Planktonic ciliate trait structure variation over Yap, Mariana, and Caroline seamounts in the tropical Western Pacific Ocean

Chaofeng WANG; Haibo LI; Yi DONG; Li ZHAO; Gérald GREGORI; Yuan ZHAO; Wuchang ZHANG; Tian XIAO

doi:10.1007/s00343-021-0476-4

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Planktonic ciliate trait structure variation over Yap, Mariana, and Caroline seamounts in the tropical Western Pacific Ocean

Seamount microbial diversity and ecology | Updated：2023-04-27

- Planktonic ciliate trait structure variation over Yap, Mariana, and Caroline seamounts in the tropical Western Pacific Ocean
- Planktonic ciliate trait structure variation over Yap, Mariana, and Caroline seamounts in the tropical Western Pacific Ocean
- 海洋湖沼学报（英文） 2021年39卷第5期页码：1705-1717
- Affiliations：
  
  1.CAS Key Laboratory of Marine Ecology and Environmental Sciences, Institute of Oceanology, Chinese Academy of Sciences, Qingdao 266071, China
  2.Laboratory for Marine Ecology and Environmental Science, Pilot National Laboratory for Marine Science and Technology (Qingdao), Qingdao 266237, China
  3.Center for Ocean Mega-Science, Chinese Academy of Sciences, Qingdao 266071, China
  4.Aix-Marseille University, Toulon University, CNRS, IRD, Mediterranean Institute of Oceanology UM110, Marseille 13288, France
- Author bio：
  
  Yuan ZHAO, E-mail: yuanzhao@qdio.ac.cn
  Wuchang ZHANG, E-mail: wuchangzhang@qdio.ac.cn
- Funds：
  
  the Science & Technology Basic Resources Investigation Program of China(2017FY100803);the Strategic Priority Research Program of Chinese Academy of Sciences(XDB42000000);the China Postdoctoral Science Foundation(2020M672149);the National Key Research and Development Program of China(2017YFA0603204);the CNRS-NSFC Joint Research Projects Program(NSFC 41711530149);the 2017-2019 Sino-French Cai Yuanpei Program, and the International Cooperation Project-Dynamics and Function of Marine Microorganisms: Insight from Physics and Remote Sensing(ICP-DYF2M);© Chinese Society for Oceanology and Limnology, Science Press and Springer-Verlag GmbH Germany, part of Springer Nature 2021
- DOI：10.1007/s00343-021-0476-4
  中图分类号：
- 收稿：2020-12-15，
  
  录用：2021-2-27，
  
  网络首发：2021-04-14，
  
  纸质出版：2021-09
- Accepted：
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Planktonic ciliate trait structure variation over Yap, Mariana, and Caroline seamounts in the tropical Western Pacific Ocean[J]. 海洋湖沼学报（英文）, 2021,39(5):1705-1717.

Chaofeng WANG, Haibo LI, Yi DONG, et al. Planktonic ciliate trait structure variation over Yap, Mariana, and Caroline seamounts in the tropical Western Pacific Ocean[J]. Journal of Oceanology and Limnology, 2021, 39(5): 1705-1717.
Planktonic ciliate trait structure variation over Yap, Mariana, and Caroline seamounts in the tropical Western Pacific Ocean[J]. 海洋湖沼学报（英文）, 2021,39(5):1705-1717. DOI： 10.1007/s00343-021-0476-4.

Chaofeng WANG, Haibo LI, Yi DONG, et al. Planktonic ciliate trait structure variation over Yap, Mariana, and Caroline seamounts in the tropical Western Pacific Ocean[J]. Journal of Oceanology and Limnology, 2021, 39(5): 1705-1717. DOI： 10.1007/s00343-021-0476-4.

摘要

Abstract

Trait structure is increasingly used in plankton ecology to understand diversity and biogeography. However

our knowledge of microzooplankton (e.g. planktonic ciliates) trait structure and its variation with hydrography is limited. In this study

we analyzed planktonic ciliate trait structure in waters with different hydrography and deep Chlorophyll

maximum (DCM) layers over three seamounts: Yap

Mariana

and Caroline seamounts. Mariana seamount had a lower surface temperature than the Yap and Caroline seamounts. DCM layers over Mariana and Caroline seamounts were deeper than Yap seamount. There was a weak upwelling in upper 50 m around top of Mariana seamount. The ciliate distribution showed bimodal pattern (high abundance appeared in the surface and DCM layers) over three seamounts. At surface layer

the large size-fraction (

30 μm) abundance proportion to aloricate ciliate over Yap seamount (44.4%) was higher than Mariana (32.8%) and Caroline (36.1%) seamounts. For tintinnid abundance proportion to total ciliate

Mariana (12.0%) and Caroline (11.5%) seamounts at about 100-m depth were higher than that of Yap seamount (6.4%). Vertically

tintinnid could be divided into 4 groups over the three seamounts. At 30-m depth

group Ⅰ (species occurring from surface to 100 m only) was dominant component over Yap and Caroline seamounts

while group Ⅳ (species occurring at every depth) changed into dominant component over Mariana seamount

the weak upwelling might be the reason.

Salpingella faurei

was the top dominant species

which corresponded to deeper DCM layers over Mariana and Caroline seamounts. Our results showed that the upwelling and the deeper DCM could influence the planktonic ciliate trait structure.

关键词

Keywords

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