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Mega Tsunami of the World Oceans: Chevron Dune Formation, Micro-Ejecta, and Rapid Climate Change as the Evidence of Recent Oceanic Bolide Impacts

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Geophysical Hazards

Part of the book series: International Year of Planet Earth ((IYPE))

Abstract

This paper deals with the physical and environmental effects resulting from oceanic impacts by sizable comets, and the rates and risks associated with such cosmic impacts. Specifically, we investigate two sets of probable oceanic impact events that occurred within the last 5,000 years, one in the Indian Ocean about 2800 BC, and the other in the Gulf of Carpentaria (Australia) about AD 536. If validated, they would be the most energetic natural catastrophes occurring during the middle-to-late Holocene with large-scale environmental and historical human effects and consequences. The physical evidence for these two impacts consists of several sets of data: (1) remarkable depositional traces of coastal flooding in dunes (chevron dunes) found in southern Madagascar and along the coast of the Gulf of Carpentaria, (2) the presence of crater candidates (29-km Burckle crater about 1,500 km southeast of Madagascar which dates to within the last 6,000 years and 18-km Kanmare and 12-km Tabban craters with an estimated age of AD 572±86 in the southeast corner of the Gulf of Carpentaria), and (3) the presence of quench textured magnetite spherules and nearly pure carbon spherules, teardrop-shaped tektites with trails of ablation, and vitreous material found by cutting-edge laboratory analytical techniques in the upper-most layer of core samples close to the crater candidates.

Although some propose a wind-blown origin for V-shaped chevron dunes that are widely distributed around the coastlines of the Indian Ocean and in the Gulf of Carpentaria, we have evidence in favor of their mega tsunami formation. In southern Madagascar we have documented evidence for tsunami wave run-up reaching 205 m above sea-level and penetrating up to 45 km inland along the strike of the chevron axis. Subtly the orientation of the dunes is not aligned to the prevailing wind direction, but to the path of refracted mega-tsunami originating from Burckle impact crater.

The results of our study show that substantive oceanic comet impacts not only have occurred more recently than modeled by astrophysicists, but also that they have profoundly affected Earth’s natural systems, climate, and human societies. If validated, they could potentially lead to a major paradigm shift in environmental science by recognizing the role of oceanic impacts in major climate downturns during the middle-to-late Holocene that have been well documented already by different techniques (tree-ring anomalies, ice-, lake- and peat bog-cores).

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References

  • Abbott DH, Biscaye P, Cole-Dai J, Breger D (2008b) Magnetite and silicate spherules from the GISP2 core at the 536 A.D. horizon. EOS Transactions, American Geophysical Union, Fall Meeting Supplement, Abstract PP41B-1454:89

    Google Scholar 

  • Abbott DH, Bryant EA, Gusiakov V, Masse WB, Breger D (2008a) Impacts, mega-tsunami, and other extraordinary claims. Comment, GSA Today, 18(6):12

    Article  Google Scholar 

  • Abbott DH, Masse WB, Burckle L, Breger D, Gerard-Little P (2005) Burckle abyssal impact crater: did this impact produce a global deluge? Proceedings of Atlantis 2005 Conference: Milos, Greece

    Google Scholar 

  • Abbott DH, Tester EW, Meyers CA (2007a) Impact ejecta and megatsunami deposits from a historical impact into the Gulf of Carpentaria. Geological Society of America, Abstracts with Programs, vol 39, p 312

    Google Scholar 

  • Abbott DH, Tester EW, Meyers CA, Breger D, Chivas AM (2007b) Sediment transport, mixing, and erosion by an impact generated tsunami: Gulf of Carpentaria, Australia. EOS Transactions, American Geophysical Union, Abstract OS31B-07:88

    Google Scholar 

  • Baillie MG (2007) Tree-rings indicate global environmental downturns could have been caused by comet debris. In: Bobrowsky, PT, Rickman H (eds) Comet/Asteroid Impacts and Human Society: An Interdisciplinary Approach. Springer, Berlin, pp 105–122

    Chapter  Google Scholar 

  • Baker VR (ed) (1981) Catastrophic flooding: the origin of the channeled scabland. Dowden Hutchinson & Ross, Stroudsburg, PA

    Google Scholar 

  • Barrientos G, Masse WB (2009) Mid-Holocene cosmic impacts in central and northeastern Argentina: exploring probable effects on human population dynamics. Submitted to American Antiquity

