Chemiosynthesis In The Ocean Floor

During chemosynthesis bacteria living on the sea floor or within animals use energy stored in the chemical bonds of hydrogen sulfide and methane to make glucose from water and carbon dioxide dissolved in sea water.

Chemiosynthesis in the ocean floor.

Our knowledge of chemosynthetic communities is relatively new brought to light by ocean exploration when humans first observed a vent on the deep ocean floor in 1977 and found a thriving community where there was no light. This graphic shows several ocean floor features on a scale from 0 35 000 feet below sea level. Hydrothermal vents are like geysers or hot springs on the ocean floor. A hydrothermal vent is like a geyser on the ocean s floor.

An entire ecosystem living without light or oxygen chemosynthesis flourishes beneath the ocean floor. Communities of creatures have adapted to survive in these inhospitable conditions and continue to thrive through the process of chemosynthesis. Chemosynthesis occurs around the hydrothermal vents at deep levels of the ocean. While most life on this planet requires sunlight to live there is an.

Photosynthesis gives off oxygen gas as a byproduct while chemosynthesis. Scientists later realized that bacteria were converting the toxic vent minerals into usable forms of energy through a process called chemosynthesis providing food for other vent organisms. 6co 2 6h 2 o 3 h 2 s c 6 h 12 o 6 3h 2 so 4 instead of photosynthesis vent ecosystems derive their energy from chemicals in a process called chemosynthesis both methods involve an energy source 1 carbon dioxide 2 and water to produce sugars 3. Far below the ocean floor scientists have discovered a microbial community away from undersea vents beyond the reach of the sun beneath the seafloor there is an ecosystem of microbes living in.

Continental shelf 300 feet continental slope 300 10 000 feet abyssal plain 10 000 feet abyssal hill 3 000 feet up from the abyssal plain seamount 6 000 feet. Chemosynthesis occurs around hydrothermal vents and methane seeps in the deep sea where sunlight is absent. The following features are shown at example depths to scale though each feature has a considerable range at which it may occur.