4.2 kiloyear event

E89401

The 4.2 kiloyear event was a major global climatic downturn around 2200 BCE, marked by widespread aridification and cooling that is thought to have contributed to the collapse or transformation of several ancient civilizations.

Aliases (1)

Statements (53)
Predicate Object
instanceOf Holocene climatic anomaly
climatic event
affects East Asia
Eastern Mediterranean
Near East
North Africa
North Atlantic region
South Asia
alsoKnownAs 4.2 ka BP event
4.2 ka event
4.2 kyr event
associatedWith collapse of the Akkadian Empire
collapse of the Indus Valley Civilization
crop failures
decline of the Old Kingdom of Egypt
famine
societal stress and migration
transformations in Early Bronze Age societies in the Levant
urban abandonment in some regions
widespread drought
characterizedBy aridification
cooling
increased climate variability
chronologyMethod layer counting in ice cores
radiocarbon dating
classifiedAs global-scale climatic perturbation
duration several centuries
endTime circa 1900 BCE
hasCause changes in atmospheric circulation
shifts in monsoon systems
hasEvidence archaeological data
ice core records
lake sediment records
marine sediment cores
pollen records
speleothem records
impactOn Indus Valley urban centers
ancient Egyptian civilization
ancient Mesopotamian civilizations
pastoral and agricultural systems
partOf Holocene
recognizedBy archaeologists
geologists
paleoclimatologists
relatedTo 8.2 kiloyear event
Holocene climatic optimum
Little Ice Age
significance considered one of the most severe Holocene climate events
startTime circa 2200 BCE
timePeriod approximately 4.2 thousand years before present
around 2200 BCE
uncertainty spatial extent and exact mechanisms are debated
usedIn studies of climate–society interactions

Referenced by (5)

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