Not logged in
PANGAEA.
Data Publisher for Earth & Environmental Science

Torres, Mark A; Paris, Guillaume; Adkins, Jess F; Fischer, Woodward W (2018): Sulfur Isotopic Measurements of Canadian and South African Rivers [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.890986, Supplement to: Torres, MA et al. (2018): Riverine evidence for isotopic mass balance in the Earth's early sulfur cycle. Nature Geoscience, 11(9), 661-664, https://doi.org/10.1038/s41561-018-0184-7

Always quote citation above when using data! You can download the citation in several formats below.

RIS CitationBibTeX CitationShow MapGoogle Earth

Abstract:
During a time of negligible atmospheric pO2, Earth's early sulfur cycle generated a spectacular geological signal seen as the anomalous fractionation of multiple sulfur isotopic ratios. The disappearance of this signal from the geologic record has been hypothesized to constrain the timing of atmospheric oxygenation, though interpretive challenges exist. Asymmetry in existing S isotopic data, for example, suggest that the Archean crust was not mass balanced, with the implication that the loss of S isotope anomalies from the geologic record might lag the rise of atmospheric O2. Here, we present new S isotopic analyses of modern surface and groundwaters that drain Archean terrains in order to independently evaluate Archean S cycle mass balance. Natural waters contain sulfur derived from the underlying bedrock and thus can be used to ascertain its S isotopic composition at scales larger than typical geological samples allow. Analyses of 52 water samples from Canada and South Africa suggest that the Archean crust was mass balanced with an average multiple S isotopic composition equivalent to the bulk Earth. Overall, our work supports the hypothesis that the disappearance of multiple S isotope anomalies from the sedimentary record provides a robust proxy for the timing of the first rise in atmospheric O2.
Coverage:
Median Latitude: 37.155885 * Median Longitude: -68.012269 * South-bound Latitude: -28.238000 * West-bound Longitude: -89.333000 * North-bound Latitude: 49.784000 * East-bound Longitude: 31.176000
Event(s):
Best_Western_Hotel * Latitude: 48.381000 * Longitude: -89.299000 * Method/Device: Water sample (WS)
Black_Sturgeon_River * Latitude: 48.905000 * Longitude: -88.376000 * Method/Device: Water sample (WS)
Blackwater_River * Latitude: 49.609000 * Longitude: -87.957000 * Method/Device: Water sample (WS)
Parameter(s):
#NameShort NameUnitPrincipal InvestigatorMethod/DeviceComment
1Event labelEventTorres, Mark A
2Latitude of eventLatitudeTorres, Mark A
3Longitude of eventLongitudeTorres, Mark A
4AreaAreakm2Torres, Mark A
5ChlorideCl-µmol/lTorres, Mark A
6Sulfate[SO4]2-µmol/lTorres, Mark A
7δ34S, dissolved sulfateδ34S [SO4]2- diss‰ CDTTorres, Mark A
8Δδ33SΔδ33S‰ CDTTorres, Mark A
9Rock, archean ageRock archean%Torres, Mark A
Size:
276 data points

Download Data

Download dataset as tab-delimited text — use the following character encoding:

View dataset as HTML