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Depositional processes of reworked tephra from the Late Pleistocene Youngest Toba Tuff deposits in the Lenggong Valley, Malaysia

Published online by Cambridge University Press:  20 January 2017

Emma Gatti ,
Mokhtar Saidin ,
Khairunnisa Talib ,
NurAsikin Rashidi ,
Philip Gibbard  and
Clive Oppenheimer
Emma Gatti*
Affiliation:
Department of Geography, Downing Place, CB2 3EN, University of Cambridge, Cambridge, UK
Mokhtar Saidin
Affiliation:
Centre for Global Archaeological Research, Universiti Sains Malaysia, Penang 11800, Malaysia
Khairunnisa Talib
Affiliation:
Centre for Global Archaeological Research, Universiti Sains Malaysia, Penang 11800, Malaysia
NurAsikin Rashidi
Affiliation:
Centre for Global Archaeological Research, Universiti Sains Malaysia, Penang 11800, Malaysia
Philip Gibbard
Affiliation:
Department of Geography, Downing Place, CB2 3EN, University of Cambridge, Cambridge, UK
Clive Oppenheimer
Affiliation:
Department of Geography, Downing Place, CB2 3EN, University of Cambridge, Cambridge, UK
*
*Corresponding author. E-mail address:eg322@cam.ac.uk (E. Gatti).
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Abstract

Two fundamental issues for tephrostratigraphic work are the differentiation of primary from reworked tephra and the characterization of reworking mechanisms. We study the depositional processes of four deposits of Youngest Toba Tuff in the Lenggong valley, Malaysia. We focus on site stratigraphy, particle-size distributions, magnetic susceptibility and mineralogical associations. Reworked tephra display variable sedimentological characteristics including polymodal and unimodal, very fine to coarse-grained distributions, and variable concentrations of ash. Particle-size distributions from this study are similar to published analyses for primary deposits, demonstrating that particle size alone cannot distinguish primary from secondary tephra. The tephra sequences are associated with fluvial and colluvial deposition. Three facies are identified: flood flow, mudflow and slumping. The ash accumulated rapidly, over a period of a few days to months. In this valley the ideal site for paleoenvironmental reconstructions is Kampung Luat 3, where ash accumulated at least in two distinct phases. Despite the rapid accumulation, the Lenggong sites are not well-suited for paleoenvironmental studies of the YTT impact. The time lag between the primary deposition and the floods is unknown and the records could have been modified by site-specific characteristics. Such variables should be considered when proposing paleo-environmental reconstructions based on reworked tephra.

Keywords

Youngest Toba TuffPrimary tephraReworked tephraFluvial stratigraphyParticle sizeMineralogyPaleoenvironmental reconstructionsLenggong valleyMalaysia
Type
Research Article
Information
Quaternary Research , Volume 79 , Issue 2 , March 2013 , pp. 228 - 241
Copyright
University of Washington

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References

Acharyya, S.K., and Basu, P.K. Toba ash on the Indian subcontinent and its implications for correlation of Late Pleistocene alluvium. Quaternary Research 40, 1 (1993). 10–19.CrossRefGoogle Scholar
Alloway, B.V., Larsen, G., Lowe, D.J., Shane, P.A.R., Westgate, J.A. Scott, A.E. Quaternary Stratigraphy | Tephrochronology, Encyclopedia of Quaternary Science. (2007). Elsevier, Oxford. 2869–2898.Google Scholar
Ambrose, S.H. Late Pleistocene human population bottlenecks, volcanic winter, and differentiation of modern humans. Journal of Human Evolution 34, 6 (1998). 623–651.CrossRefGoogle Scholar
Ambrose, S.H. Did the super-eruption of Toba cause a human population bottleneck? Reply to Gathorne-Hardy and Harcourt-Smith. Journal of Human Evolution 45, 3 (2003). 231 Google Scholar
