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Glacial events during the last glacial termination in the Pagele valley, Qiongmu Gangri peak, southern Tibetan Plateau, and their links to oceanic and atmospheric circulation

Published online by Cambridge University Press:  12 March 2020

Xiangke Xu Open the ORCID record for Xiangke Xu [Opens in a new window] ,
Tandong Yao ,
Baiqing Xu ,
Chaolu Yi ,
Yong Sun ,
Xuezhen Zeng ,
Guocheng Dong  and
Baolin Pan
Xiangke Xu*
Affiliation:
Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research, CAS, Beijing100101, China CAS Center for Excellence in Tibetan Plateau Earth Science, Beijing100101, China
Tandong Yao
Affiliation:
Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research, CAS, Beijing100101, China CAS Center for Excellence in Tibetan Plateau Earth Science, Beijing100101, China
Baiqing Xu
Affiliation:
Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research, CAS, Beijing100101, China CAS Center for Excellence in Tibetan Plateau Earth Science, Beijing100101, China
Chaolu Yi
Affiliation:
Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research, CAS, Beijing100101, China CAS Center for Excellence in Tibetan Plateau Earth Science, Beijing100101, China
Yong Sun
Affiliation:
Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research, CAS, Beijing100101, China University of Chinese Academy of Sciences, Beijing100049, China
Xuezhen Zeng
Affiliation:
Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research, CAS, Beijing100101, China University of Chinese Academy of Sciences, Beijing100049, China
Guocheng Dong
Affiliation:
State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710061, China
Baolin Pan
Affiliation:
College of Resources, Environment and Tourism, Capital Normal University, Beijing100048, China
*
*Corresponding author at: Key Laboratory of Tibetan Environment Changes and Land Surface Processes, Institute of Tibetan Plateau Research, CAS Center for Excellence in Tibetan Plateau Earth Science, Beijing100101, China. E-mail address: xkxu@itpcas.ac.cn (X. Xu).
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Abstract

During the last glacial termination, a warming trend was generally interrupted by rapid millennium-scale cold reversals, such as the Greenland (Isotope) Stadial 1 (GS-1) and GS-2a events. To understand how glaciers on the Tibetan Plateau (TP) responded to these rapid climate events, this study constrained the timing and extent of three glacial events during the late-glacial period. Specifically, using a cosmogenic 10Be exposure dating method, we dated three prominent glacial moraines (PM1, PM2, PM3) back to 15,850 ± 980, 14,140 ± 880, and 12,430 ± 790 yr in the Pagele valley, southern TP, corresponding to GS-2a, Greenland Interstadial 1 (GI-1), and GS-1, respectively. By simulating glacial extents forced by different climate scenarios, the study constrained the temperature decreases relative to present to be 2.6°C–2.9°C, ~1.6°C, and 1.4°C–1.5°C during the GS-2a, GI-1, and GS-1 periods in the region, with precipitation values of 60%–80%, ~100%, and 80%–90% of present value, respectively. Considering information from oceanic and atmospheric circulation, the study suggested that on the TP, the glacial events during the last glacial termination were well connected with the millennium-scale climate events in the North Atlantic region through the westerlies, while the Indian summer monsoon played a positive role in sustaining the glaciers under the warming climate trend.

