john hawks weblog

paleoanthropology, genetics and evolution

South Africa

  • Taung

    Tue, 2011-10-25 00:38 -- John Hawks
    Synopsis: 
    A lab station introducing the Taung specimen and considering its age.

    The face, mandible and endocast from Taung, South Africa, was the first australopithecine fossil to be discovered. We now know that the fossil dates to the period between 2.5 and 3.0 million years ago, but at the time of its discovery, the precise date was not known; only that it was likely earlier than fossil evidence for human evolution outside Africa.

    The morphology of the specimen was therefore the strongest evidence about its relationships to humans and living apes. Interpreting the morphology means coming to terms with the developmental age of the skull.

    Assess the age and morphology of the individual:

    1. What dental age would you assign to Taung, based on your knowledge of human dental development?
    2. What differences are there between Taung and the chimpanzee?
    3. Imagine that Taung was the only australopithecine specimen ever discovered, as it once was. How would you support the argument that it was a hominid?
    Study terms: 
  • Blombos pigment workshop

    Fri, 2011-10-14 02:23 -- John Hawks

    I know that some readers are starting to wonder if I've forgotten about paleoanthropology lately. Let's just say that the Neandertal and Denisova genomes have me very busy, and I don't think you'd want it any other way.

    But on the paleoanthropological front, Science has released a paper by Chris Henshilwood and colleagues [1] describing two toolkits used by ancient MSA people more than 100,000 years ago to grind pigment and mix it with animal fat, presumably for painting.

    I want to share a picture from the article (credit G. Moéll Pedersen), which shows one of the two toolkits in situ. I want to make a point about it that would be difficult without seeing the photo:

    That photo shows Tk1, the first toolkit. Now, here's the description of what Henshilwood and colleagues were able to interpret from the artifacts in the photo:

    We infer that manufacturing proceeded as follows: Pieces of ochre (FS1 and FS2) were rubbed on quartzite slabs to produce a fine red powder, and some were knapped with large lithic flakes. The ochre chips resulting from the latter were crushed with quartz, quartzite, and silcrete hammerstones/grinders. Quartzite grinders were used to crush goethite or hematite-rich lutite. Medium-sized mammal bone was crushed, probably with a stone hammer. The red or reddish brown color and cracked, flaky texture of some of the trabecular bone suggest that it was heated before crushing, probably to enhance the extraction of the marrow fat. The hematite powder, charcoal, crushed trabecular bone, stone chips, and quartz grains and a liquid were then introduced into the Haliotis shells and gently stirred (figs. S5, S25, and S26). Charcoal is rare in the layer-CP matrix, suggesting that it was a deliberate addition to the mix. The quartz and quartzite chips, produced during the action of crushing the ochre, and the quartz grains may have been incidentally incorporated.

    You can see how the complex interpretation was made possible by finding these things in association as part of one feature. If one or two of these pieces had been found separately, many archaeologists would be skeptical of such a story. Indeed, even the interpretation of this toolkit might appear incredible were it not for the second toolkit also found at the site. Archaeologists are conservative that way, they don't like to overinterpret the evidence. Even this series of events -- grinding, heating, mixing, and so on -- isn't very complicated compared to many activities that humans do every day. It's an example where Henshilwood and colleagues have advanced what archaeologically can show beyond a shadow of doubt about ancient people, but still leaves a gap in our understanding of the ancient cultural system.

    A complex behavioral pattern that is actually found cannot have been an isolated instance. Complexity implies a tradition of which these toolkits are only miniscule remnants.

    In this light, I should point out that the Blombos evidence is by far earlier than other evidence of pigment grinding and heating, but not unique in the South African MSA. Last year I linked to a Jennifer Viegas story about red ochre production at Sibudu Cave, South Africa. This is Lyn Wadley's work [2], and the research paper has since been published in the Journal of Archaeological Science. Also in that journal last year was a paper by Francesco d'Errico and colleagues [3], which described pigment nodules found in the Middle Paleolithic in Mt. Carmel site of Skhul, Israel. We have quite a lot of circumstantial evidence about pigment use in these early contexts both inside and outside Africa, and more is building all the time.

