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Phased evolution and variation of the South Asian monsoon, and resulting weathering and surface erosion in the Himalaya–Karakoram Mountains, since late Pliocene time using data from Arabian Sea core

Published online by Cambridge University Press:  27 April 2020

Huayu Lu Open the ORCID record for Huayu Lu [Opens in a new window] ,
Ruixuan Liu ,
Linhai Cheng ,
Han Feng ,
Hanzhi Zhang ,
Yao Wang ,
Rong Hu ,
Wancang Zhao ,
Junfeng Ji  and
Zhaokai Xu
...Show all authors
Huayu Lu*
Affiliation:
Key Laboratory of Coast and Island Development, Ministry of Education, School of Geography and Ocean Science, Nanjing University, Nanjing210023, China
Ruixuan Liu
Affiliation:
Key Laboratory of Coast and Island Development, Ministry of Education, School of Geography and Ocean Science, Nanjing University, Nanjing210023, China
Linhai Cheng
Affiliation:
Key Laboratory of Coast and Island Development, Ministry of Education, School of Geography and Ocean Science, Nanjing University, Nanjing210023, China
Han Feng
Affiliation:
Key Laboratory of Coast and Island Development, Ministry of Education, School of Geography and Ocean Science, Nanjing University, Nanjing210023, China
Hanzhi Zhang
Affiliation:
Key Laboratory of Coast and Island Development, Ministry of Education, School of Geography and Ocean Science, Nanjing University, Nanjing210023, China
Yao Wang
Affiliation:
Key Laboratory of Coast and Island Development, Ministry of Education, School of Geography and Ocean Science, Nanjing University, Nanjing210023, China
Rong Hu
Affiliation:
Key Laboratory of Coast and Island Development, Ministry of Education, School of Geography and Ocean Science, Nanjing University, Nanjing210023, China
Wancang Zhao
Affiliation:
Key Laboratory of Coast and Island Development, Ministry of Education, School of Geography and Ocean Science, Nanjing University, Nanjing210023, China Key Laboratory of Surficial Geochemistry, Ministry of Education, School of Earth Sciences and Engineering, Nanjing University, Nanjing210023, China
Junfeng Ji
Affiliation:
Key Laboratory of Surficial Geochemistry, Ministry of Education, School of Earth Sciences and Engineering, Nanjing University, Nanjing210023, China
Zhaokai Xu
Affiliation:
Key Laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences, Qingdao266071, China
Zhaojie Yu
Affiliation:
Key Laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences, Qingdao266071, China
Denise K. Kulhanek
Affiliation:
International Ocean Discovery Program, Texas A&M University, 1000 Discovery Drive, College 10 Station, TX77845, USA
Dhananjai K. Pandey
Affiliation:
Department of Marine Geophysics, National Centre for Antarctic and Ocean Research (NCAOR), Vasco da Gama, Goa403804, India
Peter D. Clift
Affiliation:
Department of Geology and Geophysics, Louisiana State University, Baton Rouge, LA70803, USA
*
Author for correspondence: Huayu Lu, Email: huayulu@nju.edu.cn
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Abstract

We investigate the phased evolution and variation of the South Asian monsoon and resulting weathering intensity and physical erosion in the Himalaya–Karakoram Mountains since late Pliocene time (c. 3.4 Ma) using a comprehensive approach. Neodymium and strontium isotopic compositions and single-grain zircon U–Pb age spectra reveal the sources of the deposits in the east Arabian Sea, and show a combination of sources from the Himalaya and the Karakoram–Kohistan–Ladakh Mountains, with sediments from the Indian Peninsula such as the Deccan Traps or Craton. We interpret shifts in the sediment sources to have been forced by sea-level changes that correlate with South Asian monsoon rainfall variation since late Pliocene time. We collected 908 samples from the International Ocean Discovery Program Hole U1456A, which was drilled in the east Arabian Sea. Time series of hematite content and grain size of the sediments were examined downcore. We found South Asian monsoon precipitation and weathering intensity experienced three phases from late Pliocene time. Lower monsoon precipitation, with a lower variability and strong weathering intensity, occurred during 3.4–2.4 Ma; an increased and more variable South Asian monsoon rainfall, along with strengthened but fluctuating weathering intensity, occurred at 1.8–1.1 Ma; and a reduced rainfall with lower South Asian monsoon precipitation variability and moderate weathering intensity marked the period 1.1–0.1 Ma. Maximum entropy spectral analysis and wavelet transform show that there were orbital-dominated cycles of periods c. 100 and c. 41 ka in these proxy-based time series. We propose that the monsoon, sea level, global temperature and insolation together forced the weathering and erosion in SW Asia.

