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The Maj,a Mountains Archaeological Project (MMAP):
Field lieport of the 2000 Season
Peter S. Dunhain
Jack D. Corbo
Ramon I. Vargas
Cleveland State University
Rebecca L. Hays
Tulane University
Andreu-kJ.Kindon
University of California at Los Angeles
Keith M. Prufer
Southern Illinois University at Carbondale
Cliristoplier Boehin
Marvin Cal
Jason Enberg
Mary Primer
Jaclyn Vinick
Cleveland State Unh-ersity
Boilifacio Tut
Forest Department
Government of Belize
Ebbe Brandt
University of Copenhagen
Mary McGee
Cleveland State UniversiQ
Abstract
The ninth season of the Maya Mountains Archaeological Project (MMAP) was_.compIetedduring
April and Ma)-, 2000. Work was conducted again in the upper Bladen dra&ge of the Monkey
River. Archaeological research consisted of cave reconnaissance and settlement survey and
excavations, including tombs. Multiple biological investigations were performed. Plants were
collected for studies of ancient Maya tree farming, resource phytoliths, cacao DNA, and forest
product development. We also sampled turtle and snail DNA for research on evolutionary
genetics. Soil samples were gathered from the surface for plant distribution studies and from
caves for the analysis of antibiotic properties among cave-dwelling microbes. Extensive
mapping of k e region was conducted with a Global Positioning System (GPS) for building a
,,,local Geographic Information System (GIs). A number of major finds were made. The main
operations and discoveries are summarized herein.
Introduction
I'he Majra Mountains Archaeological Prqjt'ct (MMAP) is an ongoing multidisciplina~?stud! of'
ancient Maja resource exploitation and exchange in the remote and rugged 11aja lountains of
southern Belize. Launched in 1992. the reconnaissance phase of the research consisted of a
broadscale sun7eyof mineral and biotic resources and the associated sites. .A multitude of
unusual montane resources as identified. along with o er a dozen centers that likely exploited
and exchange these materials. Recentl!.. a more intensi.e phase has been initiated. focusing on
the major finds from Phase 1. Phase I1 is concentrated at Ek Xux and 14uhlebal Tzul, the
principal centers in the upper Bladen drainage of the Monkey River.
The ninth season of the MMAP was con~pletedin April and May of the Year 2000. We finished
our recoimaissance of caves in the icinity of the t1t.o ruins. The inapping of the suburban
settlement surrounding both sites was almost completed. along with the excavation of associated
tombs and other deposits. Numerous plant specimens were collected. including materials for
studies of ancient Maya tree farming. resource phytoliths, cacao DNA, and forest product
development. Turtle and snail DNA was sampled for research on evolutionaq differentiation.
Surface and cave soils were sampled, the former for plant distribution studies and the latter for
microbes with antibiotic properties. Additiona progress was made on the GPS (satellite locator)
survey of the Ek Xux canyon system for GIs (Geographic Information System) studies. A
number of important finds were made.
Archaeological Operations and Finds
Four major archaeological operations mrere performed in the environs of Muklebal Tzul andlor
Ek Xux: (1) the reconnaissance of caves. (2) the survey of suburban settlement. (3) the
excavation of tombs and suburban settlement. and (4) the preliminary sampling of soils. The
cave reconnaissance was essentially completed. The settlement excavations and mapping are
nearly finished and will probably require one more extended season of field study. The soil
survey will lay a foundation for further study.
Cave Reconnaissance
The 2000 season concluded five years of cave surL7eyin the environs surrounding Muklebal Tzul
and Ek Xux. This year's work focused on completing the reconnaissance of three hillsides in the
Muklebal catchment and two hillsides associated with the Ek Xux pocket. Lateral transects were
conducted along the bases and summits of the hillsides. No new caves were found in the
Muklebal area; several caves with cultural deposits were encountered in the Ek Xux zone. Test
excavations were conducted in the well or pseudocave encountered last year in the stela group at
Muklebal Tzul and at Mayehal Xheton. a cave to the east of Muklebal with a large rockshelter-
like opening. The existence of a plastered collecting basin was established at the entrance to the
well. It was also demonstrated that the flooring extends under the walls of the feature, indicating
that it was installed prior to the construction of the masonry tunnel. The excavations at Mayehal
Xheton revealed evidence of additional plaster flooring and platform m a s o w but no remains of
mortuary activity. The cave apparently did not function as a burial site.
Several major survey finds were made in caves. Workmen cutting a new trail encountered a
sizable cave, U'tuch Qui, in the "rock chute" southeast of Ek Xux. This cave contained a single
polychrome plate with a well-executed black and red over cream scene on the interior, showing a
st~lizedfish apparentl!. snimming. a hall! appr(yri31~'L'ndenxorld image. The cae as
ei identlj used for one discrete ritual eIrent.probabl! more indil idual- than group-oriented. Four
tales were imrestigated on the high hillside southeast of Ek Xux and abo,e the Saki Tzul
rockshelter. To were significant. Kab'il Sah' unah contained several plastered platfornms, one
of which retains at least two lateral i.ooden retaining beams. Evidence of cvstal extraction Lvas
also found. Tno flowstone formations had been fractured and calcite crystals removed. Calcite
cqstals ere deposited elsewhere in the cae. X partial flanged censer it11 an effigy face was
also recovered. At Toq-bil Roq'ikal KabpeL. the remains of at least five vessels, including a
handled censer lid and three snmall unslipped boiils. nere found atop several unplastered
platfoinms. Numerous torch and carbon samples ere also collected for dating purposes.
Settlement and Tomb Excavations
This year. ive continued excavations in the settlement at Muhlebal Tzul and initiated excavations
in the settlement at Ek Xus. The settlement at Muklebal Tzul is notable for its many cotnplex
tombs. which appear to be thoroughly distributed throughout the site periphery. not just in the
core. Three additional tombs were excavated in order to evaluate further the social significance
of this unusual distribution. In West V. less than 300 n~from the core, we completed excavation
of the serial burial uncovered in 1999 in the tomb within Structure 36, me excavated the sealed
tomb in Structure 38 identified in 1999, and Lie conducted salvage excavations in a tomb within
Structure 34 that had been partially looted during the offseason. Medial trenches were also
excavated in structures with tombs that had already been excavated, both within West V and in
West I. 1.3 km from the core. The purpose of the medial trenches was to re~lealarchitectural
details associated with the buildings that contain the tombs. At Ek Xux. ten 1 x 1 m and one 1 x
2 m test units were excavated alongside several outlying structures in an effort to secure charcoal
from trash middens for radiocarbon dating. Two 1 x 2 units were also excavated in gaps within
settlement groups to assess the possibility that nonplatfornl structures had been present.
