Historical impacts of climate change

Climate has affected human life and civilization from the emergence of hominins to the present day. These historical impacts of climate change can improve human life and cause societies to flourish, or can be instrumental in civilization's societal collapse.

Role in human evolution

Changes in East African climate have been associated with the evolution of hominins. Researchers have proposed that the regional environment transitioned from humid jungle to more arid grasslands due to tectonic uplift[1] and changes in broader patterns of ocean and atmospheric circulation.[2] This environmental change is believed to have forced hominins to evolve for life in a savannah-type environment. Some data suggest that this environmental change caused the development of modern homimin features; however there exist other data that show that morphological changes in the earliest hominins occurred while the region was still forested.[3] Rapid tectonic uplift likely occurred in the early Pleistocene,[2] changing the local elevation and broadly reorganizing the regional patterns of atmospheric circulation.[4][5] This can be correlated with the rapid hominin evolution of the Quaternary period.[1] Changes in climate at 2.8, 1.7, and 1.0 million years ago correlate well with observed transitions between recognized hominin species.[2] It is difficult to differentiate correlation from causality in these paleopanthropological and paleoclimatological reconstructions, so these results must be interpreted with caution and related to the appropriate time-scales and uncertainties.[6]

Historic and prehistoric societies

The rise and fall of societies have often been linked to environmental factors.[7]

Societal growth and urbanization

Approximately one millennium after the 7 ka slowing of sea-level rise, many coastal urban centers rose to prominence around the world.[8] It has been hypothesized that this is correlated with the development of stable coastal environments and ecosystems and an increase in marine productivity (also related to an increase in temperatures), which would provide a food source for hierarchical urban societies.[8]

Societal collapse

The last written records of the Norse Greenlanders are from a 1408 marriage in Hvalsey Church — today the best-preserved of the Norse ruins.

Climate change has been associated with the historical collapse of civilizations, cities and dynasties. Notable examples of this include the Anasazi,[9] Classic Maya,[10] the Harappa, the Hittites, and Ancient Egypt.[11] Other, smaller communities such as the Viking settlement of Greenland[12] have also suffered collapse with climate change being a suggested contributory factor.[13]

There are two proposed methods of Classic Maya collapse: environmental and non-environmental. The environmental approach uses paleoclimatic evidence to show that movements in the intertropical convergence zone likely caused severe, extended droughts during a few time periods at the end of the archaeological record for the classic Maya.[14] The non-environmental approach suggests that the collapse could be due to increasing class tensions associated with the building of monumental architecture and the corresponding decline of agriculture,[15] increased disease,[16] and increased internal warfare.[17]

The Harappa and Indus civilizations were affected by drought 4,500–3,500 years ago. A decline in rainfall in the Middle East and Northern India 3,800–2,500 is likely to have affected the Hittites and Ancient Egypt.

Historical era

Notable periods of climate change in recorded history include the Medieval warm period and the little ice age. In the case of the Norse, the Medieval warm period was associated with the Norse age of exploration and arctic colonization, and the later colder periods led to the decline of those colonies.[18]

