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

机译:生长和氮吸收特性揭示机会性Macroalga Gracilaria tenuistipitata的爆发机制

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摘要

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' (NH4 +, NO3 ) 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 NH4 + than that with NO3 addition. Coincidentally, macroalgal bloom formed during times of moderate salinity (∼12 ‰) and high nitrogen conditions. The NH4 + and NO3 uptake characteristic was studied to understand the potential mechanism of G. tenuistipitata bloom. NH4 + uptake was best described by a linear, rate-unsaturated response, with the slope decreasing with time intervals. In contrast, NO3 uptake followed a rate-saturating mechanism best described by the Michaelis-Menten model, with kinetic parameters Vmax = 37.2 µM g−1 DM h−1 and Ks = 61.5 µM. Further, based on the isotope 15N tracer method, we found that 15N from NH4 + accumulated faster and reached an atom% twice than that of 15N from NO3 , suggesting when both NH4 + and NO3 were available, NH4 + 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.
机译:自2010年至2014年,大型藻类在中国深圳湾的咸淡湖中持续开花。江cil是致病性大型藻类。这项研究的目的是通过研究盐分和氮源对生长的影响以及不同氮源的吸收特性,来探索tenuistipitata的爆发机制。我们的实验设计基于在开花地区观察到的环境条件,并且在实验室中模拟了这些主要因素。结果表明,盐度为12至20‰适宜于G. tenuistipitata生长。当氮源(NH4 + ,NO3 -)的浓度达到40 µM或更高时,ten.stiuistipitata的生长速度显着提高。用NH4 + 培养的藻类生物量要比添加NO3 -的藻类生物质更高(约1.4倍)。巧合的是,在中等盐度(〜12‰)和高氮条件下会形成大型藻华。研究了NH4 + 和NO3 -的吸收特性,以了解G. tenuistipitata开花的潜在机理。 NH4 + 的吸收最好用线性,速率不饱和反应来描述,其斜率随时间间隔而减小。相反,NO3 -的吸收遵循Michaelis-Menten模型最好描述的速率饱和机制,动力学参数为Vmax = 37.2 µM g -1 DM h -1 ,Ks = 61.5 µM。此外,基于同位素 15 N示踪法,我们发现来自NH4 + 15 N积累速度更快,达到原子%的两倍。 N3 -中的 15 N的平均值,表明当NH4 + 和NO3 -均可用时,NH4 + 被更快地吸收。本研究的结果表明,在河口环境中,中等盐度与高铵盐的结合可能会刺激水华的形成。

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