Joseph T. Eastman, Ph.D.
Professor of Anatomy
Department of Biomedical Sciences
eastman@ohiou.edu
119 Life Sciences Building
740-593-2350
Fax: 740-593-2400
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DEPT. OF BIOMEDICAL SCIENCES
DEPT. OF BIOLOGICAL SCIENCES
EDISON BIOTECHNOLOGY INSTITUTE
COLLEGE OF OSTEOPATHIC MEDICINE
 
 
Introduction

My field and laboratory work deals with a group of perch-like Antarctic fishes called notothenioids, the dominant and most diverse fish group in the Southern Ocean. The objectives are to gain insight into the evolution and diversification of this group, and to understand the role of notothenioids in the Antarctic marine ecosystem. I study the biology of these fishes in a historical and phylogenetic context. Like much evolutionary research, my work is concerned with historical events and the approach is frequently retrospective, investigating the modern results of historical processes. I am attempting to decipher the results of a series of evolutionary events that have proceeded for 40 million years under the unusual conditions found in Antarctic waters. I seek to answer a series of questions relating to the nature of Antarctic fish diversity. Why did the fish fauna evolve the way it did? Why is the modern fauna unlike the preceding fossil faunas as well as the shelf faunas of other southern continents? Why do notothenioids contribute so heavily to Antarctic fish diversity at both the organismal and ecological levels? When did the fauna become "modern" in taxonomic composition? How did neutrally buoyant fish evolve from ancestors who were heavy bottom dwellers? Are there correlations between changes in the morphology of various body systems and the ecological changes that accompanied the notothenioid radiation? Is novel morphology required for perciform fish to live in the subzero waters of the Antarctic shelf? Are notothenioids an example of a species flock? Is Antarctica an evolutionary center of origin for marine organisms? Some of these questions will have no clear answers. The sections below provide some background information on my work.
   
Antarctica and the Southern Ocean

Antarctica is a continental island, about twice the size of Australia, with the dominant fauna inhabiting the water rather than the ice-covered landmass. The sea is the largest living space on earth and the Southern Ocean surrounding Antarctica is 10% of the world's ocean. Antarctica and its fish fauna are commanding increased attention in a world attuned to loss of biological diversity, depletion of marine fisheries and the encroachment of human activities into isolated and incompletely studied ecosystems such as the Southern Ocean. For example, the popular gourmet delicacy known as “Chilean sea bass” is actually a heavily exploited Subantarctic species (shown in Figure 1k).
 
   
Antarctica as an evolutionary center

Until recently Antarctica had been under appreciated as an evolutionary site because most Antarctic biological research had focused on adaptations to the “extreme” environment rather than on similarities between the Antarctic fauna and faunas in other isolated habitats such as islands and ancient rift lakes. Unlike other large marine ecosystems, the waters of the continental shelf around Antarctica resemble a closed basin, isolated from other shelf areas in the Southern Hemisphere by distance, current patterns, bathymetry and subzero water temperatures. As these isolating conditions developed over the past 10-30 million years, the marine biota became adapted to new shelf habitat and their ranges became highly circumscribed. For example, the level of endemism reaches 97% in the case of fishes. Antarctica has the world’s most distinctive marine fauna. The attention of evolutionary biologists is drawn to these isolated habitats because of their unusual faunas. In this sense the waters of the Antarctic shelf are comparable to, but less well known than, classic evolutionary sites such as the Galápagos, Hawaii and Lake Baikal. Research on Antarctic fishes provides insight into evolutionary processes and macroevolutionary events in the marine realm where these processes are not as well documented as in terrestrial and freshwater habitats. The Antarctic fauna occupies an extreme in the spectrum of habitats where fishes are found – it provides a glimpse of the wide scope of adaptation and evolution in a habitat once thought to be incompatible with marine life.
 
   
The Antarctic fish fauna

Over the past 40 million years there has been a complete replacement of the fish fauna on the Antarctic shelf. The highly endemic, cold adapted modern fauna succeeded a diverse, cosmopolitan temperate fauna dating from the late Eocene about 38 million years ago. Today 221 species of fishes inhabit the waters of the Antarctic shelf. The fauna is dominated by a suborder of 101 species of notothenioids. Notothenioids are phyletically derived among bony fish and are related to walleyes and perch as well as to coral reef fishes. A variety of interesting specializations distinguish Antarctic notothenioids. Among these are: glycoprotein antifreeze compounds that prevent freezing in subzero water; extreme stenothermia that allows survival only in the range of -2.5 to +6.0ºC; reduced blood viscosity through absence or decreased numbers of erythrocytes; and, in some species, neutral buoyancy without benefit of a swim bladder.

The Antarctic fish fauna lacks the higher taxonomic diversity typical of all other inshore marine habitats. On the Antarctic shelf notothenioids dominate the fauna in terms of species diversity, abundance and biomass, the latter two at levels of 90-95%. The grounding of the ice sheet on the continental shelf and changing trophic conditions may have eliminated the taxonomically diverse late Eocene fauna and initiated the original diversification of notothenioids. In a habitat with few other fishes, notothenioids underwent a depth-related diversification directed away from the ancestral benthic habitat toward pelagic or partially pelagic zooplanktivory and piscivory. Notothenioids were able to fill these niches as well as remaining the dominant benthic group. Figure 1a-1 provides an example of the range of morphological diversity within one family of notothenioids.

The diversification of notothenioids centered on the evolutionary alteration of buoyancy and the morphology associated with swimming and feeding in the water column. Although they lack swim bladders, in some species density reduction to neutral buoyancy has been achieved through a combination of reduced skeletal mineralization and lipid deposition. Pedomorphic changes in the skeleton are also associated with reduced density. Panel l in Figure 1 depicts a streamlined pelagic species that is neutrally buoyant. In the dominant family Nototheniidae, about 50% of the Antarctic species temporarily or permanently inhabit the water column rather than the ancestral benthic habitat. Referred to as pelagization, this evolutionary tailoring of morphology for life in the water column is the hallmark of the notothenioid radiation and probably arose independently in different notothenioid clades.
 
   
Notothenioids on the high Antarctic shelf – a species flock?

The notothenioid diversification has produced different life history or ecological types similar in magnitude to those displayed by taxonomically unrelated shelf fishes elsewhere in the world. This is unique in the marine realm and raises the possibility that notothenioids are one of the few known examples of a species flock of marine fishes. A species flock is an assemblage of a disproportionately high number of closely related species which evolved rapidly within a circumscribed area where most species are endemic. Classic examples include Darwin’s finches in the Galápagos, Drosophila fruit flies in Hawaii, cichlid fishes in the East African Great Lakes and sculpin fishes in Siberian Lake Baikal. Notothenioids on the high Antarctic shelf possess all the characteristics of a species flock – disproportionate speciosity, morphological and ecological diversification, habitat dominance, high endemicity and monophyly. The presence of this flock, and other marine flocks (lobodontine seals, isopods, amphipods, octopodids), reinforces the status of Antarctica as a unique evolutionary site.
 
   
See NSF Press Release on this research  
   
   
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Last updated: 12/04/2007