Abstract
The δ18O of ice core enclosed gaseous oxygen (δ18Obub) has been widely used for climate reconstruction in polar regions. Yet, less is known about its climatic implication in the mountainous glaciers as the lack of continuous record. Here, we present a long-term, continuous δ18Obub record from the Tanggula glacier in the central Tibetan Plateau (TP). Based on comparisons of its variation with regional climate and glacier changes, we found that there was a good correlation between the variation of the δ18Obub in this alpine ice core and the accumulation and melting of this glacier. The more developed the firn layer on glacier surface, the more positive the δ18Obub. Conversely, the more intense the glacier melting, the more negative the δ18Obub. Combined with the chronology of ice core enclosed gases, the glacier variations since the late Holocene in the central TP were reconstructed. The result showed that there were four accumulation and three deficit periods of glaciers in this region. The strongest glacier accumulation period was 1610-300 B.C., which corresponds to the Neoglaciation. The most significant melting period was the last 100 years, which corresponds to the recent global warming. The Medieval Warm Period was relatively significant in the central TP. However, during the Little Ice Age, there was no significant glacier accumulation in the central TP, and even short deficit events occurred. Comparisons of the late Holocene glacier variation in the central TP with glacier and climate variations in the TP and the Northern Hemisphere showed that it was closely related to the North Atlantic Oscillation.
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References
Bazin L, Landais A, Capron E, et al. (2016) Phase relationships between orbital forcing and the composition of air trapped in Antarctic ice cores. Clim past 12(3): 729–748. https://doi.org/10.5194/cp-12-729-2016
Bazin L, Landais A, Lemieux DB, et al. (2013) An optimized multiproxy, multi-site Antarctic ice and gas orbital chronology (AICC2012): 120–800 ka. Clim past 9(4): 1715–1731. https://doi.org/10.5194/cp-9-1715-2013
Bender ML (2002) Orbital tuning chronology for the Vostok climate record supported by trapped gas composition. Earth Planet Sc Lett 204: 275–289. https://doi.org/10.1016/S0012-821X(02)00980-9
Bender M, Sowers T, Labeyrie T (1994) The Dole effect and its variations during the last 130,000 years as measured in the Vostok ice core. Global Biogeochem Cy 8(3): 363–376. https://doi.org/10.1029/94GB00724
Benson BB, Krause DJ (1984) The concentration and isotopic fractionation of oxygen dissolved in freshwater and seawater in equilibrium with the atmosphere. Limnol Oceanogr 29(3): 620–632. https://doi.org/10.4319/lo.1984.29.3.0620
Bolzan JF (1985) Ice flow at the Dome C ice divide based on a deep temperature profile. J Geophys Res-Atmos 90: 8111–8124. https://doi.org/10.1029/JD090iD05p08111
Bond G, Kromer B, Beer J, et al. (2001) Persistent solar influence on North Atlantic climate during the Holocene. Science 294(5549): 2130–2136. https://doi.org/10.1126/science.1065680
Capron E, Landais A, Chappellaz J, et al. (2010) Millennial and sub-millennial scale climatic variations recorded in polar ice cores over the last glacial period. Clim past 6: 135–183. https://doi.org/10.5194/cp-6-345-2010
Chappellaz J, Stowasser C, Blunier T, et al. (2013) High-resolution glacial and deglacial record of atmospheric methane by continuous-flow and laser spectrometer analysis along the NEEM ice core. Clim past 9: 2579–2593. https://doi.org/10.5194/cp-9-2579-2013
Chauhan OS, Vogelsang E, Basavaiah N, et al. (2010) Reconstruction of the variability of the southwest monsoon during the past 3 ka, from the continental margin of the southeastern Arabian Sea. J Quaternary Sci 25(5): 798–807. https://doi.org/10.1002/jqs.1359
Chen FH, Zhu Y, Li JJ, et al. (2001) Abrupt Holocene changes of the Asian monsoon at millennial-and centennial-scales: evidence from lake sediment document in Minqin Basin, NW China. Chinese Sci Bull 46(23): 1942. https://doi.org/10.1007/BF02901902
Craig H, Horibe Y, Sowers T (1988) Gravitational separation of gases and isotopes in polar ice caps. Science 242: 1675–1678. https://doi.org/10.1126/science.242.4886.1675
Deng XF, Zhang WJ (1992) Evolution of Quatemary glaciers and environment on the eastern side of the Geladandong Peak. J Glaciol Geocryol 14(2): 153–160. (In Chinese).
