- How much salt is in the ocean?
- Where do nutrients in the ocean come from?
- What dissolved nutrients?
- What are the major components of seawater?
- Which ocean zone is lacking in nutrients?
- How does temperature affect phytoplankton?
- How many dead zones are in the ocean?
- Can phytoplankton live in warm water?
- What does a phytoplankton eat?
- Why do nutrients stay at the bottom of the ocean?
- Why is ocean water salty?
- How do you fix nutrient pollution?
- Why is too much nitrogen bad?
- What is the main cause of ocean currents?
- Why is deep water nutrient rich?
- Where are most nutrients found in the ocean?
- Why is phytoplankton called the grass of the sea?
- What is downwelling in the ocean?
- How deep ocean actually is?
- What is the dead zone in the ocean?
- What are the six most abundant elements in seawater?
How much salt is in the ocean?
By the way, the concentration of salt in seawater (salinity) is about 35 parts per thousand.
In other words, about 35 of 1,000 (3.5%) of the weight of seawater comes from the dissolved salts; in a cubic mile of seawater the weight of the salt, as sodium chloride, would be about 120 million tons..
Where do nutrients in the ocean come from?
Nutrients come from a variety of different sources. They can occur naturally as a result of weathering of rocks and soil in the watershed and they can also come from the ocean due to mixing of water currents.
What dissolved nutrients?
Introduction. Dissolved nutrients are composed of both organic and inorganic forms. By “nutrients” I mean that any molecules that can be taken up and used as “food” – catabolized or used as building locks for metabolic processes.
What are the major components of seawater?
Seawater has six major constituent dissolved elements (concentrations above 100 ppm) in seawater: chlorine, sodium, magnesium, sulfur (as sulfate), calcium, and potassium. The six major constituents together comprise 99.28% of all the dissolved salts.
Which ocean zone is lacking in nutrients?
The deepest part of the ocean, the abyssal zone, at depths of 4000 m or greater, is very cold and has very high pressure, high oxygen content, and low nutrient content. There are a variety of invertebrates and fishes found in this zone, but the abyssal zone does not have plants due to the lack of light.
How does temperature affect phytoplankton?
A short-term temperature increase of 4 °C resulted in lower phytoplankton biomass (Yvon-Durocher et al. … Another study showed that warming had positive effects on phytoplankton biomass but was strongly negatively affected by decreasing nutrient flux at higher temperatures (Lewandowska et al. 2014).
How many dead zones are in the ocean?
405According to a new study in Science, the rest of the world fares no better—there are now 405 identified dead zones worldwide, up from 49 in the 1960s—and the world’s largest dead zone remains the Baltic Sea, whose bottom waters now lack oxygen year-round. Click here to see a map of dead zones around the world.
Can phytoplankton live in warm water?
In fact, phytoplankton in warmer equatorial waters can grow much faster than their cold-water cousins. … Phytoplankton have so far adapted fairly well to local current temperatures, but based on projections of future ocean temperatures, they may not be able to do so quickly enough to changes in their current environment.
What does a phytoplankton eat?
The food web Phytoplankton are the foundation of the aquatic food web, the primary producers, feeding everything from microscopic, animal-like zooplankton to multi-ton whales. Small fish and invertebrates also graze on the plant-like organisms, and then those smaller animals are eaten by bigger ones.
Why do nutrients stay at the bottom of the ocean?
Nutrients in the ocean are cycled by a process known as biological pumping, whereby plankton extract the nutrients out of the surface water and combine them in their organic matrix. Then when the plants die, sink and decay, the nutrients are returned to their dissolved state at deeper levels of the ocean.
Why is ocean water salty?
Salt in the ocean comes from two sources: runoff from the land and openings in the seafloor. Rocks on land are the major source of salts dissolved in seawater. Rainwater that falls on land is slightly acidic, so it erodes rocks. … Ocean water seeps into cracks in the seafloor and is heated by magma from the Earth’s core.
How do you fix nutrient pollution?
Sweep up any grass clippings or fertilizer spills on driveways, sidewalks and streets. Instead of planting and mowing turfgrass here, plant wildflowers, ornamental grasses, shrubs or trees. These plantings absorb and filter runoff that contains nutrients and soil, as well as provide habitat for wildlife.
Why is too much nitrogen bad?
Too much nitrogen and phosphorus in the water causes algae to grow faster than ecosystems can handle. … Excess nitrogen in the atmosphere can produce pollutants such as ammonia and ozone, which can impair our ability to breathe, limit visibility and alter plant growth.
What is the main cause of ocean currents?
Winds, water density, and tides all drive ocean currents. Coastal and sea floor features influence their location, direction, and speed. Earth’s rotation results in the Coriolis effect which also influences ocean currents.
Why is deep water nutrient rich?
Deep waters are rich in nutrients, including nitrate, phosphate and silicic acid, themselves the result of decomposition of sinking organic matter (dead/detrital plankton) from surface waters.
Where are most nutrients found in the ocean?
Just like plants in your garden, plants in the ocean require nutrients to grow. The most important nutrients for phytoplankton growth in the ocean are nitrate and phosphate. Some types of phytoplankton, called diatoms, also require the nutrient silicate, which they use to build their cell walls.
Why is phytoplankton called the grass of the sea?
Microscopic phytoplankton have been called ‘the grass of the sea’ because they are the basic food on which all other marine life depends. They themselves are consumed by animal zooplankton that go on to provide food for larger animals and fish.
What is downwelling in the ocean?
Upwelling is a process in which deep, cold water rises toward the surface. … The reverse process, called “downwelling,” also occurs when wind causes surface water to build up along a coastline and the surface water eventually sinks toward the bottom.
How deep ocean actually is?
The ocean is deep. … Officially anything deeper than just 200 metres is considered the “deep sea”, but the average depth of the entire ocean is about 3.5km and the deepest point – the Challenger Deep in the Mariana Trench, in the western Pacific – is a little short of 11km down.
What is the dead zone in the ocean?
“Dead zone” is a more common term for hypoxia, which refers to a reduced level of oxygen in the water. … Less oxygen dissolved in the water is often referred to as a “dead zone” because most marine life either dies, or, if they are mobile such as fish, leave the area.
What are the six most abundant elements in seawater?
Chemical and physical properties of seawater The six most abundant ions of seawater are chloride (Cl−), sodium (Na+), sulfate (SO24−), magnesium (Mg2+), calcium (Ca2+), and potassium (K+). By weight these ions make up about 99 percent of all sea salts.