24.02.2013 Views

25th International Meeting on Organic Geochemistry IMOG 2011

25th International Meeting on Organic Geochemistry IMOG 2011

25th International Meeting on Organic Geochemistry IMOG 2011

SHOW MORE
SHOW LESS

You also want an ePaper? Increase the reach of your titles

YUMPU automatically turns print PDFs into web optimized ePapers that Google loves.

P-028<br />

Characterisati<strong>on</strong> of lignin degradati<strong>on</strong> products from dissolved<br />

organic matter: a comparis<strong>on</strong> of different extracti<strong>on</strong> and<br />

analysis techniques<br />

J<strong>on</strong>athan Williams 1,2 , Jennifer Dungait 2 , Roland Bol 2 , Geoffrey Abbott 1<br />

1 Newcastle University, Newcastle up<strong>on</strong> Tyne, United Kingdom, 2 Rothamsted Research North Wyke,<br />

Okehampt<strong>on</strong>, United Kingdom (corresp<strong>on</strong>ding author:j<strong>on</strong>athan.williams@ncl.ac.uk)<br />

Lignin can degrade rapidly in soils. Recent research<br />

has shown that white-rot fungi, such as Pleurotus<br />

ostreatus, can oxidise lignin within a timescale of 7 to<br />

63 days 1,2 and lignin decompositi<strong>on</strong> is m<strong>on</strong>omer<br />

specific 3 . This has highly significant implicati<strong>on</strong>s for<br />

determining the mechanisms for C sequestrati<strong>on</strong> in<br />

soils. Lignin degrades into phenolic compounds which<br />

are water-soluble and, therefore, pr<strong>on</strong>e to be<br />

transported through the soil-water c<strong>on</strong>tinuum.<br />

Guaiacyl and syringyl lignin m<strong>on</strong>omer units have been<br />

detected in fresh, estuarine and marine waters 4 , and<br />

in deep ocean dissolved organic matter (DOM) 5,6<br />

allowing these compounds to be used as geochemical<br />

biomarkers of plant inputs in diverse systems.<br />

After it is degraded at source, the initial forms in which<br />

lignin enters watercourses are not yet known. In order<br />

to characterise and quantify degraded lignin products<br />

entering the soluble phase in soils, it is first necessary<br />

to determine the best approach to extract and analyse<br />

them. Therefore, the aims of this work were to:<br />

(1) determine the best method for the extracti<strong>on</strong> of<br />

lignin-derived compounds from freshwater (draining<br />

from grassland) in terms of recovery and timeefficiency,<br />

i.e. C18 solid phase extracti<strong>on</strong> (SPE) or<br />

freeze-drying.<br />

(2) compare analytical methods, i.e. <strong>on</strong>-line py-GC-<br />

MS in the presence of TMAH versus <strong>on</strong>-line py-GC-<br />

MS versus GC-MS of trimethylsilyl (TMS) derivatives.<br />

The results showed that freeze-drying recovered<br />

c<strong>on</strong>siderably more DOM than SPE in terms of mass<br />

(Figure 1). However, C18 silica-based SPE recovered<br />

a greater proporti<strong>on</strong> of identifiable lignin- and<br />

carbohydrate-derived compounds than freeze drying<br />

Gas chromatography-mass spectrometric (GC-MS)<br />

analyses of TMS derivatives of samples extracted by<br />

SPE from freshwater identified: benzoic acid, 4-<br />

[(trimethylsilyl)oxy]-,TMS ester; benzoic acid, 3methoxy-4-[(trimethylsilyl)oxy-],<br />

TMS ester; and 3,4bis[(trimethylsilyl)oxy]-,<br />

TMS ester. Abundant<br />

carbohydrate-derived compounds were also<br />

identified: α-D-Ribofuranoside, methyl 2,3,5-tris-O-<br />

(TMS)-; α-1-Mannopyranoside, methyl 6-deoxy-2,3,4tris-O-(TMS)-;<br />

and β-L-Arabinopyranose, 1,2,3,4tetrakis-O-(TMS)-;<br />

and also lipids including C16:0 and<br />

C18:0 fatty acids. C23 to C32 n-alkanes were the most<br />

abundant compounds from the same samples<br />

extracted using freeze-drying.<br />

Figure 1. Yields of DOM recovered by solid phase<br />

extracti<strong>on</strong> (SPE) and freeze-drying (FD) in relati<strong>on</strong> to<br />

TOC from a range of natural freshwaters, showing<br />

standard error bars.<br />

References<br />

[1] Roberts<strong>on</strong>, S., Mas<strong>on</strong>, S., Hack, E., Abbott, G.D.<br />

(2008) Org. Geochem. 39: 945-951; [2] Vane, C. H.,<br />

Martin, S. C., Snape, C. E., Abbott, G. D. (2001). J.<br />

Agric. Food Chem. 49: 2709-2716; [3] Dungait, J.A.J.,<br />

Stear, N.A., van D<strong>on</strong>gen, B. E., Bol, R., Evershed,<br />

R.P., (2008). Rapid Commun. Mass Sp. 22: 1631-<br />

1639; [4] Louchouarn, P., S. Opsahl, et al. (2000).<br />

Anal. Chem. 72(13): 2780-2787; [5] Opsahl, S. and R.<br />

Benner (1997). Nature 386(6624): 480-482; [6]<br />

Opsahl, S. and R. Benner (1999). Limnol. and<br />

Oceanogr. 44(8): 2017-2023.<br />

176

Hooray! Your file is uploaded and ready to be published.

Saved successfully!

Ooh no, something went wrong!