2023 - Research.com Earth Science in United Kingdom Leader Award
His primary areas of study are Paleontology, Oceanography, Isotopes of carbon, Environmental chemistry and Organic matter. Richard D. Pancost has included themes like Sea surface temperature, TEX86 and Climate change in his Paleontology study. His Oceanography study combines topics from a wide range of disciplines, such as Sedimentary rock, Isotopes of oxygen and Diagenesis.
His Isotopes of carbon research is multidisciplinary, incorporating elements of Phytoplankton, Photic zone, Algae, Fractionation and Carbon cycle. His Environmental chemistry study combines topics in areas such as Ecology, Anaerobic oxidation of methane, Cold seep, Methane and Sediment. His Organic matter research incorporates elements of Peat, Soil water, Total organic carbon and Biogeochemical cycle.
His primary scientific interests are in Oceanography, Paleontology, Environmental chemistry, Organic matter and Ecology. Richard D. Pancost has researched Oceanography in several fields, including Sedimentary rock, Glacial period and Isotopes of carbon. His research on Paleontology often connects related topics like Sea surface temperature.
His Environmental chemistry research includes themes of Sediment, Mineralogy, Anaerobic oxidation of methane, Methane and Carbon. His Anaerobic oxidation of methane research includes elements of Archaea and Cold seep. In his study, which falls under the umbrella issue of Organic matter, Anoxic waters is strongly linked to Total organic carbon.
Paleontology, Oceanography, Geochemistry, Peat and Environmental chemistry are his primary areas of study. His work on Cretaceous, Sedimentary depositional environment and Biostratigraphy as part of general Paleontology research is often related to Cretaceous–Paleogene boundary and Term, thus linking different fields of science. His studies in Oceanography integrate themes in fields like Subtropics and Glacial period.
His work in Geochemistry addresses subjects such as Aptian, which are connected to disciplines such as Sediment. His study on Environmental chemistry also encompasses disciplines like
His scientific interests lie mostly in Peat, Paleontology, Paleogene, Environmental chemistry and Biogeochemical cycle. The concepts of his Peat study are interwoven with issues in Diagenesis, Atmospheric sciences, Holocene and Biogeochemistry. His work in Cretaceous, Cenozoic and Sedimentary depositional environment are all subfields of Paleontology research.
His biological study spans a wide range of topics, including Soil water, Organic matter, Hopanoids and Abundance. In his study, Climatology and Tropics is inextricably linked to Global warming, which falls within the broad field of Biogeochemical cycle. In his study, Oceanography is strongly linked to Carbon sequestration, which falls under the umbrella field of Total organic carbon.
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Quantifying the degradation of organic matter in marine sediments: A review and synthesis
Sandra Arndt;Sandra Arndt;Bo Barker Jørgensen;Douglas E. LaRowe;Jack Middelburg.
Earth-Science Reviews (2013)
Analysis of intact tetraether lipids in archaeal cell material and sediments by high performance liquid chromatography/atmospheric pressure chemical ionization mass spectrometry.
Ellen C. Hopmans;Stefan Schouten;Richard D. Pancost;Marcel T.J. van der Meer.
Rapid Communications in Mass Spectrometry (2000)
Alkenone and boron based Pliocene pCO2 records
Osamu Seki;Osamu Seki;Gavin L. Foster;Daniela N. Schmidt;Andreas Mackensen.
Earth and Planetary Science Letters (2010)
Consistent fractionation of 13C in nature and in the laboratory: growth-rate effects in some haptophyte algae.
Robert R. Bidigare;Arnim Fluegge;Arnim Fluegge;Katherine H. Freeman;Kristi L. Hanson.
Global Biogeochemical Cycles (1997)
Widespread occurrence of structurally diverse tetraether membrane lipids: Evidence for the ubiquitous presence of low-temperature relatives of hyperthermophiles
Stefan Schouten;Ellen C. Hopmans;Richard D. Pancost;Jaap S. Sinninghe Damsté.
Proceedings of the National Academy of Sciences of the United States of America (2000)
Stable warm tropical climate through the Eocene Epoch
Paul Nicholas Pearson;Bart E. van Dongen;Christopher J. Nicholas;Richard D. Pancost.
Two episodes of microbial change coupled with Permo/Triassic faunal mass extinction
Shucheng Xie;Richard D. Pancost;Hongfu Yin;Hongmei Wang.
Biomarker evidence for widespread anaerobic methane oxidation in Mediterranean sediments by a consortium of methanogenic archaea and bacteria
Richard D. Pancost;Jaap S. Sinninghe Damsté;Saskia de Lint;Marc J. E. C. van der Maarel.
Applied and Environmental Microbiology (2000)
CH 4 -consuming microorganisms and the formation of carbonate crusts at cold seeps
Giovanni Aloisi;Ioanna Bouloubassi;Sander K. Heijs;Richard D. Pancost.
Earth and Planetary Science Letters (2002)
Biomarkers as proxies for plant inputs to peats: an example from a sub-boreal ombrotrophic bog
Richard D Pancost;Marianne Baas;Bas van Geel;Jaap S Sinninghe Damsté.
Organic Geochemistry (2002)
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