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paleoanthropology, genetics and evolution

stable isotopes

  • Putting together australopithecine diets

    Sat, 2011-11-26 18:06 -- John Hawks

    Peter Ungar and Matt Sponheimer earlier this fall [1] reviewed the evidence for diet in early hominins, from both microwear studies (Ungar's specialty) and stable isotopes (Sponheimer's forté). I wanted to point to this article because it is a very useful short review that illuminates the cases in which these two sources of evidence lead to a single interpretation.

    [T]he isotope data also suggest enormous and unanticipated differences between contemporaneous taxa with strong morphological similarities, notably the “robust” australopiths P. robustus and P. boisei. Despite their attribution to the same genus, there is no overlap in their carbon isotope compositions (41), which is a rarity for congeners among extant mammals.

    Maybe this should give pause to those who insist that A. robustus and A. boisei are sister species. Ungar and Sponheimer here reiterate the observation that microwear is very similar between A. boisei and A. afarensis:

    The apparent continuity of microwear pattern through the putative lineage Au. anamensis–Au. afarensis–P. boisei could even suggest that morphological changes reflect increasing efficiency for grinding large quantities of tough food. Although living primates that eat tough items typically have sharp shearing crests, eastern African australopiths and especially P. boisei may have evolved a different solution for processing such foods, given the flattened, thickly enameled teeth of their close ancestors (23). Natural selection must work with the raw materials available to it. Thus, the present-day ecomorphological diversity within the primates may not be sufficient for making some paleoecological inferences, which is not surprising given that the vast majority of all primates, especially apes, that have ever lived are now extinct.

    This idea was raised earlier, for example in the context of the stable isotope findings on A. boisei ("'Nutcracker Man' debunked"). Until we have more stable isotope results from the known sample of A. afarensis or A. anamensis, we won't be able to test this "tough C4 food" hypothesis. "Ecomorphological diversity" refers to the match between food types and the topological properties of tooth crowns among living primates. Generally speaking, primates with high crowns and high cusp relief with shearing crests are thereby well-suited for eating tough foods like leaves and stems. That's the common ground between gorillas and colobines, for example. A. afarensis and especially A. boisei have exactly the opposite morphology from what would seem to be the "tough foods" pattern. So why do these species seem to be acting like grazers? Very peculiar.

    My own attitude is that if we can't clearly make sense of the anatomy of A. boisei, then we won't be able to untangle the diets of the other species. Early hominins evolved along a distinctive trajectory toward larger molars, smaller canines, and bigger jaw musculature within a common body plan. A. boisei represents the extreme of this trend. So if A. boisei is the logical morphological extreme, why does it seem to have such a different dietary strategy than every other hominin with stable isotope evidence?

    Meanwhile, if Ungar and Sponheimer are correct in asserting a common dietary strategy in the East African species, then it seems pretty clear that early Homo shares a dietary commonality with the South African species, not the East African ones. One might argue that Homo differentiated from other hominins within East Africa by adopting a fundamentally South African dietary strategy. But I would be more inclined to suppose a South African-derived hominin made incursions into East Africa, possibly repeated ones, as Homo was emerging. Ungar and Sponheimer are correct that natural selection works with the materials available. Population growth and migration are vastly more rapid than in situ evolution. What if the apparent "early Homo" record actually represents a series of successive dead-end migrations from southern Africa?


    References

    1. Ungar PS, and Sponheimer M. 2011. The diets of early hominins. Science (New York, N.Y.) 334:190-3.
    Synopsis: 
    A review of microwear and stable isotope evidence of diet prompts questions about early hominin relationships.
  • Finding the identity of animal (and plant) fats

    Sat, 2009-09-26 15:06 -- John Hawks

    Last week I made a note about some ongoing work at the Spanish site of El Salt, which suggested taxonomic identifications for burned traces of animal and plant fats.

    I was wondering how exactly that kind of identification is done. I don't know any details in the El Salt example, but I was able to find some recent work from Neolithic contexts that makes a similar kind of identification.

