2009 - Fellow of the American Association for the Advancement of Science (AAAS)
2006 - Fellow of American Geophysical Union (AGU)
His primary scientific interests are in Oceanography, Foraminifera, Upwelling, Sediment and Sediment trap. He combines subjects such as Glacial period and Total organic carbon with his study of Oceanography. His study on Pulleniatina obliquiloculata and Hastigerina pelagica is often connected to Dissolution and Comparison study as part of broader study in Foraminifera.
His study in Upwelling is interdisciplinary in nature, drawing from both Seasonality, Hydrography, δ18O and Globigerinoides. His Sediment study combines topics from a wide range of disciplines, such as Structural basin, Isotopes of nitrogen, Sedimentary rock, Biogeochemical cycle and Annual cycle. As part of the same scientific family, Robert C. Thunell usually focuses on Sediment trap, concentrating on Coccolith and intersecting with Bloom, Emiliania huxleyi and Coccolithophore.
Oceanography, Foraminifera, Structural basin, Environmental science and Upwelling are his primary areas of study. Robert C. Thunell has researched Oceanography in several fields, including Glacial period and Sediment. His Glacial period research is multidisciplinary, incorporating elements of Mediterranean climate and Holocene.
His research integrates issues of Paleontology and Paleoclimatology in his study of Foraminifera. The concepts of his Upwelling study are interwoven with issues in Phytoplankton, Coccolithophore, Thermocline, Sea surface temperature and Biogenic silica. His work deals with themes such as Environmental chemistry and Anoxic waters, which intersect with Water column.
Robert C. Thunell spends much of his time researching Oceanography, Environmental science, Foraminifera, Environmental chemistry and Structural basin. His research is interdisciplinary, bridging the disciplines of Glacial period and Oceanography. His research in Foraminifera intersects with topics in Geochemistry, Isotopes of carbon and Plankton.
His Environmental chemistry study also includes fields such as
Robert C. Thunell mostly deals with Oceanography, Environmental science, Foraminifera, Upwelling and Structural basin. His Oceanography research incorporates elements of Denitrification and Glacial period. His studies deal with areas such as Geochemistry, Paleoceanography and Ocean acidification as well as Foraminifera.
His Structural basin study integrates concerns from other disciplines, such as Trace element and Carbonate Ion. In his study, Water column is strongly linked to Globigerinoides, which falls under the umbrella field of Globigerina bulloides. His biological study spans a wide range of topics, including Phytoplankton and Dinoflagellate.
This overview was generated by a machine learning system which analysed the scientist’s body of work. If you have any feedback, you can contact us here.
Super ENSO and Global Climate Oscillations at Millennial Time Scales
Lowell Stott;Christopher Poulsen;Steve Lund;Robert Thunell.
Science (2002)
The nitrogen isotope biogeochemistry of sinking particles from the margin of the Eastern North Pacific
Mark A. Altabet;Cynthia Pilskaln;Robert Thunell;Carol Pride.
Deep-Sea Research Part I: Oceanographic Research Papers (1999)
Decline of surface temperature and salinity in the western tropical Pacific Ocean in the Holocene epoch
Lowell Stott;Kevin Cannariato;Robert Thunell;Gerald H. Haug.
Nature (2004)
Magnitude and timing of temperature change in the Indo-Pacific warm pool during deglaciation
Katherine Visser;Robert Thunell;Lowell Stott.
Nature (2003)
The importance of continental margins in the global carbon cycle
Frank E. Muller‐Karger;Ramon Varela;Robert Thunell;Remy Luerssen.
Geophysical Research Letters (2005)
Chronology of the pleistocene oxygen isotope record: 0–1.88 m.y. B.P
Douglas F. Williams;Robert C. Thunell;Eric Tappa;Domenico Rio.
Palaeogeography, Palaeoclimatology, Palaeoecology (1988)
Sedimentation of planktonic foraminifera; seasonal changes in species flux in the Panama Basin
Robert C. Thunell;Leslie A. Reynolds.
Micropaleontology (1984)
Chemoautotrophy in the redox transition zone of the Cariaco Basin: A significant midwater source of organic carbon production
Gordon T. Taylor;Maria Iabichella;Tung-Yuan Ho;Mary I. Scranton.
Limnology and Oceanography (2001)
Southern Hemisphere and deep-sea warming led deglacial atmospheric CO2 rise and tropical warming.
Lowell Stott;Axel Timmermann;Robert Thunell.
Science (2007)
Global Increase in Quaternary Explosive Volcanism
James P. Kennett;Robert C. Thunell.
Science (1975)
If you think any of the details on this page are incorrect, let us know.
We appreciate your kind effort to assist us to improve this page, it would be helpful providing us with as much detail as possible in the text box below:
University of South Florida
University of South Carolina
University of Southern California
Stony Brook University
McGill University
University of South Carolina
University of Oxford
Oregon State University
Autonomous University of Barcelona
University of Miami
University of South Florida
King Abdullah University of Science and Technology
University of Bologna
Rutgers, The State University of New Jersey
University of Montana
Henan Normal University
ETH Zurich
MIT
Dalhousie University
ETH Zurich
Stockholm University
United States Geological Survey
University of Bonn
Yale University
Cleveland Clinic
University of London