Research Articles

Nebkha(coppice dune)formation and significance to environmental change reconstructions in arid and semiarid areas

  • 1. Key Laboratory of Desert and Desertification,Cold and Arid Regions Environmental and Engineering Research Institute,CAS,Lanzhou 730000,China;
    2. College of Resources Science and Technology,Beijing Normal University,Beijing 100875,China

Received date: 2012-09-12

  Revised date: 2012-09-29

  Online published: 2013-02-20


Environments in arid and semiarid regions are extremely sensitive to climate changes.High wind activity in these regions has resulted in an extensively developed arid geomorphology,but past environmental changes are poorly understood because of the absence of relatively high-resolution proxies.The accumulation characteristics of nebkhas, which have developed extensively in these regions,can be used as a method of reconstructing environmental changes.Here we summarized recent advances in research on the formation,development,and sediment characteristics of nebkhas and their significance to environmental changes in arid and semiarid regions.Based on the studies of our colleagues, we suggested that research on nebkha formation can provide distinct clues about environmental changes in arid and semiarid regions;however,continued studies are needed.

Cite this article

LANG Lili, WANG Xunming, HASI Eerdun, HUA Ting . 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 . DOI: 10.1007/s11442-013-1014-x


[1] Anderson R S,1991.Wind modification and bed response during saltation of sand in air.Acta Mechanica,1(Suppl.):21–51.

[2] Antoine P,Rousseau D-D,Lautridou J-P et al.,1999.Last interglacial-glacial climatic cycle in loess-palaeosol successions of north-western France.Boreas,28:551–563.

[3] Ash J E,Wasson R J,1983.Vegetation and sand mobility in the Australian desert dunefield.Zeitschrift fur Geomorphologie,45(Suppl.):7–25.

[4] Bagnold R A,1941.The Physics of Blown Sand and Desert Dunes.London:Methuen.

[5] Bailey S D,Wintle A G,Duller G A T et al.,2001.Sand deposition during the last millennium at Aberffraw, Anglesey,North Wales as determined by OSL dating of quartz.Quaternary Science Reviews,20:701–704.

[6] Ballarini M,Wallinga J,Murray A S et al.,2003.Optical dating of young coastal dunes on a decadal time scale.

[7] Quaternary Science Reviews,22:1011–1017.

[8] Bestelmeyer B T,Trujillo D A,Tugel A J et al.,2006.A multi-scale classification of vegetation dynamics in arid lands:What is the right scale for models,monitoring,and restoration?Journal of Arid Environments,65: 296–318.

[9] Brown G,Porembski S,1997.The maintenance of species diversity by miniature dunes in a sand-depleted Haloxylon salicornicum community in Kuwait.Journal of Arid Environments,37:461–473.

[10] Brown G,Porembski S,2000.Phytogenic hillocks and blow-outs as‘safe sites' for plants in an oil-contaminated area of northern Kuwait.Environmental Conservation,27(3):242–249.

[11] Çakan H,Karata? Ç,2006.Interactions between mycorrhizal colonization and plant life forms along the succes- sional gradient of coastal sand dunes in the eastern Mediterranean,Turkey.Ecological Research,21:301–310.

[12] Chen J,Li G,2011.Geochemical studies on the source region of Asian dust.Science China,54(9):1279–1301.

[13] Cooke R,Warren A,Goudie A,1993.Desert Geomorphology.London:UCL Press.

[14] Day A D,Ludeke K L,1993.Plant Nutrients in Desert Environments.Berlin:Springer-Verlag.

[15] Dech J P,Maun M A,2006.Adventitious root production and plastic resource allocation to biomass determine burial tolerance in woody plants from central Canadian coastal dunes.Annals of Botany,98:1095–1105.

[16] Dhir R P,Singhvi A K,Andrews J E et al.,2010.Multiple episodes of aggradation and calcrete formation in Late Quaternary aeolian sands,Central Thar Desert,Rajasthan,India.Journal of Asian Earth Sciences,37:10–16.

