john hawks weblog

paleoanthropology, genetics and evolution

Australopithecus

  • Bipedality and the pelvis

    Mon, 2011-10-31 23:02 -- John Hawks
    Synopsis: 
    Laboratory exercise introducing the features of the pelvis related to bipedality in hominins.

    Humans are bipeds. The pelvis in humans has undergone radical changes in orientation and shape compared to other anthropoid primates. Many of these changes serve to adapt our muscle orientations to the requirements of upright stance and bipedal locomotion.

    The most significant changes to the pelvis in humans compared to other apes are:

    Ilium
    The ilium (top portion of the innominate bone) in humans is shorter and broader. It curves around the trunk, whereas in apes it is flat against the back of the trunk.
    Greater sciatic notch
    This is very wide in apes, a function of their long, tall ilium. In humans, the notch is actually a notch.
    Anterior inferior iliac spine
    This feature is prominent in the hominin pelvis, absent or small in apes.
    Sacrum
    In humans, the sacrum is broad and short, in apes it is narrow and long, usually incorporating 6 or more sacral vertebral bodies.

    What to do: This station has four pelvic bones from the species Australopithecus africanus, which existed around 2.6 million years ago in South Africa. Assess the anatomy of these bones in comparison to humans, chimpanzees and gorillas. Are these the pelvic bones of a biped? What features point to your conclusion?

    In addition, the plaques at the front of the room have the near-complete skeleton of a fossil species, Oreopithecus bambolii, found in Tuscany and Sardinia around 8 million years ago. Look carefully at the pelvis of this skeleton. Does it resemble the living apes or humans? Does it look like Australopithecus?

  • Aging juvenile fossil hominins

    Tue, 2011-10-25 00:27 -- John Hawks
    Synopsis: 
    Laboratory exercise giving the opportunity to examine the development of juvenile hominin jaws.

    The fossil record is not made up only of adults. We have abundant skeletal evidence from juvenile individuals of a broad range of ages. At this station you will find model mandibles and maxillae from human children of a range of ages. These provide a comparison for the casts at the station, each of which represents a fossil hominin specimen from Africa, between 3.6 million and 1.5 million years ago.

    The mandibles represent several different species. They include:

    1. OH 7, from Olduvai Gorge, Tanzania. This is the type specimen of Homo habilis, around 1.75 million years old.
    2. MLD 2, from Makapansgat, South Africa. This is an early specimen of Australopithecus africanus, around 2.7 million years old.
    3. LH 2, from Laetoli, Tanzania. An early specimen of Australopithecus afarensis, it is around 3.6 million years old.
    4. SK 47, from Swartkrans, South Africa. This is a juvenile specimen of Australopithecus robustus, around 1.5 million years old.
    5. A selection of other mandibles, including some adult mandibles of the same species, is also available. Examine these in comparison with the modern dental models. Which teeth are present in the fossil specimens? What teeth are in the process of eruption? What do they tell you about the ages of the individuals?

  • The Malapa Soft Tissue Project FAQ

    Sat, 2011-09-03 17:07 -- John Hawks

    These are a few of the questions that I think are essential to understand our aims with the project and how we expect it will unfold. The future depends on what we hear from people with their ideas about how to analyze this unique evidence. I'll be updating this FAQ as we learn more about the samples. This is an open science project, and we'll be reporting on some results as they occur. But it all depends on people's participation.

    If you've arrived at this page from outside the site, here's a link to the main project headquarters.

    How did the project come about?

    When I was in South Africa in July, Lee Berger gave me an extraordinary overview of the discoveries from the new Malapa site. Embedded in the breccia that surrounded the cranial remains of MH1 and MH 2 are some relatively small, thin layers that visually appear to be organic (relative to the surrounding matrix). Under a light microscope look like they could be mineralized or preserved soft tissue. They do not appear to be skin impressions within the matrix, they appear to be thin layers that are a different substance from the surrounding matrix.

    Naturally these are incredibly interesting. But it is not obvious what will be the best way to establish what they are, and what we can learn from them.

    Lee suggested that this would be an ideal test case to see if open science can help solve a problem in paleoanthropology. We want to reach the people with the best ideas and ability to test hypotheses about these objects, and we don't know in advance where the answers will come from. That's the nature of the project: finding the right people and making the science happen.

    What do we want people to do?

    We want the best suggestions about how to evaluate this unique evidence and how it can test hypotheses about human evolution. We're reading all the suggestions sent to skin@johnhawks.net.

    We're especially keen to make contact with people who have the ability to make their suggestions happen. Some people out there have the knowledge to apply highly specialized analytical methods to samples like this. We want people like that to get involved with this project.

    Some people out there may have comparative samples that will be key to interpreting this evidence. How can tissue be preserved in a context where breccia is forming? Was there natural mummification or some kind of anoxic environment? To answer those questions, we need people who study the response of tissue to those contexts and who know the right samples to examine.

