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绒毛牧豆树(Prosopis velutina)叶片暗呼吸CO₂碳同位素组成的日变化和季节变化

Diurnal and seasonal variation in the carbon isotope composition of leaf dark-respired CO(2) in velvet mesquite (Prosopis velutina).

作者信息

Sun Wei, Resco Víctor, Williams David G

机构信息

Department of Renewable Resources, University of Wyoming, Laramie, WY 82071, USA.

出版信息

Plant Cell Environ. 2009 Oct;32(10):1390-400. doi: 10.1111/j.1365-3040.2009.02006.x. Epub 2009 Jun 10.

Abstract

We evaluated diurnal and seasonal patterns of carbon isotope composition of leaf dark-respired CO(2) (delta(13)C(l)) in the C(3) perennial shrub velvet mesquite (Prosopis velutina) across flood plain and upland savanna ecosystems in the south-western USA. delta(13)C(l) of darkened leaves increased to maximum values late during daytime periods and declined gradually over night-time periods to minimum values at pre-dawn. The magnitude of the diurnal shift in delta(13)C(l) was strongly influenced by seasonal and habitat-related differences in soil water availability and leaf surface vapour pressure deficit. delta(13)C(l) and the cumulative flux-weighted delta(13)C value of photosynthates were positively correlated, suggesting that progressive (13)C enrichment of the CO(2) evolved by darkened leaves during the daytime mainly resulted from short-term changes in photosynthetic (13)C discrimination and associated shifts in the delta(13)C signature of primary respiratory substrates. The (13)C enrichment of dark-respired CO(2) relative to photosynthates across habitats and seasons was 4 to 6 per thousand at the end of the daytime period (1800 h), but progressively declined to 0 per thousand by pre-dawn (0300 h). The origin of night-time and daytime variations in delta(13)C(l) is discussed in terms of the carbon source(s) feeding respiration and the drought-induced changes in carbon metabolism.

摘要

我们评估了美国西南部洪泛平原和高地稀树草原生态系统中C3多年生灌木绒毛牧豆树(Prosopis velutina)叶片暗呼吸CO2的碳同位素组成(δ13C(l))的昼夜和季节模式。 darkened叶片的δ13C(l)在白天后期增加到最大值,并在夜间逐渐下降,在黎明前降至最小值。δ13C(l)的昼夜变化幅度受到土壤水分有效性和叶片表面蒸汽压亏缺的季节和生境相关差异的强烈影响。δ13C(l)与光合产物的累积通量加权δ13C值呈正相关,这表明白天darkened叶片释放的CO2的渐进性(13)C富集主要是由于光合(13)C歧视的短期变化以及初级呼吸底物δ13C特征的相关变化。在白天结束时(1800 h),不同生境和季节中暗呼吸CO2相对于光合产物的(13)C富集为4‰至6‰,但到黎明前(0300 h)逐渐降至0‰。根据供给呼吸的碳源以及干旱引起的碳代谢变化,讨论了δ13C(l)在夜间和白天变化的起源。

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