Intro to Paleoanthropology

🦕Intro to Paleoanthropology Unit 3 – Miocene Hominoids: Origins of Bipedalism

The Miocene epoch, spanning 23 to 5 million years ago, was crucial for understanding bipedalism in hominoids. This period saw significant climate changes, tectonic events, and the expansion of grasslands, creating new ecological niches for early apes and humans. Key fossil discoveries from this era, including Proconsul, Oreopithecus, and Ardipithecus, provide insights into the anatomical changes leading to bipedalism. These findings have sparked debates about the timing, causes, and evolutionary trajectory of this defining human characteristic.

Key Concepts and Terminology

  • Miocene a geological epoch spanning from ~23 to 5 million years ago, crucial period for understanding the origins of bipedalism in hominoids
  • Hominoids a taxonomic group including apes and humans, characterized by lack of tail, upright posture, and larger brains compared to other primates
  • Bipedalism habitual locomotion on two legs, a defining characteristic of the human lineage
  • Proconsul an early Miocene hominoid genus, considered a stem hominoid and potential ancestor to later apes and humans
  • Oreopithecus a late Miocene hominoid from Italy, exhibiting some bipedal adaptations but with debated phylogenetic position
  • Ardipithecus early hominin genus from the late Miocene and early Pliocene, showing a mosaic of bipedal and arboreal adaptations
  • Orthogrady upright posture and locomotion, as opposed to the more horizontal orientation of quadrupedal primates
  • Positional behavior the ways in which an animal moves and orients its body in its environment, including locomotion and posture

Geological Context of the Miocene

  • Miocene epoch part of the Neogene period, following the Oligocene and preceding the Pliocene
  • Began with the Miocene Climate Optimum a warm and humid period with higher sea levels and expanded tropical forests
  • Marked by tectonic events the uplift of the Tibetan Plateau, the Andes, and the East African Rift Valley, altering global climate patterns
  • Grasslands expanded particularly in the late Miocene, replacing forests in many areas and creating new ecological niches
  • Fossil sites spanning the Miocene found in Africa (East Africa and Chad), Europe (Germany, France, Italy, Spain), and Asia (Pakistan, India, China)
  • Volcanic activity in East Africa led to the preservation of numerous hominoid fossils in ash layers
  • Sahara Desert did not exist for most of the Miocene, allowing for a more continuous biogeographic distribution of fauna between Africa and Eurasia

Miocene Climate and Environment

  • Early Miocene characterized by the Miocene Climate Optimum, with global temperatures 3-4°C higher than present
  • Warm and humid conditions supported the expansion of tropical and subtropical forests
  • Middle Miocene saw a gradual cooling trend and increasing seasonality
  • Late Miocene marked by further cooling, aridification, and the expansion of grasslands and open woodlands
  • C4 grasses evolved and spread during the late Miocene, adapted to lower CO2 levels and more seasonal rainfall
  • Faunal turnover occurred in many regions, with the diversification of grazing mammals and the decline of forest-adapted species
  • East African Rift Valley began to form, creating a mosaic of habitats including forests, woodlands, and grasslands
  • Himalayan uplift intensified the Asian monsoon system, leading to increased seasonality and the development of the Sahara Desert in the late Miocene

Major Miocene Hominoid Fossils

  • Proconsul early Miocene genus from East Africa (Kenya, Uganda), with multiple species showing a mix of primitive and derived hominoid features
  • Afropithecus early Miocene genus from Kenya, with a more robust build and some dental similarities to later hominids
  • Kenyapithecus middle Miocene genus from Kenya, showing some dental and postcranial adaptations towards a more terrestrial lifestyle
  • Dryopithecus widespread middle to late Miocene genus from Europe and Asia, with a mix of primitive and derived hominoid features
  • Oreopithecus late Miocene genus from Italy, with unique adaptations suggesting a semi-terrestrial and possibly bipedal locomotion
  • Sivapithecus late Miocene genus from South Asia, closely related to orangutans and showing adaptations for a more terrestrial lifestyle
  • Ardipithecus late Miocene to early Pliocene genus from Ethiopia, with a mosaic of bipedal and arboreal adaptations, considered an early hominin

