Pub Date : 2024-09-18DOI: 10.13287/j.1001-9332.202409.030
Bin Kang
To complete the life cycle, species exhibit corresponding functional traits in morphology, physiology, ecology, etc. The eigenvalues, variation, and distribution of functional traits are the functional components of biodiversity, namely functional diversity, could maintain the service function and healthy operation of ecosystems. The application of functional diversity broadens our understanding of biodiversity and its temporal and spatial variations, and provides a breakthrough to the problem of how to combine morphological structure with ecological function. I reviewed the research process of functional diversity from the perspective of proposing, calculating, and applying the parameters of functional diversity, as well as the application of functional diversity from different purposes and perspectives. I put forward the challenges and countermeasures of related studies. In the future, researches should pay attention to establish a set of effective trait indicators, discover the internal and external mechanisms driving functional diversity variations, and map the redistribution of traits under environmental changes.
{"title":"History, challenges, and prospects of researches on fish functional diversity.","authors":"Bin Kang","doi":"10.13287/j.1001-9332.202409.030","DOIUrl":"10.13287/j.1001-9332.202409.030","url":null,"abstract":"<p><p>To complete the life cycle, species exhibit corresponding functional traits in morphology, physiology, ecology, <i>etc</i>. The eigenvalues, variation, and distribution of functional traits are the functional components of biodiversity, namely functional diversity, could maintain the service function and healthy operation of ecosystems. The application of functional diversity broadens our understanding of biodiversity and its temporal and spatial variations, and provides a breakthrough to the problem of how to combine morphological structure with ecological function. I reviewed the research process of functional diversity from the perspective of proposing, calculating, and applying the parameters of functional diversity, as well as the application of functional diversity from different purposes and perspectives. I put forward the challenges and countermeasures of related studies. In the future, researches should pay attention to establish a set of effective trait indicators, discover the internal and external mechanisms driving functional diversity variations, and map the redistribution of traits under environmental changes.</p>","PeriodicalId":35942,"journal":{"name":"应用生态学报","volume":"35 9","pages":"2338-2351"},"PeriodicalIF":0.0,"publicationDate":"2024-09-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142476611","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2024-09-18DOI: 10.13287/j.1001-9332.202409.002
Jin-Ju Wu, Bao-Ling Su, Xing-Zhi Li, Xue-Kai Sun, Xiang-Ping Tan, Yan-Xia Nie, Wen-Zhi DU, Ren-Shuang Zou, Jiao-Jiao Deng, Li Zhou, Da-Pao Yu, Qing-Wei Wang
Photodegradation driven by solar radiation has been confirmed as an important driving factor for litter decomposition. However, previous single-site studies could not quantify the relative contribution of variation in solar radiation to litter decomposition. To address it, we conducted a field experiment in Heshan National Field Research Station of Forest Ecosystem, Guangdong (Heshan Station, south subtropical climate), Jigongshan Ecological Research Station, Xinyang, Henan (Jigongshan Station, north subtropical climate) and Daqinggou Ecological Research Station, Institute of Applied Ecology, Chinese Academy of Sciences (Daqinggou Station, temperate climate) at intervals of 10 degrees. We examined litter decomposition of Populus davidiana and Larix olgensis, two species with significant differences in initial litter quality through an in-situ spectral-attenuation experiment. Treatments included full-spectrum, No-UV-B (attenuating UV-B radiation <315 nm) and No-UV & Blue (attenuating all UV and blue wavelengths <500 nm). After nearly 1-year decomposition, litter dry mass remaining of P. davidiana and L. olgensis under full-spectrum treatment was lowest at Heshan (30.2% and 36.3%), and highest at Jigongshan (37.3% and 45.8%). Among all sites, litter dry mass remaining was lowest under the full-spectrum, and lower than that of No-UV-B and No-UV & blue. UV and blue light significantly increased litter mass loss of P. davidiana and L. olgensis, with contributions of 59.7% and 57.0% (Heshan), 46.4% and 42.1% (Jigongshan), and 39.0% and 45.9% (Daqinggou), respectively. The contribution of UV-A and blue light (315-500 nm) was greater than UV-B (280-315 nm); the cumulative irradiance, soil temperature and moisture were the main driving factors for litter photodegradation.
