DSpace Angular :: Browsing by Author "Santoro, Calogero M."

Browsing by Author "Santoro, Calogero M."

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1000 years of population, warfare, and climate change in pre-Columbian societies of the Central Andes
(2023) Lima, Mauricio; Gayo, Eugenia M.; Gurruchaga, Andone; Estay, Sergio A.; Santoro, Calogero M.
Different Andean societies underwent processes of expansion and collapse during propitious or adverse climate conditions, resource boost or depletion along with population variations. Previous studies have emphasized that demographic collapses of polities in the Central Andes Area were triggered by warfare and the negative impacts of fluctuating climate (droughts) on crop productivity. Nevertheless, the interactions between climatic variability, demography and warfare have been less thoroughly evaluated. We develop population dynamic models to test feedback relationships between population growth, climate change and warfare in the Central Andes, where considerable regional hydroclimate variations have occurred over a millennium. Through population models, we found out that the rise and demise of social polities in the northern coast of the Central Andes appear to be a consequence of climate change. In contrast, for the highlands of Peru and the Titicaca basin, population models suggest that warfare intensity has a negative effect on population growth rates.
A Partially Complete Skeleton of Hippidion Saldiasi Roth, 1899 (Mammalia: Perissodactyla) from the Late Pleistocene of the High Andes in Northern Chile
(2020) Labarca, Rafael; Caro, Francisco J.; Villavicencio, Natalia A.; Capriles, Jose M.; Briones, Esteban; Latorre, Claudio; Santoro, Calogero M.
South America is well known for its abundance of Quaternary fossiliferous deposits, but well-preserved fossil remains from well-dated sites are scarce in the Atacama Desert and adjacent arid Andes. Here we report on a partially complete skeleton (46%) of a single young (ca. 3-4 years old) extinct horse discovered in the Salar de Surire, a salt flat located on the Andean altiplano of northern Chile (4,250 m asl). Comparative and osteometric morphological analyses identify the specimen as a South American endemic horse Hippidion saldiasi Roth, 1899. A direct AMS radiocarbon date on bone collagen yielded a calibrated age of 13,170 cal yr BP (2 sigma range: 13,300-13,060 cal yr BP) indicating that it lived near the end of the last glaciation. The body mass of the individual was calculated at approximately 326.4 kg, close to the upper limit of the larger sizes reported for the genus. Stable isotope evidence shows that the Salar de Surire horse relied on an almost 100% C3 diet that is mostly consistent with Hippidion specimens from other environments that also consumed either mixed C3/C4 or fully C3 diets. This finding is now the southernmost high-elevation record for this species and provides further evidence for the broad geographic and ecological distribution of this genus throughout southern South America.
Acta de Tarapacá: pueblo sin agua, pueblo muerto
(2018) Latorre Hidalgo, Claudio; Marquet Iturriaga, Pablo Angel; McRostie, Virginia; Maldonado, Antonio; Santoro, Calogero M.; Valenzuela, Daniela; Jofré, Daniela; Angelo, Dante; Gayo, Eugenia M.; Hamamé, Eva; Correa, Jacqueline; Barraza, José; Capriles, José M.; Porras, María Eugenia de; Uribe, Mauricio; Castro, Victoria; Standen, Vivien G.
El “Acta de Tarapacá” constituye un llamado de atención sobre la necesidad de cambiar la manera como las sociedades humanas han estado utilizando el agua en el Desierto de Atacama, mediante una perspectiva histórica a lo largo de milenios. El Acta, una iniciativa que resume los resultados del proyecto CONICYT/PIA Anillo SOC1405 “Cambios Sociales y Variabilidad Climática a Largo Plazo en el Desierto de Atacama”, está dirigida a la sociedad civil y a distintas instancias políticas con miras a que se generen cambios tecnológicos y culturales para detener y mitigar los efectos causados por las actividades antrópicas en uno de los desiertos más antiguos y áridos del mundo. En el transcurso del proyecto se constató la necesidad urgente de sensibilizar a la sociedad acerca del desmesurado y mal uso del agua en el Desierto de Atacama; un recurso no renovable con relación a las escalas económicas de extracción ya que depende, fundamentalmente, de aguas fósiles que fueron acumuladas durante milenios en las zonas altas del desierto. De esta manera queremos evitar que este conocimiento científico se encapsule en las universidades y hacer eco de lo señalado por Victoria Castro (2003): Para crecer hay que educar.
