减少的碳和酸盐同化推动了藻元素固态度的变化,这种变化独立于铁有限组合中的化
Michael A Maniscalco1, Mark A Brzezinski2, Robert H Lampe3
1Marine Science Institute and The Department of Ecology Evolution and Marine Biology, University of California, Santa Barbara, CA, USA. mmaniscalco@ucsb.edu.
ISME communications
|November 8, 2023
概括
在藻中铁的限制改变了元素固态几何学,增加了与碳和相对的. 这是由于碳固定和同化减少而发生的,而不是由于生物质二氧化生产增加.
科学领域:
- 海洋生物学 海洋生物学
- 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:
- 溶解的铁 (Fe) 的可用性影响了加利福尼亚流生态系统中的植物浮游生物的生长.
- 铁的限制改变了藻中的元素固态几何学,影响了碳出口效率.
研究的目的:
- 了解在铁限制下改变藻体质的分子和生理驱动因素.
- 预测低铁含量如何影响藻碳出口.
主要方法:
- 人工上游试验与船上化.
- 治疗包括控制,溶解铁修改和由desferrioxamine-B (DFB) 诱导的铁限制.
- 单细胞,分类分辨的元素比例和基因表达的测量.
主要成果:
- 木占据了社区的主导地位,在+DFB处理中表现出铁限制特征,颗粒与碳 (Si:C) 和与 (Si:N) 的比率较高.
- 尽管载体和素-1的转录丰度增加,但生物 (bSi) 含量没有增加.
- 观察到的bSi相对于C和N的增加归因于碳固定和同化减少.
结论:
- 在藻中铁的限制导致Si:C和Si:N比率增加,主要是通过减少碳和的同化,而不是增加二氧化的产生.
- 关键的铁依赖基因的减少表达驱动了这些生理变化.
- 这些发现增强了对铁在藻碳出口中的作用的预测理解.
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