Quantitative analysis of planation surfaces of the upper Yangtze River in the Sichuan-Yunnan Region, Southwest China

Abstract

Identification of the planation surfaces (PSs) is key for utilizing them as a reference in studying the long-term geomorphological evolution of the Upper Yangtze River Basin in the Sichuan-Yunnan region, Southwest China. Using a combined method of DEM-based fuzzy logic and topographic and river profiles analysis and based on a comprehensive analysis of four morphometric parameters: slope, curvature, terrain ruggedness index, and relative height, we established the relevant fuzzy membership functions, and then calculated the membership degree (MD) of the study area. Results show that patches with a MD>80% and an area>0.4 km² correspond well to the results of Google Earth and field investigation, representing the PS remnants. They consist of 1764 patches with an altitude, area, mean slope, and relief of mostly 2000–2500 m above sea level (asl), 0–10 km², 4°–9°, 0–500 m, respectively, covering 9.2% of the study area’s landscape, dipping to southeast, decreasing progressively from northwest to southeast in altitude, and with no clear relation between each patch’s altitude and slope, or relief. All these results indicate that they are remnants of once regionally continuous PSs which were deformed by both the lower crust flow and the faults in upper crust, and dissected by the network of Upper Yangtze River. Additionally, topographic and river profiles analysis show that three PSs (PS1–PS3) well developed along the main valleys in the Yongren-Huili region, indicating several phases of uplift then planation during the Late Cenozoic era. Based on the incision amount deduced from projection of relict river profiles on PSs, together with erosion rates, breakup times of the PS1, PS2, and PS3 were estimated to be 3.47 Ma, 2.19 Ma, and 1.45 Ma, respectively, indicating appearance of modern Upper Yangtze River valley started between the Pliocene to early Pleistocene.

Graphical abstract

Keywords

planation surface / fuzzy logic / topographic analysis / river profile analysis / Upper Yangtze River / Southwest China

References

[1] Adams G F (1975). Planation surfaces: peneplains, pediplains, and etchplains. Benchmark Paper in Geology 22. Stroudsburg PA: Dowden, Hutchington and Ross, 476

[2] Ahnert F (1998). Introduction to Geomorphology. London: Amold

[3] Bascom F (1921). Cycles of erosion in the Piedmont province of Pennsylvania. J Geol, 29(6): 540–559

[4] Bessin P, Guillocheau F, Robin C, Schroëtter J M, Bauer H (2015). Planation surfaces of the Armorican Massif (western France): denudation chronology of a Mesozoic land surface twice exhumed in response to relative crustal movements between Iberia and Eurasia. Geomorphology, 233: 75–91

[5] Bishop P (2007). Long-term landscape evolution: linking tectonics and surface processes. Earth Surf Process Landf, 32(3): 329–365

[6] Bonow J M (2004). Palaeosurfaces and palaeovalleys on North Atlantic previously glaciated passive margins: reference forms for conclusions on uplift and erosion. Institutionen för naturgeografi och kvartärgeologi

[7] Bonow J M, Japsen P, Lidmar-Bergström K, Chalmers J A, Pedersen A K (2006a). Cenozoic uplift of Nuussuaq and Disko, West Greenland—Elevated erosion surfaces as uplift markers of a passive margin. Geomorphology, 80(3–4): 325–337

[8] Bonow J M, Japsen P, Nielsen T F (2014). High-level landscapes along the margin of southern East Greenland—A record of tectonic uplift and incision after breakup in the NE Atlantic. Global Planet Change, 116(2): 10–29

[9] Bonow J M, Lidmar-Bergström K, Japsen P (2006b). Palaeosurfaces in central West Greenland as reference for identification of tectonic movements and estimation of erosion. Global Planet Change, 50(3–4): 161–183

[10] Bosch G V, Van Den Driessche J, Babault J, Robert A, Carballo A, Le Carlier C, Loget N, Prognon C, Wyns R, Baudin T (2016). Peneplanation and lithosphere dynamics in the Pyrenees. C R Geosci, 348: 194–202

[11] Burrough P A, McDonell R A (1998). Principles of geographical information systems. New York: Oxford University Press, 190

[12] Calvet M, Gunnell Y, Farines B (2015). Flat-topped mountain ranges: their global distribution and value for understanding the evolution of mountain topography. Geomorphology, 241: 255–291

[13] Chen F B (1992). Hengduan event: an important tectonic event of the Late Cenozoic in Eastern Asian. Mountain Research, 10(1): 195– 202