    Google Scholar 

  • Birks JW, Crutzen PJ, Roble RG (2007) Frequent ozone depletion resulting from impacts of asteroids and comets. In: Bobrowsky, PT, Rickman H (eds) Comet/Asteroid Impacts and Human Society: An Interdisciplinary Approach. Springer, Berlin, pp 225–245

    Chapter  Google Scholar 

  • Blench R (2006) New palaezoogeographical evidence for the settlement of Madagascar. Conference on The Maritime Heritage and Cultures of the Western Indian Ocean in Comparative Perspective, Zanzibar, Stone Town

    Google Scholar 

  • Bobrowsky P, Rickman H (eds) (2007) Comet/asteroid impacts and human society: an interdisciplinary approach. Springer, Berlin

    Google Scholar 

  • Bonatti E (1990) Subcontinental mantle exposed in the Atlantic Ocean on St. Peter-Paul islets. Nature, 345:800–802

    Article  Google Scholar 

  • Bourgeois J, Weiss R (2009) “Chevrons” are not mega-tsunami deposite—A sedimentologic assessment. Geology, 37:403–406.

    Google Scholar 

  • Bryant E (2001) Tsunami: the underrated hazard, Cambridge University Press, Cambridge. Praxis, Chichester

    Google Scholar 

  • Bryant E (2008) Tsunami: the underrated hazard, 2nd edition. Praxis, Chichester

    Google Scholar 

  • Bryant E, Walsh G, Abbott D (2007) Cosmogenic mega-tsunami in the Australia region: are they supported by Aboriginal and Maori Legends? In: Piccardi, L, Masse, WB (eds) Myth and Geology. Geological Society of London Special Publication 273, London, pp 203–214

    Google Scholar 

  • Bryant EA, Young RW (1996) Bedrock-sculpturing by tsunami, South Coast New South Wales, Australia. Journal of Geology, 104:565–582

    Article  Google Scholar 

  • Burney DA, Burney LP, Godfrey LR, Jungers WL, Goodman SM, Wright HT, Jull AJ (2004) A chronology for late prehistoric Madagascar. Journal of Human Evolution, 47:25–63

    Article  Google Scholar 

  • Cane MA (2005) The evolution of El Nino, past and future. Earth and Planetary Science Letters, 230:227–240

    Article  Google Scholar 

  • Chapman CR (2007) The asteroid impact hazard and interdisciplinary issues. In: Bobrowsky, PT, Rickman H (eds) Comet/Asteroid Impacts and Human Society: An Interdisciplinary Approach. Springer, Berlin, pp 145–162

    Chapter  Google Scholar 

  • Chivas A, Garcia A, van der Kaars, S, Couapel MJJ, Holt S, Reeves JM, Wheeler DJ, Switzer AD, Murray Wallace CV et al. (2001) Sea-level and environmental changes since the last interglacial in the Gulf of Carpentaria, Australia: an overview. Quaternary International, 83–85:19–46

    Article  Google Scholar 

  • Clark CD, Garrod SM, Parker-Pearson M (1998) Landscape archaeology and remote sensing in southern Madagascar. International Journal of Remote Sensing, 19:1461–1477

    Article  Google Scholar 

  • Collins GS, Melosh HJ, Marcus R (2005) Earth impact effects program: a web-based computer program for calculating the regional environmental consequences of a meteoroid impact on earth. Meteoritics and Planetary Science, 40:817–840

    Article  Google Scholar 

  • Davison T, Collins G (2007) Investigating the effect of water depth on marine impact crater morphology. Workshop on Impact Cratering II, 8041

    Google Scholar 

  • Dick HJB, Fisher RL (1984) Mineralogic studies of the residues of mantle melting: abyssal and Alpine-type peridotites. In: Komprobst, J (ed) Kimberlites II: The Mantle and Crust-Mantle Relationships. Amsterdam, Elsevier, pp 292–308

    Google Scholar 

  • Drummond BJ, Denham D, Michael-Leiba M (1985) Rheology of the lithosphere and Australian earthquakes. Geology and Geophysics, Bureau of Mineral Resources, p 60