Anatomical Changes Towards Bipedalism

  • Foramen magnum the opening at the base of the skull for the spinal cord, shifted to a more anterior position in bipeds
  • Lumbar lordosis the inward curvature of the lower spine, more pronounced in bipeds to support upright posture
  • Shorter and broader iliac blades of the pelvis, providing attachment for gluteal muscles and stabilizing the trunk during bipedal locomotion
  • Larger acetabulum the socket of the hip joint, accommodating the increased load bearing during bipedal locomotion
  • Valgus knee the inward angle of the knee joint, aligning the lower leg with the body's center of mass in bipeds
  • Longer and more robust lower limbs relative to upper limbs, a characteristic of bipedal hominins
  • Arched foot with a non-opposable big toe, providing a stable platform for push-off during bipedal walking
  • Reduced curvature of the phalanges (finger and toe bones), indicating less time spent grasping branches and more time on the ground

Theories on the Origins of Bipedalism

  • Savannah hypothesis proposes that bipedalism evolved as an adaptation to more open, grassland environments for improved visibility and efficient travel
  • Postural feeding hypothesis suggests that bipedalism originated to facilitate foraging from low branches and bushes while freeing the hands
  • Provisioning hypothesis argues that bipedalism allowed for more efficient carrying of food and other resources to provision offspring and mates
  • Thermoregulatory hypothesis posits that upright posture and bipedal locomotion helped early hominins regulate body temperature in hot, open environments
  • Threat display hypothesis proposes that bipedal posture evolved as a means of intimidation and display in male-male competition
  • Endurance running hypothesis suggests that bipedalism, combined with other adaptations, allowed early hominins to engage in persistence hunting
  • Wading hypothesis argues that bipedalism may have originated in coastal or wetland environments, with water providing support for upright posture

Comparative Analysis with Modern Primates

  • African apes (chimpanzees, bonobos, gorillas) are the closest living relatives of humans, sharing a common ancestor around 5-7 million years ago
  • Chimpanzees and bonobos exhibit occasional bipedalism, particularly in the context of carrying objects or threat displays
  • Gorillas have a more upright posture compared to chimpanzees and bonobos, but still primarily use quadrupedal knuckle-walking locomotion
  • Orangutans are more arboreal than African apes, using a form of quadrumanous climbing and suspension, but also exhibit occasional bipedalism on branches
  • Gibbons and siamangs are highly specialized for brachiation (arm-swinging), but also engage in bipedal walking along branches
  • Baboons and other terrestrial monkeys provide insights into the biomechanics and energy costs of quadrupedal locomotion on the ground
  • Bipedal locomotion is rare among non-human primates, highlighting the unique evolutionary trajectory of the human lineage

Debates and Controversies

  • Exact timing of the origin of bipedalism, with some researchers proposing a gradual transition starting in the Miocene, while others argue for a more punctuated event in the Pliocene
  • Relative importance of different selective pressures (environmental, social, dietary) in driving the evolution of bipedalism
  • Degree of arboreality and bipedalism in different Miocene hominoids, particularly in genera such as Oreopithecus and Ardipithecus
  • Phylogenetic relationships among Miocene hominoids and their connections to later hominins, with ongoing debates about the position of various genera
  • Role of climate change and tectonic events in shaping the evolution of Miocene hominoids and the origins of bipedalism
  • Interpretation of fragmentary fossil evidence and the limitations of inferring locomotor behavior from isolated anatomical features
  • Integration of new methodologies, such as 3D morphometrics and biomechanical modeling, to better understand the functional implications of Miocene hominoid morphology


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© 2024 Fiveable Inc. All rights reserved.
AP® and SAT® are trademarks registered by the College Board, which is not affiliated with, and does not endorse this website.