Articles | Volume 5, issue 1
https://doi.org/10.5194/bg-5-253-2008
© Author(s) 2008. This work is licensed under
the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 License.
the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 License.
Special issue:
https://doi.org/10.5194/bg-5-253-2008
© Author(s) 2008. This work is licensed under
the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 License.
the Creative Commons Attribution-NonCommercial-ShareAlike 2.5 License.
21 Feb 2008
A geochemical modelling study of the evolution of the chemical composition of seawater linked to a "snowball" glaciation
G. Le Hir
LSCE, CNRS-CEA-UVSQ, Gif-sur-Yvette, France
Y. Goddéris
LMTG, CNRS, Observatoire Midi-Pyrénées, Toulouse, France
Y. Donnadieu
LSCE, CNRS-CEA-UVSQ, Gif-sur-Yvette, France
G. Ramstein
LSCE, CNRS-CEA-UVSQ, Gif-sur-Yvette, France
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Cited
32 citations as recorded by crossref.
- Hematite U-Pb dating of Snowball Earth meltwater events L. Courtney-Davies et al. https://doi.org/10.1073/pnas.2410759121
- Synsedimentary diagenesis in a Cryogenian reef complex: Ubiquitous marine dolomite precipitation A. Hood & M. Wallace https://doi.org/10.1016/j.sedgeo.2012.02.004
- Cryoconite pans on Snowball Earth: supraglacial oases for Cryogenian eukaryotes? P. Hoffman https://doi.org/10.1111/gbi.12191
- Neoproterozoic syn‐glacial carbonate precipitation and implications for a snowball Earth A. Hood et al. https://doi.org/10.1111/gbi.12470
- GEOCLIM reloaded (v 1.0): a new coupled earth system model for past climate change S. Arndt et al. https://doi.org/10.5194/gmd-4-451-2011
- Mechanistic Links Between the Sedimentary Redox Cycle and Marine Acid‐Base Chemistry C. Reinhard & W. Fischer https://doi.org/10.1029/2019GC008621
- Three-stage formation of cap carbonates after Marinoan snowball glaciation consistent with depositional timescales and geochemistry T. Thomas & D. Catling https://doi.org/10.1038/s41467-024-51412-8
- Enigmatic carbonates of the Ombombo Subgroup, Otavi Fold Belt, Namibia: A prelude to extreme Cryogenian anoxia? A. Hood et al. https://doi.org/10.1016/j.sedgeo.2015.04.007
- Neoproterozoic marine carbonates and their paleoceanographic significance A. Hood & M. Wallace https://doi.org/10.1016/j.gloplacha.2017.11.006
- Ice, Fire, or Fizzle: The Climate Footprint of Earth's Supercontinental Cycles A. Jellinek et al. https://doi.org/10.1029/2019GC008464
- Coupled carbon and silica cycle perturbations during the Marinoan snowball Earth deglaciation D. Penman & A. Rooney https://doi.org/10.1130/G45812.1
- Episode of intense chemical weathering during the termination of the 635 Ma Marinoan glaciation K. Huang et al. https://doi.org/10.1073/pnas.1607712113
- Coupled dolomite and silica precipitation from continental weathering during deglaciation of the Marinoan Snowball Earth Y. Fang & H. Xu https://doi.org/10.1016/j.precamres.2022.106824
- Nonmonotonic Postdeglacial Relative Sea Level Changes at the Aftermath of Marinoan (635 Ma) Snowball Earth Meltdown Y. Irie et al. https://doi.org/10.1029/2018JB017260
- Y/Ho ratios in marine sediments unveil Neoproterozoic ocean acidification Y. Liu et al. https://doi.org/10.1016/j.scib.2026.01.028
- Continental influences on post-Marinoan (∼635 Ma) seawater: Chemostratigraphic evidence from the Puga cap carbonate, Amazon Craton margin R. dos Santos et al. https://doi.org/10.1016/j.palaeo.2025.113380
