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首页> 外文期刊>Global change biology >Development of a stable isotope index to assess decadal-scale vegetation change and application to woodlands of the Burdekin catchment, Australia
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Development of a stable isotope index to assess decadal-scale vegetation change and application to woodlands of the Burdekin catchment, Australia

机译:建立稳定的同位素指数以评估年代际尺度上的植被变化并将其应用于澳大利亚伯德金流域的林地

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Forty-four study sites were established in remnant woodland in the Burdekin River catchment in tropical north-east Queensland, Australia, to assess recent (decadal) vegetation change. The aim of this study was further to evaluate whether wide-scale vegetation 'thickening' (proliferation of woody plants in formerly more open woodlands) had occurred during the last century, coinciding with significant changes in land management. Soil samples from several depth intervals were size separated into different soil organic carbon (SOC) fractions, which differed from one another by chemical composition and turnover times. Tropical (C-4) grasses dominate in the Burdekin catchment, and thus 613 C analyses of SOC fractions with different turnover times can be used to assess whether the relative proportion of trees (C-3) and grasses (C4) had changed over time. However, a method was required to permit standardized assessment of the 613 C data for the individual sites within the 13 Mha catchment, which varied in soil and vegetation characteristics. Thus, an index was developed using data from three detailed study sites and global literature to standardize individual isotopic data from different soil depths and SOC fractions to reflect only the changed proportion of trees (C3) to grasses (C4) over decadal timescales. When applied to the 44 individual sites distributed throughout the Burdekin catchment,, 64% of the sites were shown to have experienced decadal vegetation thickening, while 29% had remained stable and the remaining 7% had thinned. Thus, the development of this index enabled regional scale assessment and comparison of decadal vegetation patterns without having to rely on prior knowledge of vegetation changes or aerial photography.
机译:在澳大利亚昆士兰州热带东北部的伯德金河流域的剩余林地中建立了44个研究地点,以评估近期(年代际)植被变化。这项研究的目的是进一步评估在上个世纪是否发生了大规模植被“增厚”(原本较开放的林地中木本植物的扩散),同时土地管理发生了重大变化。将来自多个深度间隔的土壤样品按大小分成不同的土壤有机碳(SOC)馏分,这些馏分的化学组成和周转时间彼此不同。热带(C-4)草在Burdekin流域中占主导地位,因此可以使用具有不同周转时间的SOC馏分进行613 C分析,以评估树木(C-3)和草(C4)的相对比例是否随时间变化。但是,需要一种方法来对13 Mha流域内各个地点的613 C数据进行标准化评估,因为土壤和植被特征各不相同。因此,使用来自三个详细研究地点的数据和全球文献开发了一个指数,以标准化来自不同土壤深度和SOC分数的同位素数据,以仅反映十年时间尺度上树木(C3)与草(C4)的变化比例。如果将其应用于分布在整个Burdekin流域的44个地点,则表明64%的地点经历了年代际植被增厚,而29%的地点保持稳定,其余的7%变稀。因此,该指数的发展使得能够在不依赖于植被变化或航空摄影的先验知识的情况下进行区域尺度评估和年代际植被模式的比较。

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