太阳辐射驱动的光降解已被证实是垃圾分解的一个重要驱动因素。然而,以往的单点研究无法量化太阳辐射变化对垃圾分解的相对贡献。针对这一问题,我们在广东鹤山国家森林生态系统野外研究站(鹤山站,南亚热带气候)、河南信阳鸡公山生态研究站(鸡公山站,北亚热带气候)和中国科学院应用生态研究所大青沟生态研究站(大青沟站,温带气候)进行了间隔 10 度的野外试验。我们通过原位光谱衰减实验考察了杨树和欧落叶松这两种初始枯落物质量差异显著的树种的枯落物分解情况。处理包括全光谱、无紫外线-B(衰减紫外线-B辐射)和全光谱处理,在鹤山,全光谱处理下的杨树和榆树枯落物分解率最低(分别为 30.2% 和 36.3%),而在鸡公山则最高(分别为 37.3% 和 45.8%)。在所有地点中,全光谱处理的枯落物干重最低,低于无紫外光-B 和无紫外光-蓝光处理。紫外线和蓝光明显增加了 P. davidiana 和 L. olgensis 的枯落物质量损失,贡献率分别为 59.7% 和 57.0%(鹤山)、46.4% 和 42.1%(鸡公山)以及 39.0% 和 45.9%(大清沟)。紫外线 A 和蓝光(315-500 nm)的贡献率大于紫外线 B(280-315 nm);累积辐照度、土壤温度和湿度是垃圾光降解的主要驱动因素。
{"title":"Latitudinal responses of litter decomposition to solar radiation.","authors":"Jin-Ju Wu, Bao-Ling Su, Xing-Zhi Li, Xue-Kai Sun, Xiang-Ping Tan, Yan-Xia Nie, Wen-Zhi DU, Ren-Shuang Zou, Jiao-Jiao Deng, Li Zhou, Da-Pao Yu, Qing-Wei Wang","doi":"10.13287/j.1001-9332.202409.002","DOIUrl":"10.13287/j.1001-9332.202409.002","url":null,"abstract":"<p><p>Photodegradation driven by solar radiation has been confirmed as an important driving factor for litter decomposition. However, previous single-site studies could not quantify the relative contribution of variation in solar radiation to litter decomposition. To address it, we conducted a field experiment in Heshan National Field Research Station of Forest Ecosystem, Guangdong (Heshan Station, south subtropical climate), Jigongshan Ecological Research Station, Xinyang, Henan (Jigongshan Station, north subtropical climate) and Daqinggou Ecological Research Station, Institute of Applied Ecology, Chinese Academy of Sciences (Daqinggou Station, temperate climate) at intervals of 10 degrees. We examined litter decomposition of <i>Populus davidiana</i> and <i>Larix olgensis</i>, two species with significant differences in initial litter quality through an in-situ spectral-attenuation experiment. Treatments included full-spectrum, No-UV-B (attenuating UV-B radiation <315 nm) and No-UV & Blue (attenuating all UV and blue wavelengths <500 nm). After nearly 1-year decomposition, litter dry mass remaining of <i>P. davidiana</i> and <i>L. olgensis</i> under full-spectrum treatment was lowest at Heshan (30.2% and 36.3%), and highest at Jigongshan (37.3% and 45.8%). Among all sites, litter dry mass remaining was lowest under the full-spectrum, and lower than that of No-UV-B and No-UV & blue. UV and blue light significantly increased litter mass loss of <i>P. davidiana</i> and <i>L. olgensis</i>, with contributions of 59.7% and 57.0% (Heshan), 46.4% and 42.1% (Jigongshan), and 39.0% and 45.9% (Daqinggou), respectively. The contribution of UV-A and blue light (315-500 nm) was greater than UV-B (280-315 nm); the cumulative irradiance, soil temperature and moisture were the main driving factors for litter photodegradation.</p>","PeriodicalId":35942,"journal":{"name":"应用生态学报","volume":"35 9","pages":"2511-2517"},"PeriodicalIF":0.0,"publicationDate":"2024-09-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142476613","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
For a long time, intercropping and rotation of leguminous with non-leguminous crops is widely used to reduce the application of nitrogen fertilizer and increase yield in agroecosystems. At present, most researchers considered that this management measure is helpful for reducing fertilizer consumption and increasing its efficiency, as it can improve nutrient supply of legumestonon-legumes, the spatial nutrient utilization efficiency by enhancing soil spatial heterogeneity, and improve soil structure and disease resistance. However, current theories cannot fully explain the positive effect of crop rotation and inter-cropping systems involving legumes. A large amount of hydrogen (H2) can be produced as an obligatory by-product of nitrogenase responsible for nitrogen (N2) fixation in the root nodules of leguminous plants. Despite of substantial amounts of H2 enriched in the rhizosphere of legumes, only a minor proportion of H2 is found to leak to soil surface. Increasing evidence showed that most H2 released in soil is immediately depleted in the surrounding of N2-fixing nodules by H2-oxidizing bacteria (HOB) thriving in soil. HOB can use H2 as an electron donor to assimilate and fix CO2 through redox reactions to synthesize cellular substances and consequently promote plant growth. To date, however, little is known about the biological mechanism and ecological process behind the "hydrogen fertilizer effect". Therefore, we review the H2-induced plant growth-promoting effects and its microbiological mechanisms. Our aims were to explore a new way for enhancing agroecosystem production, and to provide scientific basis for future utilization of H2 in agricultural production practices.
