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Youngest Toba eruption

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exhibits evidence of a major population decline and it has been suggested that the abundant springs of the Jurreru Valley may have offered its inhabitants unique protection. At the Jurreru Valley in southern India, Middle Paleolithic stone tools below the Toba ash layer are dated by OSL to 77±4 kyr, while the age of stone tools above the ash layer is constrained to be no older than 55 kyr. This age gap is suspected to be due to the removal of post-eruption sediments or decimation of the local population until re-occupation at 55 kyr. Additional archaeological evidence from southern and northern India also suggests a lack of evidence for effects of the eruption on local populations, causing the authors of the study to conclude, "many forms of life survived the supereruption, contrary to other research which has suggested significant animal extinctions and genetic bottlenecks". However, some researchers have questioned the techniques utilized to date artifacts to the period subsequent to the Toba supervolcano. The Toba Catastrophe also coincides with the disappearance of the
556:. Maximum global mean cooling is 2.3 °C (4.1 °F) for the lower emission and 4.1 °C (7.4 °F) for the higher emission. Strong decrease in precipitation occurs in high emission. Negative temperature anomalies return to less than 1 °C (1.8 °F) within 3 and 6 years for each emission scenario after the eruption. But so far no model can simulate aerosol microphysical processes with sufficient accuracy, empirical constraints from historical eruptions suggest that aerosol size may substantially reduce magnitude of cooling to less than 1.5 °C (2.7 °F) no matter how much sulfur emitted. 488:, whether the eruption played any role in accelerating these events is much more debated. South China Sea marine records of climate, sampled at every centennial interval, shows 1 °C (1.8 °F) cooling above Toba ash layer for a thousand years but the authors concede that it may just be GS20. Arabian Sea marine records confirm that Toba ash occurred after the onset of GS20 but also that GS20 is not colder than GS21 in the records, from which authors conclude that the eruption did not intensify GS20 cooling. Dense sampling of environmental records, at every 6 784: 798: 40: 154: 516:
sulfate loadings that have ever been identified. In the ice core records, GS20 cooling was already underway by the time of sulfate deposition, nonetheless a 110-year period of accelerated cooling followed the sulfate event, and the authors interpret this acceleration as AMOC weakened by the Toba eruption.
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No Toba ash has been identified in ice core records, but four sulfate events within the ice strata have been proposed to possibly represent the deposition of aerosols from Toba eruption. One sulfate event at 73.75–74.16 kyr, which has all the characteristics of the Toba eruption, is among the largest
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5 to glacial MIS 4, experiencing cooling and glacial expansion. This transition is a part of Pleistocene interglacial-glacial cycle driven by variations in the earth's orbit. Ocean temperature cooled by 0.9 °C (1.6 °F). Sea level fell 60 m (200 ft). Northern Hemisphere ice sheets
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found very few variants, and to account for the low frequency of variation human population must have been as low as a few thousand until very recently. More genetic studies confirmed an effective population on the order of 10,000 for much of human history. Subsequent research on the differences in
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at the Jurreru Valley in southern India were found above and below a thick layer of ash from the Toba eruption and were very similar across these layers, suggesting that the dust clouds from the eruption did not wipe out this local population. However, another site in India, the Middle Son Valley,
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In 1993, science journalist Ann Gibbons posited that population growth was suppressed by the cold climate of the last Pleistocene Ice Age, possibly exacerbated by the Toba super-eruption which at the time was dated to between 73 and 75 kyr near the beginning of glacial period MIS 4. The subsequent
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reached a nadir around 50 kyr, though the long-term declining trend already started before 200 kyr. The estimated remaining effective population sizes are around 10,000 individuals, larger than the estimated non-African size during their bottleneck. Unlike the non-African populations, there is no
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subspecies. Whole-genome analysis similarly recovers very low African population sizes around 1 million years ago. This 1 million year old bottleneck is thought to have been caused by severe ice age MIS 22 which marked the mid-Pleistocene climate transition with widespread aridity across Africa.
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hypothesized that the Toba eruption caused a human population crash to only a few thousand surviving individuals, and the subsequent recovery was suppressed by the global glacial condition of MIS 4 until the climate eventually transitioned to the warmer condition of MIS 3 about 60,000 years ago,
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to the complete set of genetic material to infer human population history. In non-African populations, studies recover a long-term steep decline in numbers starting 200 kyr and reaching the lowest point around 40–60 kyr. During this bottleneck non-African populations experienced 5- to 15-fold
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related to cold adaptations in non-African populations, of which 31 sweeps occurred during 72–97 kyr. This event of closely timed selections is named Arabian Standstill and may have been caused by the severe cold arid conditions from the onset of MIS 4 and exacerbated by Toba super-eruption.
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Fan, Shaohua; Spence, Jeffrey P.; Feng, Yuanqing; Hansen, Matthew E.B.; Terhorst, Jonathan; Beltrame, Marcia H.; Ranciaro, Alessia; Hirbo, Jibril; Beggs, William; Thomas, Neil; Nyambo, Thomas; Mpoloka, Sununguko Wata; Mokone, Gaonyadiwe George; Njamnshi, Alfred K.; Fokunang, Charles (2023).
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Schaefer, Joerg M.; Putnam, Aaron E.; Denton, George H.; Kaplan, Michael R.; Birkel, Sean; Doughty, Alice M.; Kelley, Sam; Barrell, David J.A.; Finkel, Robert C.; Winckler, Gisela; Anderson, Robert F.; Ninneman, Ulysses S.; Barker, Stephen; Schwartz, Roseanne; Andersen, Bjorn G. (2015).
536:, volcanic winter has a maximum global mean cooling of 3.5 °C (6.3 °F) and returns gradually within the range of natural variability 5 years after the eruption. An initiation of 1,000-year cold period or ice age is not supported by the model. Two other emission scenarios, 4167:
Higham, Tom; Douka, Katerina; Wood, Rachel; Ramsey, Christopher Bronk; Brock, Fiona; Basell, Laura; Camps, Marta; Arrizabalaga, Alvaro; Baena, Javier; Barroso-Ruíz, Cecillio; Bergman, Christopher; Boitard, Coralie; Boscato, Paolo; Caparrós, Miguel; Conard, Nicholas J. (2014).
504:. The Lake Malawi studies concluded that the environmental effects of the eruption were mild and limited to less than a decade in East Africa, but these studies are questioned due to sediment mixing which would have diminished the cooling signal. Environmental records from a 5089:
Fan, Shaohua; Kelly, Derek E.; Beltrame, Marcia H.; Hansen, Matthew E. B.; Mallick, Swapan; Ranciaro, Alessia; Hirbo, Jibril; Thompson, Simon; Beggs, William; Nyambo, Thomas; Omar, Sabah A.; Meskel, Dawit Wolde; Belay, Gurja; Froment, Alain; Patterson, Nick (2019-04-26).
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ScienceDaily (Mar. 17, 2005) – By analyzing the relationship between the geographic location of current human populations in relation to East Africa and the genetic variability within these populations, researchers have found new evidence for an African origin of modern
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Kappelman, John; Todd, Lawrence C.; Davis, Christopher A.; Cerling, Thure E.; Feseha, Mulugeta; Getahun, Abebe; Johnsen, Racheal; Kay, Marvin; Kocurek, Gary A.; Nachman, Brett A.; Negash, Agazi; Negash, Tewabe; O'Brien, Kaedan; Pante, Michael; Ren, Minghua (2024).
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Petraglia, Michael; Korisettar, Ravi; Boivin, Nicole; Clarkson, Christopher; Ditchfield, Peter; Jones, Sacha; Koshy, Jinu; Lahr, Marta Mirazón; Oppenheimer, Clive; Pyle, David; Roberts, Richard; Schwenninger, Jean-Luc; Arnold, Lee; White, Kevin (2007-07-06).
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Sutikna, Thomas; Tocheri, Matthew W.; Morwood, Michael J.; Saptomo, E. Wahyu; Jatmiko; Awe, Rokus Due; Wasisto, Sri; Westaway, Kira E.; Aubert, Maxime; Li, Bo; Zhao, Jian-xin; Storey, Michael; Alloway, Brent V.; Morley, Mike W.; Meijer, Hanneke J. M. (2016).
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Mallick, Swapan; Li, Heng; Lipson, Mark; Mathieson, Iain; Gymrek, Melissa; Racimo, Fernando; Zhao, Mengyao; Chennagiri, Niru; Nordenfelt, Susanne; Tandon, Arti; Skoglund, Pontus; Lazaridis, Iosif; Sankararaman, Sriram; Fu, Qiaomei; Rohland, Nadin (2016).
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has shown that the effective human population size was less than 26,000 at 1.2 million years ago; possible explanations for the low population size of human ancestors may include repeated population crashes or periodic replacement events from competing
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caused by Out-of-Africa dispersal. As a small group with a size of a few thousand people migrated from the African continent into the Near East, the drastic reduction in numbers imprinted on non-African genomic diversity. Genetic analysis identified 56
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consensus as to the cause of African bottleneck. Proposed causes include climatic deterioration (from MIS 5, Toba eruption, GS20 and/or MIS 4), reduction in substructure across African populations, and founder effects from the dispersal within Africa.
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that flowed over the ground, and approximately 800 km (190 cu mi) that fell as ash mostly to the west. However, as more outcrops become available, the most recent estimate of eruptive volume is 3,800 km (910 cu mi)
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in 3.5 cm (1.4 in), and Central Indian Ocean Basin in 10 cm (3.9 in). Its horizon of ashfall covered an area of more than 38,000,000 km (15,000,000 sq mi) in 1 cm (0.39 in) or more thickness. In
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Crick, Laura; Burke, Andrea; Hutchison, William; Kohno, Mika; Moore, Kathryn A.; Savarino, Joel; Doyle, Emily A.; Mahony, Sue; Kipfstuhl, Sepp; Rae, James W. B.; Steele, Robert C. J.; Sparks, R. Stephen J.; Wolff, Eric W. (2021-10-18).
