Integrated carbon budgets of terrestrial and aquatic ecosystems indicate that particulate organic carbon (POC) plays an important role in the transport, storage, and turnover of carbon during its transit from land to sea. However, little is known about the rates at which POC in suspension is metabolized during downstream transport. We address this deficiency by improving existing respiration methods and models to assess the biological lability of POC suspended in a headwater stream. Our method involves concentration of stream particles by tangential flow filtration, extended incubations (35-40 d) using conditions to ensure particle suspension and prevent particle aggregation, correction for the simultaneous respiration of dissolved organic carbon, and conversion from oxygen measurements into carbon with a respiratory oxidation ratio (OR) of 1.30 O 2 :C. We include analysis of the choice of OR. The POC turnover times estimated with the improved methods in this study are ~10 days. These respiration rates are among the highest reported for either suspended or benthic POC in streams and suggest that suspended POC is mineralized closer to its point of origin than was previously assumed. During incubation, keeping POC in suspension can increase respiration rates as much as 2-fold compared with allowing particles to settle and physical inhibition of POC aggregation can increase rates by 1.2-fold compared with allowing POC to aggregate. Methods that explicitly incorporate suspension and discourage aggregation of POC and longer incubation times during respiration measurements will generate data that improve our understanding of the dynamic role of POC in aquatic ecosystems.*Corresponding author: E-mail: richardsond@newpaltz.edu
AcknowledgmentsThe research was funded by grants DEB-0404860, DEB-0424681, and DEB-0543526 from the U.S. National Science Foundation. We thank Stephanie Dix, Dave Funk, Sara Geleskie, Mike Gentile, Sue Herbert, Karen Hogan, and Sherman Roberts for field and laboratory assistance and Kathryn Cappillino for scientific illustration. We thank Margaret Palmer, Laura Craig, and two anonymous reviewers for suggestions that greatly improved earlier versions of this manuscript.DOI 10.4319/lom.2013.11.247 Limnol. Oceanogr.: Methods 11, 2013, 247-261 © 2013, by the American Society of Limnology and Oceanography, Inc.
LIMNOLOGY and OCEANOGRAPHY: METHODSperiods (<24 h) to avoid anoxia. Rates are typically reported as mass of oxygen consumed per initial mass of carbon per unit time (e.g., Naiman and Sedell 1979;Webster et al. 1999) and converted to carbon turnover time using a molar respiratory oxidation ratio (OR = O 2 :CO 2 ) of 1.0 mol of O 2 per mol of C (Webster et al. 1999).There are a number of reasons to suspect that estimates of stream POC mineralization rates and turnover times determined with these methods and calculations do not reflect the in situ rates of POC in transport through stream networks. Due to hydrodynamic particle sorting, the physical, chemical, and biological properties of be...