Kelps are the largest of the marine plants found in Antarctic and sub-Antarctic waters.

The bull kelp Durvillaea antarctica is thought to be the strongest kelp in the world and is able to withstand the massive seas that are characteristic of the Southern Ocean.

Kelp has one of the fastest growth rates of any of the marine plants (up to 60cm per day or 3kg of dry weight per square metre of habitat per day recorded for the Giant Kelp).


Kelps are important contributors to some Antarctic bottom communities, but it is in sub-Antarctic latitudes that they dominate.

Two main species occur at Macquarie Island — the leathery bull kelp Durvillaea antarctica which occupies the bottom of the rocky shore, and the giant kelp Macrocystis pyrifera which forms dense forests at depths greater than 6 metres. Both species can reach lengths of over 20m.

At Heard Island, only bull kelp is present. Heard Island lies below the Antarctic Convergence, and experiences much lower water temperatures. In Heard Island’s kelp zone, one square metre of rocky shore may support up to 47 kelp plants, and over 200kg of plant tissue.

Bull kelp and giant kelp have very buoyant fronds that are capable of supporting whole plants at sea for considerable periods of time. Bull kelp is exceptionally buoyant and has been documented to carry boulders weighing up to 75kg from the lower to upper shore at Macquarie Island.

It has been hypothesised that animals associated with floating kelp (kelp rafts) can be transported between the far-flung islands across the sub-Antarctic. This could explain why many kelp-associated species are found throughout the islands of the sub-Antarctic. Recent surveys estimate that, between the latitudes of 46–53°S, over 70 million plants are afloat at any one time.

Kelp habitats

Kelp’s fast growth rates make it an important primary producer, supplying food into nearshore and intertidal marine habitats. Some animals, such as sea-urchins, shells and small crustaceans, feed directly on kelp, however, most consumers benefit through the breakdown of detached kelp plants.

Kelp plants have a strong ‘root’ system, known as a holdfast that attaches them to the substrate. Waves in the Southern Ocean are so strong that plants are often torn from the bottom and flung onto adjacent beaches. Smaller pieces of kelp also break off during heavy seas and these may strand on local beaches or sink into deeper waters. Wherever they end up, detached kelp becomes a food source for scavenging animals such as amphipods (beach hoppers) and are gradually broken down, liberating nutrients back into coastal waters.

Kelp provides a refuge from the harsh physical environment for many organisms. Long fronds of bull kelp are often packed tightly around the lower shore and absorb much of the energy from the waves crashing on the coast. This creates a lower energy environment where marine life abounds. Small plants and animals can be found living between the large holdfasts of kelp and many animals also live within the holdfast itself.

The holdfast of a bull kelp is a solid hemisphere of tough tissue, but a species of small isopod crustacean (Limnoria) makes its living consuming this tissue. In the process, the holdfast becomes riddled with tunnels and chambers which are used as living space by other small invertebrates. Different species of Limnoria are the primary space providers at Macquarie Island (L. stephenseni) and Heard Island (L. antarctica).

Studies of the kelp holdfast communities at Macquarie Island and Heard Island have revealed that they support a higher diversity than any other shore habitat with over 90 species of invertebrate finding shelter in the tunnels and chambers that riddle their large masses. A typical holdfast community includes worms of many varieties, molluscs, mites, sea-stars, sea-cucumbers and a large variety of crustaceans.

The diversity of organisms inhabiting the holdfast makes this habitat a valuable tool for monitoring changes in shore communities under the influence of both natural, and human induced impacts. After small oil spill at Macquarie Island in 1987, the holdfast community of bull kelp was the most sensitive indicator of the effects and subsequent recovery.