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Stable isotope (13C) and O2 micro-optode alternatives for measuring photosythesis in seaweeds

机译:用于测量海藻光合作用的稳定同位素(13C)和O2微光电二极管替代品

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ABSTRACT: Many photosynthetic studies with macroalgae are based on oxygen evolution. This approach is preferred over 14C tracer techniques since oxygen electrodes are generally inexpensive and radioactive wastes are not produced. Nevertheless, oxygen techniques do not directly measure carbon assimilation; thus, primary production estimates rely on the conversion of oxygen units to carbon units via a photosynthetic quotient, which may vary depending on physiological state and nutrient status of the alga. We present in detail 2 methods for measuring photosynthesis in macroalgae, both of which should enhance prospects for photosynthetic research, particularly under field conditions. First, a carbon uptake procedure is described which relies on incorporation of a stable 13C isotope label. Important advantages of the 13C method include simplicity of sample processing, avoidance of environmental hazards and restrictions of radioactive 14C, and ability to be used as a dual tracer with 15N. Second, we employed a fiber-optic micro-optode system for measurement of dissolved oxygen. The fluorescence-based optodes stabilize quickly (15 s), do not consume oxygen, and are simple to set up and maintain. Oxygen and carbon photosynthesis were assessed concurrently in a light/dark chamber design. Both techniques resolved significant decreases in light-saturated photosynthesis (Pmax) in the kelp Laminaria hyperborea collected subtidally at 10 m compared to kelp at 0 m (from mean low tide). Oxygen and carbon photosynthetic rates agreed well with published values and were mutually consistent, considering a reasonable photosynthetic quotient. Estimated measurement errors (2%) associated with the 13C technique were less than intrinsic variation (20%) in photosynthetic rates between kelp individuals with similar light histories. Both techniques should provide an alternative to traditional photosynthetic protocols and stimulate further primary production research in macrophytes.
机译:摘要:许多大型藻类的光合作用研究都是基于氧气的释放。这种方法优于 14 示踪剂技术,因为氧气电极通常价格便宜,并且不会产生放射性废物。然而,氧气技术不能直接测量碳同化。因此,初级产量估算依赖于通过光合商将氧单位转化为碳单位,这取决于藻类的生理状态和营养状况。我们详细介绍了两种测量大型藻类光合作用的方法,这两种方法都应增强光合作用研究的前景,特别是在田间条件下。首先,描述了依赖于稳定的 13 C同位素标记的碳吸收程序。 13 C方法的重要优点包括简化样品处理,避免环境危害和放射性 14 C的限制以及与一起用作双重示踪剂的能力> 15 N。其次,我们采用了光纤微光电系统来测量溶解氧。基于荧光的光电二极管可快速稳定(<15 s),不消耗氧气,并且易于设置和维护。在明/暗室设计中同时评估氧和碳的光合作用。两种技术都解决了在10 m时收集的海带 P max 的光饱和光合作用( P max )显着降低的问题,而0时的海带则明显m(来自平均退潮)。考虑到合理的光合商,氧和碳的光合速率与公布的值非常吻合,并且相互一致。与 13 C技术相关的估计测量误差(<2%)小于具有相似光历史的海带个体之间光合速率的内在变化(> 20%)。两种技术都应提供传统光合作用方案的替代方法,并刺激大型植物的进一步初级生产研究。

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