New U-series dates on the Petralona cranium, a key fossil in European human evolution.

Assigning an age to the nearly complete cranium found in the Petralona Cave in Greece is of outstanding importance because this fossil has a key position in European human evolution. This topic has been debated since its discovery more than 60 years ago, highlighting the difficulties in applying physical dating methods to prehistoric samples. Previous results obtained on various types of samples yielded a large age range between about 170 and 700 ka, precluding any consensus on the age of the human fossil.

Dentition of the Mugharet El'Aliya Fossil Human Maxilla, Morocco.

Objective: This study follows up on our recent morphological analysis of the juvenile maxilla from Mugharet el'Aliya, Morocco. Although this specimen shows a reportedly archaic morphology, likely due to its large size, 3D shape analyses indicated affinities with early Homo sapiens. Here, we conducted an in-depth comparative investigation of the associated dentition to further clarify this individual's phylogenetic and taxonomic affinities.

Human evolution: The lonely Neanderthal?

A recently excavated Neanderthal skeleton from southern France has yielded DNA from a distinct lineage, different from other late Neanderthals. This suggests Neanderthals expanded and diversified about 120,000 years ago, and some of that diversity persisted in Europe until near the time of their extinction.

Bioclimatic and masticatory influences on human cranial diversity verified by analysis of 3D morphometric homologous models.

This study analyzes the effects of bioclimate and masticatory factors on the regional variability of human cranial forms across 150 ethnic groups worldwide. Morphometric variables were generated using principal component analysis applied to 3D homologous models. Relationships between cranial form and bioclimate (temperature and precipitation) and masticatory factors (infratemporal space) were tested considering sampling bias due to past population movements during the late Pleistocene and/or early- to mid-Holocene.

Chris Stringer.

Interview with Chris Stringer, who studies human origins at the Natural History Museum of London.

Did our ancestors nearly die out?

Genetic analyses suggest an ancient human population crash 900,000 years ago.

Extreme glacial cooling likely led to hominin depopulation of Europe in the Early Pleistocene.

The oldest known hominin remains in Europe [~1.5 to ~1.1 million years ago (Ma)] have been recovered from Iberia, where paleoenvironmental reconstructions have indicated warm and wet interglacials and mild glacials, supporting the view that once established, hominin populations persisted continuously.

The development of ideas about a recent African origin for Homo sapiens.

In this contribution I will review the development of ideas about a recent African origin for our species over the last 50 years, starting from the time of my PhD in the early 1970s. I will examine the instructive and quite different interpretations placed on the 1979 discovery of a partial Neanderthal skeleton associated with a Châtelperronian industry at the rock shelter of St-Césaire in France, and then focus on the crucial years from 1987-1989, including the so-called 'Human Revolution' conference of 1987, and my 1988 Science paper with Peter Andrews: 'Genetic and Fossil Evidence for the Origin of Modern Humans'. Following the historical review, I will assess the status of five proposed models for the evolution of derived Homo sapiens: Recent African Origin (RAO); RAO and Hybridisation (RAOH); Assimilation (AM); Multiregional Evolution (MRE); and Braided Stream (BS).

Dual ancestries and ecologies of the Late Glacial Palaeolithic in Britain.

Genetic investigations of Upper Palaeolithic Europe have revealed a complex and transformative history of human population movements and ancestries, with evidence of several instances of genetic change across the European continent in the period following the Last Glacial Maximum (LGM). Concurrent with these genetic shifts, the post-LGM period is characterized by a series of significant climatic changes, population expansions and cultural diversification. Britain lies at the extreme northwest corner of post-LGM expansion and its earliest Late Glacial human occupation remains unclear.

Frontal sinuses and human evolution.

The frontal sinuses are cavities inside the frontal bone located at the junction between the face and the cranial vault and close to the brain. Despite a long history of study, understanding of their origin and variation through evolution is limited. This work compares most hominin species' holotypes and other key individuals with extant hominids.

Comparing the Boxgrove and Atapuerca (Sima de los Huesos) human fossils: Do they represent distinct paleodemes?

The early Middle Pleistocene human material from Boxgrove (West Sussex, UK) consists of a partial left tibia and two lower incisors from a separate adult individual. These remains derive from deposits assigned to the MIS 13 interglacial at about 480 ka and have been referred to as Homo cf. heidelbergensis.

Global patterns of the cranial form of modern human populations described by analysis of a 3D surface homologous model.

This study assessed the regional diversity of the human cranial form by using geometric homologous models based on scanned data from 148 ethnic groups worldwide. This method adopted a template-fitting technique for a nonrigid transformation via the iterative closest point algorithm to generate the homologous meshes. Through the application of principal component analysis to 342 sampled homologous models, the largest variation was detected in overall size, and small South Asian crania were clearly verified.

