4.7 Article

Inclusion of a suite of weathering tracers in the cGENIE Earth system model - muffin release v.0.9.23

Journal

GEOSCIENTIFIC MODEL DEVELOPMENT
Volume 14, Issue 7, Pages 4187-4223

Publisher

COPERNICUS GESELLSCHAFT MBH
DOI: 10.5194/gmd-14-4187-2021

Keywords

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Funding

  1. Natural Environment Research Council (NERC) [NE/L002434/1, NE/L011050/1, NE/P01903X/1, NE/N011112/1]
  2. NERC GW4+ Doctoral Scholarship
  3. ERC Consolidator [682760]
  4. NSF [1658024, 1702913]
  5. Heising Simons Foundation
  6. NERC [NE/P01903X/1, NE/L011050/1, NE/N011112/1] Funding Source: UKRI
  7. Directorate For Geosciences [1658024, 1702913] Funding Source: National Science Foundation
  8. Division Of Ocean Sciences [1658024, 1702913] Funding Source: National Science Foundation
  9. European Research Council (ERC) [682760] Funding Source: European Research Council (ERC)

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This study developed a new Earth system model to investigate the cycling of strontium, lithium, osmium and calcium isotopes, and their responses to environmental change. The model provides a better understanding of the relationships between these metal elements, other biogeochemical cycles, and climate change.
The metals strontium (Sr), lithium (Li), osmium (Os) and calcium (Ca), together with their isotopes, are important tracers of weathering and volcanism - primary processes which shape the long-term cycling of carbon and other biogeochemically important elements at the Earth's surface. Traditionally, because of their long residence times in the ocean, isotopic shifts in these four elements observed in the geologic record are almost exclusively interpreted with the aid of isotope-mixing, tracer-specific box models. However, such models may lack a mechanistic description of the links between the cycling of the four metals to other geochemically relevant elements, particularly carbon, or climate. Here we develop and evaluate an implementation of Sr, Li, Os and Ca isotope cycling in the Earth system model cGENIE. The model offers the possibility to study the dynamics of these metal systems alongside other more standard biogeochemical cycles, as well as their relationship with changing climate. We provide examples of how to apply this new model capability to investigate Sr, Li, Os and Ca isotope dynamics and responses to environmental change, for which we take the example of massive carbon release to the atmosphere.

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