Keywords

zircon U–Pb agesNd–Sr isotopeshematite contentgrain sizeIODP Hole U1456Aeast Arabian Seamonsoon rainfall belt
Type
Original Article
Information
Geological Magazine , Volume 157 , Special Issue 6: Climate-tectonic interactions in the eastern Arabian Sea , June 2020 , pp. 864 - 878
Copyright
© The Author(s), 2020. Published by Cambridge University Press

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References

Aciego, SM, Bourdon, B, Lupker, M and Rickli, J (2009) A new procedure for separating and measuring radiogenic isotopes (U, Th, Pa, Ra, Sr, Nd, Hf) in ice cores. Chemical Geology 266, 194–204.CrossRefGoogle Scholar
Alizai, A, Carter, A, Clift, PD, Vanlaningham, S, Williams, JC and Kumar, R (2011) Sediment provenance, reworking and transport processes in the Indus River by U-Pb dating of detrital zircon grains. Global and Planetary Change 76, 33–55.CrossRefGoogle Scholar
Amir, A, Kenyon, NH, Cramp, A and Kidd, RB (1996) Morphology of channel-levee system on the Indus deep-sea fan, Arbian Sea. Pakistan Journal of Hydrocarbon Research 8, 43–53.Google Scholar
Andersen, T (2002) Correction of common lead in U–Pb analyses that do not report 204Pb. Chemical Geology 192, 59–79.CrossRefGoogle Scholar
Andersen, T (2005) Detrital zircons as tracers of sedimentary provenance: limiting conditions from statistics and numerical simulation. Chemical Geology 216, 249–70.CrossRefGoogle Scholar
Balsam, WL and Deaton, BC (1996) Determining the composition of late Quaternary marine sediments from NUV, VIS, and NIR diffuse reflectance spectra. Marine Geology 134, 31–55.CrossRefGoogle Scholar
Betzler, C, Eberli, GP, Kroon, D, Wright, JD, Swart, PK, Nath, BN, Alvarez-Zarikian, CA, Alonso-García, M, Bialik, OM, Blättler, CL, Guo, JA, Haffen, S, Horozal, S, Inoue, M, Jovane, L, Lanci, L, Laya, JC, Mee, ALH, Lüdmann, T, Nakakuni, M, Niino, K, Petruny, LM, Pratiwi, SD, Reijmer, JJG, Reolid, J, Slagle, AL, Sloss, CR, Su, X, Yao, Z and Young, JR (2016) The abrupt onset of the modern South Asian Monsoon winds. Scientific Reports 7, 29838.CrossRefGoogle Scholar
Blöthe, JH, Munack, H, Korup, O, Fülling, A, Garzanti, E, Resentini, A and Kubik, PW (2014) Late Quaternary valley infill and dissection in the Indus River, western Tibetan Plateau margin. Quaternary Science Reviews 94, 102–19.CrossRefGoogle Scholar
Boos, WR and Kuang, Z (2010) Dominant control of the South Asian monsoon by orographic insulation versus plateau heating. Nature 463, 218–22.CrossRefGoogle ScholarPubMed
Botsyun, S, Sepulchre, P, Donnadieu, Y, Risi, C, Licht, A and Rugenstein, JKC (2019) Revised paleoaltimetry data show low Tibetan Plateau elevation during the Eocene. Science, 363, eaaq1436, doi: 10.1126/science.aaq1436.CrossRefGoogle ScholarPubMed
Bourget, J, Zaragosi, S, Rodriguez, M, Fournier, M, Garlan, T and Chamot-Rooke, N (2013) Late Quaternary megaturbidites of the Indus fan: origin and stratigraphic significance. Marine Geology 336, 10–23.CrossRefGoogle Scholar
Chen, J, Li, G, Yang, J, Rao, W, Lu, H, Balsam, W, Sun, Y and Ji, J (2007) Nd and Sr isotopic characteristics of Chinese deserts: implications for the provenances of Asian dust. Geochimica et Cosmochimica Acta 71, 3904–14.CrossRefGoogle Scholar
Clemens, SC and Oglesby, RJ (1992) Interhemispheric moisture transport in the Indian Ocean summer monsoon: data-model and model-model comparisons. Paleoceanography 7, 633–43.CrossRefGoogle Scholar
