Field School
Total Page:16
File Type:pdf, Size:1020Kb

Load more
Recommended publications
-
Homo Habilis
COMMENT SUSTAINABILITY Citizens and POLICY End the bureaucracy THEATRE Shakespeare’s ENVIRONMENT James Lovelock businesses must track that is holding back science world was steeped in on surprisingly optimistic governments’ progress p.33 in India p.36 practical discovery p.39 form p.41 The foot of the apeman that palaeo ‘handy man’, anthropologists had been Homo habilis. recovering in southern Africa since the 1920s. This, the thinking went, was replaced by the taller, larger-brained Homo erectus from Asia, which spread to Europe and evolved into Nean derthals, which evolved into Homo sapiens. But what lay between the australopiths and H. erectus, the first known human? BETTING ON AFRICA Until the 1960s, H. erectus had been found only in Asia. But when primitive stone-chop LIBRARY PICTURE EVANS MUSEUM/MARY HISTORY NATURAL ping tools were uncovered at Olduvai Gorge in Tanzania, Leakey became convinced that this is where he would find the earliest stone- tool makers, who he assumed would belong to our genus. Maybe, like the australopiths, our human ancestors also originated in Africa. In 1931, Leakey began intensive prospect ing and excavation at Olduvai Gorge, 33 years before he announced the new human species. Now tourists travel to Olduvai on paved roads in air-conditioned buses; in the 1930s in the rainy season, the journey from Nairobi could take weeks. The ravines at Olduvai offered unparalleled access to ancient strata, but field work was no picnic in the park. Water was often scarce. Leakey and his team had to learn to share Olduvai with all of the wild animals that lived there, lions included. -
Hands-On Human Evolution: a Laboratory Based Approach
Hands-on Human Evolution: A Laboratory Based Approach Developed by Margarita Hernandez Center for Precollegiate Education and Training Author: Margarita Hernandez Curriculum Team: Julie Bokor, Sven Engling A huge thank you to….. Contents: 4. Author’s note 5. Introduction 6. Tips about the curriculum 8. Lesson Summaries 9. Lesson Sequencing Guide 10. Vocabulary 11. Next Generation Sunshine State Standards- Science 12. Background information 13. Lessons 122. Resources 123. Content Assessment 129. Content Area Expert Evaluation 131. Teacher Feedback Form 134. Student Feedback Form Lesson 1: Hominid Evolution Lab 19. Lesson 1 . Student Lab Pages . Student Lab Key . Human Evolution Phylogeny . Lab Station Numbers . Skeletal Pictures Lesson 2: Chromosomal Comparison Lab 48. Lesson 2 . Student Activity Pages . Student Lab Key Lesson 3: Naledi Jigsaw 77. Lesson 3 Author’s note Introduction Page The validity and importance of the theory of biological evolution runs strong throughout the topic of biology. Evolution serves as a foundation to many biological concepts by tying together the different tenants of biology, like ecology, anatomy, genetics, zoology, and taxonomy. It is for this reason that evolution plays a prominent role in the state and national standards and deserves thorough coverage in a classroom. A prime example of evolution can be seen in our own ancestral history, and this unit provides students with an excellent opportunity to consider the multiple lines of evidence that support hominid evolution. By allowing students the chance to uncover the supporting evidence for evolution themselves, they discover the ways the theory of evolution is supported by multiple sources. It is our hope that the opportunity to handle our ancestors’ bone casts and examine real molecular data, in an inquiry based environment, will pique the interest of students, ultimately leading them to conclude that the evidence they have gathered thoroughly supports the theory of evolution. -
Curren T Anthropology