Big Fish or Small Fish? Differential Ichthyoarchaeological Representation Revealed by Different Recovery Methods in the Atacama Desert Coast, Northern Chile
(2023) Rebolledo, Sandra; Bearez, Philippe; Zurro, Debora; Santoro, Calogero M.; Latorre, Claudio
Recovery methods and techniques for archaeological sampling can yield major differences in abundance and anatomo-taxonomical representation of animals, affecting past social and ecological reconstruction. Despite being a common organic material in archaeological sites, faunal remains typically exhibit differential preservation of species and skeletal elements due to pre- and post-depositional processes. This is particularly true for small-sized animals such as certain species of fish, whose often small and fragile fragments are difficult to recover and identify. Here, we present the results of a comparative analysis between two ichthyoarchaeological assemblages from Caleta Vitor 3 in northern Chile (CV3, 18 degrees 45 ' 09 '' S), an Early to Middle Holocene (9.2-7.6 ka cal BP) Chinchorro shell midden site. We compare samples obtained and processed, both in the field and the lab, using different recovery techniques. We developed a data standardisation procedure to compare and evaluate skeletal representation, taxa distribution and variations throughout the stratigraphic sequence. Our results show that mesh screen size affects not only the abundance and density of fish but also species representation. Moreover, the identification of small pelagic fish at CV3 sheds further light upon prehistoric fishing strategies and social organisation during the site's early occupation.
Camelids in the hyperarid core of the Atacama desert 12,000-11,000 years ago? A stable isotope study and its consequences for early human settlement
(2024) Ugalde, Paula C.; Gayo, Eugenia M.; Labarca, Rafael; Santoro, Calogero M.; Quade, Jay
How did hunter-gatherers initially settle and move across extreme environments? We conducted a multi-disciplinary study to tackle this question, focusing on how Paleoindigenous populations inhabited the hyperarid core of the Atacama Desert. Particularly, we examined the stable isotopic values of similar to 12,000-11,200-year-old camelid and rodent bones and hair samples retrieved from low-elevation archaeological sites (Pampa del Tamarugal basin - PdT, 800-1200 masl). By integrating novel and existing data into a regional stable isotope ecology, we offer a baseline for interpreting our results. delta C-13 and delta N-15 values on archaeological remains show animals with different geographical origins. A first group includes camelids and rodents with lower delta N-15 values and delta C-13 values indicating a dominantly C-3 diet, corresponding to animals either local to the PdT or from the Andean Steppe, at least similar to 80 km away and between 4000 and 4500 masl. Most of these remains, however, come from residential sites and belong to young camelids, indicating a local origin. A second group presents a higher delta N-15 signal and delta C-13 values indicative of a mixed C-3-C-4 based diet. These animals were not local but source to the Puna at least similar to 60 km away between 3200 - 4000 masl. We hypothesize that the first would correspond to animals associated with hunter-gatherer bands settled around a wetland and grove environment in the PdT. The second group could correspond to remains brought by humans from the Puna to the PdT. Our results demonstrate that during the Late Pleistocene/Early Holocene the Atacama was very different than today, supporting life that included large and mid-size game. These results also show that the core of the Atacama attracted animals and people and counters the notion of this ecosystem as a barren passageway from the Andes to the coast.
