Weston K, Fernand L, Nicholls J, Marca-Bell A, Mills D, Sivyer D, Trimmer M
Laboratory of Global Marine and Atmospheric Chemistry, School of Environmental Sciences, University of East Anglia, Norwich, Norfolk NR4 7TJ, UK.
Mar Environ Res. 2008 Apr;65(3):235-49. doi: 10.1016/j.marenvres.2007.11.002. Epub 2007 Nov 12.
The purpose of this research was to investigate the potential causes of low oxygen levels in the bottom water of the Oyster Grounds region of the shallow southern North Sea, an area which provides suitable conditions for low oxygen levels to develop. At the end of the summer stratified period, relevant biogeochemical processes were investigated using a combination of sedimentary and water column rate measurements. Phytoplankton nitrate and ammonium uptake was measured throughout the water column using (15)N labelled isotopes and showed ammonium uptake dominated in the upper and bottom mixed layer with a maximum 294.4 micromol N m(-3)h(-1). In the deep chlorophyll maximum at the thermocline, primary production was dominated by nitrate uptake, with an average of 35.0 micromol N m(-3)h(-1), relative to ammonium uptake, with an average of 24.6 micromol N m(-3)h(-1). This high relative nitrate uptake will in part result in exportable new production to the isolated bottom mixed layer and sediments, as opposed to regenerated ammonium driven uptake. This biomass export was indicated by significant benthic oxygen consumption rates in the stratified region (782-1275 micromol O(2)m(-2)h(-1)micromol N m(-3)h(-1)) long after the end of the spring bloom. The sediments were also an active net source of nitrate, ammonium, phosphate and silicate into the bottom mixed layer of 4.4, 8.4, 2.3 and 68.8 micromol m(-2)h(-1), respectively. The export of new production within the thermocline to the bottom mixed layer and the consequent sediment oxygen consumption in the isolated bottom mixed layer in the Oyster Grounds are expected to have contributed to the low bottom water oxygen concentrations of 2.07 mg l(-1) (64.7 micromol l(-1)) measured. The long stratified period associated with this low oxygen is predicted to occur more regularly in the future and continued monitoring of this ecologically important region is therefore essential if the causes of these potentially damaging low oxygen levels are to be fully understood.
本研究的目的是调查北海南部浅海牡蛎滩区域底层水低氧水平的潜在成因,该区域具备低氧水平形成的适宜条件。在夏季分层期末,通过沉积速率和水柱速率测量相结合的方法,对相关生物地球化学过程进行了研究。利用¹⁵N标记同位素测量了整个水柱中浮游植物对硝酸盐和铵的吸收情况,结果表明,在上层和底层混合层中,铵的吸收占主导地位,最大值为294.4微摩尔氮·米⁻³·小时⁻¹。在温跃层的深度叶绿素最大值处,初级生产以硝酸盐吸收为主,平均为35.0微摩尔氮·米⁻³·小时⁻¹,相对于铵的吸收,平均为24.6微摩尔氮·米⁻³·小时⁻¹。这种较高的相对硝酸盐吸收量将部分导致可输出的新生产量输送到孤立的底层混合层和沉积物中,这与由再生铵驱动的吸收情况相反。在春季水华结束很久之后,分层区域显著的底栖生物耗氧率(782 - 1275微摩尔氧·米⁻²·小时⁻¹·微摩尔氮·米⁻³·小时⁻¹)表明了这种生物量的输出。沉积物也是硝酸盐、铵、磷酸盐和硅酸盐进入底层混合层的活跃净源,分别为4.4、8.4、2.3和68.8微摩尔·米⁻²·小时⁻¹。预计在牡蛎滩区域,温跃层内新生产量向底层混合层的输出以及随之而来的孤立底层混合层中的沉积物耗氧,促成了所测得的底层水低氧浓度2.07毫克/升(64.7微摩尔/升)。预计与这种低氧相关的长时间分层期在未来会更频繁地出现,因此,如果要充分了解这些潜在有害的低氧水平的成因,持续监测这个具有生态重要性的区域至关重要。