The Atacama Desert lies between the Pacific coast and the Andes in northern Chile. It is the largest desert in South America and the driest on Earth. Here, annual precipitation is almost zero. The little water that is available depends on the summer rainfall that falls on the Andean mountains. It reaches the desert by runoff and is found within some canyons or by the emergence of groundwater. The presence of life in this extreme environment may seem unimaginable today; however, fossil and archaeological records reveal that plants, animals, and even humans lived in this region during various periods over the last 18,000 years.Fil: de Porras, Maria Eugenia. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Provincia de Mendoza. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales. Universidad Nacional de Cuyo. Instituto Argentino de Nivología, Glaciología y Ciencias Ambientales; ArgentinaFil: Gayo, Eugenia M.. Centro de Ciencia del Clima y la Resiliencia; ChileFil: Uribe, Mauricio. Universidad de Chile; ChileFil: Maldonado, Antonio. Comisión Nacional de Investigación Científica y Tecnológica. Centro de Investigación Regional. Centro de Estudios en Zonas Áridas; Chil

de Porras, Maria Eugenia

Gayo, Eugenia M.

Maldonado, Antonio

Uribe, Mauricio

English

CONICET Digital

PAGES HORIZONS • VOLUME 1 • 202144 Name: GeckoScientific name: Phyllodactylus gerrhopygusWhere to find it: Northern Atacama Desert from the coast to the mountains up to 3500 m (11,500 ft) above sea level.Fun fact: Each of its fingers has two touch pads and claws between them which allow Gecko to move on the hot surface of the desert.Humans and environments in the most arid place in the world: The Atacama DesertMaría Eugenia de Porras, Eugenia M. Gayó, Mauricio Uribe and Antonio Maldonadophoto credit: Antonio MaldonadoThe Atacama Desert lies between the Pacific coast and the Andes in northern Chile. It is the largest desert in South America and the driest on Earth. Here, annual precipitation is almost zero. The little water that is available depends on the summer rainfall that falls on the Andean mountains. It reaches the desert by runoff and is found within some canyons or by the emergence of groundwater. The presence of life in this extreme environment may seem unimaginable today; however, fossil and archaeological records reveal that plants, animals, and even humans lived in this region during various periods over the last 18,000 years.doi.org/10.22498/pages.horiz.1.44Wow! Really? The Atacama Desert is like the surface of Mars! Now I get why I was sent here to be trained for my mission! But has the desert ever hosted life? Hmmm, I'm wondering … has it been less dry in the past?Hey Zoë! Scientists working with paleoenvironmental archives have indeed found evidence that there were wetter periods several times in the Atacama Desert over the last 18,000 years.Different paleoenvironmental records indicate that extensive wetlands, springs, shallow lakes, and several perennial rivers existed between 18,000 and 14,000 years ago in the core of the Atacama Desert. These landscape transformations are explained by higher precipitation over the Andes in the past (named the Central Andean pluvial Event 1), that watered the core of the desert. This led to a flourishing of life, including several perennial native trees (Prosopis tamarugoA, Escallonia angustifoliaB, Schinus molleC) growing along rivers (riparian areas) and close to wetland oases.1Such a vegetated landscape also allowed many types of animals to live in this region, including rodents, birds, and South American camelids (guanacosD), as well as some larger, now extinct, South American animals (megafauna) such as small horsesE and ground sloths.F,2 This wetter phase ended abruptly about 14,000 years ago, leading to climatic and ecological conditions similar to today, which persisted over the following 1000 years.1pacificOceanName: ZoëType: Solar- powered autonomous robotMission: Detect microorganisms and map the distribution of life in the Atacama Desert; perform tasks that could be used in future exploration of Mars.A500040003000200010000B Altitude (m above sea level)Atacama Desert coreAltiplanopacificOceanAAndean mountainsAtacamaAtlanticOcean DesertBChile18,000–14,000 yr BpPAGES HORIZONS • VOLUME 1 • 2021 45 Fortunately they didn't! Archaeologists have found evidence that people moved to the few