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DOI10.1073/pnas.2004986117
Latitudinal gradient in the respiration quotient and the implications for ocean oxygen availability
Moreno A.R.; Garcia C.A.; Larkin A.A.; Lee J.A.; Wang W.-L.; Moore J.K.; Primeau F.W.; Martiny A.C.
发表日期2020
ISSN0027-8424
起始页码22866
结束页码22872
卷号117期号:37
英文摘要Climate-driven depletion of ocean oxygen strongly impacts the global cycles of carbon and nutrients as well as the survival of many animal species. One of the main uncertainties in predicting changes to marine oxygen levels is the regulation of the biological respiration demand associated with the biological pump. Derived from the Redfield ratio, the molar ratio of oxygen to organic carbon consumed during respiration (i.e., the respiration quotient, r_O2: C) is consistently assumed constant but rarely, if ever, measured. Using a prognostic Earth system model, we show that a 0.1 increase in the respiration quotient from 1.0 leads to a 2.3% decline in global oxygen, a large expansion of low-oxygen zones, additional water column denitrification of 38 Tg N/y, and the loss of fixed nitrogen and carbon production in the ocean. We then present direct chemical measurements of r_O2: C using a Pacific Ocean meridional transect crossing all major surface biome types. The observed r_O2: C has a positive correlation with temperature, and regional mean values differ significantly from Redfield proportions. Finally, an independent global inverse model analysis constrained with nutrients, oxygen, and carbon concentrations supports a positive temperature dependence of r_O2: C in exported organic matter. We provide evidence against the common assumption of a static biological link between the respiration of organic carbon and the consumption of oxygen. Furthermore, the model simulations suggest that a changing respiration quotient will impact multiple biogeochemical cycles and that future warming can lead to more intense deoxygenation than previously anticipated. © 2020 National Academy of Sciences. All rights reserved.
英文关键词CESM; Elemental stoichiometry; Inverse modeling; Photosynthetic quotient; Redfield ratio
语种英语
scopus关键词carbon; organic matter; oxygen; water; Article; biogeochemical cycle; biome; chemical analysis; concentration (parameter); denitrification; deoxygenation; environment; environmental temperature; latitude; nitrogen fixation; nutrient; oxygen consumption; priority journal; respiratory quotient; sea; warming
来源期刊Proceedings of the National Academy of Sciences of the United States of America
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/160805
作者单位Moreno, A.R., Department of Ecology and Evolutionary Biology, University of California, Irvine, CA 92697, United States; Garcia, C.A., Department of Earth System Science, University of California, Irvine, CA 92697, United States; Larkin, A.A., Department of Earth System Science, University of California, Irvine, CA 92697, United States; Lee, J.A., Department of Earth System Science, University of California, Irvine, CA 92697, United States; Wang, W.-L., Department of Earth System Science, University of California, Irvine, CA 92697, United States; Moore, J.K., Department of Earth System Science, University of California, Irvine, CA 92697, United States; Primeau, F.W., Department of Earth System Science, University of California, Irvine, CA 92697, United States; Martiny, A.C., Department of Ecology and Evolutionary Biology, University of California, Irvine, CA 92697, United States, Department of Earth System Science, University of California, Irvine, CA 92697, United States
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Moreno A.R.,Garcia C.A.,Larkin A.A.,et al. Latitudinal gradient in the respiration quotient and the implications for ocean oxygen availability[J],2020,117(37).
APA Moreno A.R..,Garcia C.A..,Larkin A.A..,Lee J.A..,Wang W.-L..,...&Martiny A.C..(2020).Latitudinal gradient in the respiration quotient and the implications for ocean oxygen availability.Proceedings of the National Academy of Sciences of the United States of America,117(37).
MLA Moreno A.R.,et al."Latitudinal gradient in the respiration quotient and the implications for ocean oxygen availability".Proceedings of the National Academy of Sciences of the United States of America 117.37(2020).
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