{"title":"Microbiological mechanism of hydrogen fertilizer effect in soil.","authors":"Qing-Shan Feng, Qin-Jiang Mao, Jian-Guo Ma, Yu-Man Li, Xiao-Qian Yang, Xing-Xin Lu, Xiao-Bo Wang","doi":"10.13287/j.1001-9332.202409.012","DOIUrl":"10.13287/j.1001-9332.202409.012","url":null,"abstract":"<p><p>For a long time, intercropping and rotation of leguminous with non-leguminous crops is widely used to reduce the application of nitrogen fertilizer and increase yield in agroecosystems. At present, most researchers considered that this management measure is helpful for reducing fertilizer consumption and increasing its efficiency, as it can improve nutrient supply of legumestonon-legumes, the spatial nutrient utilization efficiency by enhancing soil spatial heterogeneity, and improve soil structure and disease resistance. However, current theories cannot fully explain the positive effect of crop rotation and inter-cropping systems involving legumes. A large amount of hydrogen (H<sub>2</sub>) can be produced as an obligatory by-product of nitrogenase responsible for nitrogen (N<sub>2</sub>) fixation in the root nodules of leguminous plants. Despite of substantial amounts of H<sub>2</sub> enriched in the rhizosphere of legumes, only a minor proportion of H<sub>2</sub> is found to leak to soil surface. Increasing evidence showed that most H<sub>2</sub> released in soil is immediately depleted in the surrounding of N<sub>2</sub>-fixing nodules by H<sub>2</sub>-oxidizing bacteria (HOB) thriving in soil. HOB can use H<sub>2</sub> as an electron donor to assimilate and fix CO<sub>2</sub> through redox reactions to synthesize cellular substances and consequently promote plant growth. To date, however, little is known about the biological mechanism and ecological process behind the \"hydrogen fertilizer effect\". Therefore, we review the H<sub>2</sub>-induced plant growth-promoting effects and its microbiological mechanisms. Our aims were to explore a new way for enhancing agroecosystem production, and to provide scientific basis for future utilization of H<sub>2</sub> in agricultural production practices.</p>","PeriodicalId":35942,"journal":{"name":"应用生态学报","volume":"35 9","pages":"2382-2391"},"PeriodicalIF":0.0,"publicationDate":"2024-09-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142476614","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2024-09-18DOI: 10.13287/j.1001-9332.202409.033
Xiao-Wei Guo, Yu-Xue Zhang, Ye-Ming You, Jian-Xin Sun
The turnover and stabilization of soil organic carbon are tightly associated with the properties of litter input. Due to the complexity of litter decomposition and the high heterogeneity of forest soils, there are considerable uncertainties about how soil minerals, microorganisms, and environmental factors jointly regulate the transformation and stability of litter-derived soil organic carbon. Here, we present an overview of the "microbial efficiency-matrix stabilization" framework centered on microbial metabolism and organic carbon transformation, as well as the new "microbial carbon pump" and "mineral carbon pump" theories in forest soil organic carbon transformation and stabilization. We specifically highlighted a differential mechanism of "organo-organic interfaces" from the "organo-mineral interfaces" in the effects on soil organic carbon accumulation. We further expounded the transformation processes and stability of soil organic carbon based on the "carbon material cycling" and "energy fluxes", aiming to provide theoretical support for the research on carbon sequestration in forest soils.
{"title":"Research advance in the effects of litter input on forest soil organic carbon transformation and stability.","authors":"Xiao-Wei Guo, Yu-Xue Zhang, Ye-Ming You, Jian-Xin Sun","doi":"10.13287/j.1001-9332.202409.033","DOIUrl":"10.13287/j.1001-9332.202409.033","url":null,"abstract":"<p><p>The turnover and stabilization of soil organic carbon are tightly associated with the properties of litter input. Due to the complexity of litter decomposition and the high heterogeneity of forest soils, there are considerable uncertainties about how soil minerals, microorganisms, and environmental factors jointly regulate the transformation and stability of litter-derived soil organic carbon. Here, we present an overview of the \"microbial efficiency-matrix stabilization\" framework centered on microbial metabolism and organic carbon transformation, as well as the new \"microbial carbon pump\" and \"mineral carbon pump\" theories in forest soil organic carbon transformation and stabilization. We specifically highlighted a differential mechanism of \"organo-organic interfaces\" from the \"organo-mineral interfaces\" in the effects on soil organic carbon accumulation. We further expounded the transformation processes and stability of soil organic carbon based on the \"carbon material cycling\" and \"energy fluxes\", aiming to provide theoretical support for the research on carbon sequestration in forest soils.</p>","PeriodicalId":35942,"journal":{"name":"应用生态学报","volume":"35 9","pages":"2352-2361"},"PeriodicalIF":0.0,"publicationDate":"2024-09-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142476619","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2024-09-18DOI: 10.13287/j.1001-9332.202409.025
Jiao-Jun Zhu, Tian Gao, Li-Zhong Yu, Kai Yang, Tao Sun, De-Liang Lu, Zhi-Hua Liu, Ying-Dong Chu, Jin-Xin Zhang, De-Xiong Teng, Yuan Zhu, Yi-Rong Sun, Xu-Gao Wang, Gao-Feng Wang