    Berger's team working on the Malapa hominins have access to much of the best technology. Micro-CT, microscopy, virtual dissection, chemical analysis, any of these things and more can be brought to bear.

    There's a lot more to this project than simply verifying (or refuting) that this stuff is soft tissue evidence. We need to know how it formed. If it's not soft tissue, we want to identify what it is, because there will almost certainly be more of it as the site is excavated and more specimens are prepared. If it is soft tissue, we need to know how it may have been changed as it was preserved, whether through drying, soaking in anoxic conditions, mineralization, or some combination of processes.

    We think the process of finding this out is even more exciting than knowing the result. We hope many of you see it the same way.

    If you write to us, you can expect that we may make your suggestion part of the website. This is an open project, and while we will be posting selectively, we will be sharing information as it progresses.

    Why would somebody want to participate in an open science project like this?

    We want to do the science right. We hope many people out there share this goal. It's a tremendous chance for people who don't normally operate within paleoanthropology to help us discover something fundamentally new about our evolution.

    People who perform analyses or contribute samples as part of this project happen will be full participants in the science and coauthors of any resulting publications. We want people to work together on this, and we think the best science will result from bringing together the best ideas and comparisons.

    How will the project work?

    That depends on what great ideas we hear from people. Lee's team will be carrying out analyses on these samples.

    Rachelle Keeling is coordinating the study, doing the research on what should be done, and what it will tell us about the samples. She and I will be reviewing the e-mails that the project receives, and will try to determine which approaches are feasible, and which order they should be carried out.

    As you send in ideas about what should be done, the more detail you can include about the analytical methods you can provide, the better. How much material (if any) does the method require? What hypotheses can the method test, or what information can it provide about the samples? How much time and preparation is required?

    If you have comparative samples that may be useful, what kinds of observations can you make on them? Can you point to references that have also used these samples?

    In other words, we want a bit of a plan if you can provide it. If you need more information from us to see if it's feasible, let us know -- we may be able to answer it, or have some team members carry out steps in advance.

    The project will be carried out over the next year, so the sooner we hear from you, the better!

    What is the Malapa site?

    Malapa is a cave site outside Johannesburg, South Africa, in the area where many other sites preserving remains of early hominins have been found. I have a Malapa page that gives a short introduction and links to many stories here about the fossils found at the site. I visited the site in July, 2011, and posted a narrative of the visit ("A visit to Malapa") that gives a good overview and several photos of the general area.

    Two of the most complete hominin skeletons ever described, both dating to 2 million years ago, have been discovered and described at the site. The site additionally includes further fossil materials that are still undergoing preparation and study. It is one of the most important fossil discoveries ever made in paleoanthropology, and will continue to produce new evidence about our origins for many years to come.

    How was the possible soft tissue evidence discovered?

    So far, the team at Wits has been working on breccia blocks recovered from the surface at Malapa. There has been no excavation yet at the site. The possible soft tissue evidence was discovered during the course of scanning and preparing these breccia blocks.

    The blocks are packed with bones. Many recognizable bones jut from the surfaces of the breccia, from antelopes, carnivores, small baboons and hominins. In several cases, hominin bones were recognizable at the surface, and these blocks were CT-scanned very early in the process of study and preparation. Scanning gives the preparators knowledge of what lies beneath their drill bits. In some cases, the best course of action is to leave the bones embedded within the breccia matrix, for further study by micro-CT.

    CT scan of Malapa MH1 cranium

    Initial CT scan of the MH1 cranium embedded in matrix block.

    In the initial CT-scanning of the MH1 cranium, team members noticed an area where the matrix surrounding the skull appeared irregular. As they prepared this out, it became clear that the breccia itself had pulled away from the cranium across a small region, and the breccia had a thin layer of material at its surface there. This is not the outer table of the bone (which is intact in the corresponding area), nor is it apparently an impression of the bone.

    Malapa MH1 breccia block with possible soft tissue

    Photo of breccia block including MH1 cervical vertebra (top). The smooth area, center, is a thin layer of candidate soft tissue on the surface the breccia.

    An additional section of possible soft tissue emerged as the female MH 2 mandible was prepared.

    Upon magnification, these pieces do appear to have a structure. As yet, no dissection or further sampling has been attempted. The team has no committed opinion about what these represent or how they were formed, other than that they do not appear to be simple impressions in the surface of the breccia. Disproving that they represent soft tissue may be just as interesting as demonstrating it, because either way we will discover important facts about the preservation and formation processes of this unique site.

    How could soft tissue possibly be preserved from 2 million years ago?

    Like other South African cave sites, the Malapa fossil hominins were preserved within a breccia, a cemented stone material packed with fossils, rock fragments, and other material. The Malapa breccia represents a remarkable snapshot of time, when hominins and other animals fell into a "death trap" and their complete skeletons were preserved.

    It is clear that Malapa preserves an extraordinary density of hominin remains, with nearly complete skeletons and articulated parts. These skeletons do not appear to have been disturbed after the bodies entered the site. Some plant and insect remains are preserved in the breccia as well.

