• journal_title：Geology
• Contributor：David Wacey ; Nicola McLoughlin ; Martin J. Whitehouse ; Matt R. Kilburn
• Publisher：Geological Society of America
• Date：2010-
• Format：text/html
• Language：en
• Identifier：10.1130/G31329.1
• journal_abbrev：Geology
• issn：0091-7613
• volume：38
• issue：12
• firstpage：1115
• section：Articles

A sandstone from the ca. 3400 Ma Strelley Pool Formation of Western Australia contains pristine micron-sized pyrite intimately associated with organic material coating framework quartz grains. A synsedimentary to early diagenetic origin for this pyrite is indicated by its occurrence in black, bedded sandstone at the base of the formation, and in reworked black clasts higher up in the formation. High-resolution multiple sulfur isotope analysis (³²S, ³³S, ³⁴S) using secondary ion mass spectrometry (NanoSIMS and large-radius ion microprobe) reveals δ³⁴S_VCDT (Vienna Canyon Diablo troilite) values between ∼–12‰ and +6‰, and Δ³³S values between –1.65‰ and +1.43‰, from pyrite grains within a single thin section. A large spread of δ³⁴S values over only 5–10 μm, together with the spatial association of pyrite with carbon and nitrogen, indicates biological processing of sulfur. The presence of both +Δ³³S and –Δ³³S signals overprinted by significant mass-dependent δ³⁴S fractionation in this pyrite population indicates for the first time that both microbial sulfate reduction of aqueous sulfate (–Δ³³S) and microbial disproportionation of elemental sulfur (+Δ³³S) were co-occurring in an open-marine, sedimentary hosted ecosystem in the Paleoarchean.