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Jacobs, Zenobia; Li, Bo; Shunkov, Michael V.; Kozlikin, Maxim B.; Bolikhovskaya, Nataliya S.; Agadjanian, Alexander K.; Uliyanov, Vladimir A.; Vasiliev, Sergei K.; O'Gorman, Kieran; Derevianko, Anatoly P.; Roberts, Richard G. (2019).
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Williams, Martin A.J.; Stanley H. Ambrose; Sander van der Kaars; Carsten Ruehlemann; Umesh Chattopadhyaya; Jagannath Pal; Parth R. Chauhan (30 December 2009). "Environmental impact of the 73 ka Toba super-eruption in South Asia".
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Ambrose, S. H. (2019), "Chapter 6 chronological calibration of Late Pleistocene Modern Human dispersals, climate change and Archaeology with Geochemical Isochrons", in Sahle, Yonatan; Reyes-Centeno, Hugo; Bentz, Christian (eds.),
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Svensson, A.; Bigler, M.; Blunier, T.; Clausen, H. B.; Dahl-Jensen, D.; Fischer, H.; Fujita, S.; Goto-Azuma, K.; Johnsen, S. J.; Kawamura, K.; Kipfstuhl, S.; Kohno, M.; Parrenin, F.; Popp, T.; Rasmussen, S. O. (2013-03-19).
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Du, Wenjing; Cheng, Hai; Xu, Yao; Yang, Xunlin; Zhang, Pingzhong; Sha, Lijuan; Li, Hanying; Zhu, Xiaoyan; Zhang, Meiliang; Stríkis, Nicolás M.; Cruz, Francisco W.; Edwards, R. Lawrence; Zhang, Haiwei; Ning, Youfeng (2019).
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is over 600 m (2,000 ft). The outflow sheet originally covered an area of 20,000–30,000 km (7,700–11,600 sq mi) with thickness nearly 100 m (330 ft), likely reaching into the
907: 439:. The start of GS20 cooling event corresponds to the start of Antarctic Isotope Maxima 19 (AIM19) warming event. GS20 was associated with iceberg discharges into the North Atlantic, thus it was also named 2424:
Menking, James A.; Shackleton, Sarah A.; Bauska, Thomas K.; Buffen, Aron M.; Brook, Edward J.; Barker, Stephen; Severinghaus, Jeffrey P.; Dyonisius, Michael N.; Petrenko, Vasilii V. (2022-09-16).
5491: 3668:"Had Youngest Toba Tuff (YTT, ca. 75 ka) eruption really destroyed living media explicitly in entire Southeast Asia or just a theoretical debate? An extensive review of its catastrophic event" 1808:; Johnsen, Racheal; Ren, Minghua; Fisher, Erich C.; Oestmo, Simen; Wilkins, Jayne; Harris, Jacob A.; Karkanas, Panagiotis; Fitch, Shelby; Ciravolo, Amber; Keenan, Deborah; Cleghorn, Naomi; 5529:
Shea, John. (2008). Transitions or Turnovers? Climatically-forced Extinctions of Homo sapiens and Neanderthals in the East Mediterranean Levant. Quaternary Science Reviews 27: 2253-2270.
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that started around the time of Toba eruption. The timing of the initiation of GS20 is dated to 74.0–74.2 kyr, and the entire event lasted about 1,500 years. It is the stadial part of
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Luo, Shu-Jin; Zhang, Yue; Johnson, Warren E.; Miao, Lin; Martelli, Paolo; et al. (2014). "Sympatric Asian felid phylogeography reveals a major Indochinese-Sundaic divergence".
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Jones, Sacha. (2012). Local- and Regional-scale Impacts of the ~74 ka Toba Supervolcanic Eruption on Hominin Population and Habitats in India. Quaternary International 258: 100-118.
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A, Bergstrom; SA, McCarthy; R, Hui; MA, Almarri; Q, Ayub; P, Danecek; Y, Chen; S, Felkel; P, Hallast; J, Kamm; H, Blanche; JF, Deleuze; H, Cann; S, Mallick; D, Reich (2020-10-23).
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flows. The ignimbrite phase is characterized by low eruption fountain, but co-ignimbrite column developed on top of pyroclastic flows reached a height of 32 km (20 mi).
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De Deckker, Patrick; Arnold, Lee J.; van der Kaars, Sander; Bayon, Germain; Stuut, Jan-Berend W.; Perner, Kerstin; Lopes dos Santos, Raquel; Uemura, Ryu; Demuro, Martina (2019).
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Batchelor, Christine L.; Margold, Martin; Krapp, Mario; Murton, Della K.; Dalton, April S.; Gibbard, Philip L.; Stokes, Chris R.; Murton, Julian B.; Manica, Andrea (2019-08-16).
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Shackleton, Sarah; Menking, James A.; Brook, Edward; Buizert, Christo; Dyonisius, Michael N.; Petrenko, Vasilii V.; Baggenstos, Daniel; Severinghaus, Jeffrey P. (2021-10-27).
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period. Previous volume estimates have ranged from 2,000 km (480 cu mi) to 6,000 km (1,400 cu mi). Inside the caldera, the maximum thickness of
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have estimated that the total amount of material released in the eruption was at least 2,800 km (670 cu mi)—about 2,000 km (480 cu mi) of
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and discoveries of archaeological cultures with Toba ash layer add further light to how humans had fared during the eruption and the following GS20 and MIS 4 ice age.
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ScienceDaily (Feb. 16, 2007) – When man made his way out of Africa some 60,000 years ago to populate the world, he was not alone: He was accompanied by the bacterium
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reduction, with only 1,000–3,000 remaining individuals at 50 kyr, consistent with the earliest mtDNA studies. This severe non-African contraction is consistent with
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Détroit, Florent; Mijares, Armand Salvador; Corny, Julien; Daver, Guillaume; Zanolli, Clément; Dizon, Eusebio; Robles, Emil; Grün, Rainer; Piper, Philip J. (2019).
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Ninkovich, D.; N.J. Shackleton; A.A. Abdel-Monem; J.D. Obradovich; G. Izett (7 December 1978). "K−Ar age of the late Pleistocene eruption of Toba, north Sumatra".
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Timmreck, Claudia; Graf, Hans-F.; Lorenz, Stephan J.; Niemeier, Ulrike; Zanchettin, Davide; Matei, Daniela; Jungclaus, Johann H.; Crowley, Thomas J. (2010-12-22).
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were activated within a few centuries before the eruption. The eruption commenced with small and limited air-fall and was directly followed by the main phase of
576:. However, some physical evidence disputes the association with the millennium-long cold event and genetic bottleneck, and some consider the theory disproven. 293:, depending on the existence of separate sulfur gas in the Toba magma chamber. The lower end of estimate is due to the low solubility of sulfur in the magma. 84: 2538:"Variations in the Earth's Orbit: Pacemaker of the Ice Ages: For 500,000 years, major climatic changes have followed variations in obliquity and precession" 2095: 1154:"Tephra glass chemistry provides storage and discharge details of five magma reservoirs which fed the 75 ka Youngest Toba Tuff eruption, northern Sumatra" 6661:
by Professor Stanley H. Ambrose, Department of Anthropology, University Of Illinois, Urbana, USA; Extract from "Journal of Human Evolution" 34, 623–651
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The modeled climate effects of the Toba eruption hinges on the mass of sulfurous gases and aerosol microphysical processes. Modeling on an emission of
5499: 645:, survived the Toba eruption and subsequent MIS 4 ice age, as their latest presence are dated to ca. 40 kyr, and ca. 55 kyr. Other lineages including 3131:"Subdecadal phytolith and charcoal records from Lake Malawi, East Africa imply minimal effects on human evolution from the ~74 ka Toba supereruption" 210:-forming eruptions at this location, with the earlier known caldera having formed around 1.2 million years ago. This last eruption had an estimated 4390:
Chang, Chun-Hsiang; Kaifu, Yousuke; Takai, Masanaru; Kono, Reiko T.; Grün, Rainer; Matsu'ura, Shuji; Kinsley, Les; Lin, Liang-Kong (2015-01-27).
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The exact year of the eruption is unknown, but the pattern of ash deposits suggests that it occurred during the northern summer because only the
3081:"High-resolution paleoecological records from Lake Malawi show no significant cooling associated with the Mount Toba supereruption at ca. 75 ka" 2880:"Marine Isotope Stage 4 in Australasia: A full glacial culminating 65,000 years ago – Global connections and implications for human dispersal" 6712: 993:"The exceptional magnitude and intensity of the Toba eruption, sumatra: An example of the use of deep-sea tephra layers as a geological tool" 5398: 5224:
Hu, Wangjie; Hao, Ziqian; Du, Pengyuan; Di Vincenzo, Fabio; Manzi, Giorgio; Cui, Jialong; Fu, Yun-Xin; Pan, Yi-Hsuan; Li, Haipeng (2023).
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The subsequent collapse formed a caldera that filled with water, creating Lake Toba. The island in the center of the lake is formed by a
6622: 2096:"Rapid speleothem δ13C change in southwestern North America coincident with Greenland stadial 20 and the Toba (Indonesia) supereruption" 6230: 6176: 3023:"The Toba Volcanic Event and Interstadial/Stadial Climates at the Marine Isotopic Stage 5 to 4 Transition in the Northern Indian Ocean" 484:
While Toba eruption occurred in the backdrop of rapid climate transitions of GS20 and MIS 4 triggered by changes in ocean currents and
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could have deposited Toba ashfall in the South China Sea. The eruption lasted perhaps 9 to 14 days. The most recent two high-precision
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Baxter, A. J.; Verschuren, D.; Peterse, F.; Miralles, D. G.; Martin-Jones, C. M.; Maitituerdi, A.; Van der Meeren, T.; Van Daele, M.;
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Tobler, Raymond; Souilmi, Yassine; Huber, Christian D.; Bean, Nigel; Turney, Chris S. M.; Grey, Shane T.; Cooper, Alan (2023-05-30).
