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Paleoanthropology: Reconstructing Early Hominid Behavior and Ecology

Explore the diverse field of paleoanthropology and learn how experts reconstruct the behavior, ecology, and anatomy of our early hominid ancestors. Discover the dating methods and excavations at Olduvai Gorge, as well as the fascinating concept of mosaic evolution.

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Paleoanthropology: Reconstructing Early Hominid Behavior and Ecology

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  1. Chapter 10 Paleoanthropology: Reconstructing Early Hominid Behavior and Ecology

  2. Chapter Outline • Definition of Hominid • The Strategy of Paleoanthropology • Paleoanthropology in Action—Olduvai Gorge • Dating Methods • Excavations at Olduvai

  3. Chapter Outline • Experimental Archaeology • Reconstruction of Early Hominid Environments and Behavior • Issue: The Piltdown Caper: Whodunit?

  4. Definition of Hominid • The earliest evidence of hominids dates to the end of the Miocene and includes dental and cranial pieces. • Modern humans, as well as our most immediate hominid ancestors, are distinguished from the great apes by more obvious features than tooth and jaw dimensions.

  5. Mosaic Evolution • A pattern of evolution in which the rates of evolution in one functional system vary from those in other systems. • For example, in hominid evolution, the dental system, locomotor system, and neurological system (especially the brain) all evolved at markedly different rates.

  6. Culture • Extrasomatic (non-bodily) adaptations to the environment. • This includes systematic learned behaviors that can be communicated to others. • Aspects of this capacity have been identified among our closest ape relatives.

  7. Mosaic Evolutionof Hominid Characteristics

  8. Mosaic Evolutionof Hominid Characteristics

  9. Mosaic Evolutionof Hominid Characteristics

  10. Mosaic Evolutionof Hominid Characteristics

  11. Paleoanthropology • Paleoanthropology is the study of early humans. • Paleoanthropologists reconstruct the anatomy, behavior, and ecology of our ancestors: • It is a diverse multidisciplinary pursuit seeking to reconstruct every bit of information possible concerning the dating, anatomy, behavior, and ecology of our hominid ancestors.

  12. Subdisciplines of Paleoanthropology

  13. Multidisciplinary • Refers to research involving mutual contributions and cooperation of experts from various scientific fields (i.e., disciplines).

  14. Artifacts • Objects or materials made or modified for use by hominids. • The earliest artifacts are usually made of stone or, occasionally, bone.

  15. Taphonomy • The study of how bones and other materials came to be buried in the earth and preserved as fossils. • Taphonomists study the processes of sedimentation, the action of streams, preservation properties of bone, and carnivore disturbance factors.

  16. Context • The environmental setting where an archaeological trace is found. • Primary context is the setting in which the archaeological trace was originally deposited. • A secondary context is one to which it has been moved (such as by the action of a stream).

  17. Olduvai Gorge • Louis and Mary Leakey conducted continuous excavations from the 1930's to early 1980. • Paleontological evidence includes more than 150 species of extinct animals which can provide clues to the ecological conditions of early hominid habitats.

  18. Zinjanthropus • Zinjanthropus cranium, discovered by Mary Leakey at Olduvai Gorge in 1959. • This fossil is now included as part of the genus Paranthropus.

  19. The Main Gorge at Olduvai

  20. Olduvai Gorge • Geological processes make Olduvai extremely important to paleoanthropological investigation: • Faulting exposes geological beds near the surface. • Active volcanic processes cause rapid sedimentation which preserves bone and artifacts. • Volcanic activity provides a wealth of radiometrically datable material.

  21. Dating Methods • Paleoanthropologists use two types of dating methods to tell us the age of sites and fossils: • Relative dating determines only whether an object is older or younger than other objects. • Chronometric (absolute) dating provides an estimate of age in years based on radioactive decay.

  22. Relative and Chronometric Dating

  23. Relative Dating Techniques • Stratigrapy • Based on the law of superposition, that a lower stratum (layer) is older than a higher stratum. • Fluorine analysis • Applies to buried bones and groundwater seepage. Bones incorporate fluorine during fossilization.

  24. Relative Dating Techniques • Biostratigraphy • Related to changes in the dentition of animals. • Paleomagnetism • Based on the shifting of the geomagnetic pole.

  25. Chronometric Dating Techniques • The age of an object can be determined by measuring the rate of disintegration: • Potassium/argon (k/Ar) dating involves the decay of potassium into argon gas. K/Ar has a half-life of 1.25 billion years. • Carbon-14 is a radiometric method commonly used by archeologists. Carbon 14 has a half-life of 5730 years.

