It is well known that several cetacean genera, and possibly even some species, are discontinuously distributed on either side of equator. Such distributions, often described as bipolar, have been widely discussed for other marine animals-notably by Berg (1933) and by Ekman (1953)--but no one has attempted a systematic examination of phenomenon in regard to whales and dolphins. Because most so-called bipolar marine distributions are actually bitemperate or even bisubtropical, Hubbs (1952) suggested term as more appropriate and all-inclusive. An attempt is made here to review nature of antitropical distributions in Cetacea, to account for them, and to suggest something of their evolutionary significance. Present evidence, both specific and circumstantial, suggests that earlier cetaceans lived in a warm-water environment. Thus earliest known forms are zeuglodonts from Middle Eocene of Egypt, Nigeria, and Texas and distribution of existing species still suggests an aversion to cold: only three genera (Balaena, Delphinapterus, and Monodon) breed in polar waters, none breeds in Antarctic polar waters, and majority of species frequenting cold water appear to move equatorward to breed. By end of Eocene, zeuglodonts had spread north to British Columbia, England, and Germany and probably south to Australia and New Zealand; at any rate they were certainly in southern waters by Oligocene. Toward end of Eocene also, first archaic toothed whales (Odontoceti) appeared, but are known only from North America. Although a few zeuglodonts persisted in early Miocene, both of these early stocks apparently declined markedly during Oligocene without being immediately replaced by newer forms. Kellogg (1928) remarked on the scarcity of fossil cetaceans in Oligocene and pointed out that this all more surprising in view of wide variety of types that make their appearance in formations of lower Miocene age. In addition to now extinct squalodonts, modern groups of dolphins, sperm whales, beaked whales, and river dolphins all appeared about this time, together with first of whalebone whales-the cetotheres. The marked turnover of forms at about Oligocene-Miocene boundary appears to be correlated with cooling of world climates during Tertiary, which seems generally to have been reflected in oceanic temperatures. The writer has recently suggested (Davies, 1958) that an apparently sudden enlargement of range and speeding of evolutionary rates in Pinnipedia was associated with this expansion of coldwater environment, and it seems likely that mid-Tertiary revolution in whale stocks arose for a similar reason. The older, warm-water types failed to adapt themselves to growing new cold-water environments and newer types, which appeared in force in Miocene, evolved and spread rapidly in response to these new opportunities. There are some indications in distribution of post-Oligocene as compared with pre-Miocene fossils and in almost complete fossil taxonomic discontinuity between northern and southern hemispheres that equatorial warm-water zone was an important barrier to dispersal throughout later Tertiary. However distribution and relationship of existing Cetacea show that, while equatorial zone is still a barrier, there have been relatively recent opportunities for increased dispersal
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