Geomorphic features of Quaternary glaciation in the Taniantaweng Mountain, on the southeastern Qinghai-Tibet Plateau
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摘要
We present geomorphological evidence for multiple glacial fluctuations during the Quaternary in the Taniantaweng Mountain, which is situated at the transition zone of the southeastern Qinghai-Tibet Plateau and the Yunnan-Guizhou Plateau. To reconstruct the history of glacial evolution during the Quaternary Glaciation, we present a ~13000 km~2 geomorphologic map(1:440,000) for the Quaternary glaciations, as well as three electron spin resonance(ESR) ages and three optically stimulated luminescence(OSL) ages from the landforms. By integrating these with ages from previous studies, four major glacial advances are identified during marine oxygen isotope stages(MIS) 6, 3, 2 and 1. This glacial chronology is in reasonable agreement with existing glacial chronologies from other parts of the Hengduan Mountains and surrounding mountains. Glaciers had extended to the Yuqu River during the glacial maximum advance(MIS 6), but became successively more restricted from MIS 3 to MIS 1. The glacial distribution show that precipitation brought by the south Asian monsoon might play a primary role in driving glacial advances during the last glacial period in the southeastern Qinghai-Tibet Plateau.
We present geomorphological evidence for multiple glacial fluctuations during the Quaternary in the Taniantaweng Mountain, which is situated at the transition zone of the southeastern Qinghai-Tibet Plateau and the Yunnan-Guizhou Plateau. To reconstruct the history of glacial evolution during the Quaternary Glaciation, we present a ~13000 km~2 geomorphologic map(1:440,000) for the Quaternary glaciations, as well as three electron spin resonance(ESR) ages and three optically stimulated luminescence(OSL) ages from the landforms. By integrating these with ages from previous studies, four major glacial advances are identified during marine oxygen isotope stages(MIS) 6, 3, 2 and 1. This glacial chronology is in reasonable agreement with existing glacial chronologies from other parts of the Hengduan Mountains and surrounding mountains. Glaciers had extended to the Yuqu River during the glacial maximum advance(MIS 6), but became successively more restricted from MIS 3 to MIS 1. The glacial distribution show that precipitation brought by the south Asian monsoon might play a primary role in driving glacial advances during the last glacial period in the southeastern Qinghai-Tibet Plateau.
We present geomorphological evidence for multiple glacial fluctuations during the Quaternary in the Taniantaweng Mountain, which is situated at the transition zone of the southeastern Qinghai-Tibet Plateau and the Yunnan-Guizhou Plateau. To reconstruct the history of glacial evolution during the Quaternary Glaciation, we present a ~13000 km~2 geomorphologic map(1:440,000) for the Quaternary glaciations, as well as three electron spin resonance(ESR) ages and three optically stimulated luminescence(OSL) ages from the landforms. By integrating these with ages from previous studies, four major glacial advances are identified during marine oxygen isotope stages(MIS) 6, 3, 2 and 1. This glacial chronology is in reasonable agreement with existing glacial chronologies from other parts of the Hengduan Mountains and surrounding mountains. Glaciers had extended to the Yuqu River during the glacial maximum advance(MIS 6), but became successively more restricted from MIS 3 to MIS 1. The glacial distribution show that precipitation brought by the south Asian monsoon might play a primary role in driving glacial advances during the last glacial period in the southeastern Qinghai-Tibet Plateau.
引文
Aitken MJ(1998)An introduction to optical dating.Oxford:Oxford University Press.
Benn DI,Owen LA(1998)The role of the Indian summer monsoon and the mid-latitude westerlies in Himalayan glaciation:Review and speculative discussion.Journal of the Geological Society155(2):353-363.https://doi.org/10.1144/gsjgs.155.2.0353
Benn DI,Owen LA(2002)Himalayan glacial sedimentary environments:a framework for reconstructing and dating the former extent of glaciers in high mountains.Quaternary International 97-98:3-25.https://doi.org/10.1016/S1040-6182(02)00048-4
Bi WL,Yi CL(2016)Review of ESR dating technique in Quaternary glacial chronology.Journal of Glaciology and Geocryology 38(5):1292-1299(In Chinese).
