The African-Malagasy sweepstakes envisaged by G. G. Simpson
Verreaux’s sifaka (Propithecus verreauxi) Wikimedia Commons
A primate made this journey in the Palaeocene some 57 million years ago (mya). It was the ancestor of the more than 50 species of lemur living today. Tenrecs did not arrive until the Oligocene (29 mya) but they too evolved to fill all sorts of available niches. One would think this rapid radiation would be reflected in differences in placentation. In fact lemurs have a placental type not too different from other strepsirrhine primates – the lorises and bush babies of Asia and Africa . In both groups the placenta is diffuse, with interdigitating villi and an epitheliochorial barrier. Malagasy tenrecs all have the same type of placenta: discoid, labyrinthine and haemochorial.
The capybara, a caviomorph rodent, Wikimedia Commons
Sweepstakes distribution also occurred from Africa to South America across the South Atlantic . Recently we looked at two groups of mammals that used this route. Caviomorph rodents arrived in the Middle Eocene (41 mya) and the ancestors of New World monkeys by the Late Oligocene (29 mya). Again we found that their subsequent radiation was not accompanied by major changes in placentation. Indeed the placenta of caviomorphs has the same distinctive features as in the related phiomorphs from Africa .
Perhaps the placenta is not quite as plastic as we are inclined to think.
And the hippopotamus in Simpson’s sketch – which predates the one in Dreamworks' Madagascar by 65 years? There are hippopotami in the fossil record of Madagascar, but they left no trace of their placentas.
If you look at what happened after the Japanese tsunami it is clear that on occasions large numbers of trees could find themselves at sea simultaneously - and possibly forming floating islands quite capable of transporting and supporting small mammals for several weeks. Admittedly much of the debris from Japan was as a result of human cililization - but one floating "island" of debris was reported to be 69 miles long - see http://dangerousminds.net/comments/floating_debris_japan_tsunami_across_ocean
ReplyDeleteToday the ocean currents go in the wrong direction but modelling of the Indian Ocean in the early Caenozoic, when Madagascar was in a slightly different place, show the current then went in a direction favourable to rafting from Africa (Ali & Huber Nature 2010; 463: 653-6).
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