Chronology, stratigraphy and hydrological modelling of extensive wetlands and paleolakes in the hyperarid core of the Atacama Desert during the late quaternary
(2018) Pfeiffer, Marco; Latorre H., Claudio; Santoro, Calogero M.; Gayo Hernández, Eugenia Monserrat; Rojas Ávila, Rodrigo; Laura Carrevedo, Maria; Mc Rostie Bustamante, Virginia Bernardita; Finstad, Kari M.; Heimsath, Arjun; Jungers, Matthew C.; De Pol-Holz, Ricardo; Amundson, Ronald
Continuities and discontinuities in the socio-environmental systems of the Atacama Desert during the last 13,000 years
(2017) Santoro, Calogero M.; Capriles, José M.; Gayo Hernández, Eugenia Monserrat; De Porras, María Eugenia; Maldonado, Antonio; Standen, Vivien G.; Latorre H., Claudio; Castro, Victoria; Marquet, P. A. (Pablo A.); Mc Rostie Bustamante, Virginia Bernardita; Uribe, Mauricio; Valenzuela, Daniela; Ugalde, Paula C.; Angelo, Dante
Dietary diverstiy in the Atacama desert during the Late intermediate period of northern Chile
(2019) Alfonso-Durruty, Marta P.; Gayo, Eugenia M.; Standen, Vivien; Castro, Victoria; Latorre, Claudio; Santoro, Calogero M.; Valenzuela, Daniela
The Pacific Ocean that flanks the hyperarid Atacama Desert of Northern Chile is one of the richest biomass producers around the world. Thus, it is considered a key factor for the subsistence of prehistoric societies (including mixed-economy groups), that inhabited its coastal ecosystems as well as the neighboring inland areas. This study assesses the Arica Culture groups' diet (Late Intermediate Period; 1000-1530 CE), through stable isotope (on bone-collagen; delta C-13 and delta N-15) and dental pathology data. Seventy-seven (n = 77) individuals from two inland (LLU54 and AZ8) and one coastal (CAMS) archaeological sites were studied. Results show an important, but lower than predicted by earlier studies, contribution of marine resources in the diet of all three groups. Dental pathologies and stable isotopes indicate that these groups' diet varied in correlation with their distance to the Pacific Ocean as well as group and individual preferences. The results challenge the idea that Arica Culture groups depended heavily on marine resources for their subsistence. In contrast, this study shows both that the Arica Culture groups' diet was diverse, and that the terrestrial resources consumed were mostly contributed by C-3/CAM plants instead of maize. (C) 2019 Elsevier Ltd. All rights reserved.
First record of cf. Aenocyon dirus (Leidy, 1858) (Carnivora, Canidae), from the Upper Pleistocene of the Atacama Desert, northern Chile
(2022) Caro, Francisco J.; Labarca, Rafael; Prevosti, Francisco J.; Villavicencio, Natalia; Jarpa, Gabriela M.; Herrera, Katherine A.; Correa-Lau, Jacqueline; Latorre, Claudio; Santoro, Calogero M.
Fossil records of canids are rare and incomplete in South America. In Chile, all well-identified taxa are part of the "South American Canid Clade" and come from sites located in southern Patagonia. Here, we report the first record for Chile of a taxon of the "Canis clade," assigned to cf. Aenocyon dirus. The fossil remains consist of a partially complete left hind limb, exposed by aeolian deflation, which facilitated its discovery at an isolated setting in Quebrada Mani, named QM38 site, in the southern sector of the Pampa del Tamarugal basin, part of the hyperarid core of the Atacama Desert, northern Chile. Measurements of the fossil are larger than the Protocyon troglodytes, falling in the smaller size range of A. dirus and within the larger range of Theriodictis platensis. Its morphological features compared with bone references of large extinct canids show that the fossil belongs to a small-sized Aenocyon. The remains occur in surface silty clays deposited by an alluvial fan that was active in the Pampa del Tamarugal basin in the Late Pleistocene. A radiocarbon date from bone apatite yielded an age of 14,660 cal years BP, placing it within the first half of the Central Andean Pluvial Event when this basin was wetter, well vegetated, and inhabited by large, medium, and small herbivores. No other large predator records are known from this basin, and our find affords a more complete view of this ecosystem which thrived in the hyperarid core of the Atacama during the Late Pleistocene.
