interstadial การใช้

• Interstadial climate may have been relatively warm but this is not necessarily so.
• The " Backed Point " lithics of Federmesser culture are usually dated in the Aller鴇 Interstadial.
• The interstadial ended abruptly with a cold period that reduced temperatures back to near-glacial levels within a decade.
• In regions where it is not observed, the B鴏ling-Aller鴇 is considered a single interstadial ( warm ) period.
• During an interstadial, the southern montane metapopulation and the one to the north which ranged across the Eurasian taiga split.
• In some regions, especially in northern Eurasia, there is evidence for a cold period known as the Older Dryas interrupting the interstadial.
• In contrast, during interglacial and interstadial periods, more effective coupling occurred between the surface drainage network and the internal karst drainage system.
• In some regions, a cold period known as the Older Dryas can be detected in the middle of the B鴏ling-Aller鴇 interstadial.
• The upper part of this ice-rich unit contains pollen associated with dense grass-dominated tundra, which is indicative of interstadial environments.
• A zone of peaty deposits within this ice complex accumulated during a Middle Weichselian interstadial about 40, 000 to 30, 000 years ago.
• A late Pleistocene period of warm climate ( an interstadial ) was named for the lake based on evidence gathered here ( see B鴏ling oscillation ).
• These glacial features are related to Lake Agassiz, and were deposited about 9, 500 to 10, 000 years ago during the Timiskaming Interstadial.
• This was an interstadial Northern Iberia ( to the mouth of the Douro river ), as well as the Muge Culture in the Tagus valley.
• When this interstadial period ended, with the onset of the Younger Dryas, many of these species were forced to migrate south or become regionally extinct.
• During the B鴏ling Aller鴇 Period, known in Britain as the Windermere interstadial, the northern coast of Doggerland began to recede as global sea levels rose.
• In the case of the Veiki moraines of Sweden, the interstadial during which the lagoons sedimented is believed to have occurred in the early Weichsel glaciation.
• The Aller鴇 occurred during the last interstadial of the Pleistocene : the Windermere of Britain, the Woodgrange of Ireland and the Two Creeks Interval of North America.
• In such regions the shorter oscillation ending with the Older Dryas is known as the B鴏ling oscillation, and the Aller鴇 period is the interstadial following the Older Dryas.
• Also, as the period leading up to the Preboreal Oscillation was interstadial to interglacial, the thermohaline circulation would have been more stable than during the Younger Dryas.
• However, on stratigraphic grounds, we think that it is safe to say that they should be dated to the Late Saalian Zeifen Interstadial ( MIS 6.01 ).