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People of the CoastalAtacama Desert
Living Between Sand Dunes andWaves of the Pacific Ocean
Calogero M. Santoro, Bernardo T. Arriaza,Vivien G. Standen, and Pablo A. Marquet
Introduction
When Europeans colonized the coast of the Atacama Desert region (188–278S) in
the sixteenth century they described the local people as skillful fishermen. In
particular, Bibar (1966 [1565]: 12) observed:
Those who kill sea lions do not kill other fish, as we have said, and those who kill
toninas [dolphin] do it routinely. In this way, each category of fisherman kills the type
of fish of his specialty and no other; and when they die, it is custom to place the skulls
[of marine mammals] and all the fishing tools such as nets, harpoons, and fishhooks
on top of the grave.
This specialized labor force was not linked to complex forms of social organization
as depicted in prehistoric cultures of the coasts of central Peru and northwestern
North America. For this reason, the Europeans were not able to appreciate the
cultural richness of the native populations that were settled along the coast of the
Atacama Desert. For the Spaniards, these Indians were dirty and poor, with a
simple way of life and modest possessions (Lozano-Machuca 1885 [1581]); thus,
the sixteenth century Hispanic records provide no information relating to other
cultural traits of this Amerindian population, such as funerary procedures, body
painting, or tool decoration, nor about their geoglyphs and petroglyphs.
The coastal way of life has deep roots in the cultural history of the American
continent, as it seems to be connected with the first people who immigrated into
South America, late in the Pleistocene epoch. Around 11,000–10,000 years ago,
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people focused on the coast of the Atacama territories and over several millennia
they gradually transformed their culture. They created efficient technologies and
strategies to maximize the subsistence possibilities provided by the Pacific Ocean
and the desert coast (Llagostera 1992; Nunez 1983; Rivera and Rothhammer 1991;
Standen et al. in press). This allowed them to reduce risks of the uncertainties
typical of a desert environment as they lived between diverse habitats within a large
but narrow territory along the coast. Despite the fact that the hunter-gatherers and
fishermen of the coastal Atacama Desert inhabited a landscape with limited
terrestrial resources, their descendants were able to create and develop a complex
cultural system, with rather egalitarian political structures. However, the most
fascinating creation of these early people was the development of sophisticated
systems of artificial mummification, the ideological and social principles of which
were arguably crucial for the maintenance of social ties. As we show below, artificial
mummification, and its unknown cosmological world, was the most dynamic
feature of the cultural history of these coastal desert people (Arriaza and Standen
2002).
Lying adjacent to the littoral of the Pacific Ocean in western South America, the
Atacama Desert has a very limited range of edible plants and herded animals. This
contrasts sharply with the Australian deserts or the Kalahari and Namib Deserts of
southern Africa, which offer many (albeit patchy) terrestrial food resources for
hunter-gatherers. These larger desert territories, however, lack the abundance of
water seen in the Atacama in the form of permanent or seasonal streams originat-
ing in the high Andes, located around 100–150 km to the east (see Figure 13.1).
This supporting network of water sources and the Pacific Ocean, one of the richest
and most diverse marine biomasses in the world, creates unusual conditions
allowing for the permanent occupation of this area by hunter-gatherers and
fishermen. The first known inhabitants who arrived on the Pacific coastline of
this region initiated a subsistence system that after 2,000–3,000 years of experimen-
tation became strongly dependent on a wide variety of marine resources, hidden
under the waves of the Pacific (Bird 1943; Llagostera 1992; Nunez 1983; Schiappa-
casse and Niemeyer 1984). They complemented their maritime economy with
unpredictable and dispersed terrestrial resources, located along the quebradas
(narrow deep canyons with permanent or intermittent courses of water) and
oases touched by sand dunes swept by the desert winds.
The Selknam, hunter-gatherers of Tierra del Fuego, can serve as an analogy for
understanding early Atacama populations. They inhabited an extremely harsh
environment, but also developed a complex ideological system expressed in so-
phisticated ceremonies, which included body painting, masks, and performances
representing supernatural characters. These rituals helped them to maintain and
pass on their ideology and promoted social and biological reproduction. Similarly,
Australian desert Aborigines continue to exercise complex systems of thinking and
performance through a rich iconographic rock art and curation of tjuringa (sacred
boards with painted or incised motif), comprising ‘‘a semiotic system that medi-
ates social and territorial relations’’ (Rosenfeld and Smith 2002: 112), and body
painting with the ‘‘appearance of ancestral forces’’ (Morphy 1998: 23). In these
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Santoro , Arriaza , Standen , Marquet
cases we are dealing with highly abstract thought processes and complex aesthetic
expression which appears to have originated in the late Pleistocene (cf. Mulvaney
and Kamminga 1999).
