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Nutrient-limited growth and sources of nutrients for coral reef macroalgae.

机译:珊瑚礁大型藻类的营养限制生长和营养来源。

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Net productivity of benthic macroalgae is often high in coral reef systems, yet the rates at which nutrients are supplied from oligotrophic water columns may be insufficient for sustained growth. Eleven species of macroalgae from reefs in oligotrophic Kaneohe Bay, Hawaii were cultured at the same nutrient concentrations as the water column. Nine species did not sustain positive growth. Alternative hypotheses were proposed to explain this observation: (1) access to supplementary, benthic nutrient sources is required; (2) nutrients are supplied from the overlying water column in brief pulses of sufficient concentration and duration to sustain growth; (3) sufficient nutrients for growth are provided by the water column if average flow rates are high. These hypotheses were tested in lab and field experiments using the dominant macroalga in Kaneohe Bay, Dictyosphaeria cavernosa.; The first hypothesis was examined by measuring nutrient efflux from sediments and excretion by epifaunal invertebrates. Positive efflux of inorganic nitrogen and phosphorus was measured from sediment patches. Epifauna from D. cavernosa excreted inorganic nitrogen and phosphorus. Nutrient from these sources can enhance growth, as indicated by culture experiments. Results of a field experiment confirmed that nitrogen efflux from sediments beneath D. cavernosa thalli enhanced growth.; The second hypothesis was not supported. Analyses of a 40 month data set of inorganic nutrient concentrations in the water column near a Kaneohe Bay reef slope indicated that nutrient pulses rarely occurred. Results of experiments with D. cavernosa indicated that nitrogen pulses would have to occur at 3-4 day intervals to sustain growth.; To test the third hypothesis, measurements of nitrogen and phosphorus uptake by D. cavernosa at varied water flow rates were used to estimate flow rates in the field at which advection from the water column supplies sufficient nutrients for sustained growth. Flow rates above 5 cm/s were predicted to provide sufficient nitrogen, and flow rates above 1 cm/s, sufficient phosphorus. The contributions of nutrients from different sources appear to change with changing environmental conditions; at sites with high flow rates, nutrients are supplied from the water column at sufficient rates for sustained algal growth; at sites with low flow rates, sediment efflux and invertebrate excretion may be required in addition to advection from the water column.
机译:在珊瑚礁系统中,底栖大型藻类的净生产力通常很高,但从贫营养水柱供应养分的速率可能不足以持续生长。以与水柱相同的养分浓度培养来自夏威夷贫营养型卡内奥赫湾礁石的11种大型藻类。九个物种没有维持正增长。提出了其他假设来解释这一现象:(1)需要获得补充的底栖营养源; (2)从上层水柱以足够的浓度和持续时间短暂脉冲提供营养以维持生长; (3)如果平均流速高,水柱将为生长提供足够的养分。这些假说在实验室和野外实验中使用了位于海绵体(Dictyosphaeria Cavernosa)Kaneohe湾的优势巨藻进行了测试。第一个假设是通过测量沉积物的营养外排和表皮无脊椎动物的排泄来检验的。从沉积物斑块测量了无机氮和磷的正流出。 D. Cavernosa的表生动物排出了无机氮和磷。如培养实验所示,这些来源的营养可促进生长。田间实验的结果证实,D。Cavernosa thalli下方沉积物的氮外流促进了生长。不支持第二种假设。对Kaneohe湾礁坡附近水柱中40个月的无机养分浓度数据集的分析表明,养分脉动很少发生。 D. Cavernosa的实验结果表明,氮素脉冲必须每隔3-4天出现一次,以维持生长。为了检验第三个假设,在不同的水流量下测量了D. Cavernosa对氮和磷的吸收,以估算田间的流速,水柱对流提供的营养足以维持持续生长。预计流速高于5 cm / s可提供足够的氮,流速高于1 cm / s可提供足够的磷。来自不同来源的养分的贡献似乎随着环境条件的变化而变化;在高流量的地点,水柱以足够的速率提供营养,以维持藻类的持续生长。在流速较低的地点,除了从水柱中平流外,还可能需要沉淀物外流和无脊椎动物的排泄物。

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