Global Climate Change and the Origin of Modern Benthic Communities in Antarctica

Marine benthic communities living in shallow-water habitats(<100 m depth) in Antarctica possess characteristics reminiscentof Paleozoic marine communities and modern deep-sea communities.The absence of crabs and sharks, the limited diversity of teleostsand skates, the dominance of slow-moving invertebrates at highertrophic levels, and the occurrence of dense ophiuroid and crinoidpopulations indicate that skeleton-breaking predation is limitedin Antarctica today, as it was worldwide during the Paleozoicand as it is in the deep sea today. The community structureof the antarctic benthos has its evolutionary roots in the Eocene.Data from fossil assemblages at Seymour Island, Antarctic Peninsulasuggest that shallow-water communities were similar to communitiesat lower latitudes until they were affected by global cooling,which accelerated in the late Eocene to early Oligocene. Thatlong-term cooling trend ultimately resulted in the polar climateand peculiar community structure found in Antarctica today.Declining temperatures beginning late in the Eocene are associatedwith the disappearance of crabs, sharks, and most teleosts.The sudden drop in predation pressure allowed dense ophiuroidand crinoid populations to appear and flourish. These late Eoceneechinoderm populations exhibit low frequencies of sublethaldamage (regenerating arms), demonstrating that there was littleor no predation from skeleton-breaking fish and decapods. Currentscenarios of global climate change include predictions of increasedupwelling and consequent cooling in temperate and subtropicalupwelling zones. Limited ecological evidence suggests that suchcooling could disrupt trophic relationships and favor retrogradecommunity structures in those local areas.