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Jimmy Member

Fig. 1. The Belingwe greenstone belt, Zimbabwe, showing sample locations. The thin Manjeri Fm (including Spring Valley, Shavi, Rubweruchena and Jimmy Members, not shown here) outcrops along the base of the main (Upper Greenstones) syncline. Fig. 1. The Belingwe greenstone belt, Zimbabwe, showing sample locations. The thin Manjeri Fm (including Spring Valley, Shavi, Rubweruchena and Jimmy Members, not shown here) outcrops along the base of the main (Upper Greenstones) syncline.
Jimmy Member (Manjeri Fm) Carbon sulphide -38 to -20 -14.9 to +16.7 most around 0 Sulphur mat including methanogens... [Pg.317]

Sulphur isotopes. Sulphur isotopes in the Jimmy Member show a wide range in S S (—14.9 to -l-16.7%o) with symmetrically distributed... [Pg.322]

In the Jimmy Member, in a strata-bound setting at the boundary above the clastic Manjeri sediment and before the eruption of the volcanic rocks of the Reliance Fm, the isotopic and textural evidence and C abundance implies that a non-photosynthetic bacterial mat grew, supported by a complex sulphur cycle, and by fermentation of organic debris, methanogenesis and methanotrophy. It should, however, be stressed that the evidence for depth below the... [Pg.325]


See other pages where Jimmy Member is mentioned: [Pg.292]    [Pg.292]    [Pg.293]    [Pg.312]    [Pg.312]    [Pg.312]    [Pg.313]    [Pg.313]    [Pg.314]    [Pg.315]    [Pg.315]    [Pg.315]    [Pg.316]    [Pg.318]    [Pg.318]    [Pg.318]    [Pg.318]    [Pg.320]    [Pg.321]    [Pg.321]    [Pg.322]    [Pg.322]    [Pg.322]    [Pg.324]    [Pg.325]    [Pg.326]    [Pg.233]   
See also in sourсe #XX -- [ Pg.292 , Pg.311 , Pg.312 , Pg.316 , Pg.318 , Pg.322 , Pg.323 , Pg.324 , Pg.325 ]




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