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Rapid Late Pleistocene climate change reconstructed from a lacustrine ostracod record in central Italy (Lake Trasimeno, Umbria)
Boreas ( IF 2.2 ) Pub Date : 2020-06-01 , DOI: 10.1111/bor.12450
Marta Marchegiano 1 , David J. Horne 2 , Elsa Gliozzi 3 , Alexander Francke 4 , Bernd Wagner 5 , Daniel Ariztegui 1
Affiliation  

An 8.59 m long sediment core was retrieved from Lake Trasimeno (central Italy) with the aim of performing a palaeoclimatic and palaeoenvironmental reconstruction. In this study we present, for the first time in central Italy, a quantitative palaeotemperatures reconstruction based on ostracod assemblages. The mean winter (January) and summer (July) palaeotemperatures were estimated from 44,000 to 9,000 cal yr BP by using the Mutual Ostracod Temperature Range (MOTR) method. Of the total of 19 ostracod species recovered, 13 of them were used as reliable palaeotemperature proxies on the base of their living temperature ranges.

中文翻译:

从意大利中部的湖相介形虫记录重建的快速晚更新世气候变化(特拉西梅诺湖,翁布里亚)

从特拉西梅诺湖(意大利中部)取回了一个 8.59 m 长的沉积岩心,目的是进行古气候和古环境重建。在这项研究中,我们首次在意大利中部展示了基于介形动物组合的定量古温度重建。冬季(1 月)和夏季(7 月)的平均古温度估计在 44,000 到 9,000 cal yr BP 之间,使用互斥温度范围 (MOTR) 方法。在恢复的总共 19 种介形虫中,其中 13 种被用作可靠的古温度代理,基于它们的生活温度范围。
更新日期:2020-06-01
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