在春季开花后的微生物再矿化过程中,在北波罗的海北部有过多的酸盐
Mari Vanharanta1,2, Mariano Santoro3,4, Cristian Villena-Alemany5
1Tvärminne Zoological Station, University of Helsinki, J. A. Palménin tie 260, 10900 Hanko, Finland.
FEMS microbiology ecology
|July 22, 2024
概括
微生物酶活动影响了波罗的海的循环. 碳和的添加转移了营养降解到与颗粒相关的细菌,可能会保留表面水中的营养.
科学领域:
- 海洋微生物生态学
- 海洋环境中的生物地化学循环.
背景情况:
- 在波罗的海的春季后开花中,的度正在上升.
- 这种多余 (P) 的命运和微生物过程的作用仍然不清楚.
研究的目的:
- 研究微生物降解在吸收多余中的作用.
- 检查碳 (C) 和 (N) 的修改如何影响微生物过程和P同化.
主要方法:
- 在波罗的海进行了为期17天的中宇宙实验.
- 测量了细胞外酶活动,细菌的丰富性,生产和社区组成,跨越尺寸分数.
- 应用的C和N修正单独和组合 (NC).
主要成果:
- 性酸酶活性主要被溶解,导致过量的酸盐.
- 最初,自由生活的细菌主导了酶生产.
- 通过NC处理,酶活性和单降解转移到与颗粒相关的部分.
结论:
- 微生物降解,特别是粒子相关细菌的降解,在循环中起着关键作用.
- 微生物活动的变化可能会增加地表水中的营养物质保留.
- 需要对沉积的进一步研究来证实营养保留假设.
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