    The archaeological record is bad in many ways. The wooden artifacts preserved at Abric Romani, Spain, are another example of an exceptional archaeological find. I've been meaning to write about them since Julien Riel-Salvatore mentioned them last month. Archaeologists have been working the Middle Paleolithic for nearly 150 years, yet we know next to nothing about wooden artifacts. Abric Romani is not entirely alone, but is enough to show the existence of a broader tradition occupying this blind spot, because the extensive shaping of artifacts and labor used to create them implies a cultural knowledge and utility.


    References

    Synopsis: 
    Complex toolkits from Blombos, South Africa, show pigment processing before 100,000 years ago.
  • A look at Little Foot

    Fri, 2011-09-09 13:00 -- John Hawks

    Along with the papers on the Malapa hominins, Science this week published a news story by Michael Balter that is a profile of Ron Clarke and his work on the "Little Foot" skeleton, StW 573 from Sterkfontein [1]. This specimen has been coming out of the ground for nearly seventeen years now, and Balter reports that the final pieces are to come out of the cave within two months. The article hits on the important issue of dating:

    Meanwhile, Clarke and three independent teams are getting divergent dating results. In 2000, Clarke's team, using known reversals of Earth's magnetic field, put the skeleton at 3.3 million years, making it a near contemporary of Lucy and the oldest hominin in South Africa. But since 2006, three other teams, using uranium-lead and paleomagnetic dating, have published dates ranging from 2.2 million to 2.6 million years, although they all regard the younger date to be more likely. That would make Little Foot about the age of the earliest known Homo and only a little older than Au. sediba. Clarke is now working with geologist Laurent Bruxelles of the University of Toulouse in France to produce their own new dates.

    It's striking that in an article about a complete hominin skeleton, the only informed commentary and opinion is about the foot anatomy. The foot is the only part that has yet been published in enough detail for intelligent comment, and as Balter points out, very few individuals have seen the specimens or casts of them. There are casts of the specimen in situ on display at Maropeng and the smaller museum at Sterkfontein, though. It struck me just how large the specimen is. I would describe it as the first human-sized australopithecine.


    References

    1. Balter M. 2011. Little Foot, Big Mystery. Science 333:1374 - 1374.
  • Variation in talus morphology shows the sample

    Thu, 2011-09-08 23:50 -- John Hawks

    This is the kind of thing I never get tired of: Figure S7 from the supplement of the Malapa foot paper by Bernhard Zipfel and colleagues [1].

    Figure S7 from Zipfel et al. 2011. Original caption: "Fossil hominin tali in distal view. Left tali have been reversed so that they all appear from the right side. All tali have been scaled so that the trochlear body is the same mediolateral width. There is tremendous variation in the torsion angle of the head, and in the grooving of the trochlea in fossil hominins. Notable in this orientation is the remarkably large talar head of U.W. 88-98."

    We see too many papers where a fossil is displayed next to a chimpanzee and a human, maybe another hominin, as if they were Platonic types. Here we see immediately the variation among a good sample of hominin tali from East and South Africa. Four from Sterkfontein and four from Turkana, so you can see variation within those samples arrayed right across the figure. A figure like this takes more interpretation than a graph showing measurements or principal components, but it has a visual impact that a Cartesian plot can't match.


    References

  • Synchotron illustration

    Thu, 2011-09-08 20:01 -- John Hawks

    In the supplement of Kristian Carlson and colleagues' paper on the MH1 endocast [1], there's a nice comparison of the medical CT versus synchotron images. My blog sizing can't do it justice, and to be honest, the online PDF in Science doesn't either, but you get the idea:

    Figure S10 from Carlson et al. 2011, detail. Original caption: Comparison of the same slice of the MH 1 cranium obtained with medical CT (left) and synchrotron scanning at the ESRF (right). Voxel sizes are approximately 450 μm and 45.71 μm, respectively.

    You know, someday we'll all have these data for the entire fossil record, and students won't think a thing of it.


    References

  • Announcing the Malapa Soft Tissue Project

    Sat, 2011-09-03 17:34 -- John Hawks

    I am pleased to announce a new open science initiative, focused on a discovery that is unique in paleoanthropology. Together we are going to find out if the Malapa site has preserved evidence of soft tissue from an ancient hominin species.

