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Connectivity and habitat typology drive CO 2 and CH 4 fluxes across land–water interfaces in lowland rivers
Author(s) -
Bolpagni Rossano,
Laini Alex,
Mutti Tiziana,
Viaroli Pierluigi,
Bartoli Marco
Publication year - 2019
Publication title -
ecohydrology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.982
H-Index - 54
eISSN - 1936-0592
pISSN - 1936-0584
DOI - 10.1002/eco.2036
Subject(s) - lake ecosystem , environmental science , hydrology (agriculture) , habitat , submersion (mathematics) , ecosystem , hydrobiology , water level , ecology , wetland , aquatic ecosystem , river ecosystem , atmosphere (unit) , geology , biology , mathematical analysis , geotechnical engineering , mathematics , cartography , aquatic environment , geography , differentiable function , physics , thermodynamics
Lowland rivers are assumed to be a net source of carbon dioxide (CO 2 ) and methane (CH 4 ). However, little is known about the contribution of marginal permanent and temporary riverine aquatic systems to river carbon metabolism. Elevation, in relation to flooding, hydro‐morphological, and ecological features of such habitats, can affect the gas fluxes across the water–atmosphere interfaces and the periodically air‐exposed riverbeds. This hypothesis was investigated in the lowland sector of the Po River (Northern Italy) from May to September 2008. Five different aquatic habitats were considered: the main river course; a backwater habitat; and three lateral lentic waterbodies—an oxbow and two quarry lakes of different age. The water mass was always CO 2 and CH 4 supersaturated, and gas fluxes were from the water to the atmosphere. In the highly dynamic river course and backwaters, CO 2 emission rates were nearly one order of magnitude greater than in the lentic and hypoxic oxbow and quarry lakes. By contrast, CH 4 fluxes peaked in the lentic, deeper, and permanent water bodies. At sediment–atmosphere interfaces, the CO 2 emissions increased along an organic matter, a water saturation, and a chlorophyll a gradient, attaining the maximum rates in the periodically air‐exposed riverbed and marginal sandy sediments. These differences in gas fluxes resulted from either the submersion persistence or the alternation of submersion and emersion phases, which were ultimately due to the gap between elevation and river water variations. All this stresses the critical role of marginal aquatic habitats for river C budget.