Key Takeaway:
Plankton, microscopic algae and animals found in Earth’s oceans, seas, and lakes, are critical to marine ecosystems and humans. They produce about half of Earth’s oxygen and form the base of the marine food web. Zooplankton, tiny marine animals that eat phytoplankton, include copepods, krill, and blue whales. Life cycles vary, with some zooplankton spending their entire lives in the water column, while others live in the water column during larval stages. Plankton communities vary across the Earth’s seas and oceans, with warmer waters generally having lower plankton biomass and abundance. They are sensitive to changes in their environment, such as sea temperature and acidity, and can form shells using calcium carbonate. Plankton blooms, dense aggregations of microscopic single-celled phytoplankton, can span hundreds of kilometers across the ocean’s surface and are visible from space using satellites.
If you go to the beach and dip a bucket in the sea, you might at first think it contains lifeless water. But examine that water under a microscope and you will see your bucket contains a universe of microscopic life, in the form of beautiful and fascinating plankton.
Plankton are mostly microscopic algae and animals found throughout Earth’s oceans, seas and lakes, although a few species are visible to humans. Unlike fish, plankton can’t swim against the current. Instead, they drift through the water, floating at the will of the waves and tides. Plankton are critical to marine ecosystems and to humans, but often glide under the radar of our interest.
As a plankton ecologist who has worked to raise their profile globally, I hope I can convince you that these creatures deserve your attention.
Phytoplankton, the algae plankton, are single-celled organisms. Many of them have chlorophyll, a green pigment (like land plants) they use for photosynthesis to produce the oxygen we breathe. Throughout time, phytoplankton have produced roughly half of Earth’s oxygen, making our atmosphere inhabitable today.
Like land plants, phytoplankton form the base of the marine food web. While cows graze grass on land, zooplankton, tiny marine animals, eat phytoplankton.
Zooplankton include one of Earth’s most abundant animals, the copepod: a microscopic crustacean ranging in size from 0.5 to 15mm. Large copepods are eaten by larval fish, which scientists also classify as plankton since they are too weak and small to swim against the ocean currents. These larvae grow into fish that are eaten by animals higher up the food web, such as sharks, birds and humans.
Planktonic krill, a shrimp-like crustacean up to 5cm in size, make up most of the diet of the largest vertebrate to ever live on Earth, the blue whale. Blue whales eat by filtering seawater through their comb-like baleen, pushing out water while keeping the plankton in their mouth.
Unlike most sharks, basking sharksand whale sharks don’t have teeth, and eat copepods, krill and other plankton. It’s amazing to think that microscopic animals are the diet of such huge creatures.
Life cycles
Some zooplankton, like copepods and krill, spend their entire lives in the water column between the surface and bottom of the sea, rather than on the seafloor. Other zooplankton only live in the water column during their larval stages, before maturing and settling to the sea floor or, like larval fish, developing the ability to swim against the currents.
In spring, the sea is full of planktonic crab larvae, flicking their tails to swim as they hunt small copepods and other plankton. Crab larvae don’t look like adult crabs: they have huge spines on the tops and bottoms of their heads, and are long and thin rather than round with pincers. As crab larvae grow through their life stages, they look more and more like their adult selves until, finally, they drop to the sea bottom.
Lobsters, mussels, limpets and barnacles also live as plankton in their larvae stages.
Astonishing diversity
Scientists estimate there are around 100,000 plankton species in the sea. Plankton communities vary throughout the Earth’s seas and oceans, particularly with latitude. Warmer waters generally have lower plankton biomass and abundance, and consist of species with smaller body sizes.
Jellyfish, my favourite type of zooplankton, are among the biggest plankton. Despite their large size (up to 120 metres long in the case of the Lion’s Mane jellyfish), jellyfish are still considered plankton because they can’t swim against the currents and tides. Instead, they pulse through the water.
There are other types of plankton which are much smaller. These are the pico- and nano-plankton that are too small to see with a classic microscope. These tiny plankton absorb nutrients from, and help decompose, waste such as faeces, dead organisms and other biological material from other parts of the food web. This microbial loop wasn’t discovered until the 1980s.
There is so much about plankton that we still don’t know, and there are thousands of species yet to be discovered.
Climate change canaries
Plankton are extremely sensitive to changes in their environment, which means they respond quickly to alterations in sea temperature and acidity. As sea temperatures rise, warm water plankton communities are shifting away from the equator, into newly temperate environments, while cold water plankton communities are being squeezed poleward.
In the North-east Atlantic ocean, for example, plankton have shifted 1,000 miles northward since the 1960s. But these aren’t the same individuals moving – this is the whole plankton community shifting, over millions of individual lifespans.
Some plankton groups use calcium carbonate, or chalk, to form their shells. As the oceans acidify, plankton that depend on calcium carbonate struggle to form their shells, which protect them from predators and give their bodies structure.
Coccolithophores, a phytoplankton group covered in calcium carbonate liths (external plates), developed malformations in laboratory experiments that manipulated seawater pH. We are not yet sure of the extent that wild populations of coccolithophores are affected by pH change, but they are certainly important to both marine food webs and the removal of atmospheric carbon.
Plankton may be tiny but phytoplankton blooms, which are dense aggregations of microscopic single-celled phytoplankton, can span hundreds of kilometres across the ocean’s surface, and are visible from space using satellites.
These huge blooms sink to the sea floor when the plankton die, transporting carbon to the deep sea and helping to fight climate change.
While plankton blooms like this are usually natural phenomena, they may also occur due to excess nutrients from farming or sewage. If blooms are too big or too concentrated due to excess nutrients, they can cause hypoxic (no oxygen) dead zones on the seafloor. These kill everything that lives there, including animals that can’t escape this deadzone quickly.
There are few groups that are so biodiverse and important for how our oceans, indeed our entire planet, function. The next time you are on a boat or at the beach and look out at the sea, remember that each drop of water is full of microscopic life that makes our planet what it is.