canyons within the desert that still had permanent water, or towards the	Pacific	coast	and	towards	the	Andean highlands.3,4About 13,000 years ago, the desert once again became wet (Central Andean pluvial Event 2), and freshwater oases with herbaceous vegetation and trees took root across the lowlands of the Atacama Desert.1,3,4 The megafauna was no longer part of the story, but small rodents, birds, and camelids such as guanacosD and vicuñasG became commonplace in these ecosystems.Humans also entered the scene during this period: evidence indicates that the first settlers in the desert arrived about 12,800 years ago.3,4 Attracted by the availability of biotic and water resources, these hunter-gatherers established camps around wetlands and riparian areas. However, such residential bases were only intermittently occupied as environmental and ecological conditions varied, making a nomadic lifestyle necessary during various periods in the extreme inland Atacama.3,4The lack of paleoenvironmental and archaeological records dating between 9500 and 3000 years ago has led paleoecologists and archaeologists to infer that a huge 6000-year drought took place in the Atacama Desert core due to a decrease in rainfall over the Andes.1,3,4 The heavy decrease in water availability was hard for hunter-gatherer groups, who disappeared from the landscape. in fact, the previous environment full of water and biotic resources vanished, leaving a harsh habitat resembling the modern desert.13,000–9500 yr BpEarliest human sites at presentProjectile point9500–3000 yr BpOh noooo!!! Don't tell me that humans met the same fate as the megafauna!!! Did the humans in the Atacama Desert go extinct???? Dear Gecko, please, tell me more!!!!PAGES HORIZONS • VOLUME 1 • 202146 Wet phases returned to the area about 3000 years ago, but these were only moderate in comparison to what had occurred before. paleoenvironmental evidence indicates that two wet periods at 2500–2000 and 1600–1100 years ago led to increased runoff and local water-table levels across the Atacama Desert core. However, these were not enough to activate springs or wetlands, and the vegetation cover of native herbaceous and woody plants was scarce and mostly restricted to ravines.3,4 Humans re-occupied the low-elevation desert around 2800 years ago.5 Since then, people gradually adapted their traditional hunting and gathering system to an agricultural lifestyle, despite still foraging some wild resources (plants and animals). population sizes increased when largely dispersed but concentrated villages with monumental public spaces (squares) and cemeteries were built, incorporating new forms of social organization with different economic and ritual activities. Local communities developed sophisticated technologies to manage surface water, including dams and irrigation canals for maintaining large and well-drained cultivation plots on what are now arid floodplains. Domestic South American camelids (alpacasH and llamasi) usually hung around and herded around these fields where quinoa, gourd, and maize were cultivated, as well as algarrobos or mesquite trees (Prosopis).3,4,5Abandoned village with circular-shaped buildingsAncient cultivation plots in the desertCob associated with a cultivation plotArid conditions set into the area 1000 years ago.3,4 in order to face this scenario, people moved from the desert core to the pacific coast or higher elevations (above 2400 m/7900 ft above sea level), where water was much more abundant. That is, villages were now built following a vertical arrangement at upstream oases (canyons, wetlands) or in the Altiplano.6 public spaces were separated from residential areas, located within or outside the villages. New systems of agriculture (arranged as terraced fields), defensive infrastructures (locally known as pukaras) and land-use patterns emerged. Since this phase, the number of villages and the population density started to increase, and local communities intensified agricultural activities and the husbandry of alpacasH and llamasi within these circumscribed territories at high elevations.6 The Atacama lowlands become a space that served as a place for communication and exchange between people from Andean highlands and the pacific coast (an internodal territory). Still, archaeologists have suggested that this landscape was used opportunistically by farmers after