In this chapter we present an analytical and comparative description of the
origin and cultural evolution of people in the Atacama Desert, bringing together
Northern Atacama
CentralAtacama
SouthernAtacama
Copiapó
Pac
ific
Oce
an
Iquique
9
10
67
Artica
43
2
1
Ilo
5
8
PE
RU
CH
IL
E
Figure 13.1 Relief map of the Atacama Desert obtained by interferometric C-band radar
from the space shuttle Endeavor (NASA/JPL/NIMA) showing principal hunter-gatherer
archaeological sites discussed in the text: (1) Quebrada Jaguay; (2) Ring Site; (3) Quebrada
Tacahuay; (4) Los Burros; (5) Acha and Chinchorro sites; (6) Camarones; (7) Punta
Pichalo; (8) Tiliviche and Aragon; (9) Patillo; (10) Las Conchas.
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People of the Coastal Atacama Desert
varied ecological and archaeological data to discuss the principal issues of the
natural and cultural history of the region, from the late Pleistocene to the late
Holocene (ca. 12,000–4,000 bp).
The Ecological Setting of the Atacama Desert
The Atacama/Peruvian Coastal Desert is one of the driest places on earth. Hyperar-
idity has been present in the central Atacama for at least the last 15 million years,
although recent studies have documented environmental changes (Betancourt et al.
2000; Grosjean and Nunez 1994; Latorre et al. 2002). These paleoecological changes
greatly affected the distribution of animals and plants as well as that of past human
populations in this region. This desertic landscape, located on the west coast of
South America, extends for more than 3,000 km along a narrow strip from northern
Peru (Lat. 58S) to northern Chile (Lat. 278S). It owes its existence to the drying effect
of the cold northward flowing Humboldt Current, the existence of air masses
associated with the sub-tropical high known as the South Pacific Anticyclone, and
to the rain-shadow effect of the Andean mountain ranges, which impedes the
penetration of moisture carried by the eastern trade winds. Although this desert is
continuous from Peru to Chile, it is usually broken into two main components.
The Peruvian Coastal Desert extends from Tumbes (ca. 58S) to Tacna in southern
Peru (ca. 188S), and the Atacama Desert from the area of Arica in northern Chile
(ca. 188S) to Copiapo (ca. 278S) (Marquet et al. 2002; Rauh 1985).
The northern part of the Peruvian Coastal Desert consists of a wide coastal plain
with shifting sands known as the Sechura Desert, some 100–150 km wide. During
the terminal Pleistocene and Holocene this coastal desert provided more favorable
living conditions in the form of spring water and shallow lagoons with fresh water,
as documented in Pampa de los Fosiles in the Cupisnique Desert, of northern Peru.
Further south in the Peruvian Coastal Desert, thick cloudbanks form over the
desert lands as a result of the cooling effect of the Humboldt Current, as similarly
occurs with the cold Bengela Current in the Namib Desert. When intercepted by
isolated mountains or steep coastal slopes, this cool moist air gives rise to a fog
zone known as garua in Peru and camanchaca in Chile. This moisture allows for
the development of isolated and diverse vegetation formations called lomas (small
hills), where plants are adapted to condense this humidity. The lomas, comprising
communities of annual and perennial plants (Herbaceae and Gramineae) and cacti
(Dillon 1997; Rauh 1985), grow vigorously during a short period in the winter of
the Southern Hemisphere, and attract a wide variety of animals and birds (came-
lids, rodents, foxes). These ephemeral ‘‘fog oases’’ (Lavallee 2000) were occupied
seasonally by hunter-gatherers whose base camps were located on the nearby coast
(Benfer 1999; Quilter 1991).
