iriarte 2006. world archaeology
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Landscape Transformation, Mounded Villages and Adopted Cultigens: The Rise of EarlyFormative Communities in South-Eastern UruguayAuthor(s): José IriarteSource: World Archaeology, Vol. 38, No. 4, Debates in "World Archaeology" (Dec., 2006), pp.644-663Published by: Taylor & Francis, Ltd.
Stable URL: http://www.jstor.org/stable/40024061 .
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Landscape
transformation,
mounded
villages
and
adopted
cultigens:
the rise of early Formative
communities
in
south-eastern
Uruguay
Jose Iriarte
Abstract
New research
in
lowland
South
America
is
beginning
to reveal a
diversity
of
complex
cultural
trajectories
n
a
region
that was
long-considered marginal
with
respect
to Andean and Mesoamerican
civilizations. This
paper
summarizes new
archaeological, palaeoecological
and
archaebotanical
data
from Los
Ajos
site,
south-eastern
Uruguay, showing
that a
changing
and
increasingly dry
mid-
Holocene climate was associated with
significant
cultural
transformations,
including
early
village
formation,
the
adoption
of a mixed
economy
and the construction of the earliest
public
architecture
known for the area.
Collectively,
this evidence indicates an
early
and
unexpected
development
of
social complexity that had not heretofore been recorded in this area of South America. Human-
environment
interactions,
social
processes
related to the
development
of
early village
life and the role
of
early public
architecture are discussed with reference to the
emergence
of
early
Formative
communities
in
the
region.
Keywords
Early
Formative;
middle-range
societies,
public
architecture;
Uruguay;
La Plata
Basin;
agriculture.
Introduction
Researchon the
emergence
and internal
dynamics
of
middle-range
ocieties
in
South
Americahas concentrated
mainly
on Andean coastal and
highland
valleys(Burger
1995;
Moseley
2001;
Solis et al.
2001),
and more
recently
n
the lowland forest
and riverine
regions
of
Amazonia
(Heckenberger
t al.
1999;
Lehmanet al.
2003;
Roosevelt
1999).
Historically
iewedas a
marginal
area when
compared
o the Andeanand Mesoamerican
chiefdomsand
states,
the La Plata basinand its
adjacent
ittoral
region
s a
large
and little
explored
area that is
beginning
to reveal an
early
and
long
sequence
of
unique
and
RRoutledqe
World
Archaeology
Vol.
38(4):
644-663 Debates in World
Archaeology
Tay.ors.Franciscroup
© 2006
Taylor
&
Francis
ISSN 0043-8243
print/
1470- 1375
online
DOI:
10.1080/00438240600963262
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Landscape transformation,
mounded
villages
and
adopted
cultigens
645
complex
cultural
trajectories. Multidisciplinary investigations
at
the Los
Ajos
archae-
ological
mound
complex
in
the wetlands of south-eastern
Uruguay
run
counter
to the
traditional view that the La Plata basin was inhabited by simple groups of hunters and
gatherers
for
much of the
pre-Hispanic
era
(Meggers
and Evans
1978;
Steward
1946).
The
renewed
community-focused archaeological program
at Los
Ajos
showed that
large
Preceramic mound
complexes
in
the
region
were not the result of
random,
successive
short-term
occupations
of mobile
hunter-gatherers
(Schmitz
et al.
1991)
nor the
burial
mounds or monuments of
complex hunter-gatherers
as
previously proposed
(Bracco
et al.
2000a;
Gianotti
2000;
Lopez
2001),
but
well-planned plaza
villages
built
by people
who
practised
a
mixed
economy.
In
this
paper,
I
present
new
archaeological, palaeoecological
and botanical data
indicating
that
during
an
increasingly
dry
mid-Holocene,
at around
4190
BP,
Los
Ajos
became
a
permanent
circular
plaza village
and its inhabitants
adopted
the earliest cultivars known in southern
South America
including
maize
(Zea mays
L.)
and
squash
(Cucurbita
spp.). During
the
following
Ceramic Mound Period
(between
around
3000 and
500
BP)
Los
Ajos experienced
the formalization and
spatial
differentiation of
communal
spaces through
the
development
of elaborated mounded
architecture around
the
central
plaza
area,
whose architectural
plan
reveals an
early
and distinct
form of civic-
ceremonial architectural tradition for South America.
Furthermore,
the
presence
of at
least four other mound
complexes
in the
region
with
closely comparable
dates and
similarity
in
their overall
plan
to
Los
Ajos suggests
that these mound
complexes
had been
integrated
at a
regional
level since Preceramic times
(see
Fig.
lb and Table
1) (Bracco
and
Ures
1999;
Iriarte et al.
2004;
Lopez
2001).
Brief
history
of
archaeological investigations
in
the
region
The
mound-building pre-Hispanic
cultures
dating
back to c. 4000
BP
are
generally
referred
to as 'Constructors de
Cerritos'
in
Uruguay
and are divided into the Umbu
(Archaic
Preceramic)
and Vieira
(Ceramic)
traditions
in
southern Brazil.
They
extend
along
the
coastal and inland wetlands and
grasslands
that occur in the Atlantic coast between
around 28° and
36°S
(Bracco
et al.
2000a;
Schmitz et al.
1991)
(Fig.
la).
The
study
region,
the southern sector of the
Laguna
Merin basin
(Fig.
lb),
is characterized
by
a
patchwork
of
closely packed
environments
including
wetlands,
wet
prairies, grasslands, riparian
forests, large stands of Butia palms and the Atlantic ocean coast. It has a subtropical
humid
climate
with
high average
temperatures
of 21.5°C
during
the summer and low
average temperatures
of
10.8°C
during
the winter. Total annual
rainfall
averages
1
123mm
(PROBIDES 2000).