Dole M (1935) The relative atomic weight of oxygen in water and in air. J Am Chem Soc 57(12): 2731–2731. https://doi.org/10.1063/1.1749834
Dreyfus GB, Parrenin F, Lemieux-Dudon B, et al. (2007) Anomalous flow below 2700 m in the EPICA Dome C ice core detected using δ18O of atmospheric oxygen measurements. Clim past 3: 341–353. https://doi.org/10.5194/cp-3-341-2007
Eicher O, Baumgartner M, Schilt A, et al. (2016) Climatic and insolation control on the high-resolution total air content in the NGRIP ice core. Clim past 12: 1979–1993. https://doi.org/10.5194/cp-12-1979-2016
Extier T, Landais A, Bréant C, et al. (2018) On the use of δ18Oatm for ice core dating. Quaternary Sci Rev Quaternary Sci Rev 185: 244–257. https://doi.org/10.1016/j.quascirev.2018.02.008
Gao YX (1962) On some problems of Asian monsoon. In: Some questions about the East Asian Monsoon (in Chinese with English abstract). Science Press 1–49.
Hoffmann G, Cuntz M, Weber C, et al. (2004) A model of the Earth’s Dole effect. Global Biogeochem Cy 18(1): 1. https://doi.org/10.1029/2003GB002059
Holzhauser H, Magny M, Zumbuühl HJ (2005) Glacier and lake-level variations in west-central Europe over the last 3500 years. Holocene 15: 789–801. https://doi.org/10.1191/0959683605hl853ra
Hou JZ, Huang YS, Zhao JT, et al. (2016) Large Holocene summer temperature oscillations and impact on the peopling of the northeastern Tibetan Plateau. Geophys Res Lett 43: 1323–1330. https://doi.org/10.1002/2015GL067317
Hou SG, Chappellaz J, Jouzel J, et al. (2007) Summer temperature trend over the past two millennia using air content in Himalayan ice. Clim past 3(1): 89–95. https://doi.org/10.5194/cp-3-89-2007
Hou SG, Chappellaz J, Raynaud D, et al. (2013) A new Himalayan ice core CH4 record: possible hints at the preindustrial latitudinal gradient. Clim past 9: 2549–2554. https://doi.org/10.5194/cp-9-2549-2013
Hou SG, Qin DH (2002) The effect of postdepositional process on the chemical profiles of snow pits in the percolation zone. Cold Reg Sci Technol 34(2): 111–116. https://doi.org/10.1016/S0165-232X(01)00065-9
Hou SG, Qin DH, Jouzel J, et al. (2004) Age of Himalayan bottom ice cores. J Glaciol 50: 467–468. https://doi.org/10.3189/172756504781829981
Hou SG, Qin DH, Zhang DQ, et al. (2003) A 154a high-resolution ammonium record from the Rongbuk Glacier, north slope of Mt. Qomolangma (Everest), Tibet-Himal region. Atmos Environ 37(5): 721–729. https://doi.org/10.1016/S1352-2310(02)00582-4
Huang L, Li Z, Tian BS, et al. (2013) Monitoring glacier zones and snow/firn line changes in the Qinghai-Tibetan Plateau using C-band SAR imagery. Remote Sens Environ 137: 17–30. https://doi.org/10.1016/j.rse.2013.05.016
Huber C, Beyerle U, Leuenberger M, et al. (2006) Evidence for molecular size dependent gas fractionation in firn air derived from noble gases, oxygen, and nitrogen measurements. Earth Planet Sc Lett 243(1–2): 61–73. https://doi.org/10.1016/j.epsl.2005.12.036
Jones PD, Mann ME (2004) Climate over past millennia. Rev Geophys 42(2).https://doi.org/10.1029/2003RG000143
Joswiak DR, Yao TD, Wu GJ, et al. (2010) A 70-yr record of oxygen-18 variability in an ice core from the Tanggula Mountains, central Tibetan Plateau. Clim past 6: 219–227. https://doi.org/10.5194/cp-6-219-2010
Jouzel J (2013) A brief history of ice core science over the last 50 yr. Clim past 9(4). https://doi.org/10.5194/cp-9-2525-2013
Kobashi T, Goto-Azuma K, Box JE, et al. (2013) Causes of Greenland temperature variability over the past 4000 yr: implications for northern hemispheric temperature changes. Clim past 9(5): 2299–2317. https://doi.org/10.5194/cp-9-2299-2013
Lamb HH (1985) Climatic History and the Future. Methuen 835.