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Other research has cast doubt on an association between the Toba Caldera Complex and a genetic bottleneck. For example, ancient
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Lin, Jiamei; Abbott, Peter M.; Sigl, Michael; Steffensen, Jørgen P.; Mulvaney, Robert; Severi, Mirko; Svensson, Anders (2023).
829: 941:"Toba ash layers in the South China Sea: Evidence of contrasting wind directions during eruption ca. 74 ka: Comment and Reply" 6011: 5878: 5445:"The Toba volcanic super-eruption, environmental change, and hominin occupation history in India over the last 140,000 years" 1662:"The Toba volcanic super-eruption, environmental change, and hominin occupation history in India over the last 140,000 years" 1048:"Astronomically calibrated 40 Ar/ 39 Ar age for the Toba supereruption and global synchronization of late Quaternary records" 862:"The Toba volcanic super-eruption, environmental change, and hominin occupation history in India over the last 140,000 years" 443:. Heinrich events tend to be longer, colder and with weaker AMOC in the Atlantic ocean than other DO stadials. From 74 to 58 752:
Some evidence indicates population crashes of other animals after the Toba eruption. The populations of the Eastern African
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site in Ethiopia, however, shows that a severe drought occurred concurrently with Toba ash layer which altered early human
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McGraw, Zachary; DallaSanta, Kevin; Polvani, Lorenzo M.; Tsigaridis, Kostas; Orbe, Clara; Bauer, Susanne E. (2024-02-15).
1709:"Discovery of the Toba Ash ( c. 70 ka) in a high-resolution core recovering millennial monsoonal variability off Pakistan" 610: 329:(DRE), of which 1,800 km (430 cu mi) was deposited as ash fall and 2,000 km (480 cu mi) as 3594:"Understanding the overestimated impact of the Toba volcanic super-eruption on global environments and ancient hominins" 2833:"The Last Interglacial–Glacial cycle (MIS 5–2) re-examined based on long proxy records from central and northern Europe" 6910: 6592: 3305:
Timmreck, Claudia; Graf, Hans-F.; Zanchettin, Davide; Hagemann, Stefan; Kleinen, Thomas; Krüger, Kirstin (2012-05-01).
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Oppenheimer, Clive (August 2002), "Limited global change due to largest known Quaternary eruption, Toba ≈74 kyr BP?",
2361:"A new view on abrupt climate changes and the bipolar seesaw based on paleotemperatures from Iberian Margin sediments" 6162: 4600:"Whole-genome sequencing reveals a complex African population demographic history and signatures of local adaptation" 3648: 2632:
Cutler, K.B; Edwards, R.L; Taylor, F.W; Cheng, H; Adkins, J; Gallup, C.D; Cutler, P.M; Burr, G.S; Bloom, A.L (2003).
1449: 317: 5281:"Hominin population bottleneck coincided with migration from Africa during the Early Pleistocene ice age transition" 1475:"Bipolar ice-core records constrain possible dates and global radiative forcing following the ∼74 ka Toba eruption" 239: 6687: 5738: 2974:"Cooling of the South China Sea by the Toba Eruption and correlation with other climate proxies ~71,000 years ago" 1584:"The Young Toba Tuff (73.9 ka) Magma Body – True Size and the most Extensive and Voluminous Ignimbrite Yet Known?" 6900: 6777: 6327: 4969:"The role of genetic selection and climatic factors in the dispersal of anatomically modern humans out of Africa" 533: 6659:
Mount Toba: Late Pleistocene human population bottlenecks, volcanic winter, and differentiation of modern humans
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Black, Benjamin A.; Lamarque, Jean-François; Marsh, Daniel R.; Schmidt, Anja; Bardeen, Charles G. (2021-07-20).
6915: 6895: 6818: 6795: 6771: 6143:"Volcanic winter in the Garden of Eden: The Toba supereruption and the late Pleistocene human population crash" 3534:"Volcanic winter in the Garden of Eden: The Toba supereruption and the late Pleistocene human population crash" 2071:
Guo, Z., Liu, J., Chu, G., & JFW, N. (2002). Composition and origin of tephra of the Huguangyan Maar Lake.
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may have also survived through the eruption. More recently, reconstructions of human demographic history using
6386: 1436:, Geophysical Monograph Series, vol. 139, Washington, D. C.: American Geophysical Union, pp. 11–40, 1152:
Pearce, Nicholas J.G.; Westgate, John A.; Gualda, Guilherme A.R.; Gatti, Emma; Muhammad, Ros F. (2019-10-14).
1115:"High-precision 40Ar/39Ar dating of Pleistocene tuffs and temporal anchoring of the Matuyama-Brunhes boundary" 6848: 6801: 5092:"African evolutionary history inferred from whole genome sequence data of 44 indigenous African populations" 1543:
Kutterolf, S.; Schindlbeck-Belo, J.C.; Müller, F.; Pank, K.; Lee, H.-Y.; Wang, K.-L.; Schmitt, A.K. (2023).
1203:"Constraining magma storage conditions of the Toba magmatic system: a plagioclase and amphibole perspective" 6870: 5451:. The Toba Volcanic Super-eruption of 74,000 Years Ago: Climate Change, Environments, and Evolving Humans. 823: 553: 489: 420: 3195:
Zielinski, G. A.; Mayewski, P. A.; Meeker, L. D.; Whitlow, S.; Twickler, M. S.; Taylor, K. (1996-04-15).
1545:"Revisiting the occurrence and distribution of Indian Ocean Tephra: Quaternary marine Toba ash inventory" 817: 803: 313: 187: 5813: 6940: 6875: 6655:, including bibliographic information on the two papers he has published on the Toba catastrophe theory 5623: 3080: 211: 133:
in 5 cm (2.0 in) of ash, volcanic winter may have caused a severe human population bottleneck
116: 6088:"Middle Paleolithic Assemblages from the Indian Subcontinent Before and After the Toba Super-eruption" 5867:"The Toba Supervolcanic Eruption: Tephra-Fall Deposits in India and Paleoanthropological Implications" 5812:
Huff, Chad. D; Xing, Jinchuan; Rogers, Alan R.; Witherspoon, David; Jorde, Lynn B. (19 January 2010).
5619:"Late Pleistocene human population bottlenecks, volcanic winter, and differentiation of modern humans" 5444: 4658:"Middle Paleolithic Assemblages from the Indian Subcontinent Before and After the Toba Super-Eruption" 3593: 2242: 1755: 6935: 6880: 6836: 6783: 3021:
Schulz, Hartmut; Emeis, Kay-Christian; Erlenkeuser, Helmut; Rad, Ulrich von; Rolf, Christian (2002).
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Petraglia, M.; Korisettar, R.; Boivin, N.; Clarkson, C.; Ditchfield, P.; et al. (6 July 2007).
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Petraglia, Michael D.; Ditchfield, Peter; Jones, Sacha; Korisettar, Ravi; Pal, J. N. (2012-05-01).
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Henn, Brenna M.; Botigué, Laura R.; Bustamante, Carlos D.; Clark, Andrew G.; Gravel, Simon (2015).
5226:"Genomic inference of a severe human bottleneck during the Early to Middle Pleistocene transition" 3566: 1615:"Stratigraphy of the Toba Tuffs and the evolution of the Toba Caldera Complex, Sumatra, Indonesia" 44:
Artist's impression of early stages of eruption from about 42 km (26 mi) above northern
6905: 6748: 6677: 6670: 5539: 5374: 3470:"Severe Global Cooling After Volcanic Super-Eruptions? The Answer Hinges on Unknown Aerosol Size" 3306: 2746: 1936:"Ash from the Toba supereruption in Lake Malawi shows no volcanic winter in East Africa at 75 ka" 1544: 1390: 662: 925:
Stratigraphy of the Toba Tuffs and the evolution of the Toba Caldera Complex, Sumatra, Indonesia
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Zielinski, G.A.; Mayewski, P.A.; Meeker, L.D.; Whitlow, S.; Twickler, M.S.; Taylor, K. (1996).
6359: 811: 262: 5866: 3821:"Drosophila melanogaster mitochondrial DNA: gene organization and evolutionary considerations" 2031: 6754: 6678:
Out of Africa – Bacteria, As Well: Homo Sapiens And H. Pylori Jointly Spread Across The Globe
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Hernandez, R.D.; Hubisz, M.J.; Wheeler, D.A.; Smith, D.G.; Ferguson, B.; et al. (2007).
4780:"Robust and scalable inference of population history from hundreds of unphased whole genomes" 691:
African populations experienced a slightly earlier, milder bottleneck and recovered earlier.
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explosive human expansion was believed to be the result of the end of the ice age. Geologist
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Steiper, M.E. (2006). "Population history, biogeography, and taxonomy of orangutans (Genus:
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Luo, S.-J.; Kim, J.-H.; Johnson, W.E.; Van der Walt, J.; Martenson, J.; et al. (2004).
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Petraglia, Michael D.; Ditchfield, Peter; Jones, Sacha; Korisettar, Ravi; Pal, J.N. (2012).
1430:"Petrological and volcanological constraints on volcanic sulfur emissions to the atmosphere" 860:
Petraglia, Michael D.; Ditchfield, Peter; Jones, Sacha; Korisettar, Ravi; Pal, J.N. (2012).
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by The Bradshaw Foundation – includes discussion on Toba eruption, DNA and human migrations
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Self, Stephen; Blake, Stephen (February 2008). "Consequences of Explosive Supereruptions".
