ACETATE MINERALIZATION AS A MEASURE OF SPARTINA ALTERNIFLORA ROOT ENHANCEMENT OF MICROBIAL ACTIVITY.


Rebecca Tirrell and Linda Blum.


We have been examining the potential for live roots of Spartina alterniflora to enhance belowground decomposition in marsh sediments. Data from Phillips Creek and Great Sippewissett marshes, and qualitative observaations in North Carolina marshes suggest that the presence of live roots stimulates belowground decompostion. For example, Hackney and de la Cruz (1980) observed that decomposition in buried litter bags did not begin until living plant roots came into contact with the bag contents, while Hines et al. (1991) noted a correlation between live roots and acetate concentrations in sediment porewater. These observations suggest that organic materials excreted by live marsh plant roots might enhance microbial activity in the rhizosphere, and thus decay.

We used a litter bag technique to measure decay of dead S. alterniflora roots. Three clipped (no live roots) and 3 vegetated (live roots) plots were established in both creekbank and interior sections of Phillips Creek marsh. One month later, litter bags containing dead Spartina alterniflora roots and rhizomes were buried in the marsh plots. Every 2 months, a litter bag was removed from each treatment plot and examined for decay and the presence of live roots. Samples were also collected for bacterial abundance and activity (as acetate mineralization). Over an 18-month period, little root decay was measured regardless of the location or the presence of live roots. However, significantly greater numbers of bacteria were evident in the vegetated plots of both creekbank and interior marsh locations. Rates of acetate mineralization were not correlated with bacterial abundance; rates were greater in creekbank than in interior sediments regardless of the presence or absence of live roots (Figure 1). Not surprisingly, acetate mineralization was greatest in the spring and summer, and was minimal during fall and winter. These results were presented at the last VCR-LTER All-Scientists meeting.

Because spring and summer differences in acetate mineralization between creekbank and interior sediments could be related to the concentration of acetate in sediment pore water, we have been measuring actetate mineralization and pore-water concentrations, and bacterial abundance during the past year in both vegetated and clipped plots at the creekbank and interior locations. Bacterial abundance and acetate mineralization rates were similar to those measured during the decay experiment. Pore-water acetate concentrations are currently being measured using an enzymatic assay which couples the synthesis of acetyl-CoA (from acetate) to AMP production. AMP concentrations are measured by HPLC. Once sediment acetate concentrations have been obtained, acetate turn-over rate constants will be calculate for plots with and without live roots. These data will yield evidence to indicate the potential for live roots to enhance microbial activity in the rhizosphere of intermediate (creekbank) and short-form (interior) S. alterniflora.