Abstract
The Toba eruption approximately 74,000 years ago was one of the largest volcanic events of the Quaternary and is often associated with the catastrophic hypothesis, which argues that the event caused extreme global cooling and severe reductions in human populations. However, recent studies suggest that its impacts were less destructive than previously assumed. This paper examines the position of Lida Ajer Cave within the context of the Toba eruption through a literature review of archaeological, geological, and paleoenvironmental publications. The review shows that the presence of Homo sapiens at Lida Ajer, dated to approximately 73,000–63,000 years ago, places the site within a timeframe closely associated with the Toba eruption. Although Lida Ajer lacks a direct stratigraphic association with the Youngest Toba Tuff (YTT), its chronological evidence, together with comparisons to the Jurreru Valley sites in India, provides a critical perspective on models proposing widespread human extinction caused by the eruption. This review highlights the importance of regional approaches for understanding the relationship between the Toba eruption, environmental change, and prehistoric human responses.
References
Ambrose, S. H. (1998). Late Pleistocene human population bottlenecks, volcanic winter, and differentiation of modern humans. Journal of Human Evolution, 34(6), 623–651. https://doi.org/10.1006/jhev.1998.0219
Anderson, H. E., Morley, M. W., McAdams, C., Zaim, J., Rizal, Y., Aswan, ... & Louys, J. (2024). The microstratigraphy and depositional environments of Lida Ajer and Ngalau Gupin, two fossil-bearing tropical limestone caves of west Sumatra. Scientific Reports, 14(1), 259. https://doi.org/10.1038/s41598-023-50501-8
Clarkson, C., Harris, C., Li, B., Neudorf, C. M., Roberts, R. G., Lane, C., Norman, K., Pal, J., Jones, S., Shipton, C., Koshy, J., Gupta, M. C., Mishra, D. P., Dubey, A. K., Boivin, N., & Petraglia, M. (2020). Human occupation of northern India spans the Toba super-eruption ~74,000 years ago. Nature Communications, 11(1). https://doi.org/10.1038/s41467-020-14668-4
Ge, Y., & Gao, X. (2020). Understanding the overestimated impact of the Toba volcanic super-eruption on global environments and ancient hominins. Quaternary International, 559, 24–33. https://doi.org/10.1016/j.quaint.2019.01.005
Louys, J., Albers, P. C. H., & Geer, A. van der. (2024). Quaternary palaeontology and archaeology of Sumatra. ANU Press.
Louys, J., Duval, M., Price, G. J., Westaway, K., Zaim, Y., Rizal, Y., ... & Roberts, P. (2022). Speleological and environmental history of Lida Ajer cave, western Sumatra. Philosophical Transactions of the Royal Society B: Biological Sciences, 377(1849). https://doi.org/10.1098/rstb.2021.0040
Mark, D. F., Petraglia, M., Smith, V. C., Morgan, L. E., Barfod, D. N., Ellis, B. S., Pearce, N. J., Pal, J. N., & Korisettar, R. (2014). 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, 90–103. https://doi.org/10.1016/j.quageo.2012.12.004
Oppenheimer, C. (2002). Limited global change due to the largest known Quaternary eruption, Toba ≈74 kyr BP? Quaternary Science Reviews, 21(14–15), 1593–1609. https://doi.org/10.1016/S0277-3791(01)00154-8
Petraglia, M. D., Korisettar, R., Boivin, N., Clarkson, C., Ditchfield, P., Jones, S., Koshy, J., Lahr, M. M., Oppenheimer, C., Pyle, D., Roberts, R., Schwenninger, J. L., Arnold, L., & White, K. (2007). Middle Paleolithic assemblages from the Indian subcontinent before and after the Toba super-eruption. Science, 317(5834), 114–116. https://doi.org/10.1126/science.1141564
Petraglia, M. D., Korisettar, R., & Pal, J. N. (2011). The Toba volcanic super-eruption of 74,000 years ago: Climate change, environments, and evolving humans. Quaternary International, 258, 1–4. https://doi.org/10.1016/j.quaint.2011.12.001