- Snowball Earth climate dynamics and Cryogenian geology-geobiology P. Hoffman et al. https://doi.org/10.1126/sciadv.1600983
- Neoproterozoic aragonite-dolomite seas? Widespread marine dolomite precipitation in Cryogenian reef complexes A. Hood et al. https://doi.org/10.1130/G32119.1
- A warm or a cold early Earth? New insights from a 3-D climate-carbon model B. Charnay et al. https://doi.org/10.1016/j.epsl.2017.06.029
- Four-million-year Marinoan snowball shows multiple routes to deglaciation A. Tasistro-Hart et al. https://doi.org/10.1073/pnas.2418281122
- Chapter 10 Modelling the Snowball Earth Y. Goddéris et al. https://doi.org/10.1144/M36.10
- Moderate greenhouse climate and rapid carbonate formation after Marinoan snowball Earth L. Ramme et al. https://doi.org/10.1038/s41467-024-47873-6
- Climates of the Earth and Cryosphere Evolution G. Ramstein https://doi.org/10.1007/s10712-011-9140-4
- A transient peak in marine sulfate after the 635-Ma snowball Earth Y. Peng et al. https://doi.org/10.1073/pnas.2117341119
- Understanding the causes and consequences of past marine carbon cycling variability through models D. Hülse et al. https://doi.org/10.1016/j.earscirev.2017.06.004
- Constraining the diagenesis of the Puga cap carbonate from U–Pb in‐situ dating of seafloor crystal fans, southern Amazonian craton, Brazil D. de Carvalho et al. https://doi.org/10.1111/ter.12652
- Sedimentary challenge to Snowball Earth P. Allen & J. Etienne https://doi.org/10.1038/ngeo355
- Transient marine euxinia at the end of the terminal Cryogenian glaciation X. Lang et al. https://doi.org/10.1038/s41467-018-05423-x
- The snowball Earth aftermath: Exploring the limits of continental weathering processes G. Le Hir et al. https://doi.org/10.1016/j.epsl.2008.11.010
- Climate and ocean circulation in the aftermath of a Marinoan snowball Earth L. Ramme & J. Marotzke https://doi.org/10.5194/cp-18-759-2022
- Massive Volcanism May Have Foreshortened the Marinoan Snowball Earth Z. Lan et al. https://doi.org/10.1029/2021GL097156
- WATER LOSS FROM TERRESTRIAL PLANETS WITH CO2-RICH ATMOSPHERES R. Wordsworth & R. Pierrehumbert https://doi.org/10.1088/0004-637X/778/2/154
32 citations as recorded by crossref.
- Hematite U-Pb dating of Snowball Earth meltwater events L. Courtney-Davies et al. https://doi.org/10.1073/pnas.2410759121
- Synsedimentary diagenesis in a Cryogenian reef complex: Ubiquitous marine dolomite precipitation A. Hood & M. Wallace https://doi.org/10.1016/j.sedgeo.2012.02.004
- Cryoconite pans on Snowball Earth: supraglacial oases for Cryogenian eukaryotes? P. Hoffman https://doi.org/10.1111/gbi.12191
- Neoproterozoic syn‐glacial carbonate precipitation and implications for a snowball Earth A. Hood et al. https://doi.org/10.1111/gbi.12470
- GEOCLIM reloaded (v 1.0): a new coupled earth system model for past climate change S. Arndt et al. https://doi.org/10.5194/gmd-4-451-2011
- Mechanistic Links Between the Sedimentary Redox Cycle and Marine Acid‐Base Chemistry C. Reinhard & W. Fischer https://doi.org/10.1029/2019GC008621
- Three-stage formation of cap carbonates after Marinoan snowball glaciation consistent with depositional timescales and geochemistry T. Thomas & D. Catling https://doi.org/10.1038/s41467-024-51412-8
- Enigmatic carbonates of the Ombombo Subgroup, Otavi Fold Belt, Namibia: A prelude to extreme Cryogenian anoxia? A. Hood et al. https://doi.org/10.1016/j.sedgeo.2015.04.007
