Rise in seawater sulphate concentration associated with the Paleoproterozoic positive carbon isotope excursion: Evidence from sulphate evaporites in the ∼2.2-2.1 Gyr shallow-marine Lucknow Formation, South Africa

Terra Nova

Volumn 20, Issue 2, 2008, Pages 108-117

  Schröder, Stefan ^a,d   Bekker, A ^b,e   Beukes, N J ^a   Strauss, H ^c   van Niekerk, H S ^a  

^a UNIVERSITY OF JOHANNESBURG   (South Africa)

^b GEOPHYSICAL LABORATORY   (United States)

^c UNIVERSITY OF MÜNSTER   (Germany)

^d TOTAL   (France)

^e UNIVERSITY OF MANITOBA   (Canada)

Author keywords

[No Author keywords available]

Indexed keywords

CARBON ISOTOPE; CARBONATE; CARBONATE PLATFORM; EVAPORITE; HALITE; OPEN OCEAN; PROTEROZOIC; PSEUDOMORPH; QUARTZ; REDOX CONDITIONS; SEAWATER; SELENITE; SULFATE; SULFUR ISOTOPE;

AFRICA; SOUTH AFRICA; SOUTHERN AFRICA; SUB-SAHARAN AFRICA;

EID: 41149109683     PISSN: 09544879     EISSN: 13653121     Source Type: Journal    
DOI: 10.1111/j.1365-3121.2008.00795.x     Document Type: Article

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