Abstract
Owing to the remoteness of the Longriba area and the lack of dating records, it is extremely challenging to reconstruct the chronology and extent of the paleoglaciers in this area. In this paper, we combined limited observational data with automated modelling for paleoglacial reconstructions. We first identified a broadly distributed paleoglacier from satellite imagery and field investigation based on the sediment-landform assemblage principle and dated it to 23.1±1.4∼19.5±1.2 ka by 10Be exposure dating, corresponding to the global Last Glacial Maximum (gLGM). Then, we reconstructed the extent and ice surface of 171 paleoglaciers formed during the similar period based on geomorphological evidence and ‘ice surface profile’ modelling. The results showed that the paleoglacial coverage was 426.5 km2, with an ice volume of 38.1 km3, in the Longriba area. The reconstructed equilibrium line altitudes (ELAs) based on modelled ice surfaces yielded an average of 4245±66 m above sea level (asl), ∼725±73 m lower than the present ELA (4970±29 m asl). The temperature was ∼5.51–6.68 °C lower, and the precipitation was ∼30–34% less in Longriba, during the gLGM compared to the present day. This glacial advance was mainly driven by colder climate that was synchronous with Northern Hemisphere cooling events.
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References
Bai M, Chevalier M-L, Pan J, et al. (2018) Southeastward increase of the late Quaternary slip-rate of the Xianshuihe fault, eastern Tibet. Geodynamic and seismic hazard implications. Earth Planet Sci Lett 485: 19–31. https://doi.org/10.1016/j.epsl.2017.12.045
Balco G (2011) Contributions and unrealized potential contributions of cosmogenic-nuclide exposure dating to glacier chronology, 1990–2010. Quat Sci Rev 30: 3–27. https://doi.org/10.1016/j.quascirev.2010.11.003
Balco G, Stone JO, Lifton NA, et al. (2008) A complete and easily accessible means of calculating surface exposure ages or erosion rates from 10Be and 26Al measurements. Quat Geochronol 3: 174–195. https://doi.org/10.1016/j.quageo.2007.12.001
Barr ID, Clark CD (2011) Glaciers and climate in Pacific Far NE Russia during the last Glacial maxium. J Quat Sci 26: 227–237. https://doi.org/10.1002/jqs.1450
Benn DI, Hulton NRJ (2010) An Excel™ spreadsheet program for reconstructing the surface profile of former mountain glaciers and ice caps. Comput Geosci 36: 605–610. https://doi.org/10.1016/j.cageo.2009.09.016
Benn DI, Ballantyne CK (2005) Palaeoclimatic reconstruction from Loch Lomond Readvance glaciers in the West Drumochter Hills, Scotland. J Quat Sci 20: 577–592. https://doi.org/10.1002/jqs.925
Benn DI, Owen LA, Osmaston HA, et al. (2005) Reconstruction of equilibrium-line altitudes for tropical and sub-tropical glaciers. Quat Int 138–139: 8–21. https://doi.org/10.1016/j.quaint.2005.02.003
Blatter H (1995) Velocity and stress fields in grounded glaciers: a simple algorithm for including deviatoric stress gradients. J Glaciol 41: 333–344. https://doi.org/10.3189/S002214300001621X