[14] Clark M K, House M A, Royden L H, Whipple K X, Burchfiel B C, Zhang X, Tang W (2005). Late Cenozoic uplift of southeastern Tibet. Geology, 33(6): 525–528

[15] Clark M K, Royden L H (2000). Topographic ooze: building the eastern margin of Tibet by lower crustal flow. Geology, 28(8): 703–706

[16] Clark M K, Royden L H, Whipple K X, Burchfiel B C, Zhang X, Tang W (2006). Use of a regional, relict landscape to measure vertical deformation of the eastern Tibetan Plateau. J Geophys Res, 111(F3): F03002

[17] Clark M K, Schoenbohm L M, Royden L H, Whipple K X, Burchfiel B C, Zhang X, Tang W, Wang E, Chen L (2004). Surface uplift, tectonics, and erosion of eastern Tibet from large-scale drainage patterns. Tectonics, 23(1): TC1006

[18] Clift P D, Sun Z (2006). The sedimentary and tectonic evolution of the Yinggehai – Song Hong basin and the southern Hainan margin, South China Sea: implications for Tibetan uplift and monsoon intensification. J Geophys Res, 111(B6): B06405

[19] Coltorti M, Firuzabadi D, Borri A, Fantozzi P, Pieruccini P (2015). Planation surfaces and the long-term geomorphological evolution of Ethiopia. In: Billi P, eds. Landscapes and Landforms of Ethiopia. Springer Netherlands, 51(6): 117–136

[20] Cui Z J, Li D W, Feng J L, Liu G N, Li H J (2001a). Covered karst, weathering crust and karst planation surface. Sci China Earth Sci, 31(6): 510–520

[21] Cui Z J, Li D W, Liu G N, Feng J L, Zhang W (2001b). The properties of the lateritic karst weathering crust and the formation environment of planation surfaces in Tibet, Yunnan, Guizhou, and Hunan province. Sci China Earth Sci, 31: 134–141

[22] Davis W M (1889a). The rivers and valleys of Pennsylvania. National Geographic Society, 1: 183–253

[23] Davis W M (1889b). Topographic development of the Triassic formation of the Connecticut Valley. American Journal of Science, 3rd Ser., 37: 423–434

[24] Davis W M (1899). The geographical cycle. Geogr J, 14(5): 481–504

[25] Feng J L, Cui Z J, Zhang W, Li D W, Liu G N, Zhu L P (2004). Genesis of the layered landform surfaces in Dongchuan, Yunan Province. J Mt Sci, 22(2): 165–174

[26] Flint J J (1974). Stream gradient as a function of order, magnitude, and discharge. Water Resour Res, 10(5): 969–973

[27] Foster M A, Kelsey H M (2012). Knickpoint and knickzone formation and propagation, South Fork Eel River, northern California. Geosphere, 8(2): 403–416

[28] Guillocheau F, Simon B, Baby G, Bessin P, Robin C, Dauteuil O (2018). Planation surfaces as a record of mantle dynamics: the case example of Africa. Gondwana Res, 53(1): 82–98

[29] Hack J T (1973). Stream-profile analysis and stream-gradient index. J Res US Geol Surv, 1(4): 421–429

[30] Haider V L, Dunkl I, Eynatten H V, Ding L, Frei D, Zhang L Y (2013). Cretaceous to Cenozoic evolution of the northern Lhasa Terrane and the Early Paleogene development of peneplains at Nam Co, Tibetan Plateau. J Asian Earth Sci, 70–71(1): 79–98

[31] Haider V L, Kropáček J, Dunkl I, Wagner B, von Eynatten H (2015). Identification of peneplains by multi-parameter assessment of digital elevation models. Earth Surf Process Landf, 40(11): 1477–1492

[32] Harkins N, Kirby E, Heimsath A, Robinson R, Reiser U (2007). Transient fluvial incision in the headwaters of the Yellow River, northeastern Tibet, China. J Geophys Res Earth Surf, 112(F3), https://doi.org/10.1029/2006JF000570

[33] He Z, Zhang X, Bao S, Qian Y S, Sheng Y Y, Liu X T, He X L, Yang X C, Zhao J X, Liu R, Lu C Y (2015). Multiple climatic cycles imprinted on regional uplift-controlled fluvial terraces in the lower Yalong River and Anning River, SE Tibetan Plateau. Geomorphology, 250: 95–112

