Energy flow in an arctic aquatic ecosystem

This component of the terrestrial-aquatic interaction group seeks to use the natural stable carbon isotope ratios and radiocarbon abundances to trace the movement of photosynthate from the terrestrial environment to the stream system at MS-117. In addition to estimating the total flux, we will also...

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Bibliographic Details
Main Author: Schell, D.M.
Other Authors: United States. Department of Energy.
Format: Report
Language:English
Published: Alaska Univ., Fairbanks, AK (United States). Inst. of Northern Engineering 1983
Subjects:
Usa
Online Access:https://doi.org/10.2172/6622241
https://digital.library.unt.edu/ark:/67531/metadc1186062/
Description
Summary:This component of the terrestrial-aquatic interaction group seeks to use the natural stable carbon isotope ratios and radiocarbon abundances to trace the movement of photosynthate from the terrestrial environment to the stream system at MS-117. In addition to estimating the total flux, we will also attempt to describe the relative fractions derived from modern primary production and that derived from delayed inputs of eroded peat. We will also seek to determine the coupling efficiency of these energy sources to the invertebrate faunal populations in the tundra soils and streams.