2017
DOI: 10.1016/j.revpalbo.2016.11.014
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Shedding light on sporopollenin chemistry, with reference to UV reconstructions

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Cited by 56 publications
(73 citation statements)
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“…Attenuated total reflection Fourier transform infrared (ATR‐FTIR) analysis of the UV–O treated pollen was performed to obtain a more complete understanding of surface chemistry changes, and provided verification of the observations made from X‐ray photoelectron spectroscopy (XPS) analysis. Major peaks in untreated (0 min) pollen were assigned from previous FTIR studies on sporopollenin, with peak attributions being hydroxyl (3300 cm −1 ), aliphatic (2925 cm −1 ), carbonyl (1670 cm −1 ) aromatics (1515 cm −1 , 1425 cm −1 ), and COR (1028 cm −1 ) ( Figure a and Figure S7a, Supporting Information) . Subtracting UV–O treated spectra from untreated spectra suggested reductions in absorption for most major peaks of interest, and highlighted a relatively large increase in the shoulder peak at 1718 cm −1 (Figure b), which may be attributed to CO and correlates to the increased R 2 CO binding observed from the XPS analysis.…”
Section: Resultsmentioning
confidence: 87%
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“…Attenuated total reflection Fourier transform infrared (ATR‐FTIR) analysis of the UV–O treated pollen was performed to obtain a more complete understanding of surface chemistry changes, and provided verification of the observations made from X‐ray photoelectron spectroscopy (XPS) analysis. Major peaks in untreated (0 min) pollen were assigned from previous FTIR studies on sporopollenin, with peak attributions being hydroxyl (3300 cm −1 ), aliphatic (2925 cm −1 ), carbonyl (1670 cm −1 ) aromatics (1515 cm −1 , 1425 cm −1 ), and COR (1028 cm −1 ) ( Figure a and Figure S7a, Supporting Information) . Subtracting UV–O treated spectra from untreated spectra suggested reductions in absorption for most major peaks of interest, and highlighted a relatively large increase in the shoulder peak at 1718 cm −1 (Figure b), which may be attributed to CO and correlates to the increased R 2 CO binding observed from the XPS analysis.…”
Section: Resultsmentioning
confidence: 87%
“…The pollen outer shell is known to provide ultraviolet (UV) protection for sensitive genetic material. Cinnamic acids present in the outer shell are responsible for UV absorption, and quantifying the proportion of cinnamic acids is used as a means for studying climate change from pollen shells in fossil records . There is interest in the influence of ozone as an environmental pollutant on pollen properties .…”
Section: Introductionmentioning
confidence: 99%
“…Previous studies have suggested plasticity of pollen chemistry to climate and other environmental variables (Zimmermann & Kohler, 2014;Zimmermann et al, 2017). For example, temperature has been connected to changes in protein as well as lipid content in both controlled and field experimental conditions (Lahlali et al, 2014;Zimmermann & Kohler, 2014;Jiang et al, 2015;Zimmermann et al, 2017), whilst the effects of exposure to UV-B radiation on pollen chemistry have gained increasing attention (Rozema et al, 2001;Blokker et al, 2006;Fraser et al, 2011;Willis et al, 2011;Jardine et al, 2017;Bell et al, 2018). Additionally, there may be confounding effects related to local adaptation and hybridisation.…”
Section: Prospects For Developments Using Fossil Pollenmentioning
confidence: 99%
“…Second, understanding of the potential impact of environmental variation on the pollen-chemistry signature remains limited. For example, some of the variation in lipid, protein, and carbohydrate chemistry may be explained by environmental influences such as temperature during pollen maturation (Lahlali et al, 2014;Zimmermann & Kohler, 2014;Jiang et al, 2015;Zimmermann et al, 2017), whilst sporopollenin composition may be influenced by external environmental influences such as the plant exposure to UV-B radiation (Rozema et al, 2001;Blokker, Boelen, Broekman, & Rozema, 2006;Willis et al, 2011;Wesley T. Fraser et al, 2011;P. E. Jardine, Abernethy, Lomax, Gosling, & Fraser, 2017;Bell et al, 2018).…”
Section: Main Text 1 Introductionmentioning
confidence: 99%
“…The application of methods such as Raman and Fourier-transform infrared spectroscopy (FTIR) have provided new information regarding organic molecules in Mesozoic plants (Vajda et al 2017) and older deposits (Qu et al 2015). Furthermore, FTIR of spores and pollen has been used to develop a proxy for ultraviolet irradiance (Jardine et al 2016;Jardine et al 2017). The combination of high-resolution microscopy and computational image analyses has proved useful in determining the botanical affinity of enigmatic taxa (Mander et al 2013); such approaches can be applied to many groups, thus improving vegetation reconstructions based on dispersed spores and pollen.…”
Section: Recent Developments and Future Researchmentioning
confidence: 99%