    For example, Oliver Craig and colleagues (2005) tested potsherds for fatty acid residues, and then subjected those residues to isotopic analysis. The isotopic composition of different weight fatty acids (C18:0 and C16:0) may have different carbon-13 fractions from each other, a relation that varies among different animal taxa. So basically, you fraction out the 18-carbon and 16-carbon fatty acids and measure the ratio of carbon-13 to carbon-12 in the two sample components.

    Craig and colleagues were able to show that milk fatty acids have a distinct ratio of carbon-13 fractions compared to body fat (adipose tissue) from the same taxa, basically milk has a lower carbon-13 fraction in the heavier 18-carbon fatty acids. They found most of their sampled potsherds to have a similar ratio, and interpreted that as evidence for the use of milk products in Neolithic central and eastern Europe.

    Last year, Evershed and colleagues (2008) came to a similar result, applied to potsherds from early Neolithic sites in the Near East. Evershed published a review article on organic trace analysis in archaeology last year, from which I've drawn this helpful figure:

    Figure 2 from Evershed 2008. Original caption: Simple saturated C16:0 and C18:0 fatty acids generated via hydrolysis of triacylglycerols (LHS) during processing and/or burial of fats (and oils), which on their own have limited diagnostic value as biomarkers. However, the plot (RHS) of the δ13C values for these fatty acids shows how the fats of the major Old World domesticated animals can be separated due to differences in the their metabolic and biosynthetic origins. The ellipses are confidence ranges (P = 0.684) and the theoretical mixing ranges. Such plots provide the basis for determining the origins of animal fat residues (adapted from Mukherjee et al. 2005).

    The references I've found distinguish fats by mammal taxa only by contrasting pig from ruminant, so I tend to interpret the references to "deer and goat" in the El Salt press report to the fact that they're the resident ruminants. Of course a finer statistical segregation based on more comparative sampling is also possible. Also, Evershed's review goes into some forensic contexts, and shows that human adipose tissue has its own distinctive signature. In theory that would make it possible to find evidence of cannibalism from prehistoric contexts.

    References:

    Craig OE, Chapman J, Heron C, Willis LH, Bartosiewicz L, Talor G, Whittle A, Collins M. 2005. Did the first farmers of central and eastern Europe produce dairy foods? Antiquity 79:882-894.

    Evershed RP. 2008. Organic residue analysis in archaeology: the archaeological biomarker revolution. Archaeometry 50:895-924. doi:10.1111/j.1475-4754.2008.00446.x

    Evershed RP and 21 others. 2008. Earliest date for milk use in the Near East and southeastern Europe linked to cattle herding. Nature 455:528-531. doi:10.1038/nature07180

  • Neandertals noshed on mammoth meat?

    Sun, 2005-07-31 00:07 -- John Hawks

    In an article in the Jul 2005 issue of Journal of Human Evolution, Hervé Bocherens and colleagues contribute new isotopic values for bone collagen from three Neandertals, a review of results from prior studies of Neandertal isotope ratios, and an interpretation of the values obtained for the Saint-Césaire specimen based on comparisons with contemporary hyena bones.

    The latter part of the study is the most interesting: the Neandertal bones have a substantially higher proportion of nitrogen-15 (15N) than the hyenas. This difference is assumed to come from a difference in the diet. The 15N levels of both species are much higher than plant-eaters, so the difference is apparently not the inclusion of some plant food by Neandertals. Instead, the difference must come eating animals with different 15N enrichment.

    But there are good reasons not to believe a word of it; read on for why.

    How it works

    I've discussed carbon isotope analysis before, click the link for details about how it is related to diet. The bottom line is that carbon-12 is preferentially taken up by plants during photosynthesis, but less so in grasses and certain other plants. Therefore the ratio of carbon-12 to the other stable isotope, carbon-13 is an indicator of the plant foods an animal (or its prey) ate.