[17] Diefendorf A F,Mueller K E,Wing S L et al.,2010.Global patterns in leaf 13C discrimination and implications for studies of past and future climate.PNAS,107(13):5738–5743.

[18] Dong Z,Huang N,Liu X,2005.Simulation of the probability of midair interparticle collisions in an aeolian sal- tating cloud.Journal of Geophysical Research,110,D24113.

[19] Dougill A J,Thomas A D,2002.Nebkha dunes in the Molopo Basin,South Africa and Botswana:formation con- trols and their validity as indicators of soil degradation.Journal of Arid Environments,50:413–428.

[20] Du J,Yan P,Dong Y,2010.The progress and prospects of nebkhas in arid areas.Acta Geographica Sinica,65(3): 339–350.(in Chinese)

[21] Du J,Yan P,E Y,2007.Distribution patterns and characteristics of Nitraria tanutorun nebkha at its different evolvement stages in Minqin County of Gansu Province.Chinese Journal of Ecology,26(8):1165–1170.(in Chinese)

[22] Du J,Yan P,Zhan X et al.,2008.Surface erosion-resistance of Nitraria tangutorun nebkhas at different succes- sion stages in Minqin oasis and related affecting factors.Chinese Journal of Applied Ecology,19(4):763–768. (in Chinese)

[23] Eghbal M K,Southard R J,1993.Stratigraphy and genesis of Durorthids and Haplargids on dissected alluvial fans, western Mojave Desert,California.Geoderma,59(1–4):151–174.

[24] El-Bana M I,Nijs I,Khedr A-H A,2003.The importance of phytogenic mounds(nebkhas)for restoration of arid degraded rangelands in northern Sinai.Restoration Ecology,11(3):317–324.

[25] El-Sheikh M A,Abbadi G A,Bianco P M,2010.Vegetation ecology of phytogenic hillocks(nabkhas)in coastal habitats of Jal Az-Zor National Park,Kuwait:Role of patches and edaphic factors.Flora,205:832–840.

[26] Feng X,Epstein S,1995.Carbon isotopes of trees from arid environments and implications for reconstructing atmospheric CO2 concentration.Geochimica et Cosmochimica Acta,59(12):2599–2608.

[27] Forman S L,Pierson J,2003.Formation of linear and parabolic dunes on the eastern Snake River Plain,Idaho in the nineteenth century.Geomorphology,56:189–200.

[28] Foth H D,Turk L M,Millar C E,1972.Fundamentals of Soil Science.New York:Wiley.

[29] Hanson P R,Joeckel R M,Young A R et al.,2009.Late Holocene dune activity in the Eastern Platte River Valley, Nebraska.Geomorphology,103:555–561.

[30] He Z,Zhao W,2004.Spatial pattern of two dominant shrub populations at transitional zone between oasis and desert of Heihe River Basin.Chinese Journal of Applied Ecology,15(6):947–952.(in Chinese)

[31] Herrmann H J,Durán O,Parteli E J R et al.,2010.Vegetation and induration as sand stabilizators.Journal of Coastal Research,24(6):1357–1368.

[32] Hesp P A,1981.The formation of shadow dunes.Journal of Sedimentary Petrology,51:101–111.

[33] Hesp P,McLachlan A,2000.Morphology,dynamics,ecology and fauna of Arctotheca populifolia and Gazania rigens nabkha dunes.Journal of Arid Environments,44:155–172.

[34] Hugenholtz C H,Wolfe S A,2005.Recent stabilization of active sand dunes on the Canadian prairies and relation to recent climate variations.Geomorphology,68:131–147.

[35] Indermühle A,Stocker T F,Joos F et al.,1999.Holocene carbon-cycle dynamics based on CO2 trapped in ice at Taylor Dome,Antarctica.Nature,398:121–126.

[36] Jia X,Li X,2008.Spatial pattern of sand-mound of Nitraria in different habitat at the southern fringe of the Tengger Desert.Environmental Science,29(7):2046–2053.(in Chinese)

[37] Kéfi S,Rietkerk M,van Baalen M et al.,2007.Local facilitation,bistability and transitions in arid ecosystems.

