Early Archaeological Sites Research Articles

Machine learning-based identification of geomorphological units in Quintero Bay (32°S) and its implications for the search for early drowned archaeological sites on the western coast of South America

High-resolution predictive modeling of submerged landscapes has successfully allowed the detection of early archaeological sites that are presently underwater. These models have traditionally relied on geophysical techniques, which can be both time-consuming and expensive, especially for extensive survey areas. In contrast, geomorphological mapping using Machine Learning (ML) techniques has emerged as a rapid and accessible alternative with numerous advantages over conventional methods. In this work, we employ ML algorithms (Random Forest, Support Vector Machine, Partial Least Squares, and Principal Component Analysis) trained on land to analyze the seabed of Quintero Bay to identify relic landforms that characterize the paleolandscape within which the submerged early site GNLQ1 formed. The methodology also included a multicriteria analysis that integrated geological (geomorphological, tectonic, eustatic) and archaeological (attributes of non-submerged records in the region) approaches to delineate potential areas of archaeological interest. The findings of this work can guide and enhance future archaeological research. The results underscore the importance of possessing a comprehensive understanding of the study area and its associated variables to the successful application of ML techniques. This also applies to modeling drowned paleolandscapes. Nevertheless, despite these challenges, ML-based modeling of drowned paleolandscapes can provide an overview of the distribution of geoforms comprising the paleolandscape, which in turn can help identify future geophysical survey areas to focus on in the search for archaeological evidence, thereby improving our understanding of the relationship between early human groups and these landscapes.

A female woolly mammoth's lifetime movements end in an ancient Alaskan hunter-gatherer camp.

Woolly mammoths in mainland Alaska overlapped with the region's first people for at least a millennium. However, it is unclear how mammoths used the space shared with people. Here, we use detailed isotopic analyses of a female mammoth tusk found in a 14,000-year-old archaeological site to show that she moved ~1000 kilometers from northwestern Canada to inhabit an area with the highest density of early archaeological sites in interior Alaska until her death. DNA from the tusk and other local contemporaneous archaeological mammoth remains revealed that multiple mammoth herds congregated in this region. Early Alaskans seem to have structured their settlements partly based on mammoth prevalence and made use of mammoths for raw materials and likely food.

Fire as high-elevation cold adaptation: An evaluation of fuels and Terminal Pleistocene combustion in the Central Andes

The use of fire constitutes an essential cultural adaptation to cold, and archaeological evidence for fire can be expected in high-latitude and high-elevation regions successfully inhabited by modern humans. At Cuncaicha rockshelter (4480 m above sea level, or masl) in the southern Peruvian Andes, evidence for fire is present from the earliest occupation, dating to the Terminal Pleistocene (∼12,500–11,200 cal BP). Yet, the site contains relatively few identifiable carbonized macrobotanical remains useful for identifying plants employed as combustible fuel. Based on a comprehensive review of nearly 40 early Andean archaeological sites above 2500 masl, little is known about fuels used for combustion. To understand fuel selection strategies at Cuncaicha, we conducted a combustion field experiment, evaluating the three highland plant taxa most likely to have been used as combustible fuels: Polylepis rugulosa (queñua) tree branches, Parastrephia spp. (tola) woody shrubs, and Azorella compacta (yareta) cushion plants. Temperature measurements informed on the combustion characteristics and efficiency of each fuel. We then compared the experimentally-produced fire residues to the geoarchaeological evidence from Cuncaicha. The resinous cushion plant yareta, endemic to the high Andes, may have been the primary fuel used at Cuncaicha based on the experiment outcome and the geoarchaeological evidence. Due to its high-temperature and complete combustion, yareta leaves little to no macrobotanical evidence, thus its identification at other Andean sites may require a multi-methodological approach. Because the geographic range of this plant corresponds with most early archaeological sites in the high Andes, yareta may have been a key resource enabling early settlement throughout the region.

