Abstract
Peatlands are a major carbon (C) sink globally. Organic matter quality influence greenhouse gases production. However, little is known about how organic matter from different vegetation types, influences C composition and resultant greenhouse gases production in subtropical peatland. Anoxic incubation experiments were conducted using two types of peats with different botanical origin to assess C composition, CO(2) and CH(4) production. First peat had cypress dominance and the second knotted spikerush and water lily (spike + lily). Solid-state CPMAS (13)C NMR determined C chemical stability, MESTA determined C thermal stability, stable isotopes for C source and gas chromatograph for carbon dioxide (CO(2)) and methane (CH(4)). The results indicated dominance of autochthonous C as indicated by δ(13)C signatures. Low thermal stable C (LTSC) dominated in litter, FL (fermentation layer) and spike + lily sediment, high thermal stable C was dominant in cypress peat. O-alkyl C strongly correlated with LTSC whereas aromatic C correlated negatively with R400 (LTSC:total C ratio). Generally, O-alkyl decreased and alkyl increased along litter-FL-peat continuum. Spike + lily peat exhibited initial stage of decomposition. Indicated by increased alkyl C, aromatic C and aromatic:O-alkyl ratio with increasing peat depth. Also, exhibited 3 times more CH(4) and CO(2) production compared to cypress peat that dominantly exhibited second stage of decomposition. O-alkyl C exhibited positive relationship with CH(4) (P = 0.012, r(2) = 0.57) and CO(2) (P = 0.047, r(2) = 0.41) production whereas R400 related positively with CH(4) (P = 0.05, r(2) = 0.40). Organic matter thermal and chemical composition varied between the peat types and thermally and chemically labile C influenced CO(2) and CH(4) production.