Tobias Sprafke

Dr. Tobias Sprafke

Institute of Geography, University of Bern, Hallerstrasse 12, 3012 Bern, Switzerland
orcid

Research Focus & Metrics

Academic Career Length

16Years (2011-Present)

(Calculated once Scilit publication data is synced: current year − year of first publication + 1)

Representative Publications

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1 December 2014 in Quaternary Science Reviews
Verified
Journal Article
Closed access
OHOliver Heiri
Oliver Heiri
KKKarin Koinig
Karin Koinig
CSChristoph Spötl
Christoph Spötl
SBSam Barrett
Sam Barrett
ABAchim Brauer
Achim Brauer
WTWilly Tinner
Willy Tinner

1 April 2016 in Quaternary International
Verified
Journal Article
Closed access
TSTobias Sprafke
Tobias Sprafke
IOIgor Obreht
Igor Obreht

1 March 2018 in Quaternary International
Verified
Journal Article
Closed access
KFKathryn E. Fitzsimmons
Kathryn E. Fitzsimmons
TSTobias Sprafke
Tobias Sprafke
CZChristoph Zielhofer
Christoph Zielhofer
CGChristina Günter
Christina Günter
JDJean-Marc Deom
Jean-Marc Deom
RIRadu Iovita
Radu Iovita

1 January 2015 in Palaeogeography, Palaeoclimatology, Palaeoecology
Verified
Journal Article
Closed access
BTBirgit Terhorst
Birgit Terhorst
SSSergey Sedov
Sergey Sedov
TSTobias Sprafke
Tobias Sprafke
RPRobert Peticzka
Robert Peticzka
SMSimon Meyer-Heintze
Simon Meyer-Heintze
ERElizabeth Solleiro Rebolledo
Elizabeth Solleiro Rebolledo

1 November 2020 in Quaternary Science Reviews
Verified
Journal Article
Open access
TSTobias Sprafke
Tobias Sprafke
PSPhilipp Schulte
Philipp Schulte
SMSimon Meyer-Heintze
Simon Meyer-Heintze
MHMarc Händel
Marc Händel
TEThomas Einwögerer
Thomas Einwögerer
BTBirgit Terhorst
Birgit Terhorst

25 October 2018 in Journal of Maps
Verified
Journal Article
Open access
FLFrank Lehmkuhl
Frank Lehmkuhl
JBJanina Bösken
Janina Bösken
JHJan Hošek
Jan Hošek
TSTobias Sprafke
Tobias Sprafke
SMSlobodan B. Marković
Slobodan B. Marković
CZChristian Zeeden
Christian Zeeden
Supraregional (palaeo)geoecological studies require detailed knowledge of the distribution of aeolian sediments and their sources. Such spatial data can be visualised and shared in maps, but often these are constrained in their resolution or extent. This is the case for the Carpathian Basin, where cross-border maps are not detailed enough to answer many research questions. Problems occur especially along political borders due to different geological mapping standards and varying lithological definitions. Using a Geographic Information System (GIS), we compiled a map showing the distribution of loess and related Quaternary sediments in the Carpathian Basin, with unprecedented detail. We vectorised and analysed existing data (mainly from geological maps) and combined and transferred these into a common (loess) sediment classification system. This cross-border map shows the distribution of aeolian sediments in the Carpathian Basin at a scale of 1:1,500,000. For the northwestern and the southern Carpathian Basin, we added maps that clarify the extent of late Pleistocene and Holocene terrace and floodplain deposits, which were merged in the Main Map to highlight the predominant dust source areas for this region.