The 'Constructors de
Cerritos'
are divided into two main
periods:
a
Preceramic
Mound Period
(hereafter PMP),
which
begins
around
4190
BP
and ends with
the
appearance
of ceramics
in
the
region
around
3000
BP;
and a Ceramic Mound Period
(hereafter
CMP),
which extends from around 3000
BP
to the Contact Period
(Bracco
et al.
2000a;
Iriarte
2003;
Lopez
2001)
(Fig.
2).1
Archaeological
research
in
Uruguay
and Brazil has been
permeated
by
theoretical
and
methodological
approaches
that have
hampered
researchers from
obtaining
the
information needed to examine the
processes
involved
in
the
development
of these
early
Formative societies.
During
the 1960s and
1970s,
the aim of the National
Programme
of
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646 Jose
Iriarte
Figure
A
Locationof 'Constructores e
Cerritos' tudied
egions
n
the south-eastern
ortion
of the
La Plata
Basin and its
adjacent
ittoral zone.
Figure
IB
Map
of south-eastern
Uruguayshowing
archaeological
ites:
1.
Los
Ajos;
2. EstanciaMai
Abrigo;
3. Puntasde San
Luis;
4. Isla
Larga;
. Los
Indios;
6.
Potrerillo;
. Craneo
Marcado.
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Landscape transformation,
mounded
villages
and
adopted cultigens
647
Table
1
Radiocarbon dates from
Los
Ajos
and other sites with Preceramic mound
components
from
Uruguay
Provenience Arbitrary Lab Dated Conventional 2-Sigma
(site)
depth
(cm)
number material 14C
yr
BP
cal.
yr
BP*
Los
Ajos
TBN
Trench,
sector 7
160-165 Beta- 158278 charcoal
1,050
±
40
1,050-920
(AMS)
sector
6 190-195 Beta-158281 charcoal
1,660
+
40
1,690-1,660
(AMS)
Mound Delta
205-210 Beta-158277 charcoal
2,960
+
120
3,400-2,740
Mound
Gamma,
sector
1/D
210-215 Beta-158279 charcoal
3,460
±
100
3,980-3,470**
sector 6/C 270-275 Beta- 158280 charcoal 4,190 ±40 4,840-4,580
(AMS)
Mound
Alfa,
Layer
III
280-285 URU 0052 charcoal
3,350
+
90
3,830-3,380**
285-290 URU 0033 charcoal
3,870
+
280
5,030-5,010
and
4,990-3,550**
295-300 URU 0034 charcoal
3,690
±
270
4,830-3,370**
340-345 URU
0089
charcoal
3,950
±
80
4,580-4,160
345-355 URU 0088 charcoal
3,750
+
140
4,520-4,470
and
4,450-3,710**
Punt
as de San Luis
Mound
II
Layer
II
URU 009 charcoal
3,550
+
60
3,980-3,680**
Layer III URU 009 charcoal 3,650 ± 50 4,100-3,840**
Layer
III URU
010 charcoal
3,730
±
100
4,410-3,830**
Isla
Larga
Mound
I
260-270 URU013 charcoal
3,660
+
120
4,380-3,670**
URU014 charcoal
3,630
+
60
4,100-3,820**
Potrerillo
Mound
I
basal
level URU 083 charcoal
3,790
±
90
4,420-3,900**
URU 165 charcoal
3,820
+
100
4,510-4,480
and
4,440-3,910**
Arroyo Yaguari
Lemos
Mound 27
UE02/level
11
Ua 18817 charcoal 3250
+
40 3569-3379
Yaguari
SI 6496 charcoal 3170
±
150 2962-3722**
Note:
Calibrations asedon Stuiver t al.
1998;
**C13/C12
atio estimated
Archaeological nvestigations
n
Brazil
(PRONAPA)
was to
develop
a
chronological
framework or the
yet
unstudied outh-eastern ector of the La Plata Basin
by applying
ceramic
sedation
(Meggers
and Evans
1969)
and
lithic
typologies
(Schmitz
1978,
1987).
Their
classificatory-historical
pproach
ocusedon
obtainingrepresentativeamples
rom
limited
test
units,
which allowed them to build
chronological elationships
f lithic and
ceramic
phases
but limited heir
ability
to
study
intra-site
patialrelationships.
Although
thepresenceof largeand numerousmound
complexes
an be surmised rom the regional
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648 Jose Iriarte
Figure
Chronological
hart or
south-eastern
razil
nd
Uruguay.
archaeologicalmaps
of
PRONAPA
publications
n
the inlandfreshwater
wetlandsof the
state of Rio
Grande
do
Sul
and
Uruguay,
these
investigators
ften
reduced he unit of
archaeologicalanalysisand interpretationo the study of individualmounds, which
prevented
hemfrom
studying ommunitypatterns Cope
1991:
214-
15;
Prietoet al. 1970:
map
2;
Ruthschilling
1989:
map
3).2
PRONAPA
archaeologists
nterpreted
moundsites
as
the resultof successive hort-term
occupations
of
hunters,
gatherers
nd fishers hat moved
seasonally
o
exploit
ocally
rich
environments
Brochado
1984;
Schmitz
et
al.
1991).
The
habitation
natureof the mounds
was inferredbased on the
identificationof
post-moulds,
hearths
and the
presence
of
domesticdebris
resulting
rom food
preparation,
ool manufacture nd
maintenance,
n
conjunction
with occasional
indings
of human burials.These
researchers ee
continuity
between he ArchaicUmbu Tradition
8000-2500bp)
of
generalized
unter-gatherers
nd
the PreceramicMoundoccupationsSchmitz1987).Theyalso envisiona directconnection
between he CMP
(Vieria
Tradition)
and the historic
Charrua
and Minuano
groups.