Clemens, SC, Prell, WL and Sun, Y (2010) Orbital-scale timing and mechanisms driving Late Pleistocene Indo-Asian summer monsoons: reinterpreting cave speleothem δ18O. Paleoceanography 25, PA4207.CrossRefGoogle Scholar
Clift, PD (2017) Cenozoic sedimentary records of climate-tectonic coupling in the Western Himalaya. Progress in Earth and Planetary Science 4(39), 1–22.CrossRefGoogle Scholar
Clift, PD and Giosan, L (2014) Sediment fluxes and buffering in the post-glacial Indus Basin. Basin Research 26, 369–86.CrossRefGoogle Scholar
Clift, PD, Giosan, L, Blusztajn, J, Campbell, IH, Allen, C, Pringle, M, Tabrez, AR, Danish, M, Rabbani, MM and Alizai, A (2008) Holocene erosion of the Lesser Himalaya triggered by intensified summer monsoon. Geology 36, 79–82.CrossRefGoogle Scholar
Clift, PD, Lee, JI, Hildebrand, P, Shimizu, N, Layne, GD, Blusztajn, J, Blum, JD, Garzanti, E and Khan, AA (2002) Nd and Pb isotope variability in the Indus River System: implications for sediment provenance and crustal heterogeneity in the Western Himalaya. Earth and Planetary Science Letters 200, 91–106.CrossRefGoogle Scholar
Clift, PD and Vanlaningham, S (2010) A climatic trigger for a major Oligo-Miocene unconformity in the Himalayan foreland basin. Tectonics 29, TC5014.CrossRefGoogle Scholar
Clift, PD, Wan, S and Blusztajn, J (2014) Reconstructing chemical weathering, physical erosion and monsoon intensity since 25Ma in the northern South China Sea: a review of competing proxies. Earth-Science Reviews 130, 86–102.CrossRefGoogle Scholar
Clift, PD, Zhou, P, Stockli, DF and Blusztajn, J (2019) Regional Pliocene exhumation of the Lesser Himalaya in the Indus drainage. Solid Earth 10, 647–61, doi: 10.5194/se-10-647-2019.CrossRefGoogle Scholar
Colin, C, Turpin, L, Bertaux, J, Desprairies, A and Kissel, C (1999) Erosional history of the Himalayan and Burman ranges during the last two glacial–interglacial cycles. Earth and Planetary Science Letters 171, 647–60.CrossRefGoogle Scholar
Covault, JA, Craddock, WH, Romans, BW, Fildani, A and Gosai, M (2013) Spatial and temporal variations in landscape evolution: historic and longer-term sediment flux through global catchments. Journal of Geology 121, 35–56.CrossRefGoogle Scholar
Deaton, BC and Balsam, WL (1991) Visible spectroscopy; a rapid method for determining hematite and goethite concentration in geological materials. Journal of Sedimentary Research 61, 628–32.CrossRefGoogle Scholar
DeCelles, PG, Gehrels, GE, Quade, J, Lareau, B and Spurlin, M (2000) Tectonic implications of U-Pb zircon ages of the Himalayan orogenic belt in Nepal. Science 288, 497–9.CrossRefGoogle ScholarPubMed
Derry, LA and France-Lanord, C (1996) Neogene Himalayan weathering history and river 87Sr/86Sr; impact on the marine Sr record. Earth and Planetary Science Letters 142, 59–74.CrossRefGoogle Scholar
Goldstein, SL, O’Nions, RK and Hamilton, PJ (1984) A Sm-Nd isotopic study of atmospheric dusts and particulates from major river systems. Earth and Planetary Science Letters 70, 221–36.CrossRefGoogle Scholar
Goodbred, SL and Kuehl, SA (2000) Enormous Ganges-Brahmaputra sediment discharge during strengthened early Holocene monsoon. Geology 28, 1083–6.2.0.CO;2>CrossRefGoogle Scholar