Holocene capuchin-monkey stone tool deposits shed doubts on the human origin of archeological sites from the Pleistocene of Brazil

New World capuchin monkeys are well-known by their ability to solve problems using stone tools that have the characteristics and morphology of some human-made stone tools. The aim of the present contribution is to carry out brief comparisons between the Pleistocene archeological sites from Brazil (e.g. Pedra Furada, Sitio do Meio, Vale da Pedra Furada, Toca da Tira Peia) and capuchin-made stone tool deposits. Pleistocene sites from Brazil are characterized by the exclusive use of immediately available raw material, the predominance of unifacial flaking, and abundance of cortical flakes, together with the absence of blades and bifacial thinning techniques. In all these aspects, the sites resemble capuchin-made lithic deposits and lack a number of human attributes. In sum, based on positive and negative evidence we are confident that the early archeological sites from Brazil may not be human-derived but may belong to capuchin monkeys.

Pre-Columbian cultivation of vegetatively propagated and fruit tree tropical crops in the Atacama Desert

South America is a megadiverse continent that witnessed the domestication, translocation and cultivation of various plant species from seemingly contrasting ecosystems. It was the recipient and supplier of crops brought to and from Mesoamerica (such as maize and cacao, respectively), and Polynesia to where the key staple crop sweet potato was exported. Not every instance of thetrans-ecological expansion of cultivated plants (both domesticated and wild), however, resulted in successful farming. Here, we review the transregional circulation and introduction of five food tropical crops originated in the tropical and humid valleys of the eastern Andes—achira, cassava,ahipa, sweet potato, and pacay—to the hyper-arid coastal valleys of the Atacama Desert of northern Chile, where they have been found in early archeological sites. By means of an evaluation of the contexts of their deposition and supported by direct radiocarbon dating, stable isotopes analyses, and starch grain analysis, we evaluate different hypotheses for explaining their introduction and adaptation to the hyper-arid soils of northern Chile, by societal groups that after the introduction of cultigens still retained a strong dependence on marine hunting, gathering and fishing ways of life based on wide variety of marine coast resources. Many of the studied plants were part of a broader package of introduced goods and technological devices and procedures, linked to food, therapeutic medicine, social and ritual purposes that transformed previous hunter-gatherer social, economic, and ideological institutions. Based on archeological data, we discuss some of the possible socio-ecological processes involved in the development of agricultural landscapes including the adoption of tropical crops originated several hundred kilometers away from the Atacama Desert during the Late Holocene.

Spatial and Temporal Evolution and Human–Land Relationship at Early Historic Sites in the Middle Reaches of the Yellow River in the Sanhe Region Based on GIS Technology

The Sanhe region in the middle reaches of the Yellow River is an important area for the origin and development of early civilization in China. Many early sites, from the Paleolithic to the Xia, Shang and Zhou Dynasties, remain in the region, all of which are important material carriers to record the historical process from the emergence of human beings to the formation of early civilization. In this study, all of the early archaeological sites in the research area were collected and loaded into the GIS platform. With the help of kernel density estimation, adjacent index analysis, standard deviation ellipse and other tools, the spatial and temporal distribution characteristics of these sites were explored, and the correlation between the distribution of early sites and geographical factors was explored through coupling analysis with the geographical environment. The results show that: (1) the evolution of the spatial distribution characteristics of early sites in the time dimension can reflect the development process of early civilization; (2) elevation, slope, aspect, topographic relief, hydrology and other factors are closely related to the distribution characteristics of early sites in the Sanhe region, and the correlation between site distribution and geographical factors is also different in different periods; (3) under the combined effects of elevation, slope, aspect, topographic relief and hydrological factors, the early sites show the existing spatial–temporal distribution characteristics. It is hoped that this study can provide reference ideas for the origin and development of early civilization in the future, as well as the discovery, protection and utilization of early sites.

