Nitrogen(N)deposition is a significant aspect of global change and poses a threat to terrestrial biodiversity.The impact of plant-soil microbe relationships to N deposition has recently attracted considerable attentio...Nitrogen(N)deposition is a significant aspect of global change and poses a threat to terrestrial biodiversity.The impact of plant-soil microbe relationships to N deposition has recently attracted considerable attention.Soil microorganisms have been proven to provide nutrients for specific plant growth,especially in nutrient-poor desert steppe ecosystems.However,the effects of N deposition on plant-soil microbial community interactions in such ecosystems remain poorly understood.To investigate these effects,we conducted a 6-year N-addition field experiment in a Stipa breviflora Griseb.desert steppe in Inner Mongolia Autonomous Region,China.Four N treatment levels(N0,N30,N50,and N100,corresponding to 0,30,50,and 100 kg N/(hm2•a),respectively)were applied to simulate atmospheric N deposition.The results showed that N deposition did not significantly affect the aboveground biomass of desert steppe plants.N deposition did not significantly reduce the alfa-diversity of plant and microbial communities in the desert steppe,and low and mediate N additions(N30 and N50)had a promoting effect on them.The variation pattern of plant Shannon index was consistent with that of the soil bacterial Chao1 index.N deposition significantly affected the beta-diversity of plants and soil bacteria,but did not significantly affect fungal communities.In conclusion,N deposition led to co-evolution between desert steppe plants and soil bacterial communities,while fungal communities exhibited strong stability and did not undergo significant changes.These findings help clarify atmospheric N deposition effects on the ecological health and function of the desert steppe.展开更多
凋落物分解是陆地生态系统养分循环的重要过程,在生物地球化学循环过程中发挥着重要作用。全球变化是影响凋落物分解的重要因子,其对生态系统养分循环的影响存在诸多不确定性。研究荒漠草原凋落物分解对氮沉降和降水变化及其二者交互作...凋落物分解是陆地生态系统养分循环的重要过程,在生物地球化学循环过程中发挥着重要作用。全球变化是影响凋落物分解的重要因子,其对生态系统养分循环的影响存在诸多不确定性。研究荒漠草原凋落物分解对氮沉降和降水变化及其二者交互作用的响应,是揭示这些不确定性、保护草原生态系统结构和功能的科学基础。以内蒙古四子王旗短花针茅荒漠草原为研究对象,选取建群种短花针茅和优势种无芒隐子草两种植物凋落物,开展为期4年的长期分解实验,探究两种植物凋落物分解特征及养分释放规律。实验采用裂区设计,主区为自然降水(C)、增雨30%(W)和减雨30%(R)3个水分梯度,副区为0(N0)、30(N30)、50(N50)和100(N100) kg hm^(-2)a^(-1)4个氮素梯度。结果表明:(1)增雨和氮沉降促进荒漠草原凋落物分解,减雨反之,降水对两种凋落物影响具有差异,而氮沉降的作用不依赖于物种;(2)氮沉降缩短凋落物分解周期5.12%—14.82%,增雨与氮沉降交互缩短凋落物分解周期3.69%—28.75%;(3)降水始终有利于凋落物中碳、纤维素和木质素释放,而分解后期氮沉降对其影响不显著,凋落物分解后期主要受木质素分解速率控制。综上所述,影响荒漠草原凋落物分解的主要因素为降水,其次是氮素,二者对凋落物分解具有协同作用。展开更多
为解析养分添加对贝加尔针茅草甸草原中小型土壤动物群落的影响,于2010年在内蒙古呼伦贝尔市鄂温克旗贝加尔针茅草甸草原设计氮磷添加试验,研究施N、P和NP混合施入(其中N和P的施入量均为100 kg hm-2a-1)对土壤动物群落结构和多样性的变...为解析养分添加对贝加尔针茅草甸草原中小型土壤动物群落的影响,于2010年在内蒙古呼伦贝尔市鄂温克旗贝加尔针茅草甸草原设计氮磷添加试验,研究施N、P和NP混合施入(其中N和P的施入量均为100 kg hm-2a-1)对土壤动物群落结构和多样性的变化及其与环境因子之间的关系.土壤动物于2019年牧草返青期(5月)、生长期(8月)和枯黄期(9月末)进行采集.结果显示,与对照相比,N和NP添加使土壤动物个体数显著增加了1.38倍和1.15倍,类群数显著增加28.57%和21.43%,P处理土壤动物个体数和类群数高于对照,但未达到显著水平;(2)试验区植被生长期(8月)良好的水热条件更适合土壤动物群落的发展;(3)冗余分析(RDA)的结果进一步表明,土壤动物的群落组成主要受pH和植物均匀度影响,且pH是控制中小型土壤动物群落变化的主要因子.本研究揭示长期的养分添加通过改变植物均匀度与土壤pH对中小型土壤节肢动物群落产生积极影响,且土壤pH比植物均匀度的贡献更大.(图6表3参37)展开更多
基金the National Natural Science Foundation of China(31860136,31560156)the Basic Scientific Research Service Fee Project of Colleges and Universities of Inner Mongolia Autonomous Regionthe Graduate Scientific Research Innovation Project of Inner Mongolia Autonomous Region(B20210158Z).
