古尔班通古特沙漠梭梭冠下裸斑形成土壤学机制
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自治区自然科学基金(2022D01C398)


The soil mechanism of bare patch formation under Haloxylon ammodendron canopies in Gurbantunggut Desert, Xinjiang, China
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    摘要:

    古尔班通古特沙漠梭梭与齿肋赤藓共生区域中,梭梭冠下常形成藓类结皮裸露斑块。为研究梭梭冠下裸斑形成机理,以裸斑内土壤、裸斑外藓类结皮土壤、背景裸地土壤以及背景藓类结皮土壤为研究对象,测定四类土壤营养物质含量和理化因子,并测定土壤代谢组以及分析其之间差异。结果表明,裸斑内土壤养分及生态化学计量比与裸斑外藓类结皮和背景藓类结皮土壤并无显著性差异,土壤养分及生态化学计量并非造成梭梭冠下藓类裸斑的原因。裸斑内土壤Na+、K+、Mg2+、SO2-4、CO2-3、HCO-3含量显著高于裸斑外土壤、背景裸地土壤和背景结皮土壤,总盐含量最高为1.705 g/kg。这个含量不足以对齿肋赤藓正常生长造成影响,因此裸斑内土壤中较高的离子浓度也并非藓类裸斑产生的原因。土壤代谢组结果显示不同土壤代谢物具有极显著差异,油酰胺等酰胺类化合物相对丰度最高,占总代谢物的72.68%,且在裸斑内土壤中相对丰度显著高于裸斑藓类结皮土壤、裸地土壤和背景结皮土壤,因此推测裸斑内土壤中油酰胺等酰胺类化合物可能是抑制齿肋赤藓生长的主要原因,是造成古尔班通古特沙漠梭梭冠下藓类裸斑产生的主要土壤学机制。

    Abstract:

    In the symbiotic region of Haloxylon ammodendron and Syntrichia caninervisin Gurbantunggut Desert, the bare patches of moss crust are often formed under H. ammodendron canopy. In order to study the mechanism of bare patch formation, the soil in the bare patch, the soil under the moss crust outside the bare patch, the bare ground soil of background, and the soil under the moss crust of background were used as research objects. The nutrient contents and physicochemical properties of four types of soil were measured, the soil metabolome was determined, and the differences between these soil indicators were analyzed. The results showed that there were no significant difference in nutrient content and ecological stoichiometry among the soils in the bare patches, the soil under the moss crust outside the bare patch, and the soil under the moss crust of background. Soil nutrients and ecological stoichiometry were not the cause of moss bare patches formation under H. ammodendron canopy. The contents of Na+, K+, Mg2+, SO2-4, CO2-3 and HCO-3 in the bare patch soil were significantly higher than those in the soil under the moss crust outside the bare patch, the bare ground soil of background, and the soil under the moss crust of background, with the highest total salt content being 1.705 g/kg. This salt content was not enough to affect the normal growth of the S. caninervis, so the higher ion concentration in the bare patch soil were also not the reason for moss bare patches formation. The soil metabolome results showed that there were significant differences in the metabolites of different soils, and amide compound such as oleamide had the highest relative abundance accounting for 72.68% of the total metabolites. The relative abundance of amide compound in the bare patch soil was significantly higher than that in the soil under the moss crust outside the bare patch, the bare ground soil of background, and the soil under the moss crust of background. Therefore, it is speculated that the amide compound such as oleamidein the bare patch soil may be the main reason for inhibiting the growth of S. caninervis, and are the main soil mechanism for moss bare patches formation under H. ammodendron canopy in Gurbantunggut Desert.

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张帅,吕杰,马媛,陈静,沈畅.古尔班通古特沙漠梭梭冠下裸斑形成土壤学机制.生态学报,2024,44(11):4844~4853

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