Earth System Processes 2 (8–11 August 2005)

Paper No. 3
Presentation Time: 10:00 AM

INVITED: THE SIBERIAN TRAPS, STRATOSPHERIC OZONE, UV-B FLUX AND MUTAGENESIS


LOMAX, Barry1, BEERLING, David1, CALLAGHAN, Terry2, FRASER, Wes3, HARFOOT, Mike4, PYLE, John4, SELF, Steve3, SEPHTON, Mark5 and WELLMAN, Charles1, (1)Animal and Plant Sciences, University of Sheffield, Sheffield, S10 2TN, England, (2)Animal and Plant Sciences, University of Sheffield, Sheffield, S10 2TN, (3)Department of Earth Sciences, Open University, Milton Keynes, MK7 6AA, England, (4)Centre for Atmospheric Science, Cambridge University, Cambridge, CB2 1EW, England, (5)Planetary and Space Science Research Institute, The Open University, Walton Hall, Milton Keynes, MK7 6AA, B.lomax@sheffield.ac.uk

The spores and pollen of terrestrial land plants can increase their investment in UV-B screening pigments when exposed to elevated levels of UV-B radiation. Here, we report an increase in UV-B protecting pigments from a historical record of the spores of Lycopodium magellanicum growing in South Georgia and exposed to a progressive thinning of stratospheric ozone and a corresponding increase in UV-B radiation. Our data records a strong three fold linear increase in the concentration of UV-B protecting pigments in response to a 14% thinning of the ozone column. Our results were obtained using micro FT-IR analysis of sporopollenin, which is readily preserved in the fossil record. Therefore, this newly identified response offers a potential tool for investigating natural changes in the stratospheric ozone layer and UV-B flux over geological time.

We are initially targeting the Permo-Triassic boundary for further investigation, as recent work has suggested a global collapse in the stratospheric ozone due to the emplacement of the Siberian Traps. This hypothesis can now be thoroughly tested using a combined approach, involving the examination of extant plants subjected to experimentally manipulated UV-B radiation, the geochemical study of fossil spores and pollen and the long-term modelling of stratospheric ozone.