- Neoproterozoic marine carbonates and their paleoceanographic significance A. Hood & M. Wallace https://doi.org/10.1016/j.gloplacha.2017.11.006
- Ice, Fire, or Fizzle: The Climate Footprint of Earth's Supercontinental Cycles A. Jellinek et al. https://doi.org/10.1029/2019GC008464
- Coupled carbon and silica cycle perturbations during the Marinoan snowball Earth deglaciation D. Penman & A. Rooney https://doi.org/10.1130/G45812.1
- Episode of intense chemical weathering during the termination of the 635 Ma Marinoan glaciation K. Huang et al. https://doi.org/10.1073/pnas.1607712113
- Coupled dolomite and silica precipitation from continental weathering during deglaciation of the Marinoan Snowball Earth Y. Fang & H. Xu https://doi.org/10.1016/j.precamres.2022.106824
- Nonmonotonic Postdeglacial Relative Sea Level Changes at the Aftermath of Marinoan (635 Ma) Snowball Earth Meltdown Y. Irie et al. https://doi.org/10.1029/2018JB017260
- Y/Ho ratios in marine sediments unveil Neoproterozoic ocean acidification Y. Liu et al. https://doi.org/10.1016/j.scib.2026.01.028
- Continental influences on post-Marinoan (∼635 Ma) seawater: Chemostratigraphic evidence from the Puga cap carbonate, Amazon Craton margin R. dos Santos et al. https://doi.org/10.1016/j.palaeo.2025.113380
- Snowball Earth climate dynamics and Cryogenian geology-geobiology P. Hoffman et al. https://doi.org/10.1126/sciadv.1600983
- Neoproterozoic aragonite-dolomite seas? Widespread marine dolomite precipitation in Cryogenian reef complexes A. Hood et al. https://doi.org/10.1130/G32119.1
- A warm or a cold early Earth? New insights from a 3-D climate-carbon model B. Charnay et al. https://doi.org/10.1016/j.epsl.2017.06.029
- Four-million-year Marinoan snowball shows multiple routes to deglaciation A. Tasistro-Hart et al. https://doi.org/10.1073/pnas.2418281122
- Chapter 10 Modelling the Snowball Earth Y. Goddéris et al. https://doi.org/10.1144/M36.10
- Moderate greenhouse climate and rapid carbonate formation after Marinoan snowball Earth L. Ramme et al. https://doi.org/10.1038/s41467-024-47873-6
- Climates of the Earth and Cryosphere Evolution G. Ramstein https://doi.org/10.1007/s10712-011-9140-4
- A transient peak in marine sulfate after the 635-Ma snowball Earth Y. Peng et al. https://doi.org/10.1073/pnas.2117341119
- Understanding the causes and consequences of past marine carbon cycling variability through models D. Hülse et al. https://doi.org/10.1016/j.earscirev.2017.06.004
- Constraining the diagenesis of the Puga cap carbonate from U–Pb in‐situ dating of seafloor crystal fans, southern Amazonian craton, Brazil D. de Carvalho et al. https://doi.org/10.1111/ter.12652
- Sedimentary challenge to Snowball Earth P. Allen & J. Etienne https://doi.org/10.1038/ngeo355
- Transient marine euxinia at the end of the terminal Cryogenian glaciation X. Lang et al. https://doi.org/10.1038/s41467-018-05423-x
- The snowball Earth aftermath: Exploring the limits of continental weathering processes G. Le Hir et al. https://doi.org/10.1016/j.epsl.2008.11.010
- Climate and ocean circulation in the aftermath of a Marinoan snowball Earth L. Ramme & J. Marotzke https://doi.org/10.5194/cp-18-759-2022
- Massive Volcanism May Have Foreshortened the Marinoan Snowball Earth Z. Lan et al. https://doi.org/10.1029/2021GL097156
- WATER LOSS FROM TERRESTRIAL PLANETS WITH CO2-RICH ATMOSPHERES R. Wordsworth & R. Pierrehumbert https://doi.org/10.1088/0004-637X/778/2/154
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