Last Glacial Maximum refugia

The Last Glacial Maximum map with vegetation types.

Last Glacial Maximum refugia were places (refugia) in which humans and other species survived during the Last Glacial Period, around 25,000 to 18,000 years ago.[1] Glacial refugia are areas that climate changes were not as severe, and where species could recolonize after deglaciation.[2]

Globally, the temperatures during the Last Glacial Maximum (LGM) were 4.0 ± 0.8 °C cooler than present day.[3] The colder climate contributed to ice sheet growth in North America, Europe, and Antarctica. At this time there were further major climate shifts around the world. Some areas became too dry to support much life; others housed more vegetation and animals.

The northern hemisphere was heavily impacted by ice sheets during the LGM. Some recent archaeological evidence suggests the possibility that human arrival in the Americas may have occurred prior to the Last Glacial Maximum more than 30,000 years ago. This evidence was found adjacent to ice sheets,[4] but research is still in an early stage. The best attested shelters are therefore mainly those in Eurasia. Aside from human habitation in the north, other animals and vegetation thrived in refugia south of ice sheets.

The southern hemisphere saw much less extensive glaciation, and outside Antarctica lacked continental ice sheet growth. Vast areas of Australia and Africa were too dry for human habitation of any sort,[5] even by the most specialized and well-adapted foragers. However, Sub-Saharan Africa was a refuge for many humans.[6] South America was not inhabited by humans during the LGM, but many other animals existed and thrived there.

  1. ^ Hampe, Arndt; Rodríguez-Sánchez, Francisco; Dobrowski, Solomon; Hu, Feng Sheng; Gavin, Daniel G. (2013). "Climate refugia: from the Last Glacial Maximum to the twenty-first century". The New Phytologist. 197 (1): 16–18. doi:10.1111/nph.12059. ISSN 0028-646X. PMID 23181681.
  2. ^ Stewart, John R.; Lister, Adrian M.; Barnes, Ian; Dalén, Love (2010-03-07). "Refugia revisited: individualistic responses of species in space and time". Proceedings of the Royal Society B: Biological Sciences. 277 (1682): 661–671. doi:10.1098/rspb.2009.1272. ISSN 0962-8452. PMC 2842738. PMID 19864280.
  3. ^ Annan, J. D.; Hargreaves, J. C. (2013-02-13). "A new global reconstruction of temperature changes at the Last Glacial Maximum". Climate of the Past. 9 (1): 367–376. Bibcode:2013CliPa...9..367A. doi:10.5194/cp-9-367-2013. ISSN 1814-9324.
  4. ^ Hoffecker, John F.; Elias, Scott A.; O'Rourke, Dennis H.; Scott, G. Richard; Bigelow, Nancy H. (2016). "Beringia and the Global Dispersal of Modern Humans". Evolutionary Anthropology: Issues, News, and Reviews. 25 (2): 64–78. doi:10.1002/evan.21478. PMID 27061035. Retrieved 2024-03-05.
  5. ^ Williams, Alan N.; Ulm, Sean; Cook, Andrew R.; Langley, Michelle C.; Collard, Mark (2013-12-01). "Human refugia in Australia during the Last Glacial Maximum and Terminal Pleistocene: a geospatial analysis of the 25–12 ka Australian archaeological record". Journal of Archaeological Science. 40 (12): 4612–4625. Bibcode:2013JArSc..40.4612W. doi:10.1016/j.jas.2013.06.015. ISSN 0305-4403.
  6. ^ Blinkhorn, James; Timbrell, Lucy; Grove, Matt; Scerri, Eleanor M. L. (2022-04-25). "Evaluating refugia in recent human evolution in Africa". Philosophical Transactions of the Royal Society B: Biological Sciences. 377 (1849). doi:10.1098/rstb.2020.0485. ISSN 0962-8436. PMC 8899617. PMID 35249393.