FROM THE PACIFIC TO THE TROPICAL FORESTS: NETWORKS OF SOCIAL INTERACTION IN THE ATACAMA DESERT, LATE IN THE PLEISTOCENE
(2019) Santoro, Calogero M.; Gayo, Eugenia M.; Capriles, Jose M.; Rivadeneira, Marcelo M.; Herrera, Katherine A.; Mandakovic, Valentina; Rallo, Monica; Rech, Jason A.; Cases, Barbara; Briones, Luis; Olguin, Laura; Valenzuela, Daniela; Borrero, Luis A.; Ugalde, Paula C.; Roihhanuner, Francisco; Latorre, Claudio; Szpak, Paul
The social groups that initially inhabited the hyper arid core of the Atacama Desert of northern Chile during the late Pleistocene integrated a wide range of local, regional and supra regional goods and ideas for their social reproduction as suggested by the archaeological evidence contained in several open camps in Pampa del Tamarugal (PdT). Local resources for maintaining their every-day life, included stone raw material, wood, plant and animal fibers, game, and fresh water acquired within a radius of similar to 30 km (ca. 1-2 days journey). At a regional scale, some goods were introduced from the Pacific coast (60-80 km to the west, ca. 3-4 days journey), including elongated rounded cobbles used as hammer stones in lithic production, and shells, especially from non-edible species of mollusks. From the Andes (ranging 80-150 km to the east, ca. 5-8 days of journey), they obtained camelid fiber, obsidian and a high-quality chalcedony, in addition to sharing knowledge on projectile point designs (Patapatane and Tuina type forms). Pieces of wood of a tropical forest tree species (Ceiba spp.) from the east Andean lowlands (600 km away, ca. 30 days of journey) were also brought to the PdT. While local goods were procured by the circulation of people within the PdT, the small number of foreign items would have been acquired through some sort of exchange networks that integrated dispersed local communities throughout several ecosystems. These networks may have been a key factor behind the success exhibited by these early huntergatherers in the hyper arid ecosystems of the Atacama Desert at the end of the Pleistocene.
Genetic studies of various Prosopis species (Leguminosae, Section Algarobia) co-occurring in oases of the Atacama Desert (northern Chile)
(2021) Bessega, Cecilia; Pometti, Carolina; Fortunato, Reneé; Greene, Francisca; Santoro, Calogero M.; Mc Rostie Bustamante, Virginia Bernardita
High- and low-latitude forcings drive Atacama Desert rainfall variations over the past 16,000 years
(2021) Gonzalez-Pinilla, Francisco J.; Latorre, Claudio; Rojas, Maisa; Houston, John; Ignacia Rocuant, M.; Maldonado, Antonio; Santoro, Calogero M.; Quade, Jay; Betancourt, Julio L.
Late Quaternary precipitation dynamics in the central Andes have been linked to both high- and low-latitude atmospheric teleconnections. We use present-day relationships between fecal pellet diameters from ashy chinchilla rats (Abrocoma cinerea) and mean annual rainfall to reconstruct the timing and magnitude of pluvials (wet episodes) spanning the past 16,000 years in the Atacama Desert based on 81 C-14-dated A. cinerea paleomiddens. A transient climate simulation shows that pluvials identified at 15.9 to 14.8, 13.0 to 8.6, and 8.1 to 7.6 ka B.P. can be linked to North Atlantic (high-latitude) forcing (e. g., Heinrich Stadial 1, Younger Dryas, and Bond cold events). Holocene pluvials at 5.0 to 4.6, 3.2 to 2.1, and 1.4 to 0.7 ka B.P. are not simulated, implying low-latitude internal variability forcing (i.e., ENSO regime shifts). These results help constrain future central Andean hydroclimatic variability and hold promise for reconstructing past climates from rodent middens in desert ecosystems worldwide.
