THE ELEMENTAL COMPOSITION OF SOME MARINE PHYTOPLANKTON1

微量元素 浮游植物 环境化学 硫黄 生物 氮气 藻类 有一固定的比值 生物量(生态学) 电感耦合等离子体质谱法 碳纤维 作文(语言) 植物 浮游生物 营养物 质谱法 生态学 化学 材料科学 有机化学 复合材料 哲学 复合数 色谱法 语言学
作者
Tung‐Yuan Ho,Antonietta Quigg,Zoe V. Finkel,Allen J. Milligan,Kevin Wyman,Paul G. Falkowski,François M. M. Morel
出处
期刊:Journal of Phycology [Wiley]
卷期号:39 (6): 1145-1159 被引量:667
标识
DOI:10.1111/j.0022-3646.2003.03-090.x
摘要

We analyzed the cellular content of C, N, P, S, K, Mg, Ca, Sr, Fe, Mn, Zn, Cu, Co, Cd, and Mo in 15 marine eukaryotic phytoplankton species in culture representing the major marine phyla. All the organisms were grown under identical culture conditions, in a medium designed to allow rapid growth while minimizing precipitation of iron hydroxide. The cellular concentrations of all metals, phosphorus, and sulfur were determined by high‐resolution inductively coupled plasma mass spectrometry (HR‐ICPMS) and those of carbon and nitrogen by a carbon hydrogen nitrogen analyzer. Accuracy of the HR‐ICPMS method was validated by comparison with data obtained with 55 Fe radioactive tracer and by a planktonic reference material. The cellular quotas (normalized to P) of trace metals and major cations in the biomass varied by a factor of about 20 among species (except for Cd, which varied over two orders of magnitude) compared with factors of 5 to 10 for major nutrients. Green algae had generally higher C, N, Fe, Zn, and Cu quotas and lower S, K, Ca, Sr, Mn, Co, and Cd quotas than coccolithophores and diatoms. Co and Cd quotas were also lower in diatoms than in coccolithophores. Although trace element quotas are influenced by a variety of growth conditions, a comparison of our results with published data suggests that the measured compositions reflect chiefly the intrinsic (i.e. genetically encoded) trace element physiology of the individual species. Published field data on the composition of the planktonic biomass fall within the range of laboratory values and are generally close to the approximate extended Redfield formula given by the average stoichiometry of our model species (excluding the hard parts): image While clearly this elemental stoichiometry varies between species and, potentially, in response to changes in the chemistry of seawater, it provides a basis for examining how phytoplankton influence the relative distributions of the ensemble of major and trace elements in the ocean.
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