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15 relations: Allerød oscillation, Atlantic (period), Bølling oscillation, Blytt–Sernander system, Boreal (age), Dual-phase evolution, Holocene climatic optimum, Interglacial, Last glacial period, Older Dryas, Oldest Dryas, Saksunarvatn tephra, Subboreal, Table of historic and prehistoric climate indicators, Timeline of environmental history.
Allerød oscillation
The Allerød oscillation (Allerødtiden) was a warm and moist global interstadial that occurred c.13,900 to 12,900 BP, nearly at the end of the last glacial period.
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Atlantic (period)
The Atlantic in palaeoclimatology was the warmest and moistest Blytt-Sernander period, pollen zone and chronozone of Holocene northern Europe.
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Bølling oscillation
The Bølling oscillation, also Bølling interstadial, was a cool temperate climatic interstadial between the glacial Oldest Dryas and Older Dryas stadials, between 14,700 and 14,100 BP, near to the end of the last glacial period.
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Blytt–Sernander system
The Blytt-Sernander classification, or sequence, is a series of north European climatic periods or phases based on the study of Danish peat bogs by Axel Blytt (1876) and Rutger Sernander (1908).
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Boreal (age)
In paleoclimatology of the Holocene, the Boreal was the first of the Blytt-Sernander sequence of north European climatic phases that were originally based on the study of Danish peat bogs, named for Axel Blytt and Rutger Sernander, who first established the sequence.
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Dual-phase evolution
Dual phase evolution (DPE) is a process that drives self-organization within complex adaptive systems.
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Holocene climatic optimum
The Holocene Climate Optimum (HCO) was a warm period during roughly the interval 9,000 to 5,000 years BP.
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Interglacial
An interglacial period (or alternatively interglacial, interglaciation) is a geological interval of warmer global average temperature lasting thousands of years that separates consecutive glacial periods within an ice age.
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Last glacial period
The last glacial period occurred from the end of the Eemian interglacial to the end of the Younger Dryas, encompassing the period years ago.
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Older Dryas
The Older Dryas was a stadial (cold) period between the Bølling and Allerød interstadials (warmer phases), about 14,000 years Before Present), towards the end of the Pleistocene. Its date is not well defined, with estimates varying by 400 years, but its duration is agreed to have been around 200 years. The gradual warming since the Last Glacial Maximum (27,000 to 24,000 years BP) has been interrupted by two cold spells: the Older Dryas and the Younger Dryas (c.
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Oldest Dryas
The Oldest Dryas was a climatic period, which occurred during the coldest stadial after the Weichselian glaciation in north Europe.
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Saksunarvatn tephra
In the science of tephrochronology, the Saksunarvatn tephra is volcanic ejecta that formed an ash layer that is useful in dating Northern European sediment layers that were laid down during the Boreal period, the warm climate phase that followed the cold snap of the Younger Dryas as the earth made the transition from the last Pleistocene glaciation to the current interglacial, or Holocene.
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Subboreal
The Subboreal is a climatic period, immediately before the present one, of the Holocene.
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Table of historic and prehistoric climate indicators
This table is a reference tool for rapidly locating Wikipedia articles on Historic and Prehistoric climate indicators of all types.
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Timeline of environmental history
The timeline lists events in the external environment that have influenced events in human history.
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