    Google Scholar 

  • Firestone RB, West A, Kennett JP, Becker L, Bunch TE, Revay ZS, Schulz PH, Belgya T, Kennett DJ, Erlandson JM, Dickensen OJ, Goodyear AC, Harris RS, Howard GA, Kloosterman JB, Lechler P, Mayewski PA, Montgomery J, Poreda R, Darrah T, Hee SSQ, Smith AR, Stich A, Topping W, Wittke JH, Wolbach WS (2007) Evidence for an extraterrestrial impact 12,900 years ago that contributed to the megafaunal extinctions and the Younger Dryas cooling. Proceedings of the National Academy of Sciences, 104:16016–16021

    Article  Google Scholar 

  • Gad-el-Hak M (ed) (2008) Large-scale disasters: predictions, control, and mitigation. Cambridge University Press, Cambridge

    Google Scholar 

  • Gault DE, Sonnett CP (1982) Laboratory simulation of pelagic asteroidal impact: atmospheric injection, benthic topography, and the surface wave radiation field. In: Silver, LT, and Schultz, PH (eds) Geological Implications of Impacts of Large Comets and Asteroids on the Earth. Geological Society of America Special Paper 190, pp 69–92

    Google Scholar 

  • Gisler GR, Weaver RP, Mader CL, Gittings MR (2003) Two and three dimensional simulations of asteroid ocean impacts. Science of Tsunami Hazards, 21:119

    Google Scholar 

  • Gusiakov VK (2003) NGDC/HTDB meeting on the historical tsunami database proposal. Tsunami Newsletter, 35(4):9–10

    Google Scholar 

  • Gusiakov VK (2009) Tsunami history. In: Robinson A, Bernard E (eds). The Sea, Tsunamis. Harvard University Press, Cambridge, vol 15, pp 23–53

    Google Scholar 

  • Hearty PJ, Neumann AC, Kaufman DS (1998) Chevron ridges and runup deposits in the Bahamas from storms late in Oxygen–Isotope substage 5e. Quaternary Research, 50:309–322

    Article  Google Scholar 

  • Hills JG, Mader CL (1997) Tsunami produced by the impacts of small asteroids. Annals of the New York Academy of Sciences, 822:381–394

    Article  Google Scholar 

  • Hong YT, Hong B, Lin QH, Shibata Y, Hirota M, Zhu YX, Leng XT, Wang Y, Yi L (2005) Inverse phase oscillations between the East Asian and Indian Ocean summer monsoons during the last 12,000 years and paleo-El Nino. Earth and Planetary Science Letters, 231:337–346

    Article  Google Scholar 

  • ITDB (2005) Integrated tsunami database for the Pacific and Indian Oceans, version 6.1 of 31 July 2005. Intergovernmental Oceanographic Commission – Tsunami Laboratory of the Institute of Computation Mathematics and Mathematical Geophysics, SD RAS, Novosibirsk, CD-ROM.

    Google Scholar 

  • Iwasaki SI (1997) The wave forms and directivity of a tsunami generated by an earthquake and a landslide. Science of Tsunami Hazards, 15:23–40

    Google Scholar 

  • Jones MR, Torgerson T (1988) Late quaternary evolution of Lake Carpentaria on the Australia-New Guinea continental shelf. Australian Journal of Earth Sciences, 35:313–324

    Article  Google Scholar 

  • Kawana T, Nakata T (1994) Timing of Late Holocene tsunamis originated around the Southern Ryukyu Islands, Japan, deduced from coralline tsunami deposits. Japanese Journal of Geography, 103:352–376

    Google Scholar 

  • Kelletat D (2008) Comments to Dawson, A.G. and Stewart, I. (2007) Tsunami deposits in the geological record. Sedimentary Geology, 211(3–4):87–91

    Article  Google Scholar 

  • Kelletat D, Scheffers A (2003) Chevron-shaped accumulations along the coastlines of Australia as potential tsunami evidences. Science of Tsunami Hazards, 21:174–188

    Google Scholar 

  • Kindler P, Strasser A (2000) Paleoclimatic significance of co-occuring wind and water induced sedimentary structures in the last interglacial coastal deposits from Bermuda and the Bahamas. Sedimentary Geology, 131:1–7

    Article  Google Scholar 

  • Kor PSG, Shaw J, Sharpe DR (1991) Erosion of bedrock by subglacial meltwater, Georgian Bay, Ontario: a regional view. Canadian Journal of Earth Science, 28:623–642

    Article  Google Scholar 

  • Lander JF (1996) Tsunamis affecting Alaska, 1737–1996. United States National Geophysical Data Center. Key Geophys. Research Document 31