Last year, we recovered the partially articulated eastern skeleton in the Structure 36 tomb in
Muklebal West V. This year we removed three to four disarticulated individuals and associated
ornaments in the western and southern sectors. The tomb in Structure 38 was extremely well
preserved with a crude corbelled vault. The ceiling of the tomb in Structure 34 had been
completely destroyed by the looting, but much of the deposit was still intact. It produced a large
assemblage of ceramics, including several polychrome sherds, one with partial texts, as well as a
few lithic artifacts. The medial trenching revealed simple box-like constructions. All stairways
had been added after the construction of the main platfonns. The medial trench along the south
face of Structure 1 in West I yielded a formal cache. The main part of the cache consisted of two
Ik-footed dishes placed lip to lip. A miniature incised jar. a complete obsidian prismatic blade,
and a small, crude limestone figurine were all placed behveen the vessels. An incised vase was
found immediately to the southwest of the main vessels, and may also be part of the cache.
Many of the settlement excavations at Ek Xux uncovered middens. All produced carbon. One
revealed a nonplatform structure. The settlement excavation program was highly successful.
Settlement Survey
The settlement survey was greatly extended in 2000. Approximately 100 additional mounds
were mapped with infrared total data stations. Sixty-five were in the massive West 7 group,
about 1.5 km west of the site core of Muklebal Tzul. Thirty-five were north of the creek, some
200 m north of the site core at Ek Xux. Under the direction of PhD archaeology student Andrew
I!..Kindon of UCLA, thc settlement sunel is rapidlj nearing conlpletion. Likely fener than 50
of 300 mounds remain to be mappcd at Ek Xus. An undetermined number is left at Muhlebal
Tzul. but it cannot be high. The valley has been almost completely survej~ed,particularl> along
the most heallily settled central ridge. All settlement will probably have been fully mapped at
both sites after one more extended season. The precise delimitation of the two canyons and the
settlen~entthey contain bj the surrounding precipices makes it possible to map the to sites in
their entiretj.. allowing for the first such con~pletemapping and comparative study. hluklebal
Tzul and Ek Xux are producing some of the best settlement data in the Maya area.
Settlement discoveries in 2000 were especially compelling. West 7 proved to be an enormous
group with'core-like features. The structures are arranged linearly along the spine of a major
spur of the central ridge. The ai-rangement is particularly well developed in its upper reaches.
Settlement is concentrated on the highpoints along the spur. Two of these are linked by a small
causeway, in the manner of major groups within site cores. The uppermost rise supports only
tvo mounds, the tallest just over 1 m high. Inlmediately in front of this structure are the remains
of three plain limestone stela. The occurrence of another monument complex in such close
prosiinity to the core agrees well u.it11 Kindon's hypothesis that status, wealth, authority, and
power are more dispersed throughout the site periphery at Muklebal Tzul than at Ek Xux. It also
accords well with the distribution of complex tombs and burial goods throughout the Muklebal
periphery. The fact that only one of the groups mapped north of Ek Xux even approximates a
formal courtyard again supports the contrast between the two sites. The only truly formal
organization evident at Ek Xux is in the site core.
Soil Sampling
In 1999, we excavated three test pits for a pilot study of soils in the Ek Xux valley. The goal of
these pits was to provide both profiles of the soil system and samples for pedological analysis. 1
x 1 m units were excavated in the suburban settlement near the site core, halfway down the
valley, and at the center of the distant cacao quad. The soil materials were gathered for two
primary purposes. One was to establish the relative acidity of the soils and degree to which they
are derived from the volcanic divide of the mountains. This information would help con~plement
the phytolith studies. as phytoliths would be more likely to develop and preserve in acid volcanic
soils. The other objective was to assess the distribution of cacao-favoring soils. The clustering
of the cacao trees near the ruin might be at least partly explained by a concentration of cacao
soils there. ~edolo~icafanalyses by the Ohio State University revealed a slightly acid pH,
favoring a volcanic parent material and phytolith development. Only one cacao nutrient tended
to be distributed in association with the site. To enhance our understanding of the relationship
between cacao and soils, however, it would help to sample similarly the soils of Muklebal.
In 2000, we conducted a preliminary sampling of the Muklebal soils. We excavated two 1 x 1 nl
test units, one near the center of the cacao quad and corresponding cluster close to the site core
and another at the center of the distant cacao quad. The most complex wall of each was profiled
and samples taken from every major layer. Both units were excavated to bedrock, which at less
than 1 m of depth is indicative of the difference between Muklebal Tzul and Ek Xux. The Ek
Xux soils are deep, rich alluvial deposits derived f?om the acid volcanics. The Muklebal
materials are much darker, derived from basic limestone, and considerably thinner than those of
Ek Xux. The Muklebal valley floor is less mature geologically than that of Ek Xux. Muklebal is
more h a  ili incised and still in the process of eroding. Since cacao is generall! k n o ~ i lto prefer
slightl~acid soils, the occurrence of a significant cacao population on the basic Muklebal soils
ma) pro e to be something of note. It ma1 point to the de.elopment by the ancient h4aj.a of' a
limestone tolerant or preferring species. Pedological analysis of this year's soil samples may
shed important light on the distribution and nature of the hluklebal cacao.
Botanical Operations and Finds
There were four major compoileilts to the botanical program this year. We collected (1)
reference san~plesfor phytolith studies of prehistoric plant use, (2) cacao leaves for DNA
fingerprinting of the aboriginal cacao populations, (3) data on plant distributions for research on
ancient Maya tree farming and its effects on modern forest composition, and (4) mamrney seed
specimens for development into renewable forest products.
Phytolith Reference Specimens
Phytoliths are small silica bodies that form in many plants. They sometimes preserve well and
can be indicatilre of the plants of origin. Their occurrence in a trash midden can help identifj'
those plants that Lvere used by a population. They develop and preserve better in slightly acid
conditions. Given the basic PI-I of the mainly limestone Maya lowlands, they have generally not
been recovered in quality or quantity at other lowland sites. As our preliminaly soil studies have
demonstrated. hoever, the soils of the Ek Xux canyon are derived primarily from the acid
volcanics of the main divide of the Maya Mountains. In 1999, we collected samples from three
middens associated with two structures in the inner settlement at Ek Xux. Analyses by Irwin
Rovner's laboratory at the University of North Carolina in Chapel Hill revealed that these
materials contained some of the highest and best-presen~edconcentrations of phytoliths ever
recorded in the Maya lowlands. Unfortunately, without a comparative collection of phytoliths
extracted from known local flora, it is not possible to identify the Ek Xux phytoliths.
This year, we collected specimens from over a dozen contempora~yplants of recognized
resource value in the Ek Xux environs (see Appendix I for list). These are the species that are
most likely to be represented among the Ek Xux materials. Many of them are also promising
candidates for phytolith production. We gathered samples from various portions of the plants in
order to ensure that we secured the different phytoliths from each part. It is our goal to conduct a
pilot study of the viability of reconstructing the plant resources that were used at Ek Xux by
identifying their remains among the phytoliths in the middens there. We intend to extract
phytoliths from the modern plants that we can use to identify the corresponding ancient ones. If
we are able to identify a significant amount of the prehistoric phytoliths, then we will proceed
with a full-scale study, collecting further samples, both ancient and modern. The Ek Xux
materials will probably provide a uniquely penetrating window into ancient Maya plant use.
