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岩性和高温影响土壤中携带 phoD 的细菌,从而增强亚热带森林土壤中有效磷的含量。

Lithology and elevated temperature impact phoD-harboring bacteria on soil available P enhancing in subtropical forests.

机构信息

College of Environmental and Engineering, Guangxi Key Laboratory of Theory and Technology for Environmental Pollution Control, Guilin University of Technology, Guilin 541006, Guangxi, China; Collaborative Innovation Center for Water Pollution Control and Water Safety in Karst Area, Guilin 541006, Guangxi, China.

Karst Dynamics Laboratory, Ministry of natural Resources, Institute of Karst Geology, Chinese Academy of Geological Sciences, Guilin 541004, Guangxi, China.

出版信息

Sci Total Environ. 2024 Oct 20;948:174815. doi: 10.1016/j.scitotenv.2024.174815. Epub 2024 Jul 15.

Abstract

Plants are generally limited by soil phosphorus (P) deficiency in forest ecosystems. Soil available P is influenced by lithology, temperature, and soil microbes. However, the interactive effects of these factors on soil P availability in subtropical forests remain unclear. To assess their impacts, we measured soil inorganic and available P fractions and the diversity, composition, and co-occurrence network of phoD-harboring bacteria in two contrasting forest soils (lithosols in karst forests and ferralsols in non-karst forests) in the subtropical regions of southwestern China across six temperature gradients. The present results showed that the complexities in composition and network and the diversity indices of phoD-harboring bacteria were higher in the karst forest soils than those in the non-karst forest soils, with marked differences in composition. In both types of forest soils, the complexities of composition and networks and the diversity indices were higher in the high-temperature regions (mean annual temperature (MAT) > 16 °C) compared to the low-temperature regions (MAT <16 °C). Soil total inorganic and available P contents were lower in the karst forest soils compared to the non-karst forest soils. Soil total available P contents were lower in the high temperature regions than those in the low temperature regions in both forest soils, whereas soil total inorganic P contents were contrary. Variance partitioning analysis showed that soil inorganic and available P fractions were predominantly explained by lithology and its interaction with soil microbes and climate. The present findings demonstrate that soil P availability in subtropical forests of southwestern China is influenced by lithology and temperature, which regulate the diversity, composition, and network connectivity of phoD-harboring bacteria. Furthermore, this study highlights the significance of controlling the composition of phoD-harboring bacteria for mitigating plant P deficiency in karst ecosystems.

摘要

植物通常在森林生态系统中受到土壤磷(P)缺乏的限制。土壤有效磷受岩性、温度和土壤微生物的影响。然而,这些因素对亚热带森林土壤有效磷供应的相互作用影响仍不清楚。为了评估它们的影响,我们测量了两种不同森林土壤(喀斯特森林中的土壤和非喀斯特森林中的土壤)中 phoD 携带细菌的土壤无机和有效磷组分以及多样性、组成和共生网络,在西南亚热带地区跨越六个温度梯度。本研究结果表明,喀斯特森林土壤中 phoD 携带细菌的组成和网络的复杂性以及多样性指数高于非喀斯特森林土壤,且组成差异明显。在这两种森林土壤中,高温地区(年平均温度(MAT)>16°C)的组成和网络的复杂性以及多样性指数均高于低温地区(MAT <16°C)。与非喀斯特森林土壤相比,喀斯特森林土壤中的土壤总无机和有效磷含量较低。在这两种森林土壤中,高温地区的土壤总有效磷含量低于低温地区,而土壤总无机磷含量则相反。方差分解分析表明,土壤无机和有效磷组分主要受岩性及其与土壤微生物和气候的相互作用解释。本研究结果表明,中国西南亚热带森林土壤有效磷供应受岩性和温度的影响,这两个因素调节了 phoD 携带细菌的多样性、组成和网络连通性。此外,本研究强调了控制 phoD 携带细菌组成对于缓解喀斯特生态系统中植物磷缺乏的重要性。

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