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

    In the August, 2011 issue, National Geographic reported on the Malapa fossils, including a teaser that the site may preserve skin from two hominin individuals. (I pointed to the article last month.)

    The suggestion is obviously surprising. Many readers will remember how much controversy surrounded claims about soft tissue preservation from dinosaurs several years ago. Yet extraordinary preservation contexts do exist in the fossil record. Indeed, a few years ago Lee Berger's team, including several of the people now working on the Malapa hominins, identified hair preserved inside hyena coprolites from Gladysvale cave, more than 200,000 years old and only a short distance from Malapa [1].

    Could Malapa present the first evidence of soft tissue from a fossil hominin? If so, what can it tell us about human evolution?

    The day the National Geographic article was published online, I was standing with Lee in his lab looking at what might be australopithecine skin. I'm not talking about an imprint of skin, like a skin cast. These appear to be thinly layered, possibly mineralized tissue.

    Suppose it's really skin, or some other soft tissue, I thought. How would you go about testing the hypothesis? Extraordinary claims require extraordinary evidence. Even if you could demonstrate it to your own satisfaction, what would it take to convince the doubters? How many distinct observations would be possible from these objects? What instruments would you use, and what comparative samples would you need?

    Lee said this was his problem as well. He has access to some of the most sophisticated technology in the world. Some kinds of observations are obvious. He can micro-CT the apparent soft tissue evidence, look within the rock at its structure. He can sample the chemical content, and use scanning and confocal microscopes to examine it. He could sacrifice a small sample to be microscopically dissected. At the end, he would have an answer involving all these comparisons. But would it be convincing?

    Lee then made an inspired proposal: What if the process itself were an experiment?

    Much of the criticism of other surprising fossil discoveries has been fueled by their secrecy. Science done by a closed process means fewer eyes looking at data, and too many chances for errors to pass unnoticed. Unnoticed, that is, until publication. Then, a firestorm of controversy may erupt as the scientific community at last examines the methods and results closely. In anthropology, the most critical errors are often missed comparisons -- sometimes simple things that a research team could have looked at, if they had only thought of it.

    An open process has the chance of improving research by broadening it. We want stronger, clearer results, and we want to anticipate every important criticism. If a significant comparison can be added by people who have the right tools, why not get those people involved? If we stand a chance of finding those people by making the process more open, why not do it?

    Lee suggested that this soft tissue evidence could be the basis of a true experiment in whether paleoanthropology could be done as open science. I've been agitating about open science for years, and I volunteered right away to host the experiment and work to make it a success. We went immediately to Rachelle Keeling, the graduate student who will be coordinating the project, and described how we thought it could work. She was enthusiastic about the idea of a truly new kind of scientific project, one that had the potential to involve so many people in the process of discovery.

    And so, after a month of putting things into order, here we are. How can you participate in the project, or at least follow its progress?

    I have set up a home page for the project, here as a special category page on the blog. This page is the online headquarters of the work, and includes a feed that will have all project updates. As the project proceeds, it will generate suggestions, results, and press. I'll be tracking all of these and updating as we learn more.

    The project has an official e-mail address hosted here: skin@johnhawks.net. We want to hear from anyone with the expertise or ideas to solve this problem. Rachelle and I will be reading through the e-mails, discussing them with other project members, and following up on them.

    We don't know what to expect but I hope we get hundreds of responses. We can't promise replies to anyone, but everyone will receive an automatic acknowledgement that we've received their messages, and we will follow up personally with those that have suggestions or proposals we can take action on. We're going to ask people to participate in the project, perform research, and coauthor the scientific work: this is real open science.

    Members of the Malapa team are biologists who know comparative skin and hair biology. I'll be posting quite a lot about these biological topics for people following the project.

    We know that there are many researchers who have been working with methods that would be useful on these unique samples of possible soft tissue. People working with the trace chemistry of organic compounds in mineral samples, people working with the microscopic structure of other ancient soft tissue samples, people who study preservation of organic materials in forensic contexts. There are many others that I don't even know I should be listing.

    If you know a person with the right expertise to help, please share this information and encourage her to write.

    Most important to the success of the project is showing that we can produce top quality science by this open process. That means we need journals to acknowledge the value of open science instead of penalizing it for not being secret and embargoed. If you're a journal editor reading this, I'm calling you out. And if you're a reviewer or editorial board member, you can support this project and encourage more like it by encouraging the submission of open manuscripts.

