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周期性水淹土壤中山毛榉(Fagus sylvatica L.)和栎树(Quercus robur L.)的径向生长差异模式。

Differential radial growth patterns between beech (Fagus sylvatica L.) and oak (Quercus robur L.) on periodically waterlogged soils.

机构信息

Institute of Botany and Landscape Ecology, University of Greifswald, Grimmer Str. 88, D-17487 Greifswald, Germany.

出版信息

Tree Physiol. 2013 Apr;33(4):425-37. doi: 10.1093/treephys/tpt020. Epub 2013 Apr 5.

Abstract

Climate scenarios for northern Central Europe project rising temperatures and increasing frequency and intensity of droughts but also a shift in precipitation pattern with more humid winters. This in turn may result in soil waterlogging during the following spring, leading to increasing stress for trees growing on hydric sites. The influence of waterlogging on growth of common beech and pedunculate oak has been studied intensively on seedlings under experimental conditions. However, the question remains whether results of these studies can be transferred to mature trees growing under natural conditions. To test this, we investigated general growth patterns and climate-growth relationships in four mature stands of beech and oak growing on hydromorphic soils (Stagnosols) in northeast Germany using dendrochronological methods. Our results confirmed the expected tolerance of oak to strong water-level fluctuations. Neither extremely wet conditions during spring nor summer droughts significantly affected its radial growth. Oak growth responded positively to warmer temperatures during previous year October and March of the current year of ring formation. Contrary to our expectations, also beech showed relatively low sensitivity to periods of high soil water saturation. Instead, summer drought turned out to be the main climatic factor influencing ring width of beech even under the specific periodically wet soil conditions of our study. This became evident from general climate-growth correlations over the last century as well as from discontinuous (pointer year) analysis with summer drought being significantly correlated to the occurrence of growth depressions. As ring width of the two species is affected by differing climate parameters, species-specific chronologies show no coherence in high-frequency variations even for trees growing in close proximity. We assume differences in rooting depth as the main reason for the differing growth patterns and climate correlations of the two species under study. Our results indicate that under the projected future climate scenarios, beech may suffer from increasing drought stress even on hydromorphic soils. Oak might be able to maintain a sufficient hydraulic status during summer droughts by reaching water in deeper soil strata with its root system. Wet phases with waterlogged soil conditions during spring or summer appear to have only a little direct influence on radial growth of both species.

摘要

北欧中部的气候情景预计将导致气温升高,干旱的频率和强度增加,但也会导致降水模式的转变,冬季更加潮湿。这反过来可能导致次年春季土壤积水,从而增加在湿润生境中生长的树木的压力。水淹对欧洲山毛榉和栓皮栎幼苗在实验条件下的生长的影响已经得到了深入研究。然而,这些研究的结果是否可以转移到自然条件下生长的成熟树木上,仍然是一个悬而未决的问题。为了检验这一点,我们使用树木年代学方法,调查了德国东北部四个在水成型土壤(停滞土壤)上生长的山毛榉和栎属成熟林分的一般生长模式和气候-生长关系。我们的结果证实了栎属对强烈水位波动的预期耐受性。春季极度潮湿的条件或夏季干旱都没有显著影响其径向生长。栎属的生长对前一年 10 月和当年 3 月的温暖温度有积极响应,这是形成年轮的时期。与我们的预期相反,山毛榉对高土壤水分饱和度的时期也表现出相对较低的敏感性。相反,夏季干旱是影响山毛榉年轮宽度的主要气候因素,即使在我们研究中特定的周期性湿润土壤条件下也是如此。这一点从上个世纪的一般气候-生长相关性以及夏季干旱与生长衰退发生显著相关的不连续(指针年)分析中可以明显看出。由于这两个物种的年轮宽度受到不同气候参数的影响,即使是生长在附近的树木,特定的物候序列在高频变化中也没有一致性。我们假设根系深度的差异是造成这两个物种生长模式和气候相关性差异的主要原因。我们的结果表明,根据未来的气候情景预测,山毛榉即使在水成型土壤上也可能会因干旱压力增加而受到影响。栎属可能能够通过其根系到达更深的土壤层来维持夏季干旱期间的充足水力状态。春季或夏季出现的土壤积水湿相似乎对两个物种的径向生长只有很小的直接影响。

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