Borchers B, Marrero S, Balco G, et al. (2016) Geological calibration of spallation production rates in the CRONUS-Earth project. Quat Geochronol 31: 188–198. https://doi.org/10.1016/j.quageo.2015.01.009
Caidong C, Sorteberg A (2010) Modelled mass balance of Xibu glacier, Tibetan Plateau: sensitivity to climate change. J Glaciol 56(196): 235–248. https://doi.org/10.3189/002214310791968467
Cao J, Guo J (2001) Quaternary ice age division and paleoclimate and paleoenvrionment in the Huanglong Nature Reserve, Songpan. Acta Geologica Sichuan 21: 141–146. (In Chinese)
Chandler BMP, Boston CM, Lukas S (2019) A spatially-restricted Younger Dryas plateau icefield in the Gaick, Scotland: Reconstruction and palaeoclimatic implications. Quat Sci Rev 211: 107–135. https://doi.org/10.1016/j.quascirev.2019.03.019
Chandler BMP, Lukas S (2017) Reconstruction of Loch Lomond Stadial (Younger Dryas) glaciers on Ben More Coigach, northwest Scotland, and implications for reconstructing palaeoclimate using small ice masses. J Quat Sci 32: 475–492. https://doi.org/10.1002/jqs.2941
Chevalier M-L, Leloup PH, Replumaz A, et al. (2016) Tectonic-geomorphology of the Litang fault system, SE Tibetan Plateau, and implication for regional seismic hazard. Tectonophysics 682: 278–292. https://doi.org/10.1016/j.tecto.2016.05.039
Chevalier M-L, Leloup PH, Replumaz A, et al. (2017) Temporally constant slip rate along the Ganzi fault NW Xianshuihe fault system, eastern Tibet. Geology 130: 396–410. https://doi.org/10.1130/B31691.1
Chevalier M-L, Replumaz A (2019) Deciphering old moraine age distributions in SE Tibet showing bimodal climatic signal for glaciations: Marine Isotope Stages 2 and 6. Earth Planet Sci Lett 507: 105–118. https://doi.org/10.1016/j.epsl.2018.11.033
Clark PU, Shakun JD, Baker PA, et al. (2012) Global climate evolution during the last deglaciation. Proc Natl Acad Sci USA 109: E1134–E1142. https://doi.org/10.1073/pnas.1116619109
Cui H, Wang J, Yu B, et al. (2018) Marine Isotope Stage 3 paleotemperature inferred from reconstructing the Die Shan ice cap, northeastern Tibetan Plateau. Quat Res 89: 494–504. https://doi.org/10.1017/qua.2018.9
Dong G, Xu X, Zhou W, et al. (2017) Cosmogenic 10Be surface exposure dating and glacier reconstruction for the Last Glacial Maximum in the Quemuqu Valley, western Nyainqentanglha Mountains, south Tibet. J Quat Sci 32: 639–652. https://doi.org/10.1002/jqs.2963
Embleton C, King CAM (1975) Glacial Geomorphology. Printed in Great Britain by Butler & Tanner Ltd: Frome and London.
Fu P, Heyman J, Hättestrand C, et al. (2012) Glacial geomorphology of the Shaluli Shan area, southeastern Tibetan Plateau. J Maps 8: 48–55. https://doi.org/10.1080/17445647.2012.668762
Fu P, Stroeven AP, Harbor JM, et al. (2013) Paleoglaciation of Shaluli Shan, southeastern Tibetan Plateau. Quat Sci Rev 64: 121–135. https://doi.org/10.1016/j.quascirev.2012.12.009
Graf AA, Strasky S, Zhao Z, et al. (2008) Glacier extension on the eastern TP in response to MIS 2 cooling, with a contribution to 10Be and 21Ne methodology. In: Strasky S, (Ed.), Glacial Response to Global Climate Changes: Cosmogenic Nuclide Chronologies from High and Low Latitudes. ETH.
