概括
河口沉积物中的同位素揭示了过去的盐度和河流流量. 这种方法应用于旧金山湾,重建了数千年的海平面变化和河流排放情况.
科学领域:
- 地质化学 地质化学
- 古海洋学是古海洋学.
- 同位素地球化学 同位素地球化学
背景情况:
- 生物性沉中的同位素作为古盐度的代理.
- 像旧金山湾这样的河口系统涉及河水和海水的混合,其中具有明显的成分.
- 了解这些混合动态对于古气候重建至关重要.
研究的目的:
- 研究同位素作为河口沉积物中古盐度指标的实用性.
- 评估同位素组成,盐度和河流排放率之间的关系.
- 重建旧金山湾祖先的古盐度和环境变化.
主要方法:
- 在河口沉积物和水中分析的同位素组成 ((87) Sr / ((86) Sr) 和的度.
- 测量现代河口地表水,以验证混合模型.
- 同位素代理物应用于来自沉积物核心的类植物.
主要成果:
- 对于旧金山湾,盐度和同位素组成之间确立了明确的混合关系.
- 河水具有较低的 (87) Sr / (86) Sr比率 (0.7065) 和较低的Sr度 (0.13 ppm).
- 海水具有更高的 (87) Sr / (86) Sr比率 (0.7092) 和Sr度 (7.9 ppm).
结论:
- 同位素是古盐度和河流排放在河口环境中的可靠代理.
- 来自旧金山湾的古盐度记录反映了全球海平面波动和当地河流排放变化.
- 这种代码为河口的长期环境动态提供了有价值的见解.
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