Geochemistry of organic matter by multi-proxy analyses and temperature sensitivity of methanogenesis in clearwater Amazonian lake sediments. (November 2022)

• Record Type: Journal Article
• Authors: Pereira, Vinícius B.; Lopes, Alexander A.; Dal Sasso, Marco Aurelio; Amora-Nogueira, Leonardo; Fonseca, Thairiny; Marotta, Humberto; Cordeiro, Renato C.; Azevedo, Débora A.
• Is Part Of: Applied geochemistry. Volume 146(2022)
• Publication Date: 2022-11
• Subjects: Lipid biomarkers -- Amazon basin -- Sedimentary organic matter -- Organic matter preservation -- Global warming -- Tropical environments; Environmental geochemistry -- Periodicals; Water chemistry -- Periodicals; Geochemistry -- Social aspects -- Periodicals; Geochemistry -- Periodicals; 551.9
• DOI: 10.1016/j.apgeochem.2022.105467
• Languages: English
• ISSNs: 0883-2927

Abstract

Abstract: Despite the relevance of bottom sediments from clearwater floodplain lakes in organic matter preservation and degradation, there is a scarcity of data regarding the composition of molecular biomarkers and responses of benthic methanogenesis in Amazonian lakes in global warming scenarios. Here, surface sediments from a small clearwater floodplain lake (Jacundá Lake) in the Brazilian Amazon (Tapajós River) were assessed in a combined approach between molecular biomarker composition and the sensitivity of methanogenesis under two experimental temperatures: 25 °C as control vs. + 4 °C as an Intergovernmental Panel on Climate Change (IPCC) global warming scenario for 2081–2100. Lipid biomarker composition ( n -alkanes, sterols) in a 12-cm sediment core revealed a strong predominance of terrestrial-derived organic matter over aquatic contributions, indicating more refractory preserved organic matter, while aquatic organic matter represents substrates to biological degradation. Moreover, alkanoic acids and microbial triterpenoids indicated an intense microbial contribution and elevated organic matter processing. Compound specific isotopic analysis confirmed the presence of methanotrophic microorganisms (diploptene δ 13 C = −53.5‰) and an uptake of depleted 13 C in aquatic organic matter. Diagenetic transformation of biomarkers also indicated a highly anoxic depositional environment throughout the core. Methanogenesis in the upper 15-cm sediment layer under 25 °C (39.3 mg C–CH4 m −2 d −1 ) was similar to higher rates reported in Amazonian lakes and increased about 60% in the treatment when the temperature increased by 4 °C. Despite the predominant terrestrial sources and subsequent refractory composition of organic matter, our findings integrating biomarkers and metabolic processes support that biomass stocks in clearwater lake sediments of the Amazon basin may be sensitive to global warming. Graphical abstract: Image 1 Highlights: Multi-proxy biomarkers reveal new understanding on diagenesis of refractory OM. Dominance of terrestrial OM associated with sediment anoxia and 13 C depletion. High temperature sensitivity on methanogenesis in a clearwater Amazonian lake. Diagenetic signature and CH4 production rates indicate highly anoxic environment.