Younger Dryas

Ancient climate reversal

The Younger Dryas was a period of abrupt climate cooling that occurred roughly 12,900 to 11,700 years ago, interrupting the warming trend at the end of the last ice age.

Named after *Dryas octopetala*, an Arctic flower whose pollen reappeared in European sediments from this period.

The sudden cold snap lasted over a millennium before temperatures rose sharply again.

Scientists debate its cause—a leading theory involves disrupted Atlantic Ocean circulation from glacial meltwater.

The Younger Dryas shows how quickly climate can shift.

extinction

megafauna

Species over 44 kilograms

ground sloths · dire wolves · aurochs · extinction event · large mammals · woolly rhinoceros · paleoecology · ecosystem collapse · hunting pressure

geology

stratigraphy

Study of rock layers

alluvium · geochemistry · core samples · radiocarbon dating · paleomagnetism · geomorphology · boundary layer

glacial

glaciation

Ice sheet spreading process

tundra · moraine · drumlins · outwash · till · Greenland ice sheet · ice dam · meltwater · polar desert · esker

archaeology

hunter-gatherers

Subsistence through wild resources

artifacts · subsistence · Göbekli Tepe · human adaptation · migration patterns · population decline

climate

paleoclimatology

Study of prehistoric climates

transition

domestication

Adapting species to captivity

Categories
Opposites
climatic state

Younger Dryasinterglacial

Epoch between major freezes

ice age

climate transition type

Younger Dryassmooth transition

Gradual, unnoticeable change

Family

dryad, interglacial, Holocene

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