What is he best known for?
The fields of study he is best known for:
- Sediment
- Sedimentary rock
- Paleontology
Christian Ohlendorf mainly investigates Holocene, Sediment, Maar, Glacial period and Physical geography.
His Holocene study integrates concerns from other disciplines, such as Sedimentary rock, Geochemistry, Sedimentology and Geomorphology.
His study in Sediment is interdisciplinary in nature, drawing from both Steppe, Pollen and Vegetation.
His biological study spans a wide range of topics, including Oceanography and Climate change.
Christian Ohlendorf has included themes like Paleoclimatology, Varve, Quaternary, Glacier and Snow in his Glacial period study.
His Physical geography study combines topics from a wide range of disciplines, such as Hydrology and Northern Hemisphere.
His most cited work include:
- 9000 years of geochemical evolution of lithogenic major and trace elements in the sediment of an alpine lake – the role of climate, vegetation, and land-use history (211 citations)
- Climatically induced lake level changes during the last two millennia as reflected in sediments of Laguna Potrok Aike, southern Patagonia (Santa Cruz, Argentina) (160 citations)
- Lateglacial and Holocene wet-dry cycles in southern Patagonia: chronology, sedimentology and geochemistry of a lacustrine record from Laguna Potrok Aike, Argentina (132 citations)
What are the main themes of his work throughout his whole career to date?
Christian Ohlendorf spends much of his time researching Sediment, Geochemistry, Maar, Holocene and Geomorphology.
His studies in Sediment integrate themes in fields like Sedimentology, Mineralogy, Physical geography, Sedimentary depositional environment and Erosion.
His Geochemistry research is multidisciplinary, relying on both Marine isotope stage and Sediment core.
The various areas that he examines in his Maar study include Glacial period, Tephra and Oceanography.
His research on Holocene also deals with topics like
- Westerlies which is related to area like Deglaciation,
- Isotopes of oxygen, which have a strong connection to δ18O.
His work investigates the relationship between Geomorphology and topics such as Volcano that intersect with problems in Ice core.
He most often published in these fields:
- Sediment (35.53%)
- Geochemistry (24.34%)
- Maar (19.74%)
What were the highlights of his more recent work (between 2017-2020)?
- Geochemistry (24.34%)
- Sediment (35.53%)
- Glacial period (17.76%)
In recent papers he was focusing on the following fields of study:
Geochemistry, Sediment, Glacial period, Radiocarbon dating and Paleoclimatology are his primary areas of study.
His Geochemistry research is multidisciplinary, incorporating elements of Marine isotope stage and Pollen.
His study with Sediment involves better knowledge in Paleontology.
His Glacial period study integrates concerns from other disciplines, such as Outcrop, Mineralogy and Weathering.
The concepts of his Radiocarbon dating study are interwoven with issues in Pleistocene and Holocene.
His research integrates issues of Ice core and Last Glacial Maximum in his study of Paleoclimatology.
Between 2017 and 2020, his most popular works were:
- Practical guidelines and recent advances in the Itrax XRF core-scanning procedure. (14 citations)
- Paleoenvironmental conditions and sedimentation dynamics in Central Europe inferred from geochemical data of the loess-paleosol sequence at Süttő (Hungary) (10 citations)
- A sample carrier for measuring discrete powdered samples with an ITRAX XRF core scanner (9 citations)
In his most recent research, the most cited papers focused on:
- Sedimentary rock
- Erosion
- Sediment
Christian Ohlendorf focuses on Mineralogy, Loess, Paleosol, Glacial period and Chemostratigraphy.
His Mineralogy research includes themes of Sample and Elemental composition, Analytical chemistry.
His Loess research incorporates elements of Pedogenesis, Outcrop, Provenance, Interglacial and Weathering.
His Provenance study improves the overall literature in Geochemistry.
His research on Paleosol often connects related areas such as Sediment.
His Glacial period research includes elements of Ice core and Paleoclimatology.
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