Preservation of biomolecules in sub-fossil plants from raised peat bogs - A potential paleoenvironmental proxy

Tomasz Kuder, Michael Kruge

Research output: Contribution to journalConference article

61 Citations (Scopus)

Abstract

The relationship between changes of peat bog hydrology and the mechanisms of decomposition suggests that the chemical modification of biopolymers of peat macrofossils might be used in paleoenvironmental reconstructions. A series of sedge (Eriophorum vaginatum) macrofossils from an Upper Holocene peat profile has been studied by analytical pyrolysis (Py-GC/MS). The major diagenetic changes of biopolymers included loss of ester-bound ferulic and coumaric acids, an increase of oxidation (particularly due to Cα ketones) and shortening of alkyl side-chains, demethylation of methoxy groups of the lignin/polyphenol fraction, loss of pentosan polysaccharides and modification of cellulose (relative increase in the pyrolytic yield of anhydroglucose). The yield of oxidized methoxymoieties (particularly of Cα ketones) and shortening of alkyl side-chains of methoxyphenols were suggested as the best indicators of oxidative degradation. Statistically significant differences in chemical composition between samples from individual depth increments occur, in part in agreement with a sequence of wet and dry phases determined by paleobotanical analysis. The paleoenvironmental significance of the chemical record of degradation and relationship of paleohydrology reconstructed by the present technique and by means of botanical analysis is discussed. The former was proposed to respond primarily to the frequency of seasonal droughts.

Original languageEnglish
Pages (from-to)1355-1368
Number of pages14
JournalOrganic Geochemistry
Volume29
Issue number5-7 -7 pt 2
DOIs
StatePublished - 1 Nov 1998
EventProceedings of the 1997 18th International Meeting on Organic Geochemistry. Part 2 (of 2) - Maastricht, Neth
Duration: 22 Sep 199726 Sep 1997

Fingerprint

Peat
Biomolecules
ketone
peatland
peat
ferulic acid
Biopolymers
fossil
Ketones
paleohydrology
degradation
sedge
polysaccharide
pyrolysis
ester
lignin
cellulose
Coumaric Acids
Degradation
hydrology

Keywords

  • Eriophorum vaginatum
  • Lignin
  • Paleoenvironment
  • Paleohydrology
  • Peatification
  • Pyrolysis-gas chromatography-mass spectrometry
  • Raised bog

Cite this

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abstract = "The relationship between changes of peat bog hydrology and the mechanisms of decomposition suggests that the chemical modification of biopolymers of peat macrofossils might be used in paleoenvironmental reconstructions. A series of sedge (Eriophorum vaginatum) macrofossils from an Upper Holocene peat profile has been studied by analytical pyrolysis (Py-GC/MS). The major diagenetic changes of biopolymers included loss of ester-bound ferulic and coumaric acids, an increase of oxidation (particularly due to Cα ketones) and shortening of alkyl side-chains, demethylation of methoxy groups of the lignin/polyphenol fraction, loss of pentosan polysaccharides and modification of cellulose (relative increase in the pyrolytic yield of anhydroglucose). The yield of oxidized methoxymoieties (particularly of Cα ketones) and shortening of alkyl side-chains of methoxyphenols were suggested as the best indicators of oxidative degradation. Statistically significant differences in chemical composition between samples from individual depth increments occur, in part in agreement with a sequence of wet and dry phases determined by paleobotanical analysis. The paleoenvironmental significance of the chemical record of degradation and relationship of paleohydrology reconstructed by the present technique and by means of botanical analysis is discussed. The former was proposed to respond primarily to the frequency of seasonal droughts.",
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Preservation of biomolecules in sub-fossil plants from raised peat bogs - A potential paleoenvironmental proxy. / Kuder, Tomasz; Kruge, Michael.

In: Organic Geochemistry, Vol. 29, No. 5-7 -7 pt 2, 01.11.1998, p. 1355-1368.

Research output: Contribution to journalConference article

TY - JOUR

T1 - Preservation of biomolecules in sub-fossil plants from raised peat bogs - A potential paleoenvironmental proxy

AU - Kuder, Tomasz

AU - Kruge, Michael

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N2 - The relationship between changes of peat bog hydrology and the mechanisms of decomposition suggests that the chemical modification of biopolymers of peat macrofossils might be used in paleoenvironmental reconstructions. A series of sedge (Eriophorum vaginatum) macrofossils from an Upper Holocene peat profile has been studied by analytical pyrolysis (Py-GC/MS). The major diagenetic changes of biopolymers included loss of ester-bound ferulic and coumaric acids, an increase of oxidation (particularly due to Cα ketones) and shortening of alkyl side-chains, demethylation of methoxy groups of the lignin/polyphenol fraction, loss of pentosan polysaccharides and modification of cellulose (relative increase in the pyrolytic yield of anhydroglucose). The yield of oxidized methoxymoieties (particularly of Cα ketones) and shortening of alkyl side-chains of methoxyphenols were suggested as the best indicators of oxidative degradation. Statistically significant differences in chemical composition between samples from individual depth increments occur, in part in agreement with a sequence of wet and dry phases determined by paleobotanical analysis. The paleoenvironmental significance of the chemical record of degradation and relationship of paleohydrology reconstructed by the present technique and by means of botanical analysis is discussed. The former was proposed to respond primarily to the frequency of seasonal droughts.

AB - The relationship between changes of peat bog hydrology and the mechanisms of decomposition suggests that the chemical modification of biopolymers of peat macrofossils might be used in paleoenvironmental reconstructions. A series of sedge (Eriophorum vaginatum) macrofossils from an Upper Holocene peat profile has been studied by analytical pyrolysis (Py-GC/MS). The major diagenetic changes of biopolymers included loss of ester-bound ferulic and coumaric acids, an increase of oxidation (particularly due to Cα ketones) and shortening of alkyl side-chains, demethylation of methoxy groups of the lignin/polyphenol fraction, loss of pentosan polysaccharides and modification of cellulose (relative increase in the pyrolytic yield of anhydroglucose). The yield of oxidized methoxymoieties (particularly of Cα ketones) and shortening of alkyl side-chains of methoxyphenols were suggested as the best indicators of oxidative degradation. Statistically significant differences in chemical composition between samples from individual depth increments occur, in part in agreement with a sequence of wet and dry phases determined by paleobotanical analysis. The paleoenvironmental significance of the chemical record of degradation and relationship of paleohydrology reconstructed by the present technique and by means of botanical analysis is discussed. The former was proposed to respond primarily to the frequency of seasonal droughts.

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