2016 - Fellow of American Geophysical Union (AGU)
2006 - Fellow of the American Association for the Advancement of Science (AAAS)
Fellow of the Geological Society of America
His primary areas of study are Mineralogy, Geochemistry, Ecology, Diagenesis and Dolomite. His research integrates issues of Sedimentary rock, Sample and Analytical chemistry in his study of Mineralogy. His Geochemistry research is multidisciplinary, incorporating elements of Sea level and Meteorite.
His work deals with themes such as Water mass and δ18O, which intersect with Ecology. In his study, Abundance and Fractionation is inextricably linked to δ13C, which falls within the broad field of δ18O. His Diagenesis study is focused on Paleontology in general.
Peter K. Swart mainly focuses on Oceanography, Geochemistry, Mineralogy, Diagenesis and Paleontology. His study in Oceanography is interdisciplinary in nature, drawing from both Ecology and Precipitation. His Geochemistry study frequently links to related topics such as Dolomitization.
His study looks at the relationship between Mineralogy and topics such as Isotopes of carbon, which overlap with Chondrite. The concepts of his Diagenesis study are interwoven with issues in δ18O, Carbonate rock and Carbonate platform. He combines subjects such as Reef, Seawater and Environmental chemistry with his study of Coral.
Peter K. Swart mainly investigates Geochemistry, Diagenesis, Oceanography, Environmental chemistry and Seawater. His biological study spans a wide range of topics, including δ18O, Carbonate platform and Dolomitization. His research in Diagenesis intersects with topics in Carbonate rock and Neomorphism.
Oceanography is frequently linked to Ecology in his study. His Environmental chemistry study combines topics from a wide range of disciplines, such as Coral and Isotopes of carbon. His Dolomite research is classified as research in Mineralogy.
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Natal Homing in a Marine Fish Metapopulation
Simon R. Thorrold;Christopher Latkoczy;Peter K. Swart;Cynthia M. Jones.
Climate Change in Continental Isotopic Records
P. K. Swart;K. C. Lohmann;J. McKenzie;S. Savin.
Washington DC American Geophysical Union Geophysical Monograph Series (1993)
The geochemistry of carbonate diagenesis: The past, present and future
Peter K. Swart.
Carbon and oxygen isotope fractionation in scleractinian corals: a review
Peter K. Swart.
Earth-Science Reviews (1983)
Factors determining δ13C and δ18O fractionation in aragonitic otoliths of marine fish
Simon R. Thorrold;Steven E. Campana;Cynthia M. Jones;Peter K. Swart.
Geochimica et Cosmochimica Acta (1997)
Fractionation of the stable isotopes of oxygen and carbon in carbon dioxide during the reaction of calcite with phosphoric acid as a function of temperature and technique
P.K. Swart;S.J. Burns;J.J. Leder.
Chemical Geology: Isotope Geoscience Section (1991)
The nature of the δ13C of periplatform sediments: Implications for stratigraphy and the global carbon cycle
Peter K Swart;Gregor P Eberli.
Sedimentary Geology (2005)
Accurate classification of juvenile weakfish Cynoscion regalis to estuarine nursery areas based on chemical signatures in otoliths
Simon R. Thorrold;Cynthia M. Jones;Peter K. Swart;Timothy E. Targett.
Marine Ecology Progress Series (1998)
Questioning carbonate diagenetic paradigms: evidence from the Neogene of the Bahamas
L.A Melim;H Westphal;P.K Swart;G.P Eberli.
Marine Geology (2002)
New distribution coefficient for the incorporation of strontium into dolomite and its implications for the formation of ancient dolomites
Volker C. Vahrenkamp;Peter K. Swart.
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