The
lifeways
of these
profoundly
ransformedhistoric
groups
were often
projected
nto the
past
and used as direct
ethnographicanalogues
to
interpret
he
archaeological
ecord
(Becker
1990;
Cope
1991;
Schmitzet al.
1991).
Agriculture
nd
cultigens
were
thought
to
have been
brought
by
the
Amazonian
Tupi-Guaranimmigrants uring
he late Holocene
(Schmitz 1991).
It is
hardly
surprising
that
this
interpretative
framework fitted
comfortably
with the
long-held
assumption
hat this
region
was inhabited
by marginal
hunter-gatherers
Meggers
and Evans
1978;
Steward
1946).
In
the
mid-1980s,
he
ArchaeologicalSalvageProgramme
f
the
Laguna
Merin Basin
(CRALM)
began
systematic
archaeological
ieldwork
n
Uruguay.
Initial
excavationson
small
two-paired
mound
sites,
which
yieldedcomplexarrays
of CMP
multiple
burials,
ed
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Landscape transformation,
mounded
villages
and
adopted
cultigens
649
these researchers o
characterize hese sites as ceremonial
and/or mortuary
n
nature
(Cabrera
t al.
1989)
and
typified
hese societiesas
complexhunter-gatherersdapted
o a
resource-richwetlandenvironmentLopezand Bracco 1994).While this earlyresearch
recognized
he
presence
of
large
mound
complexes
and their
high degree
of
similarity
n
groundplan,
as
well as the
presence
of an extensiveoff-moundarea associated
with the
mounds,
they generally
overlooked the
importance
of
conducting
work to articulate
mound
and off-mound ontexts o reveal
community
rganization.
However,
his renewed
work in
the
region
set the tone
for more advanced
studies on mound construction
techniques,analysis
of
mortuary
practices,
aunal
analysis,
as well as lithic and ceramic
technology
see
papers
n
Beovideet al.
2004;
Consenset al.
1995;
Duranand
Bracco
2000;
Gianotti
2000;
Lopez
and Sans
1999;
MEC
2001).
Unlike PRONAPA
researchers,
Cabrera
1992)
pointed
out
that there was a
rupture
between he 'Constructors
de Cerritos'and the historicCharnia
and Minuano
groups,
whichresulted
rom the dramatic ransformationshat historic
groupsexperienced
ue to
the
dissemination
f
European
diseases,
he
Spanish
military ampaigns
f
extermination,
the
Portuguese
slave-huntersand the introduction of cattle. These
transformations
severely
reduced their numbers and forced them to
change
their traditional
ifeways
significantly.
More
recently,
a re-examination f the earlierchroniclesand the
analysis
of
new
ethnohistorical ocumentsare
beginning
o show that the
groups
that inhabited he
area
were more
sedentary,displayed
a more
complex sociopoliticalorganization
and
practised
ood
production
Bracco
2004;
Cabrera
2000).
In
the
early
1990s,
new
investigations
n
the
upper
reshwaterwetlands
of IndiaMuerta
documented
he
presence
of
numerous
arge
and
spatially
elaboratedmound
complexes
and established he beginningof the PMP around 4000 BP(Bracco 1993). My own
preliminary
esearch
n
the area demonstrated hat the wetlandsof India Muerta
display
some of the
largest
and
spatially
most
complex
sites
in
the
region
(Iriarte
et al.
2001).
Mound sites are
circumscribed o wetland
floodplains
situated
in
ecotonal areas
characterized
y
a mosaic of
wetlands,
wet
prairies,grasslands, iparian
orestsand
palm
groves. They
showed a
dual distribution
pattern.
Small sites
(one
to three
mounds)
generally
ccur n
the wetland
loodplainspositioned
on
top
of the most
prominent
evees
following
he coursesof streams
and
exhibiting
a
linear/curvilinear
attern.
n
contrast,
n
the more
stable locations of the
landscape,
like flattened
spurs adjacent
to wetland
floodplains,
whichare secure rom
flooding
and have mmediate ccess o the rich-resource
and fertilewetlands,moundsites are arge,numerous ndspatially omplexcoveringupto
60ha.
These sites contain variedmounded
architecture
eometrically rranged
n
circular
(e.g.
EstanciaMai
Abrigo),elliptical e.g.
Damonte)
and horseshoe ormats
e.g.
Los
Ajos)
surrounding
central ommunal
paceaccompanied y
vast
outer
sectors,
which
generally
exhibit
more
disperse
and less
formally ntegrated
mounded architecture
Bracco
1993;
Braccoet al.
2000b;
Dillehay
1995;
Iriarte
2003;
Iriarte
et
al.
2001)
(Fig.
3).
New
research t
Los Indiosmound
complex Fig.
lb)
and the
Craneo
Marcadomound
(Lopez
2000,
2001;
Lopez
and Gianotti
1998;
Pintos
2000)
has led the excavators
to
interpret
he
beginning
of mound
building
as a
majorbreakthrough
n
the
history
of
the
hunter-gatherers
f the
region
marked
by
the monumentalization f the
landscape.
According
o
these
researchers,
moundsare
ceremonial
n
natureand
were built
through
discrete and
separate
construction
stages
using
refuse and sediments extracted from
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650 Jose Iriarte
Figure
3
Distribution
f moundsites
n
the
IndiaMuertawetlands
n
the southern ector
of
Laguna
Merin.
surroundingsoils. Within a landscape archaeology approach (Bradley 1998;Criado 1993),
these
investigators
have
interpreted
mounds
variously
as monuments
for the dead
(Pintos
2000),
ceremonial
spaces
and/or
territorial markers
(Gianotti
2000;
Lopez
2001;
Lopez
and
Gianotti
1998),
while the
adjacent
off-mound areas
are
generally interpreted
as the
living quarters
of these
populations.
