4.2-kiloyear event

abrupt climate change
Point in time	22. century BCE
Has characteristic	temperature

4.2 kiloyear (eya kputsun) bo aridification event (edagi eka wunciko), nan ah kpeye be 4.2 ka event'i nan, wun dan mini mini eka edagi nyan holocene epoch zhi'o^[1]. Wun baza nyan meghalayan mini holocene epoch'o..

Santatun

↑ deMenocal, Peter B. (2001). "Cultural Responses to Climate Change During the Late Holocene". https://en.wikipedia.org/wiki/Science_(journal)292 (5517): 667–673. Bibcode:https://ui.adsabs.harvard.edu/abs/2001Sci...292..667D.Doi.https://doi.org/10.1126%2Fscience.1059827. PMID 11303088 https://en.wikipedia.org/wiki/S2CID_(identifier)https://api.semanticscholar.org/CorpusID:18642937

[1] Menocal, Peter B. (2001). "Cultural Responses to Climate Change During the Late Holocene". https://en.wikipedia.org/wiki/Science_(journal)292 (5517): 667–673. Bibcode:https://ui.adsabs.harvard.edu/abs/2001Sci...292..667D.Doi.https://doi.org/10.1126%2Fscience.1059827. PMID 11303088 https://en.wikipedia.org/wiki/S2CID_(identifier)https://api.semanticscholar.org/CorpusID:18642937

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