What is he best known for?
The fields of study he is best known for:
- Paleontology
- Sedimentary rock
- Ecology
Matthew R. Saltzman spends much of his time researching Paleontology, Paleozoic, Isotopes of carbon, Excursion and Total organic carbon.
Matthew R. Saltzman conducts interdisciplinary study in the fields of Paleontology and Extinction event through his research.
His Paleozoic study integrates concerns from other disciplines, such as Productivity and Structural basin, Cenozoic, Mesozoic.
His biological study deals with issues like Carbon cycle, which deal with fields such as Dissolved organic carbon, Geochemistry, Diagenesis and Carbonate rock.
His Total organic carbon research includes themes of Proterozoic, Primary production, Total inorganic carbon and Paleoceanography.
His Laurentia course of study focuses on Glacial period and Gondwana, Katian and Tectonics.
His most cited work include:
- Geochemical evidence for widespread euxinia in the Later Cambrian ocean (261 citations)
- Long-lived glaciation in the Late Ordovician? Isotopic and sequence-stratigraphic evidence from western Laurentia (230 citations)
- Phosphorus, nitrogen, and the redox evolution of the Paleozoic oceans (220 citations)
What are the main themes of his work throughout his whole career to date?
Matthew R. Saltzman mainly focuses on Paleontology, Ordovician, Isotopes of carbon, Phanerozoic and Geochemistry.
His Paleontology research is multidisciplinary, relying on both Total organic carbon and Carbon cycle.
In general Ordovician study, his work on Laurentia often relates to the realm of Extinction event, thereby connecting several areas of interest.
His Isotopes of carbon research integrates issues from Ecosystem and Paleoceanography.
In his work, Apatite and Diagenesis is strongly intertwined with Seawater, which is a subfield of Geochemistry.
His work focuses on many connections between Conodont and other disciplines, such as Stratigraphy, that overlap with his field of interest in Stage and Isotopes of strontium.
He most often published in these fields:
- Paleontology (70.11%)
- Ordovician (39.08%)
- Isotopes of carbon (25.29%)
What were the highlights of his more recent work (between 2017-2021)?
- Geochemistry (16.09%)
- Ordovician (39.08%)
- Paleontology (70.11%)
In recent papers he was focusing on the following fields of study:
The scientist’s investigation covers issues in Geochemistry, Ordovician, Paleontology, Phanerozoic and Weathering.
His biological study spans a wide range of topics, including Seawater and Stratigraphy.
The various areas that he examines in his Stratigraphy study include Structural basin, Stage, Biostratigraphy, Baltica and Laurentia.
His Ordovician study combines topics from a wide range of disciplines, such as δ13C, Total organic carbon and Nutrient.
His work on Paleozoic as part of general Paleontology study is frequently linked to δ34S, bridging the gap between disciplines.
His Phanerozoic research incorporates elements of Late Devonian extinction, Pennsylvanian and Tetrapod.
Between 2017 and 2021, his most popular works were:
- Late inception of a resiliently oxygenated upper ocean. (67 citations)
- Phanerozoic pO2 and the early evolution of terrestrial animals. (34 citations)
- Evidence for local and global redox conditions at an Early Ordovician (Tremadocian) mass extinction (25 citations)
In his most recent research, the most cited papers focused on:
- Paleontology
- Sedimentary rock
- Ecology
Matthew R. Saltzman mainly investigates Paleontology, Paleozoic, Oceanography, δ34S and Ordovician.
His multidisciplinary approach integrates Paleontology and Insect flight in his work.
His work deals with themes such as Ice age, Glacial period, Pennsylvanian, Viséan and Tournaisian, which intersect with Paleozoic.
His studies in Oceanography integrate themes in fields like Organic matter and Carboniferous.
Δ34S combines with fields such as Water column, Extinction event, Environmental change, Baltica and Biostratigraphy in his investigation.
The concepts of his Ordovician study are interwoven with issues in Stratigraphy and Conodont.
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