6374: 6336: 6293: 6245: 6191: 6102: 6067: 6030: 5999: 5946: 5825: 5782: 5709: 5676: 5632: 5456: 5292: 5237: 5162: 4980: 4851: 4669: 4488: 4403: 4348: 4293: 4237: 4181: 4125: 4055: 3773: 3679: 3605: 3533: 3481: 3414: 3357: 3318: 3251: 3240:"New insights into the ~ 74 ka Toba eruption from sulfur isotopes of polar ice cores" 3208: 3142: 3092: 3034: 2985: 2938: 2891: 2844: 2797: 2758: 2692: 2645: 2634:"Rapid sea-level fall and deep-ocean temperature change since the last interglacial period" 2596: 2502: 2437: 2426:"Multiple carbon cycle mechanisms associated with the glaciation of Marine Isotope Stage 4" 2372: 2305: 2254: 2207: 2155: 2107: 2010: 1947: 1886: 1825: 1767: 1720: 1673: 1626: 1595: 1556: 1486: 1402: 1352: 1264: 1214: 1059: 1004: 952: 873: 453: 162: 143:(Potentially) almost all of humanity, leaving around 3,000–10,000 humans left on the planet 6281: 5661: 3789: 3378: 2243:"Compiled Southern Ocean sea surface temperatures correlate with Antarctic Isotope Maxima" 1522: 8: 6824: 6681: 820: – Most recent individual from which all organisms in a group are directly descended 606: 568:
of six to ten years and contributed to a 1,000-year-long cooling episode, resulting in a
351: 130: 6658: 6549: 6513: 6440: 6407: 6378: 6340: 6297: 6249: 6195: 6106: 6071: 6034: 6003: 5950: 5829: 5786: 5713: 5697: 5680: 5636: 5618: 5460: 5321: 5296: 5280: 5241: 5166: 5009: 4984: 4968: 4855: 4673: 4632: 4492: 4407: 4352: 4297: 4241: 4185: 4129: 4059: 3683: 3609: 3546: 3485: 3418: 3361: 3322: 3255: 3212: 3146: 3096: 3038: 2989: 2942: 2895: 2848: 2801: 2762: 2696: 2600: 2506: 2441: 2401: 2376: 2309: 2258: 2211: 2159: 2111: 2049: 2014: 1998: 1951: 1890: 1829: 1771: 1724: 1677: 1630: 1599: 1583: 1560: 1490: 1406: 1356: 1268: 1218: 1063: 1008: 956: 877: 367:, microscopic glass shards from this eruption are also discovered on the south coast of 6890: 6616: 6261: 6226: 6207: 6172: 6138: 6126: 6046: 5978: 5848: 5814:"Mobile Elements Reveal Small Population Size in the Ancient Ancestors of Homo Sapiens" 5390: 5126: 5091: 5066: 5033: 4944: 4911: 4882: 4839: 4812: 4779: 4748: 4716:"Inferring human population size and separation history from multiple genome sequences" 4715: 4559:"Insights into human genetic variation and population history from 929 diverse genomes" 4527: 4476: 4442: 4391: 4109: 4079: 4039: 4013: 3954: 3942: 3888: 3853: 3705: 3629: 3529: 3445: 3402: 3383: 3287: 3058: 3003: 2721: 2680: 2466: 2425: 2341: 1970: 1935: 1756:"New occurrence of Youngest Toba Tuff in abyssal sediments of the Central Indian Basin" 1090: 1047: 1028: 924: 602: 364: 227: 6079: 5920: 5889: 5150: 4113: 3403:"Global climate disruption and regional climate shelters after the Toba supereruption" 2657: 1779: 6598: 6588: 6487: 6452: 6309: 6265: 6158: 6142: 6118: 6007: 5970: 5962: 5925: 5874: 5853: 5800: 5725: 5648: 5472: 5394: 5326: 5308: 5261: 5253: 5186: 5178: 5131: 5113: 5071: 5053: 5014: 4996: 4949: 4931: 4887: 4869: 4817: 4799: 4753: 4735: 4693: 4685: 4637: 4619: 4574: 4532: 4514: 4447: 4429: 4372: 4364: 4317: 4309: 4282:"Revised stratigraphy and chronology for Homo floresiensis at Liang Bua in Indonesia" 4261: 4253: 4205: 4197: 4149: 4141: 4071: 4021: 4005: 3946: 3908: 3858: 3840: 3801: 3793: 3754: 3746: 3709: 3697: 3633: 3621: 3497: 3450: 3432: 3291: 3279: 3160: 3108: 3062: 3050: 3007: 2954: 2907: 2879: 2860: 2832: 2813: 2726: 2708: 2661: 2614: 2565: 2557: 2518: 2490: 2471: 2453: 2406: 2388: 2333: 2294:"Direct linking of Greenland and Antarctic ice cores at the Toba eruption (74 ka BP)" 2270: 2241:
Anderson, H. J.; Pedro, J. B.; Bostock, H. C.; Chase, Z.; Noble, T. L. (2021-03-01).
2223: 2195: 2194:
Menviel, Laurie C.; Skinner, Luke C.; Tarasov, Lev; Tzedakis, Polychronis C. (2020).
2173: 2123: 2054: 2036: 1975: 1910: 1902: 1874: 1849: 1841: 1783: 1736: 1689: 1642: 1568: 1504: 1445: 1414: 1368: 1321: 1280: 1230: 1183: 1134: 1095: 1077: 1032: 1020: 968: 889: 757: 647: 590: 347: 215: 6321:
Robock, A.; Ammann, C.M.; Oman, L.; Shindell, D.; Levis, S.; Stenchikov, G. (2009).
6130: 5982: 5767:"Demographic histories and patterns of linkage disequilibrium in Chinese and Indian 5662:"Eruptive History of Earth's Largest Quaternary caldera (Toba, Indonesia) Clarified" 4336: 4225: 3958: 3387: 2903: 2856: 2770: 2514: 2345: 2266: 1499: 1474: 6742: 6553: 6517: 6477: 6444: 6411: 6382: 6344: 6301: 6253: 6211: 6199: 6150: 6110: 6075: 6050: 6038: 5954: 5915: 5905: 5843: 5833: 5790: 5717: 5684: 5640: 5464: 5382: 5316: 5300: 5245: 5170: 5121: 5103: 5061: 5045: 5004: 4988: 4939: 4923: 4877: 4859: 4807: 4791: 4743: 4727: 4677: 4627: 4611: 4566: 4522: 4504: 4496: 4437: 4419: 4411: 4356: 4301: 4245: 4189: 4133: 4083: 4063: 3977: 3938: 3900: 3876: 3848: 3832: 3785: 3736: 3687: 3613: 3489: 3440: 3422: 3373: 3365: 3326: 3269: 3259: 3239: 3216: 3150: 3100: 3079:
Jackson, Lily J.; Stone, Jeffery R.; Cohen, Andrew S.; Yost, Chad L. (2015-09-01).
3042: 2993: 2946: 2899: 2852: 2805: 2766: 2716: 2700: 2653: 2633: 2604: 2584: 2549: 2510: 2461: 2445: 2396: 2380: 2323: 2313: 2262: 2215: 2163: 2115: 2044: 2026: 2018: 1965: 1955: 1894: 1833: 1775: 1728: 1681: 1634: 1564: 1494: 1437: 1410: 1360: 1311: 1272: 1222: 1173: 1165: 1126: 1085: 1067: 1012: 960: 881: 789: 505: 500:
after the deposition of Toba ash, but cooling-forced aridity killed high elevation
485: 338: 191: 6697: 2553: 1732: 1252: 1114: 6580: 6521: 6448: 5991: 5910: 5492:"Newly Discovered Archaeological Sites in India Reveals Ancient Life before Toba" 5468: 3836: 3617: 3536:, Volcanic Hazards and Disasters in Human Antiquity, Floyd W. McCoy, Grant Heiken 3330: 3155: 3130: 2293: 2168: 2143: 1814:"Humans thrived in South Africa through the Toba eruption about 74,000 years ago" 1707:
Von Rad, Ulrich; Burgath, Klaus-Peter; Pervaz, Muhammad; Schulz, Hartmut (2002).
1685: 1316: 1299: 1276: 1130: 885: 684: 653: 565: 359: 6652: 5721: 4599: 3820: 3692: 3667: 1202: 4615: 4477:"The Simons Genome Diversity Project: 300 genomes from 142 diverse populations" 3989: 3985: 3981: 3973: 3926: 3884: 3880: 2704: 2489:
Doughty, Alice M.; Kaplan, Michael R.; Peltier, Carly; Barker, Stephen (2021).
2449: 2219: 2022: 1994: 1931: 1898: 1809: 1805: 1661: 1226: 861: 761: 679: 493: 461: 457: 440: 428: 416: 399: 67: 6692: 6602: 6415: 6177:"Volcanic Winter and Accelerated Glaciation following the Toba Super-eruption" 5660:
Chesner, C.A.; Westgate, J.A.; Rose, W.I.; Drake, R.; Deino, A. (March 1991).
