Longitudinal patterns of metabolism in a southern Appalachian river

被引:63
作者
McTammany, ME [1 ]
Webster, JR [1 ]
Benfield, EF [1 ]
Neatrour, MA [1 ]
机构
[1] Virginia Polytech Inst & State Univ, Dept Biol, Blacksburg, VA 24061 USA
来源
JOURNAL OF THE NORTH AMERICAN BENTHOLOGICAL SOCIETY | 2003年 / 22卷 / 03期
关键词
primary production; respiration; river continuum concept; mid-order river; carbon budget; allochthonous input; southern Appalachians; BENTHIC COMMUNITY METABOLISM; STREAM ECOSYSTEM DYNAMICS; ORGANIC-MATTER; BLACKWATER RIVER; MACROINVERTEBRATE COMMUNITIES; PERIPHYTON PRODUCTION; CONTINUUM CONCEPT; LOW-GRADIENT; FORT-RIVER; FOOD WEBS;
D O I
10.2307/1468267
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
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 the 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 reaeration estimated by the energy dissipation method. Gross primary production (GPP) ranged from 0.07 to 1.92 g C m(-2) d(-1) and increased similar to3-fold from upstream to downstream. Respiration (R) ranged from 0.27 to 2.32 g C m(-2) d(-1) but did not change along the river continuum. Net ecosystem 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 allochthonous C sources) suggested that this heterotrophy-autotrophy shift occurred further upstream than where P/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 unmeasured C sources must be important for C dynamics in the LTR. 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.
引用
收藏
页码:359 / 370
页数:12
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