首页 | 本学科首页   官方微博 | 高级检索  
     检索      

贵州普定6种喀斯特石生植物及其土壤的碳酸酐酶活性
引用本文:刘天雷,从春蕾,胡 丹,王世杰,张显强.贵州普定6种喀斯特石生植物及其土壤的碳酸酐酶活性[J].中国岩溶,2017,36(2):187-192.
作者姓名:刘天雷  从春蕾  胡 丹  王世杰  张显强
作者单位:1.安顺学院
基金项目:国家自然科学基金项目(41463006)
摘    要:以贵州普定喀斯特石漠化区域石生银叶真藓(Bryum argenteum Hedw.)、扭口藓(Barbula unguiculata Hedw.)、穗枝赤齿藓(Erythrodontium julaceum(Schwaegr.)Par.)、美灰藓(Eurohypnum leptothollum(C. Muell. )Ando.)、东亚砂藓(Racomitrium japonicum Dozy et Molk.)和雪茶(地衣)(Thamnolia vermicularia(Ach.)Asa-hina)为对象,研究了这些石生植物和其基质土壤碳酸酐酶(CA)的活性,可为石生植物的生物岩溶作用机理和石漠化生态环境的治理提供一定的参考。结果表明,6种植物CA的活性存在一定的差异,以美灰藓的CA活性272.99 U·g-1(FW)最高,东亚砂藓的CA活性33.45 U·g-1(FW)最低;银叶真藓基部土壤CA活性最高,为101.81 U·g-1(干土),美灰藓CA活性15.95 U·g-1(干土)最低。CA活性与土壤全磷、全钾、石砾含量和土壤含水量之间呈极显著的相关性。 

关 键 词:喀斯特石漠化    石生植物    碳酸酐酶    土壤

Carbonic anhydrase activity of six epilithic mosses and their underlying soil in the Puding karst area,Guizhou Province
LIU Tianlei,CONG Chunlei,HU Dan,WANG Shijie and ZHANG Xianqiang.Carbonic anhydrase activity of six epilithic mosses and their underlying soil in the Puding karst area,Guizhou Province[J].Carsologica Sinica,2017,36(2):187-192.
Authors:LIU Tianlei  CONG Chunlei  HU Dan  WANG Shijie and ZHANG Xianqiang
Institution:1.Anshun University2.State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences3.Anshun University/State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences
Abstract:The samples of six moss plants include B.argenteum, B.unguiculata, E.julaceum, E.leptothollum, R japonicum and T vermicularia were collected from the karst rock desertification area in Puding of Guizhou, as the objects of this study. The carbonic anhydrase (CA) activity of the epilithic plants and the matrix of soil was studied, from which the analyses of bio-karst mechanism and governance of ecological environments in karst rocky desertification areas can be performed.The results show that there are some differences in carbonic anhydrase activity of six epilithic plants.The E. leptothollum is highest, reaching 272.99 U·g-1(FW), while the minimum is 33.45 U·g-1(FW) in R. japonicum. The B.argenteum base soil CA activity(101.81 U·g-1(dry soil) is the highest. The E. leptothollum is 15.95 U·g-1 (dry soils) as the lowest. It could be concluded that CA activity has positive correlations with plant and soil carbonic anhydrase content of total phosphorus, kalium, gravel and soil moisture, respectively.
Keywords:rock desertification in karst areas  epilithic mosses  carbonic anhydrase  underlying soil
本文献已被 CNKI 等数据库收录!
点击此处可从《中国岩溶》浏览原始摘要信息
点击此处可从《中国岩溶》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号