flashflood episodes that temporarily inundated the Atacama Desert core.2800–1000 yr Bp~1000 yr BpPAGES HORIZONS • VOLUME 1 • 2021 47 Let me guess, Gecko! Humans never settled long term in the desert core again!!!Hmmm ... I'm afraid not. They have actually inhabited this landscape since the 15th century, but in a quite different way ...During the last 700 years, climate has remained similar to present, even during very short (but decade-long) wet pulses.3,4 Despite this hostile environment, humans have continuously inhabited the core of the Atacama Desert since the European colonization (starting in 1533 CE).3,4,7 This has been achieved by a flexible lifestyle that involves the incorporation of new technologies and the large-scale exploitation of non-renewable natural resources. For example, modern urban centers have relied heavily on the groundwater stored within underground aquifers (fossil water) during past wet phases.3,4,7 The first profitable mining industry conducted between the 19th and 20th centuries in the Atacama Desert depended not only on the extraction of saltpeter but also on the use of logs of trees that grew in the core of the desert during both Central Andean pluvial Events. Today, the Atacama Desert is the world's top producer of copper, which is a key raw material to manufacture a diverse array of devices that are part of our day-to-day life (e.g. computers, batteries, pipes, clothes, cars, electrical wires, and coins). Nevertheless, such extensive copper extraction to supply global technological needs will soon consume either the entire mineral reserve or a large volume of fossil water.Old shovel used for saltpeter and fossil wood extractionAncient saltpeter/"caliche" processing plantSaltpeter village ruins at present19th–20th centuriesMajor paleontological, archaeological, and environmental changes recorded in the Atacama Desert over the last 18,000 years18,000 14,000 13,000 9500 3000 1000 150 years agoWETTEr WETTEr MODErATELYWETTErDrYErDrYEr SiMiLAr     COMpArED TO prESENTperennial native trees and megafauna inhabited the desertFirst human settlers arrived. Small rodents, birds, and camelids were presentHumans, animals, and plants abandoned the desert Humans moved back to the desert. Agricultural lifestyle emerged, associated with nodal villagesNew villages arose at higher elevations. Agricultural developmentin terraced fieldsDevelopment of new technologies. Large-scale exploitation of natural resources like saltpeter and minerals (copper)PAGES HORIZONS • VOLUME 1 • 202148 As you see, my dear Zoë, the Atacama Desert has a fascinating environmental history, and people have maintained a delicate balance for over 12,000 years, but the modern lifestyle has affected the balanced relationship that native societies used to have with the fragile Atacama Desert ecosystem …Extraction of saltpeter: Ancient, extensive economic activity performed during the 19th and 20th centuries to extract potassium nitrate (saltpeter/caliche) from the surface of the Atacama Desert to be used to cure meat and to produce fireworks, fertilizers, and toothpastes.Ground sloth: Extinct large mammal directly related to modern sloths. it was an herbivore that lived in and around the riparian and wetland oases of the Atacama Desert.Oases: isolated areas in the desert where water is available.Paleoenvironmental: related to a certain environment of the geologic past.Perennial rivers: Streams where water is found throughout the year.Water-table level: Shallowest depth of the groundwater below the Earth's surface. This depth can change through time.Wetlands: Areas in the desert where water reaches the surface most of the year, allowing plants to grow there or in the surrounding areas.GLOSSARYExposed fossil wood and plant materialAbsolutely! Now I feel a little bit ashamed since my circuits are made with Chilean copper … building me consumed a lot of fossil water! Now I understand that the Atacama Desert is not a barren landscape … its present ecosystems and archaeological heritage deserve to be protected and the extraction of fossil resources needs to be managed sustainably. I hope it is not too late …PAGES HORIZONS • VOLUME 1 • 2021 59 Miebach (pp. 38-40)1. Litt et al. (2012) Quat Sci rev 49: 95-1052. Video: Tired of reading? Take a look at this short video about pollen3. Video: Want to know more about pollen analysis? Here's an informative