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The fate of C4 and C3 macrophyte carbon in central Amazon floodplain waters: Insights from a batch experiment
- Source :
- Limnologica, Limnologica, Elsevier, 2016, 59, pp.90-98. ⟨10.1016/j.limno.2016.03.008⟩, Limnologica, 2016, 59, pp.90-98. ⟨10.1016/j.limno.2016.03.008⟩
- Publication Year :
- 2016
- Publisher :
- HAL CCSD, 2016.
-
Abstract
- The central Amazon floodplains are particularly productive ecosystems, where a large diversity of organic carbon sources are available for aquatic organisms. Despite the fact that C-4 macrophytes generally produce larger biomasses than C-3 macrophytes, food webs in the central Amazon floodplains appear dominantly based on a C-3 carbon source. In order to investigate the respective fate and degradation patterns of C-4 and C-3 aquatic plant-derived material in central Amazon floodplains, we developed a 23-days batch experiment. Fatty acid and carbon concentrations as well as stable isotope compositions were monitored over time in 60 L tanks. These tanks contained Amazon water, with different biomasses of C-3 and C-4 macrophyte, representative of in situ densities occurring in central Amazon floodplains. In the C-4 Paspalum repens treatments, organic (POC, DOC) and inorganic carbon (DIC) got rapidly enriched in C-13, whereas in the C-3 Salvinia auriculata treatments, POC and DOC showed little change in concentration and isotopic composition, and DIC got depleted in C-13. The contribution of P. repens to POC and DOC was estimated to reach up to 94.2 and 70.7%, respectively. In contrast, no differences were reported between the C-3 S. auriculata and control treatments, an observation attributed to the lower C-3 biomass encountered in the field, to a slower degradation rate of C-3 compared to C-4 compounds, and to similar isotopic compositions for river POC and DOC, and C-3 compounds. The C-13 enrichments of POC, DOC, and DIC from P. repens treatments were attributed to an enhanced bacterially-mediated hydrolysis and mineralization of C-4 material. Evolutions of bacterial abundance and branched fatty acid concentrations confirmed the role of heterotrophic microbial communities in the high P. repens decomposition rate. Our experiment highlights the predominant role of C-4 aquatic plants, as a large source of almost entirely biodegradable organic matter available for heterotrophic activity and CO2 outgassing to the atmosphere.
- Subjects :
- 0106 biological sciences
010504 meteorology & atmospheric sciences
F40 - Écologie végétale
F60 - Physiologie et biochimie végétale
[SDV]Life Sciences [q-bio]
Heterotroph
Aquatic Science
01 natural sciences
fatty acids
Degradation
Total inorganic carbon
stables isotopes
Aquatic plant
Organic matter
Ecosystem
Central amazon
Fatty acids
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces, environment
ComputingMilieux_MISCELLANEOUS
0105 earth and related environmental sciences
Central Amazon
degradation
chemistry.chemical_classification
Total organic carbon
[SDV.EE]Life Sciences [q-bio]/Ecology, environment
Ecology
010604 marine biology & hydrobiology
Floodplains
Mineralization (soil science)
15. Life on land
Macrophyte
macrophytes
Stables isotopes
Macrophytes
chemistry
floodplains
13. Climate action
Environmental chemistry
M40 - Écologie aquatique
Environmental science
Subjects
Details
- Language :
- English
- ISSN :
- 00759511
- Database :
- OpenAIRE
- Journal :
- Limnologica, Limnologica, Elsevier, 2016, 59, pp.90-98. ⟨10.1016/j.limno.2016.03.008⟩, Limnologica, 2016, 59, pp.90-98. ⟨10.1016/j.limno.2016.03.008⟩
- Accession number :
- edsair.doi.dedup.....5cd63323389586085364b00b0dfecf03