Dissolved organic matter and its role in red tide succession in the East China Sea in spring

Weihong Zhao; Pengji Zhuo

doi:10.1007/s00343-011-0508-6

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Dissolved organic matter and its role in red tide succession in the East China Sea in spring

Updated：2023-05-16

- Dissolved organic matter and its role in red tide succession in the East China Sea in spring
- Journal of Oceanology and Limnology Vol. 29, Issue 4, Pages: 795-799(2011)
- Affiliations：
  
  Key Laboratory of Marine Ecology and Environmental Sciences Institute of Oceanology Chinese Academy of Sciences
- Author bio：
- Funds：
- DOI：10.1007/s00343-011-0508-6
  CLC：
- Online First：10 July 2011，
  
  Published：2011
- Accepted：
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Zhao, W., Zhuo, P. Dissolved organic matter and its role in red tide succession in the East China Sea in spring., Chin. J. Ocean. Limnol. 29, 795–799 (2011). https://doi.org/10.1007/s00343-011-0508-6
DOI：

Zhao, W., Zhuo, P. Dissolved organic matter and its role in red tide succession in the East China Sea in spring., Chin. J. Ocean. Limnol. 29, 795–799 (2011). https://doi.org/10.1007/s00343-011-0508-6 DOI：

摘要

Abstract

Dissolved fluorescent organic matter was measured using fluorescence excitation-emission matrix spectroscopy at three temporal points during a Synechococcus bloom after diatom bloom dispersion in spring

2007. Carbohydrate and dissolved organic carbon were also analyzed. The relationship between organic matter and red tide succession was examined. The results show that after the diatom bloom

tyrosine-like fluorescence B intensity was very high within the water column and exhibited a negative correlation with chlorophyll a over the period of the Synechococcus bloom. Other organic matter did not exhibit this relationship with chlorophyll a. This implied that diatom bloom dispersion resulted in the release of large quantities of tyrosine-like compounds into the water. These may play a role as a nutrient source or growth-stimulating substance for the subsequent Synechococcus bloom.

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references

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