Quets J J,Temmerman S,EI-Bana M I,et al.Unraveling landscapes with phytogenic mounds (nebkhas):an exploration of spatial pattern[J].Acta Oecologica,2013,49:53-63.
[3]
Bainbridge D V.Recreating mesquite mounds (nebkas) in the Colorado Desert[J].Restoration Notes,2014,2(1):1-29.
[4]
King J,Nickling W G,Gillies J A.Aeolian shear stress ratio measurements within mesquite-dominated landscapes of the Chihuahuan Desert,New Mexico,USA[J].Geomorphology,2006,82:229-244.
Gillies J A,Nield J M,Nickling W G.Wind speed and sediment transport recovery in the lee of a vegetated and denuded nebkha within a nebkha dune field[J].Aeolian Research,2014,12:135-141.
[7]
Dougill A J,Thomas A D.Nebkha dunes in the Molopo Basin,South Africa and Botswana:formation controls and their validity as indicators of soil degradation[J].Journal of Arid Environments,2002,50:413-428.
[8]
Khalaf F I,Al-Hurban A E,Al-Awadhi J.Morphology of protected and non-protected Nitrariaretusa coastal nabkha in Kuwait,Arabian Gulf:a comparative study[J].Catena,2014,115:115-122.
[9]
Wang X M,Dong Z B,Zhang J W,et al.Formation of the complex linear dunes in the central Taklimakan Sand Sea,China[J].Earth Surface Processes and Landforms,2004,29:677-686.
[10]
Lang L L,Wang X M,Hasi E,et al.Nebkha(coppice dune) formation and significance to environmental change reconstructions in arid and semiarid areas[J].Journal of Geographical Sciences,2013,23(2):344-358.
Wang X M,Lang L L,Hua T,et al.Variations in the wind-energy regime of the Taklimakan Desert,central Asia,over the last 700 years as inferred from nebkha sedimentology and chronology[J].Boreas,2014,43:882-894.
[15]
Wang X M,Zhang C X,Zhang J W,et al.Nebkha formation:implications for reconstructing environmental changes over the past several centuries in the Ala Shan Plateau,China[J].Palaeogeography,Palaeoclimatology,Palaeoecology,2010,297:697-706.
[16]
Xia X C,Zhao Y J,Wang F B,et al.Environmental significance exploration to Tamarix Cone age layer in Lop Nur Lake region[J].Chinese Science Bulletin,2005,50(20):2395-2397.
[17]
Li Z Z,Wu S L,Chen S J,et al.Bio-geomorphologic features and growth process of Tamarixnabkhas in Hotan River Basin,Xinjiang[J].Journal of Geographical Sciences,2010,20(2):205-218.
Wang X M,Dong Z B,Yan P,et al.Wind energy environments and dunefield activity in the Chinese deserts[J].Geomprphology,2005,65:33-48.
[23]
Wang X M,Chen F H,Dong Z B,et al.Evolution of the southern Mu Us Desert in north China over the past 50 years:an analysis using proxies of human activity and climate parameters[J].Land Degradation & Development,2004,15:1-16.
[24]
任明达,王乃梁.现代沉积环境概论[M].北京:科学出版社,1981:1-230.
[25]
Pye K.Aeolian Dust and Dust Deposition[M].London,UK:Academic Press,1987.
[26]
Wang X M,Wang T,Dong Z B,et al.Nebkha development and its significance to wind erosion and land degradation in semi-arid northern China[J].Journal of Arid Environments,2006,65:129-141.
Lang L L,Wang X M,Hua T,et al.Moisture availability over the past five centuries indicated by carbon isotopes of Tamarix taklamakanensis leaves in a nebkha profile in the Central Taklimakan Desert,NW China[J].Aeolian Research,2013,11:101-108.
[31]
Weems S L,Monger H C.Banded vegetation-dune development during the Medieval Warm Period and 20th century,Chihuahuan Desert,New Mexico,USA[J].Ecosphere,2012,3(3):1-16.
[32]
Seifert C L,Cox R T,Forman S L,et al.Relict nebkhas (pimple mounds) record prolonged late Holocene drought in the forested region of south-central United States[J].Quaternary Research,2009,71:329-339.