Keywords

Last glacial terminationGlacial eventCosmogenic 10Be datingMillennium-scale climate eventsPagele valley
Type
Research Article
Information
Quaternary Research , Volume 95 , May 2020 , pp. 129 - 141
Copyright
Copyright © University of Washington. Published by Cambridge University Press, 2020

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References

REFERENCES

Balco, G., Stone, J.O., Lifton, N.A., Dunai, T.J., 2008. A complete and easily accessible means of calculating surface exposure ages or erosion rates from 10Be and 26Al measurements. Quaternary Geochronology 8, 174–195.CrossRefGoogle Scholar
Banakar, V.K., Baidya, S., Piotrowski, A.M., Shankar, D., 2017. Indian summer monsoon forcing on the deglacial polar cold reversals. Journal of Earth System Science 126, 87.CrossRefGoogle Scholar
Barnett, T.P., Dümenil, L., Schlese, U., Roeckner, E., 1988. The effect of Eurasian snow cover on global climate. Science 239, 504–507.CrossRefGoogle ScholarPubMed
Benn, D.I., Owen, L.A., 1998. The role of the Indian summer monsoon and the mid-latitude westerlies in Himalayan glaciation: review and speculative discussion. Journal of the Geological Society 155, 353–363.CrossRefGoogle Scholar
Berger, A.M., Loutre, F., 1991. Insolation values for the climate of the last 10 million years. Quaternary Science Reviews 10, 297–314.CrossRefGoogle Scholar
Björck, S., Walker, M.J.C., Cwynar, L.C., Johnsen, S., Knudsen, K.-L., Lowe, J.J., Wohlfarth, B., INTIMATE Members, 1998. An event stratigraphy for the Last Termination in the North Atlantic region based on the Greenland ice-core record: a proposal by the INTIMATE group. Journal of Quaternary Science 13, 283–292.3.0.CO;2-A>CrossRefGoogle Scholar
Blomdin, R., Stroeven, A. P., Harbor, J. M., Lifton, N. A., Heyman, J., Gribenski, N., Petrakov, D. A., et al. , 2016. Evaluating the timing of former glacier expansions in the Tian Shan: A key step towards robust spatial correlations. Quaternary Science Reviews 153, 78–96.CrossRefGoogle Scholar
Broecker, W.S., van Donk, J., 1970. Insolation changes, ice volume, and the 18O record in deep-sea cores. Reviews of Geophysics 8, 169–198.CrossRefGoogle Scholar
Cai, Y., Fung, I.Y., Edwards, R.L., An, Z., Cheng, H., Lee, J.-E., Tan, L., et al. ., 2015. Variability of stalagmite-inferred Indian monsoon precipitation over the past 252,000 y. Proceedings of the National Academy of Sciences USA 112, 2954–2959.CrossRefGoogle ScholarPubMed
Chevalier, M.-L., Hilley, G., Tapponnier, P., Van Der Weord, J., Liu-Zeng, J., Finkel, R.C., Ryerson, F.J., Li, H., Liu, X., 2011. Constrains on the late Quaternary glaciations in Tibet from cosmogenic exposure ages of moraine surface. Quaternary Science Reviews 30, 528–554.CrossRefGoogle Scholar
Chiang, J.C.H., Bitz, C.M., 2005. Influence of high latitude ice cover on the marine Intertropical Convergence Zone. Climate Dynamics 25, 477–496.CrossRefGoogle Scholar
Cuffey, K.M., Paterson, W.S.B., 2010. The Physics of Glaciers. 4th ed.Elsevier, Boston.Google Scholar
Dayem, K.E., Molnar, P., Battisti, D.S., Roe, G.H., 2010. Lessons learned from oxygen isotopes in modern precipitation applied to interpretation of speleothem records of paleoclimate from eastern Asia. Earth and Planetary Science Letters 295, 219–230.CrossRefGoogle Scholar
Denton, G.H., Alley, R.B., Comer, G.C., Broecker, W.S., 2005. The role of seasonality in abrupt climate change. Quaternary Science Reviews 24, 1159–1182.CrossRefGoogle Scholar
Denton, G.H., Anderson, R.F., Toggweiler, J.R., Edwards, R.L., Schaefer, J.M., Putnam, A.E., 2010. The last glacial termination. Science 328, 1652–1656.CrossRefGoogle ScholarPubMed
Dong, G., Xu, X., Zhou, W., Fu, Y., Zhang, L., Li, M., 2017. Cosmogenic 10Be surface exposure dating and glacier reconstruction for the Last Glacial Maximum in the Quemuqu Valley, western Nyainqentanglha Mountains, south Tibet. Journal of Quaternary Science 32, 639–652.CrossRefGoogle Scholar
