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首页> 外文期刊>Global change biology >Is climate an important driver of post-European vegetation change in the Eastern United States?
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Is climate an important driver of post-European vegetation change in the Eastern United States?

机译:气候是否是美国东部欧洲后植被变化的重要驱动力?

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Many ecological phenomena combine to direct vegetation trends over time, with climate and disturbance playing prominent roles. To help decipher their relative importance during Euro-American times, we employed a unique approach whereby tree species/genera were partitioned into temperature, shade tolerance, and pyrogenicity classes and applied to comparative tree-census data. Our megadata analysis of 190 datasets determined the relative impacts of climate vs. altered disturbance regimes for various biomes across the eastern United States. As the Euro-American period (ca. 1500 to today) spans two major climatic periods, from Little Ice Age to the Anthropocene, vegetation changes consistent with warming were expected. In most cases, however, European disturbance overrode regional climate, but in a manner that varied across the Tension Zone Line. To the north, intensive and expansive early European disturbance resulted in the ubiquitous loss of conifers and large increases of Acer, Populus, and Quercus in northern hardwoods, whereas to the south, these disturbances perpetuated the dominance of Quercus in central hardwoods. Acer increases and associated mesophication in Quercus-Pinus systems were delayed until mid 20th century fire suppression. This led to significant warm to cool shifts in temperature class where cool-adapted Acer saccharum increased and temperature neutral changes where warm-adapted Acer rubrum increased. In both cases, these shifts were attributed to fire suppression rather than climate change. Because mesophication is ongoing, eastern US forests formed during the catastrophic disturbance era followed by fire suppression will remain in climate disequilibrium into the foreseeable future. Overall, the results of our study suggest that altered disturbance regimes rather than climate had the greatest influence on vegetation composition and dynamics in the eastern United States over multiple centuries. Land-use change often trumped or negated the impacts of warming climate, and needs greater recognition in climate change discussions, scenarios, and model interpretations.
机译:随着时间的流逝,许多生态现象结合起来指导植被趋势,其中气候和干扰起着重要作用。为了帮助解释它们在欧美时代的相对重要性,我们采用了一种独特的方法,将树种/属划分为温度,耐荫性和热原性类别,并应用于比较的人口普查数据。我们对190个数据集进行的巨量数据分析确定了美国东部不同生物群落的气候与扰动制度的相对影响。由于欧美时期(大约从1500年到今天)跨越了两个主要的气候时期,从小冰期到人类世,预计植被会随着变暖而变化。然而,在大多数情况下,欧洲的干扰笼罩了区域气候,但其方式在整个张力带上有所不同。在北部,强烈而广泛的欧洲早期干扰导致针叶树无处不在,北部硬木中的宏cer,胡杨和栎属大量增加,而在南部,这些干扰使栎木在中部硬木中占主导地位。枫树-松树系统中的宏cer增加和相关的细化被推迟到20世纪中期灭火为止。这导致温度等级发生明显的从暖到冷的变化,其中凉爽适应的宏cer糖增加,而温度中性发生变化,暖适应的宏cer糖增加。在这两种情况下,这些变化均归因于灭火而不是气候变化。由于不断进行细化,在可预见的将来,在灾难性扰乱时期形成的美国东部森林随后将受到灭火的抑制,仍将保持气候不平衡。总体而言,我们的研究结果表明,多个世纪以来,改变的干扰方式而非气候对美国东部的植被组成和动态影响最大。土地用途的变化往往胜过或抵消了气候变暖的影响,需要在气候变化的讨论,情景和模型解释中得到更大的认可。

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