Inundation, Hydrodynamics and Vegetation Influence Carbon Dioxide Concentrations in Amazon Floodplain Lakes

• Published in: Ecosystems (New York) Vol. 25; no. 4; pp. 911 - 930
• Main Authors: Amaral, João Henrique Fernandes, Melack, John Michael, Barbosa, Pedro Maia, Borges, Alberto V., Kasper, Daniele, Cortés, Alicia Cortes, Zhou, Wencai, MacIntyre, Sally, Forsberg, Bruce Rider
• Format: Journal Article
• Language: English
• Published: New York Springer US 01-06-2022; Springer; Springer Nature B.V
• Subjects: Analysis; Annual variations; Aquatic plants; Biomedical and Life Sciences; Carbon dioxide; Carbon dioxide concentration; Carbon sources; Chlorophyll; Ecology; Environmental Management; Exchanging; Flooding; Floodplains; Fluid dynamics; Geoecology/Natural Processes; Habitats; Hydrodynamics; Hydrology/Water Resources; Inland waters; Lakes; Life Sciences; Mathematical models; Plant Sciences; Remote sensing; Statistical models; Three dimensional models; Tropical lakes; Vegetation; Water depth; Water level fluctuations; Water levels; Water temperature; Zoology; hydrological variations; tropical floodplains; Amazon basin; aquatic plants; carbon
• ISSN: 1432-9840; 1435-0629
• DOI: 10.1007/s10021-021-00692-y

Extensive floodplains and numerous lakes in the Amazon basin are well suited to examine the role of floodable lands within the context of the sources and processing of carbon within inland waters. We measured diel, seasonal and inter-annual variations of CO
2
concentrations and related environmental variables in open water and flooded vegetation and estimated their habitat area using remote sensing in a representative Amazon floodplain lake, Lake Janauacá. Variability in CO
2
concentrations in open water resulted from changes in the extent of inundation and exchange with vegetated habitats. Depth-averaged values of CO
2
in the open water of the lake, 157 ± 91 µM (mean ± SD), were less than those in an embayment near aquatic vegetation, 285 ± 116 µM, and were variable over 24-h periods at both sites. Within floating herbaceous plant mats, the mean concentration was 275 ± 77 µM, while in flooded forests it was 217 ± 78 µM. The best statistical model that included CO
2
in aquatic plant mats, water clarity, rate of change in water level and chlorophyll-
a
concentrations explained around 90% of the variability in CO
2
concentration. Three-dimensional hydrodynamic modeling demonstrated that diel differences in water temperature between plant mats and open water as well as basin-scale motions caused lateral exchanges of CO
2
between vegetated habitats and open water. Our findings extend understanding of CO
2
in tropical lakes and floodplains with measurements and models that emphasize the importance of flooded forests and aquatic herbaceous plants fringing floodplain lakes as sources of CO
2
to open waters.