一个中欧十年的同位素气候记录,从15500年到5000年B.P.P
von Grafenstein U1, Erlenkeuser, Brauer
1Laboratoire des Sciences du Climat et de l'Environnement (LSCE), F-91198 Gif-sur-Yvette, France. Leibniz-Labor fur Altersbestimmung und Isotopenforschung der Universitat Kiel, Germany. Laboratoire de Botanique Historique et Palynologie, Faculte d.
概括
德国的一个湖泊.
科学领域:
- 古气候学 古气候学
- 四年纪地质学四年纪地质学
- 同位素地球化学 同位素地球化学
背景情况:
- 深湖鸟为过去的降水提供了高分辨率的代理.
- 乌的氧同位素比率 (delta18OP) 反映了气候的变化.
- 了解过去的气候变化对于预测未来的气候变化至关重要.
研究的目的:
- 为了重建过去的气候变化,使用来自德国阿默西的鸟衍生的delta18OP.
- 将欧洲气候记录与格陵兰冰芯数据进行比较.
- 调查北大西洋循环在脱冰过程中的作用.
主要方法:
- 分析来自Ammersee沉积物的鸟中的氧同位素比率.
- 十年分辨率的气候重建.
- 与已建立的气候记录进行比较 (例如,格陵兰岛的冰核).
主要成果:
- 阿默尔湖三角洲18OP记录显示了十年级的气候变化,反映了格陵兰岛冰芯记录在公元前15,000至5000年之间.
- 负的delta18OP外游与减弱的热环循环事件相关.
- 千年规模的趋势显示,欧洲和格陵兰之间的气候梯度在不断变化.
结论:
- 北大西洋的淡水排放可能导致热环流的短期减弱.
- 北大西洋循环的逐渐重新排列影响了欧洲-格陵兰岛在脱冰过程中的气候梯度.
- 湖为古气候学提供了宝贵的陆地气候档案.
相关概念视频
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