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波罗的海东部的Bølling-Allerød过渡:环境对气候变化的反应
Olga Druzhinina1, Anna Rudinskaya1, Ksenia Filippova1
1Faculty of Geography, Herzen State Pedagogical University of Russia, 191186 Saint-Petersburg, Russia.
Biology
|June 28, 2023
概括
这项研究重建了库利科沃部分的后期冰川环境动态,揭示了盆地演变的八个阶段. 波罗的海地区的先驱风景显示出复杂的变化,以应对短期气候波动.
科学领域:
- 古气候学 古气候学
- 四年纪地质学四年纪地质学
- 古生态学 古生态学
背景情况:
- 波罗的海地区的冰河后生物进化是很少理解的.
- 库利科沃部分暴露了来自冰川后盆地的晚期普莱斯托纪沉积物.
研究的目的:
- 重建在冰河后期 (Old Dryas-Allerød) 的当地环境系统动态.
- 了解生物对气候振荡的反应 (14,00013,400卡路里年BP).
主要方法:
- 地质时间学分析.
- 石化学分析 石化学分析
- 亚原子,异构动物学和古生物学分析.
主要成果:
- 确定了盆地演化的八个不同的阶段.
- 记录了水生和陆生生物种群的变化.
- 观察到从先驱植被到森林的继承.
结论:
- 库利科沃盆地的后期冰川环境非常动态.
- 短期气候波动对当地生态系统产生了重大影响.
- 开拓者景观复杂地演变,随着水文制度和植被模式的变化.
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