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Nitrogen and carbon isotopic ratios of chlorophyll from marine phytoplankton

机译:海洋浮游植物叶绿素的氮碳同位素比

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The relationship between the nitrogen and carbon isotopic ratios of chlorophyll a and total biomass was explored in cultured marine phytoplankton to assess the utility of chlorophyll as an isotopic proxy for photoautotrophs. A near constant nitrogen isotopic depletion of 5.06 +- 1.13 per thousand (95% confidence interval) in chlorophyll a relative to total nitrogen was observed in 8 species. This value was similar to isotopic differences between chlorophyll a and marine particles (5.27 +- 1.48 per thousand (1#sigma#); n = 6) and sediments (5.39 +- 0.67 per thousand (1#sigma#); n = 4) in a variety of settings. These findings suggest that a 5.1 per thousand isotopic depletion of chlorophyll a relative to total algal nitrogen is a robust relationship that justifies the use of chlorophyll as a nitrogen isotopic surrogate for photoautotrophs. Although interspecies differences in #DELTA##delta#~(15)N_(cell-Chla) exist, and growth rate has a small effect on this parameter, the field data suggest these factors are probably minimized in the ocean where multiple species and growth rates occur. The nitrogen isotopic depletion of chlorophyll a probably occurs during the transamination of glutamic acid in #delta#-aminolevulinic acid biosynthesis, the first committed precursor to chlorophyll. The carbon isotopic composition of chlorophyll from 12 batch cultures and 7 species of marine phytoplankton was elevated by 0.32 +- 1.61 per thousand (95% confidence interval) relative to total cellular carbon. No significant interspecies variance was observed that was not attributable to intraspecies variance. There was a moderate inverse correlation between growth rate and #DELTA##delta#~(13)C_(cell-Chla) and it is hypothesized that this parameter is largely responsible for the large range of intraspecies #DELTA##delta#~(13)C_(cell-Chla) values observed in batch cultures.
机译:在养殖的海洋浮游植物中探索了叶绿素a的氮碳同位素比与总生物量之间的关系,以评估叶绿素作为光合自养生物的同位素替代品的效用。相对于总氮,在8个物种中,叶绿素a的氮同位素消耗几乎恒定,为千分之5.06±1.13(95%置信区间)。该值类似于叶绿素a与海洋颗粒(5.27 +-1.48 /千(1#sigma#); n = 6)和沉积物(5.39 +-0.67 /千(1#sigma#); n = 4 )的各种设置。这些发现表明,相对于藻类总氮而言,叶绿素a的千分之5.1的同位素消耗是牢固的关系,这证明了将叶绿素用作光合自养生物的氮同位素替代物是合理的。尽管#DELTA ## delta#〜(15)N_(cell-Chla)中存在种间差异,并且生长速度对此参数影响很小,但现场数据表明,在多种物种和生长的海洋中,这些因素可能最小化率发生。叶绿素a的氮同位素耗竭可能发生在#delta-氨基乙酰丙酸生物合成中谷氨酸的氨基转移过程中,这是叶绿素的第一个定型前体。相对于总细胞碳,来自12种分批培养物和7种海洋浮游植物的叶绿素碳同位素组成每千(95%置信区间)提高0.32±1.61。没有观察到明显的种间差异,而这不归因于种内差异。生长速率与#DELTA ## delta#〜(13)C_(cell-Chla)之间存在中等程度的反相关,并且假设此参数在很大程度上导致了种内#DELTA ## delta#〜( 13)在分批培养中观察到C_(cell-Chla)值。

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