Beddoe-Stephens, B., Aspden, J.A., and Shepherd, T.J. Glass inclusions and melt compositions of the Toba Tuffs, northern Sumatra. Contributions to Mineralogy and Petrology 83, 3 (1983). 278–287.Google Scholar
Blinkhorn, J., Parker, A.G., Ditchfield, P., Haslam, M., and Petraglia, M. Uncovering a landscape buried by the super-eruption of Toba, 74,000 years ago: a multi-proxy environmental reconstruction of landscape heterogeneity in the Jurreru Valley, south India. Quaternary International 258, (2012). 135–147.Google Scholar
Blott, S.J., and Pye, K. GRADISTAT: a grain size distribution and statistics package for the analysis of unconsolidated sediments. Earth Surface Processes and Landforms 26, 11 (2001). 1237–1248.Google Scholar
Chesner, C.A. Petrogenesis of the Toba Tuffs, Sumatra, Indonesia. Journal of Petrology 39, 3 (1998). 397–438.CrossRefGoogle Scholar
Chesner, C.A., and Rose, W.I. Stratigraphy of the Toba-Tuffs and the evolution of the Toba-Caldera Complex, Sumatra, Indonesia. Bulletin of Volcanology 53, 5 (1991). 343–356.CrossRefGoogle Scholar
Chesner, C.A., Rose, W.I., Deino, A., Drake, R., and Westgate, J.A. Eruptive history of Earth's largest Quaternary caldera (Toba, Indonesia) clarified. Geology 19, 3 (1991). 200–203.Google Scholar
Collings, H.D. Pleistocene site in the Malay Peninsula. Nature 3595, (1938). 575–576.CrossRefGoogle Scholar
Davies, S.M., Elmquist, M., Bergman, J., Wohlfarth, B., and Hammarlund, D. Cryptotephra sedimentation processes within two lacustrine sequences from west central Sweden. The Holocene 17, 3 (2007). 319–330.Google Scholar
Davies, S.M., Abbott, P.M., Pearce, N.J.G., Wastegård, S., and Blockley, S.P.E. Integrating the INTIMATE records using tephrochronology: rising to the challenge. Quaternary Science Reviews 36, (2012). 11–27.Google Scholar
Folch, A., Costa, A., Durant, A., and Macedonio, G. A model for wet aggregation of ash particles in volcanic plumes and clouds: 2. Model application. Journal of Geophysical Research 115, B9 (2010). B09202 Google Scholar
Folk, R.L., and Ward, W.C. Brazos River bar [Texas]; a study in the significance of grain size parameters. Journal of Sedimentary Research 27, 1 (1957). 3–26.CrossRefGoogle Scholar
Gathorne-Hardy, F.J., and Harcourt-Smith, W.E.H. The super-eruption of Toba, did it cause a human bottleneck?. Journal of Human Evolution 45, 3 (2003). 227–230.Google Scholar
Gatti, E., and Oppenheimer, C. Utilization of distal tephra records for understanding climatic and environmental consequences of the Youngest Toba Tuff. Giosan, L., Fuller, D., Nicoll, R., Flad, R.K., Clift, P.D. Climates, Landscapes and Civilizations, Geophys. Monogr. Ser. vol. 198, (2012). AGU, Washington, DC. 63–74.Google Scholar
Gatti, E., Durant, A.J., Gibbard, P.L., and Oppenheimer, C. Youngest Toba Tuff in the Son Valley, India: a weak and discontinuous stratigraphic marker. Quaternary Science Reviews 30, 27–28 (2011). 3925–3934.Google Scholar
Haslam, M., and Petraglia, M. Comment on “Environmental impact of the 73 ka Toba super-eruption in South Asia” by M.A.J. Williams, S.H. Ambrose, S. van der Kaars, C. Ruehlemann, U. Chattopadhyaya, J. Pal and P.R. Chauhan [Palaeogeography, Palaeoclimatology, Palaeoecology 284 (2009) 295–314]. Palaeogeography, Palaeoclimatology, Palaeoecology 296, 1–2 (2010). 199–203.Google Scholar
Haslam, M., Clarkson, C., Petraglia, M., Korisettar, R., Jones, S., Shipton, C., Ditchfield, P., and Ambrose, S.H. The 74 ka Toba super-eruption and southern Indian hominins: archaeology, lithic technology and environments at Jwalapuram Locality 3. Journal of Archaeological Science 37, 12 (2010). 3370–3384.Google Scholar
Jones, S.C. Palaeoenvironmental response to the 74 ka Toba ash-fall in the Jurreru and Middle Son valleys in southern and north-central India. Quaternary Research 73, 2 (2010). 336–350.Google Scholar
Jones, S.C. Local- and regional-scale impacts of the 74 ka Toba supervolcanic eruption on hominin populations and habitats in India. Quaternary International 258, (2012). 100–118.Google Scholar
