Resource: Antarctic Ecosystem

Both the Arctic and Antarctic regions are characterized by dramatic seasonal variations that, in turn, determine the kinds of life that inhabit these regions. Due to the manner in which Earth orbits the Sun—that is, tilted on its axis—these polar regions experience long summer days with continuous or near-continuous daylight, and winter days dominated by darkness. When one pole is exposed to the Sun's warming light, the other is pitched mostly in bitter-cold darkness.

The Antarctic ecosystem is a product of its climate. Apart from lichens and a few species of tiny insects that live in isolated regions, researchers have found virtually no other life forms in the continent's interior. Even though summer brings relative warmth, temperatures remain well below freezing, so ice and snow cover persists year-round. In contrast, the Southern Ocean and the sea ice that surrounds Antarctica undergo important seasonal changes that provide a rich habitat for abundant marine life.

Sea ice, which extends from the land over the water like a blanket, ranges from its summertime area of about 4 million square kilometers (1.5 million square miles) to 20 million square kilometers (7.5 million square miles) in winter. Water becomes denser the saltier and colder it gets, so when sea ice forms in winter, the water beneath it sinks. This sinking water drives a deep-water current that moves toward the Equator. It is replaced by less-dense rising water that contains nutrients stirred up from the depths.

Simple models called food chains depict possible paths along which energy moves through an ecosystem—as from producer A to consumer B to consumer C. Because most consumers have more than one food source, a more complex model called a food web is used to show how the various food chains in an ecosystem are connected. At the base of the Antarctic food web are microscopic, single-celled plants called phytoplankton.

During the light-filled summer months, phytoplankton float freely in the water and grow through photosynthesis. Using water, carbon dioxide, and sunlight, they produce oxygen and energy, which can be passed on throughout the ecosystem. The dense phytoplankton population feeds some animals directly, including shrimp-like crustaceans called krill, and soft transparent animals called salps. The krill and salps are food for animals further up the food chain, including penguins, seals, and whales. In the dark and cold of winter, phytoplankton are trapped inside and at the bottom edge of the ice that forms on the sea surface, where they remain until the summer thaw. As a consequence, the overall food supply shrinks.

Scientists studying this ecosystem now recognize that Antarctica's abundant marine life is largely confined to the edge of the sea ice. For this reason, they are closely monitoring the impact of climate change on sea ice.

To learn about seasonal changes in the north polar region, check out Arctic Ecosystem.

To learn more about how energy is transferred through the living members of the Antarctic ecosystem, check out Antarctic Food Web Game.

To learn more about how sea ice forms and the role it plays in polar regions, check out Antarctica: Sea Ice.

To learn more about the effect of global warming on glacial ice, including sea ice, check out Earth System: Ice and Global Warming.

• Describe the differences exhibited in summer and winter in the Antarctic ecosystem.
• Discuss some of the adaptations seen in animals that allow them to survive in the rigorous environmental conditions found at the poles.
• Which marine organisms are most reliant on sea ice and why? Which are least reliant and why?