Late Quaternary hydrological and ecological changes in the hyperarid core of the northern Atacama Desert (∼21°S)
(2012) Gayo, Eugenia M.; Latorre, Claudio; Jordan, Teresa E.; Nester, Peter L.; Estay, Sergio A.; Ojeda, Karla F.; Santoro, Calogero M.
The hyperarid core of the Atacama Desert possesses important reserves of "fossil" or ancient groundwater, yet the extent and timing of past hydrologic change during the late Quaternary is largely unknown. In situ and/or short-distance transported leaf-litter deposits abound along relict fluvial terraces inserted within four dry and unvegetated valleys that drain into the endorheic basin of Pampa del Tamarugal (PDT, 21 degrees S, 900-1000 m), one of the largest and economically important aquifers in northern Chile. Our exceptional archive offers the opportunity to evaluate the response of low-elevation desert ecological and hydrological systems to late Quaternary climate variability. Three repeated expansions of riparian/wetland ecosystems, and perennial rivers occurred along the southernmost PDT basin between 17.6-14.2 ka, 12.1-11.4 ka and from 1.01-0.71 ka. Both early and late archaic archaeological artefact are present in clear association with our fossil riparian/wetland assemblages, which suggests that these palaeoenvironmental changes facilitated past human occupations in the hyperarid core of the Atacama Desert. Using modern analogues, we estimate that these ecological and hydrological changes were triggered by a threefold increase in rainfall along the headwaters of what are presently inactive canyons. Comparisons with other regional palaeoclimatic records from the central Andes indicate that these changes were synchronous with the widespread pluvial stages now termed the Central Andean Pluvial Event (CAPE- 17.5-14.2 ka and 13.8-9.7 ka). In addition, we summarize new evidence for perennial runoff, riparian ecosystems and a major human settlement during the latest Holocene. Our findings clearly show that local hydrological changes in the PDT were coupled with precipitation variability in the adjacent eastern highlands during the late Quaternary. The long-term dynamics of low-elevation desert ecological and hydrological systems are likely driven by changes in moisture sources, with one source tied to the Amazon region (N-NE mode) and the other to the Gran Chaco region (SE mode). We conclude by linking ENSO-like variability and moisture variations over the Gran Chaco to the three major regional-scale recharge events over the last 18 ka in the PDT basin. We conclude by asserting that an important portion of the groundwater resources in the PDT is indeed fossil, inherited from past pluvial events. We recommend that the relationship between ancient recharge, together with palaeoclimate records of past headwater rainfall fluctuations should be incorporated into future water-balance models and evaluation of groundwater potential in northern Chile. (C) 2012 Elsevier B.V. All rights reserved.
Loco or no Loco? Holocene Climatic Fluctuations, Human Demography, and Community Based Management of Coastal Resources in Northern Chile
(2017) Santoro, Calogero M.; Gayo Hernández, Eugenia Monserrat; Carter, Chris; Standen, Vivien G.; Castro, Victoria; Valenzuela, Daniela; De Pol-Holz, Ricardo; Marquet, P. A. (Pablo A.); Latorre H., Claudio
Pre-European Plant Consumption and Cultural Changes in the Coastal Lluta Valley, Atacama Desert, Northern Chile (Ca. 5140-390 Cal Yr BP)
(2020) Garcia, Magdalena; Santoro, Calogero M.; McRostie, Virginia; Mendez-Quiros, Pablo; Salas-Egana, Carolina; Carter, Chris; Rothhammer, Francisco; Latorre, Claudio
Pre-European Plant Consumption and Cultural Changes in the Coastal Lluta Valley, Atacama Desert, Northern Chile (Ca. 5140-390 Cal Yr BP). The introduction of domesticated plants into ancient hunting and gathering economic systems expanded and transformed human societies worldwide during the Holocene. These transformations occurred even in the oases and hyperarid environments of the Atacama Desert along the Pacific coast. Human groups inhabiting this desert incorporated adjacent habitats to the semi-tropical valleys through transitory or logistic camps like Morro Negro 1 (MN-1), in the Lluta valley (similar to 12 km from the littoral in northernmost Chile), into their settlement patterns. During the earliest occupation (Late Archaic period, 5140-4270 cal yr BP) people collected and consumed wild plants, although crops such as Lagenaria were present. Following a gap of more than 2000 years between 4270 and 1850, people returned and introduced new domesticated plants at the site (Gossypium, Zea mays, Capsicum), which displaced the use of wild reed (Schoenoplectus) rhizomes as the chief staple during the first occupation. This change in food consumption was linked to the transformations that took place during the Archaic-Formative transition, but did not entirely shift the ways of life of these coastal marine hunter-gatherers.