[38] Theoretical Population Biology,71:367–379.

[39] Khalaf F I,Al-Awadhi J M,2012.Sedimentological and morphological characteristics of gypseous coastal nabkhas on Bubiyan Island,Kuwait,Arabian Gulf.Journal of Arid Environments,82:31–43.

[40] Khalaf F I,Misak R,Al-Dousari A,1995.Sedimentological and morphological characteristics of some nabkha deposits in the northern coastal plain of Kuwait,Arabia.Journal of Arid Environments,29:267–292.

[41] King J,Nickling W G,Gillies J A,2006.Aeolian shear stress ratio measurements within mesquite-dominated landscapes of the Chihuahuan Desert,New Mexico,USA.Geomorphology,82:229–244.

[42] Kocurek G,Lancaster N,1999.Aeolian system sediment state:Theory and Mojave Desert Kelso dune field ex- ample.Sedimentology,46(3):505–515.

[43] Kuriyama Y,Mochizuki N,Nakashima T,2005.Influence of vegetation on aeolian sand transport rate from a backshore to foredune at Hasaki,Japan.Sedimentology,52:1123–1132.

[44] Lancaster N,Baas A,1998.Influence of vegetation cover on sand transport by wind:Field studies at Owens Lake, California.Earth Surface Processes and Landforms,23:69–82.

[45] Lancaster N,1981.Paleoenvironmental implications of fixed dune systems in Southern Africa.Palaeogeography, Palaeoclimatology,Palaeoecology,33(4):327–346.

[46] Lancaster N,1995.Geomorphology of Desert Dunes.London and New York:Routledge.

[47] Langford R P,2000.Nabkha(coppice dune)fields of south-central New Mexico,U.S.A.Journal of Arid Envronments,46:25–41.

[48] Leenders J K,van Boxel J H,Sterk G,2007.The effect of single vegetation elements on wind speed and sediment transport in the Sahelian zone of Burkina Faso.Earth Surface Processes and Landforms,32:1454–1474.

[49] Li P X,Wang N,He W M et al.,2008.Fertile islands under Artemisia ordosica in inland dunes of northern China: Effects of habitats and plant developmental stages.Journal of Arid Environments,72:953–963.

[50] Li Q,He Z,Zhao W et al.,2004.Spatial pattern of Nitraria sphaerocarpa population and dynamics in different habitats.Journal of Desert Research,24(4):484–488.(in Chinese)

[51] Li W,2009.A preliminary study on Tamarix nabkhas in Aibi Lake of Xinjiang
[D].Urumqi:Xinjaing Normal University,22–25.(in Chinese)

[52] Li Z,Wu S,Chen S et al.,2010.Bio-geomorphologic features and growth process of Tamarix nabkhas in Hotan River Basin,Xinjiang.Journal of Geographical Sciences,20(2):205–218.

[53] Lipp J,Trimborn P,Edwards T et al.,1996.Climatic effects on the δ18O and δ13C of cellulose in the desert tree Tamarix jordanis.Geochimica et Cosmochimica Acta,60(17):3305–3309.

[54] Liu B,Zhao W Z,Yang R,2008.Characteristics and spatial heterogeneity of Tamarix ramosissina Nebkahas at desert-oasis ecotone.Acta Ecologica Sinica,28(4):1446–1455.(in Chinese)

[55] Liu J,Li Z,Wu S et al.,2009.The spatial heterogeneity of morphologic feature of Nitraria nebkhas around Ebi- nur Lake,Xinjiang.Journal of Desert Research,29(4):628–635.(in Chinese)

[56] Liu W,Liu Z,An Z et al.,2011.Wet climate during the‘Little Ice Age’in the arid Tarim Basin,northwestern China.Holocene,21(3):409–416.

[57] Marston R A,1986.Maneuver-caused wind erosion impacts,south central New Mexico.In:Nickling W G eds.

[58] Aeolian Geomorphology.Boston:Allen and Unwin,273–290.

