Subboreal

The Subboreal is a climatic period, immediately before the present one, of the Holocene. It lasted from 3710 to 450 BCE. The composite scientific term Subboreal, meaning 'below the Boreal,' is derived from the Latin sub (below, under) and the Greek Βορέας, from Boreas, the god of the North Wind. The word was first introduced in 1889 by Rutger Sernander to distinguish it from Axel Blytt's Boreal, which had been established in 1876. The Subboreal followed the Atlantic and was followed by the Subatlantic. The Subboreal is equivalent to W. H. Zagwijn's pollen zones IVa and IVb and T. Litt's pollen zone VIII. In the pollen scheme of Fritz Theodor Overbeck, it occupies pollen zone X. In paleoclimatology, it is divided into an Older Subboreal and a Younger Subboreal. Historically, the Subboreal is equivalent to most of the Neolithic and the entire Bronze Age, which started 4200 to 3800 years ago. The Subboreal is usually defined as 3710 to 5660 years BP. The lower limit is flexible, as some authors prefer to use 4400 BCE, or 6350 BP in northwestern Poland, even 4830 BC, or 6780 BP, And others use 5000 calendar years, or 3050 BCE. The upper limit of the Subboreal and, therefore the beginning of the Subatlantic, is also flexible and can be attributed to 1170 to 830 BCE, but it is usually fixed at 450 BCE. In varve years, the Subboreal corresponds to 5660 to 2750 years BP.