video4. Video: Some nice images from the Dead SeaDe Porras et al. (pp. 44-48)1. Workman Tr et al. (2020) Quat Sci rev 243: 1065022. Villavicencio NA et al. (2019) in: Cartes L et al. (Eds) Avances en pale-ontología Chilena. instituto Antárctico Chileno, pp. 296-2983. Maldonado A et al. (2016) pAGES Mag 24: 56-574. Santoro CM et al. (2017) J Anthropol Archaeol 46: 28-395. Uribe M et al. (2020) Lat Am Antiq 1: 81-1026. Uribe M (2006) Estudios atacameños 31: 91-1147. Gayo EM et al. (2019) Elem Sci Anth 7: 15Olatoyan (pp. 49-51)1. Ferrar AA, Lötter MC (2007) Mpumalanga biodiversity conservation plan handbook. Mpumalanga Tourism & parks Agency, pp 9-122. Huffman TN (2007) Handbook to the iron Age: the archaeology of pre-colonial farming communities in southern Africa, pp 3313. Manning K et al. (2011) J Archaeol Sci 38: 312-3224. Crowther A et al. (2018) Quat int 489: 101-1205. Humphris JE (2010) An Archaeometallurgical investigation of iron Smelting Traditions in Southern rwanda. phD thesis, pp. 37-436. MiME/ADB (1996) Cambodian Energy Statistics; Sources of Ener-gy Data and Methods of Estimation. United Nations, 69 pp7. Food and Agriculture Organization (FAO) (2010) Forestry paper, Ch. 28. Shi N et al. (1998) Veg Hist Archaeobot 7: 127-1409. Willis KJ (2019) Tribulus terrestris (85.4.1 - 1). Digitized palynological slide. Obtained from: Martin AC, Harvey WJ (2017)10. Widgren M et al. (2016) J Afr Archaeol 14: 33-53Glossary (pp. 54-55)1. Age models: On this website, under "Software and animations", you can see an animation of how fast sediments deposit and how the depth-age model is therefore built.2. radiocarbon: Here's an interesting article in The Conversation about how radiocarbon dating worksACKNOWLEDGMENTSThe editors extend their sincere gratitude to Clara Aguilar, Yassine Ait Brahim, Stella Alexandroff, María Andrés, Asfawossen Asrat, Mindy Bell, Stephanie Borg, Ed Brook, Daniel Bruno, Emilie Capron, Cristiano M. Chiessi, Elisabeth Dietze, Mike Evans, Fátima Franco, Eva Fuentes, Carmen Galián-Barrueco, Eduardo García prieto, Lindsey Gillson, Dai Grady, Alaia Herranz Franco, Darrell Kaufman, Christophe Le Gall, Quentin Lepiller, Nick Marriner, Erin Martin-Jones, Neil roberts, Enrique royuela, Deirdre ryan, Willy Tinner, and Blas Valero-Garcés for lending their expertise in reviewing the articles in this issue.Boris Vannière is supported by the Centre National de la recherche Scientifique (CNrS) and the Maison des Sciences de l'Homme et de l'Environnement (MSHE), France.Graciela Gil-romera is supported by the philipps-Märburg University, Germany, and the Spanish research and Science Council (CSiC), Spain.Sefton and Tan (pp. 16-19)Symbols are attributed to Biorender, Canva and ian.umces.edu. Styling attributed to Canva.Frisia et al. (pp. 30-33)We are indebted to the Australian research Council (ArC-Dp160101058) and the Australia Synchrotron for support. Thanks to Mohammadali Faraji who provided the Sr image for Fig. 5 and Andrea Borsato for the data used in Fig. 4 and 5.De Porras et al. (pp. 44-48)The authors are very thankful to Carla infanta Gabor (instagram: @carla_ilustraciones) for her dedication during the illustration process, and Delfina España and Zoë Fleming for their help with the design and language style, respectively. project FONDECYT #1181829 financially supported this publication.PAGES International Project OfficeHochschulstrasse 4CH-3012 Bern, SwitzerlandSeries EditorsSarah Eggleston, Boris Vannière, Graciela Gil-romera, Marie-France LoutreText EditingAngela WadeLayoutSarah EgglestonDesignsujata.designPrinted on recycled paper by  Läderach AG, Bern, SwitzerlandTelephone +41 31 631 56 11Email   pages@pages.unibe.chWebsite   pastglobalchanges.orgTwitter   @pAGES_ipOFacebook  pastGlobalChangesFind out more about PAGES Horizons atpastglobalchanges.org/products/pages-horizonsParent programpAGES is a Global research project of Future Earth.SupportersThe pAGES international project Office and its publi-cations are supported by the Swiss Academy of Sci-ences (SCNAT), the Chinese Academy of Sciences (CAS), and the University of Bern, Switzerland.doi.org/10.22498/pages.horiz.1© 2021 PAGES

Humans and environments in the most arid place of the world

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Humans and environments in the most arid place of the world

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