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Title: Longitudinal patterns of metabolism in a southern Appalachian river
Author(s): McTammany, M. E.; Webster, J. R.; Benfield, E. F.; Neatrour, M. A.
Date: 2003
Source: J. N. Am. Benthol Soc., 2003, 22(3), 359-370
Description: We investigated longitudinal patterns of ecosystem metabolism (primary production and respiration) at 4 sites along a 37-km segment of the Little tennessee River (LTR), North Carolina. These sites corresponded to 4th- to 6th- order reaches in the LTR in an attempt to identify thr transition from heterotrophic to autotrophic conditions in this river ecosystem. In addition, we compared autochthonous C production to supply of coarse organic material from direct litter fall and entrainment from the floodplain during floods to determine the contributions of each to river energetics on an annual basis. Metabolism was measured at several times of year at each site using the single-station diel oxygen change method and reaerations estimated by the engergy dissipation method. Gross primary production (GPP) ranged from 0.07 to 1.92 G C m-2d-1 and increased ~3-fold from upstream to downstream. Respiration (R) ranged from 0.27 to 2.32 G C m-2d-1 but did not change along the river continuum. Net ecysystem production {NEP} and P/R consistently showed that metabolism was heterotrophic in upstream sites and became autotrophic in the site furthest downstream. Calculated transitional P/R ( i e , where heterotrophic respiration is supported equally by autochthonous and allochtlionous C sources) suggested that this heterotrophy--autotrophy shift occurred further upstream than where I/R = 1. Annual rates of GPP were 3 times higher than litter fall and floodplain Inputs of C, but R was higher than total C input suggesting that unineasured C sources must be important for C dynamics in the ITR. the difference between measured C inputs and R decreased along the river continuum because of a 3-fold increase in GPP with little change in allochthonous input and R. Our results suggest that the LTR changes from heterotrophic to autotrophic along this stretch of river and that autochthonous C sources become more important for respiration and secondary production at downstream sites.
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