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Seabirds shaped the expansion of pre-Inca society in Peru. [PDF]
Bongers JL +5 more
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Oxidation of Organic Sulfur at the Air-Water Interface of Microdroplets: A New Way of Atmospheric Particle Precursor Formation. [PDF]
Tang H +9 more
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Mass spectrometry measurements of mercury isotope ratios support geochemical sourcing of archaeological cinnabar in the Andean region. [PDF]
Young M +9 more
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Sulfur as a proxy for identifying coast-inland human mobility in Northern Iberia during Late Prehistory. [PDF]
González-Rabanal B +12 more
europepmc +1 more source
Deciphering sulfur cycling with multiple sulfur isotopes
Laetitia Guibourdenche explains the use of multiple sulfur isotopes in understanding past and present sulfur cycling.
Laetitia Guibourdenche
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Biogeochemistry of Sulfur Isotopes
Reviews in Mineralogy and Geochemistry, 2001Sulfur, with an atomic weight of 32.06, has four stable isotopes. By far the most abundant is 32S, representing around 95% of the total sulfur on Earth. The next most abundant isotope is 34S, followed by 33S, and finally 36S is the least abundant contributing only 0.0136% to the total (Table 1⇓). The natural abundances of sulfur isotopes, however, vary
openaire +3 more sources
High-precision analysis of multiple sulfur isotopes using NanoSIMS
We report here data of multiple sulfur isotopes (32S, 33S, and 34S) measured by NanoSIMS 50L ion microprobe in Fe–Ni–Cu standards, and pyrite grains recovered from the Neoarchean Abitibi Supracrustal Terrain, Canada.
Erik H Hauri +2 more
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Sulfur Isotopic Composition of Mangroves
Isotopes in Environmental and Health Studies, 1998Abstract Sulfur isotope ratios of mangrove leaves of 19 species were compared to discuss the species-specific characteristics of sulfur uptake and assimilation. The members of Rhizophora and Bruguiera always show remarkable enrichments of the light isotope, giving negative δ(34)S values in most cases.
N, Okada, A, Sasaki
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Cenozoic evolution of the sulfur cycle: Insight from oxygen isotopes in marine sulfate
We report new data on oxygen isotopes in marine sulfate (delta(18)O(SO4)), measured in marine barite (BaSO4), over the Cenozoic. The delta(18)O(SO4) varies by 6 parts per thousand over the Cenozoic, with major peaks 3, 15, 30 and 55 Ma.
Alexandra V Turchyn, Daniel P Schrag
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