    Beyond this, any explanation so far is speculative. If there was water in the site, which seems likely, it may have included an anoxic layer that preserved some of this material. A major goal of the project will be testing different hypotheses about the preservation environment of these fossils, to try to explain what these substances may be.

    Are you telling us everything?

    :)

    Synopsis: 
    The Malapa Soft Tissue Project is an experiment in open science, trying to uncover new facts about a unique discovery.
  • Sink Australopithecus!

    Mon, 2010-08-16 14:36 -- John Hawks

    Dennis Etler has been going great guns on his blog, Sinanthropus.

    Last week's article claiming cutmarks on A. afarensis-aged fauna from Dikika (Australopithecus afarensis used stone tools) got Dennis to write a provocative post: "Its time to sink the genus Australopithecus redux."

    Either A. afarensis should be revised to H. afarensis or the possibility must be entertained that the Woranso-Mille individual and the maker of the stone tool cut marks at Dikika represent a new previously unknown species of Homo (perhaps H. antiquus Ferguson 1984) that lived contemporaneously with A. afarensis.

    He mentions the relevance of the Woranso-Mille skeleton (which I haven't yet gotten to here) and A. sediba for this conclusion. Etler's earlier post, "It's time to sink the genus Australopithecus" goes into more detail on these remains.

    To me, the key question is whether Homo as we understand it now (including H. habilis) is polyphyletic. One way to escape this question is to narrow our genus, placing H. habilis and its ilk into Australopithecus. But Australopithecus defined broadly in this way is almost certainly paraphyletic. And that's without considering the issue of robust australopithecines. I can see why one might follow Ernst Mayr and stick them all in Homo.

  • 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

  • Malapa synchotronic

    Tue, 2010-04-13 09:41 -- John Hawks

    More on the scanning of the MH1 skull in this press release: "First studies of fossil of new human ancestor take place at the European Synchrotron"

    The analysis of the terabytes of data has only just started, but the preliminary visualisation of the complete skull already available shows intriguing details. Among them are the fossilised insect eggs whose larvae could have fed on the flesh of the hominid after death. Researchers also noticed an extended low density area that could point towards a remnant of the brain after its bacterial decay.

    I'm rather hopeful about this kind of technology. The described "terabytes" of data for a single skull are really going to be difficult to make accessible for anyone unless paleoanthropologists start collaborating more with more established data-sharing programs in genomics, physics, and astronomy. With best-practices comes more standardized data access guidelines. It may not lead to open access, but then again it may.

    It would be interesting to pursue a kind of "tiered" data access, so museums and the public could have real data at, say, 0.5 mm-scale, with micron-scale data reserved to qualified researchers. That would facilitate my dream of having hominin data available for high-school science classes, while enabling replication of scientific studies. It might also eliminate some of the arguments we've seen in the last few years about "whose CT scans are adequate" to show the anatomy.

  • Malapa news

    Mon, 2010-04-12 12:51 -- John Hawks

    A story about Malapa in the Times of South Africa gives just a few more details about the discovery of the infant remains near the two reported skeletons: "Baby hominid found at Cradle"

    Meanwhile, there's also this:

    Berger took the juvenile's fossils to the European Synchrotron Radiation Facility (ESRF) in France, in February, to test them using highly sophisticated equipment.

    At ESRF - an international research institute with cutting-edge technology - a fine X-ray beam, less than half the width of a strand of human hair, was used to scan the skull over four days.

    Berger said French scientist, Dr Paul Tafforeau, based at the ESRF, suspected that the juvenile's brain was still intact.

    He said the scan created a permanent record of the skull, adding: ''If something ... should happen to that skull, there's an electronic record of it at the highest resolution that human kind can produce right now."

    (via an especially sharp reader)

  • What, if anything, is Australopithecus sediba?

    Thu, 2010-04-08 22:46 -- John Hawks

    Today we finally get to learn about the exceptional discovery of four partial hominin skeletons from Malapa Cave, South Africa. Two of the fossil skeletons are described by Lee Berger and colleagues in the current issue of Science, descriptions of two more are still forthcoming.

    A kind journalist sent me a copy of the research papers a few days ago, so my graduate students and I have had a chance to think about them a little bit and compare them with other material.

    Berger and colleagues have named a new species to contain the fossils, Australopithecus sediba. For anybody who follows paleoanthropology, the new species won't be surprising -- if I found a fossil, I'd surely make up a new name for it, even if I thought it was my great-great-grandmother. In this case, the morphological reasons for naming a new species aren't trivial, but I'll begin by approaching them skeptically, especially in comparison with the large samples of South African fossils both earlier and later than Malapa. I'll conclude that a new species within Australopithecus was probably the right call, but not an easy one.

    The press is running with a "new fossils provoke debate" storyline -- are they possible ancestors of Homo or not?

    The simple answer to that question is that the Malapa skeletons are too late to be ancestors of Homo. After all, we have early Homo nearly a half-million years earlier.

