L. Serve et al., LIGNIN-DERIVED PHENOLS IN SEDIMENTS IN LONG CORES FROM LAC DU BOUCHET(MASSIF-CENTRAL, FRANCE) - PALEOENVIRONMENTAL SIGNIFICANCE, Bulletin de la Societe geologique de France, 168(4), 1997, pp. 507-520
Lignitic remains present in the organic fraction of lake sediments con
tain monomeric phenolic structures which can be regarded as specific b
iogeotracers of the organic matter produced by higher plants growing o
n the watershed. A study of the lignin-derived phenolic monomers (keto
nic, aldehydic and acidic forms of 4-hydroxybenzyl, guaiacyl - or vani
llyl -, syringyl and cinnamyl acids) has been made on samples of a 50
metres long core from the maar-lake, Lac du Bouchet. Their qualitative
and quantitative determinations have been achieved by high-performanc
e liquid chromatography (HPLC). The data permit analysis of the taxono
mic origin of allochthonous inputs and, by comparison with palynologic
al data of climate variations from at least 350.10(3) years (350 ky).
At the same lime, comparison of lignin-derived phenol data and bulk or
ganic matter enable the mode and the extent of organic matter alterati
on to be defined. In this oligotrophic lake, sediments corresponding t
o cold periods with a steppe pollen assemblage (stadial or glacial per
iods) are generally poor in organic matter (OM). This OM is poor or la
cking in lignin-derived phenols. It contains some ubiquitous phenols w
hich map originate from algal tissues : consequently the organic compo
nent of these sediments is either autochthonous - i.e. of phytoplancto
nic and bacterial origin (at the time, the ancient lac du Bouchet was
similar to certain present Arctic lakes) - or mixed autochthonous-allo
chthonous but altered (that is particularly shown by the presence of a
bundant oxidized ligno-cellulosic debris). In contrast, the OM corresp
onding to temperate periods (interstadial and interglacial) contains h
igh proportions of lignin indicating allochthonous organic input to th
e lake from a diverse vascular plants. During these relatively warm pe
riods, the allochthonous organic phase was mixed with local autochthon
ous organic input.