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paleoanthropology, genetics and evolution

France

  • Cro-Magnon 1, dating and mtDNA

    Fri, 2013-04-26 10:57 -- John Hawks

    I'm running through the new paper from Qiaomei Fu and colleagues [1] about Upper Paleolithic mtDNA genomes. Probably several readers were wondering, as I did, about this passage in the paper concerning Cro-Magnon 1:

    The exception was the Cro-Magnon 1 sample, which belonged to the derived hg T2b1, an unexpected hg given its putative age of 30,000 years [16]. Since the radiocarbon date for this specimen was obtained from an associated shell [16], we dated the sample itself using accelerator mass spectrometry (AMS). Surprisingly, the sample had a much younger age of about 700 years, suggesting a medieval origin. Consequently, this bone fragment has now been removed from the Cro-Magnon collection at the Musée de l’Homme in Paris. Attempts to directly date other remains from the Cro-Magnon type collection unfortunately failed. The good molecular preservation of our sample for both DNA and AMS dating, in contrast, suggests that this particular bone has a different origin from the other remains in the collection.

    Cro-Magnon 1 is one of the most recognizable Upper Paleolithic cranial specimens from Europe, and its date has often been questioned -- largely because the very early excavation of this site by Louis Lartet came early in the history of European prehistory, when many excavations proceeded without appreciating the stratigraphic complexities of sites.

    I have checked with Alain Froment and Johannes Krause on the status of this bone. The bone sample was taken from a tibia fragment that was not clearly associated with the rest of the collection. None of the Cro-Magnon human remains has yet yielded a radiocarbon date, and Alain indicates that the organic carbon is gone. So the current paper does not challenge the Cro-Magnon date, it merely subtracts an intrusive element.


    References

  • Paleoclimate and shifting Neandertal strategies

    Sun, 2012-06-24 05:49 -- John Hawks

    A new paper by Guillaume Guérin and colleagues in the Journal of Archaeological Science [1] provides a detailed chronology for the Neandertal site of Roc de Marsal (near Les Eyzies, France).

    The paper includes an interesting discussion, which focuses on the emerging picture of Neandertal technological strategies to a changing climate. In short, during the middle of Marine Isotope Stage 4 (around 60,000 years ago), the regional environment in southwestern France shifted. Before this time, the Neandertals in the area made Denticulate and Typical Mousterian industries and hunted a variety of large fauna including red deer, roe deer, reindeer and horse. After the shift to a mix of steppe and some boreal forest, the Neandertals hunted mainly reindeer, some horse, and made Quina Mousterian tools. As they discuss, this picture is now consistent with the stratigraphies of many sites in the region that preserve Quina Mousterian:

    In southwest France, Roc de Marsal Layers 7–9 are not an exception, as similar faunal patterns have been observed in other archaeological sites. It is striking to see that for sequences that span both Quina and Typical Mousterian, a number of similar features have been observed: first, Quina Mousterian layers are always on top of Typical Mousterian layers (Jaubert, 2010); second, Quina Mousterian is, in Dordogne, always associated with faunal remains dominated by reindeer; third, in the layers underlying Quina industries, fauna exhibits singular patterns combining “forest-adapted” (red deer and/or roe deer) and “cold open-air” species (reindeer).

    There is some more in the discussion about the palynological record and other regional climate indicators. The meta-archaeological perspective would point out that this is a perfect synthesis of the Bordes-Binford debate: There really were different cultural groups of Neandertals and they really did use these technofacies for different activities. What was necessary is the kind of systematic comparison among sites that shows Quina Mousterian systematically overlying the Typical/Denticulate wherever they occur, along with the evidence of climatic and faunal change across sites.