[34] Hetzel R, Dunkl I, Haider V, Strobl M, Von Eynatten H, Ding L, Frei D (2011). Peneplain formation in southern Tibet predates the India-Asia collision and plateau uplift. Geology, 39(10): 983–986

[35] Huang M H (1992). Research on the stratified landform in the Southwest of China. Journal of Suzhou Railway Teachers College, 9(4): 57–63 (in Chinese)

[36] Huggett R J (2016). Fundamentals of Geomorphology. London: Routledge, 436

[37] Japsen P, Bonow J M, Green P F, Chalmers J A, Lidmar-Bergström K (2009). Formation, uplift and dissection of planation surfaces at passive continental margins—A new approach. Earth Surf Process Landf, 34(5): 683–699

[38] Jarvis A, Reuter H I, Nelson A, Guevara E (2008). Hole-filled SRTM for the globe Version 4. CGIAR-CSI SRTM 90m Database.

[39] Johansson M (1999). Analysis of digital elevation data for palaeosurfaces in south-western Sweden. Geomorphology, 26(4): 279–295

[40] Jolivet M, Ritz J F, Vassallo R, Larroque C, Braucher R, Todbileg M, Chauvet A, Sue C, Arnaud N, de Vicente R Arzhanikova A, Arzhanikov S (2007). Mongolian summits: an uplifted, flat, old but still preserved erosion surface. Geology, 35(10): 871–874

[41] Kennan L, Lamb S, Hoke L (1997). High-altitude palaeosurfaces in the Bolivian Andes: evidence for late Cenozoic surface uplift. Geol Soc Lond Spec Publ, 120(1): 307–323

[42] King L C (1962). Morphology of the Earth. Edinburgh: Oliver and Boyd

[43] Kirby E, Regalla C, Ouimet W B, Bierman P R (2010). Reconstructing temporal variation in fault slip from footwall topography: an example from Saline valley, California, 2010 Fall Meeting, American Geophysical Union, San Francisco, CA

[44] Kirby E, Whipple K X (2012). Expression of active tectonics in erosional landscapes. J Struct Geol, 44: 54–75

[45] Kühni A, Pfiffner O A (2001). The relief of the Swiss Alps and adjacent areas and its relation to lithology and structure: topographic analysis from a 250-m DEM. Geomorphology, 41(4): 285–307

[46] Legrain N, Stüwe K, Wölfler A (2014). Incised relict landscapes in the Eastern Alps. Geomorphology, 221: 124–138

[47] Lei C, Ren J Y, Sternai P, Fox M, Willett S, Xie X N, Clift P D, Liao J H, Wang Z F (2015). Structure and sediment budget of Yinggehai–Song Hong basin, South China Sea: implications for Cenozoic tectonics and river basin reorganization in Southeast Asia. Tectonophysics, 655: 177–190

[48] Li C, Jiang X, Gong W, Li D, Li C (2018). Surface uplift of the Central Yunnan Plateau since the Pliocene. Geol J, 53: 386–396

[49] Li H, Huang X Y, Deng Q L, Kusky T M, Cai X B (2012). Mapping of planation surfaces in the southwest region of Hubei Province, China—Using the DEM-derived painted relief model. J Earth Sci, 23(5): 719–730

[50] Li J J (1999). In memory of Davisian theory of erosion cycle and peneplain: a centurial study in China. Journal of Lanzhou University (Natural Sciences), 35(3): 157–163

[51] Li J J, Shi Y F, Li B Y (1995). Uplift of the Qinghai-Xizang (Tibet) Plateau and global change. Lanzhou University Press, 1451–1452

[52] Li J J, Xie S Y, Kuang M S (2001). Geomorphic evolution of the Yangtze Gorges and the time of their formation. Geomorphology, 41(2–3): 125–135

[53] Lidmar-Bergström K, Bonow J M, Japsen P (2013). Stratigraphic landscape analysis and geomorphological paradigms: Scandinavia as an example of Phanerozoic uplift and subsidence. Global Planet Change, 100: 153–171

[54] Liu-Zeng J, Tapponnier P, Gaudemer Y, Ding L (2008). Quantifying landscape differences across the Tibetan plateau: implications for topographic relief evolution. J Geophys Res Earth Surf, 113(F04018): 1–26

[55] Ma Z H, Li X M, Guo B H, Yu H, Ye X Y, Song C H, Li J J (2016). Extraction and analysis of Maxianshan planation surfaces in northeastern margin of the Tibetan Plateau. Acta Geogr Sin, 71(3): 400–411

