CARTA: Climate and Evolution: Jean-Jacques Hublin: The Climatic Framework of Neandertal Evolution

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- [Presenter] This UCSD-TV program is presented by University of California Television. Like what you learn? Visit our website, or follow us on Facebook and Twitter to keep up with the latest programs. ♪ [music] ♪ We are the paradoxical ape: bipedal, naked, large-brained. Long the master of fire, tools and language, but still trying to understand ourselves. Aware that death is inevitable, yet filled with optimism. We grow up slowly. We hand down knowledge. We empathize and deceive. We shape the future from our shared understanding of the past. CARTA brings together experts from diverse disciplines to exchange insights on who we are and how we got here, an exploration made possible by the generosity of humans like you. ♪ [music] ♪ - [Jean-Jacques] Today I'd like to present you with some thoughts about Neanderthal evolution and to what extent climate might have influenced their evolution. But before I start with the climate and Neanderthals, I wanted to show you this slide presenting, on the left side, a Neanderthal, and a modern human about the same age. And in front, you have two skulls of extant apes, a bonobo and a common chimpanzee. And this is just to show you how Neanderthals are different from us in terms of anatomy, in terms phenotype in general. Modern humans and Neanderthal's ancestors diverged probably about half a billion years ago, whereas bonobos and chimpanzees diverge much earlier, probably somewhere between two and one million years ago. And one of the mysteries regarding Neanderthals is, what kind of evolutionary process was driving this very rapid divergence? The way we like to think of the Neanderthals- the way they are presented in the literature- is this way: humans adapted to a glacial environment, a peri-artic environment. As a matter of fact, if we have a look on this very jerky climactic curve, you're going to see quite a few times today I imagine, you can see that for the last half million years, 95% of the time the climate was colder than it is today in the area where Neanderthals live, mainly western Eurasia. This being said, the climate was not always glacial, the glacial episodes were rather brief, actually, the most extreme parts of these glacial episodes. And if you look on this map, this is a map showing the distribution of places where Neanderthals have been found, you see that actually they are not documented very highly in latitude. The northernmost Neanderthal ever found was found 52 degrees of northern latitude, which is not so high. Neanderthals lived also in places like Spain, and southern Italy, or the Levant, that never really witnessed really glacial episodes. So the question is what in their environment, first of all, drove their distribution, and also drove their evolution? The distribution that you see now is, I would say, misleading somehow because it is a palimpsest of the distribution of Neanderthals through a very long period of time. In other words, at a given point in the past, they never had this extension, so it's a sort of addition of many years of distribution. It is very likely they reach their easternmost extension in southern Siberia and southwest Asia only at some point in their late evolution. So speaking about climate and the influence of climate on evolution, we have quite a number of studies showing how climate can influence the biology and morphology of modern humans. One of the most spectacular features that relate to climate in extant humans is the body shape, in general. There are a number of studies showing that the proportions of the limbs, the shape of the trunk, varies with climate. Basically, people exposed to very hot climates need to cool their bodies, so they tend to be slimmer, have narrow trunks, and longer limbs. People exposed to very cold environments tend to be huskier, to have shorter limbs, wider trunks. This kind of study is a multi-variant study taking into account many populations. It shows how you can basically rank populations from the tropics- on the right side you have people from East and West Africa- up to the high altitudes, so in green you have European populations. So if you take measurements of the body shape of a Neanderthal and you plot it in this kind of chart-- this is the case for one Neanderthal very known called [inaudible 00:07:34]. It falls beyond any modern European and even beyond modern Inuits, so it is said to have a hyper-arctic body proportion. Interestingly, if you plot on the same chart early modern humans who came into Europe about 50,000 years ago to replace Neanderthals, they plot very close to populations from modern Sudan- which, by the way, it's certainly one of the best arguments to make that come out of Africa, besides genetical arguments. However, we should be very cautious with these features, because climactic adaptation is not just a biological adaptation in humans, it is also a cultural adaptation, a technical adaptation. In other words, we suspect that even if Neanderthals were not exposed always to