TY - JOUR
T1 - Ecological, landscape, and climatic regulation of sediment geochemistry in North American sockeye salmon nursery lakes
T2 - Insights for paleoecological salmon investigations
AU - Selbie, Daniel T.
AU - Finney, Bruce P.
AU - Barto, David
AU - Bunting, Lynda
AU - Chen, Guangjie
AU - Leavitt, Peter R.
AU - Maclsaac, Erland A.
AU - Schindler, Daniel E.
AU - Shapley, Mark D.
AU - Gregory-Eaves, Irene
PY - 2009/9
Y1 - 2009/9
N2 - We used multiple linear regressions across a Northeast Pacific region 56-lake set to examine the influence of sockeye salmon spawner densities and limnological, climatic, and watershed characteristics on sediment stable nitrogen isotope (δ15N) and C:N signatures, geochemical proxies used in paleolimnological reconstructions of prehistoric salmon abundances. Across all sites (n = 56), sedimentary C:N was primarily related to variables reflecting allochthonous organic matter and nutrient fluxes, with 67% of the variance explained by watershed vegetation type, watershed area, mean slope, and salmon spawner densities. In a subset of sites with nutrient data (n = 41), 63% of variance in C: N was explained by precipitation and watershed vegetation type. Sediment <515N was most strongly related to salmon spawner densities, but C:N and watershed area: lake area ratios explained significant residual variance (total 55%). In sites with nutrient data, salmon spawner densities, vegetation type, and spring nitrate explained 62% of the variance in δ15N. Sediment C: N and δ15N values exhibited distinct interregional variation, typically varying inversely. Regional δ15N-salmon density relationships (regression slopes) varied strongly with total annual precipitation (r2 = 0.89, p = 0.016, n = 5), suggesting watershed organic matter and nutrient loading vary predictably in relation to regional biogeoclimatic conditions. Our findings demonstrate that paleolimnological analyses are useful for quantitative reconstruction of past salmon densities; however, inferences regarding past salmon populations must consider the factors regulating influxes of nitrogen from watershed sources.
AB - We used multiple linear regressions across a Northeast Pacific region 56-lake set to examine the influence of sockeye salmon spawner densities and limnological, climatic, and watershed characteristics on sediment stable nitrogen isotope (δ15N) and C:N signatures, geochemical proxies used in paleolimnological reconstructions of prehistoric salmon abundances. Across all sites (n = 56), sedimentary C:N was primarily related to variables reflecting allochthonous organic matter and nutrient fluxes, with 67% of the variance explained by watershed vegetation type, watershed area, mean slope, and salmon spawner densities. In a subset of sites with nutrient data (n = 41), 63% of variance in C: N was explained by precipitation and watershed vegetation type. Sediment <515N was most strongly related to salmon spawner densities, but C:N and watershed area: lake area ratios explained significant residual variance (total 55%). In sites with nutrient data, salmon spawner densities, vegetation type, and spring nitrate explained 62% of the variance in δ15N. Sediment C: N and δ15N values exhibited distinct interregional variation, typically varying inversely. Regional δ15N-salmon density relationships (regression slopes) varied strongly with total annual precipitation (r2 = 0.89, p = 0.016, n = 5), suggesting watershed organic matter and nutrient loading vary predictably in relation to regional biogeoclimatic conditions. Our findings demonstrate that paleolimnological analyses are useful for quantitative reconstruction of past salmon densities; however, inferences regarding past salmon populations must consider the factors regulating influxes of nitrogen from watershed sources.
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U2 - 10.4319/lo.2009.54.5.1733
DO - 10.4319/lo.2009.54.5.1733
M3 - Article
AN - SCOPUS:67949097238
SN - 0024-3590
VL - 54
SP - 1733
EP - 1745
JO - Limnology and Oceanography
JF - Limnology and Oceanography
IS - 5
ER -