Gupta, AK, Das, M and Anderson, DM (2005) Solar influence on the Indian summer monsoon during the Holocene. Geophysical Research Letters 32, L17703.CrossRefGoogle Scholar
Gupta, AK, Yuvaraja, A, Prakasam, M, Clemens, SC and Velu, A (2015) Evolution of the South Asian monsoon wind system since the late Middle Miocene. Palaeogeography, Palaeoclimatology, Palaeoecology 438, 160–7.CrossRefGoogle Scholar
Huber, M and Goldner, A (2012) Eocene monsoons. Journal of Asian Earth Sciences 44, 3–23, doi: 10.1016/j.jseaes.2011.09.014.CrossRefGoogle Scholar
Ji, J (2004) High resolution hematite/goethite records from Chinese loess sequences for the last glacial-interglacial cycle: rapid climatic response of the East Asian Monsoon to the tropical Pacific. Geophysical Research Letter 31, 171–4.CrossRefGoogle Scholar
Ji, J, Balsam, W, Chen, JU and Liu, L (2002) Rapid and quantitative measurement of hematite and goethite in the Chinese loess-paleosol sequence by diffuse reflectance spectroscopy. Clays and Clay Minerals 50, 208–16.CrossRefGoogle Scholar
Jonell, TN, Carter, A, Böning, P, Pahnke, K and Clift, PD (2017) Climatic and glacial impact on erosion patterns and sediment provenance in the Himalayan rain shadow, Zanskar River, NW India. Geological Society of America Bulletin 129, 820–36.CrossRefGoogle Scholar
Jonell, TN, Li, Y, Blusztajn, J, Giosan, L and Clift, PD (2018) Signal or noise? Isolating grain size effects on Nd and Sr isotope variability in Indus delta sediment provenance. Chemical Geology 485, 56–73CrossRefGoogle Scholar
Judd, DB and Wyszecki, G (1975) Color in Business, Science, and Industry. New York: John Wiley & Sons, 553 pp.Google Scholar
Kenyon, NH, Amir, A and Cramp, A (1995) Geometry of the younger sediment bodies of the Indus Fan. In Atlas of Deep Water Environments: Architectural Style in Turbidite System (eds Pickering, KT, Hiscott, RN, Kenyon, NH, Lucchi, F Ricci and Smith, RDA), pp. 89–93. London: Chapman & Hall.CrossRefGoogle Scholar
Khim, B-K, Horikawa, K, Asahara, Y, Kim, J-E and Ikehara, M (2019) Detrital Sr-Nd isotopes, sediment provenances, and depositional processes in the Laxmi Basin of the Arabian Sea during the last 800 ka. Geological Magazine, published online 23 November 2018, doi: 10.1017/S0016756818000596.CrossRefGoogle Scholar
Kodagali, VN and Jauhari, P (1999) The meandering Indus channels: study in a small area by the multibeam swath bathymetry system – Hydrosweep. Current Science 76(2), 240–43.Google Scholar
Kolla, V, Ray, PK and Kostecki, JA (1981) Surficial sediments of the Arabian Sea. Marine Geology 41, 183–204.CrossRefGoogle Scholar
Kroon, D, Steens, T and Troelstra, SR (1991) Onest of monsoonal related upwelling in the western Arabian Sea as revealed by planktonic foraminiferas. In Proceedings of the Ocean Drilling Program, Scientific Results (eds Prell, WL, Niitsuma, N, Emeis, KC, Al-Sulaiman, ZK, Al-Tobbah, ANK, Anderson, DM, Barnes, RO, Bilak, RA, Bloemendal, J, Bray, CJ, Busch, WH, Clemens, SC, de Menocal, P, Debrabant, P, Hayashida, A, Hermelin, JOR, Jarrad, RD, Krissek, LA, Kroom, D, Murray, DW, Nigrini, CA, Pedersen, TF, Ricken, W, Shimmield, GB, Spaulding, SA, Takayama, T, Haven, HL and Weedon, GP), pp. 257–264. College Station TX: International Ocean Discovery Program.Google Scholar