Cui ZJ,Chen YX,Zhang W,et al.(2011)Research History,glacial chronology and origins of Quaternary glaciations in China.Quaternary Sciences 31(5):749-764(In Chinese).https://doi.org/10.3969/j.issn.1001-7410.2011.05.01
Dortch JM,Owen LA,Caffee MW(2013)Timing and climatic drivers for glaciation across semi-arid western Himalayan-Tibetan orogen.Quaternary Science Reviews 78:188-208.https://doi.org/10.1016/j.quascirev.2013.07.025
Fu P,Heyman J,H?ttestrand C,et al.(2012)Glacial geomorphology of the Shaluli Shan area,southeastern Tibetan Plateau.Journal of Maps 8(1):48-55.https://doi.org/10.1080/17445647.2012.668762
Fu P,Stroeven AP,Harbor JM,et al.(2014)Paleoglaciation of Shaluli Shan,southeastern Tibetan Plateau.Quaternary Science Reviews 64(433):121-135.https://doi.org/10.1016/j.quascirev.2012.12.009
Fuchs M,Owen LA(2008)Luminescence dating of glacial and associated sediments:review,recommendations and future directions.Boreas 37:636-659.https://doi.org/10.1111/j.1502-3885.2008.00052.x
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Lehmkuhl F,Owen LA(2005)Late Quaternary glaciation of Tibet and the bordering mountains:a review.Boreas 34(2):87-100.https://doi.org/10.1111/j.1502-3885.2005.tb01008.x
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Liu BB,Zhang W,Cui ZJ,et al.(2015)Climate-tectonics coupling effect on Late Quaternary Glaciation in the Mayaxue Shan,Gansu Province.Journal of Glaciology and Geocryology 37(3):701-710.(In Chinese).https://doi.org/10.7522/j.issn.1000-0240.2015.0079
Liu CR,Yin GM,Gao L,et al.(2010)ESR dating of Pleistocene archaeological localities of the Nihewan Basin,North ChinaPreliminary results.Quaternary Geochronology 5(2-3):385-390.https://doi.org/10.1016/j.quageo.2009.05.006
Liu GN,Li YK,Chen YX,et al.(2011)Glacial landform chronology and environment reconstruction of Peiku Gangri.Himalayas.Journal of Glaciology and Geocryology 33:959-970.(In Chinese)
Liu CR,Yin GM,Gao L,et al.(2011)Research advances in ESRgeochronology of Quaternary deposits.Seismology and Geology2(33):490-498.(In Chinese).https://doi.org/10.3969/j.issn.0253-4967.2011.02.022
Liu CR,Yin GM,Grün R(2013)Research Progress of the Resetting Features of Quartz ESR Signal.Advances in Earth Science 28(1):24-30.(In Chinese).https://doi.org/10.11867/j.issn.1001-8166.2013.01.0024
Liu CR,Yin GM,Han F,et al.(2016)ESR dating methodology and its application in dating Quaternary terrestrial sediments.Quaternary Sciences 36(5):1236-1245.(In Chinese).https://doi.org/10.11928/j.issn.1001-7410.2016.05.18
Lisiecki,LE,Raymo,ME(2005)A Pliocene-Pleistocene stack of 57globally distributed benthicδ18O records.Paleoceanography 20(1):1-17.https://doi.org/10.1029/2004PA001071
Murray AS,Wintle AG(2000)Luminescence dating of quartz using an improved single-aliquot regenerative-dose protocol.Radiation Measurements 32(1):57-73.https://doi.org/10.1016/S1350-4487(99)00253-X
Norton KP,Abbuhl LM,Schlunegger F(2010)Glacial conditioning as an erosional driving force in the Central Alps.Geology 38(7):655-658.https://doi.org/10.1130/G31102.1
Ou XJ,Lai ZP,Zhou SZ,et al.(2014)Timing of glacier fluctuations and trigger mechanisms in eastern Qinghai-Tibetan Plateau during the late Quaternary.Quaternary Research 81(3):464-475.https://doi.org/10.1016/j.yqres.2013.09.007
