Rapid determination of spore chemistry using thermochemolysis gas chromatography-mass spectrometry and micro-Fourier transform infrared spectroscopy

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作者
Jonathan S. Watson
Mark A. Sephton
Sarah V. Sephton
Stephen Self
Wesley T. Fraser
Barry H. Lomax
Iain Gilmour
Charles H. Wellman
David J. Beerling
机构
[1] Open University,Planetary and Space Sciences Research Institute
[2] South Kensington Campus,Department of Earth Science and Engineering
[3] Open University,Department of Earth Sciences
[4] University of Sheffield,Department of Animal and Plant Sciences
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Spore chemistry is at the centre of investigations aimed at producing a proxy record of harmful ultraviolet radiation (UV-B) through time. A biochemical proxy is essential owing to an absence of long-term (century or more) instrumental records. Spore cell material contains UV-B absorbing compounds that appear to be synthesised in variable amounts dependent on the ambient UV-B flux. To facilitate these investigations we have developed a rapid method for detecting variations in spore chemistry using combined thermochemolysis gas chromatography-mass spectrometry and micro-Fourier transform infrared spectroscopy. Our method was tested using spores obtained from five populations of the tropical lycopsid Lycopodium cernuum growing across an altitudinal gradient (650-1981 m a.s.l.) in S.E. Asia with the assumption that they experienced a range of UV-B radiation doses. Thermochemolysis and subsequent pyrolysis liberated UV-B pigments (ferulic and para-coumaric acid) from the spores. All of the aromatic compounds liberated from spores by thermochemolysis and pyrolysis were active in UV-B protection. The various functional groups associated with UV-B protecting pigments were rapidly detected by micro-FTIR and included the aromatic C?C absorption band which was exclusive to the pigments. We show increases in micro-FTIR aromatic absorption (1510 cm−1) with altitude that may reflect a chemical response to higher UV-B flux. Our results indicate that rapid chemical analyses of historical spore samples could provide a record ideally suited to investigations of a proxy for stratospheric O3 layer variability and UV-B flux over historical (century to millennia) timescales.
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页码:689 / 694
页数:5
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