The Secrets of Laetoli Trackway
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Geologists Probe Hominid Environments
1999 PRESIDENTIAL ADDRESS Geologists Probe Hominid Environments Gail M. Ashley, Department of Geological Sciences, Rutgers University, New Brunswick, NJ 08903, USA, [email protected] ABSTRACT challenging areas of research often lie at artificially imposed disci- pline boundaries. Here lies the potential for synergy and perhaps The study of an early Pleistocene “time slice” in Olduvai even the generation of a new science (Fig. 2). However, integrat- Gorge, Tanzania, provides a successful example of a recon- ing sciences is not as easy as it might first appear. It requires peo- structed paleolandscape that is rich in detail and adds a small ple to learn language, theories, methodologies, and a bit about piece to the puzzle of hominid evolution in Africa. The recon- the “culture” of the other science and to continually walk in the struction required multidisciplinary interaction of sedimen- other person’s shoes. Simply having lots of scientists with differ- tologists, paleoanthropologists, paleoecologists, and geochro- ent backgrounds working in parallel on the same project doesn’t nologists. Geology plays an increasingly important role in produce the same end result as integrative science. unraveling the record of hominid evolution. Key questions This paper describes a study at Olduvai Gorge, Tanzania (Fig. regarding paleoclimate, paleoenvironment, and perhaps even 3), using a relatively new approach, landscape paleoanthropol- hominid land use are answered by geology, and these answers ogy, that attempts to interpret the landscape during a geologic provide a basis for multidisciplinary work. Landscape pale- instant in time. The project is the Olduvai Landscape Paleo- oanthropology integrates these data from several disciplines anthropology Project (OLAPP), involving a multidisciplinary to interpret the ecological context of hominids during a nar- team. -
Lieberman 2001E.Pdf
news and views Another face in our family tree Daniel E. Lieberman The evolutionary history of humans is complex and unresolved. It now looks set to be thrown into further confusion by the discovery of another species and genus, dated to 3.5 million years ago. ntil a few years ago, the evolutionary history of our species was thought to be Ureasonably straightforward. Only three diverse groups of hominins — species more closely related to humans than to chim- panzees — were known, namely Australo- pithecus, Paranthropus and Homo, the genus to which humans belong. Of these, Paran- MUSEUMS OF KENYA NATIONAL thropus and Homo were presumed to have evolved between two and three million years ago1,2 from an early species in the genus Australopithecus, most likely A. afarensis, made famous by the fossil Lucy. But lately, confusion has been sown in the human evolutionary tree. The discovery of three new australopithecine species — A. anamensis3, A. garhi 4 and A. bahrelghazali5, in Kenya, Ethiopia and Chad, respectively — showed that genus to be more diverse and Figure 1 Two fossil skulls from early hominin species. Left, KNM-WT 40000. This newly discovered widespread than had been thought. Then fossil is described by Leakey et al.8. It is judged to represent a new species, Kenyanthropus platyops. there was the finding of another, as yet poorly Right, KNM-ER 1470. This skull was formerly attributed to Homo rudolfensis1, but might best be understood, genus of early hominin, Ardi- reassigned to the genus Kenyanthropus — the two skulls share many similarities, such as the flatness pithecus, which is dated to 4.4 million years of the face and the shape of the brow. -
Paranthropus Through the Looking Glass COMMENTARY Bernard A
COMMENTARY Paranthropus through the looking glass COMMENTARY Bernard A. Wooda,1 and David B. Pattersona,b Most research and public interest in human origins upper jaw fragment from Malema in Malawi is the focuses on taxa that are likely to be our ancestors. southernmost evidence. However, most of what we There must have been genetic continuity between know about P. boisei comes from fossils from Koobi modern humans and the common ancestor we share Fora on the eastern shore of Lake Turkana (4) and from with chimpanzees and bonobos, and we want to know sites in the Nachukui Formation on the western side of what each link in this chain looked like and how it be- the lake (Fig. 