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首页> 外文期刊>Frontiers in Marine Science >Subsurface Chlorophyll-a Maxima in the Southern Ocean
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Subsurface Chlorophyll-a Maxima in the Southern Ocean

机译:地下叶绿素 - 南海的Maxima

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Our review of the literature has revealed Southern Ocean subsurface chlorophyll-a maxima (SCMs) to be an annually recurrent feature throughout the basin. Most of these SCMs are different to the “typical” SCMs observed in the tropics, which are maintained by the nutrient-light co-limitation of phytoplankton growth. Rather, we have found that SCMs are formed by other processes including diatom aggregation, sea-ice retreat, eddies, subduction events and photo-acclimation. At a local scale, these SCMs can facilitate increased downward carbon export, primary production and food availability for higher trophic levels. A large proportion of Southern Ocean SCMs appear to be sustained by aggregates of large diatoms that form under severe iron limitation in the seasonal mixed layer. The ability of large diatoms to regulate their buoyancy must play a role in the development of these SCMs as they appear to increase buoyancy at the SCM and thus avoid further sinking with the decline of the spring bloom or naturally iron fertilised blooms. These SCMs remain largely unobserved by satellites and it seems that ship-based sampling may not be able to fully capture their biomass. In the context of the Marine Ecosystem Assessment of the Southern Ocean it is important to consider that this phenomenon is missing in our current understanding of Southern Ocean ecology and future climate scenarios. The broader implications of SCMs for Southern Ocean ecology will only be revealed through basin-wide observations. This can only be achieved through an integrated observation system that is able to harness the detailed information encapsulated in ship-based sampling, with the increased observational capacity of fluorometers on autonomous platforms such as those in the biogeochemical Argo (BGC-Argo) and the Marine Mammals Exploring the Ocean Pole to pole (MEOP) programs. The main challenge towards achieving this is the uncertainties associated with translating fluorescence to chlorophyll-a concentrations. Until this translation is resolved, the reporting of subsurface fluorescence maxima (SFMs) in place of SCMs could still yield valuable insights with careful interpretation.
机译:我们对文献的审查已经揭示了南海地下叶绿素-A最大值(SCM)在整个盆地中的每年复发特征。这些SCM中的大多数与热带地区观察到的“典型”SCM不同,这些SCMS由浮游植物生长的营养光共同限制维持。相反,我们发现SCM由其他过程形成,包括硅藻聚集,海冰撤退,eddies,俯冲事件和照片适应。在本地规模,这些SCM可以促进增加碳出口,初级生产和粮食可用性,以获得更高的营养水平。大部分南洋SCM似乎被大硅藻的聚集体持续,这些抗硅藻在季节性混合层中的严重铁限制下形成。大硅藻来调节其浮力的能力必须在这些SCM的发展中发挥作用,因为它们似乎在SCM上增加了浮力,因此避免进一步下沉,随着春天绽放的衰落或自然铁受精绽放。这些SCM在很大程度上仍然是卫星的不可观察,似乎船舶的抽样可能无法完全捕获它们的生物量。在南海的海洋生态系统评估的背景下,重要的是考虑我们目前对南洋生态和未来气候情景的了解缺失这种现象。 SCM对Southern海洋生态学的更广泛影响只会通过盆地观察揭示。这只能通过集成的观察系统来实现,该系统能够利用封装在基于船舶的采样中的详细信息,随着自主平台(如生物地球化学ARGO(BGC-ARGO)和海洋)的自治平台上增加了荧光仪的观察能力增加哺乳动物探索海洋杆到杆(MEOP)计划。实现这一目标的主要挑战是与将荧光转化为叶绿素-A浓度相关的不确定性。在解决此翻译后,归因于SCM的地下荧光最大值(SFMS)的报告仍然可以通过仔细的解释产生有价值的见解。

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