Owen LA,Robinson R,Benn DI,et al.(2009)Quaternary glaciation of Mount Everest.Quaternary Science Reviews 28(15):1412-1433.https://doi.org/10.1016/j.quascirev.2009.02.010
Owen LA,Dortch JM(2014)Nature and timing of Quaternary glaciation in the Himalayan-Tibetan orogen.Quaternary Science Reviews 88(88):14-54.https://doi.org/10.1016/j.quascirev.2013.11.016
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 Science Reviews 24(12):1391-1411.https://doi.org/10.1016/j.quascirev.2004.10.014
Owen LA,Finkel RC,Haizhou M,et al.(2003)Timing and style of Late Quaternary glaciation in northeastern Tibet.Geological Society of America Bulletin 115(11):1356-1364.https://doi.org/10.1130/B25314.1
Prescott JR,Hutton JT(1994)Cosmic-ray contributions to doserates for luminescence and ESR dating-large depths and longterm time variations.Radiation Measurements 23(2-3):497-500.https://doi.org/10.1016/1350-4487(94)90086-8
Richards B(2000)Luminescence dating of Quaternary sediments in the Himalaya and High Asia:A practical guide to its use and limitations for constraining the timing of glaciation.Quaternary International 65-66:49-61.https://doi.org/10.1016/S1040-6182(99)00036-1
Rink WJ,Bartoll J,Schwarcz HP,et al.(2007)Testing the reliability of ESR dating of optically exposed buried quartz sediments.Radiation Measurements 42(10):1618-1626.https://doi.org/10.1016/j.radmeas.2007.09.005
Shi YF,Huang MH,Ren BH(1988)An introduction to the glaciers in China contents.Science Press,Beijing(In Chinese).
Shi YF,Liu SY(2000)Estimation on the response of glaciers in China to the global warming in the 21st century.Chinese Science Bulletin 45(7):668-672.https://doi.org/10.1007/BF02886048
Shi YF(2002)Characteristics of late Quaternary monsoonal glaciation on the Tibetan Plateau and in East Asia.Quaternary International 97(2):79-91.https://doi.org/10.1016/S1040-6182(02)00053-8
Shi YF,Yao TD(2002)MIS 3b(54-44 ka BP)cold period and glacial advance in middle and low latitudes.Journal of Glaciolgy and Geocryology 24(1):1-9.(In Chinese).
Su Z,Pu JC(1996)Development conditions,Number and morphological characteristics of glaciers in the Hengduan Mountains region.In:Li JJ,Su,Z 1996.Glaciers in the Hengduan Mountains.Science Press,Beijing,pp.1-21(In Chinese).
Tanaka K,Hataya R,Spooner NA,et al.(1997)Dating of marine terrace sediments by ESR,TL and OSL methods and their applicabilities.Quaternary Science Reviews 16(3-5):257-264.https://doi.org/10.1016/S0277-3791(96)00092-3
Tang LY,Shen CM,Liu KB,et al.(2004)Climatic changes since the Last Glacial Maximum in the southeastern Tibetan Plateau:pollen evidence.Science in China 34(34):434-442.(in Chinese)https://doi.org/10.3969/j.issn.1674-7240.2004.05.006
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Benn DI,Owen LA(2002)Himalayan glacial sedimentary environments:a framework for reconstructing and dating the former extent of glaciers in high mountains.Quaternary International 97-98:3-25.https://doi.org/10.1016/S1040-6182(02)00048-4
Bi WL,Yi CL(2016)Review of ESR dating technique in Quaternary glacial chronology.Journal of Glaciology and Geocryology 38(5):1292-1299(In Chinese).