    A more complicated answer is that it depends what we mean by Homo. My feeling is that these skeletons don't comport with what most of us mean when we say "Homo". Most of us have in mind an adaptive shift from Australopithecus to Homo that included larger brain size as a significant element, and the MH1 skeleton has a small endocranial volume.

    But if we accept that model of Homo, we have to accept its consequences, as the Malapa skeletons now make clear. One important consequence is that, if we assume that MH1 isn't Homo, we can no longer say have any skeletal evidence of Homo from before 1.95 million years ago. Because the Malapa specimens are more like Homo in their dental and mandibular features than are earlier specimens that have usually been called Homo.

    And if we throw out all those earlier Homo specimens...well, then suddenly Malapa isn't too old to be an ancestor of Homo after all.

    How old are they?

    The fossils lay above a flowstone with a U-series and paleomagnetic date consistent with an age just around 2 million years ago. That's a maximum age for the fossils; they must be younger than that.

    The hominins are in water-deposited sediments, which are inferred to represent ancient washes of subterranean water flows through the cave system. Two elements above the flowstone contain the hominin specimens, called facies D and E, and both have normal magnetic polarity. The most likely interpretation is that they belong to the Olduvai paleomagnetic subchron, which occurred between 1.95 and 1.78 million years ago. A specimen of the sabertooth cat Megantereon in one of these facies has a last appearance elsewhere in Africa at 1.5 million years ago. So it appears that 1.78 million years is a very likely minimum age for the fossils.

    That's about as good as dating gets in South Africa, where we're used to seeing very wide age brackets on hominin-bearing localities. It means that the Malapa hominins lived at around the same time as KNM-ER 1470 in the Turkana basin, or OH 24 at Olduvai Gorge. Until today, I think we could justly claim that the only australopithecines still known to occur in this time interval were the robust species A. boisei and A. robustus -- although the first appearance of A. robustus might (might) be later than Malapa.

    Why aren't they A. africanus?

    To me, this is the hardest question to answer.

    The Sterkfontein Member 4 sample of A. africanus is tremendously variable. The postcrania of both Malapa skeletons are tremendously informative, but fall within the range of variation at Sterkfontein for almost every feature that the authors reported. The few exceptions (such as humeral torsion and femur neck/shaft angle) are right at the edge of the Sterkfontein range.

    Malapa skeletons

    In other words, it's my impression that the postcrania of the Malapa skeletons fit within A. africanus. The limits of my impression are that there are a whole lot of observations here, and the paper generally does not report metrics for the postcrania. Maybe the sequel will give us some more surprises.

    I would have added a comparison with the Swartkrans A. robustus sample, which overlaps nearly totally in body size with Sterkfontein and contains elements that are in some cases more comparable to the Malapa skeletons. In particular, the os coxa of MH1 looks a lot like SK 3155, and the proximal femur looks like SK 82 to me, at least in the tiny picture provided with the paper. On the whole, I don't think that the Malapa hominins are particularly like A. robustus, I just think that if you put together a reasonably large sample of australopithecine postcrania, these two skeletons don't stand out.

    I'll take up the discussion of proportions of the different elements below. My feeling is that the proportions aren't exceptional for Australopithecus, either, but we have to temper that against the observation that really only AL 288-1 (Lucy) is comparable, and it's more than a million years older.

    What about the teeth? Generally speaking, the teeth of MH1 and MH2 are both at the small end of the A. africanus range. In a couple of cases (the lower canine of MH1, the lower second molar of MH2), the teeth are absolutely smaller than any Sterkfontein individual. The canines are within the range of A. robustus (remember that the robust australopithecines have small anterior teeth), but the premolars are nothing like the large, molarized Swarktrans sample of premolars.

    They're a little small but within the range of those known for Homo habilis at Olduvai Gorge. For example, OH 7 -- the type specimen of Homo habilis has molars that are 1.5 mm larger than MH1 in both dimensions.

    But then, Homo habilis really doesn't differ much in tooth size from Sterkfontein.

    In size, the Malapa teeth are exactly what you would expect for Homo erectus. The first molars are smaller than those of Dmanisi D2700/D2735, for example. But unlike H. erectus dentitions, the molars of the Malapa hominins get bigger toward the back -- M3>M2>M1.

    The Malapa mandibles are strikingly gracile. The MH1 mandible has a relatively vertical symphysis with a small cross-section. The long, parallel upper and lower corpus borders really strike me like a mandible of Homo erectus, something like KNM-ER 993 or OH 22 -- but this impression may be exaggerated considering the M3 of MH1 has yet to erupt. Metrically, the corpus breadth and height are most like OH 13. There are small australopithecine specimens that compare to this, such as AL 277-1, and it is worth remembering that MH1 is a juvenile mandible. I can't compare the ramus heights with those of other samples because the authors don't report those measurements.