Despite
these
advances
in
the
archaeology
of the Constructores de
Cerritos,
some
important questions
crucial to
understanding
the nature of Los
Ajos,
and
by
extension
the
large
multi-mound sites in the
area,
remain unanswered. Are these
large,
formally
laid
out
mound
complexes
the result of a succession of
randomly placed,
short-term
occupations
by
mobile
hunter-gatherers?
Are
they
burial mounds or monuments? Or
are
they
well-
planned villages incorporating public spaces? What is the occupational history
of these
sites? More
importantly,
what kind of subsistence did these societies
practise
and
what was
the
nature and
dynamics
of the societies that built these
complex
mound sites?
To address
these
questions,
I
carried out a
multidisciplinary
community-focused archaeological
investigation
at Los
Ajos
site,
which is described below.
Excavations
at Los
Ajos
Los
Ajos
is located in a flattened
spur
of the
Sierra
de Los
Ajos,
which overlooks
the
wetlands of
India Muerta. The first excavations
at Los
Ajos
by
Bracco consisted
of a block
excavation in Mound
Alfa,
a test unit in Mound Beta and a few
opportunistic
test units in
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Landscape transformation,
mounded
villages
and
adopted cultigens
651
off-mound
areas. This work established the mid-Holocene
age
of the earthen mounds
in
the area. The
Preceramic Mound Period
(PMP)
component
at Los
Ajos
yielded
five dates
between 3950 and 3350 BP(4580 and 3380 cal. BP) (Bracco 1993; Bracco and Ures 1999).
To reveal settlement
patterns,
our renewed
community-focused
excavation
programme
consisted of the
placement
of a block excavation in Mound
Gamma,
a test unit
in
Mound
Delta,
two trench transects
articulating
mound and off-mound areas and a 50m
systematic
interval transect
sampling strategy
of test units
to
target
off-mound
areas
totalling
an
excavated
area of 305m2. Our work showed that
Los
Ajos,
which
covers about
12
ha,
is
one of the
largest
and most
formally
laid out sites in the
study
area
(Fig.
4a).
Its Inner
Precinct
includes six
flat-topped, quadrangular platform
mounds
(called
6, Alfa, Delta,
Gamma,
4
and
7)
closely arranged
in
a horseshoe formation and with a
height
above
ground
level
of 1.75 to 2.5m
(Fig.
4).
Two
dome-shaped
mounds
(called
Beta and
8)
frame
the
central,
oval
plaza
with a size of 75
x
50m. The formal and
compact
inner
precinct
contrasts with more
dispersed
and
informally arranged peripheral
sectors,
which include
two
crescent-shaped
rises
(named
TBN
and
TBS),
five circular and
three
elongated
lower
dome-shaped
mounds,
borrow
pits
and
a vast off-mound area
bearing
subsurface
occupational
refuse. The
TBN
crescent-shaped
rise
(14-25m
wide and 0.40-0. 80m
tall)
extends over 150m
surrounding
Mounds Alfa and Delta. At its
base,
it becomes
wider
prolonging
to the
north east and
forming
a rounded
elongation facing
Mound
13. The
TBS,
a lower
(15-35cm)
and narrower
(4-8m)
arc-shaped
rise,
encircles Mounds
5, 8,
and 9.
The PreceramicMound Period
Our research
indicates that a series
of
major
social and economic
changes
took
place
at
Los
Ajos
during
the PMP.
The broad
contemporaneity
of
radiocarbon
dates,
artefact
Figure
A
Los
Ajos
site
planimetric
nd
topographicalmap. Figure
4B
The inner
precinct
modified
fromIriarte t al.
2004).
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652
Jose Iriarte
content
and similarities
in
Preceramic Mound
Component
(PMC)
stratigraphy among
mounds
Alfa,
Delta and
Gamma
suggest
that the Los
Ajos
inhabitants
began
to live
in
a
circular household-based community, partitioning the site into discrete domestic and
public
areas characterized
by
the
placement
of residential units around a central
plaza
area.
Eight
dates from Los
Ajos place
the PMC
occupation
between c. 4190 and 2960
BP.
The two oldest
dates from the basal levels of the
PMC
at Mound
Gamma
and Alfa
suggest
that
mound-building began
between around 4190 and 3950
BP
(4840-4160
cal.
BP)(Iriarte
2003;
Iriarte et al.
2004).
Excavation at Mound
Gamma indicates that it
grew
as a result of
multiple overlapping
of domestic
occupations
where a wide
range
of activities associated with food
preparation,
consumption,
stone tool
production
and maintenance took
place.
The PMC
Layer
4 is
characterized
by
an
85cm-thick,
compact, very
dark brown
silty
loam
organic
sediment
consisting
of
relatively
undifferentiated
deposits composed
of lithic
debitage
and
tools,
small
fragments
of charred
bone,
ash and
soot
lenses,
and
small
pieces
of burned
clay
(Fig.
5).
The
combined
analysis
of
stratigraphy,
features,
artefact and ecofact
composition
and horizontal
spatial
distribution of lithic
debitage
density
indicates
that,
during
the
PMC,
Mound Gamma was a residential
area that
grew through
the
gradual
accumulation
of
occupational
refuse.
Despite
intensive hand excavation and the
large
block excavation
placed
in
the
center
of the
mound,
no house features were identified.