5108: 5034:"Inference of human population history from individual whole-genome sequences" 4360: 4281: 4249: 4169: 4044:"Volcanic winter and accelerated glaciation following the Toba super-eruption" 3741: 3724: 3469: 2927:"Volcanic winter and accelerated glaciation following the Toba super-eruption" 2747:"The Southern Glacial Maximum 65,000 years ago and its Unfinished Termination" 1875:"Adaptive foraging behaviours in the Horn of Africa during Toba supereruption" 1813: 6864: 6664: 6646: 6154: 5966: 5476: 5412: 5312: 5257: 5225: 5182: 5117: 5057: 5000: 4935: 4873: 4803: 4739: 4689: 4657: 4623: 4578: 4518: 4433: 4368: 4313: 4257: 4201: 4145: 4075: 4009: 3912: 3844: 3797: 3750: 3701: 3625: 3501: 3493: 3436: 3283: 3112: 3054: 2958: 2911: 2864: 2817: 2712: 2665: 2618: 2561: 2522: 2457: 2392: 2360: 2337: 2274: 2227: 2177: 2144:"Timing and structure of the weak Asian Monsoon event about 73,000 years ago" 2127: 2040: 1906: 1845: 1787: 1740: 1693: 1646: 1508: 1372: 1325: 1284: 1234: 1187: 1138: 1081: 1024: 972: 940: 893: 700: 696: 436: 266: 265:
dated the eruption to 73,880 ± 320 and 73,700 ± 300 years ago. Five distinct
99: 86: 6482: 6465: 6305: 6114: 5838: 5795: 5766: 5304: 5249: 5174: 4992: 4864: 4681: 4137: 3427: 3345: 3264: 2681:"The configuration of Northern Hemisphere ice sheets through the Quaternary" 2609: 2384: 1960: 1072: 423:
20 (DO20), commonly explained by an abrupt reduction in the strength of the
6585:
When Humans Nearly Vanished: The Catastrophic Explosion of the Toba Volcano
6491: 6456: 6257: 6122: 5974: 5929: 5857: 5804: 5729: 5644: 5330: 5265: 5190: 5135: 5075: 5018: 4953: 4891: 4821: 4757: 4697: 4641: 4536: 4451: 4376: 4321: 4265: 4226:"Timing of archaic hominin occupation of Denisova Cave in southern Siberia" 4209: 4043: 3994:"Mismatch Distributions of mtDNA Reveal Recent Human Population Expansions" 3950: 3454: 3164: 3046: 2926: 2730: 2569: 2475: 2410: 2058: 1999:"Reversed Holocene temperature–moisture relationship in the Horn of Africa" 1979: 1914: 1853: 1340: 1099: 840: 772:, all expanded from very small populations around 70,000–55,000 years ago. 712: 708: 692: 674: 564:
The Toba catastrophe theory holds that the eruption caused a severe global
368: 343: 184: 6531:"Potential Atmospheric Impact of the Toba Mega-Eruption ~71,000 years ago" 6323:"Did the Toba Volcanic Eruption of ~74k BP Produce Widespread Glaciation?" 6313: 5652: 5386: 4153: 4025: 3862: 3805: 3758: 3197:"Potential atmospheric impact of the Toba Mega-Eruption ~71,000 years ago" 2972:
Huang, Chi-Yue; Zhao, Meixun; Wang, Chia-Chun; Wei, Ganjian (2001-10-15).
2318: 468:. Southern Hemisphere glaciation grew to its maximum extent during MIS 4. 6789: 6349: 6322: 5151:"Late Pleistocene Demography and the Appearance of Modern Human Behavior" 4838:
Henn, Brenna M.; Cavalli-Sforza, L. L.; Feldman, Marcus W. (2012-10-30).
3369: 3196: 2998: 2973: 741: 636: 501: 469: 415:
Greenland stadial 20 (GS20) is a millennium-long cold event in the north
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Thalman, O.; Fisher, A.; Lankester, F.; Pääbo, S.; Vigilant, L. (2007).
5049: 4558: 4509: 4500: 4305: 4193: 4017: 3993: 1837: 613:
supported her theory. In 1998, anthropologist Stanley H. Ambrose of the
6231:"Climate–Volcanism Feedback and the Toba Eruption of ~74,000 Years ago" 5996:
Comet/Asteroid Impacts and Human Society: an Interdisciplinary Approach
4570: 4415: 4170:"The timing and spatiotemporal patterning of Neanderthal disappearance" 3274: 2785: 2328: 2094:
Polyak, Victor J.; Asmerom, Yemane; Lachniet, Matthew S. (2017-09-01).
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National Geographic- Did early humans in India survive a supervolcano?
4424: 3220: 2809: 1153: 6203: 6042: 4067: 3104: 2950: 2119: 1614: 1429: 1364: 1169: 992: 642: 274: 244: 203: 195: 158: 56: 5540:"Supervolcano Eruption In Sumatra Deforested India 73,000 Years ago" 4927: 4795: 4731: 4337:"A new species of Homo from the Late Pleistocene of the Philippines" 3346:"Aerosol size confines climate response to volcanic super-eruptions" 2196:"An ice–climate oscillatory framework for Dansgaard–Oeschger cycles" 1441: 1046:
Storey, Michael; Roberts, Richard G.; Saidin, Mokhtar (2012-11-13).
908:"Surprisingly, Humanity Survived the Super-volcano 74,000 Years Ago" 3929:(1995). "Genetic Evidence for a Pleistocene Population Explosion". 3904: 3550: 1542: 1201:
Lubbers, Jordan; Kent, Adam J. R.; de Silva, Shanaka (2024-01-18).
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9 year interval, in Lake Malawi, show no cooling-induced change in
376: 372: 294: 5992:"The GGE Threat: Facing and Coping with Global Geophysical Events" 5442: 2877: 1659: 859: 552:, are investigated using state-of-art simulations provided by the 6427:) based on a population genetic meta-analysis of multiple loci". 4654: 3467: 765: 497: 473: 258: 207: 199: 77: 45: 991:
Ninkovich, D.; Sparks, R. S. J.; Ledbetter, M. T. (1978-09-01).
472:, Africa and Europe were characterized by increasingly cold and 3875: 3567:"Toba Supervolcano Not to Blame for Humanity's Near-Extinction" 3307:"Climate response to the Toba super-eruption: Regional changes" 2585:"Evolution of mean ocean temperature in Marine Isotope Stage 4" 1992: 832: – "Out of Africa" theory of the early migration of humans 797: 39: 5345:"Mount Toba Eruption – Ancient Humans Unscathed, Study Claims" 5149:
Powell, Adam; Shennan, Stephen; Thomas, Mark G. (2009-06-05).
3971: 3304: 3194: 1391:"A melt inclusion study of the Toba Tuffs, Sumatra, Indonesia" 452:
embarked on significant expansion and surpassed the extent of
6466:"The complex history of gorillas: insights from genomic data" 2786:"A climatic context for the out-of-Africa migration: COMMENT" 2582: 2423: 2193: 1997:; Haug, G. H.; Olago, D. O.; Sinninghe Damsté, J. S. (2023). 1428:
Scaillet, Bruno; Luhr, James F.; Carroll, Michael R. (2003),
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The Evolution and History of Human Populations in South Asia
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10.1130/0091-7613(1991)019<0200:EHOESL>2.3.CO;2
2678: 2536:
Hays, J. D.; Imbrie, John; Shackleton, N. J. (1976-12-10).
1526: 1341:"Dimensions and dynamics of co-ignimbrite eruption columns" 718: 631: 392: 4909: 3343: 2743: 2488: 1706: 965:
10.1130/0091-7613(2000)28<1056:talits>2.0.co;2
6387:
10.1130/0091-7613(1987)15<913:DOAITG>2.0.CO;2
6282:"Bottleneck in the Human Evolution and the Toba Eruption" 4837: 3400: 3020: 2240: 1871: 1151: 444: 277:
constraints on sulfur emission yielded a wide range from
5753:"Genetics and biogeography of East African chimpanzees ( 4778:
Terhorst, Jonathan; Kamm, John A.; Song, Yun S. (2017).
4473: 4334: 3236: 2631: 990: 618:
during which rapid human population expansion occurred.
6280:
Rampino, Michael R.; Self, Stephen (24 December 1993).
4222: 1754:
Pattan, J. N; Shane, Phil; Banakar, V. K (1999-03-01).
1472: 747: 479: 5088: 4966: 3513: 3511: 814: – Spread of humans from Africa through the world 699:
attained their lowest numbers around 70–80 kyr, while
4166: 4114:"Bottleneck in Human Evolution and the Toba Eruption" 3078: 2093: 1803: 297:
records estimate the sulfur emission on the order of
6360:"Dispersal of Ash in the Great Toba Eruption, 75 ka" 3889:"The Genetic Structure of Ancient Human Populations" 2784:
Stewart, John R.; Fenberg, Phillip B. (2018-05-01).
2535: 1581: 1300:"Petrogenesis of the Toba Tuffs, Sumatra, Indonesia" 779: 597:
of 1,000 to 10,000, sometime between 35 and 65 kyr.
