john hawks weblog

paleoanthropology, genetics and evolution

Tanzania

  • African Homo erectus

    Tue, 2011-11-08 00:14 -- John Hawks
    Synopsis: 
    African specimens from the Early Pleistocene are compared

    This station includes several casts of early fossil Homo erectus, from the Early Pleistocene of Africa. These include:

    • OH 9, from Olduvai Gorge, Tanzania, around 1.2 million years old.
    • KNM-ER 3733, from Ileret, Kenya, 1.65 million years old.
    • KNM-ER 3833, from Koobi Fora, Kenya, 1.6 million years old.
    • KNM-WT 15000, from Nariokotome, Kenya, 1.5 million years old.

    In addition to these specimens, the station has a few comparative casts from earlier hominid species and from other parts of the world.

    What to do: First, consider the issue of sexual dimorphism in these specimens. Which are male and which are female? What features lead you to that conclusion?

    Second, why are the differences between these specimens and Homo habilis, for example, KNM-ER 1813, reflective of a species distinction, instead of sex?

  • The Laetoli footprints

    Fri, 2011-09-02 00:53 -- John Hawks
    Synopsis: 
    A lab exercise in making footprints to compare to the Laetoli G footprint track.

    The most striking piece of evidence for bipedality in our earliest hominin relatives is a series of footprint trails at Laetoli, a fossil-bearing site in Tanzania. The longest trail, known as trail G, was made by at least two individuals, one much larger than the other. These individuals were probably members of a species called Australopithecus afarensis, with fossil remains that have been found in other parts of the Laetoli area from nearly the same time, 3.5 million years ago. This species lived long before any that scientists call humans, they are different from us in many, many respects. But the evidence shows that they walked bipedally in a very humanlike way.

    Studying these footprints poses many challenges to scientists. Their shape should give us clues about the shape of the feet, the way they struck the ground, the length and pattern of steps. Probably the most obvious aspect of these footprints are the big toes, which were aligned more or less with the other toes. This is a very different shape than a chimpanzee or gorilla foot, in which the big toe is relatively short and diverges from the foot, and the other toes are long and curving. Nevertheless, the toes of A. afarensis were not quite the same as ours, as you can compare as you make your own footprints.

    A comparison of one of the Laetoli footprints (bottom) with a footprint from a later site attributed two modern humans (top and middle). The human (middle) is walking with a bent-knee, bent-hip (BKBH) gait, not a normal gait for a person. The image shows the depth of different parts of the print. From a research paper by David Raichlen and colleagues [1].

    This lab station has you making footprints, to see how you might study the shape and conditions under which the Laetoli footprints were made. As you make footprints, try to use different styles of gait. Move fast or slow, maybe try to simulate a running step. Can you rule out some patterns of movement for the makers of the Laetoli footprint trail?


    References

    Study questions: 
    1. What kind of locomotion can you imagine would be intermediate between human-like bipedality and ape-like quadrupedality?
    2. One of the main points of contention about the Laetoli footprints is whether they preserve human-like arches in the midfoot. What do your comparisons indicate?
  • "Nutcracker Man" debunked

    Tue, 2011-05-03 00:44 -- John Hawks

    This week, Thure Cerling and colleagues report in PNAS [1] carbon stable isotope data from 24 specimens of Australopithecus boisei. This is a huge sample as fossil hominins go, and they give a very consistent picture about the diet of this most robust of the australopithecines. These 24 individuals got between 61 and 91 percent of their carbon from grasses.

    My 2005 explainer on stable isotope chemistry and early hominin diets fills in the details about carbon-12, carbon-13 and their relationship to 3- and 4-carbon photosynthetic cycles. The salient aspect of the comparisons involving A. boisei here is that C4 plants, mostly grasses, incorporate relatively more carbon-13 than do other plants, and herbivores assimilate this carbon-13 into their bones and teeth.

    The high ratio of grass-derived carbon in A. boisei is fundamentally different from all living and fossil apes, and it is far higher than the values found for other early hominins. The only other primate that comes close is the fossil giant gelada Theropithecus oswaldi, a savanna-living species.

    What were these extinct species really eating? Was grass the food? For living geladas, grass consumption includes seeds -- a fact that led Clifford Jolly to suggest that early hominins might also have specialized on seeds [2]. Of course, humans today also specialize on grass seeds. We call them grains, eat them in bread and drink them in soda. And beer.

