18 – Penguin History and New Fossil Material from New Zealand
18 – Penguin History and New Fossil Material from New Zealand
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18 – 企鹅的历史和来自新西兰的新化石材料
DOI:
10.1016/b978-0-08-057106-5.50029-2
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发表时间:
1990
影响因子:
2.4
通讯作者:
Craig M. Jones
中科院分区:
文献类型:
--
作者:
R. Fordyce;Craig M. Jones
Penguins are obligate marine birds with an exclusively austral history (Figure 18.1) that extends back more than 45-50 million years before present (mybp). The distribution of living and fossil penguins suggests a strong link with cool temperate waters, and it may be more than coincidence that the early evolution of penguins paralleled the evolution of essentially modern circulation patterns in the Southern Ocean between Antarctica and the other southern continents. The evolution of the Southern Ocean also paralleled the rise of other marine higher vertebrates, cetaceans and seals (Fordyce, 1989). These and the penguins radiated to fill ecological niches vacated by marine reptiles and other taxa which disappeared during the mass extinction at the end of the Cretaceous. Northern large, wing-propelled divers analogous to penguins are known (eg, extinct Plotopteridae in the North Pacific and Alcidae in the North Pacific and Atlantic), but they are neither as diverse nor as widespread as penguins; the special role of southern waters thereby seems further emphasized. This contribution reviews some broader aspects of penguin history and some new fossils from New Zealand from a zoological point of view. Our comments are based largely around recent studies on New Zealand fossil penguins, although we also consider fossils from other areas. The approach stresses that one