1A). haved. However, the clear evidence for taxic diversity The cranial and dental morphology of P.boisei is so in the human (aka hominin) clade means that we also distinctive its remains are relatively easy to identify (5). have close relatives who are not our ancestors (1). Two Unique features include its flat, wide, and deep face, papers in PNAS focus on the behavior and paleoenvi- flexed cranial base, large and thick lower jaw, and ronmental context of Paranthropus boisei, a distinctive small incisors and canines combined with massive and long-extinct nonancestral relative that lived along- chewing teeth. The surface area available for process- side our early Homo ancestors in eastern Africa between ing food is extended both forward—by having premo- just less than 3 Ma and just over 1 Ma. Both papers use lar teeth that look like molars—and backward—by the stable isotopes to track diet during a largely unknown, unusually large third molar tooth crowns, all of which but likely crucial, period in our evolutionary history. -
Tanzania.Pdf
FEATURE Tanzania field school Shaping Students and Communities in Tanzania ummer 2007: 13 students and And, of high importance to students, it costs going way back to when I was an undergrad.” two professors from UC Denver much less than most other field schools. Musiba also reached out to universities are awakened in the middle of All of those benefits and partnerships are around the globe, including the University S the night by noises normally only the result of Musiba’s relationships with locals, of Kyoto in Japan and the Bugando University heard in a zoo. Although many lie awake in his passion for the country and his drive to College of Health Sciences in Mwanza, Tanzania. their tents, one among them sleeps peacefully. create global citizens of his students. “When I talk to people at anthropology Charles Musiba, assistant professor of meetings and tell them that our field school only anthropology, was born in Tanzania, Africa, In the Beginning costs about $4,500, I tell them that it’s because and now directs UCD’s Tanzania Field School. “I was myself a graduate student and saw that we do a lot of cost sharing with these partners.” He’s been taking I could become a bridge to Tanzania and help students to his my fellow graduate students gain access to new country for 11 years. areas for their research,” says Musiba. “But The field most existing field schools in Africa are very school is located expensive. Those run at schools like Rutgers, in the Ngorongoro Harvard and Yale cost between $6,000 to Conservation Area $7,000 just for tuition, not counting airfare.” in northern Tanzania Musiba began collaborating with people he and, according to all knew in Tanzania, and they smoothed out a accounts, it offers normally difficult process. -
Vegetation of Northern Tanzania During the Plio-Pleistocene: a Synthesis of the Paleobotanical Evidences from Laetoli, Olduvai, and Peninj Hominin Sites
Quaternary International 322-323 (2014) 264e276 Contents lists available at ScienceDirect Quaternary International journal homepage: www.elsevier.com/locate/quaint Vegetation of Northern Tanzania during the Plio-Pleistocene: A synthesis of the paleobotanical evidences from Laetoli, Olduvai, and Peninj hominin sites Doris Barboni CEREGE, Aix-Marseille University, UM34, CNRS, IRD, Europole de l’Arbois, BP80, 13545 Aix-en-Provence cedex 4, France article info abstract Article history: More than 40 years of scientific investigations of the hominin bearing Plio-Pleistocene sediments of Available online 5 February 2014 northern Tanzania have provided a number of paleobotanical data, which, taken as a whole, provide today a way to investigate vegetation changes between 4 and 1 Ma, at a time when our early ancestors emerged. Here, I have integrated the data from all vegetation proxies obtained for the paleontological sites of Laetoli, Olduvai, and Peninj (i.e. macroscopic plant remains, pollen and phytolith assemblages, carbon and oxygen isotopic ratios measured on carbonates, and organic biomarkers). This important, yet discontinuous botanical record suggests some similarities between past and present-day vegetation at the regional scale: Afromontane forests with Olea, Podocarpus, Juniperus, Hagenia abyssinica in the highlands, and wooded grasslands with grasses and drought-adapted Acacia, Commiphora, Cappar- idaceae, and Chenopodiaceae and/or Amaranthaceae in the lowlands were present in the southern SerengetieCrater Highlands region since 4 Ma. Grasses of the C4 photosynthetic type made their first appearance in the record at w3.7 Ma, i.e. during the mid-Pliocene, w700 ky before major pCO2 and temperature decline. C4 grasses became dominant in the vegetation soon after (w3.66 Ma), probably in response to reduced precipitation. -