Landais A (1985) Reconstruction of climate and environment of the last 800 000 years from ice core-orbital and millennial variability. Quaternaire 27(3): 197–212.
Landais A, Dreyfus G, Capron E, et al. (2010) What drives the millennial and orbital variations of δ18Oatm?. Quaternary Sci Rev 29(1–2): 235–246. https://doi.org/10.1016/j.quascirev.2009.07.005
Lane GA, Dole M (1956) Fractionation of oxygen isotopes during respiration. Science, 123(3197): 574–576. https://doi.org/10.1126/science.123.3197.574
Leuenberger MC (1997) Modeling the signal transfer of sea water δ18O to the δ18O of atmospheric oxygen using a diagnostic box model for the terrestrial and marine biosphere. J Geophys Res-Oceans 102(C12): 26841–26850. https://doi.org/10.1029/97JC00160
Li JL, Xu BQ, Chappellaz J (2011) Variations of air content in Dasuopu ice core from AD 1570–1927 and implications for climate change. Quatern Int 236: 91–95. https://doi.org/10.1016/j.quaint.2010.05.026
Li SJ, Li SD (1992) Quaternary glacial and environmental changes in the region of Hoh Xil, Qinghai Province. J Glaciol Geocryol 14(4): 316–324 (In Chinese).
Liu X, Herzschuh U, Wang Y, et al. (2014) Glacier fluctuations of Muztagh Ata and temperature changes during the late Holocene in westernmost Tibetan Plateau based on glaciolacustrine sediment records. Geophys Res Lett 41: 6265–6273. https://doi.org/10.1002/2014GL060444
Liu Y, An ZS, Linderholm HW, et al. (2009) Annual temperatures during the last 2485 years in the mid-eastern Tibetan Plateau inferred from tree rings. Sci China Ser D 52(3): 348–359. https://doi.org/10.1007/s11430-009-0025-z
Loulergue L, Schilt A, Spahni R, et al. (2008) Orbital and millennial-scale features of atmospheric CH4 over the past 800,000 years, Nature 453: 383–386. https://doi.org/10.1038/nature06950
Lunak S, Sediak P (1992) Photoinitiated reactions of hydrogen peroxide in the liquid phase. J Photoch Photobio A 68(1): 1–33. https://doi.org/10.1016/1010-6030(92)85014-L
Luz B, Eugeni B (2011) The isotopic composition of atmospheric oxygen. Global Biogeochem Cy 25(3): 1. https://doi.org/10.1029/2010GB003883
Mader M, Schmidt C, Geldern VR, et al. (2017) Dissolved oxygen in water and its stable isotope effects: A review. Chem Geol 473: 10–21. https://doi.org/10.1016/j.chemgeo.2017.10.003
Malaize B, Paillard D, Jouzel J, et al. (1999) The Dole effect over the last two glacial-interglacial cycles. J Geophys Res-Atmos 104(D12): 14199–14208. https://doi.org/10.1029/1999JD900116
Mann ME, Bradley RS, Hughes MK (1999) Northern hemisphere temperatures during the past millennium: Inferences, uncertainties, and limitations. Geophys Res Lett 26(6): 759–762. https://doi.org/10.1029/1999GL900070
McConnell JR, Bales RC, Stewart RW, et al. (1998) Physically based modeling of atmosphere-to-snow-to-firn transfer of H2O2 at the South Pole. J Geophys Res 103(D9): 10561–10570. https://doi.org/10.1029/98JD00460
Murari MK, Owen LA, Dortch JM, et al. (2014) Timing and climatic drivers for glaciation across monsoon-influenced regions of the Himalayan-Tibetan orogeny. Quaternary Sci Rev 88: 159–182. https://doi.org/10.1016/j.quascirev.2014.01.013