Dortch, J.M., Owen, L.A., Caffee, M.W., 2013. Timing and climatic drivers for glaciation across semi-arid western Himalayan-Tibetan orogen. Quaternary Science Reviews 78, 188–208.CrossRefGoogle Scholar
Dortch, J.W., Owen, L.A., Haneberg, W.C., Caffee, M.W., Dietsch, C., Kamp, U., 2009. Nature and timing of large landslides in the Himalaya and Transhimalaya of northern India. Quaternary Science Reviews 28, 1037–1054.CrossRefGoogle Scholar
Farinotti, D., Huss, M., Fürst, J.J., Landmann, J., Machguth, H., Maussion, F., Pandit, A., 2019. A consensus estimate for the ice thickness distribution of all glaciers on Earth. Nature Geoscience 12, 168–173.CrossRefGoogle Scholar
Heyman, J., 2014. Paleoglaciation of the Tibetan Plateau and surrounding mountains based on exposure ages and ELA depression estimates. Quaternary Science Reviews 91, 30–41.CrossRefGoogle Scholar
Heyman, J., Stroeven, A.P., Harbor, J., Caffee, M.W., 2011. Too young or too old: evaluating cosmogenic exposure dating based on an analysis of compiled boulder exposure ages. Earth and Planetary Science Letters 302, 71–80.CrossRefGoogle Scholar
Kathayat, G., Cheng, H., Sinha, A., Spötl, C., Edwards, R.L., Zhang, H., Li, X., et al. ., 2016. Indian monsoon variability on millennial-orbital timescales. Scientific Reports 6, 24374.CrossRefGoogle ScholarPubMed
Kohl, C.P., Nishiizumi, K., 1992. Chemical isolation of quartz for measurement of in situ produced cosmogenic nuclides. Geochimica et Cosmochimica Acta 56, 3583–3587.CrossRefGoogle Scholar
Laabs, B.J.C., Plummer, M.A., Mickelson, D.M., 2006. Climate during the last glacial maximum in the Wasatch and southern Uinta Mountains inferred from glacier modelling. Geomorphology 75, 300–317.CrossRefGoogle Scholar
Lal, D., 1991. Cosmic ray labeling of erosion surfaces: in situ nuclide production rates and erosion models. Earth and Planetary Science Letters 104, 429–439.CrossRefGoogle Scholar
Lana, B., Nakawo, M., Fukushima, Y., Ageta, Y., 1997. Application of a conceptual precipitation-runoff model (HYCYMODEL) in a debris-covered glacierized basin in the Langtang Valley, Nepal Himalaya. Annals of Glaciology 25, 226–231.Google Scholar
Li, Y.K., 2013. Determining topographic shielding from digital elevation models for cosmogenic nuclide analysis: a GIS approach and field validation. Journal of Mountain Science 10, 355–362.CrossRefGoogle Scholar
Lifton, N.A., Sato, T., Dunai, T.J., 2014. Scaling in situ cosmogenic nuclide production rates using analytical approximations to atmospheric cosmic-ray fluxes. Earth and Planetary Science Letters 386, 149–160.CrossRefGoogle Scholar
Liu, Z., Otto-Bliesner, B.L., He, F., Brady, E.C., Tomas, R., Clark, P.U., Carlson, A.E., et al. , 2009. Transient simulation of last deglaciation with a new mechanism for Bølling-Allerød warming. Science 325, 310–313.CrossRefGoogle ScholarPubMed
Mihalcea, C., Mayer, C., Diolaiuti, G., D'Agata, C., Smiraglia, C., Lambrecht, A., Vuiller-moz, E., Tartari, G., 2008. Spatial distribution of debris thickness and melting from remote-sensing and meteorological data, at debris-covered Baltoro glacier, Karakoram, Pakistan. Annals of Glaciology 48, 49–57.CrossRefGoogle Scholar
Molnar, P., England, P., 1990. Late Cenozoic uplift of mountain-ranges and global climate change: chicken or egg? Nature 346, 29–34.CrossRefGoogle Scholar
Murari, M.K., Owen, L.A., Dortch, J.M., Caffee, M.W., Dietsch, C., Fuchs, M., Haneberg, W.C., Sharma, M.C., Townsend-Small, A., 2014. Timing and climatic drivers for glaciation across monsoon-influenced regions of the Himalayan-Tibetan orogeny. Quaternary Science Reviews 88, 159–182.CrossRefGoogle Scholar
