Перевод и анализ слов искусственным интеллектом ChatGPT
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- этимология
Что (кто) такое interstadial {{Geology}} - определение
![The [[Ark Encounter]], Kentucky, 2016 representation of Noah's ark, operated by [[Answers in Genesis]], a [[young Earth creationist]] organization.](https://commons.wikimedia.org/wiki/Special:FilePath/Ark Encounter exterior.jpg?width=200 "The [[Ark Encounter]], Kentucky, 2016 representation of Noah's ark, operated by [[Answers in Genesis]], a [[young Earth creationist]] organization.")
![In the 18th century, finds such as [[Hutton's Unconformity]] showing layers tilted, eroded, and overlaid, demonstrated the "abyss of time" in the [[geologic time scale]].](https://commons.wikimedia.org/wiki/Special:FilePath/Hutton Unconformity , Jedburgh.jpg?width=200 "In the 18th century, finds such as [[Hutton's Unconformity]] showing layers tilted, eroded, and overlaid, demonstrated the \"abyss of time\" in the [[geologic time scale]].")
![Animals boarding Noah's ark, 1846 painting by [[Edward Hicks]].](https://commons.wikimedia.org/wiki/Special:FilePath/Noahs Ark.jpg?width=200 "Animals boarding Noah's ark, 1846 painting by [[Edward Hicks]].")
![angular unconformity]] found by [[James Hutton]] in 1788 at [[Siccar Point]] demonstrated the time taken for erosion of tilted rock and deposition of overlying layers.](https://commons.wikimedia.org/wiki/Special:FilePath/Siccar point SE cliff.jpg?width=200 "angular unconformity]] found by [[James Hutton]] in 1788 at [[Siccar Point]] demonstrated the time taken for erosion of tilted rock and deposition of overlying layers.")
Википедия
Stadials and interstadials are phases dividing the Quaternary period, or the last 2.6 million years. Stadials are periods of colder climate while interstadials are periods of warmer climate.
Each Quaternary climate phase is associated with a Marine Isotope Stage (MIS) number, which describe alternation between warmer and cooler temperatures as measured by oxygen isotope data. Stadials have even MIS numbers and interstadials odd MIS numbers. The current Holocene interstadial is MIS 1 and the Last glacial maximum stadial is MIS 2.
Marine Isotope Stages are sometimes further subdivided into stadials and interstadials by minor climate fluctuations within the overall stadial or interstadial regime, which are indicated by letters. The odd-numbered interstadial MIS 5, also known as the Sangamonian interglacial, contains two periods of relative cooling, and so is subdivided into three interstadials (5a, 5c, 5e) and two stadials (5b, 5d). A stadial isotope stage like MIS 6 would be subdivided by periods of relative warming, and so in that case the first and last subdivisions would be stadials; MIS 6a, 6c and 6e are stadials while 6b and 6d are interstadials.
