1993
DOI: 10.1016/0169-5347(93)90006-b
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Mega-island or micro-continent? New Zealand and its fauna

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Cited by 120 publications
(113 citation statements)
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“…The presence of this diversity of galaxiid fishes in the Otago-Southland region is in keeping with the diverse and endemic flora of the region (McGlone 1985;Wardle 1991), and the importance of the region as a centre of diversity for New Zealand skinks (Daugherty et al 1993). This diversity may reflect the stable geological history of the area, one of the most significant land areas that persisted despite an extensive marine transgression during the Oligocene of New Zealand (Fleming 1979;Suggate et al 1978;Cooper 1989;Cooper & Cooper 1995).…”
Section: Discussionmentioning
confidence: 99%
“…The presence of this diversity of galaxiid fishes in the Otago-Southland region is in keeping with the diverse and endemic flora of the region (McGlone 1985;Wardle 1991), and the importance of the region as a centre of diversity for New Zealand skinks (Daugherty et al 1993). This diversity may reflect the stable geological history of the area, one of the most significant land areas that persisted despite an extensive marine transgression during the Oligocene of New Zealand (Fleming 1979;Suggate et al 1978;Cooper 1989;Cooper & Cooper 1995).…”
Section: Discussionmentioning
confidence: 99%
“…Because New Zealand originated as a fragment of the supercontinent Gondwana, with rifting occurring some 80 Ma, but has been isolated from major land masses by some 2000 km for the past 60 Myr, its flora and fauna have characteristics typical of both continents and islands (McDowall, 2008). Therefore, the New Zealand archipelago has been viewed as a unique system for studying the evolution of a continental fauna in a state of isolation usually seen only in volcanic islands formed in the mid-ocean (Daugherty et al, 1993;Cowie & Holland, 2006). But is there truly a Gondwanan character to the New Zealand flora and fauna?…”
Section: Introductionmentioning
confidence: 99%
“…Like many isolated islands, New Zealand is characterized by a biota that is depauperate in certain higher taxa, with rates of endemism at or near 100% in many groups (Daugherty et al, 1993;Myers et al, 2000;Gibbs, 2006). Radiations may have been driven in part by fluctuations in global sea level during the Cenozoic, as well as the dramatic Oligocene 'drowning' or 'bottleneck' period when New Zealand's land area shrank to a tiny fraction of its present size.…”
Section: Introductionmentioning
confidence: 99%
“…Low reproductive rates and compensatory greater investment in individual young have often been considered a feature of the New Zealand avifauna (King & Moors 1979;Moors 1983;King 1984;Daugherty et al 1993;Gill & Moon 1999;Holdaway 1999). This may take the form of infrequent nesting, small clutches, large eggs and hatchlings or long periods of incubation, nestling and fledglingdependence (Niethammer 1970;Reid 1971;McLean & Miskelly 1988;Williams et al 1991;Powlesland et al 1992;Elliott et al 1996).…”
Section: Introductionmentioning
confidence: 99%