[56] Miller S R, Sak P B, Kirby E, Bierman P R (2013). Neogene rejuvenation of central Appalachian topography: evidence for differential rock uplift from stream profiles and erosion rates. Earth Planet Sci Lett, 369–370: 1–12

[57] Monkhouse F J, Wilkinson H R (1952). Population Maps and Diagrams. Maps and Diagrams, Methuen, London

[58] Niemann J D, Gasparini N M, Tucker G E, Bras R L (2001). A quantitative evaluation of Playfair’s law and its use in testing long-term stream erosion models. Earth Surf Process Landf, 26(12): 1317–1332

[59] Olaya V (2009). Basic land-surface parameters. In: Hengl T, Reuter H I, eds. Developments in Soil Science, 33: 141–169

[60] Pan B T, Hu Z B, Wang J P, Vandenberghe J, Hu X F, Wen Y H, Li Q, Cao B (2012). The approximate age of the planation surface and the incision of the Yellow River. Palaeogeography, Palaeoclimatology, Palaeoecology, 356: 54–61

[61] Peckham S D, Hengl T, Evans J, Wilson J P, Gould M (2011). Profile, plan and streamline curvature: a simple derivation and applications. In: Proceedings of the International Society for Geomorphometry, Redlands, CA. 27–30

[62] Pike R J (2000). Geomorphometry: diversity in quantitative surface analysis. Prog Phys Geogr, 24(1): 1–20

[63] Qian Y, Xiong L, Li J, Tang G (2016). Landform planation index extracted from DEMs: a case study in Ordos Platform of China. Chin Geogr Sci, 26(3): 314–324

[64] Reuter H I, Nelson A, Jarvis A (2007). An evaluation of void-filling interpolation methods for SRTM data. Int J Geogr Inf Sci, 21(9): 983–1008

[65] Rigon R, Rinaldo A, Rodriguez-Iturbe I (1994). On landscape self-organization. J Geophys Res, 99(11): 911–971

[66] Riley S J, DeGloria S D, Elliot R (1999). A terrain ruggedness index that quantifies topographic heterogeneity. Intermt J Sci, 5(1–4): 23–27

[67] Ringrose P S, Migon P (1997). Analysis of digital elevation data for the Scottish Highlands and recognition of pre-Quaternary elevated surfaces. Geol Soc Lond Spec Publ, 120(1): 25–35

[68] Rowberry M D (2012). A comparison of three terrain parameters that may be used to identify denudation surfaces within a GIS: a case study from Wales, United Kingdom. Comput Geosci, 43: 147–158

[69] Rowberry M D, Brewer P A, Macklin M G (2007). The number, form and origin of sub-horizontal surfaces in north Ceredigion, Wales UK. Norwegian Journal of Geology/Norsk Geologisk Forening, 87(1–2): 207–222

[70] Royden L H, Burchfiel B C, King R W, Wang E, Chen Z, Shen F, Liu Y (1997). Surface deformation and lower crustal flow in Eastern Tibet. Science, 276(5313): 788–790

[71] Schoenbohm L M, Whipple K X, Burchfiel B C, Chen L (2004). Geomorphic constraints on surface uplift, exhumation, and plateau growth in the Red River region, Yunnan Province, China. Geol Soc Am Bull, 116(7): 895–909

[72] Sevon W D, Potter N Jr, Crowl G (1983). Appalachian peneplains: an historical review. Earth Sci Hist, 2(2): 156–164

[73] Shackleton R, Chang C (1988). Cenozoic uplift and deformation of the Tibetan Plateau: the geomorphological evidence. Philosophical Transactions of the Royal Society A, 327(1594): 365–377

[74] Shen J, Wang S M, Wang Y, Qiang X K, Xiao H F, Xiao X Y (2010). Uplift events of the Qinghai–Tibetan Plateau and environmental evolution of the southwest monsoon since 2.7 Ma, recorded in a long lake sediment core from Heqing, China. Quat Int, 218(1–2): 67–73

[75] Strobl M, Hetzel R, Ding L, Zhang L, Hampel A (2010). Preservation of a large-scale bedrock peneplain suggests long-term landscape stability in southern Tibet. Z Geomorphol, 54(4): 453–466

[76] Su H, Ming Q Z, Pan B T, Gao H S, Zhang W X, Dong M, Shi Z T (2013). The analysis and discussions on the chronological frame of Jinshajiang River valley-drainage. J Mt Sci, 31(6): 685–692