Pearce, N. J., Westgate, J. A., Gatti, E., Pattan, J. N., Parthiban, G., & Achyuthan, H. (2014). Individual glass shard trace element analyses confirm that all known Toba tephra reported from India is from the c. 75‐ka Youngest Toba eruption. Journal of Quaternary Science, 29(8), 729-734. https://doi.org/10.1002/jqs.2741
Pearce, N.J.G., Westgate, J.A., Gualda, G.A.R., Gatti, E. and Muhammad, R.F. (2020), Tephra glass chemistry provides storage and discharge details of five magma reservoirs which fed the 75 ka Youngest Toba Tuff eruption, northern Sumatra. J. Quaternary Sci., 35: 256-271. https://doi.org/10.1002/jqs.3149
Satyana, A. H., Hutagalung, R., & Latifah, U. (2013). Supererupsi Toba 74.000 tahun yang lalu: Katastrofi geologi dan kepunahan massa. In Proceedings HAGI-IAGI Joint Convention Medan (pp. 1-12). https://www.iagi.or.id/web/digital/8/2013_IAGI_Medan_Suoererupsi-Toba-74.000-Tahun.pdf
Smith, E. I., Jacobs, Z., Johnsen, R., Ren, M., Fisher, E. C., Oestmo, S., Wilkins, J., Harris, J. A., Karkanas, P., Fitch, S., Ciravolo, A., Keenan, D., Cleghorn, N., Lane, C. S., Matthews, T., & Marean, C. W. (2018). Humans thrived in South Africa through the Toba eruption about 74,000 years ago. Nature, 555(7697), 511–515. https://doi.org/10.1038/nature25967
Rampino, M. R., & Ambrose, S. H. (2000). Volcanic winter in the Garden of Eden: The Toba Supereruption and the late pleistocene human population crash. Volcanic Hazards and Disasters in Human Antiquity. https://doi.org/10.1130/0-8137-2345-0.71
Westaway, K., Louys, J., Awe, R. et al. An early modern human presence in Sumatra 73,000–63,000 years ago. Nature 548, 322–325 (2017). https://doi.org/10.1038/nature23452
Williams, M. A. J., Ambrose, S. H., van der Kaars, S., Ruehlemann, C., Chattopadhyaya, U., Pal, J., & Chauhan, P. R. (2009). Environmental impact of the 73ka toba super-eruption in South Asia. Palaeogeography, Palaeoclimatology, Palaeoecology, 284(3–4), 295–314. https://doi.org/10.1016/j.palaeo.2009.10.009
Yost, C. L., Jackson, L. J., Stone, J. R., & Cohen, A. S. (2018). Subdecadal phytolith and charcoal records from Lake Malawi, East Africa imply minimal effects on human evolution from the ∼74 ka Toba Supereruption. Journal of Human Evolution, 116, 75–94. https://doi.org/10.1016/j.jhevol.2017.11.005
Bahasa Abstract
Erupsi Gunung Toba sekitar 74.000 tahun lalu merupakan salah satu letusan vulkanik terbesar pada periode Kuarter dan sering dikaitkan dengan hipotesis katastrofik yang menyatakan bahwa peristiwa tersebut menyebabkan pendinginan global ekstrim serta penyusutan populasi manusia. Namun, penelitian terbaru menunjukkan bahwa dampak erupsi Toba kemungkinan tidak sedestruktif yang diperkirakan sebelumnya. Tulisan ini mengkaji posisi Situs Lida Ajer dalam konteks erupsi Toba melalui studi literatur terhadap berbagai publikasi arkeologi, geologi, dan paleoenvironment. Hasil kajian menunjukkan bahwa keberadaan Homo sapien di Lida Ajer yang berumur sekitar 73.000–63.000 tahun lalu menempatkan situs ini pada rentang waktu yang sangat dekat dengan erupsi Toba. Meskipun tidak memiliki hubungan stratigrafi langsung dengan endapan Youngest Toba Tuff (YTT), data kronologi dari Lida Ajer serta perbandingannya dengan situs Jurreru Valley di India memberikan perspektif kritis terhadap model kepunahan manusia secara menyeluruh akibat erupsi Toba. Kajian ini menunjukkan pentingnya pendekatan regional dalam memahami hubungan antara letusan Toba, perubahan lingkungan, dan respons manusia prasejarah.
Recommended Citation
Putri, Zulianikha S.; Nazirawati, Arni; and Fatima, Alia
(2026)
"SITUS LIDA AJER DALAM KONTEKS SUPERERUPSI ERUPSI TOBA,"
Multikultura: Vol. 5:
No.
3, Article 3.
DOI: 10.7454/multikultura.v5i3.1246
Available at:
https://scholarhub.ui.ac.id/multikultura/vol5/iss3/3
Included in
Archaeological Anthropology Commons, Human Geography Commons, Physical and Environmental Geography Commons