  26. Thermoluminiscence • Technique for dating certain archaeological materials, such as stone tools, heated in the past, that release stored energy of radioactive decay as light upon reheating.

  27. Question • The dating technique for dating stone tools heated in the past that release stored energy of radioactive decay as light upon reheating is: • radiocarbon (C-14). • thermoluminiscence. • stratigraphy. • fission-track.

  28. Answer: b • The dating technique for dating stone tools heated in the past that release stored energy of radioactive decay as light upon reheating is thermoluminiscence.

  29. Question • You want to cross-check a site in Africa that has been dated by K/Ar. You have found a fossilized pig skeleton. Which dating technique can be used to help date this site? • fluorine dating • biostratigraphy • dendrochronology • paleomagnetism

  30. Answer: b • You want to cross-check a site in Africa that has been dated by K/Ar. You have found a fossilized pig skeleton. The biostratigraphy dating technique can be used to help date this site.

  31. Principle of Superposition • In a stratigraphic sequence, the lower layers were deposited before the upper layers.

  32. Half-life • The time period in which one half the amount of a radioactive isotope is converted chemically (into a daughter product). • For example, after 1.25 billion years, half the 40K remains; after 2.5 billion years, one-fourth remains.

  33. Excavations in Progress at Olduvai • This site, more than 1 million years old, was located when a hominid ulna (arm bone) was found eroding out of the side of the gorge.

  34. Data From Oluvai Grouped into categories: • “Butchering” localities, areas containing one or a few individuals of a species of large mammal associated with a scatter of archaeological traces. • Quarry localities where early hominids extracted stone to make tools. • Multipurpose localities, areas where hominids ate, slept, and put the finishing touches on their tools.

  35. Remains at Olduvai • A dense scatter of stone and some fossilized animal bone from a site at Olduvai, dated at approximately 1.6 mya. • Some of these remains are the result of hominid activities.

  36. Stone Tool (Lithic) Technology • When struck properly, certain types of stone will fracture in a controlled way; these nodules are called blanks. • The smaller piece that comes off is called a flake, while the larger remaining chunk is called a core. • Both core and flake have sharp edges useful for cutting, sawing, or scraping. • The earliest hominid cultural inventions probably used materials that didn’t survive.

  37. Flake and Core

  38. Direct Percussion

  39. Pressure Flaking

  40. Microwear • The polish left on an experimental flint implement after scraping wood for 10 minutes. • Bright, smooth areas are the microwear polish; dark, grainy areas are the unworn flint surface. • Arrows indicate implement edge.

  41. Environmental Determinism • An interpretation that links simple environmental changes directly to a major evolutionary shift in an organism. • Such explanations tend to oversimplify the evolutionary process.

  42. Stable Carbon Isotopes • Isotopes of carbon that are produced in plants in differing proportions, depending on environmental conditions. • By analyzing the proportions of the isotopes contained in fossil remains of animals (who ate the plants), it’s possible to reconstruct aspects of ancient environments.

  43. Factors Influencing the Initial Evolution of Bipedal Locomotion

  44. Factors Influencing the Initial Evolution of Bipedal Locomotion

  45. Factors Influencing the Initial Evolution of Bipedal Locomotion

  46. Factors Influencing the Initial Evolution of Bipedal Locomotion

  47. The Bipedal Adaptation • Efficient bipedalism as the primary form of locomotion is seen only in hominids. • Advantages of bipedalism: • Freed the hands for carrying objects and for making and using tools. • In the bipedal stance, animals have a wider view of the surrounding countryside. • Bipedal walking is an efficient means of covering long distances.

  48. Obligate Bipedalism • Bipedalism as the only form of hominid terrestrial locomotion. • Since major anatomical changes in the spine, pelvis, and lower limb are required for bipedal locomotion, once hominids adapted this mode of locomotion, other forms of locomotion on the ground became impossible.

  49. Major Features of Hominid Bipedalism • The foramen magnum (shown in red) is repositioned farther underneath the skull, so that the head is more or less balanced on the spine (and thus requires less robust neck muscles to hold the head upright).

  50. Major Features of Hominid Bipedalism • The spine has two distinctive curves—a backward (thoracic) one and a forward (lumbar) one—that keep the trunk (and weight) centered above the pelvis.

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