Cacao DNA
In 1996, in conjunction with cacao scientist Vish MooleedhBr of the University of the West
Indies in Trinidad, the MMAP identified two populations of aboriginal chocolate still growing
around the ruins of Muklebal Tzul and Ek Xux. The trees fruit but reproduce by shooting, which
means that they are essentially clones of the prehistoric trees. In 1997 and 1999, we mapped
large quadrats of trees in both groups and determined that they were clustered around the two
ruins, perhaps in a fossil pattern. The distribution suggests that they may have been cultivated in
close yroi~nitjto thc a erags 1;0~:seh~Id.not in association  it11 distant rotational maize fields.
Our prt'liminar) soil assajs support this assessment. uith onlj one mqjor cacao nutrient also
concentrated near the ruins. At lull&al there ma! eken ha.e been a single groe. although it
is unclear ivhether it vas under indiidual or community control. Interestingly. the Muklebal
trees grow in limestone soils. indicating that at least one population tolerates or prospers in basic
conditions. Such a tree might be idclj cultivable in the tropical carbonates.
One of the main remaining aspects of the Maya Mountains cacao to document is its genetic
composition. It would be useful to know the relationship between the Ek Xux and Muklebal
populations. modem commercial stocks. and an). other archaic strains. Like many commercial
crops, contkmporary cacao has been highly overbred. It has lost much of its reproductive vigor
and is increasingly vulnerable to blights and substandard conditions. Consequently, there is
great interest in the chocolate industry in developing aboriginal varieties to cross with
commercial stocks. The Maya Mountains cacao ma: prove to be of significant commercial
value. The Government of Belize, living Maya, and research community are already involved in
discussions regarding its development in a mutuall). beneficial fashion. Part of deveIoping a
coinmercially riable identity for the material is to establish its broader genetic signature. We
sampled three leaves each from over twenty videspread trees in each population in order to
determine the wider genetic profile. These specimens will be submitted to DNA analysis.
Precolumbian Tree Farming
Numerous scholars have proposed in recent ycars that the Maya engaged in the cultivation of
trees or silviculture. While a great deal of provocati~eevidence has been advanced. the debate
remains unresolved. Few conclusive cases have been developed. The Maya Mountains may
offer an unusual opportunity to explore the matter further. As the cacao trees attest. we already
know that at least one tree was cultivated around sites in the Maya Mountains. The fact that the
cacao trees retain their fruit beyond the point of germination proves that these trees were
domesticated and therefore cultivated (in domesticating plants, people almost universally select
for individuals that hold their fruit for harvesting). The fact that cacao is an understory tree and
thrives under the shade of higher canopy trees suggests that another overstosy tree may have
been grown along with it. Considering that the cacao trees seem to preserve traces of their
prehistoric patterning, detailed study of contemporary plant distributions in the area might reveal
this association and other potential crop trees. Moreover, the rugged nature of the Maya
Mountains has diminished logging in the interior and may have protected these relationships.
CSU ethnobotany undergraduate student Ramon I. Vargas, former manager of the Forest
Herbarium of the Forest Department of the Go,ernment of Belize, directed a preliminasy study
of plant distributions in the Muklebal and Ek Xux pockets. Four 50-by-50 m plots were
established near the site cores and at significant remove (1 to 2 krn) within each cacao quad.
Every identifiable plant was documented and sampled along 2-m wide transects at 10-m intervals
within the plots. 180 fertile specimens -erecollected and pressed. These results of these efforts
will be utilized to devise a larger sampling strategy that might detect subtle variations in the
distributions of trees and other plants within the Muklebal and Ek Xux forests. It may well
reveal that the current forests in these areas are not just products of forest recovery from
deforestation for Maya agriculture over 1,000 years ago but also have been at least partially
conditioned by the effects of Maya tree farming.
Sustainable Forest Product De.elopment
One of the major goals of the MMAP is to help local populations delelop renelvable forest
products that 141generate additional iilconlc alternative to that supplied by poaching or looting
and to pro ids an econonlic incentive to maintain the forest and not destroy or degrade it or its
contents. It is our hope that the cacao find might prove to be particularly helpful on this front.
Last )ear. u e collected samples of the "coffee .ine," chibayal (Tjwnn(/~usgun(emu1ensis). Bark
from this ine produces a clo1.e-like tea, the ilavorant of hich might make an appealing additive
to coffee or chocolate. These samples are currently being subjected to phytochenlical studies at
Northeastern University in order to determine if they contain toxins. At the same time. ve
gathered nuts from the mammey fruit (Pou(cricrznpotu). which when dried and ground have an
almond-like taste and might make a similarly attractive flavorant. Unfortunately, the seeds were
not dried sufficiently and molded before we could send them off for analysis.
This year, u e gathered new mainmey nuts to replace the ones that we lost last year to mold. We
dried them in the sun and miped them doun with alcohol to kill off an) mold that was beginning
to develop. We managed to dry them to the point that the internal seeds are rattling around
inside their external husks. We believe that ye have now secured a sufficiently dried body of
nuts to allow us to pursue phytochemical analyses. If the chibayal and marnmey turn out not to
contain toxins, we will encourage and assist the Government of Belize and a local community
organization in developing and marketing a conmercially i~iableproduct for sale domestic all^
and perhaps even abroad. There would likely be considerable demand for such ecologically
friendly and culturally appropriate products. We have already had discussions with both the
Forest Department and Belize Indigenous Training lnstitute (BITI) regarding the development of
these materials. We hope next to turn to the lemon-leaf tree for a tea or flavor additive.
Zoolonical Operations and Finds
The MMAP helped to support two zoological investigations this year: (1) the sampling of mud
turtle and snail DNA for the study of a new evolutionary mechanism for differentiation and (2)
the collection of soil samples from caves for the analysis of antibiotic properties anlong microbes
that they might contain.
Evolutionaw Differentiation
Evolution pro-ides populations with the diverse adaptations that allow them to continue to
prosper in changing conditions. There are a variety of mechanisms that generate this diversity.
Jack Corbo. a CSU doctoral student in molecular biology, hypotheses that in branching riverine
systems, populations in the upper tributaries become adapted to the specific local conditions of
each branch. As upstream individuals are periodically washed downstream, they introduce the
associated traits and genetic signatures into the populations in the main channels. Main channel
populations. then, are composed of a mixture of these characteristics and adapted to a wider
range of situations. The tributary populations serve as a repository of specific adaptations for the
main channel populations, and main channel populations act as a reservoir of broader adaptations
for branch populations. Last year, Corbo sampled blood from white-lipped mud turtles
(Kinosternon letrcostomum) in the upper Bladen to extract DNA to test this scenario. If true,
tributary DNA would be more specific and main channel DNA more diverse. Unfortunately,
some of the blood samples were insufficient to extract adequate sequences.