very cold climates, because of the limitations of their technology, the biological response might have been higher than what we have in extant humans. And as a matter of fact, if we look at the archeological record, we find very few archeological sites left by Neanderthals in truly very arctic environments. It looks like during the coldest phases of the glacial episodes, large portions of Europe had been abandoned by the Neanderthals. There are other features that have been said to be related to climate in Neanderthals, especially their very peculiar facial morphology. They have a very strong nasal facial prominence, this very big nose projecting, and on the side of the nasal aperture, inside the face, you have these volumes which are sinuses, which.are said to be very developed in Neanderthals in general. In a sort of naive way, people have thought for a long time that the development of sinuses in Neanderthals were a kind of insulation against cold. This idea has been very criticized. Actually, it's completely abandoned today because we see more these sinuses as filling an empty space between other structures that are adapting to different functions. It is more interesting to look at another aspect of the face, which is the nose. Actually, if you look at extant humans, you will see that one of the most varying parts of the face is the nose and the shape of the nasal aperture. One of these skulls comes from Germany, and the other one from Zaire in Africa. And immediately you can see that the shape of the nasal aperture is very different in these two individuals. There is quite a number of studies showing that actually in humans, the nose, and especially the inner nose, is adapted to the climate conditions in different regions. Primarily what we have is a problem with cold and dry air. Individual populations that are exposed to cold and dry environments tend to have nasal cavities that are higher and narrower, in order to increase the turbulence of the air that is inspired, and to increase the contacts between the mucus tissues and this air to warm it and to moisten it. The nasal pharynx seems to be more depending on moisture, the nasal cavity itself with cold. So what about Neanderthals? Well, at first look, the Neanderthal seems to match very much this prediction, because they have this huge nasal aperture that is somehow unexpected if it was exposed to cold environments. Actually this nasal aperture is especially broad in its upper part, which is not what we find in modern tropical populations. But if we look inside the nasal aperture, we see that there are a number of structures that inflate the walls of the nasal aperture in order to narrow this nasal aperture. Although the nasal aperture is very broad outside, the cavity inside is much narrower and much more the prediction we would make about a cold-adapted population. Last but not least we have now, a number of information coming from paleogenetical studies, and I'm sure there are a much more to come in the future. But we know already that there are a couple of features of Neanderthals that we can relate to: the climate, the environment. And I would like at least to mention this gene called MC1R which is a receptor involved in the red hair and fair complexions. And very likely, at least on the Neanderthals on which this gene has been detected, we deal with populations that have light skin color and red hair. So we share some adaptations to the cold environment in Neanderthals, but the question is are there other effects of the climate on their evolution? I would like now to deal with something else, that I found probably more important than adaptation itself. One of the questions about Neanderthal evolution is, why do we have this divergence between an African lineage leading to us and this Eurasian line about half a million years ago? What happened at this moment? Why then, why not before? It raised the question of when exactly we have the first Neanderthals. And the first Neanderthals we have in the fossil recall are about 400,000 years old. They are found in England, they are found in the UK-- in Spain. And this age, a little bit above 400,000, has been for some time in conflict with dates that were provided by geneticists. Geneticists, using a molecular clock based on computations using the assumed time of divergence of fossil groups, came to much earlier younger ages for the divergence of Neanderthals and modern humans, something around 300,000. That was a bit problematic for paleontologists. But recently, because it's now easy to sequence the complete genomes of parents and children, we can compare this genome. It has been possible to find that the rate of mutation assumed by this molecular clock was not quite right. And new estimates came with a rate of mutation much more reduced, [inaudible 00:15:34] was initially thought. And this new rate of mutation is confirmed by the study of some fossil material- this is a femur of an early modern human found in western Siberia, for which we have the complete genome. We have the dating, it's 45,000 years old. So it's easy to compare the genome of this early modern human