    References

  • Neandertals and eagle talons

    Mon, 2012-03-12 00:31 -- John Hawks

    Eugène Morin and Véronique Laroulandie have published a new paper in PLoS ONE demonstrating evidence that some Neandertals had a fetish for eagle talons [1]. From the conclusion of the (open access) paper:

    Because claws are inedible, the specimens presented here are not compatible with human consumption. This means that the tool-marked terminal phalanges found at Combe-Grenal, Les Fieux, Pech de l'Azé IV, and Grotta di Fumane were likely used as tools and/or as items of symbolic expression. Although the sample size is small, the fact that all the terminal phalanges that show cutmarks are from eagles argues against their utilization in strictly non-symbolic contexts. This last pattern is noteworthy because eagles are among the rarest birds in the environment, a pattern explained by their high trophic position in the food web [31]. This bias toward large and powerful diurnal raptors possibly indicates that the claws were used in symbolically-oriented contexts by Neanderthals, although the latter contexts remain to be more precisely defined. One possibility is that they were used as ornaments, as has been suggested for the Upper Paleolithic occupations (dated to ca. 20 ka) at Meged Rockshelter in Israel [32].

    This is reminiscent of last year's paper about intentional feather removal from raptor wings at Fumane Cave, Italy [2]. Morin and Laroulandie provide a table listing evidence of cut marked bird remains from Middle Paleolithic contexts across Europe. More and more, we are seeing these kinds of lists, as zooarchaeologists are synthesizing the behavior patterns evidenced by low frequency faunal remains from many sites.

    Raptor phalanges showing Neandertal cutmarks

    Figure 2 from Morin and Laroulandie, 2012. Original caption: "Stone tool incisions on terminal phalanges of diurnal raptors from Middle Paleolithic occupations in France. A) example of a fully fleshed golden eagle digit. B–G show cutmarked terminal phalanges from layer 52 at Combe-Grenal (B–C, golden eagle) and layers Jbase (D–E, white-tailed eagle) and I/J (F–G, white-tailed eagle) at Les Fieux. The black bars correspond to 1 cm. Philippe Jugie took the Combe-Grenal photographs, the others were taken by V.L."

    Unambiguous evidence for ornamentation by some Neandertals has long been known, but adding more clear evidence for the use of perishable materials helps to establish the pattern. More important, the present evidence from Combe Grenal puts the non dietary use of eagle talons back to 90,000 years ago, long before any Upper Paleolithic in the area. It's one thing when archaeologists document symbolic behavior in "transitional industries", because these arguably represent a more advanced conception of technology in some way. I am more interested in the recent expansion of our understanding Mousterian and similar industries in Europe.


    References

  • Bordeaux

    Tue, 2012-01-24 12:59 -- John Hawks

    I'm in Bordeaux for the rest of this week, taking part in the meetings of the Société d'Anthropologie de Paris. The city is just as beautiful as I remember!

  • Kids leave their traces in caves with art

    Sun, 2011-10-09 09:34 -- John Hawks

    Several stories last week related the story (from a conference talk by Jessica Cooney) about evidence that very young children had left finger grooves in the Grotte de Rouffignac. Alan Boyle's gives the most details: "Prehistoric kids left marks in caves".

    Like Lascaux, the 5-mile (8-kilometer) Rouffignac cave network has plenty of drawings, depicting mammoths, rhinoceroses, horses and even a cave bear. But Cooney focuses on a different kind of art: impressions left behind in clay or "moonmilk" — a soft, white, crystalline precipitate that forms inside limestone caves. The ancient artists created the impressions by pressing or dragging their fingers through the soft material on the cave walls. Those markings are what Cooney and her research colleague, Walden University's Leslie Van Gelder, used to estimate how old the artists were.

    Rouffignac is an immense cave network. The main tourist route into the cave involves riding on an electric train for nearly a kilometer into the hillside. One problem posed by the cave is that tourists have been coming into it for hundreds of years -- there is graffiti dating to the 18th century on the ceiling near some of the most famous artwork. But it is an amazing place, in part for that long history of people interacting with the very ancient art.

    Dale Guthrie's wonderful book, The Nature of Paleolithic Art, discusses the idea that children and adolescents were involved in making much of the classic "cave art" in Europe. The famous paintings and engravings with high levels of technical execution are really exceptional, and are usually surrounded or accompanied by vastly more numerous, cruder, representations. Many of those can be analogized to art created by children today, some of them actually occur in areas where children are the most likely artists. And already we know about children's footprints in some caves, and handprint-negatives sized for young people.