27:
Volcanic supereruption 74,000 years ago in Indonesia
6727: 5936: 5148: 4596: 4389: 4090: 3508: 1582:Self, S.; Gouramanis, C.; Storey, M. (2019-12-01). 1427: 1200: 1045: 6688:Magma 'Pancakes' May Have Fueled Toba Supervolcano 5223: 1753: 1613:Chesner, Craig A.; Rose, William I. (1991-06-01). 843: – Line separating Asian and Australian fauna 252: 6502:Palaeogeography, Palaeoclimatology, Palaeoecology 6147:Volcanic Hazards and Disasters in Human Antiquity 5279:Muttoni, Giovanni; Kent, Dennis V. (2024-03-26). 3547:"Toba super-volcano catastrophe idea 'dismissed'" 2491:"A maximum in global glacier extent during MIS 4" 6862: 5994:. In Bobrowsky, Peter T.; Rickman, Hans (eds.). 5890:"Phylogeography and genetic ancestry of tigers ( 4777: 3666:Singh, Ajab; Srivastava, Ashok K. (2022-06-01). 3600:. Current Research on Prehistoric Central Asia. 2971: 1930: 1713:Geological Society, London, Special Publications 1389:Chesner, Craig A.; Luhr, James F. (2010-11-30). 938: 190:that occurred about 74,000 years ago during the 6528: 6085: 6020: 5818:Proceedings of the National Academy of Sciences 5764: 5590: 5285:Proceedings of the National Academy of Sciences 4973:Proceedings of the National Academy of Sciences 4912:"Estimating the mutation load in human genomes" 4844:Proceedings of the National Academy of Sciences 4713: 3665: 3407:Proceedings of the National Academy of Sciences 2365:Proceedings of the National Academy of Sciences 1940:Proceedings of the National Academy of Sciences 1052:Proceedings of the National Academy of Sciences 939:Bühring, Christian; Sarnthein, Michael (2000). 354:in a layer of 5 cm (2.0 in) ash, the 206:. It was the last in a series of at least four 6498: 6137: 5556: 3725:"Population size and protein variation in man" 2783: 1549:Journal of Volcanology and Geothermal Research 1395:Journal of Volcanology and Geothermal Research 1112: 410: 350:. The air-fall of this eruption blanketed the 333:, making this eruption the largest during the 6713: 6463: 5659: 3649:"The so-called Toba bottleneck didn't happen" 2140: 6320: 6279: 6225: 5739:"Human Ancestors Were an Endangered Species" 4714:Schiffels, Stephan; Durbin, Richard (2014). 1338: 668: 593:sequences dated a rapid growth from a small 214:of 8, making it the largest-known explosive 6357: 6171: 6057: 5869:. In Petraglia, M. D.; Allchin, B. (eds.). 5417:"At last, the death of the Toba bottleneck" 5278: 4108: 4038: 2925:Rampino, Michael R.; Self, Stephen (1992). 2924: 2359:Davtian, Nina; Bard, Edouard (2023-03-13). 2358: 1612: 1388: 1339:Woods, Andrew W.; Wohletz, Kenneth (1991). 621: 425:Atlantic meridional overturning circulation 6720: 6706: 6671:Geography Predicts Human Genetic Diversity 6617:Population Bottlenecks and Volcanic Winter 6358:Rose, W.I.; Chesner, C.A. (October 1987). 5811: 5411: 5204: 3722: 3128: 986: 984: 982: 918: 559: 308: 152: 38: 6481: 6393: 6348: 5919: 5909: 5887: 5847: 5837: 5794: 5601: 5372: 5320: 5125: 5107: 5065: 5008: 4943: 4881: 4863: 4811: 4747: 4631: 4526: 4508: 4441: 4423: 3852: 3740: 3723:Haigh, John; Smith, John Maynard (1972). 3691: 3444: 3426: 3377: 3273: 3263: 3154: 2997: 2720: 2608: 2465: 2400: 2327: 2317: 2167: 2048: 2030: 1969: 1959: 1498: 1315: 1207:Contributions to Mineralogy and Petrology 1179:2160/dba3b012-8369-4dbb-8a89-1102f11e92c3 1177: 1089: 1071: 726: 248:Location of Lake Toba shown in red on map 6653:Homepage of Professor Stanley H. Ambrose 6579: 5749: 5568: 5031: 3771: 1523:"Supersized eruptions are all the rage!" 243: 6422: 5989: 5760:(PhD). Harvard University, unpublished. 5736: 5695: 5616: 5579: 5208: 4096: 3818: 3774:"Allelic genealogy and human evolution" 3517: 2830: 1934:; Chorn, B. T.; Johnson, T. C. (2013). 1297: 1250: 1113:Channell, J.E.T.; Hodell, D.A. (2017). 979: 615:University of Illinois Urbana-Champaign 447:, Earth transitioned from interglacial 14: 6863: 6145:. In McCoy, F. W.; Heiken, G. (eds.). 5401:from the original on December 7, 2008. 5219: 5217: 4905: 4903: 4901: 4833: 4831: 4773: 4771: 4769: 4767: 4709: 4707: 4592: 4590: 4588: 4556: 4552: 4550: 4548: 4546: 4469: 4467: 4465: 4463: 4461: 3925: 3176: 3174: 3129:Yost, Chad; et al. (March 2018). 3074: 3072: 2200:Nature Reviews Earth & Environment 2189: 2187: 2089: 2087: 2085: 1867: 1865: 1863: 1468: 1466: 1246: 1244: 847: 830:Recent African origin of modern humans 609:and volcanologist Stephen Self of the 427:(AMOC). Weaker AMOC caused warming in 391:, Toba tephras is found in Huguangyan 6701: 5864: 3790:10.1093/oxfordjournals.molbev.a039995 3646: 3591: 3232: 3230: 3124: 3122: 2286: 2284: 1926: 1924: 1799: 1797: 1538: 1536: 1384: 1382: 934: 932: 6693:Youtube video "Stone Age Apocalypse" 6175:; Self, Stephen (2 September 1992). 4563:Yearbook of Paediatric Endocrinology 4392:"The first archaic Homo from Taiwan" 3564: 1515: 1434:Volcanism and the Earth's Atmosphere 748:Genetic bottlenecks in other mammals 480:Possible climate records of eruption 5698:"Pleistocene Population Explosions" 5214: 4898: 4828: 4764: 4704: 4585: 4543: 4458: 3171: 3069: 2638:Earth and Planetary Science Letters 2184: 2082: 1860: 1463: 1241: 744:and "other archaic human species". 519: 405: 24: 6573: 5498:. 25 February 2010. Archived from 5373:Sanderson, Katherine (July 2007). 5032:Li, Heng; Durbin, Richard (2011). 4032: 3943:10.1111/j.1558-5646.1995.tb02297.x 3672:Journal of Asian Earth Sciences: X 3640: 3592:Ge, Yong; Gao, Xing (2020-09-10). 3227: 3183:Modern Human Origins and Dispersal 3119: 3014: 2281: 2032:1854/LU-01HF6GN7WZQ65R3C82NK0HC57E 1921: 1794: 1533: 1379: 929: 532:of sulfur, which is 100 times the 435:, and this asynchrony is known as 358:in 1 mm (0.039 in), the 25: 6952: 6610: 6587:. Washington: Smithsonian Books. 318:Michigan Technological University 224:largest known explosive eruptions 5737:Gibbons, Ann (19 January 2010). 5595: 5584: 5573: 5562: 5550: 1569:10.1016/j.jvolgeores.2023.107879 1415:10.1016/j.jvolgeores.2010.06.001 796: 782: 240:List of large volcanic eruptions 6931:Volcanic eruptions in Indonesia 6729:Volcanic eruptions in Indonesia 6470:Molecular Biology and Evolution 6328:Journal of Geophysical Research 5696:Gibbons, Ann (1 October 1993). 5532: 5523: 5514: 5483: 5436: 5427: 5405: 5366: 5337: 5272: 5197: 5142: 5082: 5025: 4960: 4648: 4383: 4328: 4272: 4216: 4160: 4102: 3965: 3919: 3869: 3812: 3778:Molecular Biology and Evolution 3765: 3716: 3659: 3647:Hawks, John (9 February 2018). 3585: 3565:Choi, Charles Q. 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Elsevier: 75–94. 3097:2015Geo....43..823J 3039:2002QuRes..57...22S 3027:Quaternary Research 2990:2001GeoRL..28.3915H 2943:1992Natur.359...50R 2896:2019QSRv..204..187D 2849:2014QSRv...86..115H 2802:2018Geo....46E.442S 2763:2015QSRv..114...52S 2697:2019NatCo..10.3713B 2601:2021CliPa..17.2273S 2589:Climate of the Past 2548:(4270): 1121–1132. 2507:2021QSRv..26106948D 2442:2022NatCo..13.5443M 2377:2023PNAS..12009558D 2371:(12): e2209558120. 