Matthew O Clarkson
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View article: Unlocking Gigatonne-scale Carbon Dioxide Removal with strategic tipping point frameworks
Unlocking Gigatonne-scale Carbon Dioxide Removal with strategic tipping point frameworks Open
Achieving global climate mitigation requires a rapid acceleration of Carbon Dioxide Removal (CDR) to gigatonne (Gt) scales by 2040. Linear growth in climate solutions is insufficient to reach these targets, but system-change practices and …
View article: An assessment of the agronomic benefits of silicate rock powders in Brazil in the context of a novel classification
An assessment of the agronomic benefits of silicate rock powders in Brazil in the context of a novel classification Open
The sustainable intensification of tropical agriculture requires innovative approaches to restore soil health, reduce dependency on imported fertilizers, and increase crop productivity. Brazil has emerged as a global leader in the use of s…
View article: A review of measurement for quantification of carbon dioxide removal by enhanced weathering in soil
A review of measurement for quantification of carbon dioxide removal by enhanced weathering in soil Open
All pathways which limit global temperature rise to <2°C above pre-industrial temperatures now require carbon dioxide removal (CDR) in addition to rapid greenhouse gas emissions reductions. Novel and durable CDR strategies need to rapid…
View article: Alignment of industry, regulation and academia for quantification of carbon dioxide removal by enhanced weathering
Alignment of industry, regulation and academia for quantification of carbon dioxide removal by enhanced weathering Open
Terrestrial enhanced weathering (EW) is a promising emerging carbon dioxide removal technique which involves the acceleration of natural weathering processes via the deployment of crushed rock feedstocks, typically Ca- and Mg-rich silicate…
View article: A Review of Measurement for Quantification of Carbon Dioxide Removal by Enhanced Weathering in Soil
A Review of Measurement for Quantification of Carbon Dioxide Removal by Enhanced Weathering in Soil Open
All pathways which limit global temperature rise to <2oC above pre-industrial temperatures now require carbon dioxide removal (CDR) in addition to rapid greenhouse gas emissions reductions. Novel and durable CDR strategies need to rapidly …
View article: Uranium isotope evidence for extensive seafloor anoxia after the end-Triassic mass extinction
Uranium isotope evidence for extensive seafloor anoxia after the end-Triassic mass extinction Open
View article: Regional conditions cause contrasting behaviour in U-isotope fractionation in black shales: Constraints for global ocean palaeo-redox reconstructions
Regional conditions cause contrasting behaviour in U-isotope fractionation in black shales: Constraints for global ocean palaeo-redox reconstructions Open
View article: Source versus weathering processes as controls on the Mackenzie river uranium isotope signature
Source versus weathering processes as controls on the Mackenzie river uranium isotope signature Open
View article: Cd isotopes in carbonates deposited during ‘OAE 2’: Assessment of a novel palaeo-productivity tracer
Cd isotopes in carbonates deposited during ‘OAE 2’: Assessment of a novel palaeo-productivity tracer Open
Cadmium (Cd) displays nutrient-type patterns in the modern ocean and has potential as a tracer of the efficiency of the ‘biological pump’ and its ability to transport CO2 from the atmosphere to the deep ocean during intervals o…
View article: Extensive anoxia after the end-Triassic mass extinction: uranium isotope evidence from the Triassic-Jurassic boundary section at Csővár
Extensive anoxia after the end-Triassic mass extinction: uranium isotope evidence from the Triassic-Jurassic boundary section at Csővár Open
The end-Triassic mass extinction (ETE) ranks as one of the ’Big Five’ biotic crises in Earth history. The processes that led to the ecosystem collapse are thought to have been triggered by the volcanism of the Central Atlantic …
View article: Environmental controls on very high δ238U values in reducing sediments: Implications for Neoproterozoic seawater records
Environmental controls on very high δ238U values in reducing sediments: Implications for Neoproterozoic seawater records Open
View article: Source versus weathering processes as controls on the Mackenzie river uranium isotope signature
Source versus weathering processes as controls on the Mackenzie river uranium isotope signature Open
View article: Redox-sensitive metals and δ<sup>238</sup>U in red and grey shales: Exploring a new archive for palaeo-redox studies
Redox-sensitive metals and δ<sup>238</sup>U in red and grey shales: Exploring a new archive for palaeo-redox studies Open
View article: Co-variation systematics of uranium and molybdenum isotopes reveal pathways for descent into euxinia in Mediterranean sapropels
Co-variation systematics of uranium and molybdenum isotopes reveal pathways for descent into euxinia in Mediterranean sapropels Open
View article: Using Precambrian carbonates for seawater isotope reconstructions: constraints from LA-ICP-MS U-Pb geochronology of a post-Sturtian cap dolomite, Brazil