[59] McGlynn I O,Okin G S,2006.Characterization of shrub distribution using high spatial resolution remote sensing: Ecosystem implications for a former Chihuahuan Desert grassland.Remote Sensing of Environment,101: 554–566.

[60] Mckee E D,1982.Sediment Structures in Dunes of the Namib Desert,South West Africa.Boulder:Geological Society of America,48–49.

[61] Melton F A,1940.A tentative classification of sand dunes its application to dune history in the southern High Plains.Geology,48(2):113–174.

[62] Mountney N P,Russell A J,2006.Coastal aeolian dune development,Sólheimasandur,southern Iceland.Sedimentary Geology,192:167–181.

[63] Mu G,1994.The environmental significance of vegetation cones of the Taklimakan Desert,China.Arid Zone Research,11(1):34–41.(in Chinese)

[64] Nickling W G,Wolfe S A,1994.The morphology and origin of nabkhas,region of Mopti,Mali,West Africa.Journal of Arid Environments,28:13–30.

[65] Nield J M,Baas A C W,2008a.Investigating parabolic and nebkha dune formation using a cellular automaton modelling approach.Earth Surface Processes and Landforms,33:724–740.

[66] Nield J M,Baas A C W,2008b.The influence of different environmental and climatic conditions on vegetated aeolian dune landscape development and response.Global and Planetary Change,64:76–92.

[67] Okin G S,Gillette D A,Herrick J E,2006.Multi-scale controls on and consequences of aeolian processes in landscape change in arid and semi-arid environments.Journal of Arid Environments,65:253–275.

[68] Pye K,Tsoar H,1990.Aeolian Sand and Sand Dunes.London and Boston:Unwin Hyman.

[69] Qong M,Takamura H,1997.The formative process of Tamarix cones in the southern part of the Taklimakan Desert,China.Journal of Arid Land Studies,6:121–130.

[70] Qong M,Takamura H,Hudaberdi M,2002.Formation and internal structure of Tamarix cones in the Taklimakan Desert.Journal of Arid Environments,50:81–97.

[71] Rhodes E J,Pownall L,1994.Zeroing of the OSL signal in quartz from young glaciofluvial sediments.Radiation Measurements,23(2/3):581–585.

[72] Seifert C L,Randel T C,Forman S L et al.,2009.Relict nebkhas(pimple mounds)record prolonged late Holocene drought in the forested region of south-central United States.Quaternary Research,71:329–339.

[73] Tengberg A,1995.Nebkha dunes as indicators of wind erosion and land degradation in the Sahel zone of Burkina Faso.Journal of Arid Environments,30:265–282.

[74] Tengberg A,Chen D,1998.A comparative analysis of nebkhas in central Tunisia and northern Burkina Faso.

[75] Geomorphology,22:181–192.

[76] Tilk M,Mandre M,Kl??eiko J et al.,2011.Ground vegetation under natural stress conditions in Scots pine forests on fixed sand dunes in southwest Estonia.Journal of Forest Research,16:223–227.

[77] Tsoar H,2001.Types of aeolian sand dunes and their formation.In:Balmforth,N J,Provenzale A eds.Geomorphological Fluids Mechanics.New York:Lecture Note in Physics,Springer,582:403–429.

[78] Wang X,Wang T,Dong Z et al.,2006.Nebkha development and its significance to wind erosion and land degradation in semi-arid northern China.Journal of Arid Environments,65:129–141.

[79] Wang X,Xiao H,Li J et al.,2008.Nebkha development and its relationship to environmental change in the Alaxa Plateau,China.Environmental Geology,56:359–365.

[80] Wang X,Zhang C,Zhang J et al.,2010.Nebkha formation:Implications for reconstructing environmental changes over the past several centuries in the Ala Shan Plateau,China.Palaeogeography,Palaeoclimatology,Palaeoecology,297:697–706.

[81] Wang Y Q,Zhang X Y,Arimoto R et al.,2005.Characteristics of carbonate content and carbon and oxygen isotopic composition of northern China soil and dust aerosol and its application to tracing dust sources.Atmospheric Environment,39:2631–2642.