<p><p>The widespread utilization of fossil fuels has emitted large amounts of CO<sub>2</sub> into the atmosphere since the Industrial Revolution, leading to climate warming and frequent occurrence of extreme climate events. To effectively alleviate climate change, the international community has made various efforts to reduce carbon emissions and eliminate CO<sub>2</sub> from the atmosphere. In 2020, the Chinese government announced that carbon emission peaking and carbon neutrality will be achieved by 2030 and 2060, respectively. According to the current forecast, by the time carbon neutrality is achieved in 2060, even under the minimum conditions of fossil energy use, production, and living emissions, China will still have to emit about 1/4 of the current total emissions. These carbon must primarily be absorbed by ecosystems. Furthermore, approximately 140 ppm increase in CO<sub>2</sub> in the atmosphere since the Industrial Revolution still needs to be removed by ecosystems. Forests are the main component of terrestrial ecosystems, contributing more than 80% of the carbon sequestration capacity of all terrestrial ecosystems. However, due to the long periodicity, complexity and dynamic variability of forests, the basic concepts of ecosystem carbon sink and its time effect are still unclear, leading to problems, such as lacking technologies for improving carbon sink capacity and disorganized rules in the carbon sink trading market. In this review, we introduced carbon sink concept according to the processes of absorbing and fixing CO<sub>2</sub> by plant photosynthesis in forest ecosystems. Then, we analyzed the processes of time-scale-dependent carbon sinks of forest ecosystems, discussed the time effects of forest carbon sinks, and suggested using "t-year" as the unit of carbon sink (taking 3-6 months as the minimum measurement time, <i>i.e</i>., the beginning of carbon sequestration). Third, we proposed the approaches to improve the carbon sink capacity of forest ecosystems. One way is to improve the carbon sink capacity (expanding forest area, improving forest quality, and increasing forest soil carbon storage) of forest ecosystems. Another approach is to maintain the carbon sink of forest ecosystems as long as possible, <i>i.e</i>., to reduce temporary carbon sink (definition: carbon in the forest ecosystems emit into the atmosphere for a certain period) and to increase persistent carbon sink (definition: carbon in the forest ecosystems no longer emit into the atmosphere for a certain period; according to the relevant provisions of the Paris Agreement, the upper time limit for carbon sink measurement can be considered to be the year 2100. In order to maintain the persistent carbon sink, strateges such as efficient use of wood products (replace steel, cement, plastic with wood), control of forest fires or other disturbances-induced emissions, and turning forest biomass into biochar should be taken. Finally, we proposed to develop climate-sma
{"title":"Carbon sink of forest ecosystems: Concept, time effect and improvement approaches.","authors":"Jiao-Jun Zhu, Tian Gao, Li-Zhong Yu, Kai Yang, Tao Sun, De-Liang Lu, Zhi-Hua Liu, Ying-Dong Chu, Jin-Xin Zhang, De-Xiong Teng, Yuan Zhu, Yi-Rong Sun, Xu-Gao Wang, Gao-Feng Wang","doi":"10.13287/j.1001-9332.202409.025","DOIUrl":"10.13287/j.1001-9332.202409.025","url":null,"abstract":"<p><p>The widespread utilization of fossil fuels has emitted large amounts of CO<sub>2</sub> into the atmosphere since the Industrial Revolution, leading to climate warming and frequent occurrence of extreme climate events. To effectively alleviate climate change, the international community has made various efforts to reduce carbon emissions and eliminate CO<sub>2</sub> from the atmosphere. In 2020, the Chinese government announced that carbon emission peaking and carbon neutrality will be achieved by 2030 and 2060, respectively. According to the current forecast, by the time carbon neutrality is achieved in 2060, even under the minimum conditions of fossil energy use, production, and living emissions, China will still have to emit about 1/4 of the current total emissions. These carbon must primarily be absorbed by ecosystems. Furthermore, approximately 140 ppm increase in CO<sub>2</sub> in the atmosphere since the Industrial Revolution still needs to be removed by ecosystems. Forests are the main component of terrestrial ecosystems, contributing more than 80% of the carbon sequestration capacity of all terrestrial ecosystems. However, due to the long periodicity, complexity and dynamic variability of forests, the basic concepts of ecosystem carbon sink and its time effect are still unclear, leading to problems, such as lacking technologies for improving carbon sink capacity and disorganized rules in the carbon sink trading market. In this review, we introduced carbon sink concept according to the processes of absorbing and fixing CO<sub>2</sub> by plant photosynthesis in forest ecosystems. Then, we analyzed the processes of time-scale-dependent carbon sinks of forest ecosystems, discussed the time effects of forest carbon sinks, and suggested using \"t-year\" as the unit of carbon sink (taking 3-6 months as the minimum measurement time, <i>i.e</i>., the beginning of carbon sequestration). Third, we proposed the approaches to improve the carbon sink capacity of forest ecosystems. One way is to improve the carbon sink capacity (expanding forest area, improving forest quality, and increasing forest soil carbon storage) of forest ecosystems. Another approach is to maintain