The ocean has different zones that has plants and animals. The area along the ocean floor that consists of sand silt and dead organisms is called the benethic zone.
A lot of shells of marine organisms wind up on the ocean floor. Bones do not last on the ocean floor, they get eaten. But shells can last.
Ooze on the ocean floor is formed from the remains of marine organisms like phytoplankton and zooplankton, as well as shells and skeletons of marine animals. Over time, these organic materials accumulate and form sediment on the ocean floor.
In sea-floor spreading,the sea floor spreads apart along both sides of the mid-ocean ridge as a new crust is added.As a result,the ocean floors move like conveyor belts,carrying the continents along with them.
When an earthquake occurs where a slab of the ocean floor is displaced vertically along a fault.
Strips of ocean-floor basalt record the polarity of earth's magnetic field at the time the rock formed. These strips form a pattern that is the same on both sides of the mid-ocean ridge. the pattern shows that ocean floor forms along mid-ocean ridges and then moves away from the ridge.
There are certain organisms which have adapted to the ocean floor environment. Together, these organisms make up an ecosystem.
marine organisms
There are many things that could produced the ocean floor. Dying organisms for example are one component in the ocean floor.
On the ocean floor
A lot of shells of marine organisms wind up on the ocean floor. Bones do not last on the ocean floor, they get eaten. But shells can last.
Organisms that live above the ocean floor are apart of the pelagic environment
The draughtboard shark primarily feeds on small fish, crustaceans, and invertebrates. Its diet consists of various benthic organisms, which it hunts along the ocean floor. This shark is known for using its unique flattened body to blend into its surroundings while it searches for prey.
benthic environment
Bottom feeders.
Benthos
crustaceans/amphibians
Ocean floor.