Prof.Dr. Christoph Korte

ckorte

Fachbereich Geowissenschaften

Institut für Geologische Wissenschaften

Tektonik und Sedimentologie

Privatdozent

Fax (+49 30) 838 - 458659
E-Mail korte@geo.ku.dk

My research is focussed on palaeoceanography and palaeoclimatology of Permian, Triassic and Jurassic marine sediments. Of particular interest are the geochemical changes at the Permian-Triassic and the Triassic-Jurassic boundaries. I use oxygen, carbon, sulphur and strontium isotope signatures, as well as main and trace elements, of marine biogens and sediments, to understand interactions between hydrosphere, atmosphere, lithosphere and biosphere and enable characterisation of geologic processes. In addition, I use isotope trends for chemostratigraphy.

Selected Papers

  • Korte C., Kozur H. W., Bruckschen P. and Veizer J. (2003) Strontium isotope evolution of Late Permian and Triassic seawater. Geochim. Cosmochim. Acta 67, 47-62.
  • Korte C., Kozur H. W., Joachimski M. M., Strauss H., Veizer J. and Schwark L. (2004) Carbon, sulfur, oxygen and strontium isotope records, organic geochemistry and biostratigraphy across the Permian/Triassic boundary in Abadeh, Iran. Int. J. Earth Sci. 93, 565-581.
  • Korte C., Jasper T., Kozur H. W. and Veizer J. (2005) d 18O and d13 C of Permian brachiopods: A record of seawater evolution and continental glaciation. Palaeogeogr. Palaeoclimatol. Palaeoecol. 224, 333-351.
  • Korte C., Kozur H. W. and Veizer J. (2005) d 13C and d 18O values of Triassic brachiopods and carbonate rocks as proxies for coeval seawater and palaeotemperature. Palaeogeogr. Palaeoclimatol. Palaeoecol. 226, 287-306.
  • Korte, C., Jasper, T., Kozur, H. W. and Veizer, J. (2006) 87Sr/86Sr record of Permian seawater. Palaeogeogr. Palaeoclimatol. Palaeoecol. 240, 89-107.
  • Korte C., Brand U. , Dickins J. M., Jones P. J., Mertmann D. and Veizer J. (submitted) Permian latitudinal sea-surface temperature gradients.
  • Korte C., Hesselbo S. P., Jenkyns H. C. and Spötl C. (in preparation) Oxygen and carbon isotope values from low-Mg-calcitic oysters and whole rock carbonates across the Triassic-Jurassic boundary in the UK.