Denis Scholz mainly investigates Stalagmite, Mineralogy, Speleothem, Calcite and δ18O. His study with Stalagmite involves better knowledge in Cave. As a part of the same scientific family, Denis Scholz mostly works in the field of Cave, focusing on Holocene and, on occasion, North Atlantic oscillation, Interglacial, Physical geography and Quaternary.
While the research belongs to areas of Mineralogy, Denis Scholz spends his time largely on the problem of Inductively coupled plasma mass spectrometry, intersecting his research to questions surrounding Silicate glass, Mc icp ms and Homogeneity. His study looks at the relationship between Speleothem and topics such as Hydrology, which overlap with Isotope fractionation. His work investigates the relationship between Calcite and topics such as Fractionation that intersect with problems in Analytical chemistry, Soil science, Microanalysis and Secular equilibrium.
His primary scientific interests are in Speleothem, Stalagmite, Cave, Oceanography and Holocene. His research on Speleothem also deals with topics like
His study explores the link between δ18O and topics such as Isotope fractionation that cross with problems in Oxygen isotope ratio cycle. Denis Scholz has included themes like Geochemistry, Paleontology, Radiocarbon dating and Permafrost in his Cave study. His Oceanography study incorporates themes from Seasonality and Interglacial.
His primary areas of investigation include Speleothem, Cave, Holocene, Stalagmite and Physical geography. His Speleothem study combines topics in areas such as Glacial period, Trace element, Climate change, North Atlantic oscillation and Mediterranean climate. Denis Scholz interconnects Pleistocene, Paleoclimatology, Permafrost and Geochemistry, Calcite in the investigation of issues within Cave.
Calcite is a subfield of Mineralogy that Denis Scholz explores. His research on Stalagmite concerns the broader Paleontology. Δ13C, Isotope fractionation, Karst and Hydrology is closely connected to δ18O in his research, which is encompassed under the umbrella topic of Physical geography.
His primary scientific interests are in Speleothem, Cave, Physical geography, Holocene and Oceanography. His Speleothem research incorporates elements of Westerlies, Climate change, Mineralogy and North Atlantic oscillation. His work carried out in the field of Cave brings together such families of science as Radiocarbon dating, Pleistocene, Marine isotope stage, Trace element and Calcite.
The Physical geography study combines topics in areas such as Stalagmite, Paleoclimatology and Stadial. Much of his study explores Holocene relationship to Glacial period. In general Oceanography study, his work on Coral often relates to the realm of Diploria strigosa, thereby connecting several areas of interest.
This overview was generated by a machine learning system which analysed the scientist’s body of work. If you have any feedback, you can contact us here.
StalAge – An algorithm designed for construction of speleothem age models
Denis Scholz;Denis Scholz;Dirk L. Hoffmann.
Quaternary Geochronology (2011)
Increased seasonality in Middle East temperatures during the last interglacial period
Thomas Felis;Gerrit Lohmann;Henning Kuhnert;Stephan J. Lorenz.
Nature (2004)
Climatic dependence of stable carbon and oxygen isotope signals recorded in speleothems: From soil water to speleothem calcite
Wolfgang Dreybrodt;Denis Scholz.
Geochimica et Cosmochimica Acta (2011)
The Palaeoanthropocene – The beginnings of anthropogenic environmental change
Stephen F. Foley;Stephen F. Foley;Detlef Gronenborn;Meinrat O. Andreae;Meinrat O. Andreae;Joachim W. Kadereit.
Anthropocene (2013)
Accurate trace element analysis of speleothems and biogenic calcium carbonates by LA-ICP-MS
Klaus Peter Jochum;Denis Scholz;Brigitte Stoll;Ulrike Weis.
Chemical Geology (2012)
Procedures for accurate U and Th isotope measurements by high precision MC-ICPMS
Dirk L. Hoffmann;Julie Prytulak;David A. Richards;Tim Elliott.
International Journal of Mass Spectrometry (2007)
Modelling fractionation of stable isotopes in stalagmites.
Christian Mühlinghaus;Denis Scholz;Denis Scholz;Augusto Mangini.
Geochimica et Cosmochimica Acta (2009)
Modelling δ13C and δ18O in the solution layer on stalagmite surfaces
Denis Scholz;Christian Mühlinghaus;Augusto Mangini.
Geochimica et Cosmochimica Acta (2009)
Isotope disequilibrium effects: The influence of evaporation and ventilation effects on the carbon and oxygen isotope composition of speleothems – A model approach
Michael Deininger;Jens Fohlmeister;Denis Scholz;Augusto Mangini.
Geochimica et Cosmochimica Acta (2012)
230Th/U-dating of fossil corals and speleothems
Denis Scholz;Dirk Hoffmann.
EG Quaternary Science Journal (2008)
If you think any of the details on this page are incorrect, let us know.
We appreciate your kind effort to assist us to improve this page, it would be helpful providing us with as much detail as possible in the text box below:
Max Planck Society
University of Innsbruck
Heidelberg University
Alfred Wegener Institute for Polar and Marine Research
Ruhr University Bochum
Max Planck Institute for Chemistry
Xi'an Jiaotong University
Ruhr University Bochum
Heidelberg University
Johannes Gutenberg University of Mainz
Columbia University
Utrecht University
Missouri University of Science and Technology
University of Waterloo
Centre national de la recherche scientifique, CNRS
University of California, Los Angeles
Antoni van Leeuwenhoek Hospital
Antoni van Leeuwenhoek Hospital
Sapienza University of Rome
University of British Columbia
Imperial College London
Necker-Enfants Malades Hospital
University of California, San Francisco
University of York
Georgetown University
Smithsonian Astrophysical Observatory