Kang Jae Joong, Jang Hyo Keun, Lim Jae-Hyun, Lee Dabin, Lee Jae Hyung, Bae Hyeonji, Lee Chang Hwa, Kang Chang-Keun, Lee Sang Heon
Department of Oceanography, Pusan National University, Busan, South Korea.
East Sea Fisheries Research Institute, National Institute of Fisheries Science, Gangneung, South Korea.
Front Microbiol. 2020 Dec 21;11:560102. doi: 10.3389/fmicb.2020.560102. eCollection 2020.
The current phytoplankton community structure is expected to change, with small phytoplankton becoming dominant under ongoing warming conditions. To understand and evaluate the ecological roles of small phytoplankton in terms of food quantity and quality, the carbon uptake rates and intracellular biochemical compositions (i.e., carbohydrates, CHO; proteins, PRT; and lipids, LIP) of phytoplankton of different sizes were analyzed and compared in two different regions of the western East/Japan Sea (EJS): the Ulleung Basin (UB) and northwestern East/Japan Sea (NES). The average carbon uptake rate by the whole phytoplankton community in the UB (79.0 ± 12.2 mg C m h) was approximately two times higher than that in the NES (40.7 ± 2.2 mg C m h), although the average chlorophyll (chl ) concentration was similar between the UB (31.0 ± 8.4 mg chl m) and NES (28.4 ± 7.9 mg chl m). The main reasons for the large difference in the carbon uptake rates are believed to be water temperature, which affects metabolic activity and growth rate, and the difference in euphotic depths. The contributions of small phytoplankton to the total carbon uptake rate were not significantly different between the regions studied. However, the rate of decrease in the total carbon uptake with increasing contributions from small phytoplankton was substantially higher in the UB than in the NES. This result suggests that compared to other regions in the EJS, the primary production in the UB could decrease rapidly under ongoing climate change. The calorific contents calculated based on biochemical compositions were similar between the small (1.01 ± 0.33 Kcal m) and large (1.14 ± 0.36 Kcal m) phytoplankton in the UB, whereas the biochemical contents were higher in the large phytoplankton (1.88 ± 0.54 Kcal m) than in the small phytoplankton (1.06 ± 0.18 Kcal m) in the NES. The calorific values per unit of chl were higher for the large phytoplankton than for the small phytoplankton in both regions, which suggests that large phytoplankton could provide a more energy efficient food source to organisms in higher trophic levels in the western EJS.
预计当前的浮游植物群落结构将会发生变化,在持续变暖的条件下,小型浮游植物将占主导地位。为了从食物数量和质量方面理解和评估小型浮游植物的生态作用,对日本海西部两个不同区域,即郁陵盆地(UB)和日本海西北部(NES)中不同大小浮游植物的碳吸收速率和细胞内生化组成(即碳水化合物,CHO;蛋白质,PRT;以及脂质,LIP)进行了分析和比较。UB中整个浮游植物群落的平均碳吸收速率(79.0±12.2毫克碳/平方米·小时)大约是NES(40.7±2.2毫克碳/平方米·小时)的两倍,尽管UB(31.0±8.4毫克叶绿素a/平方米)和NES(28.4±7.9毫克叶绿素a/平方米)之间的平均叶绿素a浓度相似。碳吸收速率存在巨大差异的主要原因据信是水温,其影响代谢活动和生长速率,以及真光层深度的差异。在所研究的区域之间,小型浮游植物对总碳吸收速率的贡献没有显著差异。然而,随着小型浮游植物贡献的增加,总碳吸收的下降速率在UB中比在NES中要高得多。这一结果表明,与日本海的其他区域相比,在持续的气候变化下,UB中的初级生产力可能会迅速下降。基于生化组成计算的热值在UB中的小型(1.01±0.33千卡/平方米)和大型(1.14±0.36千卡/平方米)浮游植物之间相似,而在NES中,大型浮游植物(1.88±0.54千卡/平方米)的生化含量高于小型浮游植物(1.06±0.18千卡/平方米)。在两个区域中,大型浮游植物每单位叶绿素a的热值都高于小型浮游植物,这表明大型浮游植物可以为日本海西部较高营养级的生物提供更具能量效率的食物来源。