However,
lithic
debitage
horizontal
density
trends show a consistent
pattern
characterized
by
the
presence
of a central area
of low
density
and a
periphery exhibiting higher
artifact
density.
The
central zone of the mound is
interpreted
as a
regularly
maintained habitation
space
and
the
periphery
as a zone where
trash was
deposited
(Iriarte 2003).
The central plaza area, located around the domestic accretional mounds, is
characterized
by
low artefact densities
and a lack of
anthropogenically
altered soil
accumulations.
Thin
occupational
refuse
(10-20cm)
was
deposited
in
the
TBN
and TBS
crescent-shaped
rises. The
systematic
interval transect
sampling
in the off-mound areas
documented
a vast outer area of
subsurface domestic
debris which does not show
accumulation of
anthropogenic
soils.
Figure
5
Stratigraphy
f Mound Gamma
modified
rom Iriarte t al.
2004).
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Landscape transformation,
mounded
villages
and
adopted
cultigens
653
The lithic
assemblage
indicates that tool
manufacture,
use and maintenance took
place
at
Los
Ajos.
Local raw
materials,
mainly rhyolite
and
quartz,
were
brought
to the
site,
where
all stages of lithic reduction are represented, including core reduction, tool manufacture,
use and
maintenance/rejuvenation.
The tool
assemblage
is characterized
by
a
generalized,
non-specific assemblage
that includes a broad
range
of different
tool-types displaying
a
wide
variety
of
edge angles including
flake-knives,
end-scrapers, wedges,
notches,
point/
borers and hafted bifaces
indicating
that Mound
Gamma
was a
domestic
area where a wide
range
of activities were carried out
(Iriarte
2003;
Iriarte and Marozzi
in
press).
Plant and animal remains at
Los
Ajos
indicate that
PMP
people adopted
a mixed
economy shortly
after
they began
to live
in
more
permanent villages.
Medium to
large-sized
mammals like deer
(Ozoterus
bezoarticus and Mazama
gouazubira)
and
semi-aquatic
rodents such as otter
(Myocastor coypus)
and
capybara
{Hidrochoerus
hydrochaeris)
dominate the
bone
assemblage.
Other medium to small-sized
mammals,
including
small
rodents such as
rat-otter
{Holochilus brasilensis),
'aperea'
(Cavia
sp.)
and mouse
(Cricetidae),
in
addition to
opposums (Didelphis
alventris
and
Lutreolina
crassiculata)
and
armadillos
(Dasypus sp.
and
Euphractus
sexintus),
are also
present. Reptiles
like lizard
(Tupinambis
merianae)
and turtle
(Chelonia),
birds such as Greater Rhea
(Rhea
Americana),
dove
(Zenaida auriculata)
and Great
grebe (Podiceps
major)
and freshwater fish were also
recovered
in
minor
quantities.
A
large part
of the bone
assemblage consisting
of distinctive
spiral
fractures,
bone
splinters
and charred bones
exhibiting
cut marks indicate that
processing
and
consumption
of medium and
large
mammals took
place
in
Mound Gamma
during
the PMC
(Iriarte 2003).
Phytolith
and starch
grain analyses
documented
seeds,
leaves and
roots from a
variety
of wild and domesticated
species
marking
the earliest
occurrence of at least two domesticated crops in the region: corn (Zea mays) and squash
(Cucurbita
spp.) shortly
after 4190
BP
(Iriarte
in
press;
Iriarte et al.
2004).
The close
association between
large
mound
complexes
and the most fertile
agricultural
lands
in the
region suggest
that
PMP
people practised
flood-recessional
farming. During
the
spring
and
summer
months,
organic
soils are
exposed
on the wetland
margins.
These
superficial peat
horizons are
highly
fertile,
hold moisture and are
easy
to till.
Furthermore,
the
floodwater of
the
nearby
Cebollati River
periodically
inundates the area and
replenishes
the soils
with
nutrients,
which makes the India Muerta
wetlands
an
ideal
locale
for the
practice
of
wetland
margin
seasonal
farming
(Iriarte
2003;
Iriarte et al.
2004;
Juan Montana
pers.
comm.
2000).
Our associated
palaeoecological
data indicate that the
major
cultural transformationsthat
occurred
during
the
PMP
were associated with
significant
climatic
changes (Iriarte 2006;
Iriarteet al.
2004).
The
mid-Holocene between c. 6620 and 4020
(7580-7440
to 4570-4410 cal.
BP)
was a
period
of
significant
climate fluctuation marked
by increasing aridity.
At around
4020
BP
a maximum
drying episode
occurred,
as
evidenced
by
a massive
spike
of
Amaranthaceae/Chenopodiaceae coupled
with a
sharp drop
in
wetland
species.
The
maximum
drying episode
that took
place
around 4020
BP
probably
caused a decrease
in
the
surface water
recharge
to the
inland wetlands and
waterways,
which resulted
in the
desiccation of
grasslands.
This caused
increasing diminishing
returns from
grasslands,
deepening
the resource
gradient
between wetlands and
grasslands. Although
reduced
in
extent,
wetlands became attractive
places
for
pre-Hispanic populations by providing
abundant,
now more
highly
circumscribed
plant
and animal resources and a stable source of
water. The Los
Ajos
site indicates
that,
during
this
period,
local
populations
did not
disperse
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654
Jose Iriarte
(e.g. disaggregate
nto smaller
groups
and increased
mobility)
or
out-migrate
to
other
regions
but
opted
for
orienting
their settlement towards the
upper
freshwater wetlands where
they
established more permanent communities. Increased sedentism appears to have been a
response
to
local resource abundance
in
wetland areas
in
the face
of
regional
resource
scarcity
produced by
the
drying
trend of the mid-Holocene
(Iriarte
et al.