the carbon sink of forest ecosystems as long as possible, <i>i.e</i>., to reduce temporary carbon sink (definition: carbon in the forest ecosystems emit into the atmosphere for a certain period) and to increase persistent carbon sink (definition: carbon in the forest ecosystems no longer emit into the atmosphere for a certain period; according to the relevant provisions of the Paris Agreement, the upper time limit for carbon sink measurement can be considered to be the year 2100. In order to maintain the persistent carbon sink, strateges such as efficient use of wood products (replace steel, cement, plastic with wood), control of forest fires or other disturbances-induced emissions, and turning forest biomass into biochar should be taken. Finally, we proposed to develop climate-sma","PeriodicalId":35942,"journal":{"name":"应用生态学报","volume":"35 9","pages":"2313-2321"},"PeriodicalIF":0.0,"publicationDate":"2024-09-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142476599","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2024-09-18DOI: 10.13287/j.1001-9332.202409.017
Ning Liu, Shun-Yao Yu, Cai-Yue Zhang, Yun-Ge Zhao
Vascular plants exert significant effects on micro-environment, thereby affecting the distribution of biological soil crusts (biocrusts). The relationship between vascular plants and the spatial distribution characteristics of biocrusts is largely unknown. We investigated the distribution characteristics of biocrusts under the canopy of vascular plants in the water-wind erosion crisscross area of the Loess Plateau, where larger areas of biocrusts had been formed since the implantation of "Grain for Green" project. We analyzed the relationship between the canopy characteristics of different vascular plants and the spatial distribution of biocrusts using correlation analysis and random forest importance ranking methods, and further constructed a predictive model for the area of biocrusts under the canopy of vascular plants. The results showed that: 1) Cyanobacteria crust was the predominant biocrusts, followed by moss crust. 2) The canopy of vascular plants affected the spatial distribution of biocrusts, with notable differences in distribution pattern across different directions under the canopy of vascular plants. Biocrusts were primarily distributed in the 270°-315° and 315°-360° directions, while was less frequent in the 90°-135° and 135°-180° directions. 3) Radially, the coverage of biocrusts gradually increased from the root-base to the edge of the canopy of vascular plants. 4) The coverage of biocrusts under canopy was significantly related to the characteristics of vascular plants, including canopy area, long crown width, short crown width, litter area and plant height. 5) The relative importance of canopy area, long crown width, and short crown width to the biocrusts under the canopy was 13.7%, 12.1%, and 11.9%, respectively, while the relative importance of plant height and species type was relatively low, being 6.7% and 4.4%, respectively. 6) Results of the random forest model demonstrated strong predictive performance for biocrusts distribution based on canopy characteristics of vascular plants, with a prediction accuracy of 0.59 (R2) and a root mean square error of 1.2 m2. This model could be applied to predict and estimate the area of biocrusts under the canopy of vascular plants. This study provided a theoretical basis for in-depth understanding of the relationship between vascular plants and biocrusts in semi-arid climate regions, as well as for predicting the spatial distribution of biocrusts.
{"title":"Distribution and prediction of biocrusts under the canopy of typical vascular plants on the Loess Plateau, Northwest China.","authors":"Ning Liu, Shun-Yao Yu, Cai-Yue Zhang, Yun-Ge Zhao","doi":"10.13287/j.1001-9332.202409.017","DOIUrl":"10.13287/j.1001-9332.202409.017","url":null,"abstract":"<p><p>Vascular plants exert significant effects on micro-environment, thereby affecting the distribution of biological soil crusts (biocrusts). The relationship between vascular plants and the spatial distribution characteristics of biocrusts is largely unknown. We investigated the distribution characteristics of biocrusts under the canopy of vascular plants in the water-wind erosion crisscross area of the Loess Plateau, where larger areas of biocrusts had been formed since the implantation of \"Grain for Green\" project. We analyzed the relationship between the canopy characteristics of different vascular plants and the spatial distribution of biocrusts using correlation analysis and random forest importance ranking methods, and further constructed a predictive model for the area of biocrusts under the canopy of vascular plants. The results showed that: 1) Cyanobacteria crust was the predominant biocrusts, followed by moss crust. 2) The canopy of vascular plants affected the spatial distribution of biocrusts, with notable differences in distribution pattern across different directions under the canopy of vascular plants. Biocrusts were primarily distributed in the 270°-315° and 315°-360° directions, while was less frequent in the 90°-135° and 135°-180° directions. 3) Radially, the coverage of biocrusts gradually increased from the root-base to the edge of the canopy of vascular plants. 4) The coverage of biocrusts under canopy was significantly related to the characteristics of vascular plants, including canopy area, long crown width, short crown width, litter area and plant height. 