The impact of eddies and spring warm pool on sinking rates of phytoplankton with different shapes and sizes

IF 2.1 3区 生物学 Q2 MARINE & FRESHWATER BIOLOGY
{"title":"The impact of eddies and spring warm pool on sinking rates of phytoplankton with different shapes and sizes","authors":"","doi":"10.1007/s00227-024-04415-4","DOIUrl":null,"url":null,"abstract":"<h3>Abstract</h3> <p>Slowly sinking small particles in surface seawater are proven to be one of the major contributors to the mesopelagic carbon flux. Phytoplankton can respond rapidly to changes in the marine environment, so assessing the efficiency of their downward export can better constrain the relationship between carbon biomass and sinking fluxes. Here, we measured the sinking rates of individual phytoplankton (<em>φ</em><sub>indiv</sub>) after being subjected to Luzon cold eddy (LCE), warm eddy (WE) and spring warm pool (SWP), and explored the main influencing factors affecting cell sinking. The <em>φ</em><sub>indiv</sub> in the euphotic zone of the central South China Sea (ceSCS) was measured using the SETCOL method during the inter-monsoon period in April 2017. Diatoms (mainly rod-shaped) were sinking faster under the influence of SWP, with the highest carbon fluxes in the surface layer; WE leading to slow sinking of dinoflagellates, rapid sinking of cyanobacteria and a significant reduction in the number of phytoplankton species; diatoms sinking slowly due to the LCE. The <em>φ</em><sub>indiv</sub> of cylinder-shaped and rhombus-shaped cells in diatoms and fusiform-shaped and ellipsoid-shaped cells in dinoflagellates were significantly modulated by cell size. The setae structure of <em>Chaetoceros</em> can modulate the sinking behavior well in different environments. Our results indicate that in the open ocean, the shape and size of cells, the unique ecological niches of different species, and the original localization of cells are essential for the modulation of sinking.</p>","PeriodicalId":18365,"journal":{"name":"Marine Biology","volume":"233 1","pages":""},"PeriodicalIF":2.1000,"publicationDate":"2024-03-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Marine Biology","FirstCategoryId":"99","ListUrlMain":"https://doi.org/10.1007/s00227-024-04415-4","RegionNum":3,"RegionCategory":"生物学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"MARINE & FRESHWATER BIOLOGY","Score":null,"Total":0}
引用次数: 0

Abstract

Slowly sinking small particles in surface seawater are proven to be one of the major contributors to the mesopelagic carbon flux. Phytoplankton can respond rapidly to changes in the marine environment, so assessing the efficiency of their downward export can better constrain the relationship between carbon biomass and sinking fluxes. Here, we measured the sinking rates of individual phytoplankton (φindiv) after being subjected to Luzon cold eddy (LCE), warm eddy (WE) and spring warm pool (SWP), and explored the main influencing factors affecting cell sinking. The φindiv in the euphotic zone of the central South China Sea (ceSCS) was measured using the SETCOL method during the inter-monsoon period in April 2017. Diatoms (mainly rod-shaped) were sinking faster under the influence of SWP, with the highest carbon fluxes in the surface layer; WE leading to slow sinking of dinoflagellates, rapid sinking of cyanobacteria and a significant reduction in the number of phytoplankton species; diatoms sinking slowly due to the LCE. The φindiv of cylinder-shaped and rhombus-shaped cells in diatoms and fusiform-shaped and ellipsoid-shaped cells in dinoflagellates were significantly modulated by cell size. The setae structure of Chaetoceros can modulate the sinking behavior well in different environments. Our results indicate that in the open ocean, the shape and size of cells, the unique ecological niches of different species, and the original localization of cells are essential for the modulation of sinking.

漩涡和泉水暖池对不同形状和大小浮游植物下沉率的影响
摘要 表层海水中缓慢下沉的小颗粒被证明是中层海水碳通量的主要贡献者之一。浮游植物可以对海洋环境的变化做出快速反应,因此评估浮游植物向下输出的效率可以更好地制约碳生物量与下沉通量之间的关系。在此,我们测量了单个浮游植物在经历吕宋冷涡(LCE)、暖涡(WE)和春季暖池(SWP)后的下沉率(φindiv),并探讨了影响细胞下沉的主要影响因素。利用 SETCOL 方法测量了 2017 年 4 月季风间歇期南海中部(ceSCS)极光带的φindiv。硅藻(主要为杆状)在SWP影响下下沉较快,表层碳通量最高;WE导致甲藻下沉缓慢,蓝藻下沉较快,浮游植物种类明显减少;硅藻受LCE影响下沉缓慢。硅藻的圆柱形和菱形细胞以及甲藻的纺锤形和椭圆形细胞的φindiv受细胞大小的影响很大。Chaetoceros的刚毛结构可以很好地调节在不同环境中的下沉行为。我们的研究结果表明,在开阔的海洋中,细胞的形状和大小、不同物种独特的生态位以及细胞的原始定位是调节下沉的关键。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 求助全文
来源期刊
Marine Biology
Marine Biology 生物-海洋与淡水生物学
CiteScore
4.20
自引率
8.30%
发文量
133
审稿时长
3-6 weeks
期刊介绍: Marine Biology publishes original and internationally significant contributions from all fields of marine biology. Special emphasis is given to articles which promote the understanding of life in the sea, organism-environment interactions, interactions between organisms, and the functioning of the marine biosphere.
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术官方微信