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Growth and Nitrogen Uptake Characteristics Reveal Outbreak Mechanism of the Opportunistic Macroalga Gracilaria tenuistipitata

Macroalgae has bloomed in the brackish lake of Shenzhen Bay, China continuously from 2010 to 2014. Gracilaria tenuistipitata was identified as the causative macroalgal species. The aim of this study was to explore the outbreak mechanism of G. tenuistipitata, by studying the effects of salinity and n...

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Detalles Bibliográficos
Autores principales: Wang, Chao, Lei, Anping, Zhou, Kai, Hu, Zhengyu, Hao, Wenlong, Yang, Junda
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Public Library of Science 2014
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4192001/
https://www.ncbi.nlm.nih.gov/pubmed/25299123
http://dx.doi.org/10.1371/journal.pone.0108980
Descripción
Sumario:Macroalgae has bloomed in the brackish lake of Shenzhen Bay, China continuously from 2010 to 2014. Gracilaria tenuistipitata was identified as the causative macroalgal species. The aim of this study was to explore the outbreak mechanism of G. tenuistipitata, by studying the effects of salinity and nitrogen sources on growth, and the different nitrogen sources uptake characteristic. Our experimental design was based on environmental conditions observed in the bloom areas, and these main factors were simulated in the laboratory. Results showed that salinity 12 to 20 ‰ was suitable for G. tenuistipitata growth. When the nitrogen sources' (NH(4) (+), NO(3) (−)) concentrations reached 40 µM or above, the growth rate of G. tenuistipitata was significantly higher. Algal biomass was higher (approximately 1.4 times) when cultured with NH(4) (+) than that with NO(3) (−) addition. Coincidentally, macroalgal bloom formed during times of moderate salinity (∼12 ‰) and high nitrogen conditions. The NH(4) (+) and NO(3) (−) uptake characteristic was studied to understand the potential mechanism of G. tenuistipitata bloom. NH(4) (+) uptake was best described by a linear, rate-unsaturated response, with the slope decreasing with time intervals. In contrast, NO(3) (−) uptake followed a rate-saturating mechanism best described by the Michaelis-Menten model, with kinetic parameters V(max) = 37.2 µM g(−1) DM h(−1) and K(s) = 61.5 µM. Further, based on the isotope (15)N tracer method, we found that (15)N from NH(4) (+) accumulated faster and reached an atom% twice than that of (15)N from NO(3) (−), suggesting when both NH(4) (+) and NO(3) (−) were available, NH(4) (+) was assimilated more rapidly. The results of the present study indicate that in the estuarine environment, the combination of moderate salinity with high ammonium may stimulate bloom formation.