    And if you don't have a suggestion right now, keep watching. This project will develop and I expect it to become more interesting as it becomes broader. I can't predict how it will end, and that's pretty exciting!


    References

    Synopsis: 
    I announce and describe a project to study possible soft tissue evidence from a 2-million-year-old fossil hominin site.
  • 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.
  • Meet Australopithecus robustus

    Thu, 2011-09-01 21:39 -- John Hawks
    Synopsis: 
    This lab station gives an opportunity to examine fossil casts of A. robustus in comparison to humans and apes.

    The region just north of Johannesburg, South Africa, is a formation of ancient limestone in which groundwater has formed numerous caves and sinkholes. Some of these caves are used by animals for cool shade, water, and minerals; some are used by leopards, or in ancient times, sabretooths. By accident and predation, the skeletons of animals fall or are dragged into these caves, including our relatives the hominins. After around 2 million years ago, the most common kind of hominin in these caves was a species we call Australopithecus robustus.

    The word "robust" refers to size and strength. A. robustus was not very large in body size, but it had exceptionally large molar and premolar teeth, and a very large and thick mandible, or jawbone. The main muscles of the jaw, the temporalis muscles, were so large that they ran up the complete height of the skull to meet at the midline. The high ridge of bone where these muscles attached to the top of the skull is called the sagittal crest.

    A. robustus is one of the best-represented species of early hominins. The first specimen to be found was TM 1517, a partial skeleton with cranial remains from Kromdraai, presently in the Cradle of Humankind World Heritage Site. The largest sample of A. robustus fossils come from Swartkrans, less than 3 km from Kromdraai. The iconic skull, SK 48, provides a good illustration of the anatomy of the cranium of A. robustus with its sagittal crest, large, thick cheekbones, and relatively large molar teeth.

    The most obvious features that A. robustus shares with living people are related to locomotion. Human bipedality, or upright walking, caused many changes to the skeleton. A simple comparison of the distal end of the femur, the end nearest the knee, is enough to tell that A. robustus was bipedal like humans. Quadrupedal animals, who go on all fours, very rarely support their weight on one leg and do not have to balance their centers of mass over a single point. Their legs are typically oriented straight from the hip joint to the ground. Humans, in contrast, have to support their weight on one leg every time they take a step. To accomplish this, their legs must angle from the hip joint under the body's center of mass. The human knee angles very obviously at the distal femur, so that when the condyles of the femur rest flat on the tibia (or a table), the shaft of the bone angles markedly from vertical.

    This angle is called the valgus angle, and is one of the easiest-to-see traces of bipedality in fossil hominins.

    Study questions: 
    1. Explore the fossil skulls of A. robustus in comparison to the human and ape skulls at this station.
    2. Which features are more humanlike?
    3. Which features are more like the ape skulls?
    4. What kinds of foods do you think A. robustus would have eaten?
    5. The femur provides key evidence of locomotion. Examine the valgus angle on the distal femur from Swartkrans. Is it more like a human or an ape femur?
    6. Looking at the femur of A. robustus from Swartkrans, how big do you think these creatures were?
  • A visit to Malapa

    Sun, 2011-07-17 05:06 -- John Hawks

    I'm visiting at the Institute for Human Evolution at the University of Witwatersrand this week. Lee Berger has been a really wonderful host and among other things he very kindly took me out to the Malapa field site. As you can imagine, I'm pretty busy this week and haven't even had time to properly work up my thoughts on my Siberia trip. But I thought it would be fun to quickly share some impressions and photos of Malapa.

    Malapa is a short drive from Johannesburg, but it takes only a short drive to really be in almost total wilderness. The site lies in what is now called the Malapa Nature Reserve (after the site) and adjoins the John Nash Nature Reserve. We arrived at the gate around 7:00 am, just after the orange full moon set in the west, and as the sun was rising in the northeast. It was a beautiful morning, no question.

    IMG_0139

    We met Zach Cofran, a graduate student at Michigan, as well as a local painter that Lee has contracted to document the landscape before they construct a temporary shelter and begin systematic excavation at the site. This made for a pretty great opportunity to take in the surroundings, as we scoped out various overlooks on the area. Here's an overlook above the Malapa site itself:

    IMG_0165

    Those rocks foreground are masking a steep pitch down, we were on a pretty tall hill.

