about
Terrestrial-marine teleconnections in the Devonian: links between the evolution of land plants, weathering processes, and marine anoxic eventsRapid expansion of oceanic anoxia immediately before the end-Permian mass extinctionRedox chemistry changes in the Panthalassic Ocean linked to the end-Permian mass extinction and delayed Early Triassic biotic recovery.Uncovering the spatial heterogeneity of Ediacaran carbon cycling.Volcanic perturbations of the marine environment in South China preceding the latest Permian mass extinction and their biotic effects.Multiple episodes of extensive marine anoxia linked to global warming and continental weathering following the latest Permian mass extinction.Fe-oxide mineralogy of the Jiujiang red earth sediments and implications for Quaternary climate change, southern China.Nitrogen fixation sustained productivity in the wake of the Palaeoproterozoic Great Oxygenation Event.Oceanic response to Pliensbachian and Toarcian magmatic events: Implications from an organic-rich basinal succession in the NW TethysEnvironmental instability prior to end-Permian mass extinction reflected in biotic and facies changes on shallow carbonate platforms of the Nanpanjiang Basin (South China)Large vertical δ13CDIC gradients in Early Triassic seas of the South China craton: Implications for oceanographic changes related to Siberian Traps volcanismReconstruction of secular variation in seawater sulfate concentrationsTwo-stage marine anoxia and biotic response during the Permian–Triassic transition in Kashmir, northern India: pyrite framboid evidenceSequencing events across the Permian–Triassic boundary, Guryul Ravine (Kashmir, India)Re–Os depositional ages and seawater Os estimates for the Frasnian–Famennian boundary: Implications for weathering rates, land plant evolution, and extinction mechanismsAmelioration of marine environments at the Smithian–Spathian boundary, Early TriassicDiscerning primary versus diagenetic signals in carbonate carbon and oxygen isotope records: An example from the Permian–Triassic boundary of IranAn ancient estuarine-circulation nutrient trap: The Late Pennsylvanian Midcontinent Sea of North AmericaCongruent Permian-Triassic δ238U records at Panthalassic and Tethyan sites: Confirmation of global-oceanic anoxia and validation of the U-isotope paleoredox proxySulfur isotope evidence for transient marine-shelf oxidation during the Ediacaran Shuram ExcursionUranium and carbon isotopes document global-ocean redox-productivity relationships linked to cooling during the Frasnian-Famennian mass extinctionGlobal-ocean redox variation during the middle-late Permian through Early Triassic based on uranium isotope and Th/U trends of marine carbonatesCoupled oceanic oxygenation and metazoan diversification during the early–middle Cambrian?Late inception of a resiliently oxygenated upper oceanChanges in productivity and redox conditions in the Panthalassic Ocean during the latest PermianEnhanced nitrogen fixation in the immediate aftermath of the latest Permian marine mass extinctionAnomalous Early Triassic sediment fluxes due to elevated weathering rates and their biological consequencesNegative C-isotope excursions at the Permian-Triassic boundary linked to volcanism87Sr/86Sr stratigraphy from the Early Triassic of Zal, Iran: Linking temperature to weathering rates and the tempo of ecosystem recoveryEnvironmental analysis of paleoceanographic systems based on molybdenum–uranium covariationPaleodepositional conditions in the Orca Basin as inferred from organic matter and trace metal contentsTrace metals as paleoredox and paleoproductivity proxies: An updateOcean deoxygenation: Past, present, and futureA dolomitization event at the oceanic chemocline during the Permian-Triassic transitionSpatial variation in sediment fluxes, redox conditions, and productivity in the Permian–Triassic Panthalassic OceanEarly Triassic seawater sulfate drawdownMarine productivity changes during the end-Permian crisis and Early Triassic recoveryTotal organic carbon, organic phosphorus, and biogenic barium fluxes as proxies for paleomarine productivitySedimentary Corg:P ratios, paleocean ventilation, and Phanerozoic atmospheric pO2The silicon isotope composition ofEthmodiscus rexlaminated diatom mats from the tropical West Pacific: Implications for silicate cycling during the Last Glacial Maximum
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researcher ORCID ID = 0000-0002-3333-7035
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wetenschapper
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Thomas J Algeo
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Thomas J Algeo
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Thomas J. Algeo
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Thomas Algeo
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Thomas J Algeo
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Thomas J Algeo
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Thomas J. Algeo
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P31
P496
0000-0002-3333-7035