Estimates of net community production and export using high-resolution, Lagrangian measurements of O2, NO3-, and POC through the evolution of a spring diatom bloom in the North Atlantic

被引:81
作者
Alkire, Matthew B. [1 ]
D'Asaro, Eric [1 ]
Lee, Craig [1 ]
Perry, Mary Jane [2 ]
Gray, Amanda [1 ]
Cetinic, Ivona [2 ]
Briggs, Nathan [2 ]
Rehm, Eric [1 ]
Kallin, Emily [2 ]
Kaiser, Jan [3 ]
Gonzalez-Posada, Alba [3 ]
机构
[1] Univ Washington, Appl Phys Lab, Seattle, WA 98105 USA
[2] Univ Maine, Darling Marine Ctr, Walpole, ME 04573 USA
[3] Univ E Anglia, Sch Environm Sci, Norwich NR4 7TJ, Norfolk, England
基金
美国国家科学基金会;
关键词
North Atlantic; Spring bloom; Lagrangian float; Net community production; Carbon export; Sensors; PARTICULATE ORGANIC-CARBON; EXOPOLYMER PARTICLES TEP; IN-SITU; SURFACE WATERS; GAS-EXCHANGE; MIXED-LAYER; NITROGEN; OCEAN; FLUX; SEA;
D O I
10.1016/j.dsr.2012.01.012
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
Budgets of nitrate, dissolved oxygen, and particulate organic carbon (POC) were constructed from data collected on-board a Lagrangian, profiling float deployed between April 4 and May 25, 2008, as part of the North Atlantic Bloom Experiment. These measurements were used to estimate net community production (NCP) and apparent export of POC along the float trajectory. A storm resulting in deep mixing and temporary suspension of net production separated the bloom into early (April 23-27) and main (May 6-13) periods over which similar to 264 and similar to 805 mmol C m(-2) were produced, respectively. Subtraction of the total POC production from the NCP yielded maximum estimates of apparent POC export amounting to similar to 92 and 574 mmol C m(-2) during the early and main blooms, respectively. The bloom terminated the following day and similar to 282 mmol C m(-2) were lost due to net respiration (70%) and apparent export (30%). Thus, the majority of the apparent export of POC occurred continuously during the main bloom and a large respiration event occurred during bloom Termination. A comparison of the POC flux during the main bloom period with independent estimates at greater depth suggest a rapid rate of remineralization between 60 and 100 m. We suggest the high rates of remineralization in the upper layers could explain the apparent lack of carbon overconsumption (C:N > 6.6) in the North Atlantic during the spring bloom. Published by Elsevier Ltd.
引用
收藏
页码:157 / 174
页数:18
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