about
Clay mineral continental amplifier for marine carbon sequestration in a greenhouse ocean.Isotopic evidence for glaciation during the Cretaceous supergreenhouse.Atlantic cooling associated with a marine biotic crisis during the mid-Cretaceous periodMolybdenum drawdown during Cretaceous Oceanic Anoxic Event 2Repeated enrichment of trace metals and organic carbon on an Eocene high-energy shelf caused by anoxia and reworkingA continental-weathering control on orbitally driven redox-nutrient cycling during Cretaceous Oceanic Anoxic Event 2Phosphorus burial and diagenesis in the central Bering Sea (Bowers Ridge, IODP Site U1341): Perspectives on the marine P cycleClimate-controlled variability of iron deposition in the Central Arctic Ocean (southern Mendeleev Ridge) over the last 130,000yearsRedox sensitivity of P cycling during marine black shale formation: Dynamics of sulfidic and anoxic, non-sulfidic bottom watersEvolution of tropical watersheds and continental hydrology during the Late Cretaceous greenhouse; impact on marine carbon burial and possible implications for the futureGeochemical environment of the Coniacian–Santonian western tropical Atlantic at Demerara RiseImproved end-member characterisation of modern organic matter pools in the Ohrid Basin (Albania, Macedonia) and evaluation of new palaeoenvironmental proxiesCretaceous sea-surface temperature evolution: Constraints from TEX 86 and planktonic foraminiferal oxygen isotopesCyclic changes in Turonian to Coniacian planktic foraminiferal assemblages from the tropical Atlantic OceanMechanistic controls on diverse fates of terrestrial organic components in the East China SeaMultiple sources and extensive degradation of terrestrial sedimentary organic matter across an energetic, wide continental shelfCharacterizing the depositional settings for sedimentary organic matter distributions in the Lower Yangtze River-East China Sea Shelf SystemSources and distributions of tetraether lipids in surface sediments across a large river-dominated continental marginThe dispersal of sedimentary terrestrial organic matter in the East China Sea (ECS) as revealed by biomarkers and hydro-chemical characteristicsRapid warming and salinity changes of Cretaceous surface waters in the subtropical North AtlanticCretaceous separation of Africa and South America: the view from the West African margin (ODP Leg 159)Methane seepage in a Cretaceous greenhouse world recorded by an unusual carbonate deposit from the Tarfaya Basin, MoroccoIdentifying biogenic silica: Mudrock micro-fabric explored through charge contrast imagingBacteriohopanepolyols in tropical soils and sediments from the Congo River catchment areaVariability in aerobic methane oxidation over the past 1.2Myrs recorded in microbial biomarker signatures from Congo fan sedimentsHadley circulation and precipitation changes controlling black shale deposition in the Late Jurassic Boreal SeawayClimate–ocean coupling off North-West Africa during the Lower Albian: The Oceanic Anoxic Event 1bEuxinia and primary production in Late Cretaceous eastern equatorial Atlantic surface waters fostered orbitally driven formation of marine black shalesCorrection to “Euxinia and primary production in Late Cretaceous eastern equatorial Atlantic surface waters fostered orbitally driven formation of marine black shales”The New 14C Analysis Laboratory in Jena, GermanyImprovements of the Jena AMS system
P50
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P50
description
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Thomas Wagner
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Thomas Wagner
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Thomas Wagner
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Thomas Wagner
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Thomas Wagner
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Thomas Wagner
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Thomas Wagner
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Thomas Wagner
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Thomas Wagner
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Thomas Wagner
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Thomas Wagner
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Thomas Wagner
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Thomas Wagner
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Thomas Wagner
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Thomas Wagner
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Thomas Wagner
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P106
P21
P31
P496
0000-0001-5006-625X