Zoige Plateau wetlands are located in the northeastern corner of the Qinghai-Tibet Plateau.The landscape pattern evolution processes in the Zoige Plateau and their driving factors were identified by analyzing the dyna...Zoige Plateau wetlands are located in the northeastern corner of the Qinghai-Tibet Plateau.The landscape pattern evolution processes in the Zoige Plateau and their driving factors were identified by analyzing the dynamic changes in landscape modification and conversion and their dynamic rates of alpine wetlands over the past four decades.The results showed that the landscape conversion between wetlands and non-wetlands mainly occurred during the period from 1966 to 1986.The marsh wetland area converted from lake and river wetlands was larger because of swamping compared to other wetland landscapes.Meanwhile,the larger area of marsh wetlands was also converted to lake wetlands more than other types of wetlands.The modification processes mainly occurred among natural wetland landscapes in the first three periods.Obvious conversions were observed between wetland and nonwetland landscapes(i.e.,forestland,grassland,and other landscapes) in the Zoige Plateau.These natural wetland landscapes such as river,lake and marsh wetlands showed a net loss over the past four decades,whereas artificial wetland landscapes(i.e.,paddy field and reservoir and pond wetlands) showed a net decrease.The annual dynamic rate of the whole wetland landscape was 0.72%,in which the annual dynamic rate of river wetlands was the highest,followed by lake wetlands,while marsh wetlands had the lowest dynamic rate.The integrated landscape dynamic rate showed a decreasing trend in the first three periods.The changes in wetland landscape patterns were comprehensively controlled by natural factors and human activities,especially human activities play an important role in changing wetland landscape patterns.展开更多
以若尔盖高原湿地的泥炭沼泽土壤为样,在利用变性梯度凝胶电泳技术(Denaturing gradient gel electrophoresis,DGGE)分析该生境真菌群结构的基础上,进一步通过可培养手段进行高效低温纤维素降解菌株的筛选。DGGE结果表明:阿西茸乡土样...以若尔盖高原湿地的泥炭沼泽土壤为样,在利用变性梯度凝胶电泳技术(Denaturing gradient gel electrophoresis,DGGE)分析该生境真菌群结构的基础上,进一步通过可培养手段进行高效低温纤维素降解菌株的筛选。DGGE结果表明:阿西茸乡土样中真菌群落结构最复杂,其次是达扎寺乡、黑河乡。基于DGGE图谱条带序列的系统发育分析表明:若尔盖高原湿地中的优势真菌分属于白布勒弹孢酵母(Bulleromyces albus),曲霉属(Aspergillus),子黑附球菌(Epicoccum nigrum),假裸囊菌属(Pseudogymnoascus)和深色有隔内生真菌(Zalerion)等类群。通过纯培养从该区域分离到低温纤维素降解真菌50余株,其中S1和S7两株菌酶活最高,分别是9.36 U m L-1和23.01 U m L-1。系统发育分析显示菌株S1为白囊耙齿菌(Irpex lacteus),S7为烟曲霉(Aspergillus fumigatus)。两株菌对水稻秸秆表现出明显的降解效果,50d内S7对半纤维素、纤维素和木质素的降解率分别为46.57%,63.37%和30.74%;而S1对各组分降解率分别为30.02%,54.55%和22.95%。研究表明,若尔盖高原湿地泥炭沼泽土真菌群落结构复杂,具潜在应用价值。展开更多
The Zoige Wetland is located in the northeastern Qinghai-Tibetan Plateau, which is highly sensitive to global environment change and human disturbance because of its high elevation and cold environment, thus, it＇s a ...The Zoige Wetland is located in the northeastern Qinghai-Tibetan Plateau, which is highly sensitive to global environment change and human disturbance because of its high elevation and cold environment, thus, it＇s a hotspot for land use and land cover change （LUCC） research. We used Landsat MSS images from 1975, Landsat ETM images from 2000, and Landsat TM images fi：om 1990 and 2005 to assess the LUCC in the study area, using GIS techniques, as well as topographic, vegetation, and soil maps combined with field investigations. The monitoring result shows that the study area＇s environment degraded rapidly between 1975 and 2005, including wetland shrinkage from 5,308 km2 to 4,980 lan2, sandy land expansion from 112 krn2 to 137 krn2, forest land decreasing from 5,686 km2 to 5,443 km2, and grassland degradation from 12,309 km2 to 10,672 km2. According to the analysis of meteorological data and social-economic statistical data, we concluded that the LUCC in the Zoige Wetland was caused by both natural and anthropogenic factors, but human activities were primarily responsible for the observed LUCC, thereby, we suggest human behaviors must be adjusted to control environmental degradation.展开更多