RISE AND DECLINE OF CHINCHORRO SACRED LANDSCAPES ALONG THE HYPERARID COAST OF THE ATACAMA DESERT
(2012) Santoro, Calogero M.; Rivadeneira, Marcelo M.; Latorre, Claudio; Rothhammer, Francisco; Standen, Vivien G.
The study of complex funerary ritual development among hunters and gatherers societies should take into account how people made up for the continuity of their social system without the support of centralized organizations. This research integrates cultural and natural factors to explore how the Chinchorro carried on with their way of life isolated at geographically restricted perennial river mouths with fresh water along the Atacama Desert in the Pacific coast of South America. Within these rather crowded settlings, they created and maintained a social system catalyzed by a complex funerary tradition, embodied by a unique funerary ideological discourse that resulted in the creation of a sacred landscape or "spiritscape". We argue that the extreme hyperaridity of the coastal Atacama Desert (21 degrees-17.30 degrees S), and the extraordinary biomass production of the marine littoral constituted a fundamental milieu for the maintenance of their long-term social system. The Chinchorro belief system lasted for several millennia (8,000-4,000 BP), but new ways of life and burial practices followed major changes in the coastal ecosystem they relied on, which would have influenced how the "old tradition" was manifested over time. Conversely, we sustain that these natural "constraints" faced by the Chinchorro along the coast of the Atacama Desert, were influential, in the course of their history or the way they socially organized themselves.
Silvopastoralism and the shaping of forest patches in the Atacama Desert during the Formative Period (ca. 3000-1500 years BP)
(2022) McRostie, Virginia; Babot, Pilar; Calas, Elisa; Gayo, Eugenia; Gallardo, Francisco; Godoy-Aguirre, Carolina; Labarca, Rafael; Latorre, Claudio; Nunez, Lautaro; Ojeda, Karla; Santoro, Calogero M.; Valenzuela, Daniela
During the Formative period by the Late-Holocene (ca. 3000-1500 BP), semi-sedentary and sedentary human occupations had emerged in the oases, salares, and riverine systems in the central depression (2400-1000 masl) of the Atacama Desert, northern Chile (19-25 degrees S). This hyperarid core was marginally occupied during the post-Pleistocene and middle Holocene droughts. Settlement on these lower belts was accompanied by a rise in humidity, the introduction of Andean crops, flourishment of Prosopis spp. (algarrobo) forests, and increasing integration of domestic camelid caravans. Here, we explore lowland husbandry within risk-spreading strategies, focusing on silvopastoralism and endozoochory between camelids and algarrobos. Analysis of camelid coprolites from seven archeological sites located in the Pampa del Tamarugal, Loa River, and Salar de Atacama found intense grinding from camelid chewing and indicated a ruminal digestive system. Abundant macro and microremains in the form of tissues, phytoliths, crystals, cell structures, and others, were identified as Prosopis, Atriplex, Schoenoplectus, Distichlis, and Phragmites. We conclude that camelids were foraging for Prosopis, although the rather low number of entire seeds preserved in the coprolites leads us to think that these herbivores might not have been the main vectors for the spread and germination of algarrobos. More samples and interdisciplinary studies are needed to comprehend the complex socioecological web in the shaping of these forests and the management of the Atacama Desert landscapes.
