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Clay mineral variations in Holocene terrestrial sediments from the Indus Basin

Published online by Cambridge University Press:  20 January 2017

Anwar Alizai ,
Stephen Hillier ,
Peter D. Clift ,
Liviu Giosan ,
Andrew Hurst ,
Sam VanLaningham  and
Mark Macklin
Anwar Alizai*
Affiliation:
School of Geosciences, University of Aberdeen, Meston Building, Aberdeen, AB24 3UE, UK
Stephen Hillier
Affiliation:
The James Hutton Institute, Craigiebuckler, Aberdeen AB15 8QH, UK
Peter D. Clift
Affiliation:
School of Geosciences, University of Aberdeen, Meston Building, Aberdeen, AB24 3UE, UK
Liviu Giosan
Affiliation:
Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA
Andrew Hurst
Affiliation:
School of Geosciences, University of Aberdeen, Meston Building, Aberdeen, AB24 3UE, UK
Sam VanLaningham
Affiliation:
School of Fisheries and Ocean Sciences, University of Alaska Fairbanks, Fairbanks AK 99775-7220, USA
Mark Macklin
Affiliation:
Institute of Geography and Earth Sciences, University of Wales, Aberystwyth, UK
*
*Corresponding author. E-mail address:anwar.alizai@gmail.com (A. Alizai).
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Abstract

We employed X-ray diffraction methods to quantify clay mineral assemblages in the Indus Delta and flood plains since ~ 14 ka, spanning a period of strong climatic change. Assemblages are dominated by smectite and illite, with minor chlorite and kaolinite. Delta sediments integrate clays from across the basin and show increasing smectite input between 13 and 7.5 ka, indicating stronger chemical weathering as the summer monsoon intensified. Changes in clay mineralogy postdate changes in climate by 5–3 ka, reflecting the time needed for new clay minerals to form and be transported to the delta. Samples from the flood plains in Punjab show evidence for increased chemical weathering towards the top of the sections (6–≪ 4 ka), counter to the trend in the delta, at a time of monsoon weakening. Clay mineral assemblages within sandy flood-plain sediment have higher smectite/(illite + chlorite) values than interbedded mudstones, suggestive of either stronger weathering or more sediment reworking since the Mid Holocene. We show that marine records are not always good proxies for weathering across the entire flood plain. Nonetheless, the delta record likely represents the most reliable record of basin-wide weathering response to climate change.

Keywords

XRDClay mineralogyMonsoonHimalayaIndus DeltaFloodplainFluvial processesLarge rivers
Type
Original Articles
Information
Quaternary Research , Volume 77 , Issue 3 , May 2012 , pp. 368 - 381
Copyright
University of Washington