基金financially supported by National Natural Science Foundation of China(Grant No. 51179006)China National Funds for Distinguished Young Scientists (Grant No.51125035)+2 种基金National Science Foundation for Innovative Research Group (Grant No. 51121003)the Program for New Century Excellent Talents in University (NECT-10-0235)the Fok Ying Tung Foundation (Grant No. 132009)
文摘Zoige Plateau wetlands are located in the northeastern corner of the Qinghai-Tibet Plateau.The landscape pattern evolution processes in the Zoige Plateau and their driving factors were identified by analyzing the dynamic changes in landscape modification and conversion and their dynamic rates of alpine wetlands over the past four decades.The results showed that the landscape conversion between wetlands and non-wetlands mainly occurred during the period from 1966 to 1986.The marsh wetland area converted from lake and river wetlands was larger because of swamping compared to other wetland landscapes.Meanwhile,the larger area of marsh wetlands was also converted to lake wetlands more than other types of wetlands.The modification processes mainly occurred among natural wetland landscapes in the first three periods.Obvious conversions were observed between wetland and nonwetland landscapes(i.e.,forestland,grassland,and other landscapes) in the Zoige Plateau.These natural wetland landscapes such as river,lake and marsh wetlands showed a net loss over the past four decades,whereas artificial wetland landscapes(i.e.,paddy field and reservoir and pond wetlands) showed a net decrease.The annual dynamic rate of the whole wetland landscape was 0.72%,in which the annual dynamic rate of river wetlands was the highest,followed by lake wetlands,while marsh wetlands had the lowest dynamic rate.The integrated landscape dynamic rate showed a decreasing trend in the first three periods.The changes in wetland landscape patterns were comprehensively controlled by natural factors and human activities,especially human activities play an important role in changing wetland landscape patterns.
文摘以若尔盖高原湿地的泥炭沼泽土壤为样,在利用变性梯度凝胶电泳技术(Denaturing gradient gel electrophoresis,DGGE)分析该生境真菌群结构的基础上,进一步通过可培养手段进行高效低温纤维素降解菌株的筛选。DGGE结果表明:阿西茸乡土样中真菌群落结构最复杂,其次是达扎寺乡、黑河乡。基于DGGE图谱条带序列的系统发育分析表明:若尔盖高原湿地中的优势真菌分属于白布勒弹孢酵母(Bulleromyces albus),曲霉属(Aspergillus),子黑附球菌(Epicoccum nigrum),假裸囊菌属(Pseudogymnoascus)和深色有隔内生真菌(Zalerion)等类群。通过纯培养从该区域分离到低温纤维素降解真菌50余株,其中S1和S7两株菌酶活最高,分别是9.36 U m L-1和23.01 U m L-1。系统发育分析显示菌株S1为白囊耙齿菌(Irpex lacteus),S7为烟曲霉(Aspergillus fumigatus)。两株菌对水稻秸秆表现出明显的降解效果,50d内S7对半纤维素、纤维素和木质素的降解率分别为46.57%,63.37%和30.74%;而S1对各组分降解率分别为30.02%,54.55%和22.95%。研究表明,若尔盖高原湿地泥炭沼泽土真菌群落结构复杂,具潜在应用价值。
基金support of the National Natural Science Foundation of China(Grant No.41201002)Foundation for Excellent Youth Scholars of Cold and Arid Regions Environmental and Engineering Research Institute,Chinese Academy of Sciences(Grant No.51Y184A61)+1 种基金China Postdoctoral Science Foundation funded project(Grant No.2012M512050)the National Natural Science Foundation of China(Grant No.41130533,41171010)
文摘The Zoige Wetland is located in the northeastern Qinghai-Tibetan Plateau, which is highly sensitive to global environment change and human disturbance because of its high elevation and cold environment, thus, it＇s a hotspot for land use and land cover change （LUCC） research. We used Landsat MSS images from 1975, Landsat ETM images from 2000, and Landsat TM images fi：om 1990 and 2005 to assess the LUCC in the study area, using GIS techniques, as well as topographic, vegetation, and soil maps combined with field investigations. The monitoring result shows that the study area＇s environment degraded rapidly between 1975 and 2005, including wetland shrinkage from 5,308 km2 to 4,980 lan2, sandy land expansion from 112 krn2 to 137 krn2, forest land decreasing from 5,686 km2 to 5,443 km2, and grassland degradation from 12,309 km2 to 10,672 km2. According to the analysis of meteorological data and social-economic statistical data, we concluded that the LUCC in the Zoige Wetland was caused by both natural and anthropogenic factors, but human activities were primarily responsible for the observed LUCC, thereby, we suggest human behaviors must be adjusted to control environmental degradation.
