Articles | Volume 6, issue 5
https://doi.org/10.5194/gmd-6-1543-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/gmd-6-1543-2013
© Author(s) 2013. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
The Rock Geochemical Model (RokGeM) v0.9
G. Colbourn
School of Geographical Sciences, University of Bristol, Bristol, UK
College of Life and Environmental Sciences, University of Exeter, Exeter, UK
A. Ridgwell
School of Geographical Sciences, University of Bristol, Bristol, UK
T. M. Lenton
College of Life and Environmental Sciences, University of Exeter, Exeter, UK
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49 citations as recorded by crossref.
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- Early Cenozoic Decoupling of Climate and Carbonate Compensation Depth Trends S. Greene et al. 10.1029/2019PA003601
- Retracted: Earth System Model Analysis of How Astronomical Forcing Is Imprinted Onto the Marine Geological Record: The Role of the Inorganic (Carbonate) Carbon Cycle and Feedbacks P. Vervoort et al. 10.1029/2020PA004090
- Relationships between CO2, thermodynamic limits on silicate weathering, and the strength of the silicate weathering feedback M. Winnick & K. Maher 10.1016/j.epsl.2018.01.005
- Spatial continuous integration of Phanerozoic global biogeochemistry and climate B. Mills et al. 10.1016/j.gr.2021.02.011
- Anthropogenic CO2 of High Emission Scenario Compensated After 3500 Years of Ocean Alkalinization With an Annually Constant Dissolution of 5 Pg of Olivine P. Köhler 10.3389/fclim.2020.575744
- Carbon cycle implications of terrestrial weathering changes since the last glacial maximum M. Brault et al. 10.1139/facets-2016-0040
- Multi-proxy evidence for sea level fall at the onset of the Eocene-Oligocene transition M. De Lira Mota et al. 10.1038/s41467-023-39806-6
- Coupled decline in ocean pH and carbonate saturation during the Palaeocene–Eocene Thermal Maximum M. Li et al. 10.1038/s41561-024-01579-y
- Inter‐annual simulation of global carbon cycle variations in a terrestrial–aquatic continuum T. Nakayama 10.1002/hyp.13616
- An impulse response function for the “long tail” of excess atmospheric CO2 in an Earth system model N. Lord et al. 10.1002/2014GB005074
- Inclusion of a suite of weathering tracers in the cGENIE Earth system model – muffin release v.0.9.23 M. Adloff et al. 10.5194/gmd-14-4187-2021
- Volcanic CO 2 degassing postdates thermogenic carbon emission during the end-Permian mass extinction Y. Wu et al. 10.1126/sciadv.abq4082
- New estimates of the storage permanence and ocean co-benefits of enhanced rock weathering Y. Kanzaki et al. 10.1093/pnasnexus/pgad059
- Nanoparticle and nanomineral production by fungi Q. Li et al. 10.1016/j.fbr.2021.07.003
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- Modeling the evolution of pulse-like perturbations in atmospheric carbon and carbon isotopes: the role of weathering–sedimentation imbalances A. Jeltsch-Thömmes & F. Joos 10.5194/cp-16-423-2020
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- Unravelling the sources of carbon emissions at the onset of Oceanic Anoxic Event (OAE) 1a M. Adloff et al. 10.1016/j.epsl.2019.115947
- Late Pleistocene Carbon Cycle Revisited by Considering Solid Earth Processes P. Köhler & G. Munhoven 10.1029/2020PA004020
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- Recovering the true size of an Eocene hyperthermal from the marine sedimentary record S. Kirtland Turner & A. Ridgwell 10.1002/2013PA002541
- An abyssal carbonate compensation depth overshoot in the aftermath of the Palaeocene–Eocene Thermal Maximum D. Penman et al. 10.1038/ngeo2757
- Understanding the causes and consequences of past marine carbon cycling variability through models D. Hülse et al. 10.1016/j.earscirev.2017.06.004
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