What is he best known for?
The fields of study he is best known for:
- Sedimentary rock
- Paleontology
- Carbon dioxide
Harald Strauss spends much of his time researching Paleontology, Geochemistry, Seawater, Isotopes of carbon and Phanerozoic.
His Paleontology research is multidisciplinary, incorporating elements of Organic matter and Anoxic waters.
His research is interdisciplinary, bridging the disciplines of Sulfur cycle and Geochemistry.
His Seawater research incorporates themes from Petrology, δ34S, Geophysics and Mineralogy.
His Isotopes of carbon study combines topics in areas such as Total organic carbon, Organic geochemistry and Isotope fractionation.
His Phanerozoic research integrates issues from Calcite, Proterozoic and Paleozoic.
His most cited work include:
- 87Sr/86Sr, δ13C and δ18O evolution of Phanerozoic seawater (1768 citations)
- 87 Sr/ 86 Sr,δ 13 Candδ 18 Oevolution of Phanerozoic seawater (1491 citations)
- THE ABUNDANCE OF 13C IN MARINE ORGANIC MATTER AND ISOTOPIC FRACTIONATION IN THE GLOBAL BIOGEOCHEMICAL CYCLE OF CARBON DURING THE PAST 800 MA (570 citations)
What are the main themes of his work throughout his whole career to date?
His primary areas of study are Geochemistry, Paleontology, δ34S, Pyrite and Seawater.
His Geochemistry study integrates concerns from other disciplines, such as Sulfur cycle, Hydrothermal circulation and Mineralogy.
His research integrates issues of Total organic carbon and Isotopes of carbon in his study of Paleontology.
His study looks at the relationship between Pyrite and fields such as Anaerobic oxidation of methane, as well as how they intersect with chemical problems.
Seawater is closely attributed to Phanerozoic in his study.
His study in Proterozoic is interdisciplinary in nature, drawing from both Precambrian and Archean.
He most often published in these fields:
- Geochemistry (48.98%)
- Paleontology (20.41%)
- δ34S (18.78%)
What were the highlights of his more recent work (between 2017-2021)?
- Geochemistry (48.98%)
- δ34S (18.78%)
- Pyrite (17.55%)
In recent papers he was focusing on the following fields of study:
Geochemistry, δ34S, Pyrite, Hydrothermal circulation and Environmental chemistry are his primary areas of study.
His Geochemistry research includes themes of Seawater, Anhydrite and Oceanic crust.
His work in δ34S covers topics such as Analytical chemistry which are related to areas like Compound specific.
His Pyrite study combines topics from a wide range of disciplines, such as Anaerobic oxidation of methane and Electron microprobe.
His work on Anoxic waters as part of his general Environmental chemistry study is frequently connected to Human health, thereby bridging the divide between different branches of science.
His research investigates the link between Sulfur cycle and topics such as Organic matter that cross with problems in Sedimentary rock.
Between 2017 and 2021, his most popular works were:
- Contamination of heavy metals and isotopic tracing of Pb in surface and profile soils in a polluted farmland from a typical karst area in southern China. (30 citations)
- Multiple sulfur isotopic evidence for the origin of elemental sulfur in an iron-dominated gas hydrate-bearing sedimentary environment (14 citations)
- Contamination patterns in river water from rural Beijing: A hydrochemical and multiple stable isotope study. (11 citations)
In his most recent research, the most cited papers focused on:
- Sedimentary rock
- Carbon dioxide
- Paleontology
Harald Strauss mostly deals with Geochemistry, Pyrite, δ34S, Environmental chemistry and Aragonite.
His research in Geochemistry is mostly focused on Carbonatite.
His Pyrite research is multidisciplinary, incorporating perspectives in Kerogen and Electron microprobe.
His δ34S study incorporates themes from Catagenesis, Anaerobic oxidation of methane, Oil shale and Hydrogen sulfide.
Harald Strauss has researched Environmental chemistry in several fields, including Mineralogy and Arctica islandica.
His Aragonite research incorporates elements of Sulfur cycle, Organic matter and Diagenesis.
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.