    An interesting question: If these mandibles had been found in isolation, would we call them Australopithecus? The Olduvai H. habilis mandibles OH 7 and OH 13 have M3>M2>M1, while OH 16 has M2>M3>M1. The Malapa mandibles look much more like later Homo than do early Turkana basin mandibles like KNM-ER 1801, KNM-ER 1802, or KNM-ER 1482, all of which are much more robust and have larger, more molar-shaped premolars than MH1, and all of which have M3>M2>M1 except KNM-ER 1802 which lacks M3. This is a quick comparison on my part, but I think the Malapa mandibles look more like Homo than does the existing hypodigm of Homo habilis. It's hard to imagine that the mandibles in isolation would have been referred to Australopithecus. More on that below.

    Compared to the mandibles, the cranium of MH1 looks more like its counterparts from Sterkfontein. To be sure, it is an 11-13-year-old juvenile and more gracile in some respects than any of the Sterkfontein crania. But take a look at it next to Sts 71:

    MH1 next to Sts 71, frontal view

    MH1 (left) next to Sts 71 (right)

    They're not identical, naturally. Sts 71 has higher temporal lines, a slightly smaller vault, and more prominent cheeks. It also has more postorbital constriction compared to MH1, though that isn't obvious from this angle. MH1 has a true superorbital torus, Sts 71 has at best a shade of one. But you can see the similarities -- the angle of the zygomatic process of the maxilla, the narrow and concave interorbital region, the tall and narrow orbits. MH1 has no prominent anterior pillars (bony swellings on either side of the nasal aperture), but Sts 71 is not very different in this region. Sts 71 has bigger teeth.

    Consider also Sts 52:

    MH1 next to Sts 71, frontal view

    MH1 (left) next to Sts 52 (right)

    Again, Sts 52 has anterior pillars and bigger teeth, but the shape of the face is very comparable between these two. The nasal bones in particular are similar in this pair, almost "pinched" at the midline, with a lateral expansion both superiorly and inferiorly.

    We can do a similar exercise for most of the features of the MH1 cranium. What is exceptional, in the context of the Sterkfontein sample, is the overall gracility of the masticatory apparatus.

    One important thing that is not in the least bit exceptional: Its brain. An endocranial volume estimate of 420 ml (from CT reconstruction) puts MH1 at the bottom of the range of variation at Sterkfontein -- the best-known skull from Sterkfontein, Sts 5, has a volume of 485 ml, while STW 505 has a volume larger than 550 ml. Before MH1, the smallest of the South African crania were estimated to have volumes of 428 ml. This one seems to be smaller mainly by being flatter -- a shape that it shares with early Homo, but I wouldn't say it was without parallel in Australopithecus.

    But the smallest endocranial volume known for early Homo is KNM-ER 1813, at 510 ml. That specimen is extreme: the next smallest is 585.

    The vault fits in A. africanus, most of the facial features have comparable specimens in the Sterkfontein sample, with some exceptions, and the postcranial skeleton is unexceptional. The teeth are mostly within the range at Sterkfontein with some exceptions. But the mandible -- like those few facial characters -- stands out.

    Australopithecus sediba -- a new species within Australopithecus -- then seems like a fair diagnosis. The craniodental derived features are of the sort that would usually justify a new species. Heck, in the case of Kenyanthropus, even more minor differences in the face and size of teeth from contemporary A. afarensis caused Leakey and colleagues (2001) to name a new genus.

    Is MH1 really a male?

    Berger and colleagues (2010) infer that the MH1 skeleton (the one with the skull) is a male. It is large and more robust than the MH2 skeleton: Its teeth are bigger than the MH 2 skeleton, its mandible is more robust with a taller ramus, the articular ends of its limb bones are a bit larger. In addition, the greater sciatic notch on its preserved os coxa is narrower than other australopithecines like Lucy and Sts 14, and the pelvic inlet may (based on the anterior position of the auricular surface) have been smaller.

    But the skeleton isn't really very big. Its endocranial volume is small, its long bones are not nearly so robust as some australopithecines. There are large male australopithecine skeletons -- STW 431, for example -- and MH1 doesn't seem so large as these. Again, it's hard to tell without postcranial measurements, but the sex of this specimen isn't a clear call either way.

    The sex of the specimen is important to the way we interpret it, because the features that make it stand out from A. africanus concern masticatory gracility. If it's a female, it doesn't seem quite so different from A. africanus as if it's a male.

    Are they Homo?

    Let's start with the brain size, which at 420 ml seems to be the most obvious thing separating MH1 from our genus. Well, except for Liang Bua 1 -- with its endocranial volume of, um, 420 ml. Is brain size fundamental to Homo? Maybe. Maybe not.

    Alan Boyle's report on the fossils ("Fossils shake up our family tree") has an excellent letter from Don Johanson, who makes the argument that the Malapa fossils should be assigned to Homo. Of course, Johanson and Bill Kimbel in 1996 described a 2.33-million-year-old fossil from Hadar as the earliest clear maxilla of Homo. That maxilla, AL 666-1, resembles Homo in having a more vertical subnasal profile, a parabolic dental arcade, molars that are long relative to their breadth, and a "squared-off" jaw that is relatively straight across the anterior dentition. In other words, basically the dental features seen in the MH1 maxilla.

