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在工业化前的北大西洋中,大型的三角洲13C梯度被揭示出来
1Uni Bjerknes Centre, Allégaten 55, N-5007 Bergen, Norway. are.olsen@uni.no
概括
纠正人为引起的碳变化,揭示了原始的海洋碳同位素数据. 这些修订后的数据提供了对过去的海洋循环和气候变化的更清晰的了解.
科学领域:
- 古海洋学是古海洋学.
- 海洋地球化学 海洋地球化学
- 气候科学 气候科学
背景情况:
- 化石藻中的碳同位素组成 (δ(13) C) 是了解过去海洋通风的关键.
- 现代海洋的 δ(13) C 被人为二氧化碳改变,使历史解释复杂化.
- 北大西洋 (NA) δ(13) C 记录受到C-13 Suess效应的特别影响.
研究的目的:
- 为了纠正北大西洋的C-13苏斯效应.
- 揭示了北大西洋中原始的 δ(13) C 分布.
- 重新评估冰川 - 冰川间海洋 δ(13) C 差异及其与水体的关系.
主要方法:
- 碳同位素组成的分析 ((13) C/(12) C) 在化石菌中.
- 对北大西洋的海洋C-13苏斯效应进行校正.
- 校正的 δ(13) C 数据与现代水质分布的比较.
主要成果:
- 修正后的原始北大西洋 δ(13) C 分布表现出更详细的结构.
- 这种结构显示出与水质分布的关系比以前理解的更清楚.
- 对冰川 - 冰川间海洋 δ(13) C 差异的基本看法进行了修订.
结论:
- C-13苏斯效应显著影响了过去海洋碳同位素的解释.
- 纯 δ(13) C 数据为了解海洋通风提供了更准确的框架.
- 在现代气候变化的背景下,可以更好地理解古-δ(13) C 变化.
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