So, the big fossil news that the Leakey Foundation was teasing when last I posted? It was this:
BS&M Blog readers, meet Nyanzapithecus alesi, a new 13 million-year-old Miocene ape from Kenya. HOW COOL IS THAT?!
I will tell you how cool. VERY COOL. I’m biased (as always – because I pick the things I want to write about for the blog, which are things that I think are very cool), but seriously. There are a bunch of reasons this discovery is awesome, like:
1) You don’t often find complete crania (the skull minus the jaw) of fossil apes. Typically, the bones at the back of the skull (the ones that form the brain case) break sometime before a fossil is found (if it’s found at all, which is a whole different issue). If you want to become a primate fossil, it takes specific circumstances and a lot of luck.
2) You really don’t find fossil ape crania in Africa dated to between 10-14 million years old. Alesi is it. Other fossil ape partial crania are known from this time period in Europe (Pliobates cataloniae at 11.6 mya and Pierolapithecus catalaunicus at 12.5-13 mya from Spain, and Rudapithecus hungaricus at 10 mya from Hungary, to name a few) and Asia (Sivapithecus indicus at 12.3 from Pakistan), which might say something about where fossil apes originated or it might either be the result of less digging having happened in Africa resulting in a deficient fossil record or the difficulty in identifying the earliest apes.
3) You also rarely find infant material in the primate fossil record. (Yes, I know, the Taung Child is an exception to this rule, too.) Infant bones are smaller and more fragile than those of adults, which makes them even less likely to fossilize and be recovered later.
Alesi is also awesome, simply by virtue of being a Miocene ape (my Miocene bias is definitely showing). The Miocene (23-5.3 mya) often gets called a “planet of the apes” because there was a huge diversity of hominoids (the fancy taxonomic group name for apes, including us, is Hominoidea) that lived through Europe, Africa, and Asia at that time. Which is SUPER AWESOME because they were “experimenting” with different types of locomotion at that time (which is totally my jam), but also makes it really hard to tell our potential ancestors from our side-branch cousins. A classic problem for people who work on Miocene apes is that they have ape faces and monkey bodies, and the field disagrees about which is more important (the face or the body) for figuring out who is related to who. Hopefully one of the authors of the Alesi paper (shout out to Kelsey Pugh!) will be able to work some of these relationships out with her dissertation research.
My final thought/question (for now) on Alesi is: the authors suggest that gibbon-like features evolved in parallel several times in different branches of the hominoid lineage – why couldn’t these features be ancestral, rather than derived? If that was the case, it would just require that a different set of facial features evolved in parallel instead. So why the gibbon-like ones and not the other ones?
That’s all for now! Hopefully BS&M will be back on September 8th – catch you then!
Alba, D.M., Almécija, S., DeMiguel, D., Fortuny, J., de los Ríos, M.P., Pina, M., Robles, J.M. and Moyà-Solà, S. (2015). Miocene small-bodied ape from Eurasia sheds light on hominoid evolution. Science, 350(6260), aab2625.
Begun, D. R., Nargolwalla, M. C., & Kordos, L. (2012). European Miocene hominids and the origin of the African ape and human clade. Evolutionary Anthropology: Issues, News, and Reviews, 21(1), 10-23.
Moyà-Solà, S., Köhler, M., Alba, D. M., Casanovas-Vilar, I., & Galindo, J. (2004). Pierolapithecus catalaunicus, a new Middle Miocene great ape from Spain. Science, 306(5700), 1339-1344.
Nengo, I., Tafforeau, P., Gilbert, C.C., Fleagle, J.G., Miller, E.R., Feibel, C., Fox, D.L., Feinberg, J., Pugh, K.D., Berruyer, C. and Mana, S. (2017). New infant cranium from the African Miocene sheds light on ape evolution. Nature, 548(7666), 169.