2021 - Geochemistry Fellow Honor, Geochemical Society and the European Association of Geochemistry
The scientist’s investigation covers issues in Oceanography, Anoxic waters, Precambrian, Paleontology and Inorganic chemistry. Simon W. Poulton interconnects Glacial period and Biogeochemical cycle in the investigation of issues within Oceanography. His work carried out in the field of Anoxic waters brings together such families of science as Geochemistry, Pyrite, Total organic carbon and Sturtian glaciation.
Simon W. Poulton has researched Precambrian in several fields, including Paleoatmosphere and Earth science. His studies deal with areas such as Bottom water, Deep sea, Molybdenum isotope and Phytoplankton as well as Paleontology. As part of one scientific family, Simon W. Poulton deals mainly with the area of Inorganic chemistry, narrowing it down to issues related to the Magnetite, and often Hematite, Molybdenum and Dissolved phase.
His main research concerns Anoxic waters, Geochemistry, Paleontology, Environmental chemistry and Oceanography. His research integrates issues of Earth science, Biogeochemical cycle, Water column, Precambrian and Upwelling in his study of Anoxic waters. His Geochemistry course of study focuses on Seawater and Redox.
His Paleontology study frequently links to adjacent areas such as Deep sea. His Environmental chemistry research integrates issues from Organic matter, Ecology and Mineralogy. His work in the fields of Oceanography, such as Biogeochemistry, intersects with other areas such as Environmental science.
Simon W. Poulton mainly investigates Anoxic waters, Geochemistry, Environmental chemistry, Water column and Environmental science. His study on Anoxic waters also encompasses disciplines like
He combines subjects such as Carbonate minerals and Genetic algorithm with his study of Environmental chemistry. His biological study deals with issues like Anomaly, which deal with fields such as Paleontology. The various areas that Simon W. Poulton examines in his Biogeochemical cycle study include Syntrophy, Earth science and Biogeochemistry.
Simon W. Poulton mostly deals with Environmental science, Anoxic waters, Geochemistry, Environmental chemistry and Water column. His Anoxic waters study combines topics in areas such as Structural basin, Period, Ocean chemistry and Archean. His Geochemistry research is multidisciplinary, incorporating perspectives in Oil shale and Oxygen minimum zone.
His Water column research incorporates themes from Sedimentary depositional environment, Deep sea, Phanerozoic and Pyrite. His study brings together the fields of Precambrian and Pyrite. His research in Biogeochemical cycle intersects with topics in Earth science and Biogeochemistry.
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Late-Neoproterozoic deep-ocean oxygenation and the rise of animal life.
Donald Eugene Canfield;Simon W. Poulton;Guy M. Narbonne.
Science (2007)
Development of a sequential extraction procedure for iron: implications for iron partitioning in continentally derived particulates
Simon W. Poulton;Donald Eugene Canfield.
Chemical Geology (2005)
Tracing the stepwise oxygenation of the Proterozoic ocean
C. Scott;T. W. Lyons;A. Bekker;A. Bekker;Y. Shen.
Nature (2008)
Ferruginous Conditions Dominated Later Neoproterozoic Deep-Water Chemistry
Donald E. Canfield;Simon W. Poulton;Andrew H. Knoll;Guy M. Narbonne.
Science (2008)
Ferruginous Conditions: A Dominant Feature of the Ocean through Earth's History
Simon W. Poulton;Donald Eugene Canfield.
Elements (2011)
Fluctuations in Precambrian atmospheric oxygenation recorded by chromium isotopes
Robert Frei;Claudio Gaucher;Simon W. Poulton;Don E. Canfield.
Nature (2009)
A revised scheme for the reactivity of iron (oxyhydr)oxide minerals towards dissolved sulfide
Simon W. Poulton;Michael D. Krom;Robert Raiswell.
Geochimica et Cosmochimica Acta (2004)
The low-temperature geochemical cycle of iron: From continental fluxes to marine sediment deposition
Simon Poulton;Robert Raiswell.
American Journal of Science (2002)
The transition to a sulphidic ocean ∼ 1.84 billion years ago
Simon W. Poulton;Philip W. Fralick;Donald E. Canfield.
Nature (2004)
Spatial variability in oceanic redox structure 1.8 billion years ago
Simon W. Poulton;Philip W. Fralick;Donald Eugene Canfield.
Nature Geoscience (2010)
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