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Grass invasion causes rapid increases in ecosystem carbon and nitrogen storage in a semiarid shrubland

机译:草入侵导致半干旱灌丛中生态系统的碳和氮存储迅速增加

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Accurately predicting terrestrial carbon (C) and nitrogen (N) storage requires understanding how plant invasions alter cycling and storage. A common, highly successful type of plant invasion occurs when the invasive species is of a distinctly different functional type than the native dominant plant, such as shrub encroachment throughout the western United States and annual grass invasions in Mediterranean shrublands, as studied here. Such invasions can dramatically transform landscapes and have large potential to alter C and N cycling by influencing storage in multiple pools. We used a manipulation of non-native annual grass litter within a shrub-dominated habitat in southern California (coastal sage scrub, CSS) to study how grass invasion alters ecosystem C and N storage. We added, removed, or left unchanged grass litter in areas of high and low invasion, then followed soil and vegetation changes. Grass litter greatly increased C and N storage in soil, aboveground native and non-native biomass. Aboveground litter storage increased due to the greater inputs and slower decomposition of grass litter relative to shrub litter; shading by grass litter further reduced decomposition of both non-native and native litter, which may be due to reduced photodegradation. Soil C and N pools in areas of high litter increased ~20% relative to low litter areas in the two years following manipulation and were generally sinks for C and N, while areas with low litter were sources. We synthesize our results into a C cycle of invaded and uninvaded areas of CSS and link changes in storage to increases in the soil fungi : bacteria ratio, increased plant inputs, and decreased litter loss. Overall, we show that grasses, especially through their litter, control important abiotic and biotic mechanisms governing C and N storage, with widespread implications for C sequestration and N storage in semiarid systems undergoing grass or shrub invasions.
机译:准确预测陆地碳(C)和氮(N)的存储量需要了解植物的入侵如何改变循环和存储。当入侵物种的功能类型与天然优势植物截然不同时,就会发生一种常见的,非常成功的植物入侵类型,例如,美国西部的灌木丛入侵和地中海灌木丛中的年度草入侵,如此处所述。这样的入侵可以极大地改变景观,并通过影响多个池中的存储而具有改变碳和氮循环的巨大潜力。我们在加利福尼亚州南部的一个以灌木为主的栖息地(沿海鼠尾草灌木丛,CSS)中使用了一种非本地一年生凋落物,研究了草种入侵如何改变生态系统的碳和氮存储量。我们在高入侵和低入侵地区添加,移除或保持草屑不变,然后跟随土壤和植被的变化。草地凋落物大大增加了土壤,地上的天然和非天然生物量中的碳和氮存储量。相对于灌木垃圾,地上垃圾的存储量增加了,原因是草屑的投入增加且分解速度较慢。草窝遮阴进一步减少了非天然和天然凋落物的分解,这可能是由于光降解减少所致。在处理后的两年中,高凋落物区域的土壤碳和氮库相对于低凋落物区域增加了约20%,通常是C和N的汇,而低凋落物是来源。我们将结果合成为CSS入侵和未入侵区域的C周期,并将存储的变化与土壤真菌:细菌比率的增加,植物投入的增加和枯枝落叶的减少联系起来。总体而言,我们表明,草,尤其是通过其凋落物,控制着控制碳和氮储存的重要非生物和生物机制,这对遭受草或灌木入侵的半干旱系统中的碳固存和氮储存具有广泛的影响。

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