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• W2553547248 abstract "Organic matter represents a large pool of carbon in the ocean. Radiocarbon and chemical analyses suggest that larger particles are preferentially remineralized in the Pacific Ocean, with smaller particles and molecules persisting longer. Marine organic matter is one of Earth’s largest actively cycling reservoirs of organic carbon and nitrogen1,2. The processes controlling organic matter production and removal are important for carbon and nitrogen biogeochemical cycles, which regulate climate. However, the many possible cycling mechanisms have hindered our ability to quantify marine organic matter transformation, degradation and turnover rates3,4. Here we analyse existing and new measurements of the carbon:nitrogen ratio and radiocarbon age of organic matter spanning sizes from large particulate organic matter to small dissolved organic molecules. We find that organic matter size is negatively correlated with radiocarbon age and carbon:nitrogen ratios in coastal, surface and deep waters of the Pacific Ocean. Our measurements suggest that organic matter is increasingly chemically degraded as it decreases in size, and that small particles and molecules persist in the ocean longer than their larger counterparts. Based on these correlations, we estimate the production rates of small, biologically recalcitrant dissolved organic matter molecules at 0.11–0.14 Gt of carbon and about 0.005 Gt of nitrogen per year in the deep ocean. Our results suggest that the preferential remineralization of large over small particles and molecules is a key process governing organic matter cycling and deep ocean carbon storage." @default.
• W2553547248 created "2016-11-30" @default.
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• W2553547248 date "2016-11-14" @default.
• W2553547248 modified "2023-10-14" @default.
• W2553547248 title "Pacific carbon cycling constrained by organic matter size, age and composition relationships" @default.
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• W2553547248 doi "https://doi.org/10.1038/ngeo2830" @default.
• W2553547248 hasPublicationYear "2016" @default.
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