5) The relative importance of canopy area, long crown width, and short crown width to the biocrusts under the canopy was 13.7%, 12.1%, and 11.9%, respectively, while the relative importance of plant height and species type was relatively low, being 6.7% and 4.4%, respectively. 6) Results of the random forest model demonstrated strong predictive performance for biocrusts distribution based on canopy characteristics of vascular plants, with a prediction accuracy of 0.59 (<i>R</i><sup>2</sup>) and a root mean square error of 1.2 m<sup>2</sup>. This model could be applied to predict and estimate the area of biocrusts under the canopy of vascular plants. This study provided a theoretical basis for in-depth understanding of the relationship between vascular plants and biocrusts in semi-arid climate regions, as well as for predicting the spatial distribution of biocrusts.</p>","PeriodicalId":35942,"journal":{"name":"应用生态学报","volume":"35 9","pages":"2571-2580"},"PeriodicalIF":0.0,"publicationDate":"2024-09-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142476605","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2024-09-18DOI: 10.13287/j.1001-9332.202409.013
Shao-Shan An, Yang Hu, Bao-Rong Wang
The Loess Plateau is renowned for its deep soil layer and rich in organic carbon (C). In recent years, numerous ecological restoration projects have been undertaken on the Loess Plateau, with consequence on the stability of soil organic carbon (SOC). The SOC stability is pivotal for its capacity to sequestrate and store C. However, comprehensive review on the characteristics of SOC stability and its mechanisms during vegetation restoration on the Loess Plateau is scarce. Therefore, we summarized the dynamics of SOC stability during vegetation restoration on the Loess Plateau, discussed the mechanisms of SOC stabilization, including mineral protection, physical protection, and biological mechanisms. Furthermore, we prospected the future development directions and research focus of SOC stability research during vegetation restoration on the Loess Plateau to provide scientific support for theory and technology of soil C sequestration and stabilization during vegetation restoration, and to provide scientific reference for achieving the "double-carbon" goals.
{"title":"Research advance on soil organic carbon stabilization mechanisms during vegetation restoration on the Loess Plateau, Northwest China.","authors":"Shao-Shan An, Yang Hu, Bao-Rong Wang","doi":"10.13287/j.1001-9332.202409.013","DOIUrl":"10.13287/j.1001-9332.202409.013","url":null,"abstract":"<p><p>The Loess Plateau is renowned for its deep soil layer and rich in organic carbon (C). In recent years, numerous ecological restoration projects have been undertaken on the Loess Plateau, with consequence on the stability of soil organic carbon (SOC). The SOC stability is pivotal for its capacity to sequestrate and store C. However, comprehensive review on the characteristics of SOC stability and its mechanisms during vegetation restoration on the Loess Plateau is scarce. Therefore, we summarized the dynamics of SOC stability during vegetation restoration on the Loess Plateau, discussed the mechanisms of SOC stabilization, including mineral protection, physical protection, and biological mechanisms. Furthermore, we prospected the future development directions and research focus of SOC stability research during vegetation restoration on the Loess Plateau to provide scientific support for theory and technology of soil C sequestration and stabilization during vegetation restoration, and to provide scientific reference for achieving the \"double-carbon\" goals.</p>","PeriodicalId":35942,"journal":{"name":"应用生态学报","volume":"35 9","pages":"2413-2422"},"PeriodicalIF":0.0,"publicationDate":"2024-09-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142476620","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2024-09-18DOI: 10.13287/j.1001-9332.202409.039
Yu Tao, Wei-Xin Ou, Xiao Sun
In the past decade, research on the relationships between the supply and demand of ecosystem services has been flourishing. To address issues such as the misuse of supply and demand concepts, methods, and results in current research, we proposed five key aspects that need to be considered to enhance the scientific rigor and practical value in assessing relationships between ecosystem service supply and demand. Firstly, it is essential to clarify the distinctions and connections between the concepts related to ecosystem service supply and demand, which are crucial prerequisites and starting points for assessing their relationships. Secondly, it is necessary to integrate relevant environmental standards or policy objectives to develop reliable methods for assessing the demand for ecosystem regulating services. Furthermore, it is important to properly address the modifiable areal unit problem by determining the most appropriate spatial scale and unit for evaluating relationships between ecosystem service supply and demand. Additionally, it is crucial to differentiate between quantitative and qualitative methods for characterizing (im)balances or (mis)matches between ecosystem service supply and demand, particularly avoiding the use of qualitative methods to represent quantitative relationships between supply and demand. Lastly, it is imperative to integrate ecosystem service flows into the assessment of supply and demand relationships, and evaluate the dynamic supply and demand relationships of regional ecosystem services from a coupled "supply-flow-demand" perspective.
