What is he best known for?
The fields of study he is best known for:
- Oceanography
- Ecology
- Organic chemistry
Hydrothermal circulation, Hydrothermal vent, Mineralogy, Oceanography and Seawater are his primary areas of study.
His Hydrothermal circulation research includes elements of Rift valley and Ridge.
The concepts of his Hydrothermal vent study are interwoven with issues in Deep sea and Seafloor spreading.
Mineralogy is often connected to Environmental chemistry in his work.
His research investigates the connection between Oceanography and topics such as Paleontology that intersect with problems in Petroleum seep.
His Seawater research is multidisciplinary, incorporating elements of Trace element, Particulates, Water column and Redox.
His most cited work include:
- Hf isotope ratio analysis using multi-collector inductively coupled plasma mass spectrometry: an evaluation of isobaric interference corrections (895 citations)
- Evolution and Biogeography of Deep-Sea Vent and Seep Invertebrates (430 citations)
- Deep, diverse and definitely different: unique attributes of the world's largest ecosystem (404 citations)
What are the main themes of his work throughout his whole career to date?
Christopher R. German mostly deals with Hydrothermal circulation, Oceanography, Hydrothermal vent, Mineralogy and Geochemistry.
The various areas that Christopher R. German examines in his Hydrothermal circulation study include Seawater, Seafloor spreading, Environmental chemistry and Mid-ocean ridge.
His Seawater research incorporates themes from Sediment and Dissolution.
His Oceanography study frequently draws connections between adjacent fields such as Ridge.
His Hydrothermal vent research incorporates elements of Ecology, Biogeography and Cold seep.
He focuses mostly in the field of Mineralogy, narrowing it down to matters related to Particulates and, in some cases, Manganese.
He most often published in these fields:
- Hydrothermal circulation (53.07%)
- Oceanography (36.40%)
- Hydrothermal vent (25.88%)
What were the highlights of his more recent work (between 2018-2021)?
- Hydrothermal circulation (53.07%)
- Oceanography (36.40%)
- Hydrothermal vent (25.88%)
In recent papers he was focusing on the following fields of study:
His main research concerns Hydrothermal circulation, Oceanography, Hydrothermal vent, Deep sea and Seafloor spreading.
Christopher R. German combines subjects such as Water column, Geochemistry, Bathymetry, Geomorphology and Volcanology with his study of Hydrothermal circulation.
Oceanography and Biogeochemical cycle are frequently intertwined in his study.
His Hydrothermal vent study combines topics in areas such as Environmental chemistry, Particulates and Vehicle dynamics, Aerospace engineering.
His biological study deals with issues like Seawater, which deal with fields such as Isotope fractionation.
The Deep sea study combines topics in areas such as Ocean science, Flux and Mineralogy, Pyrite.
Between 2018 and 2021, his most popular works were:
- The NASA Roadmap to Ocean Worlds (63 citations)
- Dynamic Biogeochemistry of the Particulate Sulfur Pool in a Buoyant Deep-Sea Hydrothermal Plume (5 citations)
- Scientific Challenges and Present Capabilities in Underwater Robotic Vehicle Design and Navigation for Oceanographic Exploration Under-Ice (4 citations)
In his most recent research, the most cited papers focused on:
- Ecology
- Oceanography
- Organic chemistry
The scientist’s investigation covers issues in Environmental chemistry, Hydrothermal circulation, Hydrothermal vent, Seawater and Particulates.
Environmental chemistry and Sedimentary rock are commonly linked in his work.
His Hydrothermal circulation research is multidisciplinary, relying on both Geochemistry, Seamount and Water column.
His Hydrothermal vent study typically links adjacent topics like Biogeochemistry.
His work deals with themes such as Deep sea, Biosphere, Sulfur, Methane and Abiotic component, which intersect with Biogeochemistry.
His Seawater research integrates issues from Authigenic, Sediment, Isotopic signature, Sedimentary depositional environment and Isotope fractionation.
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