[1] El-Bana M I,Nijs I,Kockelbergh F.Microenvironmental and vegetational heterogeneity induced by phytogenic nebkhas in an arid coastal ecosystem[J].Plant and Soil,2002,247(2):283-293. [2] Tengberg A.Nebkha dunes as indicators of wind erosion and land degradation in the Sahel zone of Burkina Faso[J].Journal of Arid Environments,1995,30(3):265-282. [3] 岳兴玲,哈斯,庄燕美,等.沙质草原灌丛沙堆研究综述[J].中国沙漠,2005,25(5):738-743. [4] 靳建辉,曹相东,李志忠,等.艾比湖周边灌丛沙堆风沙沉积记录的气候环境演化[J].中国沙漠,2013,33(5):1314-1323. [5] 武胜利,李志忠,惠军,等.和田河流域灌(草)丛沙堆的形态特征与发育过程[J].地理研究,2008(2):314-322. [6] 孙祥,于卓.白刺根系的研究[J].中国沙漠,1992,12(4):50-54. [7] 来风兵,孙虎,张展赫,等.塔克拉玛干沙漠和田河西侧胡杨沙堆的形态特征及空间分布格局[J].中国沙漠,2015,35(2):284-293. [8] 高永,党晓宏,虞毅,等.乌兰布和沙漠东南缘白沙蒿(Artemisia sphaeroce phala)灌丛沙堆形态特征与固沙能力[J].中国沙漠,2015,35(1):1-7. [9] 吴正.华南海岸风沙地貌研究[M].北京:科学出版社,1995. [10] Langford R P.Nabkha (coppice dune) fields of south-central New Mexico,U.S.A.[J].Journal of Arid Environments,2000,46(1):25-41. [11] Ardon K,Tsoar H,Blumberg D G.Dynamics of nebkhas superimposed on a parabolic dune and their effect on the dune dynamics[J].Journal of Arid Environments,2009,73(11):1014-1022. [12] Mountney N P,Russell A J.Coastal aeolian dune development,Sólheimasandur,southern Iceland[J].Sedimentary Geology,2006,192(3/4):167-181. [13] Ruz M-H,Héquette A,Marin D,et al.Development of large nebkhas along an accreting ma-crotidal coastline,Northern France[J].Aeolian Research,2017,24:1-14. [14] Hesp P.Morphology,dynamics and internal stratification of some established foredunes in southeast Australia[J].Sedimentary Geology,1988,55(1/2):17-41. [15] Houser C,Ellis J.10.10 Beach and dune interaction[J].Treatise on Geomorphology,2013,10:267-288. [16] Hesp P,Mclachlan A.Morphology,dynamics,ecology and fauna of Arctotheca populifolia and Gazania rigens nabkha dunes[J].Journal of Arid Environments,2000,44(2):155-172. [17] 中国科学院中国植物志委员会.中国植物志第十卷.第一分册,被子植物门,单子叶植物纲,禾本科(四)画眉草亚科黍亚科[M].北京:科学出版社,1990. [18] 杜建会,刘安隆,董玉祥,等.华南海岸典型沙生植物根系构型特征[J].植物生态学报,2014,38(8):888-895. [19] 杨显基,杜建会,秦晶,等.福建平潭岛海岸不同演化阶段草丛沙堆表面老鼠艻叶水势日变化特征[J].应用生态学报,2017,28(10):3260-3266. [20] 李天光,高伟,周庆杰,等.东海岛东北部砂质岸滩年度冲淤变化及沉积物运移分析[J].海岸工程,2016,35(4):10-18. [21] 张萍,哈斯,岳兴玲,等.白刺灌丛沙堆形态与沉积特征[J].干旱区地理,2008,31(6):926-932. [22] 成都地质学院陕北队.沉积岩(物)粒度分析及其应用[M].北京:科学出版社,1978. [23] Folk R L,Ward W C.Brazos River bar:a study in the significance of grain size para-meters[J].Journal of Sedimentology Petrology,1957,27(1):3-26. [24] Edwin D M.世界沙海的研究[M].赵兴梁,译.银川:宁夏人民出版社,1993. [25] 张正偲,董治宝.黑河流域中游沙漠风能环境与风沙地貌[J].中国沙漠,2014,34(2):332-341. [26] 董治宝,苏志珠,钱广强,等.库姆塔格沙漠风沙地貌[M].北京:科学出版社,2011. [27] 陈东,张宇清,吴斌,等.毛乌素沙地南缘油蒿(Artemisia ordosica)灌丛沙堆形态特征[J].中国沙漠,2015,35(3):565-572. [28] 孔芳芳,谭利华,伍永秋,等.柴达木盆地不同沉积区灌丛沙堆形态与沉积特征[J].北京师范大学学报:自然科学版,2016,52(1):56-62. [29] Gao S.A FORTRAN program for grain-size trend analysis to define net sediment transport pathways[J].Computers & Eosciences,1996,22(4):449-452. [30] Le Roux J S.Linear dune trends and wind directions in the northern Cape Province,South Africa[J].South African Geographer,1990,17:35-42. [31] 朱震达.塔克拉玛干沙漠风沙地貌研究[M].北京:科学出版社,1981. [32] Martínez M L,Psuty N P.Coastal Dunes:Ecology and Conservation[M].Berlin,Germany:Springer,2004. [33] Masselink G,Hughes M G.An Introduction to Coastal Processes and Geomorphology[M].Cambridge,UK:Cambridge University Press,2003. [34] 杜建会,严平,董玉祥.干旱地区灌丛沙堆研究现状与展望[J].地理学报,2010,65(3):339-350. [35] Gao S,Collins M B,Lanckneus J,et al.Grain size trends associated with net sediment transport patterns:an example from the Belgian continental shelf[J].Marine Geology,1994,121(3/4):171-185. [36] Hesp P.Morphodynamics of incipient foredunes in New South Wales,Australia[J].Developments in Sedimentology,1983,38:325-342. |