What is he best known for?
The fields of study he is best known for:
- Carbon dioxide
- Ecology
- Redox
John W. Morse focuses on Mineralogy, Calcium carbonate, Calcite, Environmental chemistry and Pyrite.
His Calcium carbonate research includes elements of Sedimentary rock, Geochemistry and Diagenesis.
His Carbonate rock and Carbonate minerals study, which is part of a larger body of work in Geochemistry, is frequently linked to Mineral paragenesis, bridging the gap between disciplines.
His Calcite research is multidisciplinary, incorporating perspectives in Seawater and Analytical chemistry.
His research in Pyrite intersects with topics in Iron sulfide and Anoxic waters.
His research investigates the connection with Anoxic waters and areas like Inorganic chemistry which intersect with concerns in Isotopes of oxygen and Dissolved organic carbon.
His most cited work include:
- Carbon isotopic fractionation in synthetic aragonite and calcite: Effects of temperature and precipitation rate (917 citations)
- Geochemistry of Sedimentary Carbonates (907 citations)
- Pyritization of trace metals in anoxic marine sediments (655 citations)
What are the main themes of his work throughout his whole career to date?
John W. Morse mainly focuses on Mineralogy, Calcite, Environmental chemistry, Inorganic chemistry and Calcium carbonate.
His studies deal with areas such as Sedimentary rock and Table as well as Mineralogy.
John W. Morse works mostly in the field of Calcite, limiting it down to topics relating to Seawater and, in certain cases, Salinity.
His Environmental chemistry research incorporates themes from Estuary, Sediment and Pyrite.
His Inorganic chemistry study which covers Mackinawite that intersects with Greigite.
The Calcium carbonate study combines topics in areas such as Geochemistry and Dissolution.
He most often published in these fields:
- Mineralogy (31.54%)
- Calcite (30.77%)
- Environmental chemistry (23.85%)
What were the highlights of his more recent work (between 2005-2015)?
- Oceanography (17.69%)
- Sediment (18.46%)
- Calcite (30.77%)
In recent papers he was focusing on the following fields of study:
His main research concerns Oceanography, Sediment, Calcite, Dissolution and Benthic zone.
His Benthos and Seawater study in the realm of Oceanography interacts with subjects such as Technical report.
His research on Sediment also deals with topics like
- Total organic carbon which connect with Microcosm,
- Diagenesis which connect with Dolomite and Carbonate rock.
His Calcite study is concerned with Mineralogy in general.
His research in Dissolution tackles topics such as Calcium carbonate which are related to areas like Total inorganic carbon.
His work deals with themes such as Geochemistry and Anoxic waters, which intersect with Benthic zone.
Between 2005 and 2015, his most popular works were:
- Calcium Carbonate Formation and Dissolution (637 citations)
- Initial responses of carbonate-rich shelf sediments to rising atmospheric pCO2 and “ocean acidification”: Role of high Mg-calcites (227 citations)
- Calcite dissolution kinetics in Na–Ca–Mg–Cl brines (78 citations)
In his most recent research, the most cited papers focused on:
- Carbon dioxide
- Ecology
- Redox
His primary areas of study are Inorganic chemistry, Dissolution, Hypoxia, Calcite and Mineralogy.
His research integrates issues of Calcium carbonate, Reaction rate constant and Hydrogen sulfide in his study of Inorganic chemistry.
His work carried out in the field of Dissolution brings together such families of science as Seawater, Ocean acidification, Carbon dioxide in Earth's atmosphere and Aragonite.
His Calcite research incorporates themes from Dolomite and Diagenesis.
His research in Mineralogy is mostly concerned with Carbonate minerals.
The concepts of his Sediment–water interface study are interwoven with issues in Environmental chemistry, Estuary, Bay and Hydrology.
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