In 2000, Corbo returned to the upper Bladen to enhance his stud),. He sampled tissue from the
rear legs of' the mud turtles and from the font of the jure snail ( P c ~ h ~ ~ ~ l ~ i l r r . ~imlio~-ii~n).a
freshwater gastropod, in an effort to extract sufficient genetic material to detect the requisite
pattern. He sampled nearly 50 mud turtles in the Ek Xux creek. AC branch of the Bladen.
Muklebal stretch of the Bladen. Bladen headf,aters2and upper Snake Creek. While the numbers
are low in the uppelmost drainages. w~hichare smaller in extent. they may be sufficient for hi111
to document minor variations between the lower watersheds. in particular Ek Xux. AC. and
Muklebal. He also gathered some 60 samples of,jl~/etissue. The availability ofjr~res.however.
did not seem to vary so much with the size of the catchment as it did with the degree to which
water the water was derived from limestone sources. was basic. and contained adequate calcium
carbonate for the rnolluscs to secrete their shells. Patterns in the DNA among these specimens
might provide evidence that the mechanism is sufficiently generic and powerful to appl>-across
species boundaries to many aquatic organisms in dendritic or branching systems. If the
hypothesis is supported, it will become an important factor in designing consenration areas.
Antibiotic Microbes in Caves
Dark zones in caves often contain fen nutrients, especiallj, if the system is closed to the
introduction of outside organic materials. Consequently. competition is pal-titularly heavq
among microbes that inhabit cave soils in such environments. Cave-dwelling microbes of this
sort are known in some cases to secrete antibiotic chen~icalsto hold off competing organisms,
helping to ensure preferential access to an adequate food supply. At a time in which antibiotic
inedications are losing efficacy due to increasing resistance by pathogens, this phenomenon is of
growing interest. At least one company. Biomes, Inc., has been incorporated expressly for the
purpose of attempting to develop viable antibiotic products from the secretions of cave microbes.
CSU molecular biology PhD student Jack Corbo arranged with biochemist David Newrnan of the
US National Cancer Institute to analyze cave soils from the upper Bladen for antibiotic microbes.
Our intention in working with the NCI. which has a very favorable biological properties
protocol, was to avoid any commercial entanglements that might result if a find is made.
Twenty-two soil samples were gathered from four major cave systems: U'toch Qui, Black Pot
Cave, and the AC Cave in the Ek Xux system and Tusbil Pek in the middle Snake Creek. The
samples are approximately 10 mg in weight. They were obtained bjr scraping the material from
the cave floor with a ~Tbodensampling stick into a ziploc sample bag. Each bag and sample
stick was sterilized by exposing it to ultraviolet light to ensure that the samples contain only
microbes from the caves and not any that would otherwise have been introduced from the stick
and bag. Dr. Newman anticipates that the contents should remain viable for at least a month.
We are exporting the materials under our US Department of Agriculture soil importation permit.
The analyses will be conducted in the biosecure laboratories at Ft. Detrick, Maryland.
GPSIGIS Mapping .
In 1999, we began mapping the Ek Xux canyon with a Global Positioning System (GPS) or
satellite locator. The existing maps of the region were made from aerial photographs and are too
small in scale for us to be able to plot our wealth of multidisciplinary data on them. The
mapping is being conducted in several phases. The initial phase cdnsists of securing Universal
Transverse Mercator (UTM) readings for major points defining the base of the cliff faces that
form the canjons. These readings delimit the can>on~isllsh)nl the c a q o n bottoms. helping us
to delineate the habitable area. Wc also acquire GI's rcaciings for the nlain Ivatsrcourses. such as
the Bladen and the Ek Xux Creek. In the future. ive hope to map the configuration of important
features on the canyon bottomlands. like the upper riparian terraces and ridgetops that support
settlement. further enabling us to clarifj the area that as suitable for habitation. With these
figures. we maj ultimately be able to reconstruct camring capacities. We sill also be able to
construct a basenlap for plotting our data within a Geographic Information System (GIs). a
computerized management program for spatial data.
In 2000, we managed to map the narrols neck of the Bladen gorge that links the Ek Xus and AC
pockets, as well as most of the AC canyon. We Mere actuall~pleasantly surprised to con~plete
this sector. as the can>-onwalls are so high and so close as that they nearlq. prevent satellite signal
reception. We were well on schedule to finish mapping the main segment of the AC canyon.
when our work was interrupted by rainy weather and clouds. We completed mapping the
southeast, southwest, and northwest sections. The entire AC stretch of the Bladen and the AC
Creek ere also mapped. Thick cloud coverage, in conlbination with the canyon wall and dense
forest canopy, prevented mapping of the last bits of the northeast portion of the canyon Lrall. We
expect to conclude the mapping of the AC canjron in short order in 2001. when we will initiate
mapping the Muklebal valley. We will also probably employ two GPS teams on a constant basis
next year in order to ensure that we conclude the survey. We will attempt to begin the second
phase of terrace and ridge mapping at that time.
Conclusions
The 2000 season of the MMAP was another great success. We have essentially completed our
cave reconnaissance in the Muklebal Tzul - Ek Xus area. The settlement survey and excavation
programs will likely be finished next year. Preliminary soil sampling was finished in the
Muklebal valley. Reference phytolith specimens were collected, as were cacao DNA samples,
data that may reflect on ancient Maya tree farming. and mammey seeds for sustainable forest
product development. Mud turtle and snail DNA were also gathered for studies of the
eolutionary mechanisms behind genetic differentiation. Cave microbes were also sampled to
see if they exhibit any antibiotic properties. The GPS mapping of the AC Canyon was nearly
completed, making for significant progress on our GIs basemap.
A number of important finds were made. The cave reconnaissance produced the painted fish pot.
the wooden retaining beams, modeled effigy censer. and extraction locus for calcite crystals.
The Mukelbal settlement excavations completed the recovey of the serial burials from last year
and yielded a useful cache. The Ek Xux settlement excavations produced numerous charcoal
fragments for radiocarbon dating and promising midden materials for phytolith extraction. The
settlement survey uncovered a second stela plaza in large outlier of Muklebal Tzul and further
evidence that the settlement at Muklebal Tzul is more formalized and the distribution of power
there more dispersed than at Ek Xux. The season was highly productive.
