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The History of the Chatham Islands' Bird Fauna<br />

of the Last 7000 Years—A Chronicle of<br />

Change and Extinction<br />

ABSTRACT<br />

Over the past 150 years, thousands of fossil bones of extinct and<br />

living species of birds have been collected from the Chatham<br />

Islands, an isolated island group some 860 km east of New<br />

Zealand. Recent field research (1988-1993) has dramatically augmented<br />

the earlier collections and has provided, for the first time, a<br />

sound stratigraphic and radiometric chronology for this rich subfossil<br />

avifauna. Most of these bones have been found naturally<br />

deposited in the buried soil horizons of coastal sand dunes or in<br />

limestone caves, but some are of archeological origin, deposited<br />

by human agency in coastal dune middens or, occasionally, in<br />

dwelling caves. Most, if not all, of the avian remains are of early<br />

Holocene or younger age, as indicated by a series of some 65<br />

accelerator-mass-spectometry radiocarbon dates ranging from ca.<br />

7000 yrs BP to ca. 300 yrs BP. The Holocene fossil record for, and<br />

patterns of evolution and extinction within, the Chatham Islands'<br />

avifauna are documented and discussed. Taxonomic studies indicate<br />

that several taxa, all extinct, can no longer be considered<br />

inseparable from their mainland counterparts; among these are as<br />

yet undescribed species of Eudyptes, Tadorna, Mergus, and Nestor.<br />

Introduction<br />

Dune sands and cave sediments on the Chatham Islands (Figure<br />

1) have yielded thousands of Holocene fossil bones of extinct<br />

and living species of birds (Forbes, 1892a, 1892b, 1892c,<br />

1893a, 1893b; Andrews, 1896a, 1896b; Scarlett, 1955; Dawson,<br />

1957, 1958, 1959, 1960, 1961a, 1961b; Simmons, 1964;<br />

Olson, 1975, 1984, 1990; Sutton and Marshall, 1977; Sutton,<br />

1979,1982; Millener, 1981, 1991, 1996; Tennyson and Millener,<br />

1994). The Museum of New Zealand, Wellington, for example,<br />

holds more than 250,000 Chatham Islands fossil speci-<br />

Philip R. Millener<br />

Philip R. Millener, Geology Department, University of Tennessee at<br />

Chattanooga, 615 McCallie Avenue, Chattanooga, Tennessee 37403-<br />

2598, United States.<br />

85<br />

mens, whereas extensive additional material is housed at the<br />

Canterbury Museum, Christchurch, and in the Natural History<br />

Museum, <strong>Lo</strong>ndon. The diversity of this fossil avifauna, which<br />

included many endemic land birds (among them several flightless<br />

forms), numerous waterfowl, and colonies of breeding<br />

subtropical and subantarctic seabirds, contrasts markedly with<br />

that of the present. The total number of bird species, living and<br />

extinct, recorded from the Chatham Islands is more than 100.<br />

The majority of them, some 60 species, are marine birds;<br />

among them are albatrosses, petrels and shearwaters, penguins,<br />

cormorants, waders, and gulls and terns (see Table 1). Only<br />

about 25 of these marine species currently breed in the<br />

Chathams, although formerly perhaps as many as seven more<br />

did so (Bourne, 1967). The remaining seabirds are summer migrants,<br />

occasional visitors, or vagrants. The rest of the birds<br />

(those of terrestrial and freshwater habitat) can be divided into<br />

three groups: (1) those present prior to first human contact; (2)<br />

those that self-colonized more recently, some of them within<br />

the historic period (e.g., Welcome Swallow {Hirundo tahitica),<br />

White-faced Heron {Ardea novaehollandiae), Spur-winged<br />

Plover {Vanellus miles)); and (3) those that have been deliberately<br />

introduced by Europeans (e.g., Black Swan {Cygnus atratus),<br />

Weka {Gallirallus australis), House Sparrow {Passer domesticus),<br />

Blackbird {Turdus merula), Song Thrush {Turdus<br />

philomelos), Starling {Sturnus vulgaris)). This paper is primarily<br />

concerned with the composition of the prehistoric Chatham<br />

Island avifauna, so the recent self-colonists and the deliberately<br />

introduced species are not considered further. Nomenclature<br />

for species' binomials and English names of modern birds follows<br />

Turbott (1990) unless otherwise noted.<br />

METHODS<br />

Radiometric ages quoted in this paper were determined by<br />

the Rafter Radiocarbon Laboratory, Institute of Geological and<br />

Nuclear Sciences, Gracefield, New Zealand, using accelerator

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