Hydrochemical characteristics and the ecological effect of algal carbonic anhydrase in carbon cycle in the Taiyuan section of Fenhe River

Jing YANG; Xin LI; Shulian XIE; Jia FENG

doi:10.1007.s00343-024-3089-x

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Hydrochemical characteristics and the ecological effect of algal carbonic anhydrase in carbon cycle in the Taiyuan section of Fenhe River

Ecology | Updated：2024-11-19

- Hydrochemical characteristics and the ecological effect of algal carbonic anhydrase in carbon cycle in the Taiyuan section of Fenhe River
- Journal of Oceanology and Limnology Vol. 42, Issue 5, Pages: 1507-1524(2024)
- Affiliations：
  
  1.Shanxi Key Laboratory of Yuncheng Salt Lake Ecological Protection and Resource Utilization, College of Life Sciences, Yuncheng University, Yuncheng044000, China
  2.School of Life Science, Shanxi University, Taiyuan030006, China
- Author bio：
  
  fengj@sxu.edu.cn
- Funds：
- DOI：10.1007.s00343-024-3089-x
  CLC：
- Received：14 May 2023，
  
  Online First：25 December 2023，
  
  Published：01 September 2024
- Accepted：
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YANG Jing,LI Xin,XIE Shulian,et al.Hydrochemical characteristics and the ecological effect of algal carbonic anhydrase in carbon cycle in the Taiyuan section of Fenhe River[J].Journal of Oceanology and Limnology,2024,42(05):1507-1524.
DOI：

YANG Jing,LI Xin,XIE Shulian,et al.Hydrochemical characteristics and the ecological effect of algal carbonic anhydrase in carbon cycle in the Taiyuan section of Fenhe River[J].Journal of Oceanology and Limnology,2024,42(05):1507-1524. DOI： 10.1007.s00343-024-3089-x.

摘要

Abstract

Water scarcity and pollution pose a threat to the sustainable development of cities and society. Therefore

it is crucial to analyze the hy

drochemical characteristics and carbon dynamics of water-deficient areas. Taking the Taiyuan section of Fenhe River as the research object

we systematically explored the hydrochemical characteristics of surface water and its evolutionary processes

as well as the ecological effect of algal carbonic anhydrase in carbon cycle using the hydrochemical evolution method and correlation analysis. The ternary diagram demonstrates that the main water chemical type in Fenhe River was SO

·Cl

-Na

. The Gibbs and end-member diagrams of each ion display that the chemical composition of surface water was mainly controlled by silicate decomposition. The chemical ions originated mainly from dissolution of some minerals

such as plagioclase

halite

dolomite

calcite

and gypsum. The diatoms had a lower CO

requirement because they exhibited a higher abundance at a lower partial pressure of CO

(

). However

high CO

concentration had a positive effect on cyanobacteria

which reduced the active transport of HCO

saved the energy needed for this part of active transport

and indirectly improved the overall photosynthetic efficiency of algae. Carbonic anhydrase (CA) activity was significantly negatively correlated with

and positively correlated with HCO

concentration

indicating that CA in water promoted the conversion of CO

to HCO

. The HCO

generated from this process continued to participate in the erosion of silicate rocks

sequestering CO

in the form of CaCO

which has a non-negligible impact on the carbon sink in the Fenhe River. These consequences may have important implications for the biogeochemical cycling occurring in urban water.

关键词

Keywords

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