Appendix I:
Contemporar~.Plant Specimens Collected for Con~pal-ativePhtolith Anah sis
Common Name Family Genusispecies
/ Basket Vine / Palmae / Destnoncrts schiz?z?ii
BreadnutiRamon
Cocoa/Chocolate
Cedrelu niexicunu
Ol'hitiw~cohune
Cedar
Cohune Pal~n
Moraceae
Sterculiaceae
Melilaceae
Palinae
1 Mammey / Sapotaceae 1 Pouteria zapotcr
Brosimiutn alicc~s~rzm
T/~eohromucucao
CopaliPom
Gumbolimbo
Burseraceae
Burseraceae
Sapodilla
Warrie Cohune
P~.otizrnicopal
Busserer simaruhu
Cow Foot
Tapir Foot
Sapotaceae
Palmae
Mcrnilccrra zapota
A.s(roccrr.vunirnexicanuni
Piperaceae
Curcurbitaceae
Piper cutri(zcnz
Gzra~.anicrnlnkounc/

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Peter dunham, et al. the maya mountains archaeological project (mmap) field report of the 2000 season, 2000

  • 1. The Maj,a Mountains Archaeological Project (MMAP): Field lieport of the 2000 Season Peter S. Dunhain Jack D. Corbo Ramon I. Vargas Cleveland State University Rebecca L. Hays Tulane University Andreu-kJ.Kindon University of California at Los Angeles Keith M. Prufer Southern Illinois University at Carbondale Cliristoplier Boehin Marvin Cal Jason Enberg Mary Primer Jaclyn Vinick Cleveland State Unh-ersity Boilifacio Tut Forest Department Government of Belize Ebbe Brandt University of Copenhagen Mary McGee Cleveland State UniversiQ Abstract The ninth season of the Maya Mountains Archaeological Project (MMAP) was_.compIetedduring April and Ma)-, 2000. Work was conducted again in the upper Bladen dra&ge of the Monkey River. Archaeological research consisted of cave reconnaissance and settlement survey and excavations, including tombs. Multiple biological investigations were performed. Plants were collected for studies of ancient Maya tree farming, resource phytoliths, cacao DNA, and forest product development. We also sampled turtle and snail DNA for research on evolutionary genetics. Soil samples were gathered from the surface for plant distribution studies and from caves for the analysis of antibiotic properties among cave-dwelling microbes. Extensive mapping of k e region was conducted with a Global Positioning System (GPS) for building a ,,,local Geographic Information System (GIs). A number of major finds were made. The main operations and discoveries are summarized herein.
  • 2. Introduction I'he Majra Mountains Archaeological Prqjt'ct (MMAP) is an ongoing multidisciplina~?stud! of' ancient Maja resource exploitation and exchange in the remote and rugged 11aja lountains of southern Belize. Launched in 1992. the reconnaissance phase of the research consisted of a broadscale sun7eyof mineral and biotic resources and the associated sites. .A multitude of unusual montane resources as identified. along with o er a dozen centers that likely exploited and exchange these materials. Recentl!.. a more intensi.e phase has been initiated. focusing on the major finds from Phase 1. Phase I1 is concentrated at Ek Xux and 14uhlebal Tzul, the principal centers in the upper Bladen drainage of the Monkey River. The ninth season of the MMAP was con~pletedin April and May of the Year 2000. We finished our recoimaissance of caves in the icinity of the t1t.o ruins. The inapping of the suburban settlement surrounding both sites was almost completed. along with the excavation of associated tombs and other deposits. Numerous plant specimens were collected. including materials for studies of ancient Maya tree farming. resource phytoliths, cacao DNA, and forest product development. Turtle and snail DNA was sampled for research on evolutionaq differentiation. Surface and cave soils were sampled, the former for plant distribution studies and the latter for microbes with antibiotic properties. Additiona progress was made on the GPS (satellite locator) survey of the Ek Xux canyon system for GIs (Geographic Information System) studies. A number of important finds were made. Archaeological Operations and Finds Four major archaeological operations mrere performed in the environs of Muklebal Tzul andlor Ek Xux: (1) the reconnaissance of caves. (2) the survey of suburban settlement. (3) the excavation of tombs and suburban settlement. and (4) the preliminary sampling of soils. The cave reconnaissance was essentially completed. The settlement excavations and mapping are nearly finished and will probably require one more extended season of field study. The soil survey will lay a foundation for further study. Cave Reconnaissance The 2000 season concluded five years of cave surL7eyin the environs surrounding Muklebal Tzul and Ek Xux. This year's work focused on completing the reconnaissance of three hillsides in the Muklebal catchment and two hillsides associated with the Ek Xux pocket. Lateral transects were conducted along the bases and summits of the hillsides. No new caves were found in the Muklebal area; several caves with cultural deposits were encountered in the Ek Xux zone. Test excavations were conducted in the well or pseudocave encountered last year in the stela group at Muklebal Tzul and at Mayehal Xheton. a cave to the east of Muklebal with a large rockshelter- like opening. The existence of a plastered collecting basin was established at the entrance to the well. It was also demonstrated that the flooring extends under the walls of the feature, indicating that it was installed prior to the construction of the masonry tunnel. The excavations at Mayehal Xheton revealed evidence of additional plaster flooring and platform m a s o w but no remains of mortuary activity. The cave apparently did not function as a burial site. Several major survey finds were made in caves. Workmen cutting a new trail encountered a sizable cave, U'tuch Qui, in the "rock chute" southeast of Ek Xux. This cave contained a single polychrome plate with a well-executed black and red over cream scene on the interior, showing a
  • 3. st~lizedfish apparentl!. snimming. a hall! appr(yri31~'L'ndenxorld image. The cae as ei identlj used for one discrete ritual eIrent.probabl! more indil idual- than group-oriented. Four tales were imrestigated on the high hillside southeast of Ek Xux and abo,e the Saki Tzul rockshelter. To were significant. Kab'il Sah' unah contained several plastered platfornms, one of which retains at least two lateral i.ooden retaining beams. Evidence of cvstal extraction Lvas also found. Tno flowstone formations had been fractured and calcite crystals removed. Calcite cqstals ere deposited elsewhere in the cae. X partial flanged censer it11 an effigy face was also recovered. At Toq-bil Roq'ikal KabpeL. the remains of at least five vessels, including a handled censer lid and three snmall unslipped boiils. nere found atop several unplastered platfoinms. Numerous torch and carbon samples ere also collected for dating purposes. Settlement and Tomb Excavations This year. ive continued excavations in the settlement at Muhlebal Tzul and initiated excavations in the settlement at Ek Xus. The settlement at Muklebal Tzul is notable for its many cotnplex tombs. which appear to be thoroughly distributed throughout the site periphery. not just in the core. Three additional tombs were excavated in order to evaluate further the social significance of this unusual distribution. In West V. less than 300 n~from the core, we completed excavation of the serial burial uncovered in 1999 in the tomb within Structure 36, me excavated the sealed tomb in Structure 38 identified in 1999, and Lie conducted salvage excavations in a tomb within Structure 34 that had been partially looted during the offseason. Medial trenches were also excavated in structures with tombs that had already been excavated, both within West V and in West I. 1.3 km from the core. The purpose of the medial trenches was to re~lealarchitectural details associated with the buildings that contain the tombs. At Ek Xux. ten 1 x 1 m and one 1 x 2 m test units were excavated alongside several outlying structures in an effort to secure charcoal from trash middens for radiocarbon dating. Two 1 x 2 units were also excavated in gaps within settlement groups to assess the possibility that nonplatfornl structures had been present. Last year, we recovered the partially articulated eastern skeleton in the Structure 36 tomb in Muklebal West V. This year we removed three to four disarticulated individuals and associated ornaments