Catabolic profiles of cultivable microbial communities in forest soils of western Algeria along a latitudinal gradient

B. Habib, Zouidi Mohamed, Hachem Kadda, G. Raphael, Théoneste Hagenimana
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引用次数: 2

Abstract

In Algeria, the soil degradation, more particularly the one related to the biological properties in the surface layers, is a major problem to the ecological balance and the development of forest massive. This phenomenon is considered to be the most important factor limiting the growth and productivity of forest plants in arid and semi-arid zones that can go as far as to almost sterilization of these soils. In this research, it is proposed to undertake the study on catabolic profiles of cultivable microbial communities of forest soils in western Algeria along a latitudinal gradient in some sampled surface horizons of the three zones, namely Tlemcen, Saida and Naama. Like most of soils in semiarid and arid zones, they are soils with low content in organic matter and in clay, and most often the sandy to the sand-like texture. 158 Borsali Amine Habib et al. The analysis of the catabolic profiles was carried out in five study plots of about 400 m each selected in each study area, making a total of fifteen plots for the three zones (Tlemcen, Saida and Naama). On each plot, five samples of soil were taken randomly between 0 and 15 cm of depth. Catabolic profiles were determined following the modified protocol of Garland and Mills (1991). The present research study show that it is in the Tlemcen zone, considered as subhumid, that a greater diversity and catabolic wealth were found; and more down towards the arid zone, more that wealth and diversity decrease to a critical level for the Naama zone. The results showed that there is a significant effect of the bioclimatic stage on the soil biological wealth and diversity.
阿尔及利亚西部森林土壤中可培养微生物群落沿纬度梯度的分解代谢剖面
在阿尔及利亚,土壤退化,特别是与表层生物特性有关的土壤退化,是生态平衡和森林大规模发展的一个主要问题。这种现象被认为是限制干旱和半干旱地区森林植物生长和生产力的最重要因素,甚至可能使这些土壤几乎绝育。本研究拟在阿尔及利亚西部特莱姆森、赛伊达和纳马3个带的表层取样层沿纬度梯度对森林土壤可培养微生物群落的分解代谢剖面进行研究。像大多数半干旱和干旱地区的土壤一样,它们是有机质和粘土含量低的土壤,大多数是砂质到砂状质地的土壤。[8] [j]。在每个研究区选择5个研究地块,每个地块约400 m,共计15个地块用于3个区(Tlemcen, Saida和Naama)进行分解代谢分析。在每个地块上,在0至15厘米的深度上随机抽取5个土壤样本。分解代谢谱是根据Garland和Mills(1991)的修改方案确定的。目前的研究表明,在半湿润的特莱姆森带,发现了更大的多样性和更丰富的分解代谢;越往干旱区,纳玛地区的财富和多样性就越低,达到临界水平。结果表明,生物气候阶段对土壤生物丰富性和多样性有显著影响。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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