2310:2013CliPa...9..749S 2298:Climate of the Past 2259:2021QSRv..25506821A 2212:2020NRvEE...1..677M 2160:2019QuGeo..5301003D 2112:2017Geo....45..843P 2073:Quaternary Sciences 2015:2023Natur.620..336B 1952:2013PNAS..110.8025L 1891:2024Natur.628..365K 1838:10.1038/nature25967 1830:2018Natur.555..511S 1772:1999MGeol.155..243P 1725:2002GSLSP.195..445V 1678:2012QuInt.258..119P 1631:1991BVol...53..343C 1600:2019AGUFM.V51H0141S 1561:2023JVGR..44107879K 1491:2023QSRv..31208162L 1407:2010JVGR..197..259C 1357:1991Natur.350..225W 1269:2012QuInt.258....5C 1219:2024CoMP..179...12L 1064:2012PNAS..10918684S 1058:(46): 18684–18688. 1009:1978BVol...41..286N 957:2000Geo....28.1056B 878:2012QuInt.258..119P 848:Citations and notes 629:At least two other 607:New York University 510:foraging behaviours 502:afromontane forests 470:Australasian region 441:Heinrich stadial 7a 352:Indian subcontinent 263:argon–argon datings 131:Indian subcontinent 96: /  6665:Journey of Mankind 4610:(5): 923–939.e14. 4571:10.1530/ey.17.14.4 4416:10.1038/ncomms7037 3530:Michael R. Rampino 3474:Journal of Climate 1810:Lane, Christine S. 1804:Smith, Eugene I.; 1639:10.1007/BF00280226 1017:10.1007/BF02597228 711:across the entire 603:Michael R. Rampino 570:genetic bottleneck 365:Sub-Saharan Africa 348:Straits of Malacca 250: 177:Toba supereruption 100:2.6845°N 98.8756°E 6941:Asahan Toba basin 6876:Extinction events 6858: 6857: 6629:on April 22, 2011 6567:on July 18, 2011. 6558:10.1029/96GL00706 6101:(5834): 114–116. 6029:(5688): 574–577. 6013:978-3-540-32709-7 5959:10.1111/mec.12716 5939:Molecular Ecology 5904:(12): 2275–2293. 5880:978-1-4020-5561-4 5781:(5822): 240–243. 5421:john hawks weblog 5381:: news070702–15. 5236:(6661): 979–984. 5044:(7357): 493–496. 4668:(5834): 114–116. 4487:(7624): 201–206. 4347:(7751): 181–186. 4292:(7599): 366–369. 4236:(7741): 594–599. 4180:(7514): 306–309. 3978:Harpending, Henry 3729:Genetics Research 3653:john hawks weblog 3221:10.1029/96GL00706 2984:(20): 3915–3918. 2810:10.1130/g40057c.1 2009:(7973): 336–343. 1946:(20): 8025–8029. 1885:(8007): 365–372. 1824:(7697): 511–515. 1351:(6315): 225–227. 760:, central Indian 758:Bornean orangutan 591:mitochondrial DNA 339:pyroclastic flows 222:, and one of the 216:volcanic eruption 169: 168: 161:is the resulting 16:(Redirected from 6948: 6936:Volcanic winters 6881:Geology theories 6722: 6715: 6708: 6699: 6698: 6638: 6636: 6634: 6625:. 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2120:10.1130/G39149.1 2091: 2080: 2069: 2063: 2062: 2052: 2034: 1990: 1984: 1983: 1973: 1963: 1928: 1919: 1918: 1869: 1858: 1857: 1801: 1792: 1791: 1751: 1745: 1744: 1704: 1698: 1697: 1657: 1651: 1650: 1610: 1604: 1603: 1579: 1573: 1572: 1540: 1531: 1530: 1529:. 28 April 2005. 1519: 1513: 1512: 1502: 1470: 1461: 1460: 1459: 1458: 1425: 1419: 1418: 1401:(1–4): 259–278. 1386: 1377: 1376: 1365:10.1038/350225a0 1336: 1330: 1329: 1319: 1295: 1289: 1288: 1248: 1239: 1238: 1198: 1192: 1191: 1181: 1170:10.1002/jqs.3149 1164:(1–2): 256–271. 1149: 1143: 1142: 1110: 1104: 1103: 1093: 1075: 1043: 1037: 1036: 988: 977: 976: 936: 927: 922: 916: 915: 904: 898: 897: 857: 806: 801: 800: 792: 790:Volcanoes portal 787: 786: 685:selective sweeps 551: 549: 543: 541: 531: 529: 520:Climate modeling 506:Middle Stone Age 498:grassy woodlands 406:Climatic effects 304: 302: 292: 290: 284: 282: 192:Late Pleistocene 156: 111: 110: 108: 107: 106: 101: 97: 94: 93: 92: 89: 66:c. 74,000 years 42: 30: 29: 21: 6956: 6955: 6951: 6950: 6949: 6947: 6946: 6945: 6926:VEI-8 eruptions 6886:Human evolution 6861: 6860: 6859: 6854: 6807: 6760: 6731: 6726: 6632: 6630: 6621: 6613: 6595: 6576: 6574:Further reading 6571: 6564: 6533: 6373:(10): 913–917. 6362: 6335:(D10): D10107. 6272: 6233: 6218: 6190:(6390): 50–52. 6179: 6165: 6090: 6014: 5892:Panthera tigris 5881: 5708:(5130): 27–28. 5664: 5612: 5607: 5600: 5596: 5589: 5585: 5578: 5574: 5567: 5563: 5555: 5551: 5538: 5537: 5533: 5528: 5524: 5519: 5515: 5505: 5503: 5502:on 22 July 2011 5490: 5488: 5484: 5441: 5437: 5432: 5428: 5415:(5 July 2007). 5410: 5406: 5371: 5367: 5358: 5356: 5343: 5342: 5338: 5277: 5273: 5222: 5215: 5202: 5198: 5147: 5143: 5087: 5083: 5030: 5026: 4965: 4961: 4928:10.1038/nrg3931 4908: 4899: 4836: 4829: 4796:10.1038/ng.3748 4784:Nature Genetics 4776: 4765: 4732:10.1038/ng.3015 4720:Nature Genetics 4712: 4705: 4653: 4649: 4595: 4586: 4555: 4544: 4472: 4459: 4388: 4384: 4333: 4329: 4277: 4273: 4221: 4217: 4165: 4161: 4107: 4103: 4095: 4091: 4054:(6390): 50–52. 4037: 4033: 3990:Stoneking, Mark 3986:Jenkins, Trefor 3982:Soodyall, Himla 3974:Rogers, Alan R. 3970: 3966: 3927:Rogers, Alan R. 3924: 3920: 3885:Stoneking, Mark 3881:Rogers, Alan R. 3874: 3870: 3817: 3813: 3770: 3766: 3721: 3717: 3664: 3660: 3645: 3641: 3590: 3586: 3575: 3573: 3571:Livescience.com 3556: 3554: 3553:. 30 April 2013 3545: 3544: 3540: 3528: 3524: 3516: 3509: 3466: 3462: 3399: 3395: 3342: 3338: 3303: 3299: 3235: 3228: 3193: 3189: 3179: 3172: 3127: 3120: 3077: 3070: 3019: 3015: 2970: 2966: 2937:(6390): 50–52. 2923: 2919: 2876: 2872: 2829: 2825: 2782: 2778: 2742: 2738: 2677: 2673: 2630: 2626: 2581: 2577: 2534: 2530: 2487: 2483: 2422: 2418: 2357: 2353: 2289: 2282: 2239: 2235: 2206:(12): 677–693. 2192: 2185: 2139: 2135: 2092: 2083: 2070: 2066: 1991: 1987: 1929: 1922: 1870: 1861: 1806:Jacobs, Zenobia 1802: 1795: 1752: 1748: 1705: 1701: 1658: 1654: 1611: 1607: 1580: 1576: 1541: 1534: 1521: 1520: 1516: 1471: 1464: 1456: 1454: 1452: 1442:10.1029/139gm02 1426: 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R. 6135: 6083: 6055: 6018: 6012: 5987: 5934: 5885: 5879: 5862: 5809: 5762: 5747: 5734: 5693: 5675:(3): 200–203. 5657: 5631:(6): 623–651. 5613: 5611: 5608: 5606: 5605: 5594: 5583: 5572: 5561: 5549: 5531: 5522: 5513: 5482: 5435: 5426: 5404: 5365: 5336: 5271: 5213: 5196: 5141: 5096:Genome Biology 5081: 5024: 4959: 4922:(6): 333–343. 4897: 4827: 4790:(2): 303–309. 4763: 4726:(8): 919–925. 4703: 4647: 4584: 4542: 4457: 4382: 4327: 4271: 4215: 4159: 4124:(5142): 1955. 4101: 4089: 4031: 4004:(5): 761–775. 3964: 3937:(4): 608–615. 3918: 3905:10.1086/204195 3899:(4): 483–496. 3868: 3831:(4): 649–663. 3811: 3764: 3715: 3658: 3639: 3584: 3582: 3581: 3538: 3522: 3507: 3460: 3393: 3336: 3297: 3226: 3207:(8): 837–840. 3187: 3170: 3118: 3091:(9): 823–826. 3068: 3013: 2964: 2917: 2870: 2823: 2776: 2736: 2671: 2624: 2575: 2528: 2481: 2416: 2351: 2304:(2): 749–766. 2280: 2233: 2183: 2133: 2106:(9): 843–846. 2081: 2064: 1985: 1920: 1859: 1793: 1766:(3): 243–248. 1760:Marine Geology 1746: 1719:(1): 445–461. 1699: 1652: 1625:(5): 343–356. 1605: 1574: 1532: 1514: 1462: 1450: 1420: 1378: 1331: 1310:(3): 397–438. 1290: 1240: 1193: 1144: 1105: 1038: 1003:(3): 286–298. 