    Google Scholar 

  • MacCraken MC (2007) The climatic effects of asteroid and comet impacts: Consequences for an increasingly interconnected society. In: Bobrowsky P, Rickman, H (eds) Comet/Asteroid Impacts and Human Society: An Interdisciplinary Approach: Berlin. Springer, Berlin, pp 277–289

    Chapter  Google Scholar 

  • Martos SN, Abbott DH, Elkinton HD, Chivas AR, Breger D (2006) Impact spherules from the craters Kanmare and Tabban in the Gulf of Carpentaria. Geological Society of America, Abstracts with Programs, 38:299–300

    Google Scholar 

  • Masse WB (1998) Earth, air, fire, and water: the archaeology of Bronze Age cosmic catastrophes. In: Peiser BJ, Palmer T, Bailey ME (eds) Natural catastrophes during Bronze Age civilizations: archaeological, geological, astronomical, and cultural perspectives. BAR International Series 728, Archaeopress, Oxford, pp 53–92

    Google Scholar 

  • Masse WB (2007) The Archaeology and Anthropology of Quaternary Period Cosmic Impact. In: Bobrowsky P, Rickman H (eds) Comet/Asteroid Impacts and Human Society: An Interdisciplinary Approach. Springer, Berlin, pp 25–70

    Chapter  Google Scholar 

  • Masse WB, Masse MJ (2007) Myth and catastrophic reality: using myth to identify cosmic impacts and massive Plinian eruptions in Holocene South America. In: Piccardi, L, Masse, WB (eds) Myth and Geology. Geological Society of London Special Publication 273, London, pp 177–202

    Google Scholar 

  • Masse WB, Weaver RP, Abbott DH, Gusiakov VK, Bryant EA (2007) Missing in action? Evaluating the putative absence of impacts by large asteroids and comets during the quaternary period. Proceedings of the Advanced Maui Optical and Space Surveillance Technologies Conference, Wailea, Hawaii, pp 701–710

    Google Scholar 

  • Maxwell TA, Haynes CV (1989) Large-scale, low amplitude bedforms (chevrons) in the Selima Sand Sheet. Science, 243:1179–1182

    Article  Google Scholar 

  • Melosh HJ (1989) Impact cratering: a geologic process. Oxford University Press, New York

    Google Scholar 

  • Michael PJ, Bonatti E (1985) Peridotite composition from the North Atlantic: regional and tectonic variations and implications for partial melting. Earth and Planetary Science Letters, 73:91–104

    Article  Google Scholar 

  • Morrison D, Harris AW, Sommer G, Chapman CR, Carusi A (2002) Dealing with the impact hazard. In: Bottke W, Cellino A.,Paolicchi P, Binzel RP (eds) Asteroids III, University of Arizona Press, Tucson, pp 739–754

    Google Scholar 

  • Mutter JC, Detrick RS (1984) Multichannel seismic evidence for anomalously thin crust at Blake Spur Fracture Zone. Geology, 12:534–537

    Article  Google Scholar 

  • Pinegina TK, Bourgeois J (2001) Historical and paleo-tsunami deposits on Kamchatka, Russia: long-term chronologies and long-distance correlations. Natural Hazards and Earth System Sciences, 1:177–185

    Article  Google Scholar 

  • Reeves JM, Chivas AR, Garcia A, Deckker PD (2007) Paleoenvironmental change in the Gulf of Carpentaria (Australia) since the last interglacial based on Ostracoda. Paleogeography, Paleoclimatology, Paleoecology, 246:163–187

    Article  Google Scholar 

  • Rigby E, Symonds M, Ward-Thompson D (2004) A comet impact in AD 536? Astronomy and Geophysics, 45:1.23–1.26.

