What is he best known for?
The fields of study he is best known for:
- Paleontology
- Sedimentary rock
- Oceanography
Liao Chang mostly deals with Magnetite, Magnetotactic bacteria, Mineralogy, Magnetofossil and Greigite.
Liao Chang has included themes like Geochemistry and Carbonate in his Magnetite study.
He interconnects Paleomagnetism, Biogeochemical cycle and Anoxic waters in the investigation of issues within Magnetotactic bacteria.
While working on this project, Liao Chang studies both Mineralogy and Single domain.
His research investigates the connection between Greigite and topics such as Analytical chemistry that intersect with problems in Metallurgy and Crystallinity.
His work in the fields of Paleontology, such as Pleistocene and Sequence, intersects with other areas such as Plateau and Palynology.
His most cited work include:
- Magnetic properties of sedimentary greigite (Fe3S4): An update (249 citations)
- Characterization of hematite (α-Fe2O3), goethite (α-FeOOH), greigite (Fe3S4), and pyrrhotite (Fe7S8) using first-order reversal curve diagrams (135 citations)
- Searching for single domain magnetite in the “pseudo‐single‐domain” sedimentary haystack: Implications of biogenic magnetite preservation for sediment magnetism and relative paleointensity determinations (122 citations)
What are the main themes of his work throughout his whole career to date?
His primary scientific interests are in Magnetite, Mineralogy, Greigite, Paleontology and Magnetofossil.
In general Magnetite study, his work on Magnetotactic bacteria and Magnetosome often relates to the realm of Biogeosciences, thereby connecting several areas of interest.
The Magnetotactic bacteria study which covers Anoxic waters that intersects with Terrigenous sediment.
He has researched Mineralogy in several fields, including Paleomagnetism and Magnetic susceptibility.
His Paleomagnetism research is multidisciplinary, relying on both Sedimentary rock, Geochemistry and Mineral.
The concepts of his Paleontology study are interwoven with issues in Deep sea and Paleoclimatology.
He most often published in these fields:
- Magnetite (50.59%)
- Mineralogy (37.65%)
- Greigite (38.82%)
What were the highlights of his more recent work (between 2016-2020)?
- Geochemistry (24.71%)
- Magnetofossil (34.12%)
- Remanence (18.82%)
In recent papers he was focusing on the following fields of study:
His primary areas of investigation include Geochemistry, Magnetofossil, Remanence, Mineralogy and Magnetite.
His work deals with themes such as Paleomagnetism and Carbon isotope excursion, which intersect with Geochemistry.
In his study, which falls under the umbrella issue of Paleomagnetism, Magnetic nanoparticles, Geomorphology and Greigite is strongly linked to Sedimentary rock.
His study in Rock magnetism extends to Magnetofossil with its themes.
Mineralogy and Geophysics are commonly linked in his work.
His work focuses on many connections between Magnetosome and other disciplines, such as Grain size, that overlap with his field of interest in Magnetotactic bacteria.
Between 2016 and 2020, his most popular works were:
- Coupled microbial bloom and oxygenation decline recorded by magnetofossils during the Palaeocene–Eocene Thermal Maximum (25 citations)
- Continental-scale geographic change across Zealandia during Paleogene subduction initiation (21 citations)
- Remanence acquisition efficiency in biogenic and detrital magnetite and recording of geomagnetic paleointensity (18 citations)
In his most recent research, the most cited papers focused on:
- Paleontology
- Sedimentary rock
- Oceanography
Paleogene, Paleontology, Subduction, International Ocean Discovery Program and Sedimentary rock are his primary areas of study.
His Paleogene research includes themes of Deep sea, Trough, Sea level and Crust.
Liao Chang combines topics linked to Cenozoic with his work on Sea level.
The various areas that Liao Chang examines in his Cenozoic study include Global warming and Bottom water, Oceanography.
His research on Paleontology frequently links to adjacent areas such as Paleoclimatology.
His Sedimentary rock research integrates issues from Magnetite and Mineralogy.
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