Science. 1969 Feb 14;163(3868):673-5. doi: 10.1126/science.163.3868.673.
Marine paleotemperatures, determined by oxygen isotope measurement, show that Australasian Tertiary penguins, including giant forms, lived in warm to tropical environments. Evolution from smaller species also occurred in warm environments. Mid-Tertiary fluctuations of sea temperature were controlled by alternating uplift and erosion of "Tasmantis," an unstable meridional landmass occupying and extending beyond the present position of New Zealand.
海洋古温度,通过氧同位素测量确定,表明包括巨型种类在内的澳洲第三纪企鹅生活在温暖到热带的环境中。较小物种的进化也是在温暖的环境中发生的。中第三纪的海温波动受“塔斯曼尼亚”(Tasmantis)的交替隆起和侵蚀控制,“塔斯曼尼亚”是一个不稳定的经向陆地,占据并延伸到现在新西兰的位置以外。