    But what about A. boisei? The large, thick-enameled premolars and molars, with their low cusps, seem well suited to grinding small hard objects and resisting the resulting wear. But Cerling and colleagues devote a good chunk of their discussion to the description of molar wear in A. boisei and other early hominins. Their argument is that the teeth of A. boisei show no signs of "hard object" feeding:

    Of perhaps greater moment than its potential specific simila- rities, the microwear of P. boisei molars, which shows remarkable uniformity over time from about 2.3 Ma to about < 1.4 Ma (9, 24), stands in stark contrast to the wear fabrics exhibited by primate hard-object consumers. Indeed, there is no evidence beyond the anecdotal [e.g., the broken left first permanent molar crown in the KNM-ER 729 P. boisei mandible (8) and the observation that a couple of P. boisei molars show antemortem enamel chipping (25)] that these food items were hard.

    These observations are not new, but putting them together with the evidence of grass consumption makes it pretty clear that seed eating was not a predominant source of dietary carbon. The "Nutcracker Man" sobriquet, applied to A. boisei because of its powerful jaw mechanics, must be false. No significant hard object feeding, very low dietary carbon from trees and non-grassy (or sedgy) plants.

    Instead, Cerling and colleagues propose that both A. boisei and other early hominins wore their teeth on the, well, grassy parts of grass.

    P. boisei cheek teeth display notable gradients of gross wear, resulting in large, deeply excavated dentine exposures, and in this regard, they are similar to other australopith species (e.g., A. afarensis and A. africanus) that also possess low tooth cusps with thick enamel. Thus, like other australopiths, P. boisei undoubtedly had a diet that consisted of foods with abrasive qualities—the gross wear is as likely due to repetitive loading of phytolith-rich tough foods as exogenous grit. Thus, either grass or sedge consumption and/or exogenous grit might well have contributed to P. boisei’s notable wear gradient.

    And:

    Recent dental microwear studies suggest that the mechanical properties of A. afarensis (and A. anamensis) diets were nearly identical to those of P. boisei (9, 24, 40–42). If this is so, could it be that the australopith masticatory package represents an adaptation to C4 resources such as grasses or sedges? The similarity in dental microwear fabrics among the eastern African australopiths, all of which lack any evidence for hard-object food consumption (9, 24, 40–42), is consistent with the notion that their craniodental morphology could reflect “repetitive loading” rather than hard-object consumption (7, 8, 43).

    Grit might get in from eating underground parts like rhizomes. Phytoliths are small, hard silicate structures in the green parts of plants, including the stems and leaves of grass.

    Last year I wrote about carbon isotope analysis of two specimens of Australopithecus boisei, the famous OH 5 "Zinj" specimen, and the Peninj mandible. Both specimens show evidence of a high consumption of grass-derived carbon -- estimated at 77% and 81% grass-derived carbon, respectively. Those levels are characteristic of grazing animals. Cerling and colleagues show that these values are right in the middle of the range among specimens of A. boisei that cover a half million years in Kenya and Tanzania.

    In the paper reporting the carbon stable isotopes of OH 5 and Peninj, van der Merwe and colleagues [3] suggested that A. boisei may have relied on papyrus as a staple. The culms and rhizomes of papyrus both have substantial nutritional content but are very fibrous and require much chewing and spitting out fiber at intervals. The hypothesis would imply that A. boisei relied on these foodstuffs for the majority of its calories.

    Cerling and colleagues do not mention papyrus, and take a much more direct approach on grass-eating. But they do report data on oxygen stable isotopes from the specimens that may be relevant to the ecological context of grass (or sedge) consumption. Oxygen isotopes in bone and teeth reflect the pattern of water consumption by an animal. Oxygen-16 evaporates and transpires preferentially from leaves, so an animal living in an arid environment that gets most of its water from plants will be relatively enriched for the heavier oxygen-18. An animal that depends on drinking water from lakes or rivers will tend to have lower oxygen-18. A. boisei is almost as low in oxygen-18 composition as hippopotamus, suggesting they were strongly dependent on water sources.

    A highly water-dependent grass-eating A. boisei is a very different picture of the biology of this robust species. The South African robust species, A robustus, is very different in this regard. These two species are often lumped together, but this is unfair in many ways to their distinctive anatomical patterns. Knowing that their dietary adaptations were very distinct, we should be more inclined to focus on the details where they differ.

