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Dryas is a genus of perennial cushion-forming evergreen dwarf shrubs in the family Rosaceae, native to the arctic and alpine regions of Europe, Asia and North America. The genus is named after the dryads , the tree nymphs of ancient Greek mythology .
Dryas octopetala, the mountain avens, [2] eightpetal mountain-avens, white dryas or white dryad, [3] is an Arctic–alpine flowering plant in the family Rosaceae. It is a small prostrate evergreen subshrub forming large colonies.
The Younger Dryas (YD, Greenland Stadial GS-1) [2] was a period in Earth's geologic history that occurred circa 12,900 to 11,700 years Before Present (BP). [3] It is primarily known for the sudden or "abrupt" cooling in the Northern Hemisphere, when the North Atlantic Ocean cooled and annual air temperatures decreased by ~3 °C (5.4 °F) over North America, 2–6 °C (3.6–10.8 °F) in Europe ...
Dryas integrifolia is a species of flowering plant in the rose family known by the common names arctic avens, [2] entireleaf mountain-avens, white mountain-avens, northern white mountain avens, [3] and mountain avens. [4] It is native to northern parts of North America, where it occurs from Alaska across Canada to Greenland.
Dryas drummondii is a species of flowering plant in the rose family known by the common names yellow mountain-avens, yellow dryas, or yellow dryad. [3] It is native to Alaska, Canada, and the Northern United States. [1] [3] This species is actinorhizal, able to live in symbiosis with nitrogen-fixing bacteria. [4] [5] [6] Dryas drummondii Richard
Articles relating to the Dryas, a genus of perennial cushion-forming evergreen dwarf shrubs in the family Rosaceae, native to the arctic and alpine regions of Europe, Asia and North America. The genus is named after the dryads , the tree nymphs of ancient Greek mythology .
It includes five genera (Dryas, Cercocarpus, Chamaebatia, Cowania, and Purshia), all of which except the first only occur in North America. Taxonomic history
The Younger Dryas impact hypothesis (YDIH) proposes that the onset of the Younger Dryas (YD) cool period at the end of the Last Glacial Period, around 12,900 years ago was the result of some kind of cosmic event with specific details varying between publications. [1]: Sec 1 The hypothesis is widely rejected by relevant experts.
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