Unique Microbial Ecosystem Found In Red Sea Hydrothermal Vents By KAUST Researchers

Researchers from King Abdullah University of Science and Technology (KAUST) have uncovered a unique microbial ecosystem in the Hatiba Mons hydrothermal vent fields in the central Red Sea. Led by Prof. Alexandre Rosado, the study offers a detailed genome-resolved analysis of these vents, revealing both the types of microbes present and their metabolic functions. This site was initially discovered by Assistant Professor Froukje M. van der Zwan.

The research team reconstructed over 300 microbial genomes from five vent sites within the Hatiba Mons complex. They identified 314 microbial genomes, including previously unknown bacteria and archaea. These microbes demonstrate remarkable metabolic versatility, engaging in iron, sulfur, nitrogen, and carbon cycling. Such functions are crucial for chemical transformations that sustain life in extreme conditions.

Microbial Ecosystem Discovered in Red Sea Vents

Ph.D. student Sharifah Altalhi noted, "Microbes from the Hatiba Mons fields show remarkable metabolic versatility." The study highlights how geology and biology are interconnected in the Red Sea environment. The findings provide insights into how life shapes its surroundings through these intricate processes.

The Hatiba Mons fields were first documented in 2023 during a KAUST–GEOMAR expedition. This exploration revealed low-temperature venting zones and towering iron-oxide mounds at depths between 778 and 1,450 meters. These mounds represent the largest known active low-temperature iron-oxyhydroxide vent system globally.

Prof. Rosado remarked on the site's uniqueness: "What makes this site truly exceptional is the predominance of iron-driven metabolisms." Unlike typical hydrothermal vents that rely on sulfur or methane-based systems, Hatiba's iron-driven processes offer new insights into ocean resilience and global carbon cycling.

Implications for Earth and Beyond

The study underscores the importance of biogeochemical processes performed by these microbes, which are fundamental to Earth's systems. Their ability to oxidize and reduce iron, fix carbon, and metabolize sulfur and nitrogen links microbial activity to broader chemical cycles on our planet.

The research also suggests potential biotechnological applications such as metal recovery, bioenergy generation, and environmental remediation. Understanding these metabolic networks could inform future technologies aimed at addressing environmental challenges.

Moreover, studying how these organisms thrive in high-salinity, high-temperature environments provides clues about life's evolution on early Earth. It also hints at how life might exist under similar conditions elsewhere in our solar system.

With inputs from SPA

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