The Volcanic Landscapes of the Ancient Hunter-Gatherers of the Atacama Desert Through Their Lithic Remains

Since ancient times Andean societies have formed an intimate relationship with volcanoes, the beginnings of which can be traced right back to the initial peopling of the region. By studying rocks used for stone tools and other everyday artifacts, we explore the volcanic landscapes of early hunter-gatherer groups (11,500–9,500 cal BP) of the highlands of the Atacama Desert (22–24°S/67–68°W). Petrological classification of the lithic assemblages of three Early Holocene archaeological sites showed the procurement of a great diversity of volcanic and subvolcanic rocks, including pumice, granitic rocks, micro-diorites, a large variety of tuffs and andesites, dacites, cherts, basalts, obsidians, among others. Field surveys enabled us to detect many of their sources related to volcanic features such as craters, maars, caldera-domes, lava flows, probable hydrothermal deposits, and ignimbrites. In these places, we also document large quarry-workshops and campsites from different periods, indicating intense and repeated human occupation over time. By comparing the artifacts with geological samples collected in the field, it was possible to assign the source of origin of a large part of the archaeological assemblages. Our data suggest that the volcanic features of the Atacama highlands were integrated into the mobility and interaction networks of ancient hunter-gatherer groups at an early date.

Slowstands, stillstands and transgressions: Paleoshorelines and archaeology on Quadra Island, BC, Canada

On Quadra Island, west coast Canada, a series of marine terraces formed during a period of rapid marine regression from 200 m to 1 m above modern levels between ca. 14,500 and 12,000 years ago. Within this period of regional marine regression, evidence points to brief periods of sea level stillstand and even marine transgressions. It is hypothesized that during these anomalous periods, global meltwater events created a local signature on the Quadra Island sea level curve by slowing, halting and/or inversing the regional sea level regression trend. This is revealed through identification of high elevation paleoshorelines, landscape terracing and other stranded marine features from LiDAR Digital Elevation Models (DEMs) and subsurface investigation. These paleomarine terraces are believed to have developed during brief marine stillstands, slowstands and minor marine transgressions. Pauses or slowing periods of regression appear to result from global eustatic rise briefly matching or exceeding local isostatic and tectonic uplift. The ages of these terraces, based on local sea level history and radiocarbon dating of some of the raised marine features, match well to the ages of coral-based marine terraces sequences associated with periods of rapid global sea level rise. A number of early post glacial to earliest Holocene archaeological sites are associated with the Quadra marine terraces. These associations suggest an improved approach to location of early archaeological sites dating to times of rapid sea level change.

The Effect of Raw Material on the Identification of Knapping Skill: a Case Study from Olduvai Gorge, Tanzania

The identification of Oldowan hominin knapping skill levels has been a focus of numerous studies, with apparent variation in technical abilities identified between a number of Early Stone Age archaeological sites. Raw material variability, however, can play a significant role in the outcomes of knapping events as well as in the accuracy of analysis. Implications of such variability are yet to be fully understood. Here we present an experimental study to assess the effects that varying raw materials have on the identification of technological attributes typically associated with varying skill levels and whether it is possible to identify knapper skill levels across multiple raw materials. Variation was tested between raw materials from Olduvai Gorge across and between skill levels. The results suggest that knapping skill levels manifest differently in the material record across raw materials. In addition, we suggest that raw material has a significant effect on identifying knapper skill variation. This has implications for future research concerned with identifying knapper skill within and between early assemblages of differing raw materials.