Forthcoming Current Anthropology Wenner-Gren Symposium Curren Supplementary Issues (in order of appearance) t Humanness and Potentiality: Revisiting the Anthropological Object in the Anthropolog Current Context of New Medical Technologies. Klaus Hoeyer and Karen-Sue Taussig, eds. Alternative Pathways to Complexity: Evolutionary Trajectories in the Anthropology Middle Paleolithic and Middle Stone Age. Steven L. Kuhn and Erella Hovers, eds. y THE WENNER-GREN SYMPOSIUM SERIES Previously Published Supplementary Issues December 2012 HUMAN BIOLOGY AND THE ORIGINS OF HOMO Working Memory: Beyond Language and Symbolism. omas Wynn and Frederick L. Coolidge, eds. GUEST EDITORS: SUSAN ANTÓN AND LESLIE C. AIELLO Engaged Anthropology: Diversity and Dilemmas. Setha M. Low and Sally Early Homo: Who, When, and Where Engle Merry, eds. Environmental and Behavioral Evidence V Dental Evidence for the Reconstruction of Diet in African Early Homo olum Corporate Lives: New Perspectives on the Social Life of the Corporate Form. Body Size, Body Shape, and the Circumscription of the Genus Homo Damani Partridge, Marina Welker, and Rebecca Hardin, eds. Ecological Energetics in Early Homo e 5 Effects of Mortality, Subsistence, and Ecology on Human Adult Height 3 e Origins of Agriculture: New Data, New Ideas. T. Douglas Price and Plasticity in Human Life History Strategy Ofer Bar-Yosef, eds. Conditions for Evolution of Small Adult Body Size in Southern Africa Supplement Growth, Development, and Life History throughout the Evolution of Homo e Biological Anthropology of Living Human Populations: World Body Size, Size Variation, and Sexual Size Dimorphism in Early Homo Histories, National Styles, and International Networks. Susan Lindee and Ricardo Ventura Santos, eds. -
Lake Turkana and the Lower Omo the Arid and Semi-Arid Lands Account for 50% of Kenya’S Livestock Production (Snyder, 2006)
Lake Turkana & the Lower Omo: Hydrological Impacts of Major Dam & Irrigation Development REPORT African Studies Centre Sean Avery (BSc., PhD., C.Eng., C. Env.) © Antonella865 | Dreamstime © Antonella865 Consultant’s email: [email protected] Web: www.watres.com LAKE TURKANA & THE LOWER OMO: HYDROLOGICAL IMPACTS OF MAJOR DAM & IRRIGATION DEVELOPMENTS CONTENTS – VOLUME I REPORT Chapter Description Page EXECUTIVE(SUMMARY ..................................................................................................................................1! 1! INTRODUCTION .................................................................................................................................... 12! 1.1! THE(CONTEXT ........................................................................................................................................ 12! 1.2! THE(ASSIGNMENT .................................................................................................................................. 14! 1.3! METHODOLOGY...................................................................................................................................... 15! 2! DEVELOPMENT(PLANNING(IN(THE(OMO(BASIN ......................................................................... 18! 2.1! INTRODUCTION(AND(SUMMARY(OVERVIEW(OF(FINDINGS................................................................... 18! 2.2! OMO?GIBE(BASIN(MASTER(PLAN(STUDY,(DECEMBER(1996..............................................................19! 2.2.1! OMO'GIBE!BASIN!MASTER!PLAN!'!TERMS!OF!REFERENCE...........................................................................19! -
Lake Turkana National Parks - 2017 Conservation Outlook Assessment (Archived)
IUCN World Heritage Outlook: https://worldheritageoutlook.iucn.org/ Lake Turkana National Parks - 2017 Conservation Outlook Assessment (archived) IUCN Conservation Outlook Assessment 2017 (archived) Finalised on 26 October 2017 Please note: this is an archived Conservation Outlook Assessment for Lake Turkana National Parks. To access the most up-to-date Conservation Outlook Assessment for this site, please visit https://www.worldheritageoutlook.iucn.org. Lake Turkana National Parks عقوملا تامولعم Country: Kenya Inscribed in: 1997 Criteria: (viii) (x) The most saline of Africa's large lakes, Turkana is an outstanding laboratory for the study of plant and animal communities. The three National Parks serve as a stopover for migrant waterfowl and are major breeding grounds for the Nile crocodile, hippopotamus and a variety of venomous snakes. The Koobi Fora deposits, rich in mammalian, molluscan and other fossil remains, have contributed more to the understanding of paleo-environments than any other site on the continent. © UNESCO صخلملا 2017 Conservation Outlook Critical Lake Turkana’s unique qualities as a large lake in a desert environment are under threat as the demands for water for development escalate and the financial capital to build major dams becomes available. Historically, the lake’s level has been subject to natural fluctuations in response to the vicissitudes of climate, with the inflow of water broadly matching the amount lost through evaporation (as the lake basin has no outflow). The lake’s major source of water, Ethiopia’s Omo River is being developed with a series of major hydropower dams and irrigated agricultural schemes, in particular sugar and other crop plantations. -
