What is he best known for?
The fields of study he is best known for:
- Paleontology
- Ecology
- Oxygen
His scientific interests lie mostly in Carbonate, Anaerobic oxidation of methane, Geochemistry, Mineralogy and Authigenic.
His Carbonate study combines topics in areas such as Petroleum seep, Paleontology, Diagenesis and Cold seep.
Jörn Peckmann interconnects Environmental chemistry, Archaea and Carbon cycle in the investigation of issues within Anaerobic oxidation of methane.
Jörn Peckmann works in the field of Geochemistry, namely Pyrite.
His research in Mineralogy intersects with topics in Seawater, Organic matter, Archaeol and Clathrate hydrate.
His Authigenic study frequently intersects with other fields, such as Calcite.
His most cited work include:
- Microbial reefs in the Black Sea fueled by anaerobic oxidation of methane (598 citations)
- Carbon cycling at ancient methane-seeps (423 citations)
- Methane-derived carbonates and authigenic pyrite from the northwestern Black Sea (334 citations)
What are the main themes of his work throughout his whole career to date?
His primary scientific interests are in Geochemistry, Carbonate, Mineralogy, Authigenic and Paleontology.
His work in Geochemistry addresses issues such as Methane, which are connected to fields such as Carbon cycle.
The concepts of his Carbonate study are interwoven with issues in Anaerobic oxidation of methane, Cold seep, Diagenesis and Calcite.
His Anaerobic oxidation of methane research incorporates themes from Environmental chemistry, δ34S, Sulfate and Archaea.
In Mineralogy, Jörn Peckmann works on issues like Archaeol, which are connected to Methanogenesis.
His Authigenic research includes elements of Carbonate rock, Trace element and Clathrate hydrate.
He most often published in these fields:
- Geochemistry (48.98%)
- Carbonate (49.32%)
- Mineralogy (31.63%)
What were the highlights of his more recent work (between 2019-2021)?
- Geochemistry (48.98%)
- Methane (15.99%)
- Authigenic (30.27%)
In recent papers he was focusing on the following fields of study:
Jörn Peckmann spends much of his time researching Geochemistry, Methane, Authigenic, Carbonate and Sedimentary rock.
His Geochemistry study incorporates themes from Cretaceous, Petroleum seep, Clathrate hydrate, Chemosynthesis and Hydrocarbon.
His studies deal with areas such as Environmental chemistry, δ34S and Bacteria as well as Methane.
To a larger extent, Jörn Peckmann studies Diagenesis with the aim of understanding Authigenic.
His Carbonate research includes elements of Sulfate, Anaerobic oxidation of methane and Calcite.
His work carried out in the field of Anaerobic oxidation of methane brings together such families of science as Seawater, Sulfide and Fractionation, Isotope fractionation.
Between 2019 and 2021, his most popular works were:
- Trace elements in methane-seep carbonates: Potentials, limitations, and perspectives (9 citations)
- Suppressed competitive exclusion enabled the proliferation of Permian/Triassic boundary microbialites (8 citations)
- Carbon stable isotope patterns of cyclic terpenoids: A comparison of cultured alkaliphilic aerobic methanotrophic bacteria and methane-seep environments (4 citations)
In his most recent research, the most cited papers focused on:
- Paleontology
- Ecology
- Oxygen
His scientific interests lie mostly in Geochemistry, Sedimentary rock, Methane, Authigenic and Isotopes of carbon.
His Geochemistry research is multidisciplinary, relying on both Late Miocene, Aridification and Mediterranean climate, Mediterranean Basin.
Jörn Peckmann interconnects Chemosynthesis and Carbon in the investigation of issues within Methane.
His research on Authigenic is centered around Carbonate and Diagenesis.
His Carbonate research incorporates elements of Early Earth, Calcite, Hydrocarbon, Extreme environment and Brine.
His Isotopes of carbon research is multidisciplinary, incorporating elements of Methanotroph, δ13C, Archaea, Bacteria and Environmental chemistry.
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