{"title":"Some critical thinking on the integrative assessment of ecosystem service supply and demand relationships.","authors":"Yu Tao, Wei-Xin Ou, Xiao Sun","doi":"10.13287/j.1001-9332.202409.039","DOIUrl":"10.13287/j.1001-9332.202409.039","url":null,"abstract":"<p><p>In the past decade, research on the relationships between the supply and demand of ecosystem services has been flourishing. To address issues such as the misuse of supply and demand concepts, methods, and results in current research, we proposed five key aspects that need to be considered to enhance the scientific rigor and practical value in assessing relationships between ecosystem service supply and demand. Firstly, it is essential to clarify the distinctions and connections between the concepts related to ecosystem service supply and demand, which are crucial prerequisites and starting points for assessing their relationships. Secondly, it is necessary to integrate relevant environmental standards or policy objectives to develop reliable methods for assessing the demand for ecosystem regulating services. Furthermore, it is important to properly address the modifiable areal unit problem by determining the most appropriate spatial scale and unit for evaluating relationships between ecosystem service supply and demand. Additionally, it is crucial to differentiate between quantitative and qualitative methods for characterizing (im)balances or (mis)matches between ecosystem service supply and demand, particularly avoiding the use of qualitative methods to represent quantitative relationships between supply and demand. Lastly, it is imperative to integrate ecosystem service flows into the assessment of supply and demand relationships, and evaluate the dynamic supply and demand relationships of regional ecosystem services from a coupled \"supply-flow-demand\" perspective.</p>","PeriodicalId":35942,"journal":{"name":"应用生态学报","volume":"35 9","pages":"2423-2431"},"PeriodicalIF":0.0,"publicationDate":"2024-09-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142476624","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
In this study, we applied thermal dissipation probe technology to examine sap flow in various directions (east, south, west, and north) and at different depths (0-2, 2-4, 4-6 cm) within the stem of natural Picea mongolica trees in the eastern of Otindag Sandy Land to provide a scientific basis for accurately quantifying water consumption of P. mongolica forests through transpiration and to enhance the understanding of water relations. The results showed that the diurnal variation of sap flow in different directions displayed a unimodal curve, with the sap flow sequence being south>east>west>north. The sap flow at different sapwood depths exhibited an obvious unimodal curve, with a significant decrease as sapwood depth increased. Compared with that calculated from the mean sap flux density in four directions (23.57 kg·d-1), water consumption calculated using the mean value in south-east, east-west, south-west, north-east, north-south, and north-west was overestimated by 10.2%, 5.5%, 14.5%, and underestimated by 12.3%, 8.2%, 9.8%, respectively. The water consumption calculated using the values from the east, south, and west was overestimated by 6.1%, 14.4%, and 15.4%, respectively, and underestimated by 30.7% in the north. In addition, compared with the water consumption calculated from the mean value in three sapwood depths (48.51 kg·d-1), that calculated using sap flux density at sapwood depths of 0-2, 2-4, and 4-6 cm were overestimated by 18.8%, underestimated by 1.7%, and underestimated by 62.9%, respectively. These results indicated that sap flow of P. mongolica had significant azimuthal and radial variations, which considerably influence the estimation of tree water consumption. Installing probes at 0-2 cm simultaneously in both the north and east of the trunk could effectively reduce the estimation error of whole-tree water consumption by 4.2%. This approach enabled the accurate quantification of water consumption of individual P. mongolica trees in sandy areas, thereby improving the precision of transpiration water consumption estimates scaling up from individual level to stand level.