The Atacama Desert, located between 188S and 278S, can be divided in three
sections: north, central, and south (see Figure 13.1). The latter, being the driest, has
negligible archaeological data and thus is not described herein. Flanked to the east
by the high Coastal Cordillera, the littoral offers discrete bays and beaches for
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Santoro , Arriaza , Standen , Marquet
human habitation, experiencing a mild climate (see Figure 13.2). In contrast to
other Southern Hemisphere deserts (such as in Australia and southern Africa)
average yearly precipitation is near zero. Thus the supply of fresh water depends on
rain events outside the desert caused by convective air masses that cross the Andean
crest bringing moisture laden air across the altiplano from the Amazon Basin. This
phenomenon of the austral summer known as the invierno boliviano (the Bolivian
or altiplanic winter) is responsible for the radical fluctuation of superficial runoff
and groundwater that typically flows from the western slopes of the Andes to the
Pacific. In the northern Atacama the runoff creates narrow and deep quebradas
separated by 20–30 km of barren terrain with no vegetation at all. As rainfall
gradually declines toward the south the quebradas do not reach the ocean, but
rather discharge into inland basins, such as the Pampa del Tamarugal and Salar de
Atacama in the central Atacama. The southern Atacama (248–278S) is a territory
with no human habitation until recently, known as the despoblado (depopulate) de
Atacama. In sum, although terrestrial biomass production is scanty and sparse, the
existing water network, a distinctive feature of the Atacama Desert, offers a
predictable resource for hunter-gatherers and fishermen.
Figure 13.2 Typical landscape in the coast of the Atacama Desert flanked to the east by the
high Coastal Cordillera, leaving discrete bays and beaches for human habitation, with a
rather mild climate. The arrow shows shell middens of a permanent Holocene camp, south
of Camarones Valley.
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People of the Coastal Atacama Desert
In contrast to limited terrestrial resources, the ocean offers a great variety and
quantity of fish, molluscs, sea mammals, sea birds, and algae. This high productivity
is triggered by a series of oceanographic, geographic, and climatic factors that
produce very high levels of biomass (Llagostera 1992; Nunez 1983; Schiappacasse
and Niemeyer 1984; Yesner 1980) crucial to the establishment of relatively perman-
ent human occupations along the coast of Peru and Chile appearing in the late
Pleistocene (Lavallee 2000; Llagostera 1992; Nunez 1983; Sandweiss et al. 1998, 1999;
Schiappacasse and Niemeyer 1984). The Atacama Desert would have had a com-
pletely different cultural history if human populations had depended exclusively on
terrestrial resources, as did many groups of the arid zone of interior Australia and the
Kalahari (Hank 2002a). The combination of coastal and terrestrial resources is also
observed in the Namib Desert, though the latter contains a much larger terrestrial
biomass in terms of edible plants and animals (Hank 2002b).
The northern section, known as the Fertile Coast, is characterized by five valleys
or quebradas that traverse the desert (see Figures 13.1 and 13.3). In the Peruvian
Desert to the north, more than 50 wider valleys reach the coast (Lavallee 2000). At
the mouth and upstream of these valleys one finds localized habitats in the form of
oases, which host fruit-bearing plants such as Prosopis (a mesquite-like tree found
Figure 13.3 Typical valley mouth in the northern Atacama Desert. Rich habitat for hunter-
gatherers and fishermen, who enjoyed marine and oasis resources and permanent, though
brackish, water (a key feature). The shell midden in the foreground of the picture corres-
ponds to Camerones 14, a permanent early Holocene camp.
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Santoro , Arriaza , Standen , Marquet
in patches), small game (such as Ctenomys, a gopher-like fosorial animal), and
camelids (guanaco – Lama guanicoe), abundant sea birds, small quantities of
freshwater fish and crayfish, roots of reed and tomatillo (Lycopersicon chilense),
and potable water. People also appear to have moved upstream to look for lithic
raw materials, a resource which is noticeably absent on the coast. Conditions in the
terminal Pleistocene appear to have been more lacustral than today, with fluctu-
ations of a magnitude that are seen to have had varying effects on human popula-
tions – an issue which is still under vigorous debate (Grosjean and Nunez 1994;
Latorre et al. in press; Nunez et al. 2002; Usselmann et al. 1999).
