Nutrient and chlorophyll a anomaly in red-tide periods of 2003–2008 in Sishili Bay, China

Yanju Hao; Danling Tang; Long Yu; Qianguo Xing

doi:10.1007/s00343-011-0179-3

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Nutrient and chlorophyll a anomaly in red-tide periods of 2003–2008 in Sishili Bay, China

Updated：2023-05-16

- Nutrient and chlorophyll a anomaly in red-tide periods of 2003–2008 in Sishili Bay, China
- Journal of Oceanology and Limnology Vol. 29, Issue 3, Pages: 664-673(2011)
- Affiliations：
  
  1. Yantai Institute of Coastal Zone Research Chinese Academy of Sciences
  2. Research Center of Remote Sensing and Marine Ecology/Environment (RSMEE) Key Laboratory of Tropical Marine Environmental Dynamics (LED) South China Sea Institute of Oceanology Chinese Academy of Sciences
  3. Graduate University of Chinese Academy of Sciences
  4. Monitoring and Forecasting Center of the Oceanic Environment of Yantai
- Author bio：
- Funds：
- DOI：10.1007/s00343-011-0179-3
  CLC：
- Online First：15 May 2011，
  
  Published：2011
- Accepted：
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Hao, Y., Tang, D., Yu, L. et al. Nutrient and chlorophyll a anomaly in red-tide periods of 2003–2008 in Sishili Bay, China., Chin. J. Ocean. Limnol. 29, 664–673 (2011). https://doi.org/10.1007/s00343-011-0179-3
DOI：

Hao, Y., Tang, D., Yu, L. et al. Nutrient and chlorophyll a anomaly in red-tide periods of 2003–2008 in Sishili Bay, China., Chin. J. Ocean. Limnol. 29, 664–673 (2011). https://doi.org/10.1007/s00343-011-0179-3 DOI：

摘要

Abstract

Sishili Bay is the most important aquiculture and tourism area for the city of Yantai

China; however

red tides occurred frequently and have caused huge economic losses in this bay in recent years. To gain a better understanding of the local ecological environments in the bay

we conducted this research between 2003 and 2008 to analyze variations in nutrients and chlorophyll (chl-a) during high frequency red tide period (May to September). The results show that the chl-a concentration increased from 2.70 in 2003 to 7.26 mg/m3 in 2008

while the concentration of total inorganic nitrogen (TIN) and silicate (SiO3-Si) increased lineally from 5.18 and 1.45 μmol/L in 2003 to 18.57 and 9.52 μmol/L in 2008

respectively

and the annual phosphate (PO4-P) varied between 0.15 and 0.46 μmol/L. Special attention was given to a red tide in August 2007 occurred when water temperature was high and nutrient concentrations increased sharply because of a heavy rainfall. Overall

the results show the P limitation in Sishili Bay

and reveal that red tides were caused by eutrophication from terrestrial inputs and local warm weather

particularly during rainy periods. Therefore

to control red tide

greater efforts should be made to reduce sewage discharges into Sishili Bay

particularly during rainfall seasons.

关键词

Keywords

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