in the western and southern sectors. The tomb in Structure 38 was extremely well preserved with a crude corbelled vault. The ceiling of the tomb in Structure 34 had been completely destroyed by the looting, but much of the deposit was still intact. It produced a large assemblage of ceramics, including several polychrome sherds, one with partial texts, as well as a few lithic artifacts. The medial trenching revealed simple box-like constructions. All stairways had been added after the construction of the main platfonns. The medial trench along the south face of Structure 1 in West I yielded a formal cache. The main part of the cache consisted of two Ik-footed dishes placed lip to lip. A miniature incised jar. a complete obsidian prismatic blade, and a small, crude limestone figurine were all placed behveen the vessels. An incised vase was found immediately to the southwest of the main vessels, and may also be part of the cache. Many of the settlement excavations at Ek Xux uncovered middens. All produced carbon. One revealed a nonplatform structure. The settlement excavation program was highly successful. Settlement Survey The settlement survey was greatly extended in 2000. Approximately 100 additional mounds were mapped with infrared total data stations. Sixty-five were in the massive West 7 group, about 1.5 km west of the site core of Muklebal Tzul. Thirty-five were north of the creek, some 200 m north of the site core at Ek Xux. Under the direction of PhD archaeology student Andrew
  • 4. I!..Kindon of UCLA, thc settlement sunel is rapidlj nearing conlpletion. Likely fener than 50 of 300 mounds remain to be mappcd at Ek Xus. An undetermined number is left at Muhlebal Tzul. but it cannot be high. The valley has been almost completely survej~ed,particularl> along the most heallily settled central ridge. All settlement will probably have been fully mapped at both sites after one more extended season. The precise delimitation of the two canyons and the settlen~entthey contain bj the surrounding precipices makes it possible to map the to sites in their entiretj.. allowing for the first such con~pletemapping and comparative study. hluklebal Tzul and Ek Xux are producing some of the best settlement data in the Maya area. Settlement discoveries in 2000 were especially compelling. West 7 proved to be an enormous group with'core-like features. The structures are arranged linearly along the spine of a major spur of the central ridge. The ai-rangement is particularly well developed in its upper reaches. Settlement is concentrated on the highpoints along the spur. Two of these are linked by a small causeway, in the manner of major groups within site cores. The uppermost rise supports only tvo mounds, the tallest just over 1 m high. Inlmediately in front of this structure are the remains of three plain limestone stela. The occurrence of another monument complex in such close prosiinity to the core agrees well u.it11 Kindon's hypothesis that status, wealth, authority, and power are more dispersed throughout the site periphery at Muklebal Tzul than at Ek Xux. It also accords well with the distribution of complex tombs and burial goods throughout the Muklebal periphery. The fact that only one of the groups mapped north of Ek Xux even approximates a formal courtyard again supports the contrast between the two sites. The only truly formal organization evident at Ek Xux is in the site core. Soil Sampling In 1999, we excavated three test pits for a pilot study of soils in the Ek Xux valley. The goal of these pits was to provide both profiles of the soil system and samples for pedological analysis. 1 x 1 m units were excavated in the suburban settlement near the site core, halfway down the valley, and at the center of the distant cacao quad. The soil materials were gathered for two primary purposes. One was to establish the relative acidity of the soils and degree to which they are derived from the volcanic divide of the mountains. This information would help con~plement the phytolith studies. as phytoliths would be more likely to develop and preserve in acid volcanic soils. The other objective was to assess the distribution of cacao-favoring soils. The clustering of the cacao trees near the ruin might be at least partly explained by a concentration of cacao soils there. ~edolo~icafanalyses by the Ohio State University revealed a slightly acid pH, favoring a volcanic parent material and phytolith development. Only one cacao nutrient tended to be distributed in association with the site. To enhance our understanding of the relationship between cacao and soils, however, it would help to sample similarly the soils of Muklebal. In 2000, we conducted a preliminary sampling of the Muklebal soils. We excavated two 1 x 1 nl test units, one near the center of the cacao quad and corresponding cluster close to the site core and another at the center of the distant cacao quad. The most complex wall of each was profiled and samples taken from every major layer. Both units were excavated to bedrock, which at less than 1 m of depth is indicative of the difference between Muklebal Tzul and Ek Xux. The Ek Xux soils are deep, rich alluvial deposits derived f?om the acid volcanics. The Muklebal materials are much darker, derived from basic limestone, and considerably thinner than those of Ek Xux. The Muklebal valley floor is less mature geologically than that of Ek Xux. Muklebal is
  • 5. more h a ili incised and still in the process of eroding. Since cacao is generall! k n o ~ i lto prefer slightl~acid soils, the occurrence of a significant cacao population on the basic Muklebal soils ma) pro e to be something of note. It ma1 point to the de.elopment by the ancient h4aj.a of' a limestone tolerant or preferring species. Pedological analysis of this year's soil samples may shed important light on the distribution and nature of the hluklebal cacao. Botanical Operations and Finds There were four major compoileilts to the botanical program this year. We collected (1) reference san~plesfor phytolith studies of prehistoric plant use, (2) cacao leaves for DNA fingerprinting of the aboriginal cacao populations, (3) data on plant distributions for research on ancient Maya tree farming and its effects on modern forest composition, and (4) mamrney seed specimens for development into renewable forest products. Phytolith Reference Specimens Phytoliths are small silica bodies that form in many plants. They sometimes preserve well and can be indicatilre of the plants of origin. Their occurrence in a trash midden can help identifj' those plants that Lvere used by a population. They develop and preserve better in slightly acid conditions. Given the basic PI-I of the mainly limestone Maya lowlands, they have generally not been recovered in quality or quantity at other lowland sites. As our preliminaly soil studies have demonstrated. hoever, the soils of the Ek Xux canyon are derived primarily from the acid volcanics of the main divide of the Maya Mountains. In 1999, we collected samples from three middens associated with two structures in the inner settlement at Ek Xux. Analyses by Irwin Rovner's laboratory at the University of North Carolina in Chapel Hill revealed that these materials contained some of the highest and best-presen~edconcentrations of phytoliths ever recorded in the Maya lowlands. Unfortunately, without a comparative collection of phytoliths extracted from known local flora, it is not possible to identify the Ek Xux phytoliths. This year, we collected specimens from over a dozen contempora~yplants of recognized resource value in the Ek Xux environs (see Appendix I for list). These are the species that are most likely to be represented among the Ek Xux materials. Many of them are also promising candidates for phytolith production. We gathered samples from various portions of the plants in order to ensure that we secured the different phytoliths from each part. It is our goal to conduct a pilot study of the viability of reconstructing the plant resources that were used at Ek Xux by identifying their remains among the phytoliths in the middens there. We intend to extract phytoliths from the modern plants that we can use to identify the corresponding ancient ones. If we are able to identify a significant amount of the prehistoric phytoliths, then we will proceed with a full-scale study, collecting further samples, both ancient and modern. The Ek Xux materials will probably provide a uniquely penetrating window into ancient Maya plant use. Cacao DNA In 1996, in conjunction with cacao scientist Vish MooleedhBr of the University of the West Indies in Trinidad, the MMAP identified two populations of aboriginal chocolate still growing around the ruins of Muklebal Tzul and Ek Xux. The trees fruit but reproduce by shooting, which means that they are essentially clones of the prehistoric trees. In 1997 and 1999, we mapped large quadrats of trees in both groups and determined that they were clustered around the two ruins, perhaps in a fossil pattern. The distribution suggests that they may have been cultivated in
