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A synoptic survey of microbial respiration, organic matter decomposition, and carbon efflux in U.S. streams and rivers
Author(s) -
Hill Brian H.,
Elonen Colleen M.,
Herlihy Alan T.,
Jicha Terri M.,
Mitchell Richard M.
Publication year - 2017
Publication title -
limnology and oceanography
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.7
H-Index - 197
eISSN - 1939-5590
pISSN - 0024-3590
DOI - 10.1002/lno.10583
Subject(s) - streams , ecoregion , environmental science , hydrology (agriculture) , sediment , total organic carbon , organic matter , stream bed , respiration , ecosystem , ecology , environmental chemistry , chemistry , geology , biology , computer network , paleontology , botany , geotechnical engineering , computer science
We analyzed ecoenzyme activities related to organic matter processing in 1879 streams and rivers across the continental U.S. as part of the USEPA's National Rivers and Streams Assessment. Ecoenzymatic stoichiometry was used to construct models for carbon use efficiency (CUE) and decomposition (− k ). Microbial respiration ( R m ) was estimated from sediment organic carbon stocks, CUE, and − k . The streams and rivers were classified by size (headwaters: 1 st ‐order; streams: 2 nd –3 rd order; small rivers: 4 th –5 th order; big rivers 6 th –7 th order; and great rivers ≥ 8 th order) and condition class (least, intermediate, and most disturbed), and grouped into nine ecoregions. There were ecoregion, stream size, and condition class effects for CUE, − k , and R m , with R m increasing from eastern ecoregions through the plains to the western ecoregions. CUE, − k , and R m decreased with increasing streams size and increased with increasing disturbance. R m , CUE, and − k were correlated with water and sediment chemistry; CUE and − k were also correlated with stream bed fine sediments; and CUE was further correlated with catchment land cover. R m was extrapolated to ecoregional and national scales, and the results suggest that microbial assemblages account for 12% of the total CO 2 outgassing, and nearly 50% of the aquatic metabolism C losses, from U.S. streams and rivers. Cumulative respiratory C losses increased from headwaters to small streams, then decreased with increasing stream size. This U‐shaped respiration curve was not evident when streams were viewed by disturbance classes, suggesting that anthropogenic disturbances mask the expected organic matter processing signature of the river continuum.