The Dry Puna as an ecological megapatch and the peopling of South America: Technology, mobility, and the development of a late Pleistocene/early Holocene Andean hunter-gatherer tradition in northern Chile
(2017) Osorio, Daniela; Steele, James; Sepúlveda, Marcela; Gayo Hernández, Eugenia Monserrat; Capriles, José M.; Herrera, Katherine; Ugalde, Paula; De Pol-Holz, Ricardo; Latorre H., Claudio; Santoro, Calogero M.
The first peoples of the Atacama Desert lived among the trees: A 11,600-to 11,200-year- old grove and congregation site
(2024) Ugalde, Paula C.; Joly, Delphine; Latorre, Claudio; Gayo, Eugenia M.; Labarca, Rafael; Simunovic, Mikhaela; Mcrostie, Virginia; Holliday, Vance T.; Quade, Jay; Santoro, Calogero M.
In deserts, water has been singled out as the most important factor for choosing where to settle, but trees were likely an important part of the landscape for hunter - gatherers beyond merely constituting an economic resource. Yet, this critical aspect has not been considered archaeologically. Here, we present the results of mapping and radiocarbon dating of a truly unique archaeological record. Over 150 preserved stumps around five Late Pleistocene/ Early Holocene archaeological campsites (12,800 to 11,200 cal BP) show that trees were key features in the creation of everyday habitats for the first inhabitants of the Atacama Desert. At two of these sites, QM12 and QM35, the spatial and chronological correlation between trees and hearths reveals that people located their homes under the tree canopy. At residential site QM35, artifact distribution coincides with a grove dated to - 11,600 to 11,200 cal BP. A third residential area (QM32) occurred along the grove margins - 12,000 to 11,200 cal BP. Based on the distinct cultural material of these two camps, we propose that two different groups intermittently shared this rich wetland - grove environment. The tree taxa suggest a preference for the native Schinus molle, a tree scarcely present on the landscape today, over the endemic, nitrogen - fixing Strombocarpa tamarugo , both for toolmaking and firewood and even though the S. tamarugo was locally more abundant. Together with the spatial and chronological coincidence of campsites, hearths, and trees, we propose that people spared the most abundant and resilient species to create their homes, in turn promoting fertility oases amid the Atacama's hyperaridity.
THE IMPACT OF ENSO IN THE ATACAMA DESERT AND AUSTRALIAN ARID ZONE: EXPLORATORY TIME-SERIES ANALYSIS OF ARCHAEOLOGICAL RECORDS
(2008) Williams, Alan; Santoro, Calogero M.; Smith, Michael A.; Latorre, Claudio
A comparison of archaeological data in the Atacama Desert and Australian arid zone shows the impact of the El Nino-Southern Oscillation (ENSO) over the last 5,000 years. Using a dataset of > 1400 radiocarbon dates from archaeological sites across the two regions as a proxy for population change, we develop radiocarbon density plots, which are then used to explore the responses of these prehistoric populations to ENSO climatic variability. Under ail ENSO regime, precipitation is in anti-phase between Australia and coastal Chile. As ENSO also impacts marine resource productivity in Chile and advection of moisture from the Amazon Basin, the net effects of ENSO on subsistence economies on either side of the Tropical Pacific should be positively correlated. This is confirmed by cross-spectral analysis of the radiocarbon density plots, which shows that population responses oil either side of the Tropical Pacific are synchronous (r = >0.82). Both the Australian and Atacama desert records show a general increase in population from about 13 cal kyr BP, increasing through the mid-Holocene climatic optimum. Following the intensification of ENSO around 3.7 cal kyr BP, we call correlate 'boom and bust' Cycles Of Occupation on both sides of the Pacific, including the collapse of the Atacama desert coastal economy and Cultural system at 3 cal kyr BP and the decline of both the Atacama highlands and Central Australian dryland populations between 3-2 cal kyr BR After 2 cal kyr BP adaptive responses to ENSO varied between these regions, though all dryland populations show resurgence in occupation.

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