    Google Scholar 

  • Sandwell DT, Smith WHF (2005) Retracking ERS-1 altimeter waveforms for optimal gravity field recovery. Geophysical Journal International, 163:79–89

    Article  Google Scholar 

  • Scheffers A (2004) Tsunami imprints on the Leeward Netherlands Antilles (Aruba, Curaçao, Bonaire) and their relation to other coastal problems. Quaternary International, 120:163–172

    Article  Google Scholar 

  • Scheffers AM, Kelletat DH, Scheffers SR, Abbott DH, Bryant EA (2008) Chevrons-enigmatic sedimentary coastal features. Zeitschrift für Geomorphologie, 52:375–402

    Article  Google Scholar 

  • Schultz PH, Lianza RE (1992) Recent grazing impacts on the Earth recorded in the Rio Cuarto crater field, Argentina. Nature, 355:232–237

    Google Scholar 

  • Smart J (1977) Late quaternary sea-level changes, Gulf of Carpentaria, Australia. Geology, 5:755–759

    Article  Google Scholar 

  • Smith WHF, Sandwell DT (1997) Global seafloor topography from satellite altimetry and ship depth soundings. Science, 277:1956–1962

    Article  Google Scholar 

  • Sturkell E (1998) The marine Lockne impact structure, Jamtland, Sweden: a review. Geological Rundschau, 87:253–267

    Article  Google Scholar 

  • Toon OB, Zahnle K, Morrison D, Turco RP, Covey C (1997) Environmental perturbations caused by the impacts of asteroids and comets. Review of Geophysics, 35:41–78

    Article  Google Scholar 

  • Torgerson T, Hutchinson MF, Searle DE, Nix HA (1983) General bathymetry of the Gulf of Carpentaria and the quaternary physiography of Lake Carpentaria. Palaeogeography, Palaeoclimatology, Palaeoecology, 41:207–225

    Article  Google Scholar 

  • Tornberg R (1997) Impact-related resurge sediments as exemplified by the Lockne, Tvaeren and Kaerdla structures. Geological Society of America, Abstracts with Programs, 29(6):80

    Google Scholar 

  • Tsikalas F, Gudlaugsson ST, Faleide JI, Eldholm O (1999) Mjolnir Structure, Barents Sea; a marine impact crater laboratory. In: Dressler, BO, Sharpton, LV, (eds) Large meteorite impacts and planetary evolution. Geological Society of America, Special Paper 339, pp 193–204

    Chapter  Google Scholar 

  • White RS, McKenzie D, O’Nions RK (1992) Oceanic crustal thickness from seismic measurements and rare earth element inversions. Journal of Geophysical Research, 97:19683–19715

    Article  Google Scholar 

  • Young R, Bryant E, Price DM (1996) Catastrophic wave (tsunami?) transport of boulders in southern New South Wales, Australia. Zeitschrift für Geomorphologie, 40:191–207

    Google Scholar 

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Acknowledgements

The authors wish to thank Mrs. T. Kalashnikova for assistance in preparing the figures and tables, and undertaking the final formatting of the manuscript. This work was partly supported by the RFBR grants 08-07-00105, 09-05-00294, and 07-05-13583, and NSF Grant OCE06-49024. Authors also appreciate the financial support provided by the WAPMERR (Geneva, Switzerland) for the 2006 Madagascar field trip, along with the field support provided by University of Antananarivo graduate students H. Razafindrakoto and A. Raveloson. D. Breger conducted the scanning electron microscopy and assisted with the X-ray analyses. We thank the centralized research facilities of Drexel University for the use of their SEM/EDS system.

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Authors and Affiliations

  1. Tsunami Laboratory, ICMMG SD RAS, 630090, Novosibirsk, Russia

    Viacheslav Gusiakov

  2. Lamont-Doherty Earth Observatory of Columbia University, 10964, Palisades, NY, USA

    Dallas H. Abbott

  3. School of Geoscience, University of Wollongong, 2522, Wollongong, NSW, Australia

    Edward A. Bryant

  4. Los Alamos National Laboratory, 87545, Los Alamos, NM, USA

    W. Bruce Masse

  5. Centralized Research Facilities, Drexel University, 19104, Philadelphia, PA, USA

    Dee Breger

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  1. Viacheslav Gusiakov
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  2. Dallas H. Abbott
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  4. W. Bruce Masse
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  1. CSIRO Atmospheric Research, Station Street 111, Aspendale, 3195, Australia

    Tom Beer

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Gusiakov, V., Abbott, D.H., Bryant, E.A., Masse, W.B., Breger, D. (2009). Mega Tsunami of the World Oceans: Chevron Dune Formation, Micro-Ejecta, and Rapid Climate Change as the Evidence of Recent Oceanic Bolide Impacts. In: Beer, T. (eds) Geophysical Hazards. International Year of Planet Earth. Springer, Dordrecht. https://doi.org/10.1007/978-90-481-3236-2_13

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