Radiocarbon and stable carbon isotopic evidence for transport and transformation of dissolved organic carbon, dissolved inorganic carbon, and CH4 in a northern Minnesota peatland
Ls. Chasar et al., Radiocarbon and stable carbon isotopic evidence for transport and transformation of dissolved organic carbon, dissolved inorganic carbon, and CH4 in a northern Minnesota peatland, GLOBAL BIOG, 14(4), 2000, pp. 1095-1108
To elucidate the roles of hydrology and vegetation in belowground carbon cy
cling within peatlands, radiocarbon values were obtained for pore water dis
solved organic carbon (DOC), dissolved inorganic carbon (DIC), CH4, and pea
t from the Glacial Lake Agassiz peatland. The major implication of this wor
k is that the rate of microbial respiration within a peat column is greater
than the peat decomposition rate. The radiocarbon content of DOC at both b
og and fen was enriched relative to solid-phase peat by similar to 150-300
parts per thousand consistent with the advection of recently photosynthesiz
ed DOC downward into the peat column. Fen Delta C-14 values for DIC and CH4
closely track the Delta C-14 of pore water DOC at depth, indicating that t
his recent plant production was the predominant substrate for microbial res
piration. Aceticlastic methanogenesis apparently dominated the upper third
of the peat column (alpha = 1.05), shifting toward CO2 reduction with depth
(1.05 < <alpha> < 1.08). Upwelling groundwater contributed as much as 15%
of the DIC to the bulk DIC pool at depth in the fen. The similarity of <Del
ta>C-14 values for DIC and CH4 suggests that methanogens utilized DIC from
this source as well as DIC produced in situ. Bog Delta C-14 values for pore
water DIC and CH4 differ by less than or equal to 15 parts per thousand at
all depths and are depleted in C-14 relative to DOC by similar to 100 part
s per thousand, suggesting microbial utilization of a mixture of older and
modern substrate. CO2 reduction was the primary pathway for methanogenesis
at all depths in the bog (a = 1.08), and groundwater influence on bulk DIC
was negligible. For bath sites, Delta C-14-DIC and Delta C-14-CH4 are appro
ximately equal at depths where stable isotope data indicate a predominance
of CO2 reduction and dissimilar when acetate fermentation is indicated.