    We've got two choices. Maybe these are genuine shared derived features with these specimens and Homo -- in which case, we should probably name them Homo, as Kimbel and colleagues did for AL 666-1.

    Or, there were several australopithecines after 2.5 million years ago with these dental and maxillary (and for the Malapa hominins, we can add mandibular) characters. In which case, they're not signs of Homo at all. They may reflect parallel dental reduction in several australopithecine lineages, all of which faced niche differentiation from the emerging robust australopithecines. One of those lineages may have given rise to Homo, but we don't know which. Maybe it was South African, but it need not have been. It could even have been Asian.

    The question is just how important we think brain evolution was to the origin of our genus. If the brain was the key adaptation, then Malapa shows that the dental features are irrelevant to the brain -- because these skeletons have more dental reduction than most of the East African Homo habilis sample, but MH1 has a much smaller brain.

    What about tool manufacture?

    Part of the logic of pre-2-million-year-old Homo is the emergence of stone tool manufacture 2.6 million years ago. It stands to reason that this major shift in behavior and diet might have given rise to a new adaptive plateau for early hominins, and that would have been tied to the evolution of larger brains. The problem is that we don't have larger brains in any fossil remains until after 2 million years ago -- KNM-ER 1470 remains the earliest hominin with a brain larger than 600 ml. Up to now, people have conjectured that large-brained hominins may have existed earlier, even to the point of arguing about the brain size reflected by the otherwise-robust temporal bone from Chemeron. But it's worth pointing out that none of these pretenders to the Homo throne have smaller teeth than A. africanus. The diet shift that should have been made possible by a meat-eating stone tool economy didn't lead to smaller teeth until much later.

    And now we know that at least one small-toothed hominin also was a small-brained one.

    We don't know whether the Malapa hominins would have been toolmakers. The fact that they weren't found with tools isn't really evidence either way. Dirks and colleagues (2010) suggest that the skeletons were deposited by water washing them from an initial death trap into a secondary location. If true, it would be a miracle beyond belief for stone artifacts to have made the trip with them.

    We do know that stone tools are present in Sterkfontein Member 5 and Swartkrans Member 1, and cutmarked fauna are in the latter. Both these may be roughly contemporaneous with the Malapa hominins, depending on their date. So toolmaking hominins were in the immediate area, around the time that the Malapa hominins lived.

    SK 847 is from Member 1 of Swartkrans, and could be as old as the Malapa skeletons. Its endocranial volume isn't known, but facially it looks even more like Homo erectus than does MH1. It seems plausible that this skull represents the local toolmaking population, but even so, this skull does resemble MH1 in several respects, and again we don't know its volume. STW 53, probably a bit older than Sterkfontein Member 5, has also often been referred to Homo but it definitely doesn't have a substantially larger endocranial volume than MH1.

    So again, we seem to be faced with two choices: Broaden the definition of Homo to include this very australopithecine-like sample, or restrict it to later large-brained hominins. In either case, brain size and tool manufacture do not necessarily go together.

    What's the single most obvious thing that the paper doesn't describe?

    Which brings me to the fingertip. MH2 has a distal phalanx. The paper doesn't describe it, even though this bone element has taken on such importance in the evolution of Homo compared to Australopithecus. Big fingertips are supposed to be adaptations to force transfer through the fingertip grip used in tool manufacture.

    The picture of the thing is so tiny -- I mean, literally we're talking about two pixels of finger -- that I can't make anything out of it. Does it have a large apical tuft, like OH 7? Or is it like the Hadar distal phalanges, with narrow, apelike apical tufts?

    If one was wondering about whether the thing was Homo or not, I would think this is one of the first things you would check....

    What about those limb proportions?

    For fifteen years, a bunch of otherwise sensible paleoanthropologists have been engaged in a debate about the limb proportions of A. africanus and H. habilis. The reason why this particular question may not be sensible is because the debate is about the length of the arm relative to the leg, but there's no specimen of A. africanus that preserves both the length of the arm and the length of the leg.

    What there are: OH 62, a skeleton apparently of H. habilis that has a complete humerus and more than half the length of one femur, STW 431, which has an acetabulum and mostly complete humerus, and Sts 14, which has a partial femur, an acetabulum, and a piece of distal radius. On the basis of these fossils, we've seen some intense debate about the reconstruction of the OH 62 femur length, and a lot of discussion about whether the sizes of articular surfaces are relevant to the function of the limbs. Indirectly, it has appeared that A. africanus and H. habilis shared longer arms than were present in AL 288-1 (Lucy).

