KnowraYounger DryasLinked fromLinked fromThe 33 pages that link to Younger Dryas, each with the reason it gives.All 33Broader topic 9Related 19Compared with 5Neolithic RevolutionRelated: Its abrupt climate change shaped conditions around early Southwest Asian cultivation.HoloceneRelated: Its abrupt end closely precedes the formal beginning of the Holocene.PaleoecologyRelated: Its ecological shifts are traced through fossils, pollen, and other environmental records.Quaternary extinction eventRelated: This abrupt climate episode overlaps with the final losses in some regions.Pollen analysisRelated: Pollen records document abrupt vegetation changes during this late-glacial cold interval.Laurentide Ice SheetRelated: Laurentide meltwater routing has been proposed as a contributor to this abrupt cooling.Clovis cultureRelated: Its timing overlaps proposed explanations for megafaunal extinction and changes in late Ice Age lifeways.MegafaunaRelated: Its timing overlaps with ecological changes and extinctions in some regions.Natufian cultureRelated: Its climatic shift overlapped with late Natufian lifeways and settlement changes.Glacial periodRelated: This abrupt return to cold conditions complicates the story of the last deglaciation.Mammoth SteppeRelated: This abrupt cooling coincided with major ecological shifts near the steppe’s end.Pre-Pottery NeolithicRelated: Its climate shifts may have influenced subsistence choices before early farming expanded.Lake AgassizRelated: A freshwater-drainage link to this cooling episode has been proposed but remains contested.Late Pleistocene extinctionsRelated: Its abrupt climate shift overlapped with late extinctions in some regions.Ground slothRelated: Its climate shifts overlap with the extinction period of surviving American ground sloths.Pre-Pottery Neolithic BRelated: Its end preceded the climatic conditions in which PPNB farming societies developed.Allerød oscillationRelated: Its onset marks the sharp cooling that ended the Allerød.EpipalaeolithicRelated: Its environmental fluctuations affected late Epipalaeolithic communities in parts of Southwest Asia.Prehistory of the LevantRelated: Its climatic stress coincided with major changes in Levantine settlement and subsistence.
KnowraYounger DryasLinked fromLinked fromThe 33 pages that link to Younger Dryas, each with the reason it gives.All 33Broader topic 9Related 19Compared with 5Neolithic RevolutionRelated: Its abrupt climate change shaped conditions around early Southwest Asian cultivation.HoloceneRelated: Its abrupt end closely precedes the formal beginning of the Holocene.PaleoecologyRelated: Its ecological shifts are traced through fossils, pollen, and other environmental records.Quaternary extinction eventRelated: This abrupt climate episode overlaps with the final losses in some regions.Pollen analysisRelated: Pollen records document abrupt vegetation changes during this late-glacial cold interval.Laurentide Ice SheetRelated: Laurentide meltwater routing has been proposed as a contributor to this abrupt cooling.Clovis cultureRelated: Its timing overlaps proposed explanations for megafaunal extinction and changes in late Ice Age lifeways.MegafaunaRelated: Its timing overlaps with ecological changes and extinctions in some regions.Natufian cultureRelated: Its climatic shift overlapped with late Natufian lifeways and settlement changes.Glacial periodRelated: This abrupt return to cold conditions complicates the story of the last deglaciation.Mammoth SteppeRelated: This abrupt cooling coincided with major ecological shifts near the steppe’s end.Pre-Pottery NeolithicRelated: Its climate shifts may have influenced subsistence choices before early farming expanded.Lake AgassizRelated: A freshwater-drainage link to this cooling episode has been proposed but remains contested.Late Pleistocene extinctionsRelated: Its abrupt climate shift overlapped with late extinctions in some regions.Ground slothRelated: Its climate shifts overlap with the extinction period of surviving American ground sloths.Pre-Pottery Neolithic BRelated: Its end preceded the climatic conditions in which PPNB farming societies developed.Allerød oscillationRelated: Its onset marks the sharp cooling that ended the Allerød.EpipalaeolithicRelated: Its environmental fluctuations affected late Epipalaeolithic communities in parts of Southwest Asia.Prehistory of the LevantRelated: Its climatic stress coincided with major changes in Levantine settlement and subsistence.