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Distinction between the Youngest Toba Tuff and Oldest Toba Tuff from northern Sumatra based on the area density of spontaneous fission tracks in their glass shards

Published online by Cambridge University Press:  20 January 2017

John A. Westgate ,
Nicholas J.G. Pearce ,
Emma Gatti  and
Hema Achyuthan
John A. Westgate*
Affiliation:
Department of Earth Sciences, University of Toronto, Toronto M5S 3B1, Ontario, Canada
Nicholas J.G. Pearce
Affiliation:
Department of Geography and Earth Science, Aberystwyth University, Wales SY23 3DB. UK
Emma Gatti
Affiliation:
NASA Jet Propulsion Laboratory, California Institute of Technology, 4800 Oak Grove Drive, Pasadena, CA 91106, USA
Hema Achyuthan
Affiliation:
Department of Geology, Anna University, Chennai, India
*
*Corresponding author. E-mail address:[email protected] (J.A.Westgate).
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Abstract

Determination of the area density of spontaneous fission tracks (ρs) in glass shards of Toba tephra is a reliable way to distinguish between the Youngest Toba Tuff (YTT) and the Oldest Toba Tuff (OTT). The ρs values for YTT, uncorrected for partial track fading, range from 70 to 181 tracks/cm2 with a weighted mean of 108 ± 5 tracks/cm2, based on 15 samples. Corrected ρs values for YTT are in the range of 77–140 tracks/cm2 with a weighted mean of 113 ± 8 tracks/cm2, within the range of uncorrected ρs values. No significant difference in ρs exists between YTT samples collected from marine and continental depositional settings. The uncorrected ρs for OTT is 1567 ± 114 tracks/cm2 so that confusion with YTT is unlikely.

The ρs values of the Toba tephra at Bori, Morgaon, and Gandhigram in northwestern India indicate a YTT identity, in agreement with geochemical data on their glass shards, the presence of multiple glass populations, and a glass fission-track age determination. Therefore, the view of others that OTT is present at these sites – and thereby indicates an early Pleistocene age for the associated Acheulean artifacts – is incorrect.

