The climate of Antarctica shapes almost every feature of its ecosystem. First, the extreme COLD (inland means near −50°C, record low −89.2°C) makes the land almost lifeless: only mosses, lichens and a few invertebrates survive, so terrestrial biodiversity is very low and there are almost no plants. Because the environment is a polar DESERT (<50mm precipitation a year, with water frozen as ice), there is little liquid water on land to support plant growth, which is why the productive part of the ecosystem is the surrounding OCEAN rather than the continent.
Second, the seasonal climate controls how energy enters the food web. In summer the 24-hour daylight and nutrient-rich, partly ice-free Southern Ocean trigger a massive PHYTOPLANKTON bloom; these primary producers support huge swarms of KRILL, the keystone species. In winter, by contrast, 24-hour darkness halts photosynthesis, so production collapses and the whole system slows. This strong seasonality means the ecosystem depends on a short, intense growing season.
Third, the cold drives the structure of the food web and the adaptations within it. Energy flows through SHORT, simple chains (phytoplankton → krill → penguins/seals/fish → whales/orcas) with few species but very large populations of the survivors. To cope with the cold, animals show adaptations such as blubber, dense fur or waterproof feathers, huddling and counter-current heat exchange — features that exist precisely because of the climate.
Overall, the climate is the dominant control on the Antarctic ecosystem: the cold and dryness keep land biodiversity extremely low, while the seasonal light and the cold ocean concentrate life into a productive but simple, krill-based marine food web. To a large extent, then, the unusual character of the ecosystem — low biodiversity, marine focus and dependence on one keystone species — is a direct response to the extreme climate.