The Mid-Atlantic Ridge can be seen as the light-blue spine running down the centre of the Atlantic
https://commons.wikimedia.org/wiki/File:Atlantic_bathymetry.jpg
The Mid-Atlantic Ridge is a very volcanic environment. The sea-floor of this area is littered with hydrothermal vents which raise the sea temperature from near 0 degrees Celsius to up to 450 degrees. These sort of temperatures produce an environment so different from the rest of the underwater world that they harbour their own ecosystems. At these depths, no organism can rely on light in the same way that plant life on land can. Heat resistant bacteria instead sustain themselves with nutrients derived from vent-produced chemicals, by use of a process called chemosynthesis. Some of the most ancient organisms ever discovered have been thermophiles, and the Deep Sea Vent Hypothesis suggests that life itself may have its origins in this peculiar environment.
Chemosynthesising bacteria on the floor of the Mid-Atlantic Ridge provide the foundation of a diverse ecosystem.
http://oceana.org/marine-life/marine-science-and-ecosystems/deep-hydrothermal-vent
These 'thermophilic' bacteria can be of use in industrial processes, where changes in temperature would render other biological agents useless. Perhaps the most famous example is the use of Thermus aquaticus (Taq) bacteria, from geothermal vents in Yellowstone National Park. The DNA polymerase from Taq is used at high temperatures in the Polymerase Chain Reaction (PCR) to replicate DNA. This process has a wide array of applications from genetic testing in healthcare to isolating and identifying genetic material in criminal forensics.
On the topic of marine ecosystems that flourish along the Mid-Atlantic Ridge, I'll finish with this photo, taken in the geothermal pools in Iceland (also along the Mid-Atlantic Ridge).
A thermophilic organism
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