    Nitrogen stable isotopes are slightly different. Plants vary in the uptake of nitrogen-15 (compared to nitrogen-14) depending on whether they obtain their nitrogen mainly from the action of symbiotic bacteria or whether they get it directly from nitrates in the soil. Proteins are nitrogen-rich, so that most of the nitrogen content of an animal comes from the proteins in the food it eats (Ambrose 1993). This results in a trophic level effect, with each level preferentially taking up a 2-4 percent higher proportion of 15N than its food.

    Previous studies of Neandertals have found that they have isotope ratios consistent with a high trophic level. This has been asserted to be evidence that Neandertals were hunters, and that they ate a very high proportion of meat compared to plant foods: upwards of 95 percent meat or more (e.g. Richards et al. 2000).

    The current study builds on those previous observations by comparing Neandertals in more detail with another carnivore (hyenas) and attempting to figure out the proportions of different meats necessary to arrive at the isotope ratios in Neandertal bones.

    From the discussion:

    The differences observed between the amount of different prey consumed by Neanderthal and hyaena provide insights about hunting strategies of Chatelperronian Neanderthals in Saint-Césaire. Spotted hyaena is an opportunistic predator and scavenger with dietary preference for large and medium size ungulates (e.g. Cooper et al., 1999 and Silvestre et al., 2000). The isotopic signatures of spotted hyaenas in southwestern France around 36,000 years ago indicate that horse was the most abundant prey species, whereas bison, aurochs, red deer, giant deer, and reindeer were relatively abundant, woolly rhinoceros were less consumed, and mammoth were the least consumed of large herbivores. Spotted hyaenas from Belgium and Great-Britain of the same age exhibit similar isotopic signatures (Bocherens et al., 1995 and Bocherens et al., 1997), suggesting that this dietary pattern probably holds for north western Europe. Among these available prey, Neanderthals consumed much less reindeer and much more rhinoceros and mammoth than hyaenas. The low proportions of mammoth and rhinoceros in the diet of hyaena, a famed scavenger, indicates that available carcasses of these large herbivores were relatively rare in the landscape. Thus, the high proportions of these animals in the diet of Neanderthals indicate that they were obtained through another strategy than simply scavenging. Active hunting of these large herbivores by Saint-Césaire Neanderthals is thus strongly suggested by the isotopic evidence. There is some zooarchaeological evidence of proboscideans and rhinoceros hunting by Neanderthals (e.g. Scott, 1980, Auguste, 1995, Auguste et al., 1998, Locht and Patou-Mathis, 1998, Bratlund, 2000, Patou-Mathis, 2000, Patou-Mathis, 1999, Conard and Niven, 2001 and Moncel, 2001). However, mammoth and rhinoceros remains do not dominate Neanderthal faunal assemblages even if they are usually present in small numbers (e.g. Patou-Mathis, 2000) (Bocherens et al. 2005:82).

    So why don't Neandertal sites have more mammoth bones in them? Most likely answer: how were they going to carry a whole mammoth bone anywhere?

    This discrepancy between significant consumption of very large herbivores by Neanderthals and the remains of very large herbivores being scarce in Neanderthal sites might be due to transport decisions: filleted meat could have been transported to the occupation sites, leading to an underrepresentation of the role of large-bodied animals in Middle Paleolithic diet (Rabinovitch and Hovers, 2004) (Bocherens et al. 2005:82).

    Niggling doubts

    Is there any reason to doubt the result? I would like to know more about the reasons for the isotopic differences among the herbivores. The carbon isotopes are a function of the intake of different plants: in particular, plants with different carbon cycles. Browsers like elephants eat mostly plants with a three-carbon photosynthetic cycle; this results in a low carbon-13 ratio. In contrast, grazers eat a higher proportion of grasses, which have a four-carbon cycle; this leads to a higher proportion of carbon-13 in the animals' bones.

    But what about the nitrogen ratios? These are generally interpreted in terms of trophic level. But what accounts for the extreme difference between the mammoths and the other herbivores? Richards et al. (2000) cite earlier work by Bocherens in suggesting that mammoths may have targeted certain plant species that had a higher 15N ratio. Maybe so.

