CSIR- National Institute of Oceanography, Regional Centre, Kochi, India; Bharathidasan University, Tiruchirappalli, India.
CSIR- National Institute of Oceanography, Regional Centre, Kochi, India.
Mar Environ Res. 2023 May;187:105972. doi: 10.1016/j.marenvres.2023.105972. Epub 2023 Mar 31.
Phytoplankton size classes (PSCs) are important in marine ecosystems because they organise the food chain and trophic pathways, which determine the overall biological environment. Based on three FORV Sagar Sampada cruises, the current study provides changes in PSCs in the Northeastern Arabian Sea (NEAS; north of 18 N) during different phases of the Northeast Monsoon [NEM (November-February)]. During all three phases of NEM such as early (November), peak (December), and late (February), in-situ chlorophyll-a fractionation data revealed that nanoplankton (2-20 μm) predominated, followed by microplankton (>20 μm) and picoplankton (0.2-2.0 μm). This was primarily because winter convective mixing in the NEAS maintains only a moderate level of nutrients in the surface mixed layer, which is more conducive to the dominance of nanoplankton. Brewin et al. (2012) and Sahay et al. (2017) have satellite-based PSC estimation algorithms; the former was developed for the entire Indian Ocean, while the latter is a modification of the former for the Noctiluca bloom-infested NEAS, with a claim that such blooms are typical of the NEM. When current in-situ PSCs data were compared to algorithm-based NEM data, Brewin et al. (2012) revealed a more realistic PSCs contribution pattern, especially in oceanic waters, with nanoplankton predominating except during early NEM. But the PSCs data from Sahay et al. (2017) showed a high degree of variation from the in-situ data, demonstrating the dominance of pico- and microplankton and a notably small contribution from the nano phytoplankton. The current study showed that Sahay et al. (2017) is inferior to Brewin et al. (2012) at quantifying PSCs in the NEAS without Noctiluca blooms, and provided evidence to show that Noctiluca blooms are not a typical feature of the region during the NEM.
浮游植物大小类群(PSCs)在海洋生态系统中很重要,因为它们组织食物链和营养途径,从而决定整体生物环境。基于 FORV Sagar Sampada 号的三次航行,本研究提供了东北季风期间(11 月至 2 月)北印度洋东北部(18°N 以北)PSC 的变化。在东北季风的所有三个阶段(早期、高峰和晚期),包括 11 月、12 月和 2 月,现场叶绿素-a 分馏数据表明,纳米浮游植物(2-20μm)占主导地位,其次是微浮游植物(>20μm)和微微浮游植物(0.2-2.0μm)。这主要是因为东北印度洋冬季对流混合仅将营养物质维持在表层混合层的中等水平,这更有利于纳米浮游植物的优势地位。Brewin 等人(2012 年)和 Sahay 等人(2017 年)有基于卫星的 PSC 估算算法;前者是为整个印度洋开发的,后者是前者针对受夜光藻爆发影响的东北印度洋的改进版本,据称这种爆发是东北季风的典型特征。当将当前现场 PSCs 数据与基于算法的东北季风数据进行比较时,Brewin 等人(2012 年)揭示了一种更现实的 PSCs 贡献模式,特别是在海洋水域,纳米浮游植物占主导地位,除了在东北季风的早期。但是,Sahay 等人(2017 年)的 PSCs 数据与现场数据相比存在很大差异,表明微微浮游植物和微浮游植物占主导地位,纳米浮游植物的贡献明显较小。本研究表明,在没有夜光藻爆发的情况下,Sahay 等人(2017 年)在东北印度洋定量 PSCs 方面不如 Brewin 等人(2012 年),并提供证据表明,夜光藻爆发不是该地区东北季风期间的典型特征。