北大西洋放射性碳储层在阿勒罗德和新德里亚斯期间的变化
Stein Bondevik1, Jan Mangerud, Hilary H Birks
1Department of Geology, University of Tromsø, N-9037 Tromsø, Norway. stein.bondevik@ig.uit.no
概括
来自挪威的海洋贝和植物遗骸的放射性碳测年揭示了在年轻德里亚斯 (YD) 气候事件期间海面水库年龄的变化. 水库年龄大幅波动,影响了气候记录的相关性.
科学领域:
- 古气候学 古气候学
- 通过放射性碳测年法进行测年.
- 海洋地球化学 海洋地球化学
背景情况:
- 准确的放射性碳测年法对海水的测年方法至关重要,它可以将四级纪晚期的海洋和陆地气候记录联系起来.
- 年轻的干旱 (YD) 是一个显著而突然的气候变化的时期,需要精确的年龄估计,用于古气候研究.
研究的目的:
- 为了确定四级末期的海面水库年龄,特别是年轻的干旱 (YD) 周围的寒冷时期.
- 评估挪威西海岸的海洋贝和陆地植物遗骸中放射性碳年龄的变化.
主要方法:
- 海洋贝和陆地植物遗骸的放射性碳测年.
- 分析了在11.000至14.000年前在挪威两个海湾沉积的样本.
- 海洋和陆地样本之间的放射性碳年龄的比较,以计算水库年龄.
主要成果:
- 在YD早期,海面水库的年龄从400年增加到600年.
- 水库的年龄在约900年内保持稳定.
- 在一个世纪内,在YD-Holocene过渡期内,水库年龄减少了300年.
结论:
- 海洋表面水库年龄的显著波动发生在YD和其过渡到Holocene期间.
- 这些年龄差异凸显了与海洋和陆地气候记录相关的复杂性.
- 了解这些水库年龄的变化对于完善后期四分期气候重建至关重要.
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