The central Atacama lacks the coastal oases, with fresh water restricted to
brackish springs. The landscape is essentially barren and vegetation is restricted
to lomas, the vegetation depending on the coastal fog which is reduced in extent
along the coast and the Pampa del Tamarugal. This is a large inland basin
connected to 15 to 20 quebradas, with Aroma, Tarapaca, Chacarilla, Guatacondo,
and Manı being the most important (Luis Briones pers. comm.), and a series of
salares (ancient dry lakes) located behind the Coastal Cordillera. These interior
basins experienced wetter conditions by the end of the Pleistocene and also
possibly the Holocene (Latorre et al. in press).
The Peopling of the Region and Possible Migratory Routes
Three human migratory routes have been proposed for the colonization of this
desert zone by the end of the Pleistocene, linked to colonists entering South
America through the Isthmus of Panama (ca. 13,000–12,000 bp). In the first
route, people are argued to have moved from the Amazonian Basin to the cold
territories of the high Andes. On the coast of the Atacama Desert these late
Pleistocene immigrants are argued to have become hunter-gatherers and fisher-
men. Recent mitochondrial DNA analyses from late Holocene human remains of
the Atacama (ca. 4,000 bp) illustrate a strong genetic link with current tropical
forest populations (Moraga et al. 2002; Rivera and Rothhammer 1986, 1991). This
does not necessarily mean, however, that all cultural traits found in the Pacific were
imported from the Amazon Basin.
The second migratory route assumes that specialized hunter-gatherers, with
sophisticated lithic industries, colonized the Andes from northern Colombia,
next to the Isthmus of Panama (Rothhammer et al. 1984). According to Grosjean
and Nunez (1994), during the mid-Holocene a period of drought affected the
highlands of the central Atacama Desert, causing the shrinking of lakes and the
reduction of biotic resources with a subsequent loss of hunting opportunities (but
see Latorre et al. 2002; in press, for a different paleoecological perspective).
Settlements are seen to have been abandoned, creating a silencio arqueologico
(‘‘archaeological silence’’) as residential groups became more mobile or people
concentrated in local refuges or moved to the coast (Nunez 1983).
Neither of these two hypothesized migratory scenarios is currently supported, as
recent archaeological data show that the first permanent settlements occurred
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People of the Coastal Atacama Desert
slightly earlier on the coast (ca. 11,000 bp; Sandweiss et al. 1998) than within the
highlands, where occupation is dated to ca. 10,800–10,600 bp (Nunez et al. 2002).
A third route proposes a migration along the coast from North America, with a
population carrying an unspecialized lithic industry adjusted to coastal and marine
environments (Llagostera 1992). Lavallee (2000) suggests that people used water-
craft to cross the Pacific Ocean from Siberia to Alaska by the end of the Pleistocene.
This is plausible given that colonists of Australia used watercraft to cross a similar
distance from Southeast Asia along the Wallacean Islands some 40,000 years earlier
than the first Americans (cf. Mulvaney and Kamminga 1999). Although this is an
interesting and challenging hypothesis, it requires further archaeological testing
using dated sequences from both the coast and interior.
The First Coastal Squatters (11,000–10,000 bp)
Evidence for the earliest late Pleistocene inhabitants is difficult to find, since most
of the sites are now located on drowned landscapes. Richardson (1981) has
suggested investigating littoral zones with narrow continental shelves, where the
rising ocean caused less horizontal displacement of the shoreline (see Chapter 10,
this volume, for an extended discussion of this issue in the Australian context). It is
precisely this kind of context that has allowed the preservation above modern sea
level of the sites of Quebrada Jaguay, Quebrada Tacahuay, Ring Site, and Las
Conchas (see Figure 13.1). For areas with less steeply declining continental shelves
few archaeological sites are found along the coast before ca. 6,000 bp, when much
of the current coastline formed and was settled. The same phenomenon is de-
scribed for the coast of the Namib Desert (Hank 2002b) and accounts for the
appearance of later occupation of the Australian coast, as well as the coast of south
central Chile (Quiroz and Sanchez 2004).
The earliest known occupation of the Atacama Desert took place at the end of
the last glacial period, which was characterized by more humid conditions in the
highlands between 13,000 and 9,500 bp, thereby providing the coast with higher
discharges of freshwater. This process created exceptional estuarine habitats at the
mouths of major valleys and small quebradas, including the formation of shallow
freshwater lagoons, such as is found at the Ring Site (Sandweiss et al. 1989).