    Well, now we have two fossil skeletons with both hindlimb and forelimb elements. The paper doesn't address the issue directly, nor does it provide raw measuremnets that would lead to a quick answer. But the humerus is short relative to the size of the femur head, compared to earlier hominins, while a bit long relative to Homo by the same comparison. So it looks like the Malapa skeletons may be somewhere in between.

    The authors do argue that OH 62 is an odd skeleton in one respect: They consider the "diaphysial strength" of the humerus and femur. This is a cross-sectional measure of the area of cortical bone, and reflects the robusticity of both forelimb and hindlimb elements. In their estimation, OH 62 has a much stronger arm relative to its leg strength than the Malapa skeletons.

    It's not obvious how to interpret this observation. Is OH 62 more apelike in its locomotor pattern than Malapa? Or does the strength ratio vary allometrically with body size, and OH 62 is just at the smallest end of the comparison? Hard to tell without the length measurements.

    OK, what's the bottom line?

    Here's the important thing. From today forward, there are a bevy of features of the face, teeth and jaw that are no longer "derived characters" of Homo.

    Some people will want to fix this by broadening the definition to Homo to include the Malapa skeletons. Others will want to narrow the definition of Homo to include only large-brained specimens.

    Every specimen attributed to Homo before 2 million years ago is now up for grabs. Maybe they're Homo, or maybe their resemblances to Homo are just masticatory parallelism. We already know that parallelism explains many of the derived locomotor and masticatory resemblances of great apes, and many strongly suspect that parallelism explains the derived masticatory resemblances of robust australopithecines. If the dental reduction that once was a marker of Homo joins this list, it will hardly be surprising.

    If we follow the logic that connects tool use to dental reduction, however slowly and indirectly, then I think we have to conclude that A. sediba was likely a toolmaker and meat-eater. This hypothesis is testable, both by bone chemistry and dental morphology and wear.

    Malapa suggests the hypothesis that brain evolution followed the appearance of stone tool manufacture by a considerable delay. If so, I wonder what exactly caused the brain to expand. Did the diet shift to higher-quality foods unfold over a long time, allowing brains to expand only after 3/4 million year delay? Or was brain evolution caused mostly by non-dietary factors, such as social dynamics or climate instability?

    Or did the evolution of our genus happen somewhere else, far from the places where we currently have fossil samples? The Rift Valley and South African cave systems may have been wonderful for preserving fossils, but who's to say they weren't relative backwaters when it came to the evolution of Homo?

    Well, I'm running out of gas for this installment. More later....

    References:

    Berger LR, de Ruiter DJ, Churchill SE, Schmid P, Carlson KJ, Dirks PHGM, Kibii JM. 2010. Australopithecus sediba: A New Species of Homo-Like Australopith from South Africa. Science 328:195. doi:10.1126/science.1184944

    Dirks PHGM, Kibii JM, Kuhn BF, Steininger C, Churchill SE, Kramers JD, Pickering R, Farber DL, Mériaux A-S, Herries AIR, King GCP, Berger LR. 2010. Geological Setting and Age of Australopithecus sediba from Southern Africa. Science 328:205. doi:10.1126/science.1184950

    Synopsis: 
    New skeletons from Malapa, South Africa, present surprising evidence about the evolution of our genus.
  • NOVA: Becoming Human

    Tue, 2009-11-03 22:17 -- John Hawks

    OK, I'm going to live-blog this show. I've been looking forward to it for a while -- I loved the old NOVA series with Don Johanson and have often showed it in classes but I had to stop several years ago because it's getting out of date. These are great overview-type programs, unlike the more special-purpose one-topic shows.

    The producers gave me the opportunity to review the program's script a few months ago (that's explains the acknowledgement at the end), so I'm not expecting any unpleasant surprises.

    The pre-credits opening: Naked people smiling. Naked chimps grooming...

    7:01: "What set us on the path to humanity? The questions are huge, but at last, there are answers..."

    "For millions of years, many human-like species coexisted on our planet, until one day, there was only us."

    7:03: "Apes that had walked on four legs stood up and walked on two." We see apish CGI hominins. Then, to the Sahara to see Toumaï. Michel Brunet is describing the skull.

    "We, Homo sapiens, are the first ever to be alone."

    7:06: To the Afar, explaining the Rift Valley and its erosive contexts. The Insta-Zoom effect across the desert is actually kind of cool. We see Zeresenay Alemseged driving an SUV, then walking in badlands with scattered bones. Nice photographs of the Dikika skull in context.

    7:09: Zooming backward into a timeline, as if the years are sucking us back, the program explains the timespan of human evolution as a series of doublings backward in time.

    7:10: Alemseged is in the National Museum of Ethiopia, preparing the skull. It's a nice video treatment, shoing the slow preparing with dental drill. The long shots of the postcranial elements are very illustrative -- this is a good demonstration of how the anatomy informs us about the developmental schedule and lifeways.