2004).3
The
making
of
early
Formative communities: he Los
Ajos plaza village
The Los
Ajos plaza village
materialized a series of social
processes
that unfolded
during
the
PMC. When these
populations
became less mobile
and
began
to
aggregate
more
frequently
in
larger
communities,
the
problems
associated
with
forming
and
remaining
in
large groups
for
longer
periods
of time surfaced. The
incorporation
of
a central and
communal
space may
have
played
a crucial role as a social
integrative
facility (sensu
Adler
and Wilshusen
1990),
representing
the formalization of a wider social field of interaction
that
transcended the household
sphere.
Plazas are an
early prototype
of
public
architecture that
lies
at
the root of
complex
societies
in
the Americas
(Lathrap
et al.
1977).
Embodying
shared
public space,
they
constitute a threshold
in
terms of the
appropriation
and the transformation of
social
spaces,
which take
through
time
particular
sets of
meanings
and connotations
in the social
realm. Plazas not
only
represent
the
tangible
formalization of
group-level integration,
but,
as
prominent
and fixed
constructions,
they perpetuate
and sediment these
relations in
place (Dillehay
1992a;
Moseley
2001;
Sassaman and
Heckenberger
2004).
It is
in
this new
arena that communities diffuse tensions and promote social cohesion. There they also
express, negotiate
and
reaffirm their identities and
goals through
the
practice
of ritual
activities,
such as
meetings
of
sodalities,
initiation
rites,
group-sponsored
activities
(e.g.
dances or
feasts)
and multi-
village
ceremonial activities.
Circular
plaza villages gravitate
towards the central
plaza
which embraces the
community
as a
whole.
They
have been
interpreted
as
representingunity
and
egalitarian
societies,
where
the whole
community
can
participate
in
a democratic fashion.
They
denote
equal
access to
public
activities and ritual
performances
as
long
as houses are
equidistant
from the
central
public
area
(Gron
1991;
Gross
1979).
However,
it
should
not be
forgotten
that
plazas
also
mark
social differences
along
lines of
gender, age
and
lineages.
In Amazonian and Central
Brazilian
groups (e.g. Heckenberger2005;Hornborg 1988;Levi-Strauss1963;
Turner
1996),
plazas
materialize a series of ranked
oppositions
between an
inner,
public,
sacred,
male
domain versus an
outer, domestic,
profane,
female
space.
Plaza
villages
also
embody
inherent
structural
contradictions,
which
carry
the seeds of
incipient
social
differentiation;
a
development
that,
as we
will
see
below,
may
have taken
place
during
the
subsequent
CMC.
The occurrence
of other
broadly contemporaneous
PMP
mound
complexes
(Isla
Larga,
Puntas de San
Luis,
Los Indios and
Potrerillo)
(Fig.
lb,
Table
1)
and other
sites with
similarities in
overall
ground plan
to Los
Ajos (e.g.
Da
Monte,
Campo
Alto,
Estancia Mai
Abrigo
and 5
Islas)
(Fig.
3)
suggest
that these societies were
integrated through pan-tribal
institutions at a
regional
level since Preceramic times. Previous
and new research at
Arroyo Yaguari,
Tacuarembo Province
(Fig.
la),
is
beginning
to show
similar
patterns
(Gianotti
2005;
Sans
1985).
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656 Jose Iriarte
represent
n
integrated
rchitectural
lan
oriented o the northeast that contrastswith the
less
conspicuous
and
informally
arranged
outh-western
ector,
marking
an
asymmetrical
distribution f architecturen the innerprecinct.Through hesetransformations,he inner
precinctacquired
a
strong public
ritualcharacter.
Formality
s one of the most essential
characteristics f ritual and the
way
it
operates
n
society.
Public ritual communicates
through
very
specific
media,
t followsa set
pattern
and its contentsare standardizedo the
extent hat
they
usually
allow
ittlemodification
e.g.
Bell
1997;
Block
1974;
Bradley
1998).
Formalism reflects an adherence to restrictedmodes of
activities,
often viewed
by
participants
as
timeless,
invariantand tradition-laden.Formalized
activity
can
also
be
important
n
the
reproduction
of social
power.
The
apparent
contradictionsbetween
competition
and
cooperation
are not
atypical
of
middle-range
ocieties
e.g.
Fowles
2002;
Tuzin
2001).
Socialactorsand
groups
can
manipulate ublic
architectureo
legitimize
heir
political
powerdrawing
on the fact that architectures an effective ool for
structuring
he
activities that form social
organizationby
expressing
or
restricting
relations
among
individualsand
groups (e.g.
Bourdieu
1977;
Giddens
1979).
Formalceremonial ontexts
'create
opportunities
or social
control,
more
complex
architectural
xpressions,
ocial
stratification,
xchange,
and centralized
eadership'
Dillehay
1992b:
18)
-
and more so
if
thesecircumstances re
accompanied
y
populationgrowth,populationpressure
n fertile
lands,
technological hange
and territorialism:ll
processes
hat
appear
o be
takingplace
at a
regional
evel in the wetlandsof India Muerta
during
he
Ceramic
Mound Period.
The moundsthat are closer to the
plaza
area had
privileged
ccessto
public
ritualand
political
control.
Their
advantageous
location,
architectural
elaboration and the
segregation
of activities hat
they
materialize
uggest
that the membersof this
segment
of thesocietypossiblyenjoyeda somewhathigher ocialstandinghanthose iving nmore
peripheral
reas of the site. Platformmounds
may
have servedas mnemonicdevices to
establish a social
memory
of
place
and
perpetuate
asymmetrical elationshipsby
an
emerging
ector of
the
populationduring
he CMP.
