液压压力诱导溶解有机物从"海洋雪"颗粒强烈泄漏
Peter Stief1, Jutta Niggemann2, Margot Bligh3
1HADAL & Nordcee, Department of Biology, University of Southern Denmark, Odense, Denmark.
Science advances
|February 4, 2026
概括
深海压力导致海雪释放溶解有机物 (DOM),影响碳捕获. 这种不稳定的DOM为微生物群落提供燃料,改变了海洋.
科学领域:
- 海洋生物学 海洋生物学
- 海洋学 海洋学 海洋学
- 生物地质化学生物地质化学
背景情况:
- 海洋雪由沉没的有机颗粒组成,在海洋的生物碳和碳封存中起着至关重要的作用.
- 原子聚合物是海洋雪的重要组成部分,迅速沉入深海.
- 增加的静水压力是沉降颗粒所遇到的关键环境因素.
研究的目的:
- 为了研究水静压对藻聚合物的溶解有机物 (DOM) 释放的影响.
- 描述压力诱导DOM的特性和生物可用性.
- 评估对碳循环和生物碳的影响.
主要方法:
- 在旋转压力中化藻聚合物,模拟深海条件.
- 使用超高分辨率质谱分析泄露的DOM.
- 通过蛋白质类光,C:N比率和微生物利用实验评估DOM可变性和生物利用性.
主要成果:
- 液压压力 (2-6公里深) 诱导了藻衍生DOM (初始碳的50%左右) 的显著泄漏.
- 泄露DOM的特征是不稳定,具有高蛋白状光和低C:N比率.
- 性微生物迅速消耗了泄漏的不稳定DOM,留下了反抗性的DOM.
结论:
- 由海雪引起的压力诱导的DOM泄漏会削弱生物碳.
- 这一过程为深海微生物群落提供了不稳定的有机物质.
- 了解海雪上的压力影响对于准确的碳循环建模至关重要.
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