Heinrich H (1988) Origin and consequences of cyclic ice rafting in the northeast Atlantic Ocean during the past 130, 000 years. Quat Res 29: 142–152. https://doi.org/10.1016/0033-5894(88)90057-9
Herzschuh U (2006) Palaeo-moisture evolution in monsoon Central Asia during the last 50,000 years. Quat Sci Rev 25: 163–178. https://doi.org/10.1016/j.quascirev.2005.02.006
Heyman J, Hättestrand C, Stroeven AP (2008) Glacial geomorphology of the Bayan Har sector of the NE Tibetan Plateau. J Maps 4: 42–62. https://doi.org/10.4113/jom.2008.96
Heyman J, Stroeven AP, Caffee MW, et al. (2011) Palaeoglaciology of Bayan Har Shan, NE TP: exposure ages reveal a missing LGM expansion. Quat Sci Rev 30: 1988–2001. https://doi.org/10.1016/j.quascirev.2011.05.002
Hu G, Yi C, Zhang J, et al. (2016) Late Quaternary glacial advances in the eastern Qilianshan, north-eastern Tibet, as inferred from luminescence dating of fluvioglacial sediments. J Quat Sci 31: 587–597. https://doi.org/10.1002/jqs.2882
James WHM, Carrivick JL (2016) Automated modelling of spatially-distributed glacier ice thickness and volume. Comput Geosci 92: 90–103. https://doi.org/10.1016/j.cageo.2016.04.007
James WHM, Carrivick JL, Quincey DJ, et al. (2019) A geomorphology based reconstruction of ice volume distribution at the Last Glacial Maximum across the Southern Alps of New Zealand. Quat Sci Rev 219: 20–35. https://doi.org/10.1016/j.quascirev.2019.06.035
Jiang D, Lang X, Tian Z, et al. (2011) Last glacial maximum climate over China from PMIP simulations. Paleogeogr Paleoclimatol Paleoecol 309: 347–357. https://doi.org/10.1016/j.palaeo.2011.07.003
Jiang D, Liu Ye, Lang X (2019) A multi-model analysis of glacier equilibrium line altitudes in western China during the last glacial maximum. Sci China Earth Sci 62: 1241–1255. https://doi.org/10.1007/s11430-018-9266-8
Kassab C, Harbor JM (2013) Alternative coordinate systems for analyzing cross-section shapes of glaciated valleys: a case study from the Dalijia Mountains, China. Phys Geogr 34: 108–123. https://doi.org/10.1080/02723646.2013.787580
Kohl CP, Nishiizumi K (1992) Chemical isolation of quartz for measurement of in-situ-produced cosmogenic nuclides. Geochim Cosmochim Acta 56: 3583–3587. https://doi.org/10.1016/0016-7037(92)90401-4
Kong P, Na C, Fink D, et al. (2009) Moraine dam related to late Quaternary glaciation in the Yulong Mountains, southwest China, and impacts on the Jinsha River. Quat Sci Rev 28: 3224–3235. https://doi.org/10.1016/j.quascirev.2009.08.005
Lal D (1991) Cosmic ray labeling of erosion surfaces: in situ nuclide production rates and erosion models. Earth Planet Sci Lett 104: 424–439. https://doi.org/10.1016/0012-821X(91)90220-C
Li Y (2013) Determining topographic shielding from digital elevation models for cosmogenic nuclide analysis: a GIS approach and field validation. J Mt Sci 10: 355–362. https://doi.org/10.1007/s11629-013-2564-1
Li Y, Liu G, Chen Y, et al. (2014) Timing and extent of Quaternary glaciations in the Tianger Range, eastern Tian Shan, China, investigated using 10Be surface exposure dating. Quat Sci Rev 98: 7–23. https://doi.org/10.1016/j.quascirev.2014.05.009
Lifton N, Sato T, Dunai TJ (2014) Scaling in situ cosmogenic nuclide production rates using analytical approximations to atmospheric cosmic-ray fluxes. Earth Planet Sci Lett 386: 149–160. https://doi.org/10.1016/j.epsl.2013.10.052
Lindholm MS, Heyman J (2016) Glacial geomorphology of the Maidika region, Tibetan Plateau. J Maps 12: 797–803. https://doi.org/10.1080/17445647.2015.1078182
Lisiecki LE, Raymo ME (2005) A Pliocene-Pleistocene stack of 57 globally distributed benthic δ18O records. Paleoceanography 20: PA 1003. https://doi.org/10.1029/2004PA001071
Liu B, Cui Z, Peng X, et al. (2018) Using 10Be exposure dating to constrain glacial advances during the Late Glacial and Holocene on Mount Xuebaoding, eastern TP. Quat Res 90: 348–359. https://doi.org/10.1017/qua.2018.33
