极端的生物驱动沉积物生物复杂性沿着pH梯度在浅海火山喷口的浅海火山喷口
C Andolina1, G Cilluffo1, V Zammuto2
1Department of Earth and Marine Sciences, University of Palermo, via Archirafi 18, 90123 Palermo, Italy; National Biodiversity Future Center (NBFC), Piazza Marina 61, 90133 Palermo, Italy; CoNISMa, National Interuniversity Consortium for Marine Sciences, Piazzale Flaminio 9, 00196 Roma, Italy.
Marine pollution bulletin
|December 22, 2024
概括
火山的二氧化碳排放改变了海底的有机物质和微生物群落. 这些由非生物梯度驱动的变化影响了更广泛的海洋食物网.
科学领域:
- 海洋生物地质化学海洋生物地质化学
- 微生物生态学 微生物生态学
- 火山学 火山学是一门学科.
背景情况:
- 浅浅的火山口释放二氧化碳,创造了独特的海洋环境.
- 这些通风口在海底建立了明显的非生物梯度.
- 了解这些梯度是海洋生态系统动态的关键.
研究的目的:
- 研究在火山CO2喷口附近有机物和 prokaryotic 社区的空间分布.
- 为了确定沉积物中的有机物质 (风源衍生或海洋衍生) 的来源.
- 将非生物梯度与有机物和微生物社区结构的变化联系起来.
主要方法:
- 元素分析 (C,N,C:N比率).
- 同位素分析 (δ13C, δ15N, δ34S).
- Prokaryotic 社区概况. 体社区概况.
主要成果:
- 喷口来源的有机物质 (微生物) 主导着喷口附近的沉积物.
- 海洋来源的有机物 (海草) 随着距离通风口的距离而增加.
- 在通风口附近,化学自营型的Campylobacterota和过热型的Archaea繁多;远处的光营养型和化学热营养型微生物占主导地位.
结论:
- 来自火山CO2喷口的非生物梯度显著改变了沉积物有机物组成和质量.
- 这些梯度塑造了相关 prokaryotic 社区的结构和复杂性.
- 这些发现对整个海洋食物网有影响.
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