Jones, S.C., and Pal, J.N. The Palaeolithic of the Middle Son valley, north-central India: changes in hominin lithic technology and behaviour during the Upper Pleistocene. Journal of Anthropological Archaeology 28, 3 (2009). 323 Google Scholar
Kale, V.S., Patil, D.N., Powar, N.J., and Rajaguru, S.N. Discovery of a volcanic ash bed in the alluvial sediments at Morgaon, Maharashtra. Man and Environment 18, (1993). 141–143.Google Scholar
Kataoka, K. Volcaniclastic remobilization and resedimentation in distal terrestrial settings in response to large-volume rhylitic eruptions: examples from the Plio-Pleistocene volcaniclastic sediments, central Japan. Journal of Geosciences 46 (2003). 47–65.Google Scholar
Kataoka, K. Distal fluvio-lacustrine volcaniclastic resedimentation in response to an explosive silicic eruption: the Pliocene Mushono tephra bed, central Japan. Geological Society of America Bulletin 117, 1–2 (2005). 3–17.Google Scholar
Kataoka, K.S., Manville, V., Nakajo, T., and Urabe, A. Impacts of explosive volcanism on distal alluvial sedimentation: examples from the Pliocene–Holocene volcaniclastic successions of Japan. Sedimentary Geology 220, 3–4 (2009). 306 Google Scholar
Korisettar, R., Mishra, S., Rajaguru, S.N., Gogte, V.D., Ganjoo, r.K., Venkatesan, T.R., Tandon,, s.K., Somayajulu, B.L.K., and Kale, V.S. Age of the Bori volcanic ash and Lower Palaeolithic culture of the Kukdi Valley, Maharashtra. Bulletin of the Deccan College Postgraduate and Research Institute 48, (1988). 135–138.Google Scholar
Kuznetsova, E.P., Motenko, R.G., Vigasina, M.F., and Mel'chakova, L.V. IR spectroscopy and thermal study of volcanic ashes of different age: annual seminar on experimental mineralogy, petrology and geochemistry. Bulletin of Environmental Sciences RAS 1, 27 (2009). 83 Google Scholar
Lewis, L., Ditchfield, P., Pal, J.N., and Petraglia, M. Grain size distribution analysis of sediments containing Younger Toba tephra from Ghoghara, Middle Son valley, India. Quaternary International 258, (2012). 180–190.CrossRefGoogle Scholar
Lowe, D.J. Tephrochronology and its application: a review. Quaternary Geochronology 6, 2 (2011). 107–153.Google Scholar
Lowe, J.J., and Walker, M.J.C. Reconstructing Quaternary Environments. (1984). Longman Scientific and Technical, London.Google Scholar
Manville, V., Newton, E.H., and White, J.D.L. Fluvial responses to volcanism: resedimentation of the 1800a Taupo ignimbrite eruption in the Rangitaiki River catchment, North Island, New Zealand. Geomorphology 65, 1–2 (2005). 49–70.Google Scholar
Margari, V., Pyle, D.M., Bryant, C., and Gibbard, P.L. Mediterranean tephra stratigraphy revisited: results from a long terrestrial sequence on Lesvos Island, Greece. Journal of Volcanology and Geothermal Research 163, 1–4 (2007). 34 Google Scholar
Mason, B.G., Pyle, D.M., and Oppenheimer, C. The size and frequency of the largest explosive eruptions on Earth. Bulletin of Volcanology 66, 8 (2004). 735–748.CrossRefGoogle Scholar
Mastrolorenzo, G., Palladino, D.M., Vecchio, G., and Taddeucci, J. The 472 AD Pollena eruption of Somma-Vesuvius (Italy) and its environmental impact at the end of the Roman Empire. Journal of Volcanology and Geothermal Research 113, 1–2 (2002). 19–36.Google Scholar
Matthews, N.E., Smith, V.C., Costa, A., Durant, A.J., Pyle, D.M., and Pearce, N.J.G. Ultra-distal tephra deposits from super-eruptions: examples from Toba and New Zealand. Quaternary International 258, (2012). 54–79.Google Scholar
Mokhtar, S. Debu Gunung Berapi di Lembah Lenggong, Perak. Journal Arkeologi Malaysia 22, (2009). 1–12.Google Scholar
Morgan, R.P.C. The influence of scale in climatic geomorphology: a case study of drainage density in West Malaysia. Geografiska Annaler Series A, Physical Geography 55, 2 (1973). 107–115.Google Scholar
