bacteria
BACTERIA
Oceanic crust and oceanic sediments.
Trenches and undersea mountains :)
created
Biotite marble
BACTERIA
bacteria break down organic matter in seafloor sediments
Oceanic crust and oceanic sediments.
This is because the land mass is more buoyant, or lighter, than the oceanfloor.
Undisturbed seafloor sediments will carry a history of what has transpired there, much like glacial ice or peat bogs. Some interesting and potentially valuable mineral deposits are also found on the seafloor, eg. manganese nodules, metals from black smokers, and of course, deep in the rock, oil.
The bulk of oceanic crust is composed of the extrusive rock basalt, the remainder being lithified and non-lithified sediments.
The Oceanic Concerts was created in 2001.
Oceanic puffer was created in 1758.
Oceanic Linguistics was created in 1962.
New oceanic crust is created at the mid-oceanic ridges, a divergent plate boundary.
Oceanic Eclectus Parrot was created in 2006.
Narrownecked oceanic eel was created in 1884.