers to analyses of samples and data provided by the Ocean Drilling Program (ODP) and International Ocean Drilling Program (IODP). M.S.F. thanks B. Davis Barnes for informal discussions, during one of which he used the words ‘demystifying diagenesis’ that struck a chord. M.S.F. is also grateful to B. Davis Barnes for coding up the first version of the depositional carbonate recrystallization code that is used in this chapter and for sharing some of the digital art used in Figs. 1 and 3. M.K.L. acknowledges innumerable helpful discussions with M. Ingalls. The authors thank Editor Matthew Kohn for the invitation to write this chapter; we also appreciate the reviews of Ed Tipper and John Higgins.
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  • Updated Acknowledgments Show Changes
    Acknowledgments
    • This research refers to analyses of samples and data provided by the Ocean Drilling Program (ODP) and International Ocean Drilling Program (IODP). M.S.F. thanks B. Davis Barnes for informal discussions, during one of which he used the words ‘demystifying diagenesis’ that struck a chord. M.S.F. is also grateful to B. Davis Barnes for coding up the first version of the depositional carbonate recrystallization code that is used in this chapter and for sharing some of the digital art used in Figs. 1 and 3. M.K.L. acknowledges innumerable helpful discussions with M. Ingalls. The authors thank Editor Matthew Kohn for the invitation to write this chapter; we also appreciate the reviews of Ed Tipper and John Higgins.
    • This research refers to analyses of samples and data provided by the Ocean Drilling Program (ODP) and International Ocean Drilling Program (IODP). M.S.F. thanks Ben Davis Barnes for informal discussions, during one of which he used the words ‘demystifying diagenesis’ that struck a chord. M.S.F. is also grateful to Ben Davis Barnes for coding up the first version of the depositional carbonate recrystallization code that is used in this chapter and for sharing some of the digital art used in Figs. 1 and 3. M.K.L. acknowledges innumerable helpful discussions with M. Ingalls. The authors thank Editor Matthew Kohn for the invitation to write this chapter; we also appreciate the reviews of Ed Tipper and John Higgins.
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  • Updated Acknowledgments Show Changes
    Acknowledgments
    • This research refers to analyses of samples and data provided by the Ocean Drilling Program (ODP) and International Ocean Drilling Program (IODP). M.S.F. thanks Ben Davis Barnes for informal discussions, during one of which he used the words ‘demystifying diagenesis’ that struck a chord. M.S.F. is also grateful to Ben Davis Barnes for coding up the first version of the depositional carbonate recrystallization code that is used in this chapter and for sharing some of the digital art used in Figs. 1 and 3. M.K.L. acknowledges innumerable helpful discussions with M. Ingalls. The authors thank Editor Matthew Kohn for the invitation to write this chapter; we also appreciate the reviews of Ed Tipper and John Higgins.
    • This research refers to analyses of samples and data provided by the Ocean Drilling Program (ODP) and International Ocean Drilling Program (IODP). M.S.F. thanks Ben Davis Barnes for informal discussions, during one of which he used the words ‘demystifying diagenesis’ that struck a chord. M.S.F. is also grateful to Ben Davis Barnes for coding up the first version of the depositional carbonate recrystallization code that is used in this chapter and for sharing some of the digital art used in Figs. 1 and 3. M.S.F. also profusely thanks Carl Steefel, Jenny Druhan, Sergi Molins Rafa, and Nicole Fernandez for all of their patience, as well as their invaluable help with CrunchTope. M.K.L. acknowledges innumerable helpful discussions with M. Ingalls. The authors thank Editor Matthew Kohn for the invitation to write this chapter; we also appreciate the reviews of Ed Tipper and John Higgins.
  • Updated Keyword Show Changes
    Keyword
    • Ocean Drilling Program; carbon isotopes; calcium isotopes; magnesium isotopes; reactive transport model; mixing equations; carbonate authigenesis; clay authigenesis; partition coefficients
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    Publication Date
    • 2023
    • 2024
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Version 2
published

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  • Updated Keyword, Publisher, Description, and 1 more Show Changes
    Keyword
    • Ocean Drilling Program; carbon isotopes; calcium isotopes; magnesium isotopes; reactive transport model; mixing equations; carbonate authigenesis; clay authigenesis; partition coefficients
    • Ocean Drilling Program, Carbon isotopes, Calcium isotopes, Magnesium isotopes, Reactive transport model, Mixing equations, Carbonate authigenesis, Clay authigenesis, Partition coefficients
    Publisher
    • Elsevier
    Description
    • Diagenesis encompasses all physical, chemical, mineralogical changes that a sediment, rock, molecule, or mineral undergoes following deposition. Because the time that geologic materials spend in the diagenetic realm is substantial relative to the time spent in the formational environment, there is potential for primary materials to be altered diagenetically. Despite its importance, diagenesis is a difficult and complicated topic to discuss. In this contribution, we demonstrate the use of a range of quantitative tools, from mixing equations to reactive transport models, in order to facilitate diagenesis discussions. We consider simple models of CaCO_3 recrystallization and dolomitization, highlight key controls on diagenetic trajectories, present a compilation of partition coefficients for CaCO_3 and clays, and discuss model illustrations of the diagenetic generation/modification, of carbon, calcium, and lithium isotopic records in the marine sedimentary section.
    • Diagenesis encompasses all physical, chemical, mineralogical changes that a sediment, rock, molecule, or mineral undergoes following deposition. Because the time that geologic materials spend in the diagenetic realm is substantial relative to the time spent in the formational environment, there is potential for primary materials to be altered diagenetically. Despite its importance, diagenesis is a difficult and complicated topic to discuss. In this contribution, we demonstrate the use of a range of quantitative tools, from mixing equations to reactive transport models, in order to facilitate diagenesis discussions. We consider simple models of _CaCO3_ recrystallization and dolomitization, highlight key controls on diagenetic trajectories, present a compilation of partition coefficients for _CaCO3_ and clays, and discuss model illustrations of the diagenetic generation/modification, of carbon, calcium, and lithium isotopic records in the marine sedimentary section.
    Related URLs
    • https://exchange.iseesystems.com/public/matthewfantle/fantle-and-lloyd-2023-carbonate-recrystallization-model
    • https://exchange.iseesystems.com/public/matthewfantle/fantle-and-lloyd-2023-carbonate-recrystallization-model, https://doi.org/10.1016/B978-0-323-99762-1.00062-0
  • Updated Work Title Show Changes
    Work Title
    • Demystifying Diagenesis: The Future of Diagenetic Inquiry in the Geosciences
    • Data for "Demystifying Diagenesis: The Future of Diagenetic Inquiry in the Geosciences"