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Richard B. Aronson

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Department of Biology


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 Email: raronson@fit.edu
 Mail address:
    Department of Biology
    Harris Building
    Room 223
    150 West University Blvd.
    Melbourne, FL 32901
 Ph: +1 (321) 674-8034
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Ecological Effects of Climate Change in Antarctica

Climate change is drawing down the physiological barriers that have kept shell-crushing predators out of Antarctica for millions of years. Their return will likely disrupt Antarctica’s endemic seafloor communities. When ships dump their ballast waters in the Antarctic seas, the larvae of alien predators and other organisms are injected into the system.

Around the world, dense populations of brittlestars and sea lilies are found today only in habitats where pressure from shell-crushing predators is low. The incidence of arm damage in these populations is low compared to populations subjected to intense predation pressure. The examples shown are from the British Isles, but similar populations live in the coastal waters of Antarctica. The principal modern predators in Antarctica’s shallow-water environments are slow-moving invertebrates of a Paleozoic functional grade, particularly seastars such as Odontaster validus and the nemertean worm Parborlasia corrugatus.

 

Dense population of the suspension-feeding brittlestar Ophiothrix fragilis, photographed at 30 m (90 feet) off the Isle of Man. Copyright © Richard Aronson.

 

brittlestar

Top Image:  Dense population of the suspension-feeding brittlestar Ophiothrix fragilis, photographed at 30 m (90 feet) off the Isle of Man. Copyright © Richard Aronson.

The peculiar faunal composition of modern shallow-marine communities in Antarctica has its roots in the climatic cooling of Antarctica, which began 41 million years ago in the Eocene. The ongoing reinvasion of shell-crushing predators threatens the integrity of the unique shallow-benthic ecosystems in Antarctica.

This research is funded by National Science Foundation.

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