The earliest archaeological sites are dated to around 11,000–10,000 bp and
correspond to groups with ‘‘specialized fish-netting technology,’’ as recorded in
Quebrada Jahuay, the Ring Site, and Quebrada Tacahuay (Keefer et al. 1998;
Sandweiss et al. 1989, 1998). According to Sandweiss et al. (1998, 1999), site QJ
280 at Quebrada Jaguay is the only base camp dated to the late Pleistocene (ca.
11,105–11,088 bp), with evidence of post-holes representing an early form of
architecture (Daniel Sandweiss, pers. comm.). It is interesting to note that people
appear to have specialized their prey strategies in the capture of a single taxon of
fish from the family Sciaenidae (calculated to be 17 cm in length, based on the size
of the otoliths), and Mesodesma donacium, a species of mollusc bivalve normally
found in sandy beaches (Sandweiss et al. 1998, 1999). Site QJ 280 also presents
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abundant lithic debitage from the production of bifacial and unifacial artifacts,
including obsidian that was imported from outcrops located 130 km inland, at an
altitude of 2,850 m above sea level (asl) (Sandweiss et al. 1998). This suggests that
people operated within a large territorial range extending from the coast to the
Andes. At Tacahuay, a logistical camp with dates beginning ca. 10,800 bp, there is
also an extraordinary preference for small schooling fish of the same average size
and taxon (anchovies – Engrundis ringens, anchoas – Anchoa spp., shad, herring),
and sea birds such as cormorant and boobies (deFrance et al. 2001). The use of
fishing nets is inferred from the standardized size of the fish and the finding of a
net fragment at Quebrada Jaguay dated to the Holocene (Keefer et al. 1998).
In the Holocene there is evidence for people diving in the sub-tidal zone to
procure molluscs using an extraction tool known as chope used to pry molluscs
from rocks, for hunting with harpoons for large fish and marine mammals such as
sea lions (Otaria juvata and O. flavescens), for fishing with fishhook and fishing
lines, and for the collection of algae. The lack of similar evidence in the terminal
Pleistocene assemblages suggests that during the late Pleistocene and early Holo-
cene people employed different procurement strategies to access marine and
terrestrial resources.
Gifted Holocene Hunter-Gatherers (10,000–4,000 bp)
As deduced from several sites along the coast and the inland basin, by 10,000 years
ago, human groups in both the northern and central sectors of the Atacama Desert
employed a more specialized maritime economy, incorporating an integrated
transhumance system (Nunez 1983). The archaeological sites along the coast
comprise extended and more permanent open camps with shell middens that
cover several square kilometers and which have a depth of more than 4 m, such
as the Punta Pichalo site excavated by Bird in the 1940s (Bird 1943) (see Figure
13.4). Occupants employed a sophisticated tool kit that included fishhooks of
vegetal thorns, weights and composite sinker hooks made of bone, ring-necked
nets (chinguillo), and harpoon heads made of bone. They also manufactured a wide
variety of lithic tools used as projectile points, knives, and scrapers. Obsidian
implements and debitage are common at the coastal sites (Munoz 1993), indicating
that foraging included journeys to the interior highlands and/or that these and
other materials were obtained through exchange networks with peoples of these
interior areas. By the mid-Holocene (after ca. 7,000 bp) maritime technology
evolved to include fishhooks manufactured from Choromytilus chorus shell, awls,
polishers, lanceolates and double points, burins, knife blades made on thick bifacial
preforms, grinding stones, hand stones, choppers, multipurpose flaked tools made
out of chalcedony and basalt, wooden darts, bags stitched with fiber, cords, and
reed mats. Later in the Holocene (ca. 4,000 bp) the manufacture and use of shell
beads and pendants, fringed skirts, reed brushes, lithic artifacts with ocher, and
pelican skins appear in the archaeological record, pointing to the beginning of a
new cultural era.
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People of the Coastal Atacama Desert
The lack of terrestrial animals appears to be ‘‘compensated’’ by the hunting of
sea lions which were hunted with harpoons while asleep on rocky foreshores
(Standen 2003). Molluscs were another source of protein, principally loco (Con-
cholepas concholepas), lapas (Fissurella spp.), and chorito maico (Perumytilus pur-
puratus) (Luis Briones pers. comm.). The size of these species corresponds to
individuals normally found in the intertidal and supratidal zones of rocky beaches.