The inner
precinct
of the site also shows a markeddual
spatial
asymmetry.
The north-
east
sectorbecamemoreformaland
prominent,
haracterized
y
the
steep-sided, elatively
high platform
mounds
presenting arge,
fairly rectangular
ummitsframed
by
a
larger,
wider and taller
crescent-shaped
ise,
which
articulates
with
platform
Mound 13.
In
contrast,
on the
opposite
south-westend of the inner
precinct,
here is a less
formally
integrated
reacharacterized
y
low,
dome-shaped,
ircularmoundssurrounded
y
a less
prominentTBScrescent-shapedise.Giventhewidespread thnographice.g.Levi-Strauss
1963;
Nimandeju
1946;
Turner
1996)
and
archaeological e.g. Knight
1990;
Netherly
and
Dillehay
1986)
presence
of dual
organization
associatedwith dual architectural
atterns
and
plazavillages
both in
South
and
North
America,
he
Los
Ajos groundplan during
he
CMP
may
well
represent
n
expression
f a rankeddualsocial
organization.
These
patterns
require
larification
hrough
urther esearch t
Los
Ajos
and
other
sites in the
region.
Concluding
remarks
The
multidisciplinarynvestigations
t Los
Ajos
have advanced
previous nterpretations
f
cultural
development
n the
region
n
significant
ways.
First,the combined
archaeological
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Landscape transformation,
mounded
villages
and
adopted
cultigens
657
and
palaeoecological
data show that the mid-Holocenewas characterized
y significant
climatic and
ecological changes,
and that these
perturbations
were associated
with
important ultural ransitionsnvolvingpermanentmoundedsettlements ituatedwithin
resource-rich,
ircumscribed
wetlands.
Second,
the renewed
community-focused
rchae-
ological
programme
t
Los
Ajos
revealed hat Preceramicmound
complexes
are not the
result of
successive,
short-term
occupations by hunter-gatherer-fishers
ho moved
seasonally
o
exploit
the rich local environments f this
region (e.g.
Schmitzet
al.
1991)
nor the burialmounds
or monuments f
complexhunter-gatherers
s
previouslyproposed
(Gianotti
2000;
Lopez
and Bracco
1994;
Lopez
and
Giannotti
1998).
According
o our
alternative
rgument,
Los
Ajos
is a
well-planned illage ncorporating
entral
public
spaces
built
by people
who
practised
mixed
economy
combininghunting
and
gathering
withfood
production.
The domesticuse
of
moundsat
Los
Ajos during
he PMP
forming
a
village
s
not
in
agreement
with
the
monumental/ceremonial
ature
of
early mound-building
proposedby
other researchers
Gianotti
2000;
Lopez
and Gianotti
1998;
Pintos
2000).
The
presence
of at least four other Preceramicmound
complexes
with dates
broadly
contemporaneous
nd
degrees
of similarities
n
the overall
plan
of
moundedarchitectureo
Los
Ajos
suggest
hat south-eastern
Uruguay
was a locus of
earlypopulation
oncentration
in
lowland South
America.
Although
most of the
large
mound
complexes
n the
region
display
the recursive
geometrical
ayout (circular,
lliptical
and
horseshoe),
here is
also
considerable
variability
not
only
in
the formal structureof the
sites,
but
also in the
combination,
imensions nd
shapes
of mounds
Bracco
et al.
2000b;
Gianotti
2000, 2005;
Lopez
and
Pintos
2000).
Futureworkat a
regional
evelwill be able to
clarify
what
s now a
rather
omplicated icture
of settlement
ariability
llowing
a more
preciseunderstanding
of therole that LosAjos played ntheemergence f earlyFormative ocieties ntheregion.
Third,
he
archaeobotanicalvidence rom Los
Ajos
and other
contemporary
ites
n
the
region,
ncluding
sla
Larga,
EstanciaMai
Abrigo
and Los
Indios,
ndicates
hat
cultigens
suchas
maize,
squashes,
Phaseolus eansand
possibly
domesticated ubers
Canna p.
and
Calathea
p.)
were
ntroduced nd became
ntegrated
nto local food
economies
by
c. 4000
bp
(Iriarte
n
press;
riarte t al.
2001;
Iriarte t al.
2004).
Thesenew data
put
into
question
previous
nterpretations
hat
proposed
hat the
expansion
and colonizationof
the
region
by Tupi-Guarani
ropical
orestfarmers
during
he late Holocenewere
responsible
or
the
arrival
and dissemination f food
production
o
the
region
(Schmitz
1991).
Greater
expectations
The
early
Formative cultures of south-eastern
Uruguay
are
beginning
to unravel the
existenceof a
unique, ndependent
nd a more
complex
cultural
rajectory
han
previously
thought
for the La Plata
Basin.The
unexpected
ultural
equence
at Los
Ajos
revealsan
early expression
of cultural
complexity
never
before
registered
n this
region
of lowland
South
America,
which clashes with the
long-held
view that this
region
was
inhabited
by
marginal,
mall
groups
of
simple,highly
mobile
hunter-gatherers
hat had not
experienced
significant hanges
incethe
beginning
f the
Holocene
Meggers
nd Evans
1978;
Steward
1946)
and endorses
previous
views
(Andrade
and
Lopez
2001;
Braccoet
al.
2000a;
Lopez
2001).
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658
Jose Iriarte
Contemporary
with the first urban societies that
emerged
on the desertcoast of Peru
(Solis
et
al.
