Phanerozoic cycles of sedimentary carbon and sulfur, Proceedings of the National Academy of Sciences, vol.78, issue.8, pp.4652-4656, 1981. ,
DOI : 10.1073/pnas.78.8.4652
URL : http://www.pnas.org/content/78/8/4652.full.pdf
Rethinking the ancient sulfur cycle Annual Review 274 of Earth and Planetary Sciences 43. doi:10.1146/annurev-earth-060313-054802, 2015. ,
Biogeochemistry of sulfur isotopes. Reviews in Mineralogy and 276, Geochemistry, vol.43, issue.1, pp.607-636, 2001. ,
DOI : 10.2138/gsrmg.43.1.607
Oxidation of the Ediacaran Ocean, Nature, vol.33, issue.7120, pp.744-747, 2006. ,
DOI : 10.1038/nature05345
Sulfur isotopic evidence for chemocline 280 upward excursions during the end-Permian mass extinction, Geochimica et Cosmochimica 281 Acta, pp.5740-5752, 2006. ,
DOI : 10.1016/j.gca.2006.08.005
Dynamic sulfur and carbon cycling through the end-Ordovician 283 extinction revealed by paired sulfate?pyrite ? 34 S, Earth and Planetary Science Letters, vol.284, pp.363144-155, 2013. ,
DOI : 10.1016/j.epsl.2012.12.015
The sulfur isotopic evolution of Phanerozoic seawater 286 based on the analysis of structurally substituted sulfate in carbonates, Chemical Geology, vol.287, issue.204, pp.255-286, 2004. ,
Sulfur cycling in the aftermath of a 635- 289 Ma snowball glaciation: evidence for a syn-glacial sulfidic deep ocean. Earth and 290 Planetary Science Letters, pp.551-570, 2006. ,
Geochemical evidence for widespread euxinia in the Later Cambrian ocean, Nature, vol.58, issue.7328, pp.80-83, 2011. ,
DOI : 10.1016/j.gca.2006.08.021
Carbon and sulfur isotopic anomalies 294 across the Ordovician?Silurian boundary on the Yangtze Platform, pp.32-39, 2009. ,
DOI : 10.1016/j.palaeo.2008.12.016
Large perturbations of the carbon and 297 sulfur cycle associated with the Late Ordovician mass extinction in South China, Geology, vol.298, issue.4, pp.37299-302, 2009. ,
) Carbon-and sulfur-isotope geochemistry of the 300, 2012. ,
Late Ordovician) Wangjiawan (Riverside) section, South China: global 301 correlation and environmental event interpretation, pp.302-337 ,
A sulfidic driver for the end-Ordovician 304 mass extinction. Earth and Planetary Science Letters, pp.331-332128, 2012. ,
Superheavy pyrite (??34Spyr > ??34SCAS) in the terminal Proterozoic Nama Group, southern Namibia: A consequence of low seawater sulfate at the dawn of animal life, Geology, vol.37, issue.8, pp.743-746, 2009. ,
DOI : 10.1130/G25775A.1
Sedimentary sequences in the Gulf of 309, 2005. ,
Shoreface migrations at the shelf edge and sea-level changes around the Last Glacial Maximum (Gulf of Lions, NW Mediterranean), Marine Geology, vol.234, issue.1-4, pp.21-42, 2006. ,
DOI : 10.1016/j.margeo.2006.09.012
URL : https://hal.archives-ouvertes.fr/hal-00145076
Impact of climate and sea level 315 changes on the ventilation of intermediate water and benthic foraminifer assemblages in 316 the Gulf of Lions, 2011. ,
Gulf of Lions), Palaeogeography, Palaeoclimatology, Palaeoecology, vol.309, pp.215-228 ,
The response of SST to insolation and ice sheet 319 variability from MIS 3 to MIS 11 in the northwestern Mediterranean Sea (Gulf of Lions), 2015. ,
Anomalous SST warming during MIS 13 in the Gulf of Lions (northwestern Mediterranean Sea), Organic Geochemistry, vol.92, pp.16-23, 2016. ,
DOI : 10.1016/j.orggeochem.2015.12.004
A review of coastal palaeoclimate and relative sea-level reconstructions using ??13C and C/N ratios in organic material, Earth-Science Reviews, vol.75, issue.1-4, pp.29-57, 2006. ,
DOI : 10.1016/j.earscirev.2005.10.003
Phase relationship between sea level 327 and abrupt climate change, Quaternary Science Reviews, pp.1-15, 2009. ,
DOI : 10.1016/j.quascirev.2009.07.019
Sulfate reduction and oxic respiration in marine sediments: implications for organic carbon preservation in euxinic environments, Deep Sea Research Part A. Oceanographic Research Papers, vol.36, issue.1, pp.36121-138, 1989. ,
DOI : 10.1016/0198-0149(89)90022-8
