2023 - Research.com Earth Science in Switzerland Leader Award
His scientific interests lie mostly in Environmental chemistry, Isotopes of oxygen, Mineralogy, Sulfur and Isotope fractionation. His studies in Environmental chemistry integrate themes in fields like Organic matter, Soil water, Water column, Hydrology and Nitrate. His research integrates issues of δ18O, Carbonate, Mineralization and Analytical chemistry in his study of Mineralogy.
He has researched Sulfur in several fields, including Sulfide and Sulfate. In his study, Carbon, Sulfate transport, δ34S, Aptian and Cretaceous is inextricably linked to Anoxic waters, which falls within the broad field of Isotope fractionation. His work carried out in the field of Geochemistry brings together such families of science as Seawater and Paleontology.
Stefano M. Bernasconi spends much of his time researching Geochemistry, Oceanography, Environmental chemistry, Paleontology and Mineralogy. His Geochemistry research includes elements of Carbonate and Hydrothermal circulation. Stefano M. Bernasconi combines subjects such as Glacial period and Mediterranean sea with his study of Oceanography.
His research in Environmental chemistry intersects with topics in Isotopes of oxygen, Oxygen, Sulfate and Sulfur. His work is dedicated to discovering how Paleontology, Isotopes of carbon are connected with Organic matter and other disciplines. The concepts of his Mineralogy study are interwoven with issues in Sediment and Table.
Stefano M. Bernasconi focuses on Geochemistry, Carbonate, Oceanography, Mineralogy and Calcite. His Carbonate course of study focuses on Isotopes of oxygen and Siderite. Oceanography is closely attributed to δ18O in his work.
His study on Mineralogy also encompasses disciplines like
Stefano M. Bernasconi mostly deals with Carbonate, Fractionation, Geochemistry, Mineralogy and Calcite. His Carbonate study incorporates themes from Earth science and Isotope fractionation. His Fractionation study integrates concerns from other disciplines, such as Isotopes of carbon, Mass spectrometry, Acid digestion, Analytical chemistry and Calibration.
His Geochemistry research also works with subjects such as
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A Serpentinite-Hosted Ecosystem: The Lost City Hydrothermal Field
Deborah S. Kelley;Jeffrey A. Karson;Gretchen L. Früh-Green;Dana R. Yoerger.
Science (2005)
Preservation of organic matter and alteration of its carbon and nitrogen isotope composition during simulated and in situ early sedimentary diagenesis
Moritz F Lehmann;Stefano M Bernasconi;Alberto Barbieri;Judith A McKenzie.
Geochimica et Cosmochimica Acta (2002)
Microbial mediation as a possible mechanism for natural dolomite formation at low temperatures
Crisogono Vasconcelos;Judith A. McKenzie;Stefano Bernasconi;Djordje Grujic.
Nature (1995)
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 ratios
Kay-Christian Emeis;Ulrich Struck;Hans-Martin Schulz;Reinhild Rosenberg.
Palaeogeography, Palaeoclimatology, Palaeoecology (2000)
A revised isotope fractionation model for dissimilatory sulfate reduction in sulfate reducing bacteria
Benjamin Brunner;Stefano M. Bernasconi.
Geochimica et Cosmochimica Acta (2005)
30,000 Years of Hydrothermal Activity at the Lost City Vent Field
Gretchen L. Früh-Green;Deborah S. Kelley;Stefano M. Bernasconi;Jeffrey A. Karson.
Science (2003)
Calibration of the δ18O paleothermometer for dolomite precipitated in microbial cultures and natural environments
Crisogono Vasconcelos;Judith A. McKenzie;Rolf Warthmann;Stefano M. Bernasconi.
Geology (2005)
The record of nitrate utilization and productivity limitation provided by δ15N values in lake organic matter—A study of sediment trap and core sediments from Baldeggersee, Switzerland
Jane L. Teranes;Stefano M. Bernasconi.
Limnology and Oceanography (2000)
Dolomite formation within microbial mats in the coastal sabkha of Abu Dhabi (United Arab Emirates)
Tomaso R. R. Bontognali;Crisógono Vasconcelos;Rolf J. Warthmann;Stefano M. Bernasconi.
Sedimentology (2010)
Hypersulfidic deep biosphere indicates extreme sulfur isotope fractionation during single-step microbial sulfate reduction
Ulrich G. Wortmann;Stefano M. Bernasconi;Michael E. Böttcher.
Geology (2001)
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