文摘Nitrogen(N)deposition is a significant aspect of global change and poses a threat to terrestrial biodiversity.The impact of plant-soil microbe relationships to N deposition has recently attracted considerable attention.Soil microorganisms have been proven to provide nutrients for specific plant growth,especially in nutrient-poor desert steppe ecosystems.However,the effects of N deposition on plant-soil microbial community interactions in such ecosystems remain poorly understood.To investigate these effects,we conducted a 6-year N-addition field experiment in a Stipa breviflora Griseb.desert steppe in Inner Mongolia Autonomous Region,China.Four N treatment levels(N0,N30,N50,and N100,corresponding to 0,30,50,and 100 kg N/(hm2•a),respectively)were applied to simulate atmospheric N deposition.The results showed that N deposition did not significantly affect the aboveground biomass of desert steppe plants.N deposition did not significantly reduce the alfa-diversity of plant and microbial communities in the desert steppe,and low and mediate N additions(N30 and N50)had a promoting effect on them.The variation pattern of plant Shannon index was consistent with that of the soil bacterial Chao1 index.N deposition significantly affected the beta-diversity of plants and soil bacteria,but did not significantly affect fungal communities.In conclusion,N deposition led to co-evolution between desert steppe plants and soil bacterial communities,while fungal communities exhibited strong stability and did not undergo significant changes.These findings help clarify atmospheric N deposition effects on the ecological health and function of the desert steppe.
文摘凋落物分解是陆地生态系统养分循环的重要过程,在生物地球化学循环过程中发挥着重要作用。全球变化是影响凋落物分解的重要因子,其对生态系统养分循环的影响存在诸多不确定性。研究荒漠草原凋落物分解对氮沉降和降水变化及其二者交互作用的响应,是揭示这些不确定性、保护草原生态系统结构和功能的科学基础。以内蒙古四子王旗短花针茅荒漠草原为研究对象,选取建群种短花针茅和优势种无芒隐子草两种植物凋落物,开展为期4年的长期分解实验,探究两种植物凋落物分解特征及养分释放规律。实验采用裂区设计,主区为自然降水(C)、增雨30%(W)和减雨30%(R)3个水分梯度,副区为0(N0)、30(N30)、50(N50)和100(N100) kg hm^(-2)a^(-1)4个氮素梯度。结果表明:(1)增雨和氮沉降促进荒漠草原凋落物分解,减雨反之,降水对两种凋落物影响具有差异,而氮沉降的作用不依赖于物种;(2)氮沉降缩短凋落物分解周期5.12%—14.82%,增雨与氮沉降交互缩短凋落物分解周期3.69%—28.75%;(3)降水始终有利于凋落物中碳、纤维素和木质素释放,而分解后期氮沉降对其影响不显著,凋落物分解后期主要受木质素分解速率控制。综上所述,影响荒漠草原凋落物分解的主要因素为降水,其次是氮素,二者对凋落物分解具有协同作用。
文摘为解析养分添加对贝加尔针茅草甸草原中小型土壤动物群落的影响,于2010年在内蒙古呼伦贝尔市鄂温克旗贝加尔针茅草甸草原设计氮磷添加试验,研究施N、P和NP混合施入(其中N和P的施入量均为100 kg hm-2a-1)对土壤动物群落结构和多样性的变化及其与环境因子之间的关系.土壤动物于2019年牧草返青期(5月)、生长期(8月)和枯黄期(9月末)进行采集.结果显示,与对照相比,N和NP添加使土壤动物个体数显著增加了1.38倍和1.15倍,类群数显著增加28.57%和21.43%,P处理土壤动物个体数和类群数高于对照,但未达到显著水平;(2)试验区植被生长期(8月)良好的水热条件更适合土壤动物群落的发展;(3)冗余分析(RDA)的结果进一步表明,土壤动物的群落组成主要受pH和植物均匀度影响,且pH是控制中小型土壤动物群落变化的主要因子.本研究揭示长期的养分添加通过改变植物均匀度与土壤pH对中小型土壤节肢动物群落产生积极影响,且土壤pH比植物均匀度的贡献更大.(图6表3参37)
