Calibration of Sulfate Levels in the Archean Ocean

By K. Habicht, M. Gade, B. Thamdrup, Peter Berg, D. Canfield. Science, 2002

785 citations recorded by the source corpus.

Subfields: Geochemistry and Petrology, Oceanography, Paleontology

View Paper: https://www.semanticscholar.org/paper/e9b36287f8eb0ba4c3279123024489b8af5baf3c

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Geochemistry and Petrology

In Oceanography

In Paleontology

Citations in the corpus

Dating the rise of atmospheric oxygen (2004, background): “Early diagenetic pyrite in these successions has δ 34 S values consistent with a seawater sulphate content of”
The antiquity of microbial sulfate reduction (2004, background): “As the sulfur cycle is involved in atmospheric oxygen regulation, Precambrian sulfur isotopic records over geological time have been used to help understand the evolution of atmospheric oxygenation (Hayes et al., 1992; Canfield and Teske, 1996; Knoll and Canfield, 1998; Canfield et al., 2000; Habich”
Temperature and its control of isotope fractionation by a sulfate-reducing bacterium (2006, neutral): “E-mail address: dec@biology.sdu.dk (D.E. Canfield). berg, 1964; Habicht et al., 2002).”
Microbial Kinetic Controls on Calcite Morphology in Supersaturated Solutions (2005, methodology): “…that contained little sulfate relative to the modern-day oceans (Anbar and Knoll 2002; Grotzinger and James 2000; Grotzinger and Knoll 1999; Habicht et al. 2002), little sulfate and high DIC in our experimental solutions are relevant not only for modern-day high-DIC environments but also…”
Biological activity and the Earth's surface evolution: Insights from carbon, sulfur, nitrogen and iron stable isotopes in the rock record (2009, background): “• the organism involved [34]; • the sulfate concentration [17,48]; • the sulfate reduction rates [16,34,47].”
Late Ediacaran redox stability and metazoan evolution (2012, background): “This later scenario could reflect an extreme deficiency in seawater sulfate concentrations (Habicht et al., 2002), but is more likely associated with simple sulfate limitation within the sediments.”
The Biogeochemical Sulfur Cycle of Marine Sediments (2019, result): “These recent findings contradict previous conclusions that low sulfate concentrations consistently diminish 34ε (Habicht et al., 2002; Nakagawa et al., 2012; Gomes and Hurtgen, 2013).”
Multiple sulphur isotopic interpretations of biosynthetic pathways: implications for biological signatures in the sulphur isotope record (2003, methodology): “Also plotted are data from sulphate reduction experiments with Archaeglobus fulgidus (Habicht et al., 2002).”
The rise of oxygen in Earth’s early ocean and atmosphere (2014, background): “…atmosphere assert that comparatively large amounts of methane(CH 4 ),alongwithhigherhydrocarbongasessuchasethane(C 2 H 6 ) resultingfrommethanephotochemistry,wereproducedandpersistedunder thegenerallylowsulphate(SO 42 2 )conditionsoftheArchaeanoceanand low O 2 in the ocean and atmosphere 45–48 .”
Biogeochemical modelling of the rise in atmospheric oxygen (2006, background): “Unlike today, there was very little sulfate in the Archean oceans (Habicht et al., 2002), which were deeply anoxic as evidenced by the transport of ferrous iron (Holland, 1984; pp. 379–388).”