    On the other hand, what if 15N enrichment were related to longevity in some way? Isotopic ratios in teeth differ from those in bones, presumably because infants before weaning are at a "higher trophic level," consuming only the mother's milk. Teeth develop early in life, therefore their isotope levels reflect the diet composition early in life. It is interesting that the two highest 15N ratios among the herbivores are found in woolly rhinoceros and mammoth. Could these ratios be connected not to diet but to development in these large, long-developing species? And if so, could Neandertals follow a similar pattern?

    Another wrench

    And there is the question of fish. In the abstracts to the Third International Mammoth Conference in 2003, Bocherens and colleagues had an abstract on the subject of Neandertals eating mammoth that included this line:

    However, an uncertainty remains about the possible contribution of freshwater fish, which may be similar in isotopic signature to mammoth meat.

    A full text search of the JHE paper yields the word "fish" zero times. So what happened with that? Fish have relatively high nitrogen-15 levels because the aquatic food chain is generally longer than the terrestrial one, and this high 15N ratio may also characterize aquatic birds (Richards et al. 2001). Likewise, freshwater ecosystems have relatively low carbon-13 ratios, because of the availability of carbon from geological sources. Richards and colleagues (2001) focus on the combination of high 15N and low C13 as an indicator of freshwater resource use. And the Neandertals are substantially lower in 15N than Mesolithic humans who used aquatic foods extensively (Richards et al. 2001). So would it take much fish to make Neandertals look different from hyenas? Probably not.

    My take

    It would be nice if the isotope people would get together and settle this little problem. Richards et al. (2001) found higher 15N in Upper Paleolithic Europeans than in Neandertals; they concluded an increase in aquatic resource consumption. But one might as easily assert that later Europeans ate more mammoth -- we do, after all, find a lot more mammoth bones associated with later sites than with Neandertals. How could you tell a high proportion of mammoth from a low proportion of fish?

    From these data you can't. The bottom line is that all these estimates are working on only two observations: carbon and nitrogen isotope ratios. But they are trying to estimate parameters along at least four dimensions: trophic level, aquatic vs. terrestrial, C4 vs. C3 plant consumption, and 15N plant selectivity (the explanation for the mammoth level). The computer graphic estimating the proportion of different animals in the Neandertal and hyena diets is especially silly: how can two observations estimate seven parameters simultaneously?

    A little luck restricts the range of possibilities a lot: Bocherens et al. (2005) can settle on a high mammoth consumption because only the mammoths as high in 15N than Neandertals. But even this requires a severe limiting assumption: that there were no aquatic resources in the Neandertal diet.

    With assumptions like that, who needs conclusions?

    UPDATE: An earlier reference by Drucker and Bocherens (2004) discusses the freshwater aquatic resources; I've discussed the story in a later post.

    References:

    Bocherens H, Drucker DG, Billiou D, Patou-Mathis M, Vandermeersch B. 2005. Isotopic evidence for diet and subsistence pattern of the Saint-Césaire I Neanderthal: review and use of a multi-source mixing model. J Hum Evol 49:71-87.

    Ambrose SH. 1993. Isotopic analysis of paleodiets: methodological and interpretive considerations. In Investigations of Ancient Human Tissue, edited by M. K. Sandford. Gordon and Breach Science Publishers, Langhorne, PA. pp. 59-130.

    Richards MP, Pettitt PB, Trinkaus E, Smith FH, Paunovic M, Karavanic I. 2000. Neanderthal diet at Vindija and Neanderthal predation: the evidence from stable isotopes. Proc Nat Acad Sci USA 97:7663-7666. Full text online

    Richards MP, Pettitt PB, Stiner MC, Trinkaus E. 2001. Stable isotope evidence for increasing dietary breadth in the European mid-Upper Paleolithic. Proc Nat Acad Sci USA 98:6528-6532. Full text online

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Neandertals

For years, I've worked on their bones. Now I'm working on their genes. Read more about the science studying these ancient people.

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Malapa

Just outside Johannesburg, the Malapa site is producing some of the most exciting finds in human evolution. This site is the headquarters of the Malapa Soft Tissue Project.