Li, Y, Clift, PD, Böning, P, Blusztajn, J, Murray, RW, Ireland, T, Pahnke, K and Giosan, L (2018) Continuous signal propagation in the Indus submarine canyon since the last deglacial. Marine Geology 406, 159–176.CrossRefGoogle Scholar
Li, Y, Clift, PD and O’Sullivan, PB (2019) Millennial and centennial variations in zircon U-Pb ages in the Quaternary Indus Submarine Canyon. Basin Research 31, 155–70.CrossRefGoogle Scholar
Licht, A, Van Cappelle, M, Abels, HA, Ladant, JB, Trabucho-Alexandre, J, France-Lanord, C, Donnadieu, Y, Vandenberghe, J, Rigaudier, T, Lécuyer, C, Terry, D Jr, Adriaens, R, Boura, A, Guo, Z, Soe, AN, Quade, J, Dupont-Nivet, G and Jaeger, JJ (2014) Asian monsoons in a late Eocene greenhouse world. Nature 513, 501–6.CrossRefGoogle Scholar
Lisiecki, LE and Raymo, ME (2005) A Pliocene-Pleistocene stack of 57 globally distributed benthic δ 18O records. Paleoceanography 20, PA1003.Google Scholar
Liu, R, Lu, H, Wang, Y, Yu, Z, Xu, Z, Feng, H and Hu, R (2018) Grain size analysis of a depositional sequence in the Laxmi basin (IODP hole U1456A, Arabian Sea) reveals the Indian monsoon shift at the mid-Pleistocene climatic transition. Quaternary Sciences 38(5), 1120–1129.Google Scholar
Long, S, Mcquarrie, N, Tobgay, T and Grujic, D (2011) Geometry and crustal shortening of the Himalayan fold-thrust belt, eastern and central Bhutan. Geological Society of America Bulletin 123, 1427–47.CrossRefGoogle Scholar
Lu, H, Chang, H, Guo, Z and Zhang, P (2015) Continental collision, Qinghai-Tibetan Plateau growth and climate evolution—An introduction to Professor Peter Molnar’s scientific contribution. Scientia Sinica Terrae 45, 770–9.Google Scholar
Lu, H, Wang, X, An, Z, Miao, X, Zhu, R, Ma, H, Li, Z, Tan, H and Wang, X (2004) Geomorphologic evidence of phased uplift of the northeastern Qinghai-Tibet Plateau since 14 million years ago. Science in China (Series D) 34, 855–64.Google Scholar
Lu, H, Zhang, H, Wang, Y, Zhao, L, Wang, H, Sun, W and Zhang, H (2018) Cenozoic depositional sequence in the Weihe Basin (Central China): a long-term record of Asian monsoon precipitation from the greenhouse to icehouse Earth. Quaternary Sciences 38, 1057–67 (in Chinese with English abstract), doi: 10.11928/j.issn.1001-7410.2018.05.01.Google Scholar
Mahar, GA and Zaigham, NA 2014. Examining spatio-temporal change detection in the Indus River Delta with the help of satellite data. Arabian Journal for Science and Engineering 40, 1933–46.CrossRefGoogle Scholar
Mehra, OP and Jackson, ML (1960) Iron oxide removal from soils and clays by a dithionite–citrate system buffered with sodium bicarbonate. In Proceedings of 7th National Conference on Clays and Clay Minerals, pp. 317–327. Washington: National Academy of Sciences.Google Scholar
Meyer, I, Davies, GR and Stuut, J-BW (2011) Grain size control on Sr-Nd isotope provenance studies and impact on paleoclimate reconstructions: an example from deep-sea sediments offshore NW Africa. Geochemistry, Geophysics, Geosystems 12, Q03005.CrossRefGoogle Scholar
Mishra, R, Pandey, DK, Ramesh, P and Clift, PD (2016) Identification of new deep-sea sinuous channels in the eastern Arabian Sea. SpringerPlus 5(1), 844–62.CrossRefGoogle ScholarPubMed
Mishra, R, Pandey, DK, Ramesh, P and Shipboard Scientific Party SK-306 (2015) Active channel system in the middle Indus fan: results from high-resolution bathymetry surveys. Current Science 108(3), 409–12.Google Scholar
