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首页> 外文期刊>Quaternary Science Reviews: The International Multidisciplinary Review Journal >A new Dead Sea pollen record reveals the last glacial paleoenvironment of the southern Levant
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A new Dead Sea pollen record reveals the last glacial paleoenvironment of the southern Levant

机译:一个新的死海花粉记录揭示了南部黎兰的最后冰川古环境

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The southern Levant is a key region for studying vegetation developments in relation to climate dynamics and hominin migration processes in the past due to the sensitivity of the vegetation to climate variations and the long history of different anthropogenic occupation phases. However, paleoenvironmental conditions in the southern Levant during the Late Pleistocene were still insufficiently understood. Therefore, we investigated the vegetation and fire history of the Dead Sea region during the last glacial period. We present a new palynological study conducted on sediments of Lake Lisan, the last glacial precursor of the Dead Sea. The sediments were recovered from the center of the modern Dead Sea within an ICDP campaign. The palynological results suggest that Irano-Turanian steppe and Saharo-Arabian desert vegetation prevailed in the Dead Sea region during the investigated period (ca. 88,000 -14,000 years BP). Nevertheless, Mediterranean woodland elements significantly contributed to the vegetation composition, suggesting moderate amounts of available water for plants. The early last glacial was characterized by dynamic climate conditions with pronounced dry phases and high but unstable fire activity. Anatomically modern humans entered the southern Levant during a climatically stable phase (late MIS 4 MIS 3) with diverse habitats, constant moisture availability, and low fire activity. MIS 2 was the coldest phase of the investigated timeframe, causing changes in woodland composition and a widespread occurrence of steppe. We used a biome modeling approach to assess regional vegetation patterns under changing climate conditions and to evaluate different climate scenarios for the last glacial Levant. The study provides new insights into the environmental responses of the Dead Sea region to climate variations through time. It contributes towards our understanding of the paleoenvironmental conditions in the southern Levant, which functioned as an important corridor for
机译:由于植被对气候变化和不同人为职业阶段的漫长历史,南方利纳是研究与气候动态和母体迁移过程相关的关键地区,这些关键区域是过去植被的敏感性和不同人为占领阶段的漫长历史。然而,晚熟期间南方叶叶中的古环境条件仍然不够理解。因此,我们在最后的冰川期间调查了死海地区的植被和火灾历史。我们展示了在Lake Lisan Lake Lisan沉积物中进行的新的椎相论研究,死海的最后冰川前身。在ICDP活动中,从现代死海的中心回收了沉积物。 Palynological结果表明,在调查期间死海地区的伊朗 - 村草原和撒哈里亚 - 阿拉伯沙漠植被(约88,000 -14,000年BP)。尽管如此,地中海林地元素显着促成植被组成,表明植物中适量的可用水。最后的冰川早期的特点是动态气候条件具有明显的干阶段和高但不稳定的火灾活动。解剖学现代人类在稳定的阶段(晚期MIS 4 MIS 3)期间进入了南部的黎凡,具有多种栖息地,持续的水分可用性和低火活动。 MIS 2是调查时间框架最寒冷的阶段,导致林地组成的变化和普遍存在的草原发生。我们使用了生物群系建模方法来评估在不断变化的气候条件下的区域植被模式,并评估最后冰川利息的不同气候情景。该研究向死海地区的环境反应提供了新的洞察,通过时间来实现气候变化。它有助于了解南部黎班古环境条件,这是一个重要的走廊

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