The Larger Mammal Fossil Assemblages from Beds Iii and Iv, Olduvai Gorge
THE LARGER MAMMAL FOSSIL ASSEMBLAGES FROM BEDS III AND IV, OLDUVAI GORGE, TANZANIA: IMPLICATIONS FOR THE FEEDING BEHAVIOR OF HOMO ERECTUS by MICHAEL C. PANTE A Dissertation submitted to the Graduate School‐New Brunswick Rutgers, The State University of New Jersey In partial fulfillment of the requirements For the degree of Doctor of Philosophy Graduate Program in Anthropology Written under the direction of Professor Robert Blumenschine And approved by ________________________ ________________________ ________________________ ________________________ New Brunswick, New Jersey October, 2010 2010 Michael C. Pante ALL RIGHTS RESERVED ii ABSTRACT OF THE DISSERTATION THE LARGER MAMMAL FOSSIL ASSEMBLAGES FROM BEDS III AND IV, OLDUVAI GORGE, TANZANIA: IMPLICATIONS FOR THE FEEDING BEHAVIOR OF HOMO ERECTUS By MICHAEL C. PANTE Dissertation Director: Professor Robert Blumenschine This dissertation represents the first taphonomically‐informed assessment of the feeding behavior of Homo erectus. Until now studies of the feeding behavior of Early Stone Age hominins based on the assemblage‐wide proportions of tooth, cut, and percussion marks have focused on Oldowan sites attributed to Homo habilis leaving assessments of the subsistence capabilities of Homo erectus to inference. This trend is the direct result of the river/channel depositional settings for most sites that are attributed to Homo erectus and the lack of a theoretically‐grounded basis for interpreting fossil assemblages from such sites. Using a flume I have generated the first experimental sample designed to interpret bone assemblages that were modified by hominins and carnivores and subsequently disturbed by flowing water. Results show that the transportability of bone fragments is inversely related to the size of bone fragments as measured by length, iii width, cortical thickness, and indirectly by the size group of the carcass from which the fragments were generated. -
Meave Leakey
Meave Leakey Paleoanthropologist Paleontologist and zoologist Meave Leakey is a prominent member of the famed Leakey family of paleoanthropologists who have dominated their field for over a century. Her life-long search for clues about our past has led her to every corner of the remote, windswept semi-deserts of Kenya’s Lake Turkana Basin. In 2013, the National Academy of Science elected her a Foreign Associate. Over the last four decades, the Koobi Fora Research Project, which she co-directs with her eldest daughter Louise, has unearthed much of the evidence behind our current understanding of our past. Dr. Leakey is focused on the origins of our own genus, Homo, and the emergence of Homo erectus, the first human ancestor to move out of Africa. Her research focuses on the sites around Lake Turkana, which are between 8 and 3 million years old. In 1999, 2000, and again in 2007 the project made sensational new discoveries of early Homo that indicate Ausralopithecus afarensis (also known as the skeleton named “Lucy”) might not be the only species from which the human race descended. National Geographic remarked that Dr. Leakey's findings “challenge the straight-line story of human evolution.” The announcement of these discoveries was featured in Nature and The New York Times. In August 2012 Dr. Leakey and Louise announced the discovery of 3 new fossils that indicate there were more extinct human species than previously thought. Dr. Leakey is a National Geographic Explorer-in-Residence in recognition of the 50-year relationship between “the National Geographic Society and the Leakey family dynasty of pioneering fossil hunters.” She is also a Research Professor at Stony Brook University and was the head of the division of paleontology at the National Museums of Kenya for over 30 years. -
Lake Turkana & Nabuyatom Crater