Using Precambrian carbonates for seawater isotope reconstructions: constraints from LA-ICP-MS U-Pb geochronology of a post-Sturtian cap dolomite, Brazil Open
<p>Global seawater isotope reconstructions from Precambrian marine carbonates must overcome particular difficulties on two fronts: i) accurate age constraints for global stratigraphic correlations and interpretations, and ii) the rel…
View article: The meaning of carbonate Zn isotope records: Constraints from a detailed geochemical and isotope study of bulk deep-sea carbonates
The meaning of carbonate Zn isotope records: Constraints from a detailed geochemical and isotope study of bulk deep-sea carbonates Open
View article: Cd isotopes in carbonates deposited during ‘OAE 2’: Assessment of a novel palaeo-productivity tracer
Cd isotopes in carbonates deposited during ‘OAE 2’: Assessment of a novel palaeo-productivity tracer Open
Cadmium (Cd) displays nutrient-type patterns in the oceans and offers potential as a tracer of the efficiency of the ocean's 'biological pump' and its ability to transport CO 2 from the atmosphere to the deep ocean during intervals of majo…
View article: Carbonate associated uranium isotopes as a novel local redox indicator in oxidatively disturbed reducing sediments
Carbonate associated uranium isotopes as a novel local redox indicator in oxidatively disturbed reducing sediments Open
View article: The Sedimentary Geochemistry and Paleoenvironments Project
The Sedimentary Geochemistry and Paleoenvironments Project Open
Geobiology explores how Earth's system has changed over the course of geologic history and how living organisms on this planet are impacted by or are indeed causing these changes. For decades, geologists, paleontologists, and geochemists h…
View article: Temporally and spatially dynamic redox conditions on an upwelling margin: The impact on coupled sedimentary Mo and U isotope systematics, and implications for the Mo-U paleoredox proxy
Temporally and spatially dynamic redox conditions on an upwelling margin: The impact on coupled sedimentary Mo and U isotope systematics, and implications for the Mo-U paleoredox proxy Open
View article: Toward a quantitative framework for assessing the global severity of Oceanic Anoxic Events
Toward a quantitative framework for assessing the global severity of Oceanic Anoxic Events Open
<p>Oceanic anoxia is a common response to past climate perturbations and often invoked as a direct cause of mass extinctions and faunal turnover events. During the Phanerozoic, there are numerous events that show qualitatively simila…
View article: Upper limits on the extent of seafloor anoxia during the PETM from uranium isotopes
Upper limits on the extent of seafloor anoxia during the PETM from uranium isotopes Open
View article: Magnesium and Uranium isotope composition of the Sturtian Jacoca Formation cap dolomite, Brazil
Magnesium and Uranium isotope composition of the Sturtian Jacoca Formation cap dolomite, Brazil Open
The Early Cryogenian period is marked by the Sturtian glaciation episode (ca.720-660 Ma) that triggered a global perturbation to ocean chemistry and to the surface cycles of many elements.However, reconstructing variations in seawater chem…
View article: Uranium isotopes in marine carbonates as a global ocean paleoredox proxy: A critical review
Uranium isotopes in marine carbonates as a global ocean paleoredox proxy: A critical review Open
View article: Examining pelagic carbonate-rich sediments as an archive for authigenic uranium and molybdenum isotopes using reductive cleaning and leaching experiments
Examining pelagic carbonate-rich sediments as an archive for authigenic uranium and molybdenum isotopes using reductive cleaning and leaching experiments Open
View article: Oceanographic and climatic evolution of the southeastern subtropical Atlantic over the last 3.5 Ma
Oceanographic and climatic evolution of the southeastern subtropical Atlantic over the last 3.5 Ma Open
View article: Uranium isotope evidence for two episodes of deoxygenation during Oceanic Anoxic Event 2
Uranium isotope evidence for two episodes of deoxygenation during Oceanic Anoxic Event 2 Open
Significance Past “Oceanic Anoxic Events” (OAEs) represent important carbon cycle perturbations that offer the opportunity to study Earth’s response to extreme climate warming. A fundamental limitation for understanding OAEs is quantifying…
View article: Low-oxygen waters limited habitable space for early animals
Low-oxygen waters limited habitable space for early animals Open
View article: Dynamic anoxic ferruginous conditions during the end-Permian mass extinction and recovery
Dynamic anoxic ferruginous conditions during the end-Permian mass extinction and recovery Open
View article: Effective use of cerium anomalies as a redox proxy in carbonate-dominated marine settings
Effective use of cerium anomalies as a redox proxy in carbonate-dominated marine settings Open
Rare earth elements and yttrium (REY) have a distinct distribution pattern in seawater, and this pattern may be faithfully preserved in carbonate sediments and rocks. Anomalous concentrations of redox-sensitive cerium (Ce) compared with ne…