[82] Weems S L,Monger H C,2012.Banded vegetation-dune development during the Medieval Warm Period and 20th century,Chihuahuan Desert,New Mexico,USA.Ecological Society of America,3(3):1–16.

[83] White B R,Greeley R,Iversen J D et al.,1976.Estimated grain saltation in a martian atmosphere.Journal of Geophysical Research,81(32):5643–5650.

[84] Wiggs G F S,Thomas D S G,Bullard J E et al.,1995.Dune mobility and vegetation cover in the southwest Ka- lahari Desert.Earth Surface Processes and Landforms,20:515–529.

[85] Wu S,Jiao L,Chen S et al.,2009.The shape character and development stage of nebkha.High Technology Let-ters,15(4):440–445.

[86] Wu S,Li Z,Hui J et al.,2008.The morphological characteristics and growth mode of nabkha in the basin of Hotan River,Xinjiang.Geographical Research,27(2):314–322.(in Chinese)

[87] Wu S,Li Z,Xiao C et al.,2006.Research progress on nebkhas and research significance.Journal of Desert Research,26(5):734–738.(in Chinese)

[88] Xia X,Cao Q,Wang F et al.,2005a.Significance of studying age layers of Tamarix ramosissima sand-hillock in Lop Nur region,Xinjiang.Arid Land Geography,28(5):565–568.(in Chinese)

[89] Xia X,Zhao Y,Wang F et al.,2004.Stratification features of Tamarix cone and its possible age significance.

[90] Chinese Science Bulletin,49(14):1539–1540.

[91] Xia X,Zhao Y,Wang F et al.,2005b.Nebkha formation and its environmental significances in the Lop Nor, China.Chinese Science Bulletin,50(19):2176–2177.(in Chinese)

[92] Xie G,Steinberger Y,2005.Nitrogen and carbon dynamics under the canopy of sand dune shrubs in a desert ecosystem.Arid Land Research and Management,19:147–160.

[93] Yakir D,Issar A,Gat J et al.,1994.13C and 18O of wood from the Roman siege rampart in Masada,Israel(AD 70–73):Evidence for a less arid climate for the region.Geochimica et Cosmochimica Acta,58(16): 3535–3539.

[94] Yue X,Hasi,Zhuang Y et al.,2005.Studies on sandy grassland nebkhas:A review.Journal of Desert Research, 25(5):738–743.(in Chinese)

[95] Zhang P,Hasi E,Yue X et al.,2008.Nitaria nebkhas:Morphology and sediments.Arid Land Geography,31(6): 926–932.(in Chinese)

[96] Zhang P,Yang J,Zhao L et al.,2011.Effect of Caragana tibetica nebkhas on sand entrapment and fertile islands in steppe-desert ecotones on the Inner Mongolia Plateau,China.Plant and Soil,347:79–90.

[97] Zhao Y,Li X,Xia X et al.,2011.C and N contents in organic matter of Tamarix dune sedimentary veins and environmental change in Lop Nur region.Journal of Arid Land Resources and Environment,25(4):149–154. (in Chinese)

[98] Zhao Y,Song Y,Xia X et al.,2009.Grain-size features of sand materials in sedimentary veins of Tamarix cone in Lop Nur region.Journal of Arid Land Resources and Environment,23(12):103–107.(in Chinese)

[99] Zhao Y,Xia X,Wang F et al.,2007.Grain-size features of sand materials in Tamarix cone veins and theirs environmental indication significance in Lop Nur region.Arid Land Geography,30(6):791–796.(in Chinese)

[100] Zhu Z,Chen G,1994.Sandy Desertification in China.Beijing:Science Press.(in Chinese)

[101] Zuo X A,Zhao X Y,Zhao H L et al.,2010.Spatial pattern and heterogeneity of soil organic carbon and nitrogen in sand dunes related to vegetation change and geomorphic position in Horqin Sandy Land,northern China.

[102] Environmental Monitoring and Assessment,164:29–42.