在东方赤道大西洋中,间歇性酸盐概况和沉积性有机物氧化
概括
在赤道大西洋的海洋沉积物显示出显著的酸盐减少. 这些海底沉积物中的脱可能是海洋循环的关键过程.
科学领域:
- 海洋地质学 海洋地质学
- 生物地质化学生物地质化学
- 海洋学 海洋学 海洋学
背景情况:
- 酸盐是海洋生态系统的关键营养素.
- 上游区域对于海洋生产力和营养循环至关重要.
- 沉积过程会影响海洋中的营养度和流量.
研究的目的:
- 调查孔水中酸盐度及其深度概况在东方赤道大西洋的海底沉积物中.
- 了解海洋沉积物中酸盐度,氧化还原区和脱之间的关系.
- 估计酸盐的底层流量及其对全球海洋酸盐预算的贡献.
主要方法:
- 从六个海底沉积物核心中分析孔水中酸盐度.
- 在沉积物柱内确定酸盐度梯度.
- 盆地酸盐流量和脱率的估计.
主要成果:
- 孔水中酸盐度从底水值增加到5厘米深处的峰值,然后下降到40厘米的不可检测水平.
- 酸盐度概况显示了氧气减少,酸盐减少和硫酸盐减少的不同区域.
- 估计的盆地酸盐流量低于全球流量到深水,尽管研究区域是一个上游区域.
结论:
- 位于赤道东部大西洋的海藻沉积物表现出显著的酸盐减少.
- 估计的脱率表明,这些沉积物在海洋脱中发挥着潜在的重要作用.
- 海洋沉积物,特别是在生产区,可能是从海洋中去除的重要地点.
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