The evidence for watercraft at this time is still uncertain and seems to have been a
later technological development.
Sites in the inland basin of Pampa del Tamarugal such as Tiliviche and Aragon
(see Figure 13.1), located 40 km from the littoral and about 950 m asl, appear to
have served as transitory logistical camps. It is thought that groups traveled there to
gather raw material for lithic artifacts, to collect reed fiber, to gather scanty
terrestrial plants, and to hunt small game. These camps were occupied from
9,000–4,500 bp when this region experienced wetter conditions (Latorre at al. in
press). At Tiliviche there is evidence for domestic structures consisting of simple
circular and shallow depressions surrounded by post-holes dug into the hard
ground of the terrace (Nunez 1983; see Figure 13.5). These kinds of wind shelters
were possibly covered with reed mats, fur, and branches. Domestic refuse was
dispersed around these enclosures, and after their abandonment, they were covered
Figure 13.4 Shell midden at Punta Pichalo in central Atacama Desert, which demonstrates
the permanent and intense occupation of the coast based on a hunting-gathering marine
economy, during the Holocene (picture taken by Junius Birds in 1939; reproduced courtesy
of the American Museum of Natural History). Grete Mostny, fomer Director of the Museo
Nacional de Historia Natural, is shown in the right corner.
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Santoro , Arriaza , Standen , Marquet
by refuse from nearby dwellings (see also Quiani 9, a middle Archaic camp, located
in the south of Arica; cf. Munoz 1993).
Social and Ideological Complexity in the Atacama Desert Coast
According to Arriaza and Standen (2002), one of the most remarkable aspects of
coastal Atacama Desert people were the processes they used to mummify their
dead. This cultural trait is labeled ‘‘Chinchorro’’ after the name of a beach, north of
Arica, where the first evidence was found by Max Uhle, early in the twentieth
century (Uhle 1919). Geographically this phenomenon has a rather narrow distri-
bution from Ilo in southern Peru, to Patillo south of Iquique, approximately
300 km in length (see Figure 13.1); to date there is no evidence of artificial
mummification away from the coast. The earliest evidence to date for mummifi-
cation was located at the mouth of the valley of Camarones (see Figures 13.1 and
13.3), where Virgilio Schiappacasse y Hans Niemeyer established the association of
domestic debris and Chinchorro inhumation. These findings in the Atacama
represent the most ancient (ca. 8,000–7,000 bp and 3,500 bp) artificial mummi-
fication known in the world, a typical trait of the northern and central Atacama
Figure 13.5 Open camp of Tiliviche, an inland oasis around 40 km from the coast. Post-
holes correspond to an early Holocene wind breaker (photo courtesy of Lautaro Nunez).
Note the shallow midden deposit compared with Punta Pichalo (Figure 13.3).
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Desert. South of Patillo, still in central Atacama and in the southern Atacama,
artificial mummification was not part of the Huentelauquen Tradition linked to
the Las Conchas site (see Figure 13.1) in Antofagasta (Costa-Junqueira 2001;
Llagostera et al. 2000). Although natural mummification was likely known to the
Chinchorro, they created their own unique artificial mummification methods.
These methods drastically transformed the bodies, halting decomposition, and
were seen to allow the dead to ‘‘participate’’ in a new social context of unknown
meanings within an egalitarian social system. It is important to note that the
highland and coastal hunter-gatherers of western South America developed a
wide variety of procedures to ‘‘manipulate’’ their dead. These practices become
associated with ceremonial centers linked to the elite of highly stratified societies of
the central Andes (Santoro et al. in press).
Arriaza and Standen (2002: 23) point out ‘‘societies with centralized socio-
political power and class differentiation would have richer and more sophisticated
mortuary rites allocated for elite members than hunter-gatherer societies.’’ They
created a ‘‘variety of techniques of artificial mummification that transformed the
bodies into gleaming black or red statues, a sharp contrast to the opaque shades of
the desert’’ that rivals those of complex societies. Arriaza (1995) classified the body
preparation procedures as black, red, bandaged, and mud-coated mummies. The
black, red, and bandaged mummies correspond to the category known as complex
preparation (Uhle 1919). This great variety of mummification methods changed
through time from black to red, and from red to mud-coated techniques.