[77] Van der Beek P, van Melle J, Guillot S, Pêcher A, Reiners P W, Nicolescu S, Latif M (2009). Eocene Tibetan Plateau remnants preserved in the northwest Himalaya. Nat Geosci, 2(5): 364–368

[78] Twidale C R (1976). On the survival of paleoforms. Am J Sci, 276(1): 77–95

[79] Vandenberghe J (2016). From planation surfaces to river valleys. BSGLg, 67: 93–106

[80] Veselský M, Bandura P, Burian L, Harciníková T, Bella P (2015). Semi-automated recognition of planation surfaces and other flat landforms: a case study from the Aggtelek Karst, Hungary. Open Geosciences, 7(1): 799–811

[81] Wang E, Burchfiel B C (2000). Late Cenozoic to Holocene deformation in southwestern Sichuan and adjacent Yunnan, China, and its role in formation of the southeastern part of the Tibetan Plateau. Geol Soc Am Bull, 112(3): 413–423

[82] Wang E, Burchfiel B C, Royden L H, Chen L, Chen J, Li W, Chen Z (1998). Late Cenozoic Xianshuihe-Xiaojiang, Red River, and Dali fault systems of southwestern Sichuan and central Yunnan, China. Spec Pap Geol Soc Am, 327: 1–108

[83] Wang X, Lu H, Vandenberghe J, Zheng S, van Balen R (2012). Late Miocene uplift of the NE Tibetan Plateau inferred from basin filling, planation and fluvial terraces in the Huang Shui catchment. Global Planet Change, 88– 89: 10–19

[84] Wang Y, Pan B, Gao H, Liu Y (2005). Planation surface extraction and quantitative analysis based on high-resolution digital elevation models. International Geoscience and Remote Sensing Symposium, 8: 5369–5371

[85] Whipple K X, Dibiase R A, Ouimet W B, Forte A M (2017). Preservation or piracy: diagnosing low-relief, high-elevation surface formation mechanisms. Geology, 45(1): 91–94

[86] Widdowson M (1997). The geomorphological and geological importance of palaeosurfaces. Geol Soc Lond Spec Publ, 120(1): 1–12

[87] Wobus C W, Crosby B T, Whipple K X (2006). Hanging valleys in fluvial systems: controls on occurrence and implications for landscape evolution. J Geophys Res, 111(F2): F02017

[88] Xie M (1990). Neotectonic uplift velocity and type along the Changjiang River during Quaternary. Quaternary Sciences, 4: 308–315 (in Chinese)

[89] Xiong L Y, Tang G A, Zhu A X, Qian Y Q (2017). A peak-cluster assessment method for the identification of upland planation surfaces. Int J Geogr Inf Sci, 31(2): 387–404

[90] Yang R, Willett S D, Goren L (2015). In situ low-relief landscape formation as a result of river network disruption. Nature, 520(7548): 526–529

[91] Zadeh L A (1968). Fuzzy algorithms. Inf Control, 12(2): 94–102

[92] Zárate M, Folguera A (2014). Planation surfaces of Central Western Argentina. In: Rabassa J, Ollier C, eds. Gondwana Landscapes in Southern South America. Springer Netherlands, 365–392

[93] Zevenbergen L W, Thorne C R (1987). Quantitative analysis of land surface topography. Earth Surf Process Landf, 12(1): 47–56

[94] Zhang K, Huang Y K (1995). Researches on the planation surfaces in north Guangdong. Trop Geogr, 15(4): 295–305

[95] Zhang Y C, Li J J, Zhu J J, Kuang M S, Chen Y (1999). Studies on development of Yuanmou basin and valleys during Late Cenozoic. Journal of Lanzhou University (Natural Sciences), 35(1): 199–205

[96] Zheng H, Clift P D, Wang P, Tada R, Jia J, He M, Jourdan F (2013). Pre-Miocene birth of the Yangtze River. Proc Natl Acad Sci USA, 110(19): 7556–7561

[97] Zhou S, Xu L, Cui J, Zhang X, Zhao J (2005). Geomorphologic evolution and environmental changes in the Shaluli Mountain region during the Quaternary. Chin Sci Bull, 50(1): 52–57

[98] Zhu R X, Potts R, Pan Y X, Lü L Q, Yao H T, Deng C L, Qin H F (2008). Paleomagnetism of the Yuanmou Basin near the southeastern margin of the Tibetan Plateau and its constraints on late Neogene sedimentation and tectonic rotation. Earth Planet Sci Lett, 272(1–2): 97–104

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