Harrison CV Jan 2018
January 4, 2018 Terry Harrison CURRICULUM VITAE CONTACT INFORMATION * Center for the Study of Human Origins Department of Anthropology 25 Waverly Place New York University New York, NY 10003-6790, USA 8 [email protected] ) 212-998-8581 WEB LINKS http://anthropology.as.nyu.edu/object/terryharrison.html http://csho.as.nyu.edu/object/terryharrison.html https://nyu.academia.edu/TerryHarrison http://orcid.org/0000-0003-4224-0152 zoobank.org:author:43DA2256-CF4D-476F-8EA8-FBCE96317505 ACADEMIC BACKGROUND Graduate: 1978–1982: Doctor of Philosophy. Department of Anthropology, University College London, London. Doctoral dissertation: Small-bodied Apes from the Miocene of East Africa. 1981–1982: Postgraduate Certificate of Education. Institute of Education, London University, London. Awarded with Distinction. Undergraduate: 1975–1978: Bachelor of Science. Department of Anthropology, University College London, London. First Class Honours. POSITIONS 2014- Silver Professor, Department of Anthropology, New York University. 2003- Director, Center for the Study of Human Origins, New York University. 1995- Professor, Department of Anthropology, New York University. 2010-2016 Chair, Department of Anthropology, New York University. 1995-2010 Associate Chair, Department of Anthropology, New York University. 1990-1995 Associate Professor, Department of Anthropology, New York University. 1984-1990 Assistant Professor, Department of Anthropology, New York University. HONORS & AWARDS 1977 Rosa Morison Memorial Medal and Prize, University College London. 1978 Daryll Forde Award, University College London. 1989 Golden Dozen Award for excellence in teaching, New York University. 1996 Golden Dozen Award for excellence in teaching, New York University. 2002 Distinguished Teacher Award, New York University. 2006 Fellow, American Association for the Advancement of Science. -
Isotopic Evidence for the Timing of the Dietary Shift Toward C4 Foods in Eastern African Paranthropus Jonathan G
Isotopic evidence for the timing of the dietary shift toward C4 foods in eastern African Paranthropus Jonathan G. Wynna,1, Zeresenay Alemsegedb, René Bobec,d, Frederick E. Grinee, Enquye W. Negashf, and Matt Sponheimerg aDivision of Earth Sciences, National Science Foundation, Alexandria, VA 22314; bDepartment of Organismal Biology and Anatomy, The University of Chicago, Chicago, IL 60637; cSchool of Anthropology, University of Oxford, Oxford OX2 6PE, United Kingdom; dGorongosa National Park, Sofala, Mozambique; eDepartment of Anthropology, Stony Brook University, Stony Brook, NY 11794; fCenter for the Advanced Study of Human Paleobiology, George Washington University, Washington, DC 20052; and gDepartment of Anthropology, University of Colorado Boulder, Boulder, CO 80302 Edited by Thure E. Cerling, University of Utah, Salt Lake City, UT, and approved July 28, 2020 (received for review April 2, 2020) New approaches to the study of early hominin diets have refreshed the early evolution of the genus. Was the diet of either P. boisei or interest in how and when our diets diverged from those of other P. robustus similar to that of the earliest members of the genus, or did African apes. A trend toward significant consumption of C4 foods in thedietsofbothdivergefromanearliertypeofdiet? hominins after this divergence has emerged as a landmark event in Key to addressing the pattern and timing of dietary shift(s) in human evolution, with direct evidence provided by stable carbon Paranthropus is an appreciation of the morphology and dietary isotope studies. In this study, we report on detailed carbon isotopic habits of the earliest member of the genus, Paranthropus evidence from the hominin fossil record of the Shungura and Usno aethiopicus, and how those differ from what is observed in later Formations, Lower Omo Valley, Ethiopia, which elucidates the pat- representatives of the genus. -
Large Mammal Evidence for the Paleoenvironment of the Upper Laetolil and Upper Ndolanya Beds of Laetoli, Tanzania
