Simon Poulton
Poulton, Simon, 19..-....
Poulton, Simon W.
VIAF ID: 624165573916137800007 (Personal)
Permalink: http://viaf.org/viaf/624165573916137800007
Preferred Forms
- 100 1 _ ‡a Poulton, Simon W.
- 100 1 _ ‡a Poulton, Simon, ‡d 19..-....
- 100 0 _ ‡a Simon Poulton
4xx's: Alternate Name Forms (6)
Works
Title | Sources |
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Aerobic iron and manganese cycling in a redox-stratified Mesoarchean epicontinental sea | |
Anaerobic ammonium-oxidising bacteria: A biological source of the bacteriohopanetetrol stereoisomer in marine sediments | |
Analysis of mass dependent and mass independent selenium isotope variability in black shales | |
Anoxia in the terrestrial environment during the late Mesoproterozoic | |
Anoxic development of sapropel S1 in the Nile Fan inferred from redox sensitive proxies, Fe speciation, Fe and Mo isotopes | |
The Bacteriohopanepolyol Inventory of Novel Aerobic Methane Oxidising Bacteria Reveals New Biomarker Signatures of Aerobic Methanotrophy in Marine Systems | |
Bioavailability of zinc in marine systems through time | |
Biological regulation of atmospheric chemistry en route to planetary oxygenation | |
A bistable organic-rich atmosphere on the Neoarchaean Earth | |
Chemical and physical characteristics of iron oxides in riverine and glacial meltwater sediments | |
Co-diagenesis of iron and phosphorus in hydrothermal sediments from the southern East Pacific Rise: Implications for the evaluation of paleoseawater phosphate concentrations | |
Controls on Mo isotope fractionations in a Mn-rich anoxic marine sediment, Gullmar Fjord, Sweden | |
Decoupled oxygenation of the Ediacaran ocean and atmosphere during the rise of early animals | |
Determination of the stable iron isotopic composition of sequentially leached iron phases in marine sediments | |
Development of a sequential extraction procedure for iron: implications for iron partitioning in continentally derived particulates | |
Did anoxia terminate Ediacaran benthic communities? Evidence from early diagenesis | |
Does the Paleoproterozoic Animikie Basin record the sulfidic ocean transition?: COMMENT | |
Dynamic anoxic ferruginous conditions during the end-Permian mass extinction and recovery | |
Early Palaeozoic ocean anoxia and global warming driven by the evolution of shallow burrowing. | |
Early phosphorus redigested | |
An emerging picture of Neoproterozoic ocean chemistry: Insights from the Chuar Group, Grand Canyon, USA | |
Evolution of the oceanic sulfur cycle at the end of the Paleoproterozoic | |
Ferruginous conditions dominated later neoproterozoic deep-water chemistry | |
Fluctuations in Precambrian atmospheric oxygenation recorded by chromium isotopes | |
Fraction-specific controls on the trace element distribution in iron formations: Implications for trace metal stable isotope proxies | |
Green rust formation controls nutrient availability in a ferruginous water column | |
The iron paleoredox proxies: A guide to the pitfalls, problems and proper practice | |
The iron speciation paleoredox proxy, 2021: | |
Latest Permian carbonate carbon isotope variability traces heterogeneous organic carbon accumulation and authigenic carbonate formation | |
Links between seawater paleoredox and the formation of sediment-hosted massive sulphide (SHMS) deposits — Fe speciation and Mo isotope constraints from Late Devonian mudstones | |
Low-oxygen waters limited habitable space for early animals | |
Marine oxygen production and open water supported an active nitrogen cycle during the Marinoan Snowball Earth | |
Microfossils from the late Mesoproterozoic – early Neoproterozoic Atar/El Mreïti Group, Taoudeni Basin, Mauritania, northwestern Africa | |
Mo isotope fractionation during adsorption to Fe (oxyhydr)oxides | |
A model for the oceanic mass balance of rhenium and implications for the extent of Proterozoic ocean anoxia | |
Molybdenum drawdown during Cretaceous Oceanic Anoxic Event 2 | |
Molybdenum isotope constraints on the extent of late Paleoproterozoic ocean euxinia | |
Molybdenum record from black shales indicates oscillating atmospheric oxygen levels in the early Paleoproterozoic | |
Multiple oscillations in Neoarchaean atmospheric chemistry | |
A multiproxy study distinguishes environmental change from diagenetic alteration in the recent sedimentary record of the inner Cadiz Bay (SW Spain) | |
Nitrogen cycle feedbacks as a control on euxinia in the mid-Proterozoic ocean | |
A nutrient control on expanded anoxia and global cooling during the Late Ordovician mass extinction | |
Ocean acidification and the Permo-Triassic mass extinction. | |
Ocean euxinia and climate change “double whammy” drove the Late Ordovician mass extinction | |
Onset of the aerobic nitrogen cycle during the Great Oxidation Event | |
The onset of widespread marine red beds and the evolution of ferruginous oceans | |
Palaeoceanographic controls on spatial redox distribution over the Yangtze Platform during the Ediacaran-Cambrian transition | |
Pathways for Neoarchean pyrite formation constrained by mass-independent sulfur isotopes | |
Pervasive oxygenation along late Archaean ocean margins | |
Potentially Bioavailable Iron Delivery by Iceberg-hosted Sediments and Atmospheric Dust to the Polar Oceans | |
Re–Os age constraints and new observations of Proterozoic glacial deposits in the Vazante Group, Brazil | |
Redox changes in Early Cambrian black shales at Xiaotan section, Yunnan Province, South China | |
A revised scheme for the reactivity of iron (oxyhydr)oxide minerals towards dissolved sulfide | |
Rise to modern levels of ocean oxygenation coincided with the Cambrian radiation of animals | |
Selenium isotope evidence for progressive oxidation of the Neoproterozoic biosphere | |
Shallow water anoxia in the Mesoproterozoic ocean: Evidence from the Bashkir Meganticlinorium, Southern Urals | |
Solid phase associations, oceanic fluxes and the anthropogenic perturbation of transition metals in world river particulates | |
Spatial variability in oceanic redox structure 1.8 billion years ago | |
Stability of the nitrogen cycle during development of sulfidic water in the redox-stratified late Paleoproterozoic Ocean | |
Stepwise Earth oxygenation is an inherent property of global biogeochemical cycling | |
Sulfide oxidation and iron dissolution kinetics during the reaction of dissolved sulfide with ferrihydrite | |
Surface charge and growth of sulphate and carbonate green rust in aqueous media | |
Trace elements at the intersection of marine biological and geochemical evolution | |
Tracing the stepwise oxygenation of the Proterozoic ocean | |
The transition to a sulphidic ocean ∼ 1.84 billion years ago | |
The use of hydrous iron (III) oxides for the removal of hydrogen sulphide in aqueous systems |