L a k e Tu rk a n a Day trip by Helicopter - 2019 Suguta sand dunes © Sam Stogdale Highlights Suguta - Turkana - Mathews Low level over the wildlife rich landscapes of Laikipia Silali Crater ‘Hoodoo’ and ‘Painted’ valleys Suguta sand dunes Flamingo on the soda lake of Logipi Southern shores of Lake Turkana & Nabuyatom crater Cycad forests of the Mathews Range Ewaso Nyiro river and the savannah landscapes of Samburu Hoodoo Valley © Tullow Oil L a k e Tu rk a n a 6 hours From the wildlife plains of Laikipia, we head north west into the Gregory Rift. Our first stop is on the summit of Silale crater, and then we drop down into the Suguta Valley. The landscape is constantly changing - desolate salt plains, lava flows and crocodile pools, through the colourful ‘painted’ and ‘hoodoo’ valleys. We touch down on the sand dunes, fly over the soda lake of Logipi where flocks of flamingo paint the shores pink, and we finally arrive at the fresh waters of Lake Turkana. Besides Nabuyatom Crater we touch down for refreshments. We return following the most scenic route, over the Ndotos and Mathews - a dominant mountain range that rises from the arid plains, with mist forests and ancient cycads on its summit. Our final leg takes us low level over the savannahs of Samburu. Lake Turkana © Sam Stogdale Silali Crater, southern end of the Suguta Valley A vast caldera, carpeted by grasses and shrubs, located at the southern tip of the Suguta Valley. @ Michael Poliza Suguta Valley Geologists have long been fascinated with this part of the Great Rift Valley. -
Case Study: Friends of Lake Turkana
Case Study: Friends of Lake Turkana Read the passage below. Ikal Angelei, 2012 winner of the prestigious Goldman Environmental Prize, works in the remote Lake Turkana region of Kenya and Ethiopia. Friends of Lake Turkana, a nonprofit organization she founded in 2007, works to stop construction of Ethiopia’s Gilgel Gibe III Dam on the Omo River. The Omo is the major tributary to Lake Turkana, and a dam upstream would drastically impact the lake environment. Changes to the lake’s chemistry and shoreline would devastate the ecology of the region, as well as the local economies that have developed around it, such as fishing, agriculture, and pastoralism. Angelei remembers being shocked on learning of the dam’s likely impact. “At first, I thought, it can’t be real,” she told the New York Times. “I couldn’t imagine the area without the lake.” Geography Located in northern Kenya, the Lake Turkana Basin is a 70,000-square-kilometer (27,027-square- mile) region that is home to Lake Turkana, the most saline lake in East Africa and the largest desert lake in the world. The area includes three national parks: Sibiloi National Park, South Island National Park, and Central Island National Park. Lake Turkana, nicknamed the “Jade Sea” due to its striking color, is a major stopover for migrating waterfowl. The surrounding area is a major breeding ground for Nile crocodiles, hippopotamuses, and a range of venomous snakes. The basin surrounding Lake Turkana is arid and receives little rainfall outside the “long rain” season of March, April, and May. -
(Kenya) National Park 1 Aberdare National Park 765.700 2 Amboseli National Park 392.000 3 Arabuko
Name Category Area (Sq. Km) % (Kenya) National Park 1 Aberdare National Park 765.700 2 Amboseli National Park 392.000 3 Arabuko Sokoke National Park 6.000 4 Central Island National Park 5.000 5 Chuylu National Park 734.270 6 Hell's Gate National Park 93.000 7 Kora National Park 1,787.000 8 Lake Nakuru National Park 188.000 9 Longonot National Park 52.000 10 Malka Mari National Park 876.000 11 Meru National Park 870.000 12 Mount Elgon National Park 169.000 13 Mount Kenya National Park 704.720 14 Nairobi National Park 117.000 15 Ndere Island National Park 4.200 16 Ol Donyo Sabuk National Park 18.000 17 Ruma National Park 120.000 18 Saiwa Swamp National Park 2.000 19 Sibiloi National Park 1,573.920 20 South Island National Park 39.000 21 Tsavo East National Park 11,747.000 22 Tsavo West National Park 9,065.000 Sub-Total (National Parks) 29,328.810 5.034 Proposed National Park 1 Bonjoge Forest Reserve Proposed National Park 21.400 2 Laikipia Proposed National Park 69.204 3 Marsabit Proposed National Park 316.587 4 Ras Tenewi Proposed National Park 0.010 Total (National Parks) 29,736.011 5.104 National Reserve 1 Arawale National Reserve 533.000 2 Bisanadi National Reserve 606.000 3 Boni National Reserve 1,339.000 4 Buffalo Springs National Reserve 131.000 5 Chepkitale National Reserve 178.200 6 Dodori National Reserve 877.000 7 Kakamega National Reserve 44.700 8 Kamnarok National Reserve 87.700 9 Laikipia National Reserve 165.000 10 Lake Bogoria National Reserve 107.000 11 Lake Kanyaboli National Reserve 41.420 12 Losai National Reserve 1,806.000 -
