What is he best known for?
The fields of study he is best known for:
- Climate change
- Carbon dioxide
- Ecosystem
His primary areas of study are Weathering, Geochemistry, Earth science, Phanerozoic and Glacial period.
His Weathering research incorporates themes from Watershed, Total organic carbon, Oceanography, Biogeochemistry and Carbon dioxide.
As part of his studies on Geochemistry, Yves Goddéris often connects relevant subjects like Carbon cycle.
The concepts of his Earth science study are interwoven with issues in Global warming, Basalt and Arctic.
Yves Goddéris interconnects Seawater and Isotopes of oxygen in the investigation of issues within Phanerozoic.
His Glacial period research focuses on Carbon dioxide in Earth's atmosphere and how it connects with Paleoclimatology, Proterozoic, Paleoatmosphere, Precambrian and Aragonite.
His most cited work include:
- 87Sr/86Sr, δ13C and δ18O evolution of Phanerozoic seawater (1768 citations)
- 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)
What are the main themes of his work throughout his whole career to date?
His primary scientific interests are in Weathering, Earth science, Paleontology, Geochemistry and Carbon cycle.
His study on Weathering also encompasses disciplines like
- Erosion which intersects with area such as Bedrock,
- Ecosystem most often made with reference to Atmospheric sciences.
His Earth science study combines topics from a wide range of disciplines, such as Snowball Earth, Glacial period, Climate model, Basalt and Oceanography.
Yves Goddéris works mostly in the field of Geochemistry, limiting it down to topics relating to Isotopes of carbon and, in certain cases, Biogeochemical cycle.
His Phanerozoic research is multidisciplinary, incorporating perspectives in Continental drift, Trace element, Mineralogy and Isotopes of oxygen.
Yves Goddéris merges Paleozoic with δ18O in his study.
He most often published in these fields:
- Weathering (36.65%)
- Earth science (35.40%)
- Paleontology (21.12%)
What were the highlights of his more recent work (between 2015-2021)?
- Earth science (35.40%)
- Weathering (36.65%)
- Geochemistry (19.88%)
In recent papers he was focusing on the following fields of study:
His main research concerns Earth science, Weathering, Geochemistry, Paleontology and Phanerozoic.
His Earth science study integrates concerns from other disciplines, such as Glacial period, Paleozoic, Climate change, Carbon sink and Plate tectonics.
His Paleozoic research is multidisciplinary, incorporating elements of Ice age, Biosphere, Biogeochemistry and Geologic record.
The study incorporates disciplines such as Geochemical modeling, Oil shale, Erosion and Quaternary in addition to Weathering.
Yves Goddéris is interested in Volcano, which is a branch of Geochemistry.
The various areas that he examines in his Phanerozoic study include Continental drift, Ordovician and Colonization.
Between 2015 and 2021, his most popular works were:
- Onset and ending of the late Palaeozoic ice age triggered by tectonically paced rock weathering (58 citations)
- Paleogeographic forcing of the strontium isotopic cycle in the Neoproterozoic (24 citations)
- Reconstructing first-order changes in sea level during the Phanerozoic and Neoproterozoic using strontium isotopes (23 citations)
In his most recent research, the most cited papers focused on:
- Climate change
- Carbon dioxide
- Ecosystem
Yves Goddéris focuses on Paleontology, Weathering, Earth science, Climate change and Erosion.
His study in Paleontology is interdisciplinary in nature, drawing from both Geochemistry and Ocean surface topography.
His Geochemistry study incorporates themes from Glacial period, Rodinia and Phanerozoic.
His Phanerozoic research integrates issues from Volcano, Transition zone and Isotopes of carbon.
In his study, which falls under the umbrella issue of Weathering, Ice age is strongly linked to Carbon cycle.
His biological study spans a wide range of topics, including Mantle convection and Carbon sink.
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