Are Zooplankton Primary Consumers

James Lee
• Friday, 15 January, 2021
• 10 min read

These organisms serve as an intermediary species in the food chain, transferring energy from planktonic algae (primary producers) to the larger invertebrate predators and fish who in turn feed on them. The effects of environmental disturbances can be detected through changes in species composition, abundance and body size distribution.

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Information on the kinds of zooplankton that are found in the water, and the abundance of certain species relative to one another, serves as a measure of biological condition. Zooplankton are primary consumers or the second step in the food chain.

The primary consumers in the Arctic Ocean are phytoplankton and crustaceans that consume the zooplankton. The top predators, or tertiary consumers, are polar bears and the Orca whale.

Plankton Revealed | National Geographic Society Tiny plankton form the base of the ocean food web, which further supports all other aquatic and terrestrial ecosystems across the planet. This lists the logos of programs or partners of NG Education which have provided or contributed the content on this page.

They include bacteria and algae that form the base of aquatic food webs. With 71% of the Earth covered by the ocean, phytoplankton are responsible for producing up to 50% of the oxygen we breathe.

These microscopic organisms also cycle most of the Earth’s carbon dioxide between the ocean and atmosphere. In turn, zooplankton then become food for larger, secondary consumer s such as fish.

energy pyramid ocean food webs biomass producers chains primary consumers numbers units secondary ppt powerpoint presentation unit decrease 1000 slideserve
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Marine snow often includes fecal matter, sand, soot, skin, and other organic and inorganic particles descending to the seafloor. Through plankton sampling, scientists like Richard Lamott can monitor this important component of life on Earth.

Why do Dr. Lamott and his team find more phytoplankton at the top of the water column (near the ocean surface)? Answer Phytoplankton rely on sunlight (as well as temperature and nutrients) for photosynthesis.

Answer 1) Ocean phytoplankton provide up to 50% of the oxygen we breathe. This makes them an important part in the regulation of climate change.

The tests, or shells, of this plankton are so abundant that they form the majority of seafloor sediment in many parts of the ocean. The chemicals found in form tests are also be used by oceanographers to study what the Earth’s climate was like in the past.

Plankton provides the most ancient evidence of life on Earth. Marine snow got its name because it looks like snowflakes sinking down to the bottom of the ocean.

web food ocean animals java trench brittany dolphin
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Some marine “snowflakes” can grow to be more than 5 centimeters (1.9 inches) in diameter and can take weeks to reach the seafloor. (singular: alga) diverse group of aquatic organisms, the largest of which are seaweeds.

Predatory marine worms that drift in the deep sea as plankton. Layers of gases surrounding a planet or other celestial body.

(singular: bacterium) single-celled organisms found in every ecosystem on Earth. Type of aquatic bacteria that can photosynthesize light to create energy.

Community and interactions of living and nonliving things in an area. Continuous fall of organic and inorganic particles (including the remains of marine organisms, fecal matter, shells, and sand) from the upper layers of the water column to the seafloor.

Organism on the food chain that can produce its own energy and nutrients. Sticky black particles produced as some fuels, such as coal and wood, are burned.

food web aquatic carnivore marine britannica feeding network phytoplankton
(Source: kids.britannica.com)

Rise and fall of the ocean's waters, caused by the gravitational pull of the moon and sun. Area reaching from the sediment of a body of water to its surface.

Join our community of educators and receive the latest information on National Geographic's resources for you and your students. Join our community of educators and receive the latest information on National Geographic's resources for you and your students.

No, it is not a producer because it eats phytoplankton and therefore is a primary consumer even though it's midget. (depending on the type of web you are constructing) krill is a primary consumer or secondary because the primaries include phytoplanktons, zooplankton algae etc and since kill eat photo and zoo plankton it would be a primary consumer or in a food web it would be in the second bottom row making it secondary in the food pyramid or web.

Bottom row: phytoplankton and zooplankton second bottom row: krill, prawns, and fish then the next up are the tertiary and quaternary row, which are the higher levels in the food web. Zooplankton is both primary and secondary consumers.

If they eat other zooplankton then they would be secondary consumers. Zooplankton are primary consumers or the second step in the food chain.

chain food ocean phytoplankton chains marine oceanic example plankton ecosystem sea zooplankton oceans science animal preschool animals bing bottom many
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For example grass (producer) is eaten by rabbits (primary consumer) who are eaten by foxes (secondary consumer). In addition, food webs are closely linked to climate change, since marine organisms capture a huge amount of carbon dioxide as they photosynthesize, which would otherwise boost the greenhouse effect and add to present levels of warming.

A food web doesn’t just follow one path, because sometimes marine animals don’t respond how they should. Instead, it follows all the eating habits that exist, while also examining the impact of tiny microorganisms (like bacteria) on the food chain, in mechanisms such as the microbial loop.

Image: © Joint Nature Conservation Committee (JCC)/ Alejandra Size/ WISE Marine. Here is a very simple explanation of the aquatic food web and is only one of several differing versions, depending on which animals and organisms are included.

The foundation of the ocean food web is occupied by single-celled algae and other tiny plant-like organisms, who create their own energy out of sunlight. Collectively known as phytoplankton (Greek for “drifting plant”) these microorganisms are the starting point for the entire marine food.

