The response of zooplankton abundance in saline meromictic Lake Shira to a change in circulation regime

Yuri V. BARKHATOV; Alexander P. TOLOMEEV; Anton V. DROBOTOV; Egor S. ZADEREEV

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The response of zooplankton abundance in saline meromictic Lake Shira to a change in circulation regime

Special Section on Salt Lake Research | Updated：2024-10-14

- The response of zooplankton abundance in saline meromictic Lake Shira to a change in circulation regime
- Journal of Oceanology and Limnology Vol. 41, Issue 4, Pages: 1321-1330(2023)
- Affiliations：
  
  1.1.Krasnoyarsk Research Center, Institute of Biophysics, Siberian Branch of Russian Academy of Sciences, Akademgorodok, Krasnoyarsk 660036, Russia
  2.Institute of Fundamental Biology and Biotechnology, Siberian Federal University, Krasnoyarsk 660041, Russia
- Author bio：
  
  barkh@ibp.ru
- Funds：
- DOI：
  CLC：
- Received：30 March 2022，
  
  Accepted：05 May 2022，
  
  Published：01 July 2023
- Accepted：
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BARKHATOV Yuri V.,TOLOMEEV Alexander P.,DROBOTOV Anton V.,et al.The response of zooplankton abundance in saline meromictic Lake Shira to a change in circulation regime[J].Journal of Oceanology and Limnology,2023,41(04):1321-1330.
DOI：

BARKHATOV Yuri V.,TOLOMEEV Alexander P.,DROBOTOV Anton V.,et al.The response of zooplankton abundance in saline meromictic Lake Shira to a change in circulation regime[J].Journal of Oceanology and Limnology,2023,41(04):1321-1330. DOI：

摘要

Abstract

The long-term data (1996‍–‍2021) on the summer abundances of the dominant zooplankt

on species (copepod

Arctodiaptomus salinus

(Daday

1885)

rotifers

Brachionus plicatilis

(Müller

1786) and

Hexarthra

sp.) in saline Lake Shira were used to analyze the response of zooplankton to air temperature and a change in the circulation regime of the lake: breakdown and reestablishment of meromixis. All groups of zooplankton responded to prolonged summer elevated temperatures by increasing their abundance. During the breakdown of the stable stratification of Lake Shira (2015‍–‍2016)

zooplankton abundance increased on average by a factor of two and amounted to 9×10

‍inds./m

in the water column for copepods. That increase coincided with similar responses of other components of the lake’s mixolimnion ecosystem

whose biomasses increased approximately two-fold during that period. After the reestablishment of the meromixis

the abundance of zooplankton decreased to previous values. Thus

the abundance of zooplankton is largely determined by weather (the effect of temperature) and ecological factors (mixing regime).

关键词

Keywords

references

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