    Bottom line: A. boisei represents a highly distinctive dietary pattern, not present in any living ape, that no longer exists. At least the giant gelada, T. oswaldi, may also have exploited similar resources. Some grass resources, including papyrus corms and rhizomes, have high caloric and nutritional value, but require adaptations to deal with the fibrous content.


    References

  • Papyrus and A. boisei

    Fri, 2010-06-11 17:20 -- John Hawks

    I've had on my stack for quite a long time, a short paper by Nicholas van der Merwe and colleagues, assessing the stable carbon isotope ratios in several specimens from Tanzania. These include the Homo habilis specimens OH7, OH62 and OH65, and the A. boisei specimens OH5 and the Peninj mandible.

    The ratio of stable carbon-13 and carbon-12 enable an assessment of the amount of C4 versus C3 plants in the diet. I discussed the basic ideas in a longer post from 2005.

    The results on the Homo specimens are not too surprising. All three specimens overlap with South African A. africanus. OH7 and OH62 in particular have values around 20% C4, which is right near the mean observed for South African Homo and A. robustus from Swartkrans. OH65 has a higher C4 percentage than the other two, but within the range observed for Sterkfontein Member 4 A. africanus, which was significantly higher than Makapansgat or the other South African samples. So it would appear that the diet of Homo habilis did not differ from earlier hominins in terms of the ultimate origin of carbon in grasses versus non-grass plants.

    What is more surprising is the extremely high amount of C4-derived carbon in OH5 and Peninj. They score 77% and 81% C4, respectively. These are the only two specimens of A. boisei for which these stable isotopes are known, and they are very far from the observed range in the South African A. robustus.

    The authors suggest an interesting source for this high C4 proportion -- papyrus. They described a tasting tour of the wild plants of the Okavango:

    Bamford and van der Merwe investigated (and ate) the edible plants of the Okavango Delta in Botswana during the dry season (July 2003), assisted by Ezaya Karesaza, a tourist guide who grew up in this extensive wetland. Among the C3 plants that are traditionally eaten raw in this region are a variety of fruits and seeds, as well as plants of which the leaves and rhizomes are eaten. The latter include Aeschynomene fluitans, a floating legumi- nous plant, of which the leaves taste like lettuce; Typha capensis, which grows in thick stands along the water’s edge, of which the rhizomes have a pleasant taste; and Schoenoplectus corymbosus, a big water sedge, of which the stem is succulent at the bottom end. Among C4 plants, the rhizomes and culms of three other species of sedges are edible. These include Cyperus denudatus and C. dives, which grow in the grasslands of the floodplains. Unlike the grasses, they are green year-round, although not particularly prolific. The most common C4 sedge, by far, is Cyperus papyrus, which grows in dense thickets along the water edge. This species has culms as high as 4 m, of which the lowermost 0.5 m is frequently chewed by local people. It has a soft, white rind about 0.5 cm thick; the interior, about 2 to 3 cm in diameter, is more fibrous. It is chewy and pleasant tasting. The thick rhizome of papyrus is more fibrous and starchy than the culm, somewhat astringent, and requires considerable chewing effort. It produces a bolus in the mouth that has to be spat out at intervals.

    They then reported the results of a nutritional analysis of the papyrus culm and rhizome, which have roughly the nutritional and caloric value of domestic potatos, although would require a significant gut flora to deal with the cellulosic content.

    All in all, it's very curious that A. boisei is so different in these isotopic values compared to other early hominins. The theme was picked up last year in a paper by Richard Wrangham and colleagues, who focused on the idea of "fallback foods" -- the kinds of foods that an animal does not prefer, but eats when other more highly preferred foods are not available. Considering the very high C4 proportion indicated by the OH5 and Natron isotope values, it doesn't seem likely that this reflects a fallback strategy, but possibly an initial exploitation of such resources as fallbacks facilitated a later, more developed adaptation to them.

    Related posts:

    "Chemistry and early hominid diets"

    "Robust australopithecine diet ablated"

    "Average diet versus extreme diet in robust australopithecines"

    References:

    van der Merwe NJ, Masao FT, Bamford MK. 2008. Isotopic evidence for contrasting diets of early hominins Homo habilis and Australopithecus boisei of Tanzania. S Afr J Sci 104:153-155.

    Wrangham R, Cheney D, Seyfarth R, Sarmiento E. 2009. Shallow-water habitats as sources of fallback foods for hominins. Am J Phys Anthropol 140:630-642. doi:10.1002/ajpa.21122

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