[1]Harper K T,Marble J R. A role for non-vascular plants in management of arid and semi-arid rangelands[C]//Tueller P T.Application of Plant Sciences to Rangeland Management and Inventory.Amsterdam:Martinus Nijhoff/W Junk,1998:135-169.[2]Eldridge D J,Greene R S B.Microbiotic soil crusts: a review of their roles in soil and ecological processes in the rangelands of Australia[J].Australia Journal of Soil Research,1994,32:389-415.[3]陈亚宁,李卫红,张元明,等.新疆古尔班通古特沙漠生物结皮在沙丘尺度的生态与环境解释[J].自然科学进展,2005,15(10):1211-1216.[4]张元明,陈晋,王雪芹,等.古尔班通古特沙漠生物结皮的分布特征[J].地理学报,2005,60(1):53-60.[5]郑云普,赵建成,张丙昌,等.荒漠生物结皮中藻类和苔藓植物研究进展[J].植物学报,2009,44(3):371-378.[6]饶本强,刘永定,胡春香,等.人工藻结皮技术及其在沙漠治理中的应用[J].水生生物学报,2009,33(4):756-761.[7]王岩,沈其荣,史瑞和,等.土壤微生物量及其生态效应[J].南京农业大学学报,1996,19(4):45-51.[8]王少昆,赵学勇,曲浩,等.科尔沁沙地和浑善达克沙地流动沙丘中土壤微生物学特征比较[J].环境科学研究,2010,23(12):1516-1522.[9]刘恩科,赵秉强,李秀英,等.长期施肥对土壤微生物量及土壤酶活性的影响[J].植物生态学报,2008,32(1):176-182.[10]Dias-Ravina M,Acea M J,Carbanas T.Microbial biomass and its contribution to nutrient concentration in forest soils[J].Soil Biology and Biochemistry,1993,25:25-31.[11]刘艳梅,李新荣,何明珠,等.生物土壤结皮对土壤微生物量碳的影响[J].中国沙漠,2012,32(3):669-673.[12]杨梅焕,曹明明,朱志梅.毛乌素沙地东南缘沙漠化过程中土壤酶活性的演变研究[J].生态环境学报,2012,21(1):69-73.[13]吴楠,潘伯荣,张元明.土壤微生物在生物结皮形成中的作用及生态学意义[J].干旱区研究,2004,21(4):444-450.[14]韩新宁.土壤酶对土壤环境质量的作用及影响[J].内蒙古农业科技,2008(4):90-92[15]张水印,余明泉,朱玲,等.退化红壤区不同重建模式森林土壤微生物碳氮特征研究[J].江西农业大学学报,2010,32(1):101-107.[16]张其水,俞新妥.杉木连栽林地营造混交林后土壤微生物的季节性动态研究[J].生态学报,1990,10(2):121-126.[17]张丙昌,张元明,王敬竹.古尔班通古特沙漠南缘典型沙垄藻类的时空分布[J].中国沙漠,2011,31(4):919-926.[18]关松荫.土壤酶及其研究方法[M].北京:农业出版社,1986.[19]苏延桂,李新荣,贾小红,等.温带荒漠区藻结皮固氮活性沿时间序列的变化[J].中国沙漠,2012,32(2):421-427.[20]吴楠,张元明.古尔班通古特沙漠生物土壤结皮影响下的土壤酶分布特征[J].中国沙漠,2010,30(5):1128-1136.[21]张元明.荒漠地表生物土壤结皮的微结构及其早期发育特征[J].科学通报,2005,50(1):42-47.[22]周晓兵,张元明,陶冶,等.古尔班通古特沙漠土壤酶活性和微生物量氮对模拟氮沉降的响应[J].生态学报,2011,31(12):3340-3349.[23]Nunan N,Mogan M A,Herlihy M.Ultraviolet absorbance (280 nm) of compounds released from soil during chloroform fumigation as an estimate of the microbial biomass[J].Soil Biology and Biochemistry,1998,30(12):1599-1603.[24]吴金水,林启美,黄巧云,等.土壤微生物生物量测定方法及其应用[M].北京:气象出版社,2006.[25]吴秀臣,孙辉,杨万勤.土壤酶活性对温度和CO2浓度升高的响应研究[J].土壤,2007,39(3):358-363.[26]张丙昌,张元明,赵建成,等.古尔班通古特沙漠生物结皮不同发育阶段中藻类的变化[J].生物学报,2009,29(1):9-17.[27]Mager D M,Thomas A D.Extracellular polysaccharides from cyanobacterial soil crusts:a review of their role in dry land soil processes[J].Journal of Arid Environments,2011,75:91-97.[28]Hernandez D L,Hobbie S E.The effects of substrate composition,quantity,and diversity on microbial activity[J].Plant and Soil,2010,335:397-411.[29]王雪芹,蒋进,雷加强,等.古尔班通古特沙漠短命植物分布及其沙面稳定意义[J].地理学报,2003,58(4):598-605.[30]Shields L M,Dcrrell L W.Algae in relation fertility[J].The Botanical Review,1964,30:92-128.[31]钱亦兵,吴兆宁,张立运,等.古尔班通古特沙漠风沙土微量元素对植被格局的影响[J].中国沙漠,2009,29(6):1100-1108.[32]张静,张元明,周晓兵,等.生物结皮影响下沙漠土壤表面凝结水的形成与变化特征[J].生态学报,2009,29(12):6600-6608.[33]吴楠,张元明,张静,等.生物结皮恢复过程中土壤生态因子分异特征[J].中国沙漠,2007,27(3):397-404.[34]陈荣毅,张元明,潘伯荣,等.古尔班通古特沙漠土壤养分空间分异与干扰的关系[J].中国沙漠,2007,27(2):257-265.[35]Brockett B F T,Prescott C E,Grayston S J.Soil moisture is the major factor influencing microbial community structure and enzyme activities across seven biogeoclimatic zones in western Canada[J].Soil Biology and Biochemistry,2012,44:9-20.[36]吕国红,周广胜,赵先丽,等.土壤碳氮与土壤酶相关性研究进展[J].辽宁气象,2005,(2):6-8.[37]胡君利,林先贵,尹睿,等.浙江慈溪不同利用年限水稻土微生物生物量与酶活性比较[J].生态学报,2008,28(4):1552-1557.[38]Asencio A D,Morte A,García-Carmona F,et al.Partial purification and characterization of a calcium-dependent alkaline phosphatase from the cyanobacterium Arthrospira platensis[J].Journal of Phycology,2012,48:347-354.[39]Rose C,Axler R P.Uses of alkaline phosphatase activity in evaluating phytoplankton community phosphorus deficiency[J].Hydrobiologia,1998,361:145-156. |