Morley, M.W., and Woodward, J.C. The Campanian Ignimbrite (Y5) tephra at Crvena Stijena Rockshelter, Montenegro. Quaternary Research 75, 3 (2011). 683–696.Google Scholar
Mullins, C.E. Magnetic susceptibility of the soil and its significance in soil science—a review. Journal of Soil Science 28, 2 (1977). 223–246.Google Scholar
Nakayama, K. Subaerial liquefied flow of volcaniclastic sediments, central Japan. Peakall, J., McCaffrey, B., Kneller, B. Sediment Transport and Deposition by Particulate Gravity Currents: International Association of Sedimentologist Special Publication vol. 31, (2001). 233–244.Google Scholar
Nakayama, K., and Yoshikawa, S. Depositional processes of primary to reworked volcaniclastics on an alluvial plain; an example from the Lower Pliocene Ohta tephra bed of the Tokai Group, central Japan. Sedimentary Geology 107, 3–4 (1997). 211 Google Scholar
Ninkovich, D. Distribution, age and chemical composition of tephra layers in deep-sea sediments off western Indonesia. Journal of Volcanology and Geothermal Research 5, 1–2 (1979). 67–86.CrossRefGoogle Scholar
Ninkovich, D., Shackleton, N.J., Abdel-Monem, A.A., Obradovich, J.D., and Izett, G. K–Ar age of the late Pleistocene eruption of Toba, north Sumatra. Nature 276, 5688 (1978). 574–577.Google Scholar
Oppenheimer, C. Limited global change due to the largest known Quaternary eruption, Toba 74 kyr BP?. Quaternary Science Reviews 21, 14–15 (2002). 1593–1609.CrossRefGoogle Scholar
Oppenheimer, C. Eruptions that Shook the World. (2012). Elsevier Inc., (408 pp.)Google Scholar
Pearce, N.J.G., Bendall, C.A., and Westgate, J.A. Comment on “Some numerical considerations in the geochemical analysis of distal microtephra” by A.M. Pollard, S.P.E. Blockley and C.S. Lane. Applied Geochemistry 23, 5 (2008). 1353–1364.Google Scholar
Petraglia, M., Korisettar, R., Boivin, N., Clarkson, C., Ditchfield, P., Jones, S., Koshy, J., Lahr, M.M., Oppenheimer, C., Pyle, D., Roberts, R., Schwenninger, J.-L., Arnold, L., and White, K. Middle Paleolithic assemblages from the Indian subcontinent before and after the Toba super-eruption. Science 317, 5834 (2007). 114–116.Google Scholar
Petraglia, M.D., Ditchfield, P., Jones, S., Korisettar, R., and Pal, J.N. The Toba volcanic super-eruption, environmental change, and hominin occupation history in India over the last 140,000 years. Quaternary International 258, (2012). 119–134.Google Scholar
Pyne-O'Donnell, S. The taphonomy of Last Glacial–Interglacial Transition (LGIT) distal volcanic ash in small Scottish lakes. Boreas 40, 1 (2011). 131–145.Google Scholar
Rampino, M.R., and Self, S. Volcanic winter and accelerated glaciation following the Toba super-eruption. Nature 359, 6390 (1992). 50 Google Scholar
Rampino, M.R., and Self, S. Climate–volcanism feedback and the Toba eruption of 74,000 years ago. Quaternary Research 40, 3 (1993). 269 Google Scholar
Rose, W.I., and Chesner, C.A. Dispersal of ash in the great Toba eruption, 75 ka. Geology 15, 10 (1987). 913–917.2.0.CO;2>CrossRefGoogle Scholar
Rose, W.I., and Chesner, C.A. Worldwide dispersal of ash and gases from earth's largest known eruption: Toba, Sumatra, 75 ka. Palaeogeography, Palaeoclimatology, Palaeoecology 89, 3 (1990). 269–275.Google Scholar
Sarna-Wojcicki, A.M., and Davis, J.O. Quaternary tephrochronology. Morrison, R.B. The Geology of North America, Quaternary Nonglacial Geology: Conterminous U.S. The Geological Society of America, Boulder, Colorado. (1991). 93–116.Google Scholar
Sarna-Wojcicki, A.M., Meyer, C.E., Bowman, H.R., Timothy Hall, N., Russell, P.C., Woodward, M.J., and Slate, J.L. Correlation of the Rockland ash bed, a 400,000-year-old stratigraphic marker in northern California and western Nevada, and implications for middle Pleistocene palaeogeography of central California. Quaternary Research 23, 2 (1985). 236–257.Google Scholar