978: 928: 917: 899: 851: 849: 846: 845: 844: 838: 833: 827: 821: 815: 808: 807: 793: 777: 774: 749: 746: 728: 725: 680:founder effect 670: 667: 626: 620: 581: 578: 561: 558: 521: 518: 481: 478: 462:Northeast Asia 458:eastern Europe 437:bipolar seesaw 429:Southern Ocean 417:Atlantic ocean 412: 409: 407: 404: 400:resurgent dome 310: 307: 259:summer monsoon 254: 251: 235: 232: 167: 166: 157: 149: 148: 145: 144: 141: 135: 134: 127: 123: 122: 119: 113: 112: 75: 71: 70: 64: 60: 59: 54: 50: 49: 43: 35: 34: 26: 9: 6: 4: 3: 2: 6953: 6942: 6939: 6937: 6934: 6932: 6929: 6927: 6924: 6922: 6919: 6917: 6914: 6912: 6909: 6907: 6904: 6902: 6899: 6897: 6894: 6892: 6889: 6887: 6884: 6882: 6879: 6877: 6874: 6872: 6869: 6868: 6866: 6850: 6847: 6844: 6841: 6838: 6837:Anak Krakatoa 6835: 6832: 6829: 6826: 6823: 6820: 6817: 6816: 6814: 6810: 6803: 6800: 6797: 6794: 6791: 6788: 6785: 6782: 6779: 6776: 6773: 6772:Mount Tambora 6770: 6769: 6767: 6763: 6756: 6753: 6750: 6747: 6744: 6741: 6740: 6738: 6734: 6730: 6723: 6718: 6716: 6711: 6709: 6704: 6703: 6700: 6694: 6691: 6689: 6686: 6683: 6679: 6676: 6672: 6669: 6666: 6663: 6660: 6657: 6654: 6651: 6649: 6648: 6647:The Economist 6644:– Article in 6643: 6640: 6628: 6624: 6620: 6618: 6615: 6614: 6604: 6600: 6596: 6590: 6586: 6582: 6578: 6577: 6563: 6559: 6555: 6551: 6547: 6543: 6539: 6532: 6527: 6523: 6519: 6515: 6511: 6507: 6503: 6497: 6493: 6489: 6484: 6479: 6475: 6471: 6467: 6462: 6458: 6454: 6450: 6446: 6442: 6438: 6434: 6430: 6426: 6421: 6417: 6413: 6409: 6405: 6401: 6397: 6392: 6388: 6384: 6380: 6376: 6372: 6368: 6361: 6356: 6351: 6346: 6342: 6338: 6334: 6330: 6329: 6324: 6319: 6315: 6311: 6307: 6303: 6299: 6295: 6291: 6287: 6283: 6278: 6271: 6267: 6263: 6259: 6255: 6251: 6247: 6243: 6239: 6232: 6228: 6224: 6217: 6213: 6209: 6205: 6201: 6197: 6193: 6189: 6185: 6178: 6174: 6170: 6166: 6164:0-8137-2345-0 6160: 6156: 6152: 6148: 6144: 6140: 6136: 6132: 6128: 6124: 6120: 6116: 6112: 6108: 6104: 6100: 6096: 6089: 6084: 6081: 6077: 6073: 6069: 6065: 6061: 6056: 6052: 6048: 6044: 6040: 6036: 6032: 6028: 6024: 6019: 6015: 6009: 6005: 6001: 5997: 5993: 5988: 5984: 5980: 5976: 5972: 5968: 5964: 5960: 5956: 5952: 5948: 5944: 5940: 5935: 5931: 5927: 5922: 5917: 5912: 5907: 5903: 5899: 5895: 5893: 5886: 5882: 5876: 5872: 5868: 5863: 5859: 5855: 5850: 5845: 5840: 5835: 5831: 5827: 5823: 5819: 5815: 5810: 5806: 5802: 5797: 5792: 5788: 5784: 5780: 5776: 5772: 5770: 5763: 5759: 5756: 5752: 5748: 5744: 5740: 5735: 5731: 5727: 5723: 5719: 5715: 5711: 5707: 5703: 5699: 5694: 5690: 5686: 5682: 5678: 5674: 5670: 5663: 5658: 5654: 5650: 5646: 5642: 5638: 5634: 5630: 5626: 5625: 5620: 5615: 5614: 5603: 5598: 5592: 5587: 5581: 5576: 5570: 5569:Goldberg 1996 5565: 5558: 5553: 5545: 5541: 5535: 5526: 5517: 5501: 5497: 5493: 5486: 5478: 5474: 5470: 5466: 5462: 5458: 5454: 5450: 5446: 5439: 5430: 5422: 5418: 5414: 5408: 5400: 5396: 5392: 5388: 5384: 5380: 5376: 5369: 5355:on 2008-01-11 5354: 5350: 5346: 5340: 5332: 5328: 5323: 5318: 5314: 5310: 5306: 5302: 5298: 5294: 5290: 5286: 5282: 5275: 5267: 5263: 5259: 5255: 5251: 5247: 5243: 5239: 5235: 5231: 5227: 5220: 5218: 5210: 5206: 5200: 5192: 5188: 5184: 5180: 5176: 5172: 5168: 5164: 5160: 5156: 5152: 5145: 5137: 5133: 5128: 5123: 5119: 5115: 5110: 5105: 5101: 5097: 5093: 5085: 5077: 5073: 5068: 5063: 5059: 5055: 5051: 5047: 5043: 5039: 5035: 5028: 5020: 5016: 5011: 5006: 5002: 4998: 4994: 4990: 4986: 4982: 4978: 4974: 4970: 4963: 4955: 4951: 4946: 4941: 4937: 4933: 4929: 4925: 4921: 4917: 4913: 4906: 4904: 4902: 4893: 4889: 4884: 4879: 4875: 4871: 4866: 4861: 4857: 4853: 4849: 4845: 4841: 4834: 4832: 4823: 4819: 4814: 4809: 4805: 4801: 4797: 4793: 4789: 4785: 4781: 4774: 4772: 4770: 4768: 4759: 4755: 4750: 4745: 4741: 4737: 4733: 4729: 4725: 4721: 4717: 4710: 4708: 4699: 4695: 4691: 4687: 4683: 4679: 4675: 4671: 4667: 4663: 4659: 4651: 4643: 4639: 4634: 4629: 4625: 4621: 4617: 4613: 4609: 4605: 4601: 4593: 4591: 4589: 4580: 4576: 4572: 4568: 4564: 4560: 4553: 4551: 4549: 4547: 4538: 4534: 4529: 4524: 4520: 4516: 4511: 4506: 4502: 4498: 4494: 4490: 4486: 4482: 4478: 4470: 4468: 4466: 4464: 4462: 4453: 4449: 4444: 4439: 4435: 4431: 4426: 4421: 4417: 4413: 4409: 4405: 4401: 4397: 4393: 4386: 4378: 4374: 4370: 4366: 4362: 4358: 4354: 4350: 4346: 4342: 4338: 4331: 4323: 4319: 4315: 4311: 4307: 4303: 4299: 4295: 4291: 4287: 4283: 4275: 4267: 4263: 4259: 4255: 4251: 4247: 4243: 4239: 4235: 4231: 4227: 4219: 4211: 4207: 4203: 4199: 4195: 4191: 4187: 4183: 4179: 4175: 4171: 4163: 4155: 4151: 4147: 4143: 4139: 4135: 4131: 4127: 4123: 4119: 4115: 4111: 4105: 4098: 4093: 4085: 4081: 4077: 4073: 4069: 4065: 4061: 4057: 4053: 4049: 4045: 4041: 4035: 4027: 4023: 4019: 4015: 4011: 4007: 4003: 3999: 3998:Human Biology 3995: 3991: 3987: 3983: 3979: 3975: 3968: 3960: 3956: 3952: 3948: 3944: 3940: 3936: 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799: 794: 791: 785: 780: 773: 771: 767: 763: 759: 755: 745: 743: 739: 734: 724: 721: 720: 714: 710: 709:Alu sequences 705: 702: 701:Yoruba people 698: 697:Maasai people 694: 689: 686: 681: 676: 666: 664: 660: 656: 655: 654:H. luzonensis 650: 649: 644: 640: 639: 634: 633: 625: 619: 616: 612: 608: 604: 598: 596: 592: 587: 577: 575: 571: 567: 557: 555: 535: 517: 513: 511: 507: 503: 499: 495: 491: 487: 477: 476:environment. 475: 471: 467: 463: 459: 455: 450: 446: 442: 438: 434: 430: 426: 422: 418: 403: 401: 396: 394: 390: 386: 382: 378: 375:of northwest 374: 370: 366: 361: 357: 353: 349: 345: 340: 336: 332: 328: 323: 319: 315: 306: 296: 276: 272: 268: 264: 260: 246: 241: 231: 229: 225: 221: 217: 213: 209: 205: 201: 197: 193: 189: 186: 185:supervolcanic 182: 178: 174: 173:Toba eruption 164: 160: 155: 150: 146: 142: 140: 136: 132: 128: 124: 120: 118: 114: 109: 79: 76: 72: 69: 65: 61: 58: 55: 51: 47: 41: 36: 31: 19: 6849:Mount Marapi 6819:Mount Merapi 6812:21st century 6802:Mount Marapi 6645: 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Retrieved 3541: 3525: 3518:Ambrose 1998 3477: 3473: 3463: 3410: 3406: 3396: 3353: 3349: 3339: 3314: 3310: 3300: 3247: 3243: 3204: 3200: 3190: 3182: 3138: 3134: 3088: 3084: 3033:(1): 22–31. 3030: 3026: 3016: 2981: 2977: 2967: 2934: 2930: 2920: 2887: 2883: 2873: 2840: 2836: 2826: 2793: 2789: 2779: 2754: 2750: 2739: 2688: 2684: 2674: 2641: 2637: 2627: 2592: 2588: 2578: 2545: 2541: 2531: 2498: 2494: 2484: 2433: 2429: 2419: 2368: 2364: 2354: 2301: 2297: 2250: 2246: 2236: 2203: 2199: 2151: 2147: 2136: 2103: 2099: 2076: 2072: 2067: 2006: 2002: 1988: 1943: 1939: 1882: 1878: 1821: 1817: 1763: 1759: 1749: 1716: 1712: 1702: 1669: 1665: 1655: 1622: 1618: 1608: 1591: 1587: 1577: 1552: 1548: 1517: 1482: 1478: 1455:, retrieved 1433: 1423: 1398: 1394: 1348: 1344: 1334: 1307: 1303: 1293: 1260: 1256: 1210: 1206: 1196: 1161: 1157: 1147: 1122: 1118: 1108: 1055: 1051: 1041: 1000: 996: 951:(11): 1056. 948: 944: 920: 911: 902: 869: 865: 855: 841:Wallace Line 751: 742:Neanderthals 730: 717: 713:human genome 706: 690: 675:Markov model 672: 652: 646: 637: 630: 628: 623: 599: 583: 563: 523: 514: 494:lake ecology 483: 414: 397: 369:South Africa 344:Indian Ocean 312: 275:Petrological 267:magma bodies 256: 180: 176: 172: 170: 129:Covered the 6833:(2017–2019) 6831:Mount Agung 6790:Mount Agung 6736:Before 1800 6476:: 146–158. 5506:28 February 5455:: 119–134. 4402:(1): 6037. 3784:(1): 2–22. 3356:(24): n/a. 3275:10023/24161 2890:: 187–207. 2843:: 115–143. 2796:(5): e442. 2691:(1): 3713. 2436:(1): 5443. 2329:2158/774798 1995:Lane, C. S. 1932:Lane, C. 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Index

Toba catastrophe theory

Sumatra
Toba Caldera Complex
BP
Sumatra
2°41′04″N 98°52′32″E / 2.6845°N 98.8756°E / 2.6845; 98.8756
VEI
Indian subcontinent
Deaths

Lake Toba
crater lake
supervolcanic
eruption
Late Pleistocene
Lake Toba
Sumatra
Indonesia
caldera
VEI
volcanic eruption
Quaternary
largest known explosive eruptions
Earth's history
List of large volcanic eruptions

summer monsoon
argon–argon datings
magma bodies

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