Molnar, P (2001) Climate change, flooding in arid environments, and erosion rates. Geology 29, 1071–5.2.0.CO;2>CrossRefGoogle Scholar
Molnar, P, England, P and Martinod, J (1993) Mantle dynamics, uplift of the Tibetan Plateau, and the Indian monsoon. Reviews of Geophysics 31, 357–96.CrossRefGoogle Scholar
Pandey, DK, Clift, PD, Kulhanek, DK and The Expedition 355 Scientists (2016a) Arabian Sea Monsoon. In Proceedings of the International Ocean Discovery Program (eds Pandey, DK, Clift, PD, Kulhanek, DK and The Expedition 355 Scientists). College Station, TX: International Ocean Discovery Program.Google Scholar
Pandey, DK, Clift, PD, Kulhanek, DK, Andò, S, Bendle, JAP, Bratenkov, S, Griffith, EM, Gurumurthy, GP, Hahn, A, Iwai, M, Khim, B-K, Kumar, A, Kumar, AG, Liddy, HM, Lu, H, Lyle, MW, Mishra, R, Radhakrishna, T, Routledge, CM, Saraswat, R, Saxena, R, Scardia, G, Sharma, GK, Singh, AD, Steinke, S, Suzuki, K, Tauxe, L, Tiwari, M, Xu, Z and Yu, Z (2015) Expedition 355 Preliminary Report: Arabian Sea Monsoon. College Station TX: International Ocean Discovery Program.Google Scholar
Pandey, DK, Clift, PD, Kulhanek, DK, Andò, S, Bendle, JAP, Bratenkov, S, Griffith, EM, Gurumurthy, GP, Hahn, A, Iwai, M, Khim, B-K, Kumar, A, Kumar, AG, Liddy, HM, Lu, H, Lyle, MW, Mishra, R, Radhakrishna, T, Routledge, CM, Saraswat, R, Saxena, R, Scardia, G, Sharma, GK, Singh, AD, Steinke, S, Suzuki, K, Tauxe, L, Tiwari, M, Xu, Z and Yu, Z (2016b) Site U1456. In Arabian Sea Monsoon. In Proceedings of the International Ocean Discovery Program, 355 (eds Pandey, DK, Clift, PD, Kulhanek, DK and the Expedition 355 Scientists). College Station TX: International Ocean Discovery Program.Google Scholar
Pearce, NJG, Perkins, WT, Westgate, JA, Gorton, MP, Jackson, SE, Neal, CR and Chenery, SP (1997) A compilation of new and published major and trace element data for NIST SRM 610 and NIST SRM 612 glass reference materials. Geostandards and Geoanalytical Research 21, 115–44.CrossRefGoogle Scholar
Prell, WL and Kutzbach, JE (1987) Monsoon variability over the past 150,000 years. Journal of Geophysical Research 92, 8411–25.CrossRefGoogle Scholar
Prell, WL, Murray, DW, Clemens, SC and Anderson, DM (1992) Evolution and variability of the Indian Ocean summer monsoon: evidence from the western Arabian Sea Drilling Program. In Synthesis of Results from Scientific Drilling in the Indian Ocean (eds Duncan, RA, Rea, DK, Kidd, RB, von Rad, U and Weissel, JK), pp. 447–469. Washington DC: Amercian Geophysical Union.Google Scholar
Prins, MA, Postma, G, Cleveringa, J, Cramp, A and Kenyon, NH (2000) Controls on terrigenous sediment supply to the Arabian Sea during the late Quaternary: the Indus Fan. Marine Geology 169, 327–49.CrossRefGoogle Scholar
Ren, JS (2013) The 1:5 000 000 International Geological Map of Asia (IGMA5000). Acta Geologica Sinica 87(5), 1474.Google Scholar
Roe, GH, Ding, Q, Battisti, DS, Molnar, P, Clark, MK and Garzione, CN (2016) A modeling study of the response of Asian summertime climate to the largest geologic forcings of the past 50 Ma. Journal of Geophysical Research 121, 5453–70.Google Scholar
Scheinost, AC (1998) Use and limitations of second-derivative diffuse reflectance spectroscopy in the visible to near-infrared range to identify and quantify Fe oxide minerals in soils. Clays and Clay Minerals 46, 528–36.CrossRefGoogle Scholar