Chapter 19 Large Mammal Evidence for the Paleoenvironment of the Upper Laetolil and Upper Ndolanya Beds of Laetoli, Tanzania Denise F. Su Abstract There has been much debate on the environment of faunal and paleoecological analyses (papers in Leakey and Pliocene Laetoli. These disagreements reflect the complexity Harris 1987; Reed 1997; Kovarovic and Andrews 2007; Su and of the paleoenvironment and the difficulties in reconciling Harrison 2007, 2008), it is clear that Pliocene Laetoli was most contradictory evidence. In this paper, the community struc- likely ecologically heterogenous, but it is unclear as to the ture of the large mammal fauna at Laetoli is compared to that proportion and the changes in the geographical and temporal of modern faunal communities and the relative abundances distribution of the different habitats. Taphonomic and geologic of bovid tribes are examined. The results of these analyses analyses suggest that the heterogeneity seen in the Laetoli large are interpreted within the context of other lines of evidence, mammal fauna was not the result of time-averaged and trans- including those based on rodents, gastropods, phytoliths, sta- ported assemblages, but rather a reflection of the mosaic nature ble isotopes and mesowear. The balance of evidence suggests of the environment at the time of deposition (Su and Harrison that the ecology of the Upper Laetolil Beds was a mosaic of 2007, 2008). The lack of higher-level resolution in the data and grassland-shrubland-open woodland habitats with extensive the difficulty in resolving and integrating the contradictory woody vegetation in the form of shrubs, thickets, and bush. inferences from different lines of evidence are major factors in There was also a significant presence of dense woodland and the debate. -
UNIVERSITY of CALGARY Lithic Raw Material Characterisation At
UNIVERSITY OF CALGARY Lithic Raw Material Characterisation at Olduvai Gorge, Tanzania by Julien Favreau A THESIS SUBMITTED TO THE FACULTY OF GRADUATE STUDIES IN PARTIAL FULFILMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF ARTS GRADUATE PROGRAM IN ARCHAEOLOGY CALGARY, ALBERTA APRIL, 2019 © Julien Favreau 2019 Abstract Olduvai Gorge is located within the Ngorongoro Conservation Area, a UNESCO World Heritage Site in northern Tanzania along the western margin of the East African Rift System. Olduvai’s sedimentary record exhibits a complex sequence of inter-stratified lithic technologies including Oldowan, Acheulean, Middle Stone Age, and Later Stone Age assemblages. While diachronic technological change is perceptible, one aspect that remained largely unchanged through time was the totality of locally available rock types. This study constitutes Olduvai Gorge’s first systematic survey and characterisation of source lithologies using thin section petrography. The primary objectives of this thesis were to establish the range of available lithic raw materials, petrographically characterise these, and determine if there were unique inter-outcrop petrographic signatures to determine if it is feasible to source lithic artifacts at the mineralogical level. Geological samples were collected in primary and secondary positions within the greater Olduvai Gorge region. A total of seventy-four thin sections of sixty-two geological samples from nineteen sources were analysed. By way of comparative analyses, it is shown that four quartzitic outcrops have unique mineral compositions, four meta-granite varieties are unique to individual outcrops, Engelosin phonolite samples are texturally and mineralogically unique, and magmatic samples recovered in secondary position may be sourced to their volcanic centre. -
Ngorongoro Conservation Area Tanzania
NGORONGORO CONSERVATION AREA TANZANIA An immense concentration of wild animals live in the huge and perfect crater of Ngorongoro. It is home to a small relict population of black rhinoceros and some 25,000 other large animals, largely ungulates, alongside the highest density of mammalian predators in Africa. Lake-filled Empakaai crater and the active volcano of Oldonyo Lenga are nearby. Excavations in the Olduvai Gorge and Laetoli to the west, have resulted in discoveries such as Homo habilis and 3.5 million-year old human footprints which have made the area one of the world’s most important for research on the evolution of the human species. Threats to the site: The greatly increased pressures of tourism and high numbers of Maasai pastoralists and settlers have begun to degrade the quality of the site. COUNTRY Tanzania NAME Ngorongoro Conservation Area MIXED NATURAL AND CULTURAL WORLD HERITAGE SITE 1979: Inscribed on the World Heritage List under Natural Criteria vii, viii, ix and x. 1984-1988: Listed as World Heritage in danger owing to conflict with the Maasai. 