4.3 Article

Sphagnum δ13C values as indicators of palaeohydrological changes in a peat bog

Journal

HOLOCENE
Volume 20, Issue 2, Pages 285-291

Publisher

SAGE PUBLICATIONS LTD
DOI: 10.1177/0959683609350389

Keywords

Carbon isotopes; peat bogs; Canada; late-Holocene; testate amoebae; Sphagnum

Funding

  1. Hydro-Quebec Production
  2. NSERC
  3. FQRNT
  4. NSTP-Canada

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Late-Holocene peat stratigraphy of a Canadian boreal peat bog was examined to evaluate the potential of Sphagnum delta C-13 values as surface moisture proxy indicators. Isotopic measurements were compared to testate amoebae-inferred water-table depth reconstructions, plant macrofossil assemblages and past decomposition levels inferred by colorimetric humification. AMS radiocarbon dates were coupled with Pb-210 dates to establish peat chronology. Although the mechanisms underlying carbon fractionation processes in peatlands are not well understood, we demonstrate that Sphagnum delta C-13 values have potential for palaeohydrological reconstructions, since variations presented by the isotopic values can generally be correlated with the other proxy records, especially during drier episodes.

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