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. Quaternary Sci Rev 24: 1391–1411. https://doi.org/10.1016/j.quascirev.2004.10.014
Parrenin F, Barnola JM, Beer J, et al. (2007) The EDC3 chronology for the EPICA Dome C ice core. Clim past 3: 485–497. https://doi.org/10.5194/cp-3-485-2007
Parrenin F, Delmotte VM, Köhler P, et al. (2013) Synchronous change of atmospheric CO2 and Antarctic temperature during the last deglacial warming. Science 339: 1060–1063. https://doi.org/10.1126/science.1226368
Petit JR, Jouzel J, Raynaud D, et al. (1999) Climate and atmospheric history of the past 420,000 years from the Vostok ice core, Antarctica. Nature 399: 429–436. https://doi.org/10.1038/20859
Petrenko VV, Severinghaus JP, Brook EJ, et al. (2006) Gas records from the West Greenland ice margin covering the Last Glacial Termination: a horizontal ice core. Quaternary Sci Rev 25: 865–875. https://doi.org/10.1016/j.quascirev.2005.09.005
Raynaud D, Lipenkov V, Lemieux B, et al. (2007) The local insolation signature of air content in Antarctic ice: A new step toward an absolute dating of ice records. Earth Planet Sc Lett 261: 337–349. https://doi.org/10.1016/j.epsl.2007.06.025
Severinghaus JP, Beaudette R, Headly MA, et al. (2009) Oxygen-18 of O2 records the impact of abrupt climate change on the terrestrial biosphere. Science 324(5933): 1431–1434. https://doi.org/10.1126/science.1169473
Severinghaus JP, Sowers T, Brook EJ, et al. (1998) Timing of abrupt climate change at the end of the Younger Dryas interval from thermally fractionated gases in polar ice. Nature 391: 141–146. https://doi.org/10.1038/34346
Shackleton NJ (2000) The 100,000-year ice-age cycle identified and found to lag temperature, carbon dioxide, and orbital eccentricity. Science 289(5486): 1897–1902. https://doi.org/10.1126/science.289.5486.1897
Shakun JD, Clark PU, He F, et al. (2012) Global warming preceded by increasing carbon dioxide concentrations during the last deglaciation. Nature 484(7392): 49. https://doi.org/10.1038/nature10915
Sowers T, Bender M, Raynaud D (1989) Elemental and isotopic composition of occluded O2 and N2 in polar ice. J Geophys Res 94(D4): 5137–5150. https://doi.org/10.1029/JD094iD04p05137
Sowers T, Bender M, Raynaud D, et al. (1991) The δ18O of atmospheric O2 from air inclusions in the Vostok ice core: timing of CO2 and ice volume changes during the penultimate deglaciation. Paleoceanography 6(6): 679–696. https://doi.org/10.1029/91PA02023
Thompson LG, Yao TD, Davis ME, et al. (2006) Holocene climate variability archived in the Puruogangri ice cap on the central Tibetan Plateau. Ann Glaciol 43: 61–69. https://doi.org/10.3189/172756406781812357
Xu BQ, Yao TD (2001) Dasuopu ice core record of atmospheric methane over the past 2000 years. Sci China Ser D 44(8): 689–699. https://doi.org/10.1007/BF02907198
Xu P, Chen YX, Li YK, et al. (2020) Late Holocene glacier fluctuations in the Bhutanese Himalaya. Global Planet Change 187: 103137. https://doi.org/10.1016/j.gloplacha.2020.103137
Xu T, Zhu LP, Lü XM, et al. (2019) Mid-to late-Holocene paleoenvironmental changes and glacier fluctuations reconstructed from the sediments of proglacial lake Buruo Co, northern Tibetan Plateau. Palaeogeogr Palaeocl 517: 74–85. https://doi.org/10.1016/j.palaeo.2018.12.023