2010: Inscribed on the World Heritage List as a Cultural Landscape under Cultural Criterion iv. STATEMENT OF OUTSTANDING UNIVERSAL VALUE The UNESCO World Heritage Committee issued the following Statement of Outstanding Universal Value at the time of inscription: Brief Synthesis The Ngorongoro Conservation Area (809,440 ha) spans vast expanses of highland plains, savanna, savanna woodlands and forests, from the plains of the Serengeti National Park in the north-west, to the eastern arm of the Great Rift Valley. The area was established in 1959 as a multiple land use area, with wildlife coexisting with semi- nomadic Maasai pastoralists practising traditional livestock grazing. -
Australopithecus Afarensis Postcranium from Woranso-Mille, Ethiopia
An early Australopithecus afarensis postcranium from Woranso-Mille, Ethiopia Yohannes Haile-Selassiea,b,c,1, Bruce M. Latimera,b,c, Mulugeta Alened, Alan L. Deinoe, Luis Giberte, Stephanie M. Melillof, Beverly Z. Saylorg, Gary R. Scotte, and C. Owen Lovejoya,h,1 aThe Cleveland Museum of Natural History, Cleveland, OH 44106; bDepartment of Anthropology, cThe Institute for the Science of Origins, and gDepartment of Geological Sciences, Case Western Reserve University, Cleveland, OH 44106; dDepartment of Earth Sciences, Addis Ababa University, Addis Ababa, Ethiopia 1176; eBerkeley Geochronology Center, Berkeley, CA 94709; fDepartment of Biology, Stanford University, Stanford, CA 94305; and hDepartment of Anthropology, School of Biomedical Sciences, Kent State University, Kent, OH 44242 Contributed by C. Owen Lovejoy, April 16, 2010 (sent for review February 22, 2010) Only one partial skeleton that includes both forelimb and hindlimb Taxonomy elements has been reported for Australopithecus afarensis. The di- KSD-VP-1/1 antedates A.L. 288–1 (4) by roughly 0.4 Ma and is minutive size of this specimen (A.L. 288-1 ["Lucy"]) has hampered generally contemporaneous with specimens from Laetoli (in- our understanding of the paleobiology of this species absent the cluding the type specimen) (5). Although the absence of cranial potential impact of allometry. Here we describe a large-bodied (i.e., and dental elements imposes some restrictions on the specimen’s well within the range of living Homo) specimen that, at 3.58 Ma, taxonomic assignment, it shares a substantial number of post- – also substantially antedates A.L. 288 1. It provides fundamental cranial elements with homologs in A.L. -
Australopithecus Afarensis
Australopithecus afarensis Nickname: Lucy's species Where Lived: Eastern Africa (Ethiopia, Kenya, Tanzania) When Lived: Between about 3.85 and 2.95 million years ago Australopithecus afarensis is one of the longestlived and bestknown early human species—paleoanthropologists have uncovered remains from more than 300 individuals! Found between 3.85 and 2.95 million years ago in Eastern Africa (Ethiopia, Kenya, Tanzania), this species survived for more than 900,000 years, which is over four times as long as our own species has been around. It is best known from the sites of Hadar, Ethiopia (‘Lucy’, AL 2881 and the 'First Family', AL 333); Dikika, Ethiopia (Dikika ‘child’ skeleton); and Laetoli (fossils of this species plus the oldest documented bipedal footprint trails). Similar to chimpanzees, Au. afarensis children grew rapidly after birth and reached adulthood earlier than modern humans. This meant Au. afarensis had a shorter period of growing up than modern humans have today, leaving them less time for parental guidance and socialization during childhood. Au. afarensis had both ape and human characteristics: members of this species had apelike face proportions (a flat nose, a strongly projecting lower jaw) and braincase (with a small brain, usually less than 500 cubic centimeters about 1/3 the size of a modern human brain), and long, strong arms with curved fingers adapted for climbing trees. They also had small canine teeth like all other early humans, and a body that stood on two legs and regularly walked upright. Their adaptations for living both in the trees and on the ground helped them survive for almost a million years as climate and environments changed.