概括
在相当深处发现的化石美国 (Crassostrea virginica) 表明古代湖被海平面上升淹没. 这些发现可以追溯到8000到11000年前,是继最后一个冰川时期之后.
科学领域:
- 古生物学的古生物学
- 海洋生物学 海洋生物学
- 四年纪地质学四年纪地质学
背景情况:
- 美国,Crassostrea virginica,通常居住在较浅的河口环境中.
- 了解过去的海平面变化对于沿海生态系统研究至关重要.
研究的目的:
- 根据化石贝分布来研究Crassostrea virginica的古老环境.
- 确定古代种群的年龄及其与海平面波动的关系.
主要方法:
- 在71个站点系统地采集化石贝的样本.
- 收集的Crassostrea virginica贝的放射性碳测年代 (14C).
主要成果:
- 在14米至82米的深度发现了贝.
- 放射性碳测年法显示,的年龄在现在之前的8000到11000年之间.
- 发现贝的深度超过了这种物种典型的现代河口息地.
结论:
- Crassostrea virginica的贝表明存在水下湖或河口.
- 这些古老的环境因在最后一个冰川时代后海平面上升而被淹没.
- 这些发现提供了证据,证明研究区域的四次纪海平面变化显著.
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