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The Preboreal-Boreal in Europe was a time of transition from the Palaeolithic cultures to the Mesolithic. Forests and drowned coastlands were places of plenty. Human settlements avoided the deep forest in favor of streams, lakes, and especially bays of the ocean. Pre-Boreal settlements have been found in north-central Europe, such as at ...
Blytt hypothesized that the darker layers were deposited in drier times and lighter in moister times, applying his terms Atlantic (warm, moist) and Boreal (cool, dry). In 1926 C. A. Weber [2] noticed the sharp boundary horizons, or Grenzhorizonte, in German peat, which matched Blytt's classification. Sernander defined the subboreal and ...
A boreal ecosystem is an ecosystem with a subarctic climate located in the Northern Hemisphere, approximately between 50° and 70°N latitude. These ecosystems are commonly known as taiga and are located in parts of North America, Europe, and Asia. [1] The ecosystems that lie immediately to the south of boreal zones are often called hemiboreal ...
It is preceded by the Tarantian and succeeded by the Boreal. It lasted from 10,300 to 9,000 BP in radiocarbon years or 8350 BC to 7050 BC in Gregorian calendar years (8th millennium BC). It is the first stage of the Holocene epoch. The preboreal oscillation was a short (ca. 150 years) cooling episode within the preboreal.
The subarctic climate (also called subpolar climate, or boreal climate) is a continental climate with long, cold (often very cold) winters, and short, warm to cool summers. It is found on large landmasses, often away from the moderating effects of an ocean, generally at latitudes from 50°N to 70°N, poleward of the humid continental climates .
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 [1] to distinguish it from Axel Blytt's Boreal, which had been established in 1876. [2]
Irruptive growth is a growth pattern over time, defined by a sudden rapid growth in the population of an organism. Irruptive growth is studied in population ecology. [1] Population cycles often display irruptive growth, but with a predictable pattern of subsequent decline. [2] It is a phenomenon typically associated with r-strategists.
The eastern forest–boreal transition is a temperate broadleaf and mixed forests ecoregion of North America, mostly in eastern Canada. It is a transitional zone or region between the predominantly coniferous Boreal Forest and the mostly deciduous broadleaf forest region further south.