## Abstract Dissolved nitrogen (N), phosphorus (P), and organic carbon (C) were sampled along two transects in a first‐order montane tropical (2414 m.a.s.l.) rainforest catchment of the Peruvian Amazon to investigate spatial and temporal controls on nutrient concentrations from uplands to streams.
Organic carbon fluxes within and streamwater exports from headwater catchments in the southern Amazon
✍ Scribed by Mark S. Johnson; Johannes Lehmann; Evandro Carlos Selva; Mara Abdo; Susan Riha; Eduardo Guimarães Couto
- Publisher
- John Wiley and Sons
- Year
- 2006
- Tongue
- English
- Weight
- 386 KB
- Volume
- 20
- Category
- Article
- ISSN
- 0885-6087
- DOI
- 10.1002/hyp.6218
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✦ Synopsis
Abstract
Forms and quantities of organic carbon (C) fluxes at the soil surface, and organic C exports from four small (1–2 ha) headwater catchments were quantified and contrasted in the seasonally dry southern Amazon for 1 year to compare C fluxes within the terrestrial ecosystem with exports to the aquatic ecosystem. At the soil surface, the flux of litterfall C was 43 times greater than the dissolved organic carbon (DOC) flux in throughfall, with the highest rates of C deposition during the dry season. The form and timing of organic C was reversed for watershed exports, where DOC comprised 59% of the annual total organic C export, and exports were greatest during the 4‐month rainy season (63% of total annual exports). Fine particulate organic carbon (FPOC) in streamwater was a substantially larger flux than coarse particulate organic carbon (CPOC), representing 37 and 4% of total annual organic C exports, respectively. Particulate organic C exports exhibited substantial seasonal variability, with FPOC and CPOC mobilized primarily in the rainy season and strongly connected to storm events. Storm flow comprised 6% of total streamflow for the year studied, and 10% of streamflow during the rainy season. In the rainy season, over 90% of FPOC exports were transported by storm flow, while only 32% of DOC exports were exported by storm flow during this period. Streamwater DOC concentrations were found to increase linearly with increasing terrestrial litterfall during the dry season (r^2^ = 0·92, p < 0·001), indicating that in‐stream processing of allochthonous litterfall is an important source of DOC during the dry season. Copyright © 2006 John Wiley & Sons, Ltd.
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