Bacteria flourish in plumes of deep ocean volcanoes

low-res (4)

Source: HACON cruise 2021, REV Ocean

Deep down in the ocean at tectonic plate boundaries, hot fluids rise from so-called hydrothermal vents. The fluids are devoid of oxygen and contain large amounts of metals such as iron, manganese or copper. Some may also transport sulphides, methane and hydrogen.

 Registered users, subscribers or members - SIGN IN

To continue reading this article

Membership

Included as a benefit

Members of Applied Microbiology International have unlimited access to The Microbiologist as a benefit of membership. Just sign in with your usual membership credentials.

I AM A MEMBER

Find out more about how to join.

 

Register

FREE

Want to read more before deciding on a subscription? It only takes a minute to sign up for a free account and you’ll get to enjoy more free content each month.

REGISTER

 

Subscribe

3.75 per month / £35 annually

Get unlimited access to The Microbiologist.

SUBSCRIBE