    7:13: Don Johanson is explaining how he found AL 129-1. Then, he explains the difference between the chimpanzee and human pelvis. Too bad they couldn't have included Ardipithecus; it would be interesting.... I'm really liking the fact that you have people interacting with actual casts instead of lots of CGI images. You have a much better impression of the scale

    7:15: Now the scene moves to Kenya, this is going to be about paleoenvironments. Yannic Garcin and Daniel Melnick are describing how the now-desert landscape was once much wetter. We go back to the Afar, with Alemseged explaining the fauna that's just eroding up out of the ground (wonder how set up that scene was...).

    7:18: Bipedalism. It's like Saturday Night Fevur. Brian Richmond appears to explain theories about why bipedality was adaptive. This is all accompanied by contemporary dancers wiggling around. Chimpanzee-like ancestors are illustrated with video of actual chimpanzees (wonder what Lovejoy is thinking...). Dan Lieberman is talking about energy budgets. People and chimps on treadmills hooked up to oxygen meters.

    7:22: Mark Stoneking explains the molecular clock. "The dates that one almost always gets are 5 to 7 million years ago for when humans and chimpanzees shared a common ancestor."

    7:24: We go to Chad. Brunet explaining why they needed to recover fossils from somewhere other than East Africa. "Everyone said 'no', there just aren't any [human-like] fossils there."

    7:26: "There were no bones apart from the skull..." Er...

    7:27: The skull is reconstructed with a CT scanner and then cast. Oops...the rest of the shots of casts are all taken directly from the skull, not the 3-d scan version. Nice artist's rendering of Toumaï here.

    7:30: I'd hate to be one of the dancers walking by on the screen with the voiceover, "Walking upright didn't mean that they had big brains."

    7:33: Brain growth in Selam. Hints of a longer childhood -- of course, at 330 cc, it's almost the size of a full-grown chimpanzee. Todd Preuss is discussing the evolution of the brain, showing us actual pickled brains of human and chimpanzees. Lunate sulcus -- was Selam like a human or a chimpanzee?

    7:35: Ralph Holloway is describing the brain reorganization -- great shot of him with his collection of endocasts. The conclusion is that the lunate sulcus was human-like.

    7:37: Now we have stone tools appearing, Brian Richmond explains how we recognize tools. Unlikely they were made by Australopithecus, because they didn't make them earlier. Skip forward to KNM-ER 1470, "the dawn of a new era, beginning around 2 million years ago." Tools were used for meat processing. Homo habilis was small in body size, but had a much bigger brain than Australopithecus.

    7:41: Viktor Deak is reconstructing Homo habilis. I like it, more apish than the usual rendering.

    7:43: "Africa's gradual drying trend was punctuated by bursts of rapid climate fluctuation." We see Rick Potts explaining the stratigraphy of a lake alternating with desert and volcanic layers over time. The idea of "variability selection" is explained.

    7:45: Analyzing diatoms in layers of rock -- the species tell the alternation of shallow and deep lake levels. It's a record of strong fluctuations. We see rapid clips of three different scientists (Potts, John Kingston, and Mark Maslin) talking about water fluxes. It's a good way of explaining the climate instability -- although they could have gone a bit further: when they mention "Lake Victoria-sized lakes appearing and disappearing", for example, they might have pointed out that Lake Victoria itself has appeared recently.

    7:48: Dust from ocean cores. Once again, it comes down to tiny sea creatures whose anatomy correlates with date.

    7:50: We get a rapid montage reviewing the climate instability idea. Hmmm...I have to say that the very fast cutting of clips and louder music doesn't really add to the credibility of the idea -- it seems like something is being left out.

    7:51: Rick Potts restates the variability selection argument. "Simple but revolutionary idea -- human evolution is nature's experiment with versatility...we are creatures of climate change."

    That's the end. I think the paleoenvironment story was well done. The shots of how this science is done were very illustrative -- from the field to the lab, the program showed the fine layers of sediment and careful study of microscopic creatures.

    On the other hand, the show may have gone a little too far in the "climate made everything happen" direction. I don't think the "variability selection" idea explains the origin of Homo, and while the program did briefly list alternative views about the adaptive value of bipedality, it left no doubt that African desiccation and loss of forest was the ultimate cause.

    I think everything with actual fossils, dirt, or rocks was well done. In particular, we got a good view of most of the Selam skeleton, with the notable exception of the hyoid bone. These are the best available images of the specimen to date. Holloway's descriptions of endocast evolution were well done, placed in the middle of a big table of fossil casts. I like the solidity with which the program showed the fossil record. Hopefully the next two segments will also follow this technique -- much preferred over the CGI-reconstruction technique.

    I will be out of the country for the next two parts of the trilogy, so I'll have to see if I can get them online. The NOVA Evolution website has the first episode online now, so there's some hope.

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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.

Denisova

From a finger bone of an ancient human came the record of a completely unexpected population. My lab is working on the science of the Denisova genome.

Acceleration

The advent of agriculture caused natural selection to speed up greatly in humans. We're uncovering some of the ways that populations have rapidly changed during the last 10,000 years.

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.