Footprint evidence of early hominin locomotor diversity at Laetoli, Tanzania.

Bipedal trackways discovered in 1978 at Laetoli site G, Tanzania and dated to 3.66 million years ago are widely accepted as the oldest unequivocal evidence of obligate bipedalism in the human lineage1-3. Another trackway discovered two years earlier at nearby site A was partially excavated and attributed to a hominin, but curious affinities with bears (ursids) marginalized its importance to the paleoanthropological community, and the location of these footprints fell into obscurity3-5. In 2019, we located, excavated and cleaned the site A trackway, producing a digital archive using 3D photogrammetry and laser scanning. Here we compare the footprints at this site with those of American black bears, chimpanzees and humans, and we show that they resemble those of hominins more than ursids. In fact, the narrow step width corroborates the original interpretation of a small, cross-stepping bipedal hominin. However, the inferred foot proportions, gait parameters and 3D morphologies of footprints at site A are readily distinguished from those at site G, indicating that a minimum of two hominin taxa with different feet and gaits coexisted at Laetoli.

Examining biological continuity across the late holocene occupation of the Aleutian Islands using cranial morphometrics and quantitative genetic permutation.

OBJECTIVES: The number of distinct human migrations into the Aleutian Islands during the Holocene has been a recurrent debate in the anthropological literature. Stemming from Hrdlicka's sorting of the prehistoric remains into two distinct populations based on archaeological context and cranial measurements, the human occupation of the Aleutian Islands has long been thought to be the consequence of two distinct human migrations, a Paleo-Aleut migration that provided the initial settlement of the islands, and a Neo-Aleut migration that replaced the original settlers around 1000 BP. This study examines the relationship of the Aleut cranial assemblages in the context of greater Alaskan population variability to assess the evidence for a substantial migration into the Aleutian Islands during the late Holocene. MATERIALS AND METHODS: A battery of 29 cranial measurements that quantify global cranial shape were analyzed using Euclidean morphometric methods and quantitative genetic permutation methods to examine the plausibility for two distinct Aleut occupations ("Paleo-Aleut" and "Neo-Aleut"), the latter of which is held to share closer phenetic affinities to mainland Alaskan populations than the former. The Aleut skeletal assemblages were arranged according to temporal association, geographic location, and cranial typology, and analyzed within a comparative framework of mainland Alaskan samples using principal coordinates, biological distance and random skewers permutation methods. RESULTS: Regardless of how the Aleut assemblages are divided, they show greater similarity to each other than to any of the mainland Alaskan assemblages. These findings are consistent across the methodological approaches. DISCUSSION: The results obtained in this study provide no support for a cranial morphology-based subdivision of the Aleuts into two distinct samples, Hence, there is no evidence for a substantial population migration of so-called Neo-Aleuts, nor for a population replacement event of an extant Paleo-Aleut population by a mainland-affiliated Neo-Aleuts population at or after 1000 BP.

Persistent Early to Middle Holocene tropical foraging in southwestern Amazonia.

The Amazon witnessed the emergence of complex societies after 2500 years ago that altered tropical landscapes through intensive agriculture and managed aquatic systems. However, very little is known about the context and conditions that preceded these social and environmental transformations. Here, we demonstrate that forest islands in the Llanos de Moxos of southwestern Amazonia contain human burials and represent the earliest settlements in the region between 10,600 and 4000 years ago. These archaeological sites and their contents represent the earliest evidence of communities that experienced conditions conducive to engaging with food production such as environmental stability, resource disturbance, and increased territoriality in the Amazonian tropical lowlands.

Brief communication: paleopathology of the Kiik-Koba 1 Neandertal.

The Kiik-Koba 1 Neandertal partial skeleton (canine, partial hands, partial leg, and feet), of a approximately 40-year-old probable male, exhibits a suite of pathological lesions, including hypercementosis, minor fibrous ossifications, pedal phalangeal fracture, and pronounced enthesopathies on the patella and calcanei in the context of no articular degenerations. The first two sets of lesions are related to age in the context of advanced dental attrition and physical strains. The third lesion joins a series of healed minor traumatic lesions among the Neandertals. The last represents either pronounced tendinous inflammation, albeit in the context of no articular degenerations, or a case of diffuse idiopathic skeletal hyperostosis (DISH) in the Late Pleistocene. Kiik-Koba 1 therefore adds to the high incidence of pathological lesions among the Neandertals and, if a diagnosis of DISH is correct, to a high frequency of this disorder among older Neandertals.

Neanderthal reconstructed.

A century and a half of controversy concerning the differences between Neanderthals (or Neandertals) and modern humans has left us with many questions and no sign of abatement. One of these remaining questions concerns the articulated structure of the Neanderthal skeleton and how it compares to that of a modern human. Although this question has been tackled many times by more artistic avenues, never has a complete, fully articulated Neanderthal skeleton been constructed systematically using castings from real Neanderthal bones. In an attempt to provide a more objective understanding of Neanderthal stature and biomechanics, a complete Neanderthal skeleton was reconstructed and articulated. This reconstruction was primarily based on the La Ferrassie 1 specimen, with missing or incomplete elements filled in from other Neanderthal cast collections.