Ancient mitochondrial DNA connects house mice in the British Isles to trade across Europe over three millennia

BackgroundThe earliest records in Britain for the western European house mouse (Mus musculus domesticus) date from the Late Bronze Age. The arrival of this commensal species in Britain is thought to be related to human transport and trade with continental Europe. In order to study this arrival, we collected a total of 16 ancient mouse mandibulae from four early British archaeological sites, ranging from the Late Bronze Age to the Roman period.ResultsFrom these, we obtained ancient mitochondrial DNA (mtDNA) house mouse sequences from eight house mice from two of the sites dating from the Late Bronze to Middle Iron Age. We also obtained five ancient mtDNA wood mouse (Apodemus spp.) sequences from all four sites. The ancient house mouse sequences found in this study were from haplogroups E (N = 6) and D (N = 2). Modern British house mouse mtDNA sequences are primarily characterised by haplogroups E and F and, much less commonly, haplogroup D.ConclusionsThe presence of haplogroups D and E in our samples and the dating of the archaeological sites provide evidence of an early house mouse colonisation that may relate to Late Bronze Age/Iron Age trade and/or human expansion. Our results confirm the hypothesis, based on zooarchaeological evidence and modern mtDNA predictions, that house mice, with haplogroups D and E, were established in Britain by the Iron Age and, in the case of haplogroup E, possibly as early as the Late Bronze Age.

Archaeological evidences on early peopling in the fluvio-volcanic Pereira-Armenia fan (Colombia): Volcanic activity influence on cultural adaptation and depopulation events

Archaeological research in the Middle Cauca region of west-central Colombia over the past 20 years has produced new information regarding early preceramic archaeology and environmental changes in the Central Cordillera landscapes. Stratigraphic, sedimentological, and geomorphic studies provided important contextual information for locating and interpreting the region's earliest archaeological sites, from a geoarchaeological perspective. This article presents results on the Pereira-Armenia Fluvio-Volcanic Fan studies and surrounding areas, during the Late Pleistocene through Middle Holocene periods. Twenty-five archaeological sites with preceramic deposits were tested and some have been excavated in a region measuring 30 b y 100 km. The region contains data with occupations ranging dates from approximately 13,540 to 3600 14C years BP (Aceituno, 2019; Dickau, 2015). These sites included cultural and natural deposits, within in situ tephras and polygenic soils with buried soil sequences. Cultural materials, sediments and soils from these sites have the potential to yield important data about the processes of site formation, environmental adaptation, early subsistence, depopulation and lithic technology in the Middle Cauca region. Layers of volcanic ashes demonstrated that in areas proximal to the Cerro Bravo-Cerro Machín Volcanic Complex, humans suffered impacts. However, depopulations was not generalized. In some places in the Fluvio-Volcanic Fan, far enough form volcanic impacts, people could stay.

Late Pleistocene marine resources from the Bering Glacier Foreland and human coastal migration in the northern Gulf of Alaska region

AbstractRecent research on the Bering Glacier forelands in the northern Gulf of Alaska provides new insights into late Pleistocene/early Holocene shorelines, providing a favorable route for human migration as early as ~16,000 cal yr BP. This route included an irregular coastline with embayments and islands offering protection from the open ocean; edible marine invertebrates dating from 15,000 to 5,500 cal yr BP; and marine vertebrates dating as early as 16,000 cal yr BP. The latter included walrus (Odobenus rosmarus), bearded seal (Erignathus barbatus), and ringed seal (Phoca cf. hispida), all associated with pack ice conditions unlike those present today. While this ecosystem could have supported humans migrating along the coastline, and coastal refugia may have existed elsewhere in the region, coastal archaeological sites in the northern Gulf of Alaska and southwest Alaska are no older than ~9,500 cal yr BP. This suggests that the earliest sites have been eroded or destroyed, that the earliest migrants ignored available marine resources, and/or that these migrants did not use a coastal route. In contrast, the earliest archaeological sites in southeast Alaska date to ~12,500 cal yr BP, suggesting migration from interior Alaska to the coast somewhere east of the Copper River delta.