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References

Adatte, T., Keller, G., Stinnesbeck, W., (2002). Late Cretaceous to early Paleocene climate and sea-level fluctuations: the Tunisian record. Palaeogeography, Palaeoclimatology, Palaeoecology. 178, 165–196.Google Scholar
Agrawal, D., Datta, P., Hussain, Z., Krishnamurthy, R., Misra, V., Rajaguru, S., Thomas, P., (1980). Palaeoclimate, stratigraphy and prehistory in north and west Rajasthan. Journal of Earth System Science. 89, 1 51–66.Google Scholar
Alizai, A., Carter, A., Clift, P.D., VanLaningham, S., Williams, J.C., Kumar, R., (2011a). 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
Alizai, A., Clift, P.D., Giosan, L., (2011b). Pb isotopic variability in the Modern and Holocene Indus River System measured by ion microprobe in detrital K-feldspar grains. Geochimica et Cosmochimica Acta. 75, 4771–4795. .Google Scholar
Birkeland, P.W., (1984). Soils and Geomorphology. Oxford University Press, Oxford, 310 pp.Google Scholar
Biscaye, P.E., (1965). Mineralogy and sedimentation of recent deep-sea clay in the Atlantic Ocean and adjacent seas and oceans. Geological Society of America Bulletin. 76, 803–832.Google Scholar
Bockheim, J.G., (1982). Properties of a chronosequence of ultra-xerous soils in the Trans-Antarctic mountains. Geoderma. 28, 239–255.Google Scholar
Bookhagen, B., Burbank, D.W., (2006). Topography, relief, and TRMM-derived rainfall variations along the Himalaya. Geophysical Research Letters. 33, L08405 .Google Scholar
Bookhagen, B., Fleitmann, D., Nishiizumi, K., Strecker, M.R., Thiede, R.C., (2006). Holocene monsoonal dynamics and fluvial terrace formation in the northwest Himalaya, India. Geology (Boulder). 34, 601–604.Google Scholar
Boulay, S., Colin, C., Trentesaux, A., Clain, S., Liu, Z., Lauer-Leredde, C., (2007). Sedimentary responses to the Pleistocene climatic variations recorded in the South China Sea. Quaternary Research. 68, 162–172.Google Scholar
Campbell, I.B., Claridge, G., (1982). The influence of moisture on the development of soils of the cold deserts of Antarctica. Geoderma. 28, 221–228.Google Scholar
Chamley, H., (1989). Clay Sedimentology. Springer-Verlag, Berlin, 267 pp.Google Scholar
Clift, P., Giosan, L., Blusztajn, J., (2008). Holocene erosion of the Lesser Himalaya triggered by intensified summer monsoon. Geology. 36, 1 79–82. .Google Scholar
Clift, P.D., Giosan, L., Henstock, T., Tabrez, A.R., VanLaningham, S., Alizai, A., Limmer, D., Danish, M., (2009). Sediment buffering and transport in the Holocene Indus River system. American Geophysical Union Eos Trans. AGU, Fall Meet. Suppl., Abstract, T35B-1950.Google Scholar
Clift, P.D., Carter, A., Giosan, L., Durcan, J., Tabrez, A.R., Alizai, A., VanLaningham, S., Duller, G.A.T., Macklin, M.G., Fuller, D.Q., Danish, M., (2012). U-Pb zircon dating evidence for a Pleistocene Sarasvati River and Capture of the Yamuna River. Geology .CrossRefGoogle Scholar
Colin, C., Siani, G., Sicre, M.-A., Liu, Z., (2010). Impact of the East Asian monsoon rainfall changes on the erosion of the Mekong River basin over the past 25,000 yr. Marine Geology. 271, 1–2 84–92. .CrossRefGoogle Scholar
Enzel, Y., Ely, L.L., Mishra, S., (1999). High-resolution Holocene environmental changes in the Thar Desert, northwestern India. Science. 284, 125–128.Google Scholar
Fagel, N., Hillaire-Marcel, C., Vernal, A.d., (2007). Marine clay minerals, deep circulation and climate. Paleoceanography of the Late Cenozoic. Volume 1, Methods, Elsevier, Amsterdam, 139–184.Google Scholar
Fleitmann, D., Burns, S.J., Mudelsee, M., Neff, U., Kramers, J., Mangini, A., Matter, A., (2003). Holocene forcing of the Indian monsoon recorded in a stalagmite from southern Oman. Science. 300, 5626 1737–1739.Google Scholar
Ghose, B., Kar, A., Husain, Z., (1979). The lost courses of the Saraswati River in the Great Indian Desert; new evidence from Landsat imagery. The Geographical Journal. 145, 3 446–451.Google Scholar
Giosan, L., Clift, P.D., Blusztajn, J., Tabrez, A., Constantinescu, S., Filip, F., (2006). On the control of climate- and human-modulated fluvial sediment delivery on river delta development: the Indus. Eos, Transactions, American Geophysical Union. 87, 52OS14A-04.Google Scholar
Griffin, J., Windom, H., Goldberg, E., (1968). The Distribution of Clay Minerals in the World Ocean. Elsevier, Amsterdam.CrossRefGoogle Scholar
Gupta, A.K., Anderson, D.M., Overpeck, J.T., (2003). Abrupt changes in the Asian southwest monsoon during the Holocene and their links to the North Atlantic Ocean. Nature. 421, 354–356.Google Scholar
Hamann, Y., Ehrmann, W., Schmiedl, G., Kuhnt, T., (2009). Modern and late Quaternary clay mineral distribution in the area of the SE Mediterranean Sea. Quaternary Research. 71, 3 453–464.CrossRefGoogle Scholar
Hillier, S., (1995). Erosion, sedimentation, and sedimentary origin of clays. Velde, B., Clays and the environment, Springer Verlag, Berlin, 162–219.Google Scholar
