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• W2158292005 abstract "During the summers of 2002–2013, we measured rates of carbon metabolism in surface waters of six sites across a land-to-lake gradient from the upstream end of drowned river-mouth Muskegon Lake (ML) (freshwater estuary) to 19 km offshore in Lake Michigan (LM) (a Great Lake). Despite considerable inter-year variability, the average rates of gross production (GP), respiration (R) and net production (NP) across ML (604 ± 58, 222 ± 22 and 381 ± 52 µg C L−1 day−1, respectively) decreased steeply in the furthest offshore LM site (22 ± 3, 55 ± 17 and −33 ± 15 µg C L−1day−1, respectively). Along this land-to-lake gradient, GP decreased by 96 ± 1%, whereas R only decreased by 75 ± 9%, variably influencing the carbon balance along this coastal zone. All ML sites were consistently net autotrophic (mean GP:R = 2.7), while the furthest offshore LM site was net heterotrophic (mean GP:R = 0.4). Our study suggests that pelagic waters of this Great Lakes coastal estuary are net carbon sinks that transition into net carbon sources offshore. Reactive and dynamic estuarine coastal zones everywhere may contribute similarly to regional and global carbon cycles." @default.
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• W2158292005 date "2014-08-11" @default.
• W2158292005 modified "2023-10-16" @default.
• W2158292005 title "Systematically variable planktonic carbon metabolism along a land-to-lake gradient in a Great Lakes coastal zone" @default.
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• W2158292005 doi "https://doi.org/10.1093/plankt/fbu066" @default.
• W2158292005 hasPubMedCentralId "https://www.ncbi.nlm.nih.gov/pmc/articles/4226232" @default.
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