Cui ZJ,Chen YX,Zhang W,et al.(2011)Research History,glacial chronology and origins of Quaternary glaciations in China.Quaternary Sciences 31(5):749-764(In Chinese).https://doi.org/10.3969/j.issn.1001-7410.2011.05.01
Dortch JM,Owen LA,Caffee MW(2013)Timing and climatic drivers for glaciation across semi-arid western Himalayan-Tibetan orogen.Quaternary Science Reviews 78:188-208.https://doi.org/10.1016/j.quascirev.2013.07.025
Fu P,Heyman J,H?ttestrand C,et al.(2012)Glacial geomorphology of the Shaluli Shan area,southeastern Tibetan Plateau.Journal of Maps 8(1):48-55.https://doi.org/10.1080/17445647.2012.668762
Fu P,Stroeven AP,Harbor JM,et al.(2014)Paleoglaciation of Shaluli Shan,southeastern Tibetan Plateau.Quaternary Science Reviews 64(433):121-135.https://doi.org/10.1016/j.quascirev.2012.12.009
Fuchs M,Owen LA(2008)Luminescence dating of glacial and associated sediments:review,recommendations and future directions.Boreas 37:636-659.https://doi.org/10.1111/j.1502-3885.2008.00052.x
Gao L,Ying GM,Liu CR,et al.(2009)Nature sunlight bleaching of Ti center ESR signal in quartz.He Jishu/Nuclear Techniques32(2):116-118.https://doi.org/10.3321/j.issn:0253-3219.2009.02.010
Lai ZP(2010)Chronology and the upper dating limit for loess samples from Luochuan section in Chinese Loess Plateau using quartz OSL SAR protocol.Journal of Asian Earth Sciences 37:176-185.https://doi.org/10.1016/j.jseaes.2009.08.003
Lehmkuhl F,Owen LA(2005)Late Quaternary glaciation of Tibet and the bordering mountains:a review.Boreas 34(2):87-100.https://doi.org/10.1111/j.1502-3885.2005.tb01008.x
Li JJ(1991)The environmental effects of the uplift of the QinghaiXizang Plateau.Quaternary Science Reviews 10(6):479-483.https://doi.org/10.1016/0277-3791(91)90041-R
Li JJ,Zheng BX,Yang XJ,et al.(1986)The series of the scientific expedition to Qinghai-Xizang Plateau.Science Press,Beijing(In Chinese).
Lindholm MS,Heyman J(2015)Glacial geomorphology of the Maidika region,Tibetan Plateau.Journal of Maps 12:1-7.https://doi.org/10.1080/17445647.2015.1078182
Liu BB,Zhang W,Cui ZJ,et al.(2015)Climate-tectonics coupling effect on Late Quaternary Glaciation in the Mayaxue Shan,Gansu Province.Journal of Glaciology and Geocryology 37(3):701-710.(In Chinese).https://doi.org/10.7522/j.issn.1000-0240.2015.0079
Liu CR,Yin GM,Gao L,et al.(2010)ESR dating of Pleistocene archaeological localities of the Nihewan Basin,North ChinaPreliminary results.Quaternary Geochronology 5(2-3):385-390.https://doi.org/10.1016/j.quageo.2009.05.006
Liu GN,Li YK,Chen YX,et al.(2011)Glacial landform chronology and environment reconstruction of Peiku Gangri.Himalayas.Journal of Glaciology and Geocryology 33:959-970.(In Chinese)
Liu CR,Yin GM,Gao L,et al.(2011)Research advances in ESRgeochronology of Quaternary deposits.Seismology and Geology2(33):490-498.(In Chinese).https://doi.org/10.3969/j.issn.0253-4967.2011.02.022
Liu CR,Yin GM,Grün R(2013)Research Progress of the Resetting Features of Quartz ESR Signal.Advances in Earth Science 28(1):24-30.(In Chinese).https://doi.org/10.11867/j.issn.1001-8166.2013.01.0024
Liu CR,Yin GM,Han F,et al.(2016)ESR dating methodology and its application in dating Quaternary terrestrial sediments.Quaternary Sciences 36(5):1236-1245.(In Chinese).https://doi.org/10.11928/j.issn.1001-7410.2016.05.18
Lisiecki,LE,Raymo,ME(2005)A Pliocene-Pleistocene stack of 57globally distributed benthicδ18O records.Paleoceanography 20(1):1-17.https://doi.org/10.1029/2004PA001071