{"title":"Azimuthal and radial variations in sap flow and its effects on the estimation of transpiration for <i>Picea mongolica</i>.","authors":"Xin Liu, Li-Ning Song, Jin-Xin Zhang, Xin-Wei Zhu, Yu-Min Zhao, Qing-Shan Zheng","doi":"10.13287/j.1001-9332.202409.005","DOIUrl":"10.13287/j.1001-9332.202409.005","url":null,"abstract":"<p><p>In this study, we applied thermal dissipation probe technology to examine sap flow in various directions (east, south, west, and north) and at different depths (0-2, 2-4, 4-6 cm) within the stem of natural <i>Picea mongolica</i> trees in the eastern of Otindag Sandy Land to provide a scientific basis for accurately quantifying water consumption of <i>P. mongolica</i> forests through transpiration and to enhance the understanding of water relations. The results showed that the diurnal variation of sap flow in different directions displayed a unimodal curve, with the sap flow sequence being south>east>west>north. The sap flow at different sapwood depths exhibited an obvious unimodal curve, with a significant decrease as sapwood depth increased. Compared with that calculated from the mean sap flux density in four directions (23.57 kg·d<sup>-1</sup>), water consumption calculated using the mean value in south-east, east-west, south-west, north-east, north-south, and north-west was overestimated by 10.2%, 5.5%, 14.5%, and underestimated by 12.3%, 8.2%, 9.8%, respectively. The water consumption calculated using the values from the east, south, and west was overestimated by 6.1%, 14.4%, and 15.4%, respectively, and underestimated by 30.7% in the north. In addition, compared with the water consumption calculated from the mean value in three sapwood depths (48.51 kg·d<sup>-1</sup>), that calculated using sap flux density at sapwood depths of 0-2, 2-4, and 4-6 cm were overestimated by 18.8%, underestimated by 1.7%, and underestimated by 62.9%, respectively. These results indicated that sap flow of <i>P. mongolica</i> had significant azimuthal and radial variations, which considerably influence the estimation of tree water consumption. Installing probes at 0-2 cm simultaneously in both the north and east of the trunk could effectively reduce the estimation error of whole-tree water consumption by 4.2%. This approach enabled the accurate quantification of water consumption of individual <i>P. mongolica</i> trees in sandy areas, thereby improving the precision of transpiration water consumption estimates scaling up from individual level to stand level.</p>","PeriodicalId":35942,"journal":{"name":"应用生态学报","volume":"35 9","pages":"2483-2491"},"PeriodicalIF":0.0,"publicationDate":"2024-09-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142476598","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2024-09-18DOI: 10.13287/j.1001-9332.202409.032
Wen-Jie Bao, Ling-Jie Shen, Shang-Wen Xia, Xiao-Dong Yang
Collar rot caused by Fusarium spp. is a serious threat to the production of Passiflora edulis. However, biocontrol methods are lacking. Trichoderma spp., as the most widely applied biocontrol fungus, can be effective in managing crop diseases. The effectiveness is significantly influenced by environmental factors, such as soil pH. To screen potential biocontrol strains against collar rot of P. edulis, and to explore the effect of pH on the inhibition rate of Trichoderma spp., we selected four Trichoderma species and four Fusarium species isolated from P. edulis planting area in Xishuangbanna. The growth dynamics of different strains under different pH conditions were determined using the mycelial growth rate method. The effect of pH on the growth inhibition of Fusarium spp. by Trichoderma spp. was investigated using the plate confrontation assay. The results showed that the optimal growth pH range was 4-6 for Trichoderma spp. and 7-9 for Fusarium spp. All four Trichoderma strains exhibited significant inhibitory effects on the growth of the four Fusarium strains. T. harzianum showed the most notable inhibition, reaching up to a 72% inhibitory rate. Moreover, pH significantly influenced the inhibitory effect of Trichoderma spp., with variations observed depending on the specific species of Trichoderma spp. and Fusarium spp. Therefore, it is essential to consider the environmental pH impact on the efficacy of biocontrol agents when applying biological control measures in the field, tailored to the specific pathogen and biocontrol agent involved.
{"title":"Effect of pH on the growth and competition of <i>Trichoderma</i> spp. and <i>Fusarium</i> spp.","authors":"Wen-Jie Bao, Ling-Jie Shen, Shang-Wen Xia, Xiao-Dong Yang","doi":"10.13287/j.1001-9332.202409.032","DOIUrl":"10.13287/j.1001-9332.202409.032","url":null,"abstract":"<p><p>Collar rot caused by <i>Fusarium</i> spp. is a serious threat to the production of <i>Passiflora edulis</i>. However, biocontrol methods are lacking. <i>Trichoderma</i> spp., as the most widely applied biocontrol fungus, can be effective in managing crop diseases. The effectiveness is significantly influenced by environmental factors, such as soil pH. To screen potential biocontrol strains against collar rot of <i>P. edulis</i>, and to explore the effect of pH on the inhibition rate of <i>Trichoderma</i> spp., we selected four <i>Trichoderma</i> species and four <i>Fusarium</i> species isolated from <i>P. edulis</i> planting area in Xishuangbanna. The growth dynamics of different strains under different pH conditions were determined using the mycelial growth rate method. The effect of pH on the growth inhibition of <i>Fusarium</i> spp. by <i>Trichoderma</i> spp. was investigated using the plate confrontation assay. The results showed that the optimal growth pH range was 4-6 for <i>Trichoderma</i> spp. and 7-9 for <i>Fusarium</i> spp. All four <i>Trichoderma</i> strains exhibited significant inhibitory effects on the growth of the four <i>Fusarium</i> strains. <i>T. harzianum</i> showed the most notable inhibition, reaching up to a 72% inhibitory rate. Moreover, pH significantly influenced the inhibitory effect of <i>Trichoderma</i> spp., with variations observed depending on the specific species of <i>Trichoderma</i> spp. and <i>Fusarium</i> spp. Therefore, it is essential to consider the environmental pH impact on the efficacy of biocontrol agents when applying biological control measures in the field, tailored to the specific pathogen and biocontrol agent involved.</p>","PeriodicalId":35942,"journal":{"name":"应用生态学报","volume":"35 9","pages":"2535-2542"},"PeriodicalIF":0.0,"publicationDate":"2024-09-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"142476607","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}