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Last glacial period and Pollen zone

Shortcuts: Differences, Similarities, Jaccard Similarity Coefficient, References.

Difference between Last glacial period and Pollen zone

Last glacial period vs. Pollen zone

The last glacial period occurred from the end of the Eemian interglacial to the end of the Younger Dryas, encompassing the period years ago. Pollen zones are a system of subdividing the last glacial period and Holocene paleoclimate using the data from pollen cores.

Similarities between Last glacial period and Pollen zone

Last glacial period and Pollen zone have 13 things in common (in Unionpedia): Allerød oscillation, Bølling oscillation, Core sample, Flandrian interglacial, Holocene, Last glacial period, Mesolithic, Older Dryas, Oldest Dryas, Palynology, Pleistocene, Varve, Younger Dryas.

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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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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Core sample

A core sample is a cylindrical section of (usually) a naturally occurring substance.

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Flandrian interglacial

The Flandrian interglacial or stage is the name given by geologists and archaeologists in the British Isles to the first, and so far only, stage of the Holocene epoch (the present geological period), covering the period from around 12,000 years ago, at the end of the last glacial period to the present day.

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Holocene

The Holocene is the current geological epoch.

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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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Mesolithic

In Old World archaeology, Mesolithic (Greek: μέσος, mesos "middle"; λίθος, lithos "stone") is the period between the Upper Paleolithic and the Neolithic.

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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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Palynology

Palynology is the "study of dust" (from palunō, "strew, sprinkle" and -logy) or "particles that are strewn".

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Pleistocene

The Pleistocene (often colloquially referred to as the Ice Age) is the geological epoch which lasted from about 2,588,000 to 11,700 years ago, spanning the world's most recent period of repeated glaciations.

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Varve

A varve is an annual layer of sediment or sedimentary rock.

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Younger Dryas

The Younger Dryas (c. 12,900 to c. 11,700 years BP) was a return to glacial conditions which temporarily reversed the gradual climatic warming after the Last Glacial Maximum started receding around 20,000 BP.

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The list above answers the following questions

Last glacial period and Pollen zone Comparison

Last glacial period has 188 relations, while Pollen zone has 40. As they have in common 13, the Jaccard index is 5.70% = 13 / (188 + 40).

References

This article shows the relationship between Last glacial period and Pollen zone. To access each article from which the information was extracted, please visit:

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