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首页> 外文期刊>Quaternary Science Reviews: The International Multidisciplinary Review Journal >An early advance of glaciers on Mount Akda?, SW Turkey, before the global Last Glacial Maximum; insights from cosmogenic nuclides and glacier modeling
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An early advance of glaciers on Mount Akda?, SW Turkey, before the global Last Glacial Maximum; insights from cosmogenic nuclides and glacier modeling

机译:在全球末次冰河最高峰之前,土耳其西南部阿克达山的冰川提前发展。宇宙成因核素和冰川建模的见解

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摘要

For the first time in Turkey, we report an early advance of glaciers before the broadly defined global Last Glacial Maximum (LGM). Forty-one moraine boulders from three glacial valleys on Mount Akda? (36.54°N, 29.57°E, 3016 m), southwest coast of Turkey, were dated with cosmogenic ~(36)Cl. Valleys on the north side of the mountain were filled with few km long glaciers that terminated at elevations of about 2000 m above sea level (a.s.l). The pre-LGM glaciations reached their maximum positions (2150 m a.s.l) by 35.1 ± 2.5 ka ago (1σ; ka = 1000 calendar years). The glaciers readvanced during the global LGM and reached their farthest locations (2050 m a.s.l) by around 21.7 ± 1.2 ka ago. Later, glaciers retreated and shortly stabilized during the Lateglacial at around 15.1 ± 0.9 ka ago. Using the glacier modeling and paleoclimate proxies from the Eastern Mediterranean, we estimated that if temperatures during the LGM were 8-11 ℃ colder than modern, which is suggested by paleotemperature proxies from the region, precipitation was up to two times more than that of today. Previous estimates on southwest coast of Turkey indicate a similar precipitation value while central Turkey requires drier conditions, implying regional heterogeneity on LGM climates in Turkey.
机译:我们首次在土耳其报道了在广泛定义的全球“全球最大冰川”(LGM)之前冰川的早期发展。来自阿克达山三个冰川山谷的41个冰ora巨石? (36.54°N,29.57°E,3016 m),土耳其西南海岸,被定为具有宇宙成因的〜(36)Cl。这座山北侧的山谷充满了几公里长的冰川,这些冰川终止于海拔约2000 m的海拔。 LGM之前的冰川在35.1±2.5 ka以前(1σ; ka = 1000历年)达到了最大位置(2150 m a.s.l)。在全球LGM期间,冰川重新出现,并在21.7±1.2 ka之前到达最远的位置(2050 m a.s.l.)。后来,冰川在晚冰期退缩并稳定在15.1±0.9 ka之前。利用来自东地中海的冰川模型和古气候代理,我们估计,如果该地区的古温度代理表明,LGM期间的温度比现代温度低8-11℃,则该降水量最多是今天的两倍。 。先前对土耳其西南海岸的估计显示出相似的降水值,而土耳其中部则需要较干燥的条件,这意味着土耳其LGM气候存在区域异质性。

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