What is he best known for?
The fields of study he is best known for:
- Paleontology
- Sedimentary rock
- Erosion
Steven G. Driese spends much of his time researching Paleosol, Paleontology, Geochemistry, Pedogenesis and Diagenesis.
Steven G. Driese interconnects Soil water, Vertisol and Paleoclimatology in the investigation of issues within Paleosol.
His studies link Dominance with Paleontology.
His research in Geochemistry is mostly concerned with Weathering.
Steven G. Driese combines subjects such as Vadose zone and Mineralogy with his study of Weathering.
As a part of the same scientific family, Steven G. Driese mostly works in the field of Pedogenesis, focusing on Precambrian and, on occasion, Proterozoic, Craton, Paleozoic and Petrography.
His most cited work include:
- Neoarchean paleoweathering of tonalite and metabasalt: Implications for reconstructions of 2.69Ga early terrestrial ecosystems and paleoatmospheric chemistry (105 citations)
- Paleopedologic and Paleohydrologic Records of Precipitation Seasonality from Early Pennsylvanian "Underclay" Paleosols, U.S.A. (77 citations)
- Distinguishing Climate in the Soil Record Using Chemical Trends in a Vertisol Climosequence from the Texas Coast Prairie, and Application to Interpreting Paleozoic Paleosols in the Appalachian Basin, U.S.A. (64 citations)
What are the main themes of his work throughout his whole career to date?
Steven G. Driese mainly investigates Paleontology, Paleosol, Geochemistry, Pedogenesis and Weathering.
His studies in Sedimentary depositional environment, Fluvial, Facies, Pleistocene and Sedimentary rock are all subfields of Paleontology research.
His research investigates the connection with Paleosol and areas like Vertisol which intersect with concerns in Hydrology.
His Geochemistry research includes elements of Holocene and Geomorphology.
His study in the field of Alluvium also crosses realms of Groundwater flow.
His work deals with themes such as Mineralogy, Isotopes of oxygen and Soil horizon, which intersect with Pedogenesis.
He most often published in these fields:
- Paleontology (37.95%)
- Paleosol (32.53%)
- Geochemistry (25.90%)
What were the highlights of his more recent work (between 2016-2021)?
- Paleosol (32.53%)
- Geochemistry (25.90%)
- Paleontology (37.95%)
In recent papers he was focusing on the following fields of study:
Paleosol, Geochemistry, Paleontology, Weathering and Paleoclimatology are his primary areas of study.
Steven G. Driese studied Paleosol and Pleistocene that intersect with Chronology and Holocene.
His research in Geochemistry intersects with topics in Pedogenesis and Proterozoic.
Steven G. Driese has researched Pedogenesis in several fields, including Tectonics, Dolomite and Carboniferous.
His research is interdisciplinary, bridging the disciplines of Tufa and Paleontology.
His work in the fields of Weathering, such as Saprolite, overlaps with other areas such as Regolith.
Between 2016 and 2021, his most popular works were:
- Reconstructing pH of Paleosols Using Geochemical Proxies (12 citations)
- The early miocene critical zone at karungu, western Kenya: An equatorial, open habitat with few primate remains (12 citations)
- Reconstruction of Late Pleistocene Paleoenvironments using bulk geochemistry of paleosols from the Lake Victoria Region (11 citations)
In his most recent research, the most cited papers focused on:
- Paleontology
- Sedimentary rock
- Erosion
His main research concerns Paleosol, Weathering, Geochemistry, Paleontology and Pleistocene.
His Paleosol research is multidisciplinary, incorporating perspectives in Siderite, Calcite and Dolomite.
The Weathering study combines topics in areas such as Environmental chemistry, Soil water, Nutrient and Great Oxygenation Event.
His study on Protolith, Metasomatism, Unconformity and Archean is often connected to Humid subtropical climate as part of broader study in Geochemistry.
His biological study spans a wide range of topics, including Tufa, National park and Ecosystem.
His Pleistocene research is multidisciplinary, incorporating perspectives in Chronology and Holocene.
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