TY - JOUR
T1 - Using multi-tracer inference to move beyond single-catchment ecohydrology
AU - Abbott, B.W.
AU - Baranov, V.
AU - Mendoza-Lera, C.
AU - Nikolakopoulou, M.
AU - Harjung, A.
AU - Kolbe, T.
AU - Balasubramanian, M.N.
AU - Vaessen, T.N.
AU - Ciocca, F.
AU - Campeau, A.
AU - Wallin, M.B.
AU - Romeijn, P.
AU - Antonelli, M.
AU - Gonçalves, J.
AU - Datry, T.
AU - Laverman, A.M.
AU - de Dreuzy, J.R.
AU - Hannah, D.M.
AU - Krause, S.
AU - Oldham, Carolyn
AU - Pinay, G.
PY - 2016
Y1 - 2016
N2 - © 2016 The AuthorsProtecting or restoring aquatic ecosystems in the face of growing anthropogenic pressures requires an understanding of hydrological and biogeochemical functioning across multiple spatial and temporal scales. Recent technological and methodological advances have vastly increased the number and diversity of hydrological, biogeochemical, and ecological tracers available, providing potentially powerful tools to improve understanding of fundamental problems in ecohydrology, notably: 1. Identifying spatially explicit flowpaths, 2. Quantifying water residence time, and 3. Quantifying and localizing biogeochemical transformation. In this review, we synthesize the history of hydrological and biogeochemical theory, summarize modern tracer methods, and discuss how improved understanding of flowpath, residence time, and biogeochemical transformation can help ecohydrology move beyond description of site-specific heterogeneity. We focus on using multiple tracers with contrasting characteristics (crossing proxies) to infer ecosystem functioning across multiple scales. Specifically, we present how crossed proxies could test recent ecohydrological theory, combining the concepts of hotspots and hot moments with the Damköhler number in what we call the HotDam framework.
AB - © 2016 The AuthorsProtecting or restoring aquatic ecosystems in the face of growing anthropogenic pressures requires an understanding of hydrological and biogeochemical functioning across multiple spatial and temporal scales. Recent technological and methodological advances have vastly increased the number and diversity of hydrological, biogeochemical, and ecological tracers available, providing potentially powerful tools to improve understanding of fundamental problems in ecohydrology, notably: 1. Identifying spatially explicit flowpaths, 2. Quantifying water residence time, and 3. Quantifying and localizing biogeochemical transformation. In this review, we synthesize the history of hydrological and biogeochemical theory, summarize modern tracer methods, and discuss how improved understanding of flowpath, residence time, and biogeochemical transformation can help ecohydrology move beyond description of site-specific heterogeneity. We focus on using multiple tracers with contrasting characteristics (crossing proxies) to infer ecosystem functioning across multiple scales. Specifically, we present how crossed proxies could test recent ecohydrological theory, combining the concepts of hotspots and hot moments with the Damköhler number in what we call the HotDam framework.
U2 - 10.1016/j.earscirev.2016.06.014
DO - 10.1016/j.earscirev.2016.06.014
M3 - Article
VL - 160
SP - 19
EP - 42
JO - Earth-Science Reviews
JF - Earth-Science Reviews
SN - 0012-8252
ER -