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季节性干旱与大气二氧化碳浓度升高对原核生物根际群落的交互作用。

Interactive effects of seasonal drought and elevated atmospheric carbon dioxide concentration on prokaryotic rhizosphere communities.

作者信息

Drigo Barbara, Nielsen Uffe N, Jeffries Thomas C, Curlevski Nathalie J A, Singh Brajesh K, Duursma Remko A, Anderson Ian C

机构信息

University of South Australia, FII, Mawson Lakes, GPO Box 2471, Adelaide, SA, 5001, Australia.

Hawkesbury Institute for the Environment, Western Sydney University, Locked Bag 1797, Penrith, NSW 2751, Australia.

出版信息

Environ Microbiol. 2017 Aug;19(8):3175-3185. doi: 10.1111/1462-2920.13802. Epub 2017 Aug 7.

Abstract

Global change models indicate that rainfall patterns are likely to shift towards more extreme events concurrent with increasing atmospheric carbon dioxide concentration ([CO ]). Both changes in [CO ] and rainfall regime are known to impact above- and belowground communities, but the interactive effects of these global change drivers have not been well explored, particularly belowground. In this experimental study, we examined the effects of elevated [CO ] (ambient + 240 ppm; [eCO ]) and changes in rainfall patterns (seasonal drought) on soil microbial communities associated with forest ecosystems. Our results show that bacterial and archaeal communities are highly resistant to seasonal drought under ambient [CO ]. However, substantial taxa specific responses to seasonal drought were observed at [eCO ], suggesting that [eCO ] compromise the resistance of microbial communities to extreme events. Within the microbial community we were able to identify three types of taxa specific responses to drought: tolerance, resilience and sensitivity that contributed to this pattern. All taxa were tolerant to seasonal drought at [aCO ], whereas resilience and sensitivity to seasonal drought were much greater in [eCO ]. These results provide strong evidence that [eCO ] moderates soil microbial community responses to drought in forests, with potential implications for their long-term persistence and ecosystem functioning.

摘要

全球变化模型表明,随着大气二氧化碳浓度([CO₂])的增加,降雨模式可能会转向更极端的事件。已知[CO₂]的变化和降雨模式都会影响地上和地下群落,但这些全球变化驱动因素的交互作用尚未得到充分研究,尤其是在地下。在这项实验研究中,我们研究了升高的[CO₂](环境浓度 + 240 ppm;[eCO₂])和降雨模式变化(季节性干旱)对与森林生态系统相关的土壤微生物群落的影响。我们的结果表明,在环境[CO₂]条件下,细菌和古菌群落对季节性干旱具有高度抗性。然而,在[eCO₂]条件下观察到了大量分类群对季节性干旱的特异性响应,这表明[eCO₂]会损害微生物群落对极端事件的抗性。在微生物群落中,我们能够识别出对干旱的三种分类群特异性响应类型:耐受性、恢复力和敏感性,这些导致了这种模式。在[aCO₂]条件下,所有分类群都对季节性干旱具有耐受性,而在[eCO₂]条件下,对季节性干旱的恢复力和敏感性要大得多。这些结果提供了强有力的证据,表明[eCO₂]会调节森林土壤微生物群落对干旱的响应,这对它们的长期存续和生态系统功能可能具有潜在影响。

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