Naik, S.S., Basak, C., Goldstein, S.L., Naidu, P.D., Naik, S.N., 2019. A 16-kyr record of ocean circulation and monsoon intensification from the central Bay of Bengal. Geochemistry, Geophysics, Geosystems 20, 872–882.CrossRefGoogle Scholar
Naughton, F., Sánchez Goñi, M.F., Kageyama, M., Bard, E., Duprat, J., Cortijo, E., Desprat, S., et al. , 2009. Wet to dry climatic trend in north-western Iberia within Heinrich events. Earth and Planetary Science Letters 284, 329–342.CrossRefGoogle Scholar
Nicholson, L., Benn, D., 2006. Calculating ice melt beneath a debris layer using meteorological data. Journal of Glaciology 52, 463–470.CrossRefGoogle Scholar
Nishiizumi, K., Imamura, M., Caffee, M.W., Southon, J.R., Finkel, R.C., McAninch, J., 2007. Absolute calibration of 10Be AMS standards. Nuclear Instruments and Methods in Physics Research Section B 258, 403–413.CrossRefGoogle Scholar
Owen, L.A., Caffee, M.W., Finkel, R.C., Seong, Y.B., 2008. Quaternary glaciation of the Himalayan-Tibetan orogen. Journal of Quaternary Science 23, 513–531.CrossRefGoogle Scholar
Owen, L.A., Dortch, J.M., 2014. Nature and timing of Quaternary glaciation in the Himalayan-Tibetan orogeny. Quaternary Science Reviews 88, 14–54.CrossRefGoogle Scholar
Owen, L.A., Finkel, R.C., Barnard, P.L., Haizhou, M., Asahi, K., Caffee, M.W., Derbyshire, E., 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 Science Reviews 24, 1391–1411.CrossRefGoogle Scholar
Peirce, B., 1852. Criterion for the rejection of doubtful observations. Astronomical Journal 2, 161–163.CrossRefGoogle Scholar
Plummer, M.A., 2002. Paleoclimate Conditions during the Last Deglaciation Inferred from Combined Analysis of Pluvial and Glacial Records. Ph.D. thesis, New Mexico Institute of Mining and Technology, Socorro, NM. pp. 346.Google Scholar
Plummer, M.A., Phillips, F.M., 2003. A 2-D numerical model of snow/ice energy balance and ice flow for paleoclimatic interpretation of glacial geomorphic features. Quaternary Science Reviews 22, 1389–1406.CrossRefGoogle Scholar
Prell, W.L., Kutzbach, J.E. 1992. Sensitivity of the Indian monsoon to forcing parameters and implications for its evolution. Nature 360, 647–652.CrossRefGoogle Scholar
Pu, J., Yao, T., Duan, K., 2003. An observation on surface ablation on the Yangbark glacier in the Muztag Ata, China. [In Chinese with English abstract.] Journal of Glaciology and Geocryology 25, 680–684.Google Scholar
Rasmussen, S.O., Andersen, K.K., Svensson, A.M., Steffensen, J.P., Vinther, B.M., Clausen, H.B., Siggaard-Andersen, M.-L., et al. ., 2006. A new Greenland ice core chronology for the last glacial termination. Journal of Geophysical Research 111, D06102.CrossRefGoogle Scholar
Raymo, M.E., Ruddiman, W.F. 1992. Tectonic forcing of late Cenozoic climate. Nature 359, 117–124.CrossRefGoogle Scholar
Rehfeld, K., Münch, T., Ho, S.L., Laepple, T., 2018. Global patterns of declining temperature variability from the Last Glacial Maximum to the Holocene. Nature 554, 356–359.CrossRefGoogle ScholarPubMed
Ressen, H., Isarin, R.F.B., 2001. The two major warming phases of the last deglaciation at ~14.7 and ~11.5 ka cal BP in Europe: climate reconstructions and AGCM experiments. Global and Planetary Change 30, 117–153.CrossRefGoogle Scholar
Schaefer, J.M., Denton, G.H., Kaplan, M., Putnam, A., Finkel, R.C., Barrell, D.J.A., Andersen, B.G., et al. , 2009. High-frequency Holocene glacier fluctuations in New Zealand differ from the northern signature. Science 324, 622–625.CrossRefGoogle ScholarPubMed
Sinha, A., Cannariato, K.G., Stott, L.D., Li, H., You, C., Chen, H., Edwards, R.L., Singh, I.B., 2005. Variability of Southwest Indian summer monsoon precipitation during the Bølling-Allerød. Geology 33, 813–816.CrossRefGoogle Scholar
Stone, J.O., 2000. Air pressure and cosmogenic isotope production. Journal of Geophysical Research 105, 23753–23759.CrossRefGoogle Scholar