  • 6. close yroi~nitjto thc a erags 1;0~:seh~Id.not in association it11 distant rotational maize fields. Our prt'liminar) soil assajs support this assessment. uith onlj one mqjor cacao nutrient also concentrated near the ruins. At lull&al there ma! eken ha.e been a single groe. although it is unclear ivhether it vas under indiidual or community control. Interestingly. the Muklebal trees grow in limestone soils. indicating that at least one population tolerates or prospers in basic conditions. Such a tree might be idclj cultivable in the tropical carbonates. One of the main remaining aspects of the Maya Mountains cacao to document is its genetic composition. It would be useful to know the relationship between the Ek Xux and Muklebal populations. modem commercial stocks. and an). other archaic strains. Like many commercial crops, contkmporary cacao has been highly overbred. It has lost much of its reproductive vigor and is increasingly vulnerable to blights and substandard conditions. Consequently, there is great interest in the chocolate industry in developing aboriginal varieties to cross with commercial stocks. The Maya Mountains cacao ma: prove to be of significant commercial value. The Government of Belize, living Maya, and research community are already involved in discussions regarding its development in a mutuall). beneficial fashion. Part of deveIoping a coinmercially riable identity for the material is to establish its broader genetic signature. We sampled three leaves each from over twenty videspread trees in each population in order to determine the wider genetic profile. These specimens will be submitted to DNA analysis. Precolumbian Tree Farming Numerous scholars have proposed in recent ycars that the Maya engaged in the cultivation of trees or silviculture. While a great deal of provocati~eevidence has been advanced. the debate remains unresolved. Few conclusive cases have been developed. The Maya Mountains may offer an unusual opportunity to explore the matter further. As the cacao trees attest. we already know that at least one tree was cultivated around sites in the Maya Mountains. The fact that the cacao trees retain their fruit beyond the point of germination proves that these trees were domesticated and therefore cultivated (in domesticating plants, people almost universally select for individuals that hold their fruit for harvesting). The fact that cacao is an understory tree and thrives under the shade of higher canopy trees suggests that another overstosy tree may have been grown along with it. Considering that the cacao trees seem to preserve traces of their prehistoric patterning, detailed study of contemporary plant distributions in the area might reveal this association and other potential crop trees. Moreover, the rugged nature of the Maya Mountains has diminished logging in the interior and may have protected these relationships. CSU ethnobotany undergraduate student Ramon I. Vargas, former manager of the Forest Herbarium of the Forest Department of the Go,ernment of Belize, directed a preliminasy study of plant distributions in the Muklebal and Ek Xux pockets. Four 50-by-50 m plots were established near the site cores and at significant remove (1 to 2 krn) within each cacao quad. Every identifiable plant was documented and sampled along 2-m wide transects at 10-m intervals within the plots. 180 fertile specimens -erecollected and pressed. These results of these efforts will be utilized to devise a larger sampling strategy that might detect subtle variations in the distributions of trees and other plants within the Muklebal and Ek Xux forests. It may well reveal that the current forests in these areas are not just products of forest recovery from deforestation for Maya agriculture over 1,000 years ago but also have been at least partially conditioned by the effects of Maya tree farming.
  • 7. Sustainable Forest Product De.elopment One of the major goals of the MMAP is to help local populations delelop renelvable forest products that 141generate additional iilconlc alternative to that supplied by poaching or looting and to pro ids an econonlic incentive to maintain the forest and not destroy or degrade it or its contents. It is our hope that the cacao find might prove to be particularly helpful on this front. Last )ear. u e collected samples of the "coffee .ine," chibayal (Tjwnn(/~usgun(emu1ensis). Bark from this ine produces a clo1.e-like tea, the ilavorant of hich might make an appealing additive to coffee or chocolate. These samples are currently being subjected to phytochenlical studies at Northeastern University in order to determine if they contain toxins. At the same time. ve gathered nuts from the mammey fruit (Pou(cricrznpotu). which when dried and ground have an almond-like taste and might make a similarly attractive flavorant. Unfortunately, the seeds were not dried sufficiently and molded before we could send them off for analysis. This year, u e gathered new mainmey nuts to replace the ones that we lost last year to mold. We dried them in the sun and miped them doun with alcohol to kill off an) mold that was beginning to develop. We managed to dry them to the point that the internal seeds are rattling around inside their external husks. We believe that ye have now secured a sufficiently dried body of nuts to allow us to pursue phytochemical analyses. If the chibayal and marnmey turn out not to contain toxins, we will encourage and assist the Government of Belize and a local community organization in developing and marketing a conmercially i~iableproduct for sale domestic all^ and perhaps even abroad. There would likely be considerable demand for such ecologically friendly and culturally appropriate products. We have already had discussions with both the Forest Department and Belize Indigenous Training lnstitute (BITI) regarding the development of these materials. We hope next to turn to the lemon-leaf tree for a tea or flavor additive. Zoolonical Operations and Finds The MMAP helped to support two zoological investigations this year: (1) the sampling of mud turtle and snail DNA for the study of a new evolutionary mechanism for differentiation and (2) the collection of soil samples from caves for the analysis of antibiotic properties anlong microbes that they might contain. Evolutionaw Differentiation Evolution pro-ides populations with the diverse adaptations that allow them to continue to prosper in changing conditions. There are a variety of mechanisms that generate this diversity. Jack Corbo. a CSU doctoral student in molecular biology, hypotheses that in branching riverine systems, populations in the upper tributaries become adapted to the specific local conditions of each branch. As upstream individuals are periodically washed downstream, they introduce the associated traits and genetic signatures into the populations in the main channels. Main channel populations. then, are composed of a mixture of these characteristics and adapted to a wider range of situations. The tributary populations serve as a repository of specific adaptations for the main channel populations, and main channel populations act as a reservoir of broader adaptations for branch populations. Last year, Corbo sampled blood from white-lipped mud turtles (Kinosternon letrcostomum) in the upper Bladen to extract DNA to test this scenario. If true, tributary DNA would be more specific and main channel DNA more diverse. Unfortunately, some of the blood samples were insufficient to extract adequate sequences.
