Read a book and u will find out
Diatoms are microscopic algae that have silica shells, or frustules, that are resistant to decomposition. When diatoms die, their shells sink to the ocean floor where they accumulate over time in sediments, forming diatomaceous earth. This accumulation is due to their abundance in aquatic environments and slow degradation rate, making them a common component of ocean-floor sediments.
i just did this to tell everyone that this page sucks
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.
sand (sometimes shells)
Mussels absorb carbon into their shells from the ocean water. The carbon is in the form of calcium carbonate, which mussels extract from the water to build their shells. When carbon dioxide in the atmosphere dissolves in the ocean, it forms carbonic acid, which can break down to release carbonate ions that mussels use to create their shells.
the color of the ocean floor is a light brown with specs of some shells at the bottom (very grainy)
dead organisms A+
Yes, huge amounts of carbon dioxide are effectively locked up in the shells of tiny marine organisms, such as foraminifera and coccolithophores. These organisms utilize dissolved carbon dioxide in the ocean to form calcium carbonate shells, which eventually sink to the ocean floor when they die. This process helps sequester carbon from the atmosphere and plays a crucial role in the global carbon cycle. Over geological time, this carbon can become part of sedimentary rock formations, further contributing to long-term carbon storage.
Shale
Shale
Shale Rock
fool