Yang B, Braűning A, Shi YF (2003) Late Holocene temperature fluctuations on the Tibetan Plateau. Quaternary Sci Rev 21–22: 2335–2344. https://doi.org/10.1016/S0277-3791(03)00132-X
Yao TD, Thompson LG, Shi YF, et al. (1997) Climate variation since the last interglaciation recorded in the Guliya ice core. Sci China Ser D 40(6): 662–668. https://doi.org/10.1007/BF02877697
Yao TD, Thompson LG, Yang W, et al. (2012) Different glacier status with atmospheric circulations in Tibetan Plateau and surroundings. Nat Clim Change 2: 663–667. https://doi.org/10.1038/nclimate1580
Yi CL, Chen HL, Yang JQ, et al. (2008) Review of Holocene glacial chronologies based on radiocarbon dating in Tibet and its surrounding mountains. J Quaternary Sci 23: 533–543. https://doi.org/10.1002/jqs.1228
Zhang JF, Xu BQ, Turner F, et al. (2017) Long-term glacier melt fluctuations over the past 2500 yr in monsoonal High Asia revealed by radiocarbon-dated lacustrine pollen concentrates. Geology 45(4): 359–362. https://doi.org/10.1130/G38690.1
Zheng BX (1997) Glacier variation in the monsoon maritime glacial region since the last glaciation on the Qinghai-Xizang (Tibetan) Plateau. In: The Changing Face of East Asia during the Tertiary and Quaternary. Center of Asian Studies, the University of Hong Kong 103–112.
Zheng W, Yao TD, Joswiak DR, et al. (2010) Major ions composition records from a shallow ice core on Mt. Tanggula in the central Qinghai-Tibetan Plateau. Atmos Res 97(1–2): 70–79. https://doi.org/10.1016/j.atmosres.2010.03.008
Zhu LP, Lü XM, Wang JB, et al. (2015) Climate change on the Tibetan Plateau in response to shifting atmospheric circulation since the LGM. Sci Rep 5: 13318. https://doi.org/10.1038/srep13318
Acknowledgments
This study was supported by the National Natural Science Foundation of China (Grant No. 42271312, 41201058), the Strategic Priority Research Program of Chinese Academy of Sciences (Grant No. XDA20070102), the National Key R&D Program of China (Grant No. 2018YFB1307504) and the Science and Technology Program of Tibet Autonomous Region of China (Grant No. XZ202101ZD0014G). We thank all of the field workers for the hard work of ice core collection on the glacier. We also thank Dr. Chenglong ZHANG from Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences for the help of ice core pretreatments in the cold room. Thanks are also given to Dr. Dongmei QU and Dr. Shaopeng GAO of the Institute of Tibetan Plateau Research Chinese Academy of Sciences for their help in the determination of the ice core air bubbles. Thanks also go to two anonymous reviewers and editor whose comments and suggestions have helped greatly improve the manuscript.
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Li, Jl., Xu, Bq., Wang, Nl. et al. Late Holocene glacier variations indicated by the δ18O of ice core enclosed gaseous oxygen in the central Tibetan Plateau. J. Mt. Sci. 20, 325–337 (2023). https://doi.org/10.1007/s11629-022-7705-y
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DOI: https://doi.org/10.1007/s11629-022-7705-y