Microscopically small (about 1-5 mm in length), phytoplankton saturate the sunlit near-surface waters around the world in their billions. Like their terrestrial counterparts, these marine plants use photosynthesis to convert sunlight, carbon dioxide (CO2) and water to create complex carbohydrates, like sugars.

food web antarctic ocean chain webs sea chains antarctica animals environment marine prey predator land arctic ecosystem science atlantic north
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Phytoplankton is the primary producers” of the organic carbon needed by all marine animals in order to live. The most common type of primary producer (photoautotrophs) uses the sun’s energy to build carbohydrates.

These organisms use chemosynthesis to metabolize chemical compounds emitted from hydrothermal vents, methane seeps, and other geological features. It includes the world’s smallest known photosynthetic microbe, known as Prochlorococcus, which measures less than one millionth of a meter, but is one of the most plentiful species on Earth.

Krill is one of the largest zooplankton (most adults are actually one step up in the food chain), so, when they consume plankton, they turn themselves into an even bigger and more convenient meal for larger fish. In this sense, krill serve as a nutrient bridge from microscopic phytoplankton to larger fish and mammals.

Phytoplankton is aquatic plants or bacteria, while zooplankton are tiny fish, crustaceans and other marine animals. Phytoplankton inhabits the near-surface of the sea (the euphoric zone) in order to photosynthesize sunlight; zooplankton live in the darker and colder depths.

Although they vary enormously in size, herbivores share a prodigious appetite for marine vegetation, as well as a common fate. Almost every other living thing in the marine biosphere “consumes” the energy initially created by phytoplankton.

ecosystem ocean emma consumers posters fish miller producers glogster ecosystems science edu complex
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In other words, all marine life depends on phytoplankton creating enough usable energy in their bodies. According to a 2010 study published in Nature, the numbers of phytoplankton in the ocean had declined substantially over the past century.

These bacterial microbes absorb chemicals released by decomposing phytoplankton, and then enter the main food chain when they are eaten by zooplankton. Studies have found that marine mammals like whales enhance primary productivity through the release of fecal plumes.

Traditionally regarded as minor players in the marine food web, due to having a gelatinous, watery body with little nutritional value, jellyfish are now thought to be a major constituent of the diets of swordfish and tuna, as well as octopus and crabs. Species of forage fish include: anchovies, herrings, Hilda, mackerel, menhaden, sardines, shad, sprats, as well as captain, half beaks, silver sides, squid and smelt.

To compensate for their size and to deter predators, forage fish form large shoals which follow regular routes along coastlines, and also across the open sea, pursued by large numbers of marine predators, including whales, seals, tuna, dolphins and seabirds. Some larger species of whales rely upon forage fish for up to three quarters of their food intake.

Marine tertiary consumers include: baleen, humpback and Mike whales; harbor seals, cod, tuna, Chinook salmon, barracuda, dolphins and porpoises, swordfish, penguins and seals, as well as seabirds like pelicans, shear waters, cormorants and gannets. Unfortunately, removing sharks from the ocean leads to population growth among larger predators, such as groupers.

zoologica stazione isabelle schulz glomar
(Source: www.marum.de)

Another study off the southeastern coast of the United States revealed that the loss of large sharks resulted in an increase of the ray population. The hungry rays ate all the coastal scallops, forcing the closure of the local shellfish industry.

Roughly 300-400 million tons of heavy metals, solvents, and other toxic slurry from industrial plants are dumped annually into the world’s oceans. In addition, millions of tons of nitrogen and phosphorus from agricultural and industrial runoff arrive in the ocean every year, causing more hypoxic ‘dead zones’.

If all this wasn’t having a big enough impact on the world’s oceans, we also use them as a dumping ground for plastic, especially microplastic. Plastic pollution, which has skyrocketed since 1980, is now found in all parts of the ocean, from shallow coastal waters to the bottom of the 36,000-foot Mariana Trench.

Microplastic waste is ingested by almost every creature in the sea, and so far has been found to block the digestive tracts of at least 267 different species. European countries, such France, Germany and the UK, had the lowest contamination rate (72 percent).

A recent study published in Science magazine suggests the long-term viability of half the killer whale population around the globe is now in question, due to their ingestion of polychlorinated biphenyls, or PCBs. These highly toxic pollutants, now banned, damage the ovaries of female orcas, limiting their ability to breed.

resources class natural
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It also absorbs 93 percent of the excess heat produced by global warming, whose impact on water temperature, oxygen and pH levels, and marine life, is intensifying. The effects of global warming on the oceans are also becoming noticeable throughout the marine food chain, which acts as a barometer of change.

Species are becoming disoriented and damaged by marine heatwaves, ocean warming, acidification and oxygenation. Here are two specific instances of how global warming is forecast to impact on the ocean food web.

• A new study published in Los Biology suggests that levels of commercial fish stocks could fall as rising sea temperatures affect their source of food. • Predicted increases in greenhouse gas emissions might suppress oceanic biological productivity for an entire millennium.

Because as the climate warms, westerly winds in the Southern Hemisphere are likely to strengthen and shift towards the pole. As a result, surface waters will warm, sea ice will disappear, and upwelling of thermohaline circulation currents will increase around Antarctica.

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