Mix AC, Bard E, Schneider R (2001) Environmental processes of the ice age: land, oceans, glaciers (EPILOG). Quat Sci Rev 20: 627–657. https://doi.org/10.1016/S0277-3791(00)00145-1
Nishiizumi K, Imamura M, Caffee MW, et al. (2007) Absolute calibration of 10Be AMS standards. Nucl Instrum Meth B 258: 403–413. https://doi.org/10.1016/j.nimb.2007.01.297
Nye DJF (1952) A method of calculating the thickness of the ice-stress. Nature 169: 529–530. https://doi.org/10.1038/169529a0
Ohmura A, Kasser P, Funk M (1992) Climate at the equilibrium line of glaciers. J Glaciol 38: 397–411. https://doi.org/10.3189/S0022143000002276
Ou X, Lai Z, Zhou S, et al. (2014) Timing of glacier fluctuations and trigger mechanisms in eastern Qinghai-Tibetan Plateau during the late Quaternary. Quat Res 81: 464–475. https://doi.org/10.1016/j.yqres.2013.09.007
Owen LA, Benn DI (2005) Equilibrium-line altitudes of the Last Glacial Maximum for the Himalaya and Tibet: an assessment and evaluation of results. Quat Int 138–139: 55–78. https://doi.org/10.1016/j.quaint.2005.02.006
Owen LA, Dortch JM (2014) Nature and timing of Quaternary glaciation in the Himalayan-Tibetan orogeny. Quat Sci Rev 88: 14–54. https://doi.org/10.1002/jqs.1203
Owen LA, Finkel RC, Barnard PL, et al. (2005) Climatic and topographic controls on the style and timing of Late Quaternary glaciation throughout Tibet and the Himalaya defined by 10Be cosmogenic radionuclide surface exposure dating. Quat Sci Rev 24: 1391–1411. https://doi.org/10.1016/j.quascirev.2004.10.014
Owen LA, Finkel RC, Ma H, et al. (2003a) Timing and style of Late Quaternary glaciations in northeastern Tibet. Geology 115: 1356–1364. https://doi.org/10.1130/B25314.1
Owen LA, Ma H, Derbyshire E, et al. (2003b) The timing and style of Late Quaternary glaciation in the La Ji Mountains, NE Tibet: evidence for restricted glaciation during the latter part of the Last Glacial. Z Geomorphol 130: 263–276. https://doi.org/10.1016/S0277-3791(02)00164-6
Owen LA, Spencer JQ, Ma H, et al. (2003c) Timing of Late Quaternary glaciation along the southwestern slopes of the Qilian Shan. Boreas 32: 281–291. https://doi.org/10.1016/S0277-3791(02)00164-6
Peirce B (1852) Criterion for the rejection of doubtful observations. Astron J 2: 161. https://doi.org/10.1086/100259
Pellitero R, Fernández-Fernández JM, Campos N, et al. (2019) Late Pleistocene climate of the northern Iberian Peninsula: New insights from palaeoglaciers at Fuentes Carrionas (Cantabrian Mountains). J Quat Sci 34: 342–354. https://doi.org/10.1002/jqs.3106
Pellitero R, Rea BR, Spagnolo M, et al. (2015) A GIS tool for automatic calculation of glacier equilibrium-line altitudes. Comput Geosci 82: 55–62. https://doi.org/10.1016/j.cageo.2015.05.005
Pellitero R, Rea BR, Spagnolo M, et al. (2016) GlaRe, a GIS tool to reconstruct the 3D surface of palaeoglaciers. Comput Geosci 94: 77–85. https://doi.org/10.1016/j.cageo.2016.06.008
Peng X, Chen Y, Li Y, et al. (2020) Late Holocene glacier fluctuations in the Bhutanese Himalaya. Glob Planet Change 187: 103137. https://doi.org/10.1016/j.gloplacha.2020.103137
Peng X, Chen Y, Liu G, et al. (2018) Late Quaternary glaciations in the Cogarbu valley, Bhutanese Himalaya. J Quat Sci 2018: 40–50. https://doi.org/10.1002/jqs.3079
Porter SC (1975) Equilibrium-line altitudes of late Quaternary glaciers in the Southern Alps, New Zealand. Quat Res 5: 27–47. https://doi.org/10.1016/0033-5894(75)90047-2
Ramage JM, Smith JA, Rodbell DT, et al. (2005) Comparing reconstructed Pleistocene equilibrium-line altitudes in the tropical Andes of central Peru. J Quat Sci 20: 778–788. https://doi.org/10.1002/jqs.982
Rea BR (2009) Defining modern day area-altitude balance ratios (AABRs) and their use in glacier-climate reconstructions. Quat Sci Rev 28: 237–248. https://doi.org/10.1016/j.quascirev.2008.10.011
Ross SM (2003) Peirce’s criterion for the elimination of suspect experimental data. J Eng Technol 20: 38–41.
