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Simon H. Bottrell
Researcher at University of Leeds
Publications - 187
Citations - 8419
Simon H. Bottrell is an academic researcher from University of Leeds. The author has contributed to research in topics: Aquifer & Pyrite. The author has an hindex of 48, co-authored 184 publications receiving 7773 citations. Previous affiliations of Simon H. Bottrell include University of Sheffield & University of Liverpool.
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The reactivity of sedimentary iron minerals toward sulfide
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Reconstruction of changes in global sulfur cycling from marine sulfate isotopes
TL;DR: Recently, a number of case studies using carbonate-associated sulfate (CAS) and marine biogenic barite data have been presented as mentioned in this paper, which can be used to infer a new evolutionary curve of marine sulfate concentrations and therefore a protracted oxidation of the Earth's biosphere.
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Thermochemical sulphate reduction and the generation of hydrogen sulphide and thiols (mercaptans) in Triassic carbonate reservoirs from the Sichuan Basin, China
TL;DR: In this paper, the authors collected data on H2S, thiophene and thiol concentrations and gas stable isotopes (δ34S and δ13C) for predominantly gas phase petroleum samples from Jurassic, Triassic, Permian and Upper Proterozoic (Sinian) reservoirs.
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Volcanism, mass extinction, and carbon isotope fluctuations in the Middle Permian of China.
Paul B. Wignall,Yadong Sun,David P.G. Bond,Gareth Izon,Robert J. Newton,Stéphanie Védrine,Mike Widdowson,Jason R. Ali,Xulong Lai,Haishui Jiang,Helen Cope,Simon H. Bottrell +11 more
TL;DR: Fossiliferous rocks from southwest China show that a major extinction in the Middle Permian coincided with extensive volcanic eruptions, and the onset of volcanism was marked by both large phreatomagmatic eruptions and extinctions amongst fusulinacean foraminifers and calcareous algae.
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The importance of the relationship between scale and process in understanding long-term DOC dynamics
Joanna M. Clark,Joanna M. Clark,Simon H. Bottrell,Chris D. Evans,Don Monteith,Rebecca Bartlett,Rob Rose,Robert J. Newton,Pippa J. Chapman +8 more
TL;DR: It is argued that regional differences in acid deposition loading may account for the apparent discrepancies between studies of dissolved organic carbon trends, and that the data behind the majority of these studies is more compatible than is often conveyed.