The naming of Homo bodoensis by Roksandic and colleagues does not resolve issues surrounding Middle Pleistocene human evolution.

Roksandic et al. (2022) proposed the new species name Homo bodoensis as a replacement name for Homo rhodesiensis Woodward, 1921, because they felt it was poorly and variably defined and was linked to sociopolitical baggage. However, the International Code of Zoological Nomenclature includes regulations on how and when such name changes are allowed, and Roksandic et al.

Modern human incursion into Neanderthal territories 54,000 years ago at Mandrin, France.

Determining the extent of overlap between modern humans and other hominins in Eurasia, such as Neanderthals and Denisovans, is fundamental to understanding the nature of their interactions and what led to the disappearance of archaic hominins. Apart from a possible sporadic pulse recorded in Greece during the Middle Pleistocene, the first settlements of modern humans in Europe have been constrained to ~45,000 to 43,000 years ago. Here, we report hominin fossils from Grotte Mandrin in France that reveal the earliest known presence of modern humans in Europe between 56,800 and 51,700 years ago.

Comment on "A global environmental crisis 42,000 years ago".

Cooper . (Research Articles, 19 February 2021, p. 811) propose that the Laschamps geomagnetic inversion ~42,000 years ago drove global climatic shifts, causing major behavioral changes within prehistoric groups, as well as events of human and megafaunal extinction.

Geochemical provenancing and direct dating of the Harbin archaic human cranium.

As one of the most complete archaic human fossils, the Harbin cranium provides critical evidence for studying the diversification of the genus and the origin of . However, the unsystematic recovery of this cranium and a long and confused history since the discovery impede its accurate dating. Here, we carried out a series of geochemical analyses, including non-destructive X-ray fluorescence (XRF), rare earth elements (REE), and the Sr isotopes, to test the reported provenance of the Harbin cranium and get better stratigraphic constraints.

Massive cranium from Harbin in northeastern China establishes a new Middle Pleistocene human lineage.

It has recently become clear that several human lineages coexisted with during the late Middle and Late Pleistocene. Here, we report an archaic human fossil that throws new light on debates concerning the diversification of the genus and the origin of . The fossil was recovered in Harbin city in northeastern China, with a minimum uranium-series age of 146 ka.

Widespread Denisovan ancestry in Island Southeast Asia but no evidence of substantial super-archaic hominin admixture.

The hominin fossil record of Island Southeast Asia (ISEA) indicates that at least two endemic 'super-archaic' species-Homo luzonensis and H. floresiensis-were present around the time anatomically modern humans arrived in the region >50,000 years ago. Intriguingly, contemporary human populations across ISEA carry distinct genomic traces of ancient interbreeding events with Denisovans-a separate hominin lineage that currently lacks a fossil record in ISEA.

Nubian Levallois technology associated with southernmost Neanderthals.

Neanderthals occurred widely across north Eurasian landscapes, but between ~ 70 and 50 thousand years ago (ka) they expanded southwards into the Levant, which had previously been inhabited by Homo sapiens. Palaeoanthropological research in the first half of the twentieth century demonstrated alternate occupations of the Levant by Neanderthal and Homo sapiens populations, yet key early findings have largely been overlooked in later studies. Here, we present the results of new examinations of both the fossil and archaeological collections from Shukbah Cave, located in the Palestinian West Bank, presenting new quantitative analyses of a hominin lower first molar and associated stone tool assemblage.

Origins of modern human ancestry.

New finds in the palaeoanthropological and genomic records have changed our view of the origins of modern human ancestry. Here we review our current understanding of how the ancestry of modern humans around the globe can be traced into the deep past, and which ancestors it passes through during our journey back in time. We identify three key phases that are surrounded by major questions, and which will be at the frontiers of future research.

The morphology of the Late Pleistocene hominin remains from the site of La Cotte de St Brelade, Jersey (Channel Islands).

Thirteen permanent fully erupted teeth were excavated at the Paleolithic site of La Cotte de St Brelade in Jersey in 1910 and 1911. These were all found in the same location, on a ledge behind a hearth in a Mousterian occupation level. They were originally identified as being Neanderthal.

The morphological affinity of the Early Pleistocene footprints from Happisburgh, England, with other footprints of Pliocene, Pleistocene, and Holocene age.

Fossil hominin footprints provide a direct source of evidence of locomotor behavior and allow inference of other biological data such as anthropometrics. Many recent comparative analyses of hominin footprints have used 3D analytical methods to assess their morphological affinities, comparing tracks from different locations and/or time periods. However, environmental conditions can sometimes preclude 3D digital capture, as was the case at Happisburgh (England) in 2013.