Rowe P (2015) The paired t-test: comparing two related sets of measurements. In: Essential statistics for the pharmaceutical sciences. John Wiley & Sons, Ltd. pp 163–175.
Saha S, Owen LA, Orr EN, et al. (2019) High-frequency Holocene glacier fluctuations in the Himalayan-Tibetan orogeny. Quat Sci Rev 220: 372–400. https://doi.org/10.1016/j.quascirev.2019.07.021
Sanchez Goñi MF, Harrison SP (2010) Millennial-scale climate variability and vegetation changes during the Last Glacial: concepts and terminology. Quat Sci Rev 29: 2823–2827. https://doi.org/10.1016/j.quascirev.2009.11.014
Shen C, Tang L, Wang S (1996) Vegetation and climate during the last 250000 years in Zoigê region. Acta Micropalaeontol Sin 13: 373–385. (In Chinese)
Shi YF (2002) Characteristics of late Quaternary monsoonal glaciation on the Tibetan Plateau andin East Asia. Quat Int 97–98: 79–91. https://doi.org/10.1016/S1040-6182(02)00053-8
Shi Y, Huang M, Ren B (1988) Introduction on Glaciers in China. Beijing Science Press: Beijing (In Chinese).
Shi Y, Zheng B, Yao T (1997) Glaciers and environments during the Last Glacial Maximum (LGM) on the Tibetan Plateau. Journal of Glaciology and Geocryology 19: 97–113. (In Chinese)
Stone JO (2000) Air pressure and cosmogenic isotope production. J Geophys Res 105(B10): 23753–23759. https://doi.org/10.1029/2000JB900181
Strasky S, Graf AA, Zhao Z, et al. (2009) Late Glacial ice advances in southeast Tibet. J Asian Earth Sci 34: 458–465. https://doi.org/10.1016/j.jseaes.2008.07.008
Svensson H (1959) Is the cross-section of a glacial valley a parabola? J Glaciol 3: 362–363. https://doi.org/10.3189/S0022143000017032
Thompson LG, Yao T, Davis ME, et al. (1997) Tropical climate instability: the last glacial cycle from a Qinghai-Tibetan ice core. Science 276: 1821–1825. https://doi.org/10.1126/science.276.5320.1821
Wang J, Cui H, Harbor JM, et al. (2015) Mid-MIS3 climate inferred from reconstructing the Dalijia Shan ice cap, northeastern Tibetan Plateau. J Quat Sci 30: 558–568. https://doi.org/10.1002/jqs.2802
Wang J, Kassab C, Harbor JM, et al. (2013) Cosmogenic nuclide constraints on late Quaternary glacial chronology on the Dalijia Shan, northeastern TP. Quat Res 79: 439–451. https://doi.org/10.1016/j.yqres.2013.01.004
Wang J, Yao P, Yu B, et al. (2018) Controls on spatial variations of glacial erosion in the Qilian Shan, northeastern Tibetan Plateau. Geomorphology 318: 128–138. https://doi.org/10.1016/j.geomorph.2018.06.004
Whipple K, Kirby E, Brocklehurst SH (1999) Geomorphic limits to climate-induced increases in topographic relief. Nature 401: 39–43. https://doi.org/10.1038/43375
Xu X (2014) Climates during Late Quaternary glacier advances: glacier-climate modeling in the Yingpu Valley, eastern Tibetan Plateau. Quat Sci Rev 101: 18–27. https://doi.org/10.1016/j.quascirev.2014.07.007
Xu X, Dong G, Pan B (2014) Modelling glacier advances and related climate conditions during the last glaciation cycle in the Kuzigun Valley, Tashkurgan catchment, on the north-west Tibetan Plateau. J Quat Sci 29: 279–288. https://doi.org/10.1002/jqs.2701
