Yes, sediments do affect the ocean. There are a couple ways in which sediments affect the oceans. If too many sediments on the ocean floor get stirred up in the surface water it can potentially harm the water life by suffocating and killing the life. It can also make visibility worse and can harm commercial fishing corporations.
Marine life and oxygen for those organisms to survive ! And sediments, which are none living !
Chuck Norris
Neritic sediments are the unconsolidated particles, such as sand, silt, and clay, that accumulate in the shallow waters of the continental shelf. These sediments are typically derived from the erosion of land and then transported by rivers or currents to the nearshore marine environment. Neritic sediments play a crucial role in the marine ecosystem and can provide important habitats for various organisms.
Marine sediments are typically classified into four main classes: terrigenous, biogenous, hydrogenous, and cosmogenous. Terrigenous sediments originate from land, consisting of eroded rocks and soil transported by rivers and wind. Biogenous sediments are derived from biological materials, primarily the remains of marine organisms like foraminifera and diatoms. Hydrogenous sediments form directly from the precipitation of minerals from seawater, while cosmogenous sediments come from extraterrestrial sources, such as meteorites.
Biogenous sediments are primarily composed of the remains of marine organisms. The two main types are calcareous ooze, which is formed from the calcium carbonate shells of organisms like foraminifera and coccolithophores, and siliceous ooze, composed of silica from diatoms and radiolarians. These sediments accumulate on the ocean floor and play a crucial role in the carbon cycle and marine ecosystem dynamics.
Sediments that originate from living organisms are known as biogenic sediments. These include materials such as shells, coral fragments, and skeletal remains of marine organisms, which accumulate on the ocean floor. Additionally, organic matter from plants and animals, including peat formed from decaying plant material in wetlands, contributes to biogenic sediments. Such sediments play a crucial role in the carbon cycle and can lead to the formation of fossil fuels over geological time.
Sediments that originate from elements in seawater that precipitate out of solution are primarily known as chemical sediments. These include carbonate sediments, such as limestone, formed from the precipitation of calcium carbonate, and evaporite deposits, like halite and gypsum, which result from the evaporation of seawater. Additionally, siliceous sediments can form from the precipitation of silica from marine organisms, such as diatoms and radiolarians. These sediments play a crucial role in the geological record and marine ecosystems.
Terrigenous sediments, which originate from land and are composed of materials like sand, silt, and clay. Biogenous sediments, made up of the remains of marine organisms such as shells, coral, and diatoms. Hydrogenous sediments, formed from minerals that precipitate directly from seawater and include materials like manganese nodules and metal sulfides.
Layers of sediment forming at the bottom of the ocean are called "marine sediments." These sediments are made up of a variety of materials such as mineral particles, organic matter, and remains of marine organisms, which accumulate over time to form distinct layers.
Sediments mixed with seawater can settle on the seafloor and create layers of sediment. These layers can provide a record of past environmental conditions and the history of the Earth. Sediments can also provide habitats for certain marine organisms and influence ocean currents and nutrient cycling.
Marine Ecology is the scientific study of marine-life habitat, populations, and interactions among organisms and the surrounding environment including their abiotic (non-living physical and chemical factors that affect the ability of organisms to survive and reproduce) and biotic factors (living things or the materials that directly or indirectly affect an organism in its environment).
None. An Ocean is a Marine environment.