Contrasting organic matter composition in pristine and eutrophicated mangroves revealed by fatty acids and stable isotopes (Rio de Janeiro, Brazil). (31st October 2022)

• Record Type: Journal Article
• Authors: Chynel, Mathias; Rockomanovic, Sofia; Abril, Gwenaël; Barroso, Glenda; Marotta, Humberto; Machado, Wilson; Sanders, Christian J.; Thiney, Najet; Meziane, Tarik
• Is Part Of: Estuarine, coastal and shelf science. Volume 277(2022)
• Publication Date: 2022-10-31
• Subjects: Blue carbon -- Organic matter biodegradability -- Cultural eutrophication -- Microalgal blooms -- Fungi -- Bacteria; NPP: Net Primary Production -- OM: Organic Matter -- POM: Particulate Organic Matter -- SOM: Sedimentary Organic Matter -- FA: Fatty Acid -- BrFA: Branched Fatty Acid -- LCFA: Long Chain Fatty Acid -- MUFA: MonoUnsaturated Fatty Acid -- PUFA: PolyUnsaturated Fatty Acid -- SFA: Saturated Fatty Acid; Estuarine oceanography -- Periodicals; Coasts -- Periodicals; Estuarine biology -- Periodicals; Seashore biology -- Periodicals; Coasts; Estuarine biology; Estuarine oceanography; Seashore biology; Periodicals; 551.461805
• DOI: 10.1016/j.ecss.2022.108061
• Languages: English
• ISSNs: 0272-7714

Abstract

Abstract: Mangrove sediments have a high capacity of carbon storage, as the result of larger organic matter (OM) inputs from mangrove trees (litter fall and fine roots production) than OM microbial degradation and export to coastal waters. Mangrove sediments also act as traps for suspended matter and particulate OM (POM) from surrounding water masses. Fatty acids (FAs) markers, δ 13 C and δ 15 N signatures were used here to characterize the OM composition in three mangroves located in three coastal embayments of the Rio de Janeiro state (Brazil) with increasing urbanization from a pristine mangrove M1 to a moderately impacted mangrove M2 and a highly impacted mangrove M3. In these mangroves, the δ 15 N signature of tree leaves and sediments increases with anthropogenic influence, consistent with a large-scale eutrophication gradient along the three regions. At mangrove M1, predominant OM inputs from mangrove trees are highlighted by high proportions of long-chain fatty acids, particularly in the inland station, where high organic carbon concentrations (126 ± 108 mg g −1 ) indicate limited sedimentation of mineral particles and high carbon storage capacities. The sedimentary OM of M3 mangrove was more labile as confirmed by the higher proportions of algal fatty acids, enriched δ 13 C signature and the C/N ratio 1.6 times lower (p < 0.001) than in the pristine mangrove M1. At the M2 mangrove site, high contribution of bacterial FAs (around 20%) to sedimentary OM and high proportion of poorly biodegradable saturated fatty acids suggest that bacteria degrade algal labile OM in surface sediments but do not mineralize the most refractory fraction of OM. At the eutrophic M3 site, our findings suggest that deposition of labile POM induced an increase of fungal biomass on the sediment, apparently enhancing the microbial loop, and potentially leading to mineralization of refractory OM and carbon losses through a priming effect. Graphical abstract: Image 1 Highlights: The δ 15 N signatures of tree leaves and sediments show a eutrophication gradient. Sedimentary OM is more labile in highly impacted than in the pristine mangrove. Fungal proliferation may lead to carbon losses in highly impacted mangrove soils. Bacteria in the moderately impacted mangrove remineralizes labile part of OM. The inputs of litter OM drive the high carbon storage ability of pristine mangrove.