The biogeochemistry of photosynthetic pigments in the Jiulong River estuary and Western Xiamen Bay[J]. 海洋湖沼学报(英文), 2001,19(2):164-171.
Xu, L., Hong, Hs., Wang, Hl. et al. The biogeochemistry of photosynthetic pigments in the Jiulong River estuary and Western Xiamen Bay., Chin. J. Ocean. Limnol. 19, 164–171 (2001). https://doi.org/10.1007/BF02863042
The biogeochemistry of photosynthetic pigments in the Jiulong River estuary and Western Xiamen Bay[J]. 海洋湖沼学报(英文), 2001,19(2):164-171. DOI: 10.1007/BF02863042.
Xu, L., Hong, Hs., Wang, Hl. et al. The biogeochemistry of photosynthetic pigments in the Jiulong River estuary and Western Xiamen Bay., Chin. J. Ocean. Limnol. 19, 164–171 (2001). https://doi.org/10.1007/BF02863042DOI:
The biogeochemistry of photosynthetic pigments in the Jiulong River estuary and Western Xiamen Bay
摘要
Abstract
High performance liquid chromatography (HPLC) analysis of photosynthetic pigments in samples from Western Xiamen Bay and the Jiulong River Estuary showed that their major carotenoids were fucoxanthin
peridinin
zeaxanthin
violaxanthin
and diadinoxanthin. Diatoms dominated in the spring bloom
dinoflagellates in summer. Violaxanthin and chlorophyll b indicated the appearance of chrysophytes and green algae
most of which were freshwater species. The high phytoplankton biomass region was located at the inner part of the bay. Diatoms and dinoflagellates dominnated phytoplankton communities
contributing to over 50% of total biomass. All the main diagnostic carotenoids were significantly (P<0.01) correlated negatively to dissolved inorganic phosphorus
suggesting that they were limited by phosphorus. The high negative linear relationship (P<0.0001) between dissolved inorganic phosphorus and peridinin (dinoflagellates indicator) implied the potential of dissolved inorganic phosphorus for triggering red tide events in this region.
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Keywords
references
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