Schildgen, TF, Van Der Beek, PA, Sinclair, HD and Thiede, RC (2018) Spatial correlation bias in late-Cenozoic erosion histories derived from thermochronology. Nature 559, 89–93.CrossRefGoogle ScholarPubMed
Thiede, RC, Arrowsmith, JR, Bookhagen, B, Mcwilliams, MO, Sobel, ER and Strecker, M R (2005) From tectonically to erosionally controlled development of the Himalayan orogen. Geology 33, 689–92.CrossRefGoogle Scholar
Thiede, RC, Bookhagen, B, Arrowsmith, JR, Sobel, ER and Strecker, MR (2004) Climatic control on rapid exhumation along the Southern Himalayan Front. Earth and Planetary Science Letters 222, 791–806.CrossRefGoogle Scholar
Thiede, RC and Ehlers, TA (2013) Large spatial and temporal variations in Himalayan denudation. Earth and Planetary Science Letters 371–372, 278–93.CrossRefGoogle Scholar
Valdes, PJ, Ding, L, Farnsworth, A, Spicer, RA, Li, SH and Su, T (2019) Comment on “Revised paleoaltimetry data show low Tibetan Plateau elevation during the Eocene”. Science 365(6459), eaax8474, doi: 10.1126/science.aax8474.CrossRefGoogle Scholar
Vermeesch, P (2004) How many grains are needed for a provenance study? Earth and Planetary Science Letters 224, 441–51.CrossRefGoogle Scholar
Wang, P, Wang, B, Cheng, H, Fasullo, J, Guo, Z, Kiefer, T and Liu, Z (2017) The global monsoon across time scales: mechanisms and outstanding issues. Earth-Science Review 174, 84–121.CrossRefGoogle Scholar
Yin, A (2006) Cenozoic tectonic evolution of the Himalayan orogen as constrained by along-strike variation of structural geometry, exhumation history, and foreland sedimentation. Earth-Science Reviews 76, 1–131.CrossRefGoogle Scholar
Yu, Z, Colin, C, Wan, S, Saraswat, R, Song, L, Xu, Z, Clift, P, Lu, H, Lyle, M, Kulhanek, D, Hahn, A, Tiwari, M, Mishra, R, Miska, S and Kumar, A (2019) Sea level-controlled sediment transport to the eastern Arabian Sea over the past 600 kyr: Clay minerals and SrNd isotopic evidence from IODP Site U1457. Quaternary Science Reviews 205, 22–34.CrossRefGoogle Scholar
Zhang, H, Lu, H, Stevens, T, Feng, H, Fu, Y, Geng, J and Wang, H (2018) Expansion of dust provenance and aridification of Asia since ~7.2 Ma revealed by detrital zircon U-Pb dating. Geophysical Research Letters 45, 13437–48.CrossRefGoogle Scholar
Zhang, H, Lu, H, Xu, X, Liu, X, Yang, T, Stevens, T, Bird, A, Xu, Z, Zhang, T, Lei, F and Feng, H (2016) Quantitative estimation of the contribution of dust sources to Chinese loess using detrital zircon U-Pb age patterns. Journal of Geophysical Research: Earth Surface 121, 2085–99.Google Scholar
Zhang, P, Molnar, P and Downs, WR (2001) Increased sedimentation rates and grain sizes 2–4 Myr ago due to the influence of climate change on erosion rates. Nature 410, 891–7.Google Scholar
Zhang, W, Chen, J and Li, G (2015) Shifting material source of Chinese loess since ~2.7 Ma reflected by Sr isotopic composition. Scientific Reports 5, 10235.CrossRefGoogle ScholarPubMed
Zhang, Y, Ji, J, Balsam, WL, Liu, L and Chen, J (2007) High resolution hematite and goethite records from ODP 1143, South China Sea: Co-evolution of monsoonal precipitation and El Niño over the past 600,000 years. Earth and Planetary Science Letters 264, 136–50.CrossRefGoogle Scholar
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