2012
DOI: 10.1016/j.epsl.2012.07.039
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A novel palaeoaltimetry proxy based on spore and pollen wall chemistry

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Cited by 35 publications
(59 citation statements)
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“…This is of importance since the concentration of phenylpropanoid components in wall biopolymers can be used as UV-B proxy and changes in the flux of UV-B radiation can be tracked over geological time (Lomax et al 2012). Therefore, the aim of this study was to investigate to what extend FTIR and Raman microspectroscopy measurements can reveal spatially resolved chemical information of pure grain biopolymers of Pinaceae pollen.…”
Section: Introductionmentioning
confidence: 99%
“…This is of importance since the concentration of phenylpropanoid components in wall biopolymers can be used as UV-B proxy and changes in the flux of UV-B radiation can be tracked over geological time (Lomax et al 2012). Therefore, the aim of this study was to investigate to what extend FTIR and Raman microspectroscopy measurements can reveal spatially resolved chemical information of pure grain biopolymers of Pinaceae pollen.…”
Section: Introductionmentioning
confidence: 99%
“…Indicators of solar activity such as counts of sunspot numbers and cosmogenic radionuclides ( 10 Be and 14 C) are limited to timescales of 10 2 to 10 3 years, respectively1, but the relationship between solar activity and UV flux is uncertain4. Calculated TSI variability across Milankovitch orbital cycles10 provides an expected pattern for incoming UV radiation over timescales of 10 4 to 10 7 years, but cannot detect short-term, surface-level departures from the orbital signal, for example those due to ozone thinning9, volcanic events11, dust clouds from bolide impacts12, or continental uplift13. A direct proxy for palaeo-UV flux would therefore provide both an indicator of UV as a climatic, environmental, and evolutionary forcing mechanism, and a recorder of atmospheric change across some of the major perturbations in Earth history.…”
mentioning
confidence: 99%
“…Within sporopollenin, protection from the deleterious effects of UV-B is provided by the phenolic compounds para -coumaric acid and ferulic acid1516. These UV absorbing compounds (UACs) covary with UV irradiance in a range of modern settings131516171819, demonstrating that plants actively control the chemical composition of sporopollenin with up-regulation in UACs in response to elevated UV doses16. The high preservation potential of sporopollenin, and the resultant high abundances of sporomorphs in the fossil record, suggests that a UAC-based proxy could be used to reconstruct UV flux in deep time settings1620.…”
mentioning
confidence: 99%
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“…Pollen size has also been correlated with genome size and may indicate polyploidy (three or more chromosome sets) in plants (Gould 1957;Kapadia & Gould 1964;Bennett 1972;Tate et al 2005;Knight et al 2010;De Storme et al 2013). Increasingly, geochemical studies utilising pollen, such as stable isotope analysis for palaeoclimate reconstructions (Amundson et al 1997;Loader & Hemming 2004;Nelson et al 2006Nelson et al , 2007King et al 2012;Nelson 2012;Bell et al 2017) and biomarker analysis for UV-B reconstructions (Rozema et al 2001(Rozema et al , 2002Fraser et al 2011;Willis et al 2011;Lomax et al 2012;, require detailed knowledge of grain size for developing techniques to isolate specific grains from fossil assemblages. For example, the use of micro-sieving to concentrate pollen from sediment (Heusser & Stock 1984;Brown et al 1989) can be modified to target grains within a specified size range to facilitate the isolation of pollen for specific species.…”
Section: Introductionmentioning
confidence: 99%