  • Combe Capelle redated

    Sun, 2011-03-20 14:13 -- John Hawks

    I missed this earlier this month, but Julien Riel-Salvatore did not: "Burial Site at Combe Capelle in France is Not as Old as Previously Assumed, by Several Thousands Years"

    After an initial sample of the famous skull failed to yield results in radiocarbon dating, a second sample was taken from a molar in the lower jaw for testing in June 2009 in Kiel. In previous cases, compact tooth enamel had shown better preservation conditions of the collagen needed for radiocarbon dating. A sufficient amount of collagen was able to be extracted after preparation and intense cleaning of the tooth substance. Subsequent analysis using accelerator mass spectrometry at the laboratory in Kiel assigned a date of 7575 BCE to the remains of what had previously been assumed to be an early Homo sapiens specimen, meaning earlier assumptions had been out by several thousands of years.

    This does not come as a surprise; the provenience of the skeleton has always been doubtful. It was unearthed by Otto Hauser in 1909. Excavations from a century ago were not often conducted with a fastidiousness for stratigraphy, Hauser being a prime offender. Remember this is three years before Piltdown; a time when finding "modern" looking skeletons in association with old archaeology could make someone's fame.

    There are some great pictures of the discovery and Hauser posing with the bones, at the Past Horizons site.

  • LIFE photo-essay at Lascaux, 1947

    Wed, 2010-09-15 08:30 -- John Hawks

    A LIFE magazine photo-essay brings 15 previously unpublished pictures of Lascaux by Ralph Morse, who was the first professional photographer to enter the site: "Inside Lascaux: Rare, Unpublished."

    "LIFE re-opened its Paris bureau after the second World War ended, in the same offices we rented before the war" Morse recalls. "One day we get a message from New York about some cave that people have been talking about. We do a little research, and find out that even though the cave was discovered a few years before, no one's ever photographed the paintings. In fact, hardly anyone has ever been down there, except some guys who climb around in caves for fun. We know that the first thing we need is a generator to power our lights, but getting a generator anywhere after the war was almost impossible. We had to have people in London ship one over. Once it arrived, we were ready to go."

    This is starting to seem like "cave art" week around here, but there have just been a lot of interesting links.

    (via Savage Minds)

  • Arthouse cave art

    Tue, 2010-09-14 16:24 -- John Hawks

    A new film to debut at the Toronto Film Festival is a 90-minute 3-D exploration of Chauvet Cave, directed by Werner Herzog. The LA Times reports on the film: "Is Werner Herzog's new 3-D documentary a huge forward leap or total folly?"

    For Herzog, 3-D was the perfect tool to capture the drawings, since after all, the cave that held the drawings was akin to a modern-day theater or gallery where primitive people could view, by torchlight, this mysterious new form of art. "Once you see the cave with your own eyes, you realize it had to be filmed in 3-D," Herzog says. "I've never used the process in the 58 films I made before and I have no plans to do it ever again, but it was important to capture the intentions of the painters. Once you saw the crazy niches and bulges and rock pendants in the walls, it was obvious it had to be in 3-D."

    I really hope it comes to Madison. I think this is a great use for 3-D. Truly some aspects of the cave art depend on the actual 3-dimensional form of the underlying rock. Ninety minutes is a long tour, and I hope that the film uses the time to explore the place -- not jam it with speculative narration.

  • French Neolithic discontinuities

    Sun, 2010-08-22 19:47 -- John Hawks

    Marie-France Deguilloux and colleagues [1] present a short analysis of ancient mtDNA recovered from a Neolithic burial at Prissé-la-Charrière, between the Loire and Garonne valleys of western France.

    The mtDNA sample in the end was only three individuals -- one haplogroup X2, one U5a and one N1a. Each is intriguing, as far as a single sequence can be, because all are rare or absent from France today. I think one shouldn't go far interpreting three samples, but they contribute to the view that Neolithic mitochondrial variation in Europe was very different from recent Europeans. The N1a and U5b sequences fit within the already-known Neolithic (and for U5a, Mesolithic) variation in central and northern Europe.

    It is from the U5a that Deguilloux and colleagues make a point about possible Mesolithic population continuity.

