Allerod oscillation

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Allerod oscillation

[′al·ə‚räd ‚äs·ə′lā·shən]
(climatology)
A temporary increase in temperature during the closing stages of the Pleistocene ice age, dated in Europe about 9850-8850 B.C.
References in periodicals archive ?
Bottom sandy deposits from this period show a decrease in organics content and cover peat, gyttja and freshwater lime of Allerod age (Kabailiene 2006).