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小麦中碳分配与根际沉积的时间动态

Temporal dynamics of carbon partitioning and rhizodeposition in wheat.

作者信息

Dilkes Nigel B, Jones David L, Farrar John

机构信息

School of Biological Sciences, University of Wales, Bangor, Gwynedd, LL57 2UW, United Kingdom.

出版信息

Plant Physiol. 2004 Feb;134(2):706-15. doi: 10.1104/pp.103.032045. Epub 2004 Feb 5.

Abstract

The temporal dynamics of partitioning and rhizodeposition of recent photosynthate in wheat (Triticum aestivum) roots were quantified in situ in solution culture. After a 30-min pulse of (14)CO(2) to a single intact leaf, (14)C activities of individual carbon fluxes in the root, including exudation, respiration, and root content, were measured continuously over the next 20 h concurrently with (14)C efflux from the leaf. Immediately after the end of the (14)CO(2) pulse, (14)C activity was detected in the root, the hydroponic solution, and in root respiration. The rate of (14)C exudation from the root was maximal after 2 to 3 h, and declined to one-third of maximum after a further 5 h. Completion of the rapid phase of (14)C efflux from the leaf coincided with peak (14)C exudation rate. Thus, exudation flux is much more rapidly and dynamically coupled to current photosynthesis than has been appreciated. Careful cross-calibration of (14)C counting methods allowed a dynamic (14)C budget to be constructed for the root. Cumulative (14)C exudation after 20 h was around 3% of (14)C fixed in photosynthesis. Partitioning of photosynthate between shoot and root was manipulated by partial defoliation before applying the (14)CO(2) pulse to the remaining intact leaf. Although the rate of photosynthesis was largely unaffected by partial defoliation, the proportion of new photosynthate subsequently partitioned to and exuded from the root was substantially reduced. This clearly indicates that exudation depends more on the rate of carbon import into the root than on the rate of photosynthesis.

摘要

在溶液培养中对小麦(Triticum aestivum)根系近期光合产物的分配和根际沉积的时间动态进行了原位定量研究。对一片完整叶片进行30分钟的(14)CO₂脉冲处理后,在接下来的20小时内,连续测量根系中各个碳通量(包括渗出、呼吸和根系碳含量)的(14)C活性,同时测量叶片的(14)C流出量。(14)CO₂脉冲结束后立即在根系、水培溶液和根系呼吸中检测到(14)C活性。根系(14)C渗出率在2至3小时后达到最大值,并在接下来的5小时后降至最大值的三分之一。叶片(14)C流出的快速阶段结束与(14)C渗出率峰值同时出现。因此,渗出通量与当前光合作用的耦合比以往认识的要迅速得多且动态性更强。对(14)C计数方法进行仔细的交叉校准后,得以构建根系的动态(14)C收支。20小时后累积(14)C渗出量约为光合作用固定(14)C的3%。在对剩余完整叶片施加(14)CO₂脉冲之前,通过部分去叶处理来控制光合产物在地上部和根系之间的分配。尽管部分去叶处理对光合作用速率影响不大,但随后分配到根系并从根系渗出的新光合产物比例大幅降低。这清楚地表明,渗出更多地取决于碳进入根系的速率,而不是光合作用速率。

相似文献

1
Temporal dynamics of carbon partitioning and rhizodeposition in wheat.小麦中碳分配与根际沉积的时间动态
Plant Physiol. 2004 Feb;134(2):706-15. doi: 10.1104/pp.103.032045. Epub 2004 Feb 5.

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