Keywords

Volcanic glass shardsSpontaneous fission tracksPartial track fadingToba tuffsAcheulean artifactsSumatraIndia
Type
Articles
Information
Quaternary Research , Volume 82 , Issue 2 , September 2014 , pp. 388 - 393
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, (1993). 10–19.CrossRefGoogle Scholar
Arias, C., Bigazzi, G., and Bonadonna, F.P. Size corrections and plateau age in glass shards. Nuclear Tracks 5, (1981). 129–136.CrossRefGoogle Scholar
Biswas, R.H., Williams, M.A.J., Raj, R., Juyal, N., and Singhvi, A.K. Methodological studies on luminescence dating of volcanic ashes. Quaternary Geochronology 17, (2013). 14–25.CrossRefGoogle Scholar
Chen, C.-H., Lee, M.-Y., Iizuka, Y., Dehn, J., Wei, K., and Carey, S.N. First Toba supereruption revival: comment and reply. Geology 35, (2004). 54–55.CrossRefGoogle Scholar
Chesner, C.A. The Toba caldera complex. Quaternary International 258, (2012). 5–18.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, (1991). 200–203.2.3.CO;2>CrossRefGoogle Scholar
Dehn, J., Farrell, J.W., and Schmincke, H.-U. Neogene tephrochronology from Site 758 on northern Ninety East Ridge: Indonesian arc volcanism of the past 5 Ma. Weissel, J., Peirce, J., Taylor, E., Alt, J. et al. Proceedings Ocean Drilling Program, Scientific Results 121, (1991). 273–295.Google Scholar
Diehl, J.F., Onstott, T.C., Chesner, C.A., and Knight, M.D. No short reversals of Brunhes age recorded in the Toba tuffs, north Sumatra, Indonesia. Geophysical Research Letters 14, (1987). 753–756.Google Scholar
Fleischer, R.L., Price, R.B., and Walker, R.M. Effects of temperature, pressure and ionization on the formation and stability of fission tracks in minerals and glasses. Journal of Geophysical Research 70, (1965). 1497–1502.CrossRefGoogle Scholar
Gaillard, C., Mishra, S., Singh, M., Deo, S., and Abbas, R. Lower and Early Middle Pleistocene Acheulian in the Indian subcontinent. Quaternary International 223–224, (2010). 234–241.CrossRefGoogle Scholar
Hall, C.H., and Farrell, J.W. Laser 40Ar/39Ar ages of tephra from Indian Ocean deep-sea sediments: tie points for the astronomical and geomagnetic polarity time scales. Earth and Planetary Science Letters 133, (1995). 327–338.CrossRefGoogle Scholar
Horn, P., Müller-Sohnius, D., Storzer, D., and Zöller, L. K-Ar, fission-track, and thermoluminescence ages of Quaternary volcanic tuffs and their bearing on Acheulian artifacts from Bori, Kukdi Valley, Pune district, India. Zeitschrift der Deutschen Geologischen Gesellschaft 144, (1993). 326–329.CrossRefGoogle Scholar
Kale, V.S., Ganjoo, R.K., Rajaguru, S.N., and Ota, S.B. Discovery of an Acheulian site at Bori, District Pune. Bulletin of the Deccan College Postgraduate and Research Institute 45, (1986). 47–49.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
Lane, C.S., Chorn, B.T., and Johnson, T.C. Ash from the Toba supereruption in Lake Malawi shows no volcanic winter in East Africa at 75 ka. Proceedings of the National Academy of Sciences 110, (2013). 8025–8029.CrossRefGoogle ScholarPubMed
Lee, M.-Y., Chen, C.-H., Wei, K.-Y., Iizuka, Y., and Carey, S. First Toba supereruption revival. Geology 32, (2004). 61–64.CrossRefGoogle Scholar
Mark, D.F., Petraglia, M., Smith, V.C., Morgan, L.E., Barfod, D.N., Ellis, B.S., Pearce, N.J., Pal, J.N., and Korisettar, R. A high-precision 40Ar/39Ar age for the Young Toba Tuff and dating of ultra-distal tephra: forcing of Quaternary climate and implications for hominin occupation of India. Quaternary Geochronology 21, (2014). 90–103.CrossRefGoogle Scholar
Mishra, S., Venkatesan, T.R., Rajaguru, S.N., and Somayajulu, B.L.K. Earliest Acheulian industry from Peninsula India. Current Anthropology 36, (1995). 847–851.CrossRefGoogle Scholar
Mishra, S., Deo, S.G., Abbas, R., Naik, S., Shete, G., Agrawal, N., and Rajaguru, S.N. Excavations at the early Acheulian site of Morgaon, Maharashtra (2000–2007). Paddayya, K., Joglekar, P.P., Basa, K.K., and Sawant, R. Recent Research Trends in South Asian Archaeology. (2009). Deccan College Postgraduate and Research Institute, Pune, 121–137.Google Scholar
Naeser, C.W., Izett, G.A., and Obradovich, J.D. Fission-track and K-Ar ages of natural glasses. United States Geological Survey Bulletin 1489, (1980). 31 Google Scholar
Naeser, N.D., Westgate, J.A., Hughes, O.T., and Péwé, T.L. Fission-track ages of late Cenozoic distal tephra beds in the Yukon Territory and Alaska. Canadian Journal of Earth Sciences 19, (1982). 2167–2178.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, (1978). 574–577.CrossRefGoogle Scholar
Pattan, J.N., Prasad, M.S., and Babu, E.V.S.S.K. Correlation of the oldest Toba Tuff to sediments in the central Indian Ocean Basin. Journal of Earth System Science 119, (2010). 531–539.CrossRefGoogle Scholar
Petraglia, M.D. Assessment and critique of chronometric ages associated with “Early” Acheulean assemblages in the Indian subcontinent. Yi, S. Handaxes in the Imjin Basin. (2011). Seoul National University Press, Seoul. 157–177.Google Scholar
Petraglia, M.D., Korisettar, R., and Pal, J.N. The Toba volcanic super-eruption of 74,000 year ago: climate change, environments, and evolving humans. Quaternary International 25, (2012). 1–4.CrossRefGoogle Scholar
Sandhu, A.S., and Westgate, J.A. The correlation between reduction in fission-track diameter and areal track density in volcanic glass shards and its application in dating tephra beds. Earth and Planetary Science Letters 131, (1995). 289–299.CrossRefGoogle Scholar
Sangode, S.J., Mishra, S., Naik, S., and Deo, S. Magnetostratigraphy of the Quaternary sediments associated with some Toba tephra and Acheulian artefact bearing localities in the western and central India. Gondwana Geological Magazine Special volume 10, (2007). 111–121.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, (2011). 97–104.CrossRefGoogle Scholar
Storzer, D., and Wagner, G.A. Correction of thermally lowered fission-track ages of tektites. Earth and Planetary Science Letters 5, (1969). 463–468.CrossRefGoogle Scholar
Wagner, G.A., and Van den haute, P. Fission-Track Dating. (1992). Ferdinand Enke Verlag, Stuttgart. (285 pp.)Google Scholar
Westaway, R., Mishra, S., Deo, S., and Bridgland, D.R. Methods for determination of the age of Pleistocene tephra, derived from eruption of Toba, in central India. Journal of Earth System Science 120, (2011). 503–530.CrossRefGoogle Scholar
Westgate, J.A., Shane, P.A.R., Pearce, N.J.G., Perkins, W.T., Korisettar, R., Chesner, C.A., and Williams, M.A.J. All Toba tephra occurrences across Peninsular India belong to the 75,000 yr B.P. eruption. Quaternary Research 50, (1998). 107–112.CrossRefGoogle Scholar
Westgate, J.A., Naeser, N.D., and Alloway, B.V. Fission-track dating. Elias, S. Encyclopedia of Quaternary Science. (2007). Elsevier, Amsterdam. 651–672.Google Scholar
Westgate, J.A., Pearce, N.J.G., Perkins, W.T., Preece, S.J., Chesner, C.A., and Muhammad, R.F. Tephrochronology of the Toba tuffs: four primary glass populations define the 75-ka Youngest Toba Tuff, northern Sumatra, Indonesia. Journal of Quaternary Science 28, (2013). 772–776.CrossRefGoogle Scholar