Shomer-Ilan A, Nissenbaum A, Galun M, Waisel Y
Department of Botany, The George S. Wise Faculty of Life Sciences Tel Aviv University, Tel Aviv, Israel.
Plant Physiol. 1979 Jan;63(1):201-5. doi: 10.1104/pp.63.1.201.
delta(13)C values of the lichens Ramalina duriaei and Teloschistes villosus collected in their natural habitat were repeatedly measured during 2 years. Results show variations in the stable carbon isotope ratios ((13)C/(12)C). Such variations are correlated to the seasonal rainfall, i.e. low values of delta(13)C of the lichens during the winter and high values of delta(13)C during the dry summer. Relatively low delta(13)C values were obtained also in laboratory experiments with lichens grown under controlled humid conditions and in lichens collected from humid habitats.The variations in carbon isotopes were associated with quantitative metabolic changes. Under humid conditions an increase was obtained in the total amount of the extracted water-soluble fraction of the plant tissues as well as in the relative content of soluble carbohydrates.Analysis of the possible factors which may cause such variations indicates that the quantity of precipitation and the exposure time to high humidity were the main environmental factors causing seasonal variations in the delta(13)C values of the lichens. Such variations are dependent mainly on enzymic reactions and are probably less influenced by purely physicochemical processes. In view of the data presented here the balance between carboxylation and decarboxylation reactions seems to be the major factor for the observed seasonal differences. Winter accumulation of (12)C enriched components causes an over-all decrease in delta(13)C. During the summer, those storage materials are respired with concomitant increase in the delta(13)C of the residual plant material.
对在自然栖息地采集的地衣Ramalina duriaei和Teloschistes villosus的δ(13)C值进行了为期两年的反复测量。结果显示了稳定碳同位素比率((13)C/(12)C)的变化。这种变化与季节性降雨相关,即地衣在冬季的δ(13)C值较低,而在干燥的夏季δ(13)C值较高。在实验室控制湿度条件下生长的地衣以及从潮湿栖息地采集的地衣中也获得了相对较低的δ(13)C值。碳同位素的变化与定量代谢变化有关。在潮湿条件下,植物组织中提取的水溶性部分的总量以及可溶性碳水化合物的相对含量都有所增加。对可能导致这种变化的因素进行分析表明,降水量和高湿度暴露时间是导致地衣δ(13)C值出现季节性变化的主要环境因素。这种变化主要取决于酶促反应,可能受纯物理化学过程的影响较小。鉴于此处给出的数据,羧化反应和脱羧反应之间的平衡似乎是观察到的季节性差异的主要因素。富含(12)C的成分在冬季积累导致δ(13)C总体下降。在夏季,这些储存物质被呼吸,同时残留植物材料的δ(13)C增加。