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首页> 外文期刊>Biogeosciences >Contrasting patterns of litterfall seasonality and seasonal changes in litter decomposability in a tropical rainforest region
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Contrasting patterns of litterfall seasonality and seasonal changes in litter decomposability in a tropical rainforest region

机译:热带雨林地区凋落物季节变化和凋落物可分解性季节变化的对比模式

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摘要

The seasonality of litter inputs in forests has important implications for understanding ecosystem processes and biogeochemical cycles. We quantified the drivers of seasonality in litterfall and leaf decomposability using plots throughout the Australian wet tropical region. Litter fell mostly in the summer (wet, warm) months in the region, but other peaks occurred throughout the year. Litterfall seasonality was modelled well with the level of deciduousness of the site (plots with more deciduous species had lower seasonality than evergreen plots), temperature (higher seasonality in the uplands), disturbance (lower seasonality with more early secondary species) and soil fertility (higher seasonality with higher N: P / P limitation) (SL total litterfall model 1=deciduousness+soil N: P+early secondary sp.: r~2 = 0.63, n = 30; model 2=temperature+early secondary sp.+soil N: P: r~2 = 0.54, n = 30; SL leaf=temperature+early secondary sp.+rainfall seasonality: r~2 = 0.39, n = 30). Leaf litter decomposability was lower in the dry season than in the wet season, driven by higher phenolic concentrations in the dry, with the difference exacerbated particularly by lower dry season moisture. Our results are contrary to the global trend for tropical rainforests; in that seasonality of litterfall input was generally higher in wetter, cooler, evergreen forests, compared to generally drier, warmer, semi-deciduous sites that had more uniform monthly inputs. We consider this due to more diverse litter shedding patterns in semi-deciduous and raingreen rainforest sites, and an important consideration for ecosystem modellers. Seasonal changes in litter quality are likely to have impacts on decomposition and biogeochemical cycles in these forests due to the litter that falls in the dry season being more recalcitrant to decay.
机译:森林凋落物投入的季节性对理解生态系统过程和生物地球化学循环具有重要意义。我们使用整个澳大利亚湿热带地区的地块对凋落物和叶片可分解性的季节性驱动因素进行了量化。凋落物主要在该地区的夏季(潮湿,温暖)月份下降,但全年仍出现其他高峰。利用该地点的落叶水平(落叶物种较多的地块的季节季节性比常绿地块低),温度(高地季节较高),扰动(较低季节,更多的次生物种较多)和土壤肥力(较高的季节性,同时具有较高的N:P / P限制)(SL凋落物总量模型1 =落叶+土壤N:P +次要早期sp.:r~2 = 0.63,n = 30;模型2 =温度+次要早期sp。+土壤N:P:r〜2 = 0.54,n = 30; SL叶=温度+初生sp。+降雨季节:r〜2 = 0.39,n = 30)。在干燥季节,叶片凋落物的可分解性要比在潮湿季节要低,这是由于干燥过程中酚浓度较高,尤其是干燥季节的水分较低,这种差异加剧了。我们的结果与热带雨林的全球趋势相反;相比之下,在潮湿,凉爽,常绿的森林中,凋落物投入的季节通常更高,而通常情况下,每月投入量更为统一的较干燥,温暖,半落叶的地方。我们认为这是由于半落叶和雨林热带雨林地区的凋落物分布更加多样化,并且是生态系统建模者的重要考虑因素。凋落物质量的季节性变化可能会影响这些森林中的分解和生物地球化学循环,这是因为干旱季节的凋落物更难以腐烂。

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