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Journal ArticleDOI

The Transformation of Energy by a Stream Detritivore, Pteronarcys Scotti (Plecoptera)

Wayne F. McDiffett
- 01 Nov 1970 - 
- Vol. 51, Iss: 6, pp 975-988
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TLDR
The bioenergetics of a detritus—feeding stonefly Pteronarcys scotti, were invetigated and a 17—month energy budget for the average nymph was tabulated.
Abstract
The bioenergetics of a detritus—feeding stonefly Pteronarcys scotti, were invetigated. The nymphs were collected from a north Georgia trout stream and held under simulated field conditions of temperature and photoperiod in a laboratory stream. Rates of respiration and egestion were measured at temperatures approximating those in the field at the time of collection. An estimate of the growth rate of nymphs was made from a statistical analysis of monthly field samples. Calorimetric determinations were made of nymphs, molted exoskeletons, and feces. A 17—month energy budget for the average nymph was tabulated on the basis of the data collected. Assimilation and growth efficiencies were found to be low with mean values of 10.6%, 34.2%, and 3.6% for assimilation and net and gross growth efficiencies, respectively. An assessment was made of the rate of leaf breakdown by the nymphs, and a value of approximately 29.1% of the dry body weight per day was calculated. The functional importance of the organism to the ...

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The role of macroinvertebrates in stream ecosystem function.

TL;DR: This review focuses on some of the roles of macroinvertebrate functional groups, i.e. grazers, shredders, gatherers, filterers, and predators, in stream-ecosystem processes, and the importance of their conservation.
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The stream and its valley

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Forest hydrology and ecology at Coweeta.

TL;DR: A complete review and summary of more than 50 years study of the hydrological and ecological responses of baseline and managed Southern Appalachian hardwood forests at Coweeta is provided in this article.
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Stream Ecosystem Theory: A Global Perspective

TL;DR: The idea of longitudinal succession on a geological time scale is wrong but that the concept when considered at the level of the flow-through time of a river is not, and areas where the simultaneous consideration of space and time in streams is important include longitudinal succession, climate, and disturbance.