The respiration of flocculent detrital organic matter (floc) is driven by phosphorus limitation and substrate quality in a subtropical wetland

Publication date: March 2015
Source:Geoderma, Volumes 241–242
Author(s): Oliva Pisani , Leonard J. Scinto , Jay W. Munyon , Rudolf Jaffé
The aerobic respiration of flocculent detrital organic material (floc) from Everglades National Park was found to be dependent on phosphorus limitation and carbon quality and is likely influenced by substrate age, hydrology, and local biomass productivity. Floc was collected at four sites along the Shark River and Taylor Sloughs of Everglades National Park and incubated for up to one week at room temperature in the dark. Floc respiration was determined by measuring the total amount of CO2 evolved and CO2 generation rates. To investigate the effect of hydrological conditions, samples were collected in a typical dry (April) and wet (October) season and from short- and long-hydroperiod sites. Floc from the short-hydroperiod freshwater site generated more CO2 compared to the long-hydroperiod site due to the labile nature of the periphyton-derived organic matter at the former and the presence of more degraded and aged material at the latter. The tidally-influenced Shark River Slough mangrove site generated more CO2 compared to the Taylor Slough mangrove site, likely as a result of phosphorus inputs from the adjacent Gulf of Mexico at the former and reduced phosphorus inputs and prolonged inundation at the latter. Generally, more CO2 was generated during the dry season. Floc respiration rates were faster in the wet season, suggesting that fresh vegetation inputs to the floc can influence this process. Phosphorus and glucose additions enhanced CO2 generation suggesting that phosphorus limitation and carbon quality are important factors regulating floc decomposition.