Locating the Lost Gupta Period Ramayana Reliefs from Katingara, Uttar Pradesh

This article collates a fascinating group of early fifth-century ce terracotta temple reliefs, some bearing short Brahmi inscriptions. The panels entered numerous museum and private collections in India and abroad from the 1960s and early 70s. Of the panels, which comprise animated narrative scenes, amorous couples, lesser-divinities and composite creatures, it is those depicting episodes of the Sanskrit epic Ramayana that this article is specifically concerned with. Although the images share a bold, idiosyncratic style, and a likeness in scale, material and finish, they have never been acknowledged as having a shared origin, with most being loosely described as hailing from Uttar Pradesh. The central aims of this article are to analyse the iconography of this remarkable collection of panels and to put forward an argument for their place of origin being a small archaeological site near the village of Katingara, located in the alluvial plains beside the Kali Nadi river (a tributary of the Ganges) in District Etah, Uttar Pradesh. Katingara will also be positioned within the context of recorded early archaeological sites in the region. Importantly, the panels constitute one of the earliest and most extensive collections of terracotta Ramayana images surviving from the Gupta period, and this is the first time since their illicit removal from Katingara that they have been 're-assembled'.

Collagen Fingerprinting and the Earliest Marine Mammal Hunting in North America

The submersion of Late Pleistocene shorelines and poor organic preservation at many early archaeological sites obscure the earliest effects of humans on coastal resources in the Americas. We used collagen fingerprinting to identify bone fragments from middens at four California Channel Island sites that are among the oldest coastal sites in the Americas (~12,500-8,500 cal BP). We document Paleocoastal human predation of at least three marine mammal families/species, including northern elephant seals (Mirounga angustirostris), eared seals (Otariidae), and sea otters (Enhydra lutris). Otariids and elephant seals are abundant today along the Pacific Coast of North America, but elephant seals are rare in late Holocene (<1500 cal BP) archaeological sites. Our data support the hypotheses that: (1) marine mammals helped fuel the peopling of the Americas; (2) humans affected marine mammal biogeography millennia before the devastation caused by the historic fur and oil trade; and (3) the current abundance and distribution of recovering pinniped populations on the California Channel Islands may mirror a pre-human baseline.

Ancient DNA evidence for the introduction and dispersal of dogs in New Zealand

When people first arrived in New Zealand around 700 years ago, they brought their dogs (Canis familiaris) with them. To investigate the introduction and dispersal of dogs across the country we generated twenty-three new complete, or nearly complete, mitogenomes from ancient DNA from dog teeth sampled from four early archaeological sites in New Zealand and from one archaeological site in the southern Cook Islands. When considered together with fourteen previously reported mitogenomes from the New Zealand colonisation era site of Wairau Bar these sequences reveal a striking lack of mitochondrial genetic diversity in early New Zealand dogs. Our analysis shows that a group of closely-related dogs were brought to New Zealand, probably from an East Polynesian source population, and that these dogs and their offspring were widely dispersed throughout the country during the colonisation process. This pattern is consistent with the current model of rapid colonisation of New Zealand undertaken by highly mobile groups of people.

Dental caries at Lapa do Santo, central-eastern Brazil: An Early Holocene archaeological site.

The origin and dispersion of the first Americans have been extensively investigated from morphological and genetic perspectives, but few studies have focused on their health and lifestyle. The archaeological site of Lapa do Santo, central-eastern Brazil, has exceptionally preserved Early Holocene human skeletons, providing 19 individuals with 327 permanent and 122 deciduous teeth dated to 9,250 to 7,500 years BP. In this study, we test whether the inhabitants of Lapa do Santo had high prevalence of dental caries as previous studies of Lagoa Santa collection have indicated, using individual and tooth as units of analyses. The results show a high prevalence of dental caries in the permanent dentition (5.50%, n=327 teeth; 69.23%, n=13 individuals) compared to other samples of hunter-gatherers worldwide. In addition, dental caries in deciduous teeth start occurring as early as 3 to 4 years old, suggesting an early start to caries. Compared with other samples from Lagoa Santa, Lapa do Santo shows statistically similar prevalence of overall caries but different caries location pattern. We believe that a subsistence adaptation to a tropical environment rich in sources of carbohydrates, such as fruits, is the best explanation for the overall caries prevalence.