with extant Europeans and to have a notion of the rate of mutation along this lineage. It confirms this reduced rate of mutation that has been recently proposed. So it means that the time coalescence time required for Neanderthals and modern humans fits rather well this emergence in the phenotype, in the morphology, around 400 or 450,000. What has been going on in this time period? We have a list of features proper to Neanderthals that we see emerging through time by a process of accretion, and it's basically a shift in frequency of these features that we see more and more along time. About 200,000 years ago, in the isotopic stage seven, we have basically reached the Neanderthal morphology completely. So the story unfolds between, say, 450-- I'm talking about morphology here, and a little bit less than 200,000. And it goes at different speed, depending on the different anatomical areas, and we suspect that one of the mechanisms driving this evolution is not adaptation, it is not selection, it is something that geneticists call drift. And this drift is mostly depending on demography. So what is it about? It's simple. You have variability of a population in terms of genes and in terms of morphological features, and if you reduce the size of this population-- if you reduce it dramatically, and then re-expand this population, you are going to have, again, a large population, but with reduced variability just by chance. Just because only some of these features went through this bottleneck. And we have something like that with Neanderthals along the Neanderthal lineage- I could go through several features, cranial features, facial features. I'll just pick one example which what we call non-metrical dental features. And these non-metrical dental features have a frequency that increases along the Neanderthal lineage. We know they were part of the variability of Neanderthals of the middle Pleistocine hominids before the Neanderthal emerges, and they seem to be fixed a little bit by chance in Neanderthals and reach a very high frequency in later forms. So what could drive this evolution? We think this jerky curve that you saw several times already, in this period of time, say around 800 to 400,000, becomes even more jerky. And we have 600,000 years ago for the first time, first major glacial episode in western Eurasia. We think that this first major glacial episode resulted in, for the first time, an isolation of western Eurasia, and a dramatic reduction of the population living there. This is confirmed also, now, by paleogenetics using the high-resolution sequencing of Neanderthal genomes. It is possible to make assumptions on the evolution of the population size through time, and we see that contrary to what we have in the ancestry of modern humans, we have around five to 600,000-- dramatic reduction of the population size of this group. So the story unfolds this way: we have in the early Pleistocene western Eurasian hominids, we still see a lot of changes between southwest Asia, Africa, central Asia, western Eurasia. And with the isotopic stage 16, about 600,000 years, we have probably for the first time, this separation that matched the genetic data. We have another major bottleneck with isotopic stage 12, and soon after, this is when we have for the first time, Neanderthal features emerging in the phenotype of European hominids. And let's say 200,000 years later, after a number of bottlenecks, we have basically fixed this Neanderthal morphology. So to finish I would just like to say one word about Neanderthal extinction, and I think I-- I hope I convinced you that climate played a major role in the rise of the Neanderthals. The question is, did the climate play a role in the fall of the Neanderthals? There's a number of theories about that, that Neanderthals got extinct naturally before modern humans moved into Europe. What we think about the emergence of modern humans into Europe is a scenario that is a bit more complicated today than it was a few years ago. We think we have two major episodes of colonization of western Eurasia, one corresponding to what we call initial [inaudible 00:21:42] sometime around 48,000. And a later one for western Eurasia around 42 to 43,000. It has been argued that in this time period, the climactic curve is especially jerky, and that that would have driven the Neanderthal to extinction before-- or facilitate the replacement by modern humans. Well, I think when you look at this curve it is very difficult to see more jerkiness in this period than before. I think Neanderthals survived all sort of climactic changes before modern humans arrived in western Eurasia, and I think the main disaster Neanderthals had to face was not a climatic disaster: it was us. Thank you. ♪ [music] ♪
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Channel: University of California Television (UCTV)
Views: 50,400
Rating: undefined out of 5
Keywords: CARTA, anthropogeny, biology, climate, evolution, Jean-Jacques Hublin
Id: tFBbIzqIH08
Channel Id: undefined
Length: 23min 43sec (1423 seconds)
Published: Tue Jul 21 2015
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