The Piora Oscillation and the domesticated Horse

[bioblitzkrieg]

Piora Oscillation
From Wikipedia, the free encyclopedia

The Piora Oscillation was an abrupt cold and wet period in the climate history of the Holocene Epoch; it is generally dated to the period of c. 3500 to 3000 BCE.[1] Some researchers associate the Piora Oscillation with the end of the Atlantic climate regime, and the start of the Sub-Boreal, in the Blytt-Sernander sequence of Holocene climates.

The phenomenon is named after the Val Piora or Piora Valley in Switzerland, where it was first detected; some of the most dramatic evidence of the Piora Oscillation comes from the region of the Alps.[2] Glaciers advanced in the Alps, apparently for the first time since the Holocene climatic optimum; the Alpine tree line dropped by 100 meters. Yet the climate change extended far beyond the Alps and Europe. It affected what is now the New England region of North America, where hemlock and elm trees suffered a dramatic decline. Similar evidence comes from California and elsewhere; some changes in flora proved permanent. In the Middle East, the surface of the Dead Sea rose nearly 100 meters (300 feet), then receded to a more usual level. A few commentators have associated the climate changes of this period with the floods of the Gilgamesh epic and Noah's flood of the Book of Genesis.[3]

The Piora Oscillation has also been linked to the domestication of the horse. In Central Asia, a colder climate favored the use of horses: "The horse, since it was so adept at foraging with snow on the ground, tended to replace cattle and sheep."[4] The Piora period seems associated with a period of colder drier air over the Western and Eastern Mediterranean, and may have depressed rainfalls as far afield as the Middle East. It is also associated with a sudden onset of drier weather in the central Sahara. Ötzi, the frozen neolithic mummy found in Northern Italy, may also have been a victim of this climatic shift.

While much of the most blatant evidence of the Piora Oscillation relates to cold and flooding, the effects of the period were multifarious, and included a few centuries of general drought in East Africa.

The cause or causes of the Piora Oscillation are debated. A Greenland ice core, GISP2, shows a sulfate spike and methane trough c. 3250 BCE, suggesting an unusual occurrence — either a volcanic eruption or an meteor or asteroid impact event. Other authorities associate the Piora Oscillation with other comparable events, like the 8.2 kiloyear event, that recur in climate history, as part of a larger 1500-year climate cycle.