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A key challenge in climate change research is apportioning the greenhouse gas methane (CH) between various natural and anthropogenic sources. Isotopic source fingerprinting of CH releases, particularly with radiocarbon analysis, is a promising approach. Here, we establish an analytical protocol for preparing CH from seawater and other aqueous matrices for high-precision natural abundance radiocarbon measurement. Methane is stripped from water in the optionally field-operated system (STRIPS), followed by shore-based purification and conversion to carbon dioxide (CO) in the CH Isotope Preparation System (CHIPS) to allow Accelerator Mass Spectrometry analysis. The blank (±1σ) of the combined STRIPS and CHIPS is low (0.67 ± 0.12 μg C), allowing natural sample sizes down to 10 μg C-CH (i.e., 30 L samples of 40 nM CH). The full-system yield is >90% for both CH-spiked seawater and ambient samples from CH hotspots in the Baltic Sea and the Arctic Ocean. Furthermore, the radiocarbon isotope signal of CH remains constant through the multistage processing in the STRIPS and the CHIPS. The developed method thus allows for in-field sampling and sample size reduction followed by precise and CH-specific radiocarbon analysis. This enables powerful source apportionment of CH emitted from aquatic systems from the tropics to the polar regions.
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http://dx.doi.org/10.1021/acs.analchem.4c03525 | DOI Listing |
Glob Chang Biol
September 2025
Aix Marseille Univ., CNRS, IRD, INRAE, Coll France, CEREGE, Aix en Provence, France.
Soil is a major terrestrial carbon reservoir, and enhancing its carbon stock is a central strategy to mitigate climate change. Earth system models project a net soil carbon sink by 2100, the magnitude of which is still under debate, differing significantly between approaches. Radiocarbon-based studies often suggest a limited soil carbon accumulation capacity, but these estimates are biased by the presence of ancient, radiocarbon-free, organic carbon (aOC).
View Article and Find Full Text PDFMicrobiome
September 2025
Key Laboratory of Marine Genetic Resources, Third Institute of Oceanography, Ministry of Natural Resources of People's Republic of China, Xiamen, 361005, China.
Background: Mangroves are hotspots of carbon sequestration in transitional zones between marine and terrestrial ecosystems. Microbially driven dark carbon fixation (DCF) is prominent in sediments, yet our understanding of the DCF process across this continuum remains limited. In this study, we explored DCF activities and associated chemoautotrophs along the sediment depth of different mangrove sites in Fujian Province, China, using radiocarbon labeling and molecular techniques.
View Article and Find Full Text PDFRadiat Prot Dosimetry
August 2025
Medical Radiation Physics Malmö, Department of Translational Medicine, Lund University Skåne University Hospital Malmö, SUS Malmö, Inga Maria Nilssons gata 47, SE-205 02 Malmö, Sweden.
Carbon-14 often dominates the effective dose to the public from authorized discharges from Swedish nuclear power plants (NPPs). In contrast to air-borne releases, water-borne discharges of 14C are currently not routinely monitored at Swedish NPPs. We have measured 14C in Fucus spp.
View Article and Find Full Text PDFSci Rep
August 2025
Environment and Climate Change Canada, National Wildlife Research Centre, Ottawa, ON, Canada.
Rivers are major conduits that connect terrestrial carbon cycling with downstream receiving environments. In large lakes, the utilization of river-transported carbon in biological production remains poorly constrained. Lake Athabasca, the eighth largest lake in Canada, receives inflow from the Athabasca River and a large boreal wetland, the Peace-Athabasca Delta.
View Article and Find Full Text PDFProc Natl Acad Sci U S A
September 2025
Department of Environmental Science and the Bolin Centre for Climate Research, Stockholm University, Stockholm 11418, Sweden.
Black carbon (BC) aerosols exacerbate air pollution and climate warming, but their climatic impacts and sources are poorly constrained by bottom-up emission inventories (EIs). China's Clean Air Action (CAA), which was launched in 2013, provides an excellent opportunity for investigating interannual variations in source contributions and validate the accuracy of EIs. Here, we present an 11-y (2008-2018) record of the BC concentration and its source-diagnostic radiocarbon (C) and stable carbon isotope (C) signatures at a receptor site in the Pearl River Delta (PRD) region, South China.
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