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- W3012078412 abstract "Abstract Epilithic mosses are early colonizers of the terrestrial biosphere, which constitute a special ecosystem regulating rock‐atmosphere interactions. Terrestrial mosses can take up nitrate (NO 3 − ), a major form of bioavailable N, from soil substrates. However, the importance of substrate NO 3 − relative to atmospheric NO 3 − remains unclear in moss NO 3 − utilization. This has prevented the understanding of moss NO 3 − dynamics and their responses to environmental N loadings. This study investigated monthly concentrations, δ 15 N, and δ 18 O of NO 3 − in four epilithic moss species from August 2006 to August 2007 in Guiyang, southwestern China. We developed a non‐steady state isotope mass‐balance model to evaluate fractional contributions of atmospheric NO 3 − ( Ф atm ) and soil NO 3 − ( Ф soil ), moss NO 3 − uptake flux ( F influx ), moss NO 3 − reduction flux ( F reduction ), and the percentage of NO 3 − reduction in moss NO 3 − uptake ( f reduced ). The monthly Ф soil values averaged 53 ± 13% and the monthly f reduced values averaged 50 ± 35%. Both the monthly F reduction and f reduced increased as the monthly F influx increased, particularly when the Ф soil values were higher than Ф atm values. However, the amount of annual NO 3 − reduction (219.7 ± 30.5 μg‐N/g, dw) accounted for only 1.0 ± 0.2% of the bulk N of the mosses. We conclude that half of the NO 3 − in epilithic mosses is derived from the soil NO 3 − and that NO 3 − uptake from the soil induces moss NO 3 − reduction, but the total NO 3 − assimilation contributed a low fraction of the total N in the studied mosses. These findings are important for understanding N sources and N dynamics in terrestrial mosses." @default.
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- W3012078412 date "2020-06-01" @default.
- W3012078412 modified "2023-10-15" @default.
- W3012078412 title "A Non‐steady State Model Based on Dual Nitrogen and Oxygen Isotopes to Constrain Moss Nitrate Uptake and Reduction" @default.
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- W3012078412 doi "https://doi.org/10.1029/2019jg005498" @default.
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