The estimation of gross oxygen production and community respiration from autonomous time-series measurements in the oligotrophic ocean

被引:18
|
作者
Barone, Benedetto [1 ,2 ]
Nicholson, David [1 ,3 ]
Ferron, Sara [1 ,2 ]
Firing, Eric [2 ]
Karl, David [1 ,2 ]
机构
[1] Daniel K Inouye Ctr Microbial Oceanog Res & Educ, Honolulu, HI 96822 USA
[2] Univ Hawaii Manoa, Dept Oceanog, Honolulu, HI 96822 USA
[3] Woods Hole Oceanog Inst, Marine Chem & Geochem Dept, Woods Hole, MA 02543 USA
基金
美国国家科学基金会;
关键词
NORTH PACIFIC GYRE; EUPHOTIC ZONE; MIXED-LAYER; METABOLIC BALANCE; SUBTROPICAL GYRE; CORAL-REEF; NET; SEA; VARIABILITY; DYNAMICS;
D O I
10.1002/lom3.10340
中图分类号
Q [生物科学];
学科分类号
07 ; 0710 ; 09 ;
摘要
Diel variations in oxygen concentration have been extensively used to estimate rates of photosynthesis and respiration in productive freshwater and marine ecosystems. Recent improvements in optical oxygen sensors now enable us to use the same approach to estimate metabolic rates in the oligotrophic waters that cover most of the global ocean and for measurements collected by autonomous underwater vehicles. By building on previous methods, we propose a procedure to estimate photosynthesis and respiration from vertically resolved diel measurements of oxygen concentration. This procedure involves isolating the oxygen variation due to biological processes from the variation due to physical processes, and calculating metabolic rates from biogenic oxygen changes using linear least squares analysis. We tested our method on underwater glider observations from the surface layer of the North Pacific Subtropical Gyre where we estimated rates of gross oxygen production and community respiration both averaging 1.0 mmol O-2 m(-3) d(-1), consistent with previous estimates from the same environment. Method uncertainty was computed as the standard deviation of the fitted parameters and averaged 0.6 and 0.5 mmol O-2 m(-3) d(-1) for oxygen production and respiration, respectively. The variability of metabolic rates was larger than this uncertainty and we were able to discern covariation in the biological production and consumption of oxygen. The proposed method resolved variability on time scales of approximately 1 week. This resolution can be improved in several ways including by measuring turbulent mixing, increasing the number of measurements in the surface ocean, and adopting a Lagrangian approach during data collection.
引用
收藏
页码:650 / 664
页数:15
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