贝加尔湖长沉积物核心的年龄
Alexander A Prokopenko1, Eugene B Karabanov, Douglas F Williams
1Department of Geological Sciences, University of South Carolina, Columbia, South Carolina 29208, USA. sasha@geol.sc.edu
Nature
|March 5, 2002
概括
贝加尔钻井项目BDP-98核心提供了一个罕见的亚洲古气候记录. 我们的石质分析表明,从其年龄模型中排除一个100米的段落是不合理的.
科学领域:
- 古气候学 古气候学
- 沉积地质学的地质学
- 亚洲的气候历史 亚洲的气候历史
背景情况:
- 贝加尔钻井项目BDP-98核心代表着一个关键的,长期的,连续的亚洲大陆古气候档案.
- 这样的高分辨率沉积物记录在全球范围内很少,这使得BDP-98对于重建过去的气候动态至关重要.
研究的目的:
- 从BDP-98核心的年龄模型中重新评估100米间隔的排除.
- 为了评估Kashiwaya等人对信号处理和年龄模型构建的有效性. 使用石质学分析.
主要方法:
- 详细地对BDP-98钻井核心部分进行了石化检查.
- 对沉积物学数据与现有年龄模型进行比较分析.
主要成果:
- 石器学研究表明,Kashiwaya等人切除的100米间隔. 不表现出错误数据的特征.
- 根据沉积物学证据,将这一重要部分排除在年龄模型之外被认为是不合理的.
结论:
- BDP-98古气候记录的完整性可能会因大量间隔的不合理切除而受到损害.
- 为了准确地重建古气候,需要对BDP-98年龄模型进行进一步的研究和可能的修订.
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