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Advances in the aquatic sciences
COMMENT AND RESPONSE

The Yellow Sea Warm Current flushes the Bohai Sea microbial community in winter

Caixia Wang https://orcid.org/0000-0003-2847-5959 A C D , Yibo Wang A B C , Pengyuan Liu A B C , Lin Wu A , James S. Paterson D , James G. Mitchell D , Andrew T. Revill E and Xiaoke Hu A C F
+ Author Affiliations
- Author Affiliations

A Key Laboratory of Coastal Biology and Bioresource Utilisation, Yantai Institute of Coastal Zone Research, Chinese Academy of Sciences, 17# Chunhui Road, Laishan District, Yantai 264003, China.

B University of Chinese Academy of Sciences, No.19(A) Yuquan Road, Shijingshan District, Beijing 100049, China.

C Laboratory for Marine Biology and Biotechnology, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266237, China.

D School of Biological Sciences, Flinders University, GPO Box 2100, Adelaide, SA 5001, Australia.

E CSIRO Oceans and Atmosphere, GPO Box 1538, Hobart, Tas. 7001, Australia.

F Corresponding author. Email: xkhu@yic.ac.cn

Marine and Freshwater Research 71(12) 1616-1627 https://doi.org/10.1071/MF19399
Submitted: 29 December 2019  Accepted: 15 May 2020   Published: 4 July 2020

Abstract

The effect of the Yellow Sea Warm Current (YSWC) on virio- and bacterioplankton communities in the Bohai Sea is unknown. In this study, the composition and dynamic changes of virio- and bacterioplankton at the entrance of the Bohai Sea were measured to determine the influence of the YSWC on those communities and vice versa. In the Bohai Strait, there were east to west gradients of water chemistry and hydrology. The turbulent mixing between the deep north-western ‘warm’ current, which is 9°C, and the cold, nutrient-rich Bohai Sea water at 7–8°C appears to stimulate the abundance of both viruses and heterotrophic bacteria, with numbers at the junction of ‘warm’ and cold water being almost 10-fold greater than in the low-thermohaline areas, and peaking where the temperature is the highest. The average viral and bacterial abundances in the north-eastern area are much higher than in the south-western area. It proved that the YSWC entered the Bohai Sea with poor biomass and exited with rich biomass, which, in turn, enriches the Yellow Sea microbial loop. Our results showed the dramatic effect of temperature rise and increasing eutrophication on microbial abundance and marine microbial communities.

Additional keywords: bacterioplankton, biomass, eutrophication, flow cytometry, virioplankton.


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