Murray AS,Wintle AG(2000)Luminescence dating of quartz using an improved single-aliquot regenerative-dose protocol.Radiation Measurements 32(1):57-73.https://doi.org/10.1016/S1350-4487(99)00253-X
Norton KP,Abbuhl LM,Schlunegger F(2010)Glacial conditioning as an erosional driving force in the Central Alps.Geology 38(7):655-658.https://doi.org/10.1130/G31102.1
Ou XJ,Lai ZP,Zhou SZ,et al.(2014)Timing of glacier fluctuations and trigger mechanisms in eastern Qinghai-Tibetan Plateau during the late Quaternary.Quaternary Research 81(3):464-475.https://doi.org/10.1016/j.yqres.2013.09.007
Owen LA,Robinson R,Benn DI,et al.(2009)Quaternary glaciation of Mount Everest.Quaternary Science Reviews 28(15):1412-1433.https://doi.org/10.1016/j.quascirev.2009.02.010
Owen LA,Dortch JM(2014)Nature and timing of Quaternary glaciation in the Himalayan-Tibetan orogen.Quaternary Science Reviews 88(88):14-54.https://doi.org/10.1016/j.quascirev.2013.11.016
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 Science Reviews 24(12):1391-1411.https://doi.org/10.1016/j.quascirev.2004.10.014
Owen LA,Finkel RC,Haizhou M,et al.(2003)Timing and style of Late Quaternary glaciation in northeastern Tibet.Geological Society of America Bulletin 115(11):1356-1364.https://doi.org/10.1130/B25314.1
Prescott JR,Hutton JT(1994)Cosmic-ray contributions to doserates for luminescence and ESR dating-large depths and longterm time variations.Radiation Measurements 23(2-3):497-500.https://doi.org/10.1016/1350-4487(94)90086-8
Richards B(2000)Luminescence dating of Quaternary sediments in the Himalaya and High Asia:A practical guide to its use and limitations for constraining the timing of glaciation.Quaternary International 65-66:49-61.https://doi.org/10.1016/S1040-6182(99)00036-1
Rink WJ,Bartoll J,Schwarcz HP,et al.(2007)Testing the reliability of ESR dating of optically exposed buried quartz sediments.Radiation Measurements 42(10):1618-1626.https://doi.org/10.1016/j.radmeas.2007.09.005
Shi YF,Huang MH,Ren BH(1988)An introduction to the glaciers in China contents.Science Press,Beijing(In Chinese).
Shi YF,Liu SY(2000)Estimation on the response of glaciers in China to the global warming in the 21st century.Chinese Science Bulletin 45(7):668-672.https://doi.org/10.1007/BF02886048
Shi YF(2002)Characteristics of late Quaternary monsoonal glaciation on the Tibetan Plateau and in East Asia.Quaternary International 97(2):79-91.https://doi.org/10.1016/S1040-6182(02)00053-8
Shi YF,Yao TD(2002)MIS 3b(54-44 ka BP)cold period and glacial advance in middle and low latitudes.Journal of Glaciolgy and Geocryology 24(1):1-9.(In Chinese).
Su Z,Pu JC(1996)Development conditions,Number and morphological characteristics of glaciers in the Hengduan Mountains region.In:Li JJ,Su,Z 1996.Glaciers in the Hengduan Mountains.Science Press,Beijing,pp.1-21(In Chinese).
Tanaka K,Hataya R,Spooner NA,et al.(1997)Dating of marine terrace sediments by ESR,TL and OSL methods and their applicabilities.Quaternary Science Reviews 16(3-5):257-264.https://doi.org/10.1016/S0277-3791(96)00092-3
Tang LY,Shen CM,Liu KB,et al.(2004)Climatic changes since the Last Glacial Maximum in the southeastern Tibetan Plateau:pollen evidence.Science in China 34(34):434-442.(in Chinese)https://doi.org/10.3969/j.issn.1674-7240.2004.05.006
Tang LY,Shen CM,Kong ZZ,et al.(1998)Pollen evidence of climate during the Last Glacial Maximum in eastern Tibetan Plateau.Journal of Glaciology and Geocryology 20(2):133-140.(In Chinese).
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