about
Characterization, Quantification and Compound-specific Isotopic Analysis of Pyrogenic Carbon Using Benzene Polycarboxylic Acids (BPCA)A serpentinite-hosted ecosystem: the Lost City hydrothermal field.Activity and diversity of sulfate-reducing bacteria in a petroleum hydrocarbon-contaminated aquifer.Bacterial, archaeal and fungal succession in the forefield of a receding glacier.30,000 years of hydrothermal activity at the lost city vent field.Microbial diversity of Loki's Castle black smokers at the Arctic Mid-Ocean Ridge.Biomarker evidence for a major preservation pathway of sedimentary organic carbon.Biosignatures in chimney structures and sediment from the Loki's Castle low-temperature hydrothermal vent field at the Arctic Mid-Ocean Ridge.Characterization of multiple-substrate utilization by anthracene-degrading Mycobacterium frederiksbergense LB501T.A dual isotopic approach using radioactive phosphorus and the isotopic composition of oxygen associated to phosphorus to understand plant reaction to a change in P nutritionAn automated method for 'clumped-isotope' measurements on small carbonate samples.The reversibility of dissimilatory sulphate reduction and the cell-internal multi-step reduction of sulphite to sulphide: insights from the oxygen isotope composition of sulphate.Use of isotopic and molecular techniques to link toluene degradation in denitrifying aquifer microcosms to specific microbial populations.Hydrogen and carbon isotope fractionation during aerobic biodegradation of benzene.Long-term performance of the Kiel carbonate device with a new correction scheme for clumped isotope measurements.PALEOCEANOGRAPHY. A warm and poorly ventilated deep Arctic Mediterranean during the last glacial period.Influence of the growth substrate on ester-linked phospho- and glycolipid fatty acids of PAH-degrading Mycobacterium sp. LB501T.Efficiency of monolaurin in mitigating ruminal methanogenesis and modifying C-isotope fractionation when incubating diets composed of either C3 or C4 plants in a rumen simulation technique (Rusitec) system.18O enrichment in phosphorus pools extracted from soybean leaves.SoilTrEC: a global initiative on critical zone research and integration.Penultimate deglacial warming across the Mediterranean Sea revealed by clumped isotopes in foraminifera.Carbonate clumped isotope analyses with the long-integration dual-inlet (LIDI) workflow: scratching at the lower sample weight boundaries.Deeply-sourced formate fuels sulfate reducers but not methanogens at Lost City hydrothermal field.Global change: an Earth on fire.A simple method for the removal of dissolved organic matter and δ15N analysis of NO3(-) from freshwater.Temperature and salinity variations of Mediterranean Sea surface waters over the last 16,000 years from records of planktonic stable oxygen isotopes and alkenone unsaturation ratiosNitrogen retention and transport differ by hillslope aspect at the rain-snow transition of the Colorado Front RangeA model for oxygen and sulfur isotope fractionation in sulfate during bacterial sulfate reduction processesA revised isotope fractionation model for dissimilatory sulfate reduction in sulfate reducing bacteriaGiant lacustrine pockmarks with subaqueous groundwater discharge and subsurface sediment mobilizationSoil processes and functions across an international network of Critical Zone Observatories: Introduction to experimental methods and initial resultsSoil Processes and Functions in Critical Zone Observatories: Hypotheses and Experimental DesignChemical and Biological Gradients along the Damma Glacier Soil Chronosequence, SwitzerlandHydrological control of stream water chemistry in a glacial catchment (Damma Glacier, Switzerland)New methods for the environmental chemist’s toolboxStable isotope analysis of macroinvertebrates and their food sources in a glacier streamPurification of fire derived markers for μg scale isotope analysis (δ13C, Δ14C) using high performance liquid chromatography (HPLC)Genesis of folia in a non-thermal epigenic cave (Matanzas, Cuba)Source and genesis of sulphate and phosphate-sulphate minerals in a quartz-sandstone cave environmentThe role of serpentinites in cycling of carbon and sulfur: Seafloor serpentinization and subduction metamorphism
P50
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P50
description
hulumtues
@sq
onderzoeker
@nl
researcher
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հետազոտող
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name
Stefano M. Bernasconi
@ast
Stefano M. Bernasconi
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Stefano M. Bernasconi
@es
Stefano M. Bernasconi
@nl
Stefano M. Bernasconi
@sl
type
label
Stefano M. Bernasconi
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Stefano M. Bernasconi
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Stefano M. Bernasconi
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Stefano M. Bernasconi
@nl
Stefano M. Bernasconi
@sl
prefLabel
Stefano M. Bernasconi
@ast
Stefano M. Bernasconi
@en
Stefano M. Bernasconi
@es
Stefano M. Bernasconi
@nl
Stefano M. Bernasconi
@sl
P1053
E-5394-2010
P106
P108
P1153
57191830195
7102680456
P21
P2798
P31
P3829
P3835
stefano-bernasconi2
P496
0000-0001-7672-8856