Lignin-derived phenolic compounds in the particulate organic matter of a French Mediterranean river: seasonal and spatial variations

Citation
Lc. Da Cunha et al., Lignin-derived phenolic compounds in the particulate organic matter of a French Mediterranean river: seasonal and spatial variations, ORG GEOCHEM, 32(2), 2001, pp. 305-320
Citations number
57
Categorie Soggetti
Earth Sciences
Journal title
ORGANIC GEOCHEMISTRY
ISSN journal
01466380 → ACNP
Volume
32
Issue
2
Year of publication
2001
Pages
305 - 320
Database
ISI
SICI code
0146-6380(2001)32:2<305:LPCITP>2.0.ZU;2-#
Abstract
Samples from the Tech river (French Mediterranean river) were analysed for particulate organic carbon (POC) and lignin phenols, to characterise spatia l and seasonal variations. A decreasing gradient of lignin phenols (from ca . 0.8 to 0.5 mg 100 mg OC-1) was observed downstream, together with an incr ease of p-hydroxyl (H) phenols. Seasonal variations in total and lignin-phe nols composition were very noticeable and seemed to be connected directly t o rainfall variations. Lignin-phenol concentrations were higher in the wet periods (up to 12.1 mug/1) while the dry periods were characterised by the predominance of H phenols over lignin-phenols (Lambda) (H/Lambda ratios rea ching values of 245 during summer). This predominance of H phenols was also associated with high chlorophyll a concentrations, which may indicate an a utochthonous (and fresher) source of these phenols to the water column. Mea n vanillic acid/vanillin ratios were higher than those of fresh plant mater ial (0.4 for POM against 0.2 for fresh plant tissues), indicating that the lignin component had already been degraded before entering the river. The s yringyl/vanillyl (S/V) and cinnamyl/vanillyl (C/V) ratios indicate a predom inance of angiosperm + gymnosperm woody material in the lower sector and th e presence of some angiosperm non-woody material in the mountain sector. co rresponding to alpine and sub-alpine vegetation. (C) 2001 Elsevier Science Ltd. All rights reserved.