    The valley winding into the background is the Malapa drainage. Most of the dark green patches of trees are associated with some kind of karstic feature, either current caves or old ones that have largely eroded out. The landscape is really alive with cave formation processes -- the streambed itself drains into an extensive cave system and eventually emerges on the opposite side of the near hills.

    We drove down from here along the track into the valley. Lee showed us the ranch house that will house a field school, and took us down the river track (sometimes actually in the streambed) to the site.

    I would describe Malapa itself as a former cave. There is still a deep pit element, enhanced or largely created by blasting in the early twentieth century. Miners went prospecting for flowstones and other calcium carbonate features in caves, which they could reduce into lime by burning it in kilns. To get the stuff out, they had to blast through a lot of breccia -- essentially cemented sediments and debris that collect inside of caves. The breccia often contains bones of ancient animals, including in some cases hominins, sometimes very densely. At Malapa, the breccia is exposed at the surface, partly obscured by the miners' activity creating a road track along which the exploited other caves further up the hill.

    Here's the existing pit:

    IMG_0184

    That's Zach Cofran on the opposite side there.

    The skeletons recovered thus far were found in surface blocks of breccia blasted out of this pit and in the edges of the pit itself. The breccia however extends over a much greater surface, making this an incredibly promising site for further excavation and discovery.

    Well, it may not look like much in photos, but in terms of hominin fossils, it may end up being the most important fifty square meters in the world.

    IMG_0198

    I'm almost ashamed to admit that after much turning over of blocks, I didn't find any hominins. At least not any that haven't already been found by somebody else first. But we had plenty left to see. A drive up a further track would take us to some other very interesting places. Lee drove us to the spot where the river comes welling back up out of its cave system -- as he described it, the water exits 75 years after it first enters. Here he is with his ridgeback companions:

    IMG_0247

    After some geology I won't describe, along with an empty leopard den, we continued onward encountering many of the other species of large mammals on the nature reserve. Luckily, I use a Canon body so I could borrow the 400 mm telephoto lens to get some great shots. There were plenty of wildebeest:

    IMG_0298

    And some giraffes (for Goodwin!):

    IMG_0310

    And a kudu bull with a wonky horn:

    IMG_0325

    Now, in my ordinary life I really have few occasions when a long lens would be very useful, but I could get used to having one for these situations.

    Near the end of this little safari, we hit Gladysvale Cave, which has a very impressive large upper gallery and two lower ones we didn't enter. Lee worked Gladysvale for many years finding a handful of hominin remains but endless antelope bones.

    IMG_0286

    It's a problem with field sites -- the hominins are only a part of an ancient landscape which was occupied by many species. Our relatives were patchily distributed, but they did end up in caves sometimes due to several different causes. The skeletons in Malapa are remarkably complete, suggesting a distinctive history of formation of the site. Large sites may be made up of many such episodes.

    As for Gladysvale, it is still actively used by large herbivores, whose tracks go right into the cave. They may be seeking minerals, as there is no water pool inside.

    This was near the end of our drive, and so I'll stop the story. Again, I've got lots to see ahead of me this week, but hopefully I'll have some Denisova news typed up soon.

    Synopsis: 
    Lee Berger took me out to the Malapa site. Here's the story.
  • MSA ochre "factory"

    Thu, 2010-06-03 11:49 -- John Hawks

    Jennifer Viegas covers the recent discoveries at Sibudu Cave, South Africa: "Stone Age color, glue 'factory' found".

    A once-thriving 58,000-year-old ochre powder production site has just been discovered in South Africa. The discovery offers a glimpse of what early humans valued and used in their everyday lives.

    The finding, which will be described in the Journal of Archaeological Science, also marks the first time that any Stone Age site has yielded evidence for ochre powder processing on cemented hearths -- an innovation for the period. A clever caveman must have figured out that white ash from hearths can cement and become rock hard, providing a sturdy work surface.

    This appears to have been a site of intensive processing, with thousands of pieces of ochre nearby. I wonder whether the intensification implies a trade network for exchange of the product.

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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.