The ‘‘black mummies’’ were the most elaborate, requiring more time and
knowledge of anatomy for their preparation. Examples of these mummies have
been radiocarbon dated from 7,000 to 4,800 bp. According to Arriaza and Standen
(2002), these bodies were completely skinned, disarticulated, and the organs and
muscles were removed. Subsequently, the skeleton was rearticulated and the bones
reinforced with sticks and reeds. The body cavities (head and trunk) were stuffed
with ashes or dry grasses. Later, they modeled the entire body with an ash paste,
recreating the original volume of the corpse. Following this process, the morticians
reattached the skin, possibly the body’s own or that of an animal (seal or sea lion)
and the head was adorned with a short, black haired wig. The Chinchorros also kept
and modeled some of the facial features and genitalia. As a final touch they painted
the mummy with a thin layer of black-blue manganese paste; hence the reason for
the title ‘‘black mummy’’ (Arriaza and Standen 2002: 29).
The ‘‘red mummies’’ were simpler than the black ones in their preparations,
characterized by incisions and sutures at the shoulders, groin, knees, and ankles
with the objective of removing the organs and part of the muscles. The head was
disconnected from the trunk and the brain removed. All the body cavities were
dried with glowing coals and ashes, a custom known also in the coast of central
Peru, where people added salt to treat their dead (Benfer 1999). Wooden poles were
slipped under the skin through the arms, legs, and spine of the deceased to provide
support and rigidity. The cavities were stuffed with feathers from sea birds
(pelicans, seagulls), different types of soils, and wool from camelids (llamas
(Lama glama), alpacas (Lama paco), guanacos, or vicunas (Vicugna vicugna), the
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other wild American camelid only found in the high Andes, >4,000 m asl). The
head was treated similarly – they added a long wig made from locks of human hair
and a paste of manganese paint for the face, modeling the facial characteristics, as
well as securing the wig to the head. Afterwards, the entire body except the face and
wig was painted with red ocher. This red style first appeared approximately 4,000
years bp and continued for almost 500 years (Arriaza and Standen 2002).
The ‘‘bandaged mummies’’ were basically a variation on the red mummies
except the skin was reattached in the form of bandages. The ‘‘mud-coated mum-
mies’’ were naturally dried bodies that were covered with a layer of mud, possibly
prepared with a mixture of earth, water, and an adhesive of unknown origin
(Arriaza and Standen 2002).
Why did these groups expend so much energy and engage in such complex
procedures to prepare their dead? Perhaps it was thought that the dead were going
to face an unknown world of supernatural metaphysical forces or perhaps, instead,
they would start a new life within their own community; therefore becoming a new
category of social actor. It may be that their function was to mitigate the impact
their death caused in their own social group. We do not know the reasons why
different mummification procedures were applied to members of the same group
and if the members who received greater attention enjoyed greater social prestige
during their lifetime and had certain privileges that they maintained even after
death. These questions warrant further investigation.
Arriaza and Standen (2002) suggest that through the act of mummification
groups produced inanimate beings with simultaneous spiritual bonds to the living,
their ancestors, and to the gods. Particularly, it might be possible that post-mortem
manipulation of the dead began due to beliefs that ‘‘the soul of the deceased runs
the risk of losing its existence if the body decomposes, or the living would lose
contact with the soul of the deceased should the body decompose’’ (Arriaza and
Standen 2002: 40–1).
Thus, these mortuary rituals may have been necessary to ensure the eternal
existence of the body and the soul of the deceased, as well as the continuity of the
group (Arriaza and Standen 2002: 40–1). What is certain, however, is that the
Chinchorro invested a considerable amount of time and energy in mummifying
their dead, which makes these mummies a unique phenomenon in the world, as
much for their antiquity as for the social context in which they were produced. The
technical knowledge and ideological concepts tied to mummification, as well as the
subsistence patterns which underpinned these, all required a system that allowed
for the preservation of a historic memory for several millennia. To ensure the
cultural continuity of such a legacy from one generation to the next, people
adopted a course of action which included mummification. This practice may
have served to preserve internal cohesion, reinforce social integrity, and perpetuate
a collective historic memory. The momentum created by the actual process of
mummifying a newly deceased member of the community may have created a self-
sustaining milieu for the Chinchorro people. Codes of social conduct could be
instilled during the process of mummification, as this practice may have created
the necessary conditions for cultural transmission and reproduction.