Xu X, Glasser NF (2015) Glacier sensitivity to equilibrium line altitude and reconstruction for the Last Glacial cycle: glacier modeling in the Payuwang Valley, western Nyaiqentanggulha Shan, Tibetan Plateau. Paleogeogr Paleoclimatol Paleoecol 440: 614–620. https://doi.org/10.1016/j.palaeo.2015.09.025
Xu X, Hu G, Qiao B (2013) Last glacial maximum climate based on cosmogenic Be exposure ages and glacier modelling for the head of Tashkurgan Valley, northwest Tibetan Plateau. Quat Sci Rev 80: 91–101. https://doi.org/10.1016/j.quascirev.2013.09.004
Xu X, Kleidon A, Miller L, et al. (2009) Late Quaternary glaciation in the Tianshan and implications for palaeoclimatic change: a review. Boreas 39: 215–232. https://doi.org/10.1111/j.1502-3885.2009.00118.x
Xu X, Pan B, Dong G, et al. (2017) Last Glacial climate reconstruction by exploring glacier sensitivity to climate on the southeastern slope of the western Nyaiqentanglha Shan, Tibetan Plateau. J Glaciol 63: 361–371. https://doi.org/10.1017/jog.2016.147
Xu X, Wang L, Yang J (2010) Last Glacial Maximum climate inferences from integrated reconstruction of glacier equilibrium-line altitude for the head of the Urumqi River, Tianshan Mountains. Quat Int 218: 3–12. https://doi.org/10.1016/j.quaint.2009.11.027
Xu X, Yao T, Xu B, et al. (2019) Last Glacial Maximum glacier modelling in the Quemuqu valley, southern Tibetan Plateau, and its climatic implications. Boreas. https://doi.org/10.1111/bor.12422
Xu X, Yi C (2017) Timing and configuration of the Gongga II glaciation in the Hailuogou valley, eastern Tibetan Plateau: A glacier-climate modeling method. Quat Int 444: 151–156. https://doi.org/10.1016/j.quaint.2017.01.011
Yao T, Thompson L, Yang W, et al. (2012) Different glacier status with atmospheric circulations in Tibetan Plateau and surroundings. Nat Clim Chang 2: 663–667. https://doi.org/10.1038/nclimate1580
Zhang W, Chai L, Lan S. Evans, et al. (2019) Geomorphic features of Quaternary glaciation in the Taniantaweng Mountain, on the southeastern Qinghai-Tibet Plateau. J Mt Sci 16(2): 256–274. https://doi.org/10.1007/s11629-018-4977-3
Acknowledgements
This work was supported by the National Science Foundation of China (NSFC 41771005 and 41230743). We gratefully acknowledge Yanwu Lv from the Institute of Crustal Dynamics of China (ICDC) for 10Be extraction, and PRIME Lab, Purdue University for AMS measurements.
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Paleoglacial and Paleoclimate reconstructions during the global Last Glacial Maximum in the Longriba area, eastern Tibetan Plateau
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Yang, Wl., Han, Ys., Peng, X. et al. Paleoglacial and paleoclimate reconstructions during the global Last Glacial Maximum in the Longriba area, eastern Tibetan Plateau. J. Mt. Sci. 18, 307–322 (2021). https://doi.org/10.1007/s11629-020-6238-5
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DOI: https://doi.org/10.1007/s11629-020-6238-5