    Subhaplogroup U5b has also been encountered in German Neolithic remains from the Corded Ware Culture (Haak et al., 2008) and in the hunter-gatherers studied by Bramanti et al. (2009), although in both instances, the branches concerned were distinct from the U5b in the Prissé sample. It is, however, worth noting that haplogroup U5 has been encountered in surprising frequency in the hunter-gatherers studied by Bramanti et al. (2009) and could correspond to a Mesolithic heritage.

    The story of N1a is that it was very common in the central European Neolithic, even though it is very rare today. That was first noted by Wolfgang Haak and colleagues [2], and has in subsequent years been joined by the observation that the pre-Neolithic hunter-gatherers had yet other common haplogroups. The population history of Europe was a lot more interesting than we suspected 10 years ago.

    Deguilloux and colleagues attempt a conservative explanation for the frequencies of N1a in Neolithic samples:

    The widespread distribution of the N1a lineage in Early and Middle Neolithic northwestern Europe may indicate genetic continuity from Mesolithic populations. This scenario would support a Mesolithic contribution to the earliest Neolithic of Atlantic Europe. This would imply that the N1a lineage was already common in indigenous north European populations and that the spread of the Neolithic was principally the result of cultural diffusion. Although so far the N1a lineage has not been encountered among late European hunter-gatherers in central and north Europe (Bramanti et al., 2009; Malmström et al., 2009), it is worth noting that less than half of the hunter-gatherers' paleogenetic data come indeed from the pre-Neolithic period (predating LBK expansion). Finally, no paleogenetic data currently exist for the Mesolithic period in Western Europe. This prevents any conclusion being drawn about N1a occurrence during the Mesolithic period in those regions.

    I will note this -- the more that N1a is replicated across the Neolithic of Europe, the less and less likely that its subsequent vast reduction in frequency could result from genetic drift. When there was only one or two samples from Central Europe with high N1a, it was at least possible that this was a local founder population that did not spread its mtDNA diversity very far. If it were localized, even in the central Danube (a fairly big region) it might be possible to maintain that the later decline of N1a to its present low frequency had been due to population replacement.

    Now N1a seems like a real marker of the LBK, spread widely into Western Europe. It may be, as Deguilloux and colleagues suggest, that it will be found at substantial frequencies in earlier samples somewhere in Europe. We do want some explanation for how it got to be common in this culture area.

    Dienekes has written about the study. His point is a good one: If N1a were present somewhere in pre-Neolithic Europe, it would require some kind of "partition" of the pre-Neolithic population, along with its propagation -- presumably southeastward -- into the LBK of central Europe. Seems doubtful.

    The study includes an illuminating paragraph about the sources of contaminating sequence in these Neolithic extractions.

    Strict precautions were followed during all procedures (including precautions during excavation) and proved to be effective, because all researchers who directly participated in this study (from people working in the field to those working in the laboratory) were genotyped and their sequences were never observed during analyses. However, European sequences were randomly found in clones (28% of the sequences obtained). These specific sequences are regularly observed in the laboratory, whatever the project tackled (including samples from Polynesia or South America), in clones from samples or negative controls. They are not reproducible for a specific sample and are different from researchers' sequences. These facts lead us to suspect the contamination of PCR reagents (Leonard et al., 2007). It was relatively easy, however, to discard those contaminating sequences from our analyses because they were largely in the minority when compared with endogenous sequences.

    It would not be very difficult to compare the results from different labs and do a forensic-quality analysis of these reagent contamination events. Surely a good fraction of ancient DNA results prior to the last few years must represent such contamination. Nowadays people have the expectation that Neolithic-era remains may have rare or exotic haplogroups, but it hasn't been so long since people assumed that French equals French. I expressed some concern about this criterion before -- "strange" stands in for "non-contaminated" in too many studies.

    It might be very helpful to have a paper outlining the actual contamination pathways that have been found to affect multiple labs. Then the results could be compared against reports that have come out over the years. If people are reluctant to cull doubtful ancient DNA results, at the very least they can target a set for replication studies.


    References

    Synopsis: 
    Study of mtDNA from a Neolithic-era burial in France contributes to an overall picture of Neolithic population replacement in Europe

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