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People of the Coastal Atacama Desert
Conclusion
The cultural history of the people in the Atacama Desert can be divided into three
major epochs, summarized as follows. The early epoch corresponds to immigrants
arriving on the coast of the Atacama no later than 11,000 bp at Quebrada Jaguay
and Quebrada Tacahuay, north of Arica. The available archaeological data show
that these people were equipped with simple and non-specialized technologies and
focused their procurement on a narrow spectrum of molluscs, sea birds, and fish.
There is, however, evidence for the possible use of nets for fishing, even at this early
stage. Populations also occupied the high Andes at altitudes of 3,000–4,500 m asl
on the margins of the desert from around 10,800 bp, but here they employed a
more technologically sophisticated lithic industry characterized by highly formal-
ized tools for the capture and butchering of large game (including camelids,
deer, and occasionally the American horse), as well as small rodents and birds
(Aldenderfer 1999; Nunez et al. 2002; Santoro and Nunez 1987). This different
adaptation may be linked to the arrival of two cultural ‘‘traditions’’ to the Atacama
Desert, which maintained their character through prehistory. While the modern
descendents of these original coastal peoples are hard to distinguish among the
current population of the coastal cities, the highland people have survived
the pressure of European invasion and the acculturation trends of the modern
republic and today they assert different forms of social and ethnic recognition.
The first populations detected archaeologically in the Atacama may be related to
earlier immigrants into the Americas, from 13,000–12,000 bp (or even earlier).
They may have moved rapidly through new lands, as Birdsell (1977) suggested for
Australia, leaving behind parties that started the more serious process of coloniza-
tion as seen in Quebrada Jaguay (site QJ 280) at around 11,000 years bp (Sandweiss
et al. 1989). This fast movement of the colonists is consistent with the tight
chronological sequence of the first Americans, given that there is no clear chrono-
logical gap between the earliest known settlements in North vs South America. In
fact, the earliest Paleo-Indian site in the South Americas is Monte Verde, south of
Chile, dated between 13,500 and 12,500 bp, with other early sites from Patagonia
(i.e., Cueva del Medio, Piedra Museo, and Los Toldos) dated to between 12,390 and
12,890 bp (Massone and Prieto 2004). The occurrence of later dates for the first
occupants of the Atacama Desert provides a challenge for future archaeologists to
investigate whether a cline in settlement of this desert has occurred (a lag effect) or
whether sites of comparable age have simply not been investigated yet or have not
survived due to taphonomic processes.
In the second epoch, dated to the Holocene, the coastal desert people show a
clear shift in their subsistence technology, as well as their social and ideological
strategies, which persevered, with only minor changes, for several millennia. The
material expressions of this new ideology seem to have been quite dynamic, as seen
in the wide variety of methods used for artificial mummification. Specialized
technological solutions for exploitation of marine resources were developed by
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the mid-Holocene, and remained in place with only minor changes until late
prehistory.
A distinctive feature of the hunter-gatherer-fishermen of the Atacama Desert was
the opportunity to engage in agriculture, afforded by the presence of valleys and
quebradas that cross-cut the desert in the northern section (see Figure 13.3). From
ca. 4,000–3,000 bp the introduction of agriculture is seen to complement a
maritime focused economy, thereby allowing desert people to establish permanent
settlements in the form of small hamlets, with simple architecture (wooden posts,
reed mats, and cane) of no more that 10 hectares in extension, as seen late in
prehistory. This kind of infrastructure is commonly found along the quebradas and
inland basins, such as Pampa del Tamarugal. Along the coast, people maintained
more simple open camps until the sixteenth century ad; the time of the European
invasion. This change in the way of life of the peoples of the coastal Atacama Desert
can be accommodated by the concept of the ‘‘Neolithic Revolution,’’ as coined by
the influential Australian archaeologist V. Gordon Childe, whose ideas were in-
corporated into the interpretation of Andean cultural history during the 1960s and
1970s. This ‘‘revolution’’ within the coastal economies of the Atacama did not
result in substantial change in staple foods, however, as these were still provided by
the ocean. Processes of social class differentiation and other cultural ‘‘sophistica-
tion’’ classified elsewhere as ‘‘civilization’’ took a different form here. The waves of
the ocean and the sand dunes of the desert witness a different human social
creation that we have attempted to shed some light on within this chapter.
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