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Shallow Hydrothermal Fluids Shape Microbial Dynamics at the Tagoro Submarine Volcano (Canary Islands, Spain)
Clàudia Pérez-Barrancos1,2, Eugenio Fraile-Nuez1, Juan Pablo Martín-Díaz1,3
1Centro Oceanográfico de Canarias, Instituto Español de Oceanografía, Consejo Superior de Investigaciones Científicas (IEO-CSIC), Santa Cruz de Tenerife, Spain.
Shallow hydrothermal vents boost marine life! Nutrients from underwater volcanoes significantly increase phytoplankton and bacteria, enhancing primary production and element cycling in ocean surface waters.
Area of Science:
- Marine Biology
- Oceanography
- Geochemistry
Background:
- Shallow underwater hydrothermal systems are crucial yet understudied marine environments.
- The Tagoro submarine volcano provides a unique, long-term model for investigating diffuse hydrothermal fluid impacts.
Purpose of the Study:
- To assess the effects of Tagoro's hydrothermal fluids on phytoplankton and bacterial communities.
- To understand how these inputs influence primary production and biogeochemical cycling in shallow waters.
Main Methods:
- Experimental manipulation of hydrothermal fluid dilution levels.
- Monitoring of chlorophyll a concentration, picoeukaryote and Synechococcus abundances.
- Analysis of phytoplankton and bacterial community composition shifts.
Main Results:
- Chlorophyll a concentrations doubled with hydrothermal enrichment, peaking earlier than controls.
- Small eukaryotic phytoplankton, dinoflagellates, diatoms, and radiolarians showed increased abundance.
- Both phototrophic and chemoautotrophic bacteria benefited, indicating enhanced microbial activity.
Conclusions:
- Shallow hydrothermal systems significantly enhance primary production via phototrophic microbes.
- Hydrothermal inputs stimulate microbial communities, influencing nutrient and element cycling.
- Protistan grazing and parasitism play key roles in regulating these planktonic communities.
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