Eroded Dunes: Inspiration from Mars

  • Zhibao DONG ,
  • Chao LI ,
  • Ping Lü ,
  • Guangyin HU
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  • Planetary Aeolian Research Institute,Shaanxi Normal University,Xi'an 710119,China
Dong Zhibao (1966-), male, Hengshan County, Shaanxi Province, Professor. Research areas include physics of blown sand and aeolian geomorphology. E-mail:zbdong@snnu.edu.cn

Received date: 2020-11-18

  Revised date: 2021-01-28

  Online published: 2021-04-19

Supported by

the National Natural Science Foundation of China "Weathering rate of the dry denudated mountains surrounding the Tarim Basin"(41930641);"Formation of the meagadune system in China's Badain Jaran Sand Sea"(41871008)

Abstract

Aeolian landforms are divided into two categories: wind deposition landforms and wind erosion landforms. The former refers to various types of sand dunes with their shapes being determined by the spatio-temporal variation of wind erosion and deposition. Wind erosion may play a significant role in reshaping the cumulated dunes which results in the formation of eroded dunes. This discovery is contrary to traditional understanding, therefore, eroded dunes have been ignored for a long time. However, many Martian dunes with subtle differences from dunes on the earth due to limited sediment supply have been found. We reviewed the description of eroded dunes by French M. Mainguet, and conceptual framework of controlling factors on dune morphology, and then pointed out clearly the necessity of studying eroded dunes. After systematic study on Martian dunes, we found ten types of eroded dunes, and then analyzed the morphology, development environment and possible formation mechanism. The vast saline-alkali land in the arid area of the earth which is similar to the limited sand supply environment on Mars is most likely to develop eroded dunes. Based on this, it can be inferred that eroded dunes are common on the earth, and the study on them is of great significance to the development of aeolian geomorphology theories and the Mars exploration in China.

Cite this article

Zhibao DONG , Chao LI , Ping Lü , Guangyin HU . Eroded Dunes: Inspiration from Mars[J]. Advances in Earth Science, 2021 , 36(2) : 125 -138 . DOI: 10.11867/j.issn.1001-8166.2021.023

References

1 SCHATZ V, TSOAR H, DGETT K S, et al. Evidence for indurated sand dunes in the Martian north polar region[J]. Journal of Geophysical Research, 2006, 111(E4): E04006.
2 DONG Zhibao,Lü Ping,LI Chao. Research methodology of Martian aeolian geomorphology[J]. Advances in Earth Science,2020,35(8):771-788.
2 董治宝, 吕萍, 李超. 火星风沙地貌研究方法[J]. 地球科学进展, 2020, 35(8): 771-788.
3 DONG Zhibao,Lü Ping,LI Chao,et al. Characteristics and formation mechanism of wind streaks on Mars[J]. Advances in Earth Science,2020,35(9):902-911.
3 董治宝, 吕萍, 李超, 等. 火星风条痕特征及其形成机制[J]. 地球科学进展, 2020, 35(9): 902-911.
4 DONG Zhibao,Lü Ping,LI Chao,et al. Unique aeolian bedforms of Mars:Transverse Aeolian Ridges(TARs)[J]. Advances in Earth Science,2020,35(7):661-677.
4 董治宝, 吕萍, 李超, 等. 火星独特风沙地貌之横向沙脊[J]. 地球科学进展, 2020, 35(7): 661-677.
5 LI Chao, DONG Zhibao, Lü Ping, et al. A morphological insight into the Martian dune geomorphology [J]. Chinese Science Bulletin, 2020, 65(1): 80-90.
5 李超, 董治宝, 吕萍, 等. 火星沙丘地貌的形态学窥究[J]. 科学通报, 2020, 65(1): 80-90.
6 MAINGUET M: A classification of dunes based on aeolian dynamics and the sand budget[M]//El-Baz F. Deserts and arid lands. Dordrecht: Springer Netherlands, 1984: 31-58.
7 LIVINGSTONE I, WARREN A. Aeolian geomorphology: An introduction[M]. Harlow: Addison Wesley Longman Ltd., 1996.
8 HACK J T. Dunes of the Western Navajo Country[J]. Geographical Review, 1941, 31(2): 240-263.
9 MCKEE E D. A study of global sand seas[M]. Washington D C: U.S. Government Printing Office, 1979.
10 FRYBERGER S G, DEAN G. Dune forms and wind regime[M]//Mckee E D. A study of global sand seas, Washington DC: U.S. Government Printing Office, 1979: 137-169.
11 WASSON R J, HYDE R. Factors determining desert dune type[J]. Nature, 1983, 304(5 924): 337-339.
12 LANCASTER N. Geomorphology of desert dunes[M]. New York: Routledge, 1995.
13 LANCASTER N. The Namib sand and sea dune forms, processes and sediments[M]. Rotterdam: A. A. Balkema, 1989.
14 KERR R C, NIGRA J O. Eolian sand control[J]. AAPG Bulletin, 1952, 36(8): 1 541-1 573.
15 BOURKE M C, GOUDIE A S. Varieties of barchan form in the Namib Desert and on Mars[J]. Aeolian Research, 2009, 1(1/2): 45-54.
16 EDGETT K S, MALIN M C. Examples of Martian Sandstone: Indurated, Lithified, and Cratered Eolian Dunes in MGS MOC Images [C]. 31st Annual Lunar and Planetary Science Conference, 2000.
17 ZIMBELMAN J R, BOURKE M C, LORENZ R D. Recent developments in planetary Aeolian studies and their terrestrial analogs[J]. Aeolian Research, 2013, 11: 109-126.
18 CARDINALE M, SILVESTRO S, VAZ D A, et al. Present-day aeolian activity in Herschel Crater, Mars[J]. Icarus, 2016, 265: 139-148.
19 FISHBAUGH K E. Chasma Boreale, Mars: Topographic characterization from Mars Orbiter Laser Altimeter data and implications for mechanisms of formation[J]. Journal of Geophysical Research, 2002, 107(E3): 5 013.
20 DAY M D, CATLING D C. Dune casts preserved by Partial Burial: The first identification of Ghost Dune Pits on Mars[J]. Journal of Geophysical Research: Planets, 2018, 123(6): 1 431-1 448.
21 DE Silva S L, SPAGNUOLO M G, BRIDGES N T, et al. Gravel-mantled megaripples of the Argentinean Puna: A model for their origin and growth with implications for Mars[J]. Geological Society of America Bulletin, 2013, 125(11/12): 1 912-1 929.
22 XIAO Long, WANG Jiang, DANG Yanan, et al. A new terrestrial analogue site for Mars research: The Qaidam Basin, Tibetan Plateau (NW China)[J]. Earth-Science Reviews, 2017, 164: 84-101.
23 DONG Zhibao. Atlass of Tibet Plateau aeolian geomorphology[M]. Xi'an: Xi'an Map Publishing House, 2017.
23 董治宝. 青藏高原风沙地貌图集[M]. 西安: 西安地图出版社, 2017.
24 RUBIN D M, RUBIN A M. Origin and lateral migration of linear dunes in the Qaidam Basin of NW China revealed by dune sediments, internal structures, and optically stimulated luminescence ages, with implications for linear dunes on Titan: Discussion[J]. Geological Society of America Bulletin, 2013, 125(11/12): 1 943-1 946.
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