Hillier, S., (2003). Quantitative analysis of clay and other minerals in sandstones by X-ray powder diffraction (XRPD). Worden, R.H., Morad, S., Clay Mineral Cements in Sandstones. Special Publication, International Association of Sedimentologists.Google Scholar
Jacobs, M., (1970). Clay mineral investigations of Cretaceous and Quaternary deep sea sediments of the North American Basin. Journal of Sedimentary Research. 40, 3 864–868.Google Scholar
Jeong, G.Y., Hillier, S., Kemp, R.A., (2011). Changes in mineralogy of loess–paleosol sections across the Chinese Loess Plateau. Quaternary Research. 75, 1 245–255.Google Scholar
Lamy, F., Hebbeln, D., Wefer, G., (1998). Late Quaternary precessional cycles of terrigenous sediment input off the Norte Chico, Chile (27.5°S) and palaeoclimatic implications. Palaeogeography Palaeoclimatology Palaeoecology. 141, 233–251.Google Scholar
Moore, D., Reynolds, R., (1989). X-ray Diffraction and the Identification and Analysis of Clay Minerals. Oxford University Press, Oxford, 332 pp.Google Scholar
Morgan, R., (1973). The influence of scale in climatic geomorphology: a case study of drainage density in West Malaysia. Geografiska Annaler. Series A. Physical Geography. 55, 107–115.CrossRefGoogle Scholar
Overpeck, J., Anderson, D., Trumbore, S., Prell, W., (1996). The southwest Indian Monsoon over the last 18000 years. Climate Dynamics. 12, 213–225.Google Scholar
Pandarinath, K., (2009). Clay minerals in SW Indian continental shelf sediment cores as indicators of provenance and palaeomonsoonal conditions: a statistical approach. International Geology Review. 51, 2 145–165.Google Scholar
Prell, W.L., Curry, W.B., (1981). Faunal and isotopic indices of monsoonal upwelling: western Arabian Sea. Oceanologica Acta. 4, 91–98.Google Scholar
Rao, D.R., Sharma, K.K., (1995). Petrological and geochemical constraints on the petrogenesis of the Jaspa granitic pluton, Lahual region, NW Himalaya. Journal of the Geological Society of India. 45, 6 629–642.Google Scholar
Rateev, M., Gorbunova, Z., (1969). The distribution of clay minerals in the oceans. Sedimentology. 13, 1–2 21–43.Google Scholar
Singer, A., (1984). The paleoclimatic interpretation of clay minerals in sediments—a review. Earth-Science Reviews. 21, 251–293.Google Scholar
Srodon, J., Eberl, D., (1984). Illite. Reviews in Mineralogy and Geochemistry. 13, 1 495–544.Google Scholar
Stern, L.A., Chamberlain, C.P., Reynolds, R.C., Johnson, G.D., (1997). Oxygen isotope evidence of climate change from pedogenic clay minerals in the Himalayan molasse. Geochimica et Cosmochimica Acta. 61, 4 731–744.Google Scholar
Stuiver, M., Grootes, P.M., (2000). GISP2 oxygen isotope ratios. Quaternary Research (New York). 53, 3 277–284.Google Scholar
Thamban, M., Rao, V.P., (2005). Clay minerals as palaeomonsoon proxies: evaluation and relevance to the late Quaternary record from SE Arabian Sea. Rajan, S., Pandey, P.C., Antarctic Geoscience: Ocean-atmosphere Interaction and Paleoclimatology, National Centre for Antarctic & Ocean Research, Goa, India, 198–215.Google Scholar
Thamban, M., Rao, V.P., Schneider, R.R., (2002). Reconstruction of late Quaternary monsoon oscillations based on clay mineral proxies using sediment cores from the western margin of India. Marine Geology. 186, 527–539.Google Scholar
Thiry, M., (2000). Palaeoclimatic interpretation of clay minerals in marine deposits; an outlook from the continental origin. Earth-Science Reviews. 49, 1–4 201–221.CrossRefGoogle Scholar
Törnqvist, T.E., Bick, S.J., Gonzalez, J.L., van der Borg, K., de Jong, A.F.M., (2004). Tracking the sea-level signature of the 8.2 ka cooling event: new constraints from the Mississippi Delta. Geophysical Research Letters. 31, L23309 .CrossRefGoogle Scholar
Valdiya, K.S., (2002). Saraswati: The River that Disappeared. 1st. University Press, India, Limited, Hyderabad, India, 116 pp.Google Scholar
Wan, S., Li, A., Clift, P.D., Stuut, J.-B.W., (2007). Development of the East Asian monsoon: mineralogical and sedimentologic records in the northern South China Sea since 20 Ma. Palaeogeography, Palaeoclimatology, Palaeoecology. 254, 3–4 561–582.Google Scholar
Wilson, M.J., (1999). The origin and formation of clay minerals in soils: past, present and future perspectives. Clay Minerals. 34, 1 7–25.Google Scholar
Wünnemann, B., Demske, D., Tarasov, P., (2010). Hydrological evolution during the last 15 kyr in the Tso Kar lake basin (Ladakh, India), derived from geomorphological, sedimentological and palynological records. Quaternary Science Reviews. 29, 1138–1155.CrossRefGoogle Scholar
Zimmermann, H.B., (1977). Clay–mineral stratigraphy and distribution in the South Atlantic ocean. Initial Reports of the Deep Sea Drilling Project. 39, 395–405.Google Scholar
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