FN Archimer Export Format
PT J
TI Globally asynchronous sulphur isotope signals require re-definition of the Great Oxidation Event
BT 
AF PHILIPPOT, Pascal
   AVILA, Janaina N.
   KILLINGSWORTH, Bryan A.
   TESSALINA, Svetlana
   BATON, Franck
   CAQUINEAU, Tom
   MULLER, Elodie
   PECOITS, Ernesto
   CARTIGNY, Pierre
   LALONDE, Stefan
   IRELAND, Trevor R.
   THOMAZO, Christophe
   VAN KRANENDONK, Martin J.
   BUSIGNY, Vincent
AS 1:1,2;2:3;3:4;4:5;5:1;6:1;7:1;8:1,8;9:1;10:4;11:3;12:6;13:7;14:1;
FF 1:;2:;3:;4:;5:;6:;7:;8:;9:;10:;11:;12:;13:;14:;
C1 Univ Paris Diderot, Inst Phys Globe Paris, Sorbonne Paris Cite, CNRS, 1 Rue Jussieu, F-75238 Paris, France.
   Univ Montpellier, Geosci Montpellier, CNRS, UMR 5243, F-34095 Montpellier, France.
   Australian Natl Univ, Res Sch Earth Sci, 142 Mills Rd, Canberra, ACT 2601, Australia.
   European Inst Marine Studies, UMR6538, Lab Geociences Ocean, Pl Nicolas Copernic, F-29280 Plouzane, France.
   Curtin Univ, John de Laeter Ctr Isotope Res, Fac Sci & Engn, Bld 301,GPO Box U1987, Perth, WA 6845, Australia.
   Univ Bourgogne Franche Comte, UMR Biogeosci UB6282, CNRS, 6 Bd Gabriel, F-21000 Dijon, France.
   Univ New South Wales, Sch Biol Earth & Environm Sci, Kensington, NSW 2052, Australia.
   Uruguay Technol Univ UTEC, Dept Environm Sci, Francisco Antonio Maciel 97000, Durazno, Uruguay.
C2 UNIV PARIS 07, FRANCE
   UNIV MONTPELLIER, FRANCE
   UNIV AUSTRALIAN NATL, AUSTRALIA
   UBO, FRANCE
   UNIV CURTIN, AUSTRALIA
   UNIV BOURGOGNE FRANCHE COMTE, FRANCE
   UNIV NEW S WALES, AUSTRALIA
   UNIV TECH URUGUAY (UTEC), URUGUAY
UM LGO
IN DOAJ
IF 11.878
TC 76
UR https://archimer.ifremer.fr/doc/00638/74983/75853.pdf
   https://archimer.ifremer.fr/doc/00638/74983/75854.pdf
   https://archimer.ifremer.fr/doc/00638/74983/75855.pdf
   https://archimer.ifremer.fr/doc/00638/74983/75856.pdf
   https://archimer.ifremer.fr/doc/00638/74983/75858.xlsx
   https://archimer.ifremer.fr/doc/00638/74983/75859.xlsx
   https://archimer.ifremer.fr/doc/00638/74983/75860.xlsx
LA English
DT Article
AB The Great Oxidation Event (GOE) has been defined as the time interval when sufficient atmospheric oxygen accumulated to prevent the generation and preservation of mass-independent fractionation of sulphur isotopes (MIF-S) in sedimentary rocks. Existing correlations suggest that the GOE was rapid and globally synchronous. Here we apply sulphur isotope analysis of diagenetic sulphides combined with U-Pb and Re-Os geochronology to document the sulphur cycle evolution in Western Australia spanning the GOE. Our data indicate that, from similar to 2.45 Gyr to beyond 2.31 Gyr, MIF-S was preserved in sulphides punctuated by several episodes of MIF-S disappearance. These results establish the MIF-S record as asynchronous between South Africa, North America and Australia, argue for regional-scale modulation of MIF-S memory effects due to oxidative weathering after the onset of the GOE, and suggest that the current paradigm of placing the GOE at 2.33-2.32 Ga based on the last occurrence of MIF-S in South Africa should be re-evaluated. 
PY 2018
PD JUL
SO Nature Communications
SN 2041-1723
PU Nature Publishing Group
VL 9
IS 2245
UT 000434648400001
DI 10.1038/s41467-018-04621-x
ID 74983
ER

EF