  • 8. In 2000, Corbo returned to the upper Bladen to enhance his stud),. He sampled tissue from the rear legs of' the mud turtles and from the font of the jure snail ( P c ~ h ~ ~ ~ l ~ i l r r . ~imlio~-ii~n).a freshwater gastropod, in an effort to extract sufficient genetic material to detect the requisite pattern. He sampled nearly 50 mud turtles in the Ek Xux creek. AC branch of the Bladen. Muklebal stretch of the Bladen. Bladen headf,aters2and upper Snake Creek. While the numbers are low in the uppelmost drainages. w~hichare smaller in extent. they may be sufficient for hi111 to document minor variations between the lower watersheds. in particular Ek Xux. AC. and Muklebal. He also gathered some 60 samples of,jl~/etissue. The availability ofjr~res.however. did not seem to vary so much with the size of the catchment as it did with the degree to which water the water was derived from limestone sources. was basic. and contained adequate calcium carbonate for the rnolluscs to secrete their shells. Patterns in the DNA among these specimens might provide evidence that the mechanism is sufficiently generic and powerful to appl>-across species boundaries to many aquatic organisms in dendritic or branching systems. If the hypothesis is supported, it will become an important factor in designing consenration areas. Antibiotic Microbes in Caves Dark zones in caves often contain fen nutrients, especiallj, if the system is closed to the introduction of outside organic materials. Consequently. competition is pal-titularly heavq among microbes that inhabit cave soils in such environments. Cave-dwelling microbes of this sort are known in some cases to secrete antibiotic chen~icalsto hold off competing organisms, helping to ensure preferential access to an adequate food supply. At a time in which antibiotic inedications are losing efficacy due to increasing resistance by pathogens, this phenomenon is of growing interest. At least one company. Biomes, Inc., has been incorporated expressly for the purpose of attempting to develop viable antibiotic products from the secretions of cave microbes. CSU molecular biology PhD student Jack Corbo arranged with biochemist David Newrnan of the US National Cancer Institute to analyze cave soils from the upper Bladen for antibiotic microbes. Our intention in working with the NCI. which has a very favorable biological properties protocol, was to avoid any commercial entanglements that might result if a find is made. Twenty-two soil samples were gathered from four major cave systems: U'toch Qui, Black Pot Cave, and the AC Cave in the Ek Xux system and Tusbil Pek in the middle Snake Creek. The samples are approximately 10 mg in weight. They were obtained bjr scraping the material from the cave floor with a ~Tbodensampling stick into a ziploc sample bag. Each bag and sample stick was sterilized by exposing it to ultraviolet light to ensure that the samples contain only microbes from the caves and not any that would otherwise have been introduced from the stick and bag. Dr. Newman anticipates that the contents should remain viable for at least a month. We are exporting the materials under our US Department of Agriculture soil importation permit. The analyses will be conducted in the biosecure laboratories at Ft. Detrick, Maryland. GPSIGIS Mapping . In 1999, we began mapping the Ek Xux canyon with a Global Positioning System (GPS) or satellite locator. The existing maps of the region were made from aerial photographs and are too small in scale for us to be able to plot our wealth of multidisciplinary data on them. The mapping is being conducted in several phases. The initial phase cdnsists of securing Universal Transverse Mercator (UTM) readings for major points defining the base of the cliff faces that
  • 9. form the canjons. These readings delimit the can>on~isllsh)nl the c a q o n bottoms. helping us to delineate the habitable area. Wc also acquire GI's rcaciings for the nlain Ivatsrcourses. such as the Bladen and the Ek Xux Creek. In the future. ive hope to map the configuration of important features on the canyon bottomlands. like the upper riparian terraces and ridgetops that support settlement. further enabling us to clarifj the area that as suitable for habitation. With these figures. we maj ultimately be able to reconstruct camring capacities. We sill also be able to construct a basenlap for plotting our data within a Geographic Information System (GIs). a computerized management program for spatial data. In 2000, we managed to map the narrols neck of the Bladen gorge that links the Ek Xus and AC pockets, as well as most of the AC canyon. We Mere actuall~pleasantly surprised to con~plete this sector. as the can>-onwalls are so high and so close as that they nearlq. prevent satellite signal reception. We were well on schedule to finish mapping the main segment of the AC canyon. when our work was interrupted by rainy weather and clouds. We completed mapping the southeast, southwest, and northwest sections. The entire AC stretch of the Bladen and the AC Creek ere also mapped. Thick cloud coverage, in conlbination with the canyon wall and dense forest canopy, prevented mapping of the last bits of the northeast portion of the canyon Lrall. We expect to conclude the mapping of the AC canjron in short order in 2001. when we will initiate mapping the Muklebal valley. We will also probably employ two GPS teams on a constant basis next year in order to ensure that we conclude the survey. We will attempt to begin the second phase of terrace and ridge mapping at that time. Conclusions The 2000 season of the MMAP was another great success. We have essentially completed our cave reconnaissance in the Muklebal Tzul - Ek Xus area. The settlement survey and excavation programs will likely be finished next year. Preliminary soil sampling was finished in the Muklebal valley. Reference phytolith specimens were collected, as were cacao DNA samples, data that may reflect on ancient Maya tree farming. and mammey seeds for sustainable forest product development. Mud turtle and snail DNA were also gathered for studies of the eolutionary mechanisms behind genetic differentiation. Cave microbes were also sampled to see if they exhibit any antibiotic properties. The GPS mapping of the AC Canyon was nearly completed, making for significant progress on our GIs basemap. A number of important finds were made. The cave reconnaissance produced the painted fish pot. the wooden retaining beams, modeled effigy censer. and extraction locus for calcite crystals. The Mukelbal settlement excavations completed the recovey of the serial burials from last year and yielded a useful cache. The Ek Xux settlement excavations produced numerous charcoal fragments for radiocarbon dating and promising midden materials for phytolith extraction. The settlement survey uncovered a second stela plaza in large outlier of Muklebal Tzul and further evidence that the settlement at Muklebal Tzul is more formalized and the distribution of power there more dispersed than at Ek Xux. The season was highly productive.
  • 10. Appendix I: Contemporar~.Plant Specimens Collected for Con~pal-ativePhtolith Anah sis Common Name Family Genusispecies / Basket Vine / Palmae / Destnoncrts schiz?z?ii BreadnutiRamon Cocoa/Chocolate Cedrelu niexicunu Ol'hitiw~cohune Cedar Cohune Pal~n Moraceae Sterculiaceae Melilaceae Palinae 1 Mammey / Sapotaceae 1 Pouteria zapotcr Brosimiutn alicc~s~rzm T/~eohromucucao CopaliPom Gumbolimbo Burseraceae Burseraceae Sapodilla Warrie Cohune P~.otizrnicopal Busserer simaruhu Cow Foot Tapir Foot Sapotaceae Palmae Mcrnilccrra zapota A.s(roccrr.vunirnexicanuni Piperaceae Curcurbitaceae Piper cutri(zcnz Gzra~.anicrnlnkounc/