See also

References

  1. 1 2 Gani, Nahid DS; Gani, M. Royhan; Abdelsalam, Mohamed G. (2007). "Blue Nile incision on the Ethiopian Plateau: Pulsed plateau growth, Pliocene uplift, and hominin evolution". GSA Today. 17 (9): 4. doi:10.1130/GSAT01709A.1.
  2. 1 2 3 Demenocal, P. B. (1995). "Plio-Pleistocene African Climate" (PDF). Science. 270 (5233): 53–9. Bibcode:1995Sci...270...53D. doi:10.1126/science.270.5233.53. PMID 7569951.
  3. ↑ Winfried Henke, Ian Tattersall (eds.); in collaboration with Thorolf Hardt. (2007). Handbook of paleoanthropology. New York: Springer. ISBN 978-3-540-32474-4.
  4. ↑ Sepulchre, P; Ramstein, G; Fluteau, F; Schuster, M; Tiercelin, Jj; Brunet, M (Sep 2006). "Tectonic uplift and Eastern Africa aridification". Science. 313 (5792): 1419–23. Bibcode:2006Sci...313.1419S. doi:10.1126/science.1129158. ISSN 0036-8075. PMID 16960002.
  5. ↑ Maslin, Ma; Christensen, B (Nov 2007). "Tectonics, orbital forcing, global climate change, and human evolution in Africa: introduction to the African paleoclimate special volume". Journal of Human Evolution. 53 (5): 443–64. doi:10.1016/j.jhevol.2007.06.005. ISSN 0047-2484. PMID 17915289.
  6. ↑ Behrensmeyer, Ak (Jan 2006). "Atmosphere. Climate change and human evolution". Science. 311 (5760): 476–8. doi:10.1126/science.1116051. ISSN 0036-8075. PMID 16439650.
  7. ↑ The Great Warming: Climate Change and the Rise and Fall of Civilizations. New York: Bloomsbury Press. 2008. ISBN 978-1-59691-392-9.
  8. 1 2 Day, John W.; Gunn, Joel D.; Folan, William J.; Yáñez-Arancibia, Alejandro; Horton, Benjamin P. (2007). "Emergence of Complex Societies After Sea Level Stabilized". Eos, Transactions, American Geophysical Union. 88 (15): 169. Bibcode:2007EOSTr..88..169D. doi:10.1029/2007EO150001.
  9. ↑ Demenocal, P. B. (2001). "Cultural Responses to Climate Change During the Late Holocene" (PDF). Science. 292 (5517): 667–673. Bibcode:2001Sci...292..667D. doi:10.1126/science.1059827. PMID 11303088.
  10. ↑ Hodell, David A.; Curtis, Jason H.; Brenner, Mark (1995). "Possible role of climate in the collapse of Classic Maya civilization". Nature. 375 (6530): 391. Bibcode:1995Natur.375..391H. doi:10.1038/375391a0.
  11. ↑ Jonathan Cowie (2007). Climate change: biological and human aspects. Cambridge University Press. ISBN 9781107603561.
  12. ↑ transl. with introd. by Magnus Magnusson ... (1983). The Vinland sagas: the Norse discovery of America. Harmondsworth, Middlesex: Penguin Books. ISBN 978-0-14-044154-3.
  13. ↑ Diamond, Jared (2005). Collapse: How Societies Choose to Fail or Succeed. Viking Adult. ISBN 0-670-03337-5.
  14. ↑ Haug, Gh; Günther, D; Peterson, Lc; Sigman, Dm; Hughen, Ka; Aeschlimann, B (Mar 2003). "Climate and the collapse of Maya civilization". Science. 299 (5613): 1731–5. Bibcode:2003Sci...299.1731H. doi:10.1126/science.1080444. ISSN 0036-8075. PMID 12637744.
  15. ↑ Hosler D, Sabloff JA, Runge D (1977). "Simulation model development: a case study of the Classic Maya collapse". In Hammond, Norman, Thompson, John L. Social process in Maya prehistory: studies in honour of Sir Eric Thompson. Boston: Academic Press. ISBN 0-12-322050-5.
  16. ↑ Santley, Robert S.; Killion, Thomas W.; Lycett, Mark T. (Summer 1986). "On the Maya Collapse". Journal of Anthropological Research. 42 (2): 123–59.
  17. ↑ Foias, Antonia E.; Bishop, Ronald L. (1997). "Changing Ceramic Production and Exchange in the Petexbatun Region, Guatemala: Reconsidering the Classic Maya Collapse". Ancient Mesoamerica. 8 (2): 275. doi:10.1017/S0956536100001735.
  18. ↑ Patterson, W.P.; Dietrich, K.A.; Holmden, C. (2007). Sea Ice and sagas: stable isotope evidence for two millennia of North Atlantic seasonality on the north Icelandic shelf. Arctic Natural Climate Change Workshop. Tromsø, Norway. CiteSeerX 10.1.1.132.4973Freely accessible.

Further reading

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