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首页> 外文期刊>Estuaries and coasts >Seasonal Oxygen Dynamics in a Warm Temperate Estuary: Effects of Hydrologic Variability on Measurements of Primary Production, Respiration, and Net Metabolism
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Seasonal Oxygen Dynamics in a Warm Temperate Estuary: Effects of Hydrologic Variability on Measurements of Primary Production, Respiration, and Net Metabolism

机译:温带季节性氧气动力学中的季节性氧气动力学:水文变异性对初级生产,呼吸和净新陈代谢测量的影响

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摘要

Seasonal responses in estuarine metabolism (primary production, respiration, and net metabolism) were examined using two complementary approaches. Total ecosystem metabolism rates were calculated from dissolved oxygen time series using Odum's open water method. Water column rates were calculated from oxygen-based bottle experiments. The study was conducted over a spring-summer season in the Pensacola Bay estuary at a shallow seagrass-dominated site and a deeper bare-bottomed site. Water column integrated gross production rates more than doubled (58.7 to 130.9 mmol O-2 m(-2) day(-1)) from spring to summer, coinciding with a sharp increase in water column chlorophyll-a, and a decrease in surface salinity. As expected, ecosystem gross production rates were consistently higher than water column rates but showed a different spring-summer pattern, decreasing at the shoal site from 197 to 168 mmol O-2 m(-2) day(-1) and sharply increasing at the channel site from 93.4 to 197.4 mmol O-2 m(-2) day(-1). The consistency among approaches was evaluated by calculating residual metabolism rates (ecosystem - water column). At the shoal site, residual gross production rates decreased from spring to summer from 176.8 to 99.1 mmol O-2 m(-2) day(-1) but were generally consistent with expectations for seagrass environments, indicating that the open water method captured both water column and benthic processes. However, at the channel site, where benthic production was strongly light-limited, residual gross production varied from 15.7 mmol O-2 m(-2) day(-1) in spring to 86.7 mmol O-2 m(-2) day(-1) in summer. The summer rates were much higher than could be realistically attributed to benthic processes and likely reflected a violation of the open water method due to water column stratification. While the use of sensors for estimating complex ecosystem processes holds promise for coastal monitoring programs, careful attention to the sampling design, and to the underlying assumptions of the m
机译:使用两种互补方法检查河口新陈代谢(初级生产,呼吸和净代谢)中的季节性反应。使用Odum的开放水法计算总生态系统代谢率。从氧气瓶实验计算水柱速率。该研究在浅景观的海湾河口的春夏,在浅海草主导地点和深入赤裸裸的网站上进行了春夏。水专栏综合生产率增加了一倍多(58.7至130.9 mmol O-2 M(-2)天(-1))从春季到夏天,致水叶绿素-A的急剧增加,表面减少盐度。正如预期的那样,生态系统总生产率始终高于水柱率,但显示出不同的春季夏季模式,从197年到168 mmol O-2 M(-2)天(-1)次数下降,并急剧增加频道位点为93.4至197.4 mmol O-2 m(-2)天(-1)。通过计算残留新陈代谢率(生态系统 - 水列)来评估方法之间的一致性。在浅滩网站,剩余的总生产率从春季到夏季减少到夏季,从176.8到99.1 mmol O-2 M(-2)天(-1),但通常与海草环境的预期一致,表明开放水方法都捕获水柱和底栖工艺。但是,在通道部位,底栖产量强烈限制,剩余生产总产量在35.7mmol O-2 m(-2)天(-1)变化,弹簧为86.7mmol O-2 m(-2)天(-1)夏天。夏季费率远远高于底栖过程的现实归因于终身过程,并且可能反映出由于水柱分层引起的违反开放水方法。虽然使用传感器来估算复杂的生态系统流程,但仍然承担沿海监控程序的承担,仔细关注采样设计,以及M的潜在假设

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