Source, transport and fate of terrestrial 332 organic carbon on the western Mediterranean Sea, Gulf of Lions, France. Marine 333, Chemistry, vol.105, pp.101-117, 2007. ,
Sulfur isotopes track the global extent and 335 dynamics of euxinia during Cretaceous Oceanic Anoxic Event 2, pp.18407-18412, 2013. ,
Low marine sulphate and protracted oxygenation of the Proterozoic biosphere, Nature, vol.44, issue.7010, pp.834-838, 2004. ,
DOI : 10.1016/S0016-7037(00)00572-X
CARBON, SULFUR, AND 339 OXYGEN ISOTOPE GEOCHEMISTRY OF INTERSTITIAL WATERS FROM THE 340 WESTERN MEDITERRANEAN, Proceedings of Ocean Drillings Program, Scientific 341 results, pp.413-421, 1999. ,
Sea-level and deep-sea- 343 temperature variability over the past 5.3 million years, Nature, vol.504, pp.477-482, 2014. ,
Onset of Mediterranean outflow into the North Atlantic, Science, vol.6, issue.6800, pp.1244-1250, 2014. ,
DOI : 10.1038/ngeo1680
Effect of electron donors on the 347 fractionation of sulfur isotopes by a marine Desulfovibrio sp, Geochimica et 348 Cosmochimica Acta, pp.4244-4259, 2011. ,
Influence of sulfate reduction rates on the 350 Phanerozoic sulfur isotope record, pp.11244-11249, 2013. ,
Yttrium and REE signature recognized in Central Mediterranean Sea (ODP Site 963) during the MIS 6???MIS 5 transition, Palaeogeography, Palaeoclimatology, Palaeoecology, vol.292, issue.1-2, pp.201-210, 2010. ,
DOI : 10.1016/j.palaeo.2010.03.045
Sulfur isotope systematics of a euxinic, low-sulfate lake: Evaluating the importance of the reservoir effect in modern and ancient oceans, Geology, vol.41, issue.6, pp.41663-666, 2013. ,
DOI : 10.1130/G34187.1
Ventilation of marine sediments indicated by depth profiles of pore water sulfate and ??34S, The Geochemical Society Special Publications, vol.9, pp.59-65, 2004. ,
DOI : 10.1016/S1873-9881(04)80007-5
Large Carbonate Associated Sulfate 360 isotopic variability between brachiopods, micrite, and other sedimentary components in 361, 2015. ,
DOI : 10.1016/j.epsl.2015.10.005
A paired sulfate?pyrite ? 34 S approach to understanding 363 the evolution of the Ediacaran?Cambrian sulfur cycle, Geochimica et Cosmochimica Acta, vol.364, pp.722636-2648, 2008. ,
Multiple sulfur isotope evidence for massive 366 oceanic sulfate depletion in the aftermath of Snowball Earth, Nature Communications, vol.7, 2016. ,
Reconstructing marine redox conditions for the Early Cambrian Yangtze Platform: Evidence from biogenic sulphur and organic carbon isotopes, Palaeogeography, Palaeoclimatology, Palaeoecology, vol.254, issue.1-2, pp.175-193, 2007. ,
DOI : 10.1016/j.palaeo.2007.03.015
Reconstruction of paleo-redox conditions and early sulfur cycling during deposition of the Cryogenian Datangpo Formation in South China, Gondwana Research, vol.18, issue.4, pp.632-637, 2010. ,
DOI : 10.1016/j.gr.2010.02.011
Early oxygenation of the terrestrial environment during the Mesoproterozoic, Nature, vol.66, issue.7321, pp.290-293, 2010. ,
DOI : 10.1038/nature09538
The use of chromium reduction 377 in the analysis of reduced inorganic sulfur in sediments and shales, Chemical Geology, vol.378, pp.54149-155, 1986. ,
An analytical scheme for determining forms of sulphur in oil shales and associated rocks, Talanta, vol.33, issue.12, pp.953-961, 1986. ,
DOI : 10.1016/0039-9140(86)80234-X
A simple and inexpensive chromium-reducible sulfur method for acid-sulfate soils, Applied Geochemistry, vol.23, issue.9, pp.2759-383, 2008. ,
DOI : 10.1016/j.apgeochem.2008.07.007
Sea-level variability over five glacial 385 cycles, Nature Communications, vol.5, pp.10-1038, 2014. ,
DOI : 10.1038/ncomms6076
URL : http://www.nature.com/articles/ncomms6076.pdf
000 years of abrupt climate 387 variability, Science, vol.800, issue.334, pp.347-351, 2011. ,
DOI : 10.1126/science.1203580
An optimized scheme of lettered marine isotope substages for the last 1.0 million years, and the climatostratigraphic nature of isotope stages and substages, Quaternary Science Reviews, vol.111, pp.94-106, 2015. ,
DOI : 10.1016/j.quascirev.2015.01.012