Schneider, J.L., Le Ruyet, A., Chanier, F., Buret, C., Ferriåre, J., Proust, J.-N.l, and Rosseel, J.-B. Primary or secondary distal volcaniclastic turbidites: how to make the distinction? An example from the Miocene of New Zealand (Mahia Peninsula, North Island). Sedimentary Geology 145, 1–2 (2001). 1–22.Google Scholar
Schulz, H., Emeis, K.-C., Erlenkeuser, H., von Rad, U., and Rolf, C. The Toba volcanic event and interstadial/stadial climates at the marine isotopic stage 5 to 4 transition in the Northern Indian Ocean. Quaternary Research 57, 1 (2002). 22–31.Google Scholar
Scrivenor, J.B. A recent rhyolite-ash with sponge-spicules and diatoms in Malaya. Geological Magazine 67, 9 (1930). 385–393.Google Scholar
Shane, P., Westgate, J., Williams, M., and Korisettar, R. New geochemical evidence for the youngest Toba Tuff in India. Quaternary Research 44, 2 (1995). 200–204.Google Scholar
Smith, V.C., Pearce, N.J.G., Matthews, N.E., Westgate, J.A., Petraglia, M.D., Haslam, M., Lane, C.S., Korisettar, R., and Pal, J.N. Geochemical fingerprinting of the widespread Toba tephra using biotite compositions. Quaternary International 246, 1–2 (2011). 97–104.Google Scholar
Stauffer, P.H. Cenozoic. Gobbett, D.J., and Hutchison, C.S. Geology of the Malay Peninsula (West Malaysia and Singapore). Regional Geology (1972). John wiley and Sons, 143–176.Google Scholar
Stauffer, P.H. Late Pleistocene age indicated for volcanic ash in west Malaysia. Geological Society of Malaysia Newsletter 40, (1973). 1–4.Google Scholar
Van der Kaars, S., Williams, M.A.J., Bassinot, F., Guichard, F., Moreno, E., Dewilde, F., and Cook, E.J. The influence of the 73 ka Toba super-eruption on the ecosystems of northern Sumatra as recorded in marine core BAR94-25. Quaternary International 258, (2012). 45–53.Google Scholar
Walker, D. Studies on the Quaternary of the Malay Peninsula. Pt. I. Alluvial deposits of Perak and the relative levels of land and sea. Federal Museum Journal 1–2, (1956). 19–34.Google Scholar
Westgate, J.A., Perkins, W.T., Fuge, R., Pearce, N.J.G., and Wintle, A.G. Trace-element analysis of volcanic glass shards by laser ablation inductively coupled plasma mass spectrometry: application to tephrochronological studies. Applied Geochemistry 9, 3 (1994). 323–335.Google Scholar
Westgate, J.A., Shane, P.A.R., Pearce, N.J.G., Perkins, W.T., Korisettar, R., Chesner, C.A., Williams, M.A.J., and Acharyya, S.K. All Toba tephra occurrences across peninsular India belong to the 75,000 yr B.P. eruption. Quaternary Research 50, 1 (1998). 107–112.Google Scholar
Williams, M. The 73 ka Toba super-eruption and its impact: history of a debate. Quaternary International 258, (2012). 19–29.Google Scholar
Williams, M. Did the 73 ka Toba super-eruption have an enduring effect? Insights from genetics, prehistoric archaeology, pollen analysis, stable isotope geochemistry, geomorphology, ice cores, and climate models. Quaternary International 269, (2012). 87–93.Google Scholar
Williams, M.A.J., Ambrose, S.H., van der Kaars, S., Ruehlemann, C., Chattopadhyaya, U., Pal, J., and Chauhan, P.R. Environmental impact of the 73 ka Toba super-eruption in South Asia. Palaeogeography, Palaeoclimatology, Palaeoecology 284, 3–4 (2009). 295–314.Google Scholar
Williams, M.A.J., Ambrose, S.H., der Kaars, S. v, Ruehlemann, C., Chattopadhyaya, U., Pal, J., and Chauhan, P.R. Reply to the comment on “Environmental impact of the 73 ka Toba super-eruption in South Asia” by M. A. J. Williams, S. H. Ambrose, S. van der Kaars, C. Ruehlemann, U. Chattopadhyaya, J. Pal, P. R. Chauhan [Palaeogeography, Palaeoclimatology, Palaeoecology 284 (2009) 295–314]. Palaeogeography, Palaeoclimatology, Palaeoecology 296, 1–2 (2010). 204–211.Google Scholar
Zielinski, G.A., Mayewski, P.A., Meeker, L.D., Whitlow, S., Twickler, M.S., and Taylor, K. Potential atmospheric impact of the Toba mega-eruption ~ 71,000 years ago. Geophysical Research Letters 23, (1996). Google Scholar