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Marine snow is a shower of organic and inorganic particles that drifts through the ocean and settles on the seafloor. It is made up of a variety of materials, including dead plankton, fecal matter, and other debris, and plays a crucial role in transporting nutrients and carbon to deep-sea ecosystems.
Deep sea detritivores are organisms that feed on organic matter that falls to the ocean floor, such as dead animals, fecal matter, and decaying plant material. These creatures play a vital role in breaking down and recycling nutrients in deep-sea ecosystems. Examples include deep-sea worms, crustaceans, and bacteria.
The deep marine water that never receives sunlight is called the aphotic zone. This layer of the ocean is typically found below a depth of about 1,000 meters (3,280 feet) and is characterized by complete darkness. Due to the absence of sunlight, photosynthesis cannot occur, and the environment relies on organic matter that sinks from the upper layers of the ocean for sustenance.
The Earth absorbs carbon primarily through natural processes such as photosynthesis, where plants, algae, and some bacteria convert carbon dioxide (CO2) from the atmosphere into organic matter. Oceans also play a significant role by absorbing CO2 directly from the atmosphere, where it is utilized by marine organisms or stored in deep waters. Additionally, soil acts as a carbon sink by capturing organic carbon from decaying plant and animal matter. These processes help regulate atmospheric CO2 levels and mitigate climate change.
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Marine snow is a shower of organic and inorganic particles that drifts through the ocean and settles on the seafloor. It is made up of a variety of materials, including dead plankton, fecal matter, and other debris, and plays a crucial role in transporting nutrients and carbon to deep-sea ecosystems.
Deep Bay Marine Field Station was created in 2011.
depends on how deep but there is marine life almost anywhere in the salty waters of the ocean.
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Deep sea detritivores are organisms that feed on organic matter that falls to the ocean floor, such as dead animals, fecal matter, and decaying plant material. These creatures play a vital role in breaking down and recycling nutrients in deep-sea ecosystems. Examples include deep-sea worms, crustaceans, and bacteria.
Yes, nutrients in the deep ocean primarily come from the decomposition of dead marine organisms. When these organisms die, their bodies sink to the ocean floor, where bacteria and other decomposers break them down, releasing essential nutrients like nitrogen and phosphorus into the surrounding water. This process, along with the input of organic matter from surface waters, helps sustain deep-sea ecosystems. Additionally, upwelling currents can bring these nutrients back to the surface, supporting marine life.
Density currents play a crucial role in distributing nutrients and oxygen throughout the deep ocean, supporting marine life in these regions. These currents also help to transport organic material and provide a means for organisms to disperse over vast distances, facilitating biodiversity and ecosystem connectivity in the deep sea.
Yes
deep marine animals have short narrow body to overcome water pressure, having no eyes or reduced eyes, low physical and metabolic activities. shallow marine animals have reverse properties to that.
Five scavengers in the ocean include the hagfish, which feeds on dead and decaying marine animals; the sea cucumber, which consumes organic matter on the ocean floor; the black vulture, often seen scavenging on dead fish near shorelines; the scavenging sea star, which can feed on carrion; and the deep-sea amphipod, known for consuming organic debris in the deep ocean. These organisms play a crucial role in the marine ecosystem by recycling nutrients and helping to maintain the health of ocean environments.
It varies according to the type of freshwater biome
The deep marine water that never receives sunlight is called the aphotic zone. This layer of the ocean is typically found below a depth of about 1,000 meters (3,280 feet) and is characterized by complete darkness. Due to the absence of sunlight, photosynthesis cannot occur, and the environment relies on organic matter that sinks from the upper layers of the ocean for sustenance.