2001)
and the
development
f the AmazonianFormative
Heckenberger
005),
the socialchangesexperienced ytheearlyFormativepeoples n south-easternUruguayn
the
midstof a
changing
mid-Holocene nvironment id not take
place
n
a vacuum.
At the
moment,
it is difficult
to assess the role that local
developments
and
interregional
interactions
layed
n
the
emergence
f
early
Formative ocieties
n
the La PlataBasin.No
doubt,
as we learnmore
about the mid and late Holocenecultural
developments
n
the
La
Plata
basin,
we
will
come to realizethat interactions t a broad
geographical
cale with
contemporary
developments,
such as the Preceramic
mound-building
ultures of the
Pantanal
Schmitz
et
al.
1998),
he
pit-housevillages
of the
Itarare/Taquara
raditionof
the
southernBrazilian
Highlands
Beber
2005;
Schmitz
2002),
the
sambaqui
hell-middens
of the
southernAtlanticcoast of Brazil
Andrade
and
Lopez
2001;
DeBlasiset al.
1998),
and
possibly
the
ring
villages
of southern
ringes
of Amazonia
Wust
and Barreto
1999),
must
have
played
a
major
role in
shaping
he
emergence
f
these societies.
The
research
resented
n
this
paper
not
only
showshow flawed s the
concept
of
marginal
area
by
exposing
the
potential
of
grasslands
and wetlands for
pre-Hispanic
cultural
development
Stahl 2004),
but is also
starting
o reveala
diversity
of different
pathways
towards ocial
complexity
aken
by early
Formative
eople
n
the
region.
Theevidence rom
Los
Ajos
has
provided
a basis for the
interpretation
of the rise of
early
Formative
communities n the
La Plata
basin,
which
will
now allow for a broaderconsideration
of the role that
dynamic
human-environment
nteractions,
mported
cultivarsand social
conditions
played
n the
emergence
f
early
complex
societies
n
the La Plata Basin.
Acknowledgements
Research
at Los
Ajos
was funded
by grants
from the National Science
Foundation,
Wenner-Gren oundation or
Anthropological
Research,
Smithsonian
Tropical
Research
Instituteand the
University
of
Kentucky
GraduateSchool. I also received
upport
rom
the
ComisionNacionalde
Arqueologia,
Ministeriode Education
y
Cultura,
Uruguay
and
the
Rotary
Club of
Lascano, Rocha,
Uruguay.
Sean Goddard from the
University
of
Exeter
drafted
Figures
1
and
3.
My
work at Los
Ajos
benefited rom the advice and
insightful
omments
uggested
over the
years by my
Ph.D.
advisory
committee
ncluding
Jim
Brown,George Crothers,Tom Dillehay, RichardJefferies,Tassos Karathanasis,
Dolores
Piperno,
Chris
Pool,
and SisselSchroeder.Tom
Dillehay
helped
me
conceptualize
early
Formative
societies
in
broad
anthropological
erms and also
pushed
me to think
beyond
the confines of
Uruguay
and South America.
I
am also
particularly
rateful
o
OscarMarozzi.The
occupationalhistory
of Los
Ajos
came into
sharper
ocus
during
our
long
discussions over
many
mates while
digging
at Los
Ajos.
I
should also like to
acknowledge
Roberto
Bracco,
Leonel
Cabrera,
and Jose
Lopez
for their
pioneering
and
continuedwork
in
south-eastern
Uruguay;
t is
upon
their foundations hat this
paper
stands.All
statementsmade
herein,however,
are
my
own
responsibility.
Department f Archaeology,University f
Exeter,
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Landscape transformation,
mounded
villages
and
adopted
cultigens
659
Notes
1 A bulk sediment ampleextractedwith a bucketaugerfrom an unspecified ontextin
the basal
area of Cerrode la Viuda was radiocarbondated to
5,420
±260
(URU014)
(Bracco
and
Ures
1999).
More work is neededat the site to
prove
ts association
with a
culturalcontext.
2
When
evaluating
the
PRONAPA
in
hindsight,
t must be remembered hat
it was
a
pioneering
and ambitious
undertaking
which tried to
explore
and
study
Brazil's
8,500,000km2
erritory
with
only
a small handful of
archaeologists.
n
Rio Grande
do
Sul
state,
the work of PRONAPA
represented
he first reconnaissanceof an
archaeologically
unknown
region, generated
the first
chronological
scheme for the
area,
provided
us with the first
systematicdescription
f
sites and artifacts n the
region,
and
broadenedour
understanding
f
past
human-environmentelations.
3 Recent
multiproxy
paleoenvironmental
econstruction
n the
region
by
Braccoand his
collaborators
2005)
should be
regarded
with
considerable aution
since the
changes
n
the Poaceae
phytolithpercentages
hat
they
used to infer broaderclimaticreconstruc-
tion in termsof
temperature
nd
humidity
or the mid and late Holocene
may simply
be
reflecting
he
dynamic
natureof the
Laguna
Negra
salt marsh
during
he mid-Holocene
highstands
and not climatic
changes
(see
Iriarte2006:
28-9).
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Jose
Iriarte s a lecturer
n
the
Department
f
Archaeology,
University
of Exeter.He is an
archaeologist
and
palaeoethnobotanist
whose
principal
research interests are
the
development
of
early
plant
food
production
and the rise of Formativesocietiesin the
Americas.He
receivedhis
PhD
in
anthropology
rom
the
University
of
Kentucky
and has
conducted
archaeological
esearch n
Uruguay,Argentina,
Brazil,
Peruand Mexico. He is
currently
ontinuing
his
investigations
f
early
agriculture
nd
emergent omplexity
n
the
ParanaRiver
Basin
(Misiones,
Argentina).