The carbonate-silicate geochemical cycle and its effect on atmospheric carbon dioxide over the past 100 million years, American Journal of Science, vol.283, pp.641-683, 1983. ,
Stromatolite and ooid deposits within the fluvial and lacustrine sediments of the Precambrian Ventersdorp Supergroup of South Africa, Precambrian Research, vol.12, pp.311-330, 1980. ,
Exploring the faint young Sun problem and the possible climates of the Archean Earth with a 3-D GCM, Journal of Geophysical Research: Atmospheres, vol.118, p.431, 2013. ,
URL : https://hal.archives-ouvertes.fr/hal-01092200
Bugs or Gunk? Nanoscale Methods for Assessing the Biogenicity of Ancient Microfossils and Organic Matter, Earliest Life on Earth: Habitats, Environments and Methods of Detection, vol.13, pp.239-289, 2011. ,
The Raman-derived carbonization continuum: A tool to select the best preserved molecular structures in Archean kerogens, Astrobiology, vol.16, pp.407-417, 2016. ,
URL : https://hal.archives-ouvertes.fr/hal-01321479
5-Ga hydrothermal fields and diamictites in the Barberton Greenstone Belt -Paleoarchean crust in cold environments, Science Advances, vol.3, 2016. ,
Low-latitude glaciation in the Palaeoproterozoic era, Nature, vol.386, pp.262-266, 1997. ,
The evolution of the 87 Sr/ 86 Sr of marine carbonates does not constrain continental growth, Precambrian Research, vol.229, pp.704-707, 2008. ,
URL : https://hal.archives-ouvertes.fr/hal-00829915
The Late Proterozoic glacial era. Palaeogeography, Palaeoclimatology, Solar Physics, vol.74, pp.255-272, 1981. ,
Continental extensional setting for the Archean Belingwe Greenstone Belt, Zimbabwe. Geology, vol.26, pp.883-886, 1998. ,
The oxygen isotope evolution of seawater: A critical review of a long-standing controversy and an improved geological water cycle model for the past 3.4 billion years, Earth-Science Reviews, vol.83, pp.83-122, 2007. ,
Terrestrial water fluxes dominated by transpiration, Nature, vol.496, pp.347-351, 2013. ,
Palaeoclimates: the first two billion years, Philosophical Transactions of the Royal Society B, vol.361, pp.917-929, 2006. ,
) Paleoclimates, ocean depth, and the oxygen isotopic composition of seawater, Earth and Planetary Science Letters, vol.252, pp.82-93, 2006. ,
Hydrogen and oxygen isotope ratios in nodular and bedded cherts, Geochimica et Cosmochimica Acta, vol.40, pp.1095-1108, 1976. ,
High Archean climatic temperature inferred from oxygen isotope geochemistry of cherts in the 3.5 Ga Swaziland Supergroup, America Bulletin, vol.115, pp.566-580, 2003. ,
Modelling of the oxygen isotope evolution of seawater: Implications for the climate interpretation of the d 18 O of marine sediments, Geochimica et Cosmochimica Acta, vol.63, pp.351-361, 1999. ,
Micrometer-scale chemical and isotopic criteria (O and Si) on the origin and history of Precambrian cherts: implications for paleotemperature reconstructions, Geochimica et Cosmochimica Acta, vol.92, pp.129-147, 2012. ,
Nitrogen isotopic composition and density of the Archean atmosphere, Science, vol.342, pp.101-104, 2013. ,
URL : https://hal.archives-ouvertes.fr/hal-01346331
Isotope composition and volume of Earth's early oceans, Proceedings of the National Academy of Science of the United States of America, vol.109, pp.4371-4376, 2012. ,
Duration and nature of the end-Cryogenian (Marinoan) glaciation, Geology, vol.44, pp.631-634, 2016. ,
A palaeo-temperature curve for the Precambrian oceans based on silicon isotopes in cherts, Nature, vol.443, pp.969-972, 2006. ,
There is no temperature dependence of net biochemical fractionation of Hydrogen and Oxygen isotopes in tree-ring cellulose, Isotopes in Environmental and Health Studies, vol.36, pp.303-317, 2000. ,
Multi-factorial in vivo stable isotope fractionation: causes, correlations, consequences and applications, Isotopes in Environmental and Health Studies, vol.51, pp.155-199, 2015. ,
URL : https://hal.archives-ouvertes.fr/hal-02142135
Air density 2.7 billion years ago limited to less than twice modern levels by fossil raindrop imprints, Nature, vol.484, pp.359-362, 2012. ,
Divergent biochemical fractionation, not convergent temperature, explains cellulose Oxygen isotope enrichment across latitudes, PLoS ONE, vol.6, 2011. ,