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低地龙脑香林林分茎围对土壤水势的响应:个体时间序列分析。

Stem girth changes in response to soil water potential in lowland dipterocarp forest in Borneo: An individualistic time-series analysis.

机构信息

Institute of Plant Sciences, University of Bern, Bern, Switzerland.

出版信息

PLoS One. 2022 Jun 30;17(6):e0270140. doi: 10.1371/journal.pone.0270140. eCollection 2022.

Abstract

Time-series data offer a way of investigating the causes driving ecological processes as phenomena. To test for possible differences in water relations between species of different forest structural guilds at Danum (Sabah, NE Borneo), daily stem girth increments (gthi), of 18 trees across six species were regressed individually on soil moisture potential (SMP) and temperature (TEMP), accounting for temporal autocorrelation (in GLS-arima models), and compared between a wet and a dry period. The best-fitting significant variables were SMP the day before and TEMP the same day. The first resulted in a mix of positive and negative coefficients, the second largely positive ones. An adjustment for dry-period showers was applied. Interactions were stronger in dry than wet period. Negative relationships for overstorey trees can be interpreted in a reversed causal sense: fast transporting stems depleted soil water and lowered SMP. Positive relationships for understorey trees meant they took up most water at high SMP. The unexpected negative relationships for these small trees may have been due to their roots accessing deeper water supplies (if SMP was inversely related to that of the surface layer), and this was influenced by competition with larger neighbour trees. A tree-soil flux dynamics manifold may have been operating. Patterns of mean diurnal girth variation were more consistent among species, and time-series coefficients were negatively related to their maxima. Expected differences in response to SMP in the wet and dry periods did not clearly support a previous hypothesis differentiating drought and non-drought tolerant understorey guilds. Trees within species showed highly individual responses when tree size was standardized. Data on individual root systems and SMP at several depths are needed to get closer to the mechanisms that underlie the tree-soil water phenomena in these tropical forests. Neighborhood stochasticity importantly creates varying local environments experienced by individual trees.

摘要

时间序列数据提供了一种研究生态过程驱动因素的方法,这些因素表现为现象。为了检验丹浓(沙巴,婆罗洲东北部)不同森林结构类型物种之间水分关系的可能差异,对六种物种的 18 棵树的每日树干周长增量(gthi)分别进行回归分析,自变量为土壤水分势(SMP)和温度(TEMP),并考虑了时间自相关(在 GLS-arima 模型中),同时在湿季和干季之间进行比较。最佳拟合的显著变量是前一天的 SMP 和当天的 TEMP。第一个变量导致正系数和负系数的混合,第二个变量主要是正系数。对干季降雨进行了调整。在干季,交互作用更强。对上层树木的负相关关系可以从相反的因果意义上解释:快速运输的茎干耗尽了土壤水分并降低了 SMP。对下层树木的正相关关系意味着它们在高 SMP 时吸收了大部分水分。这些小树出现意外的负相关关系可能是由于它们的根系可以获取更深的水源(如果 SMP 与表层的 SMP 呈反比),而这受到与较大邻树竞争的影响。可能存在一个树-土壤通量动态流形。物种之间的平均日周长变化模式更为一致,时间序列系数与最大值呈负相关。对湿季和干季 SMP 响应的预期差异并未明确支持之前区分耐旱和不耐旱下层林带的假说。当树木大小标准化时,物种内的树木表现出高度的个体响应。需要有关个体根系和几个深度处的 SMP 的数据,才能更接近这些热带森林中树木-土壤水分现象的潜在机制。林分内的随机波动会显著改变个体树木所经历的局部环境。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/c117/9246238/4de634558485/pone.0270140.g001.jpg

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