Ancient tortoise hunting in the southwest Pacific.

We report the unprecedented Lapita exploitation and subsequent extinction of large megafauna tortoises (?Meiolania damelipi) on tropical islands during the late Holocene over a 281,000 km2 region of the southwest Pacific spanning from the Vanuatu archipelago to Viti Levu in Fiji. Zooarchaeological analyses have identified seven early archaeological sites with the remains of this distinctive hornless tortoise, unlike the Gondwanan horned meiolaniid radiation to the southwest. These large tortoise radiations in the Pacific may have contributed to the rapid dispersal of early mobile Neolithic hunters throughout southwest Melanesia and on to western Polynesia. Subsequent rapid extinctions of these terrestrial herbivorous megafauna are likely to have led to significant changes in ecosystems that help explain changes in current archaeological patterns from Post-Lapita contexts in the region.

Ethnoarchaeology and Plio-Pleistocene sites: Some lessons from the Hadza

Exploration and analyses of early archaeological sites and their faunal assemblages have grown increasingly sophisticated since the sites were first proposed to be home bases where ancestral hunters brought meat to share with their mates and offspring. Debates about that proposition motivated quantitative attention to hunting, scavenging, butchery and transport of big game among modern Hadza and the faunal assemblage characteristics and archaeological sites they create. Findings prompted a hypothesis about competitive scavenging that might explain the character and ecological context of the early sites, a hypothesis since strengthened by consensus among archaeologists working at Olduvai that the sites are not home bases. Hadza carcass procurement rates calibrate estimates for ancestral populations without similar technology, underscoring the likelihood that other food resources were especially important in human evolution.

Lions as Bone Accumulators? Paleontological and Ecological Implications of a Modern Bone Assemblage from Olduvai Gorge

Analytic models have been developed to reconstruct early hominin behaviour, especially their subsistence patterns, revealed mainly through taphonomic analyses of archaeofaunal assemblages. Taphonomic research is used to discern which agents (carnivores, humans or both) generate the bone assemblages recovered at archaeological sites. Taphonomic frameworks developed during the last decades show that the only large-sized carnivores in African biomes able to create bone assemblages are leopards and hyenas. A carnivore-made bone assemblage located in the short-grassland ecological unit of the Serengeti (within Olduvai Gorge) was studied. Taphonomic analyses of this assemblage including skeletal part representation, bone density, breakage patterns and anatomical distribution of tooth marks, along with an ecological approach to the prey selection made by large carnivores of the Serengeti, were carried out. The results show that this bone assemblage may be the first lion-accumulated assemblage documented, although other carnivores (namely spotted hyenas) may have also intervened through postdepositional ravaging. This first faunal assemblage potentially created by lions constitutes a new framework for neotaphonomic studies. Since lions may accumulate carcasses under exceptional circumstances, such as those documented at the site reported here, this finding may have important consequences for interpretations of early archaeological and paleontological sites, which provide key information about human evolution.

The Slotted Antler Points from Trail Creek Caves, Alaska: New Information on Their Age and Technology

Despite their occurrences in Siberian and Alaskan late Pleistocene and early Holocene archaeological sites, we know little about the temporal and geographic variability of slotted osseous projectile points. Here we present the results of an analysis of seven slotted antler points from Trail Creek Cave 2 on the Seward Peninsula in western Alaska. The points are morphologically uniform in that they are small and symmetrical. Three concordant AMS 14C radiocarbon ages obtained on gelatin with calibrated median probabilities ranging from 11,350 to 11,257 calendar years ago suggest their manufacture and use during the earliest Holocene. A fourth point yielded a calibrated median probability of 10,335 calendar years ago, suggesting the cave saw reuse, which is consistent with Helge Larsen’s original contention. The analysis provides a benchmark for understanding the temporal context of the small form of slotted points found in Alaska’s early record, which are often referred to as ‘arrowheads'.