Sun, W., Zhang, E., Shulmeister, J., Bird, M.I., Chang, J., Shen, J., 2019. Abrupt changes in Indian summer monsoon strength during the last deglaciation and early Holocene based on stable isotope evidence from Lake Chenghai, southwest China. Quaternary Science Reviews 218, 1–9.CrossRefGoogle Scholar
Thackray, G.D., Owen, L.A., Yi, C.L., 2008. Timing and nature of late Quaternary mountain glaciation. Journal of Quaternary Science 23, 503–508.CrossRefGoogle Scholar
Thompson, L.G., Yao, T., Davis, M.E., Henderson, K.A., Mosley-Thompson, E., Lin, P., Beer, J., Synal, H., Cole-Dai, J., Bolzan, J.F., 1997. Tropical climate instability: the Last Glacial Cycle from a Qinghai-Tibetan ice core. Science 276, 1821–1825.CrossRefGoogle Scholar
Tierney, J.E., Pausata, F.S.R., de Menocal, P., 2016. Deglacial Indian monsoon failure and North Atlantic stadials linked by Indian Ocean surface. Nature Geoscience 9, 46–50.CrossRefGoogle Scholar
Xu, X., Dong, G., Pan, B., Hu, G., Bi, W., Liu, J., Yi, C., 2017b. Late Glacial glacier-climate modeling in two valleys on the eastern slope of Samdainkangsang Peak, Nyaiqentanggulha Mountains. Science China Earth Sciences 60, 135–162.CrossRefGoogle Scholar
Xu, X., Hu, G., Qiao, B., 2013. Last Glacial Maximum climate based on cosmogenic 10Be exposure ages and glacier modeling for the head of Tashkurgan Valley, northwest Tibetan Plateau. Quaternary Science Reviews 80, 91–101.CrossRefGoogle Scholar
Xu, X., Pan, B., Dong, G., Yi, C., Glasser, N.F., 2017a. Last Glacial climate reconstruction by exploring glacier sensitivity to climate on the southeastern slope of the western Nyaiqentanglha Shan, Tibetan Plateau. Journal of Glaciology 63, 361–371.CrossRefGoogle Scholar
Yang, Y., Yuan, D.X., Cheng, H., Zhang, M.L., Qin, J.M., Lin, Y.S., Zhu, X.Y., Edwards, R.L., 2010. Precise dating of abrupt shifts in the Asian Monsoon during the last deglaciation based on stalagmite data from Yamen Cave, Guizhou Province, China. Science China Earth Sciences 53, 633–641.CrossRefGoogle Scholar
Yao, T.D., Masson-Delmotte, V., Gao, J., Yu, W., Yang, X., Risi, C., Sturm, C., et al. ., 2013. A review of climatic controls on δ18O in precipitation over the Tibetan Plateau: observations and simulations. Reviews of Geophysics 51, 525–548.CrossRefGoogle Scholar
Young, N.E., Briner, J.P., Schaefer, J., Zimmerman, S., Finkel, R.C., 2019. Early Younger Dryas glacier culmination in southern Alaska: implications for North Atlantic climate change during the last deglaciation. Geology 47, 550–554.CrossRefGoogle Scholar
Yuan, D., Cheng, H., Edwards, R.L., Dykoski, C.A., Kelly, M.J., Zhang, M., Qing, J., et al. , 2004. Timing, duration, and transitions of the last interglacial Asian monsoon. Science 304, 575–578.CrossRefGoogle ScholarPubMed
Zech, R., Zech, M., Kubik, P.W., Kharki, K., Zech, W., 2009. Deglaciation and landscape history around Annapurna, Nepal, based on 10Be surface exposure dating. Quaternary Science Reviews 28, 1106–1118.CrossRefGoogle Scholar
Zhang, E., Chang, J., Shulmeister, J., Langdon, P., Sun, W., Cao, Y., Yang, X., Shen, J., 2019. Summer temperature fluctuations in Southwestern China during the end of the LGM and the last deglaciation. Earth and Planetary Science Letters 509, 78–87CrossRefGoogle Scholar
Zhang, Y., Li, B., Zheng, D., 2002. A discussion on the boundary and area of the Tibetan Plateau in China. Geographical Research 21, 1–8.Google Scholar
Zheng, B., Xu, Q., Shen, Y., 2002. The relationship between climate change and Quaternary glacial cycles on the Qinghai-Tibetan Plateau: review and speculation. Quaternary International 97/98, 93–101.CrossRefGoogle Scholar
Zhu, L., Lü, X., Wang, J., Peng, P., Kasper, P., Daut, G., Haberzettl, T., et al. ., 2015. Climate change on the Tibetan Plateau in response to shifting atmospheric circulation since the LGM. Scientific Reports 5, 13318.CrossRefGoogle ScholarPubMed
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