about
The discovery of new deep-sea hydrothermal vent communities in the southern ocean and implications for biogeography.Holocene variations in peatland methane cycling associated with the Asian summer monsoon systemWarm climates of the past--a lesson for the future?Archaeol: an indicator of methanogenesis in water-saturated soilsThe organic preservation of fossil arthropods: an experimental studyUncertainty as knowledgeLipid biomolecules in silica sinters: indicators of microbial biodiversity.Two episodes of microbial change coupled with Permo/Triassic faunal mass extinction.Biogeochemistry and biodiversity of methane cycling in subsurface marine sediments (Skagerrak, Denmark).Functional diversity of bacteria in a ferruginous hydrothermal sediment.Biogeochemical controls on microbial diversity in seafloor sulphidic sediments.Lipid biomarkers and carbon isotope signatures of a microbial (Beggiatoa) mat associated with gas hydrates in the gulf of Mexico.Carbon and chlorine isotope fractionation during microbial degradation of tetra- and trichloroethene.Temperature and pH control on lipid composition of silica sinters from diverse hot springs in the Taupo Volcanic Zone, New Zealand.Plio-Pleistocene climate sensitivity evaluated using high-resolution CO2 records.Arsenic release and attenuation in low organic carbon aquifer sediments from West Bengal.Microbial ecology of arsenic-mobilizing Cambodian sediments: lithological controls uncovered by stable-isotope probing.Source Apportionment of Polycyclic Aromatic Hydrocarbons in Central European Soils with Compound-Specific Triple Isotopes (δ(13)C, Δ(14)C, and δ(2)H).Dual carbon-chlorine stable isotope investigation of sources and fate of chlorinated ethenes in contaminated groundwater.Changing atmospheric CO2 concentration was the primary driver of early Cenozoic climate.High-resolution alkenone palaeobarometry indicates relatively stable pCO(2) during the Pliocene (3.3-2.8 Ma).Biogeochemistry: Ancient algae crossed a threshold.Increased terrestrial methane cycling at the Palaeocene-Eocene thermal maximum.Paleoceanographic changes in the Eastern Equatorial Pacific over the last 10 MyrAlkenone and boron-based Pliocene pCO2 recordsResponse of carbon cycle to drier conditions in the mid-Holocene in central China.Further insights into how sediment redox status controls the preservation and composition of sedimentary biomarkersSignature of organic matter exported from naturally Fe-fertilised oceanic watersQuantifying export production in the Southern Ocean: Implications for the BaxsproxyProductivity variation around the Crozet Plateau: A naturally iron fertilised area of the Southern OceanAlgal biomarkers in surface waters around the Crozet plateauEarly Paleogene temperature history of the Southwest Pacific Ocean: Reconciling proxies and modelsStable warm tropical climate through the Eocene EpochThe archaeal lipid composition of partially lithified cold seep matsFormation of iron sulfide nodules during anaerobic oxidation of methaneCorrelations between microbial tetraether lipids and environmental variables in Chinese soils: Optimizing the paleo-reconstructions in semi-arid and arid regionsDynamics of sediment flux to a bathyal continental margin section through the Paleocene–Eocene Thermal MaximumOrbital forcing of terrestrial hydrology, weathering and carbon sequestration during the Palaeocene-Eocene Thermal MaximumOrigin of light volatile hydrocarbon gases in mud volcano fluids, Gulf of Cadiz — Evidence for multiple sources and transport mechanisms in active sedimentary wedgesEarly Paleogene evolution of terrestrial climate in the SW Pacific, Southern New Zealand
P50
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P50
description
geochemicus
@nl
geochemist
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name
Richard D Pancost
@es
Richard D Pancost
@nl
Richard D Pancost
@sl
Richard D. Pancost
@en
Richard D. Pancost
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type
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Richard D Pancost
@es
Richard D Pancost
@nl
Richard D Pancost
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Richard D. Pancost
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Richard D. Pancost
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Richard Pancost
@en
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Richard D Pancost
@es
Richard D Pancost
@nl
Richard D Pancost
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Richard D. Pancost
@en
Richard D. Pancost
@sq
P21
P31
P496
0000-0003-0298-4026