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Dr Kaja Fenn
Quaternary Geochronologist, Geochemist, and Sedimentologist
MY RESEARCH INTERESTS
PALAEOCLIMATE AND PALEOENVIRONMENT


Provenance is often neglected in Quaternary environmental reconstructions. Sediment source, whether geomorphological (more immediate) or geological (the proto-source), can provide information about past landscapes and sediment transport including sediment production, atmospheric circulation, landscape evolution, and the wider dust cycle.
SEDIMENT
PROVENANCE

LOESS-PALAEOSOL DEPOSITS

GEOCHEMISTRY - ZIRCON DATING AND ISOTOPES

The key techniques I use to address provenance questions revolve around sediment geochemistry, in particular single grain zircons. Zircon U-Pb dating and isotopic hafnium content enable tracing individual loess grains to the bedrock(s) they were eroded from.
GEOCHEMISTRY - ZIRCON DATING AND ISOTOPES

GEOCHRONOLOGY - LUMINESCENCE DATING (OSL)

Geochronology provides a basis for a robust comparison of environmental change between sites, regions, and archives. I am an OSL specialist with an extensive background in dating quartz and feldspars minerals, and using luminescence dating to determine the timing of loess deposition.
GEOCHRONOLOGY - LUMINESCENCE DATING (OSL)

SEDIMENTOLOGY

Loess typically provides lithological evidence of past processes. In my research I focus on stratigraphic description and sedimentological proxies, such as grain size, colour, magnetic susceptibility, and organic and carbonate content.
SEDIMENTOLOGY
Research Interests
Sample locations
SAMPLE LOCATIONS
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