We Are╦Marshall, April 4, 2003
Marshall University Marshall Digital Scholar We Are ... Marshall: the Newsletter for Marshall Marshall Publications University 4-4-2003 We Are…Marshall, April 4, 2003 Office ofa M rshall University Communications Follow this and additional works at: http://mds.marshall.edu/mu_newsletter Recommended Citation Office of Marshall University Communications, "We Are…Marshall, April 4, 2003" (2003). We Are ... Marshall: the Newsletter for Marshall University. Paper 125. http://mds.marshall.edu/mu_newsletter/125 This Newsletter is brought to you for free and open access by the Marshall Publications at Marshall Digital Scholar. It has been accepted for inclusion in We Are ... Marshall: the Newsletter for Marshall University by an authorized administrator of Marshall Digital Scholar. For more information, please contact [email protected]. We Are...Marshall! THE NEWSLETTER FOR MARSHALL UNIVERSITY • APRIL 4, 2003 Convocation, Speakers Celebrate Academics Dr. Meave G. Leakey, a paleoanthropologist who in daughter-in-law of Louis and Mary Leakey, who are August 1999 led a research team in Africa that found a 3.5 famous for their fossil finding. For decades, Meave million-year-old skull and partial jaw said to belong to a Leakey has spent summer months in the dried riverbeds direct ancestor of humans, is the featured speaker at the around Lake Turkana in Kenya. In addition to her field Elizabeth Gibson Drinko Honors work there, Leakey’s research has focused on the evolu- Convocation, April 4 tion of East African fossil mammals and mammalian The convocation highlights the faunas as documented in the Turkana Basin. ninth annual John Deaver Drinko and “This is a wonderful, unique opportunity for Marshall Elizabeth Gibson Drinko Celebration students to hear one of the foremost scientists in the field of Academics, which is taking place of paleontology,” said Dr. -
The Annual Flood of the Omo River
ABSTRACT The multiple impacts of a major hydrodam development project on Ethiopia’s Omo River are examined through a resource use and natural system analysis focused on the half million indigenous people whose lives would be radically changed by the dam’s downstream environmental consequences. The author warns of an impending human rights and ecological catastrophe that is being minimized by the governments of the three nation states that border the Omo and Lake Turkana basins. The very real threat of mass starvation and armed conflict in the border region of Kenya, Ethiopia and South Sudan is attributed to government and development agency inaction and indifference to the impacts of the dam project. Despite ample data to the contrary, development banks, industrial firms and governmental agencies have produced reports and plans that minimize the impacts and exaggerate the benefits. This interdisciplinary report serves as a critique of this process as it examines well funded and ostensibly authoritative studies that use limnological data, biological data, hydrology, and geology to make a case for the dam, while the author expands on the analysis using field data, socioeconomic studies and ecological as well as geological studies to call the wisdom of the project into question. The author has several decades of experience in the area, has published a monograph and articles on the Lower Omo Basin, and is currently engaged in cooperative research within the broader transborder region. PREFATORY NOTE At stake with the planned Gibe III hydrodam on Ethiopia's Omo River is the political choice to either provide for the survival of hundreds of thousands of Sub-Saharan Africa's most impoverished and marginalized indigenous people and maintain the fragile peace in one of the world's most volatile border areas, or to bring mass starvation and death to these people, with the very high likelihood of unleashing regional armed conflict reaching across the borders of all three nations.