Ancient Maya subsistence diversity: root and tuber remains from Cuello, Belize.
Hather, Jon G. ; Hammond, Norman
A first notice of the mushy element in the subsistence base of the
Maya realms.
Introduction
The question of prehispanic subsistence in the Maya lowlands has been
vigorously debated, since the assessment of Classic Maya (AD 250-900)
structural development, particularly in terms of urbanism, has hinged,
somewhat precariously, on the nature of their subsistence economy. A
model based on retrodiction of the historic regime of swidden or milpa
agriculture of predominantly maize, beans and squashes (e.g.. Morley
1946: 441-2) did not easily account for the population densities and
proportion of non-farmers projected for Classic cities such as Tikal
once survey revealed their unexpected size (Carr & Hazard 1961).
Bronson (1966) therefore reconsidered the subsistence economy of
Classic Maya lowland society, suggesting the supplementation of maize
with root crops: in this model agricultural yield is sufficiently
increased and nutritionally enhanced to meet the needs of a population
of greater density than would be possible under a standard milpa regime.
Bronson considered that documentary and botanical evidence for four
crops -- the sweet potato or camote (Ipomoea batatas); yam bean or
jicama (Pachyrrhizus erosus); manioc (cassava, yuca) (Manihot
esculenta); and malanga (yautia) (Xanthosoma spp.) -- suggested that the
Maya region was a centre for either domestication or diversification. He
argued that the Maya had a variety of root crops available to them
before the colonial age, and arguably in the Classic Period. Marcus
(1982) argued instead for a much later, post-Columbian introduction of
three of these root crops, while admitting that a Classic Maya knowledge
of wild roots and tubers, particularly for use as famine foods, may have
been comprehensive. Pachyrrhizus, she suggests, was likely to have been
a Postclassic (AD 900-1500) introduction and possibly a famine food.
Pachyrrhizus erosus is a very fleshy leguminous root crop and by
virtue of its anatomy -- large thin walled parenchyma cells, sparsely
distributed xylem vessels, high water content -- may be eaten without
preparation or cooking; modern consumption is raw, as a snack or salad.
These characters are not conducive to good preservation by charring:
cellular characters will be largely destroyed by the expansion and
release under pressure of water contained in the tissues; the resulting
carbonized remains will be extremely fragile, almost certainly unable to
survive most post-de-positional environments. Ipomoea batatas has been
recovered from archaeological contexts (Rosendahl & Yen 1972; Hather
& Kirch 1992), though not in the Maya lowlands; although variable in
its morphology and anatomy, it is often not difficult to identify even
from highly fragmented remains. The whole of the tuber is eaten,
however, usually without preparation before cooking by boiling, steaming
or roasting: the likelihood of its presence in the archaeological record
is low. Different varieties of Manihot esculenta are boiled, or grated
and dried into flour. Detecting its prehispanic utilization is
inextricably bound up with the preservation of identifiable remains from
such culinary practices; we report here the results of recent research
at the Preclassic Maya site of Cuello, Belize, which advance our
knowledge of ancient Maya root crop utilization.
Cuello is a small site located on the limestone ridge between the Rio
Hondo and Rio Nuevo in northern Belize at 18 [degrees] 05' N, 88
[degrees] 35' W. Excavations between 1975 and 1993 have documented
occupation from c. 1200 BC onwards, the earliest settlement known in the
Maya lowlands, and a cultural development leading to the emergence of a
complex Late Preclassic society after 400 BC (Hammond 1991). Floatation
of more than 10 tonnes of soil recovered numerous plant macrofossils,
which have been used to reconstruct the Preclassic environment and
economy (Miksicek 1991). More than 1100 maize cupule and kernel
fragments were recovered (Miksicek et al. 1981), together with
carbonized fruits and/or wood from trees yielding edible crops such as
avocado. Explanations for the virtual absence of root crops from the
flot samples have been discussed by Miksicek (1991: 80).
Recovery and identification of carbonized root crop remains from
humid tropical soils elsewhere (Hather 1991) led to a renewed attempt to
resolve the problem of whether the Maya had cultivated them. Plant
remains, preserved by charring, were recovered from midden deposits at
Cuello in 1992 by on-site flotation and laboratory-based deflocculation
and by wet sieving of five-litre bulk samples. Both resulted in the
recovery of similar assemblages, but the materials recovered in the
laboratory were less fragmented and eroded, allowing greater chance of
identification. A combination of flotation and more careful
laboratory-based separation is necessary to recover a complete
assemblage of charred plant remains from archaeological contexts.
Analysis concentrated on the recovery and identification of soft
tissues or parenchyma. Most root crops, certainly the ones under
discussion here, are composed largely of parenchyma, a tissue comprising
often large, thin-walled cells whose function is the storage of starch
and related compounds. Possible fragments of such tissues were pressure
fractured to obtain a clean, uneroded surface and examined under
scanning electron microscopy. Comparative material from modern Maya
root-crops was experimentally charred and examined in the same way, as
well as being thin-sectioned and stained for transmitted light
microscopy. Identifications were based upon anatomical and morphological
characters of the type outlined by Hather (1991; 1993).
Parenchymatous tissues at Cuello
Ten samples were examined for charred plant remains. Six, from
samples associated with the Early Middle Preclassic period (Swasey
(1200-900 BC) and Bladen Xe (900-600 BC) ceramic complexes), and the
Late Middle Preclassic period (Lopez Mamom ceramic complex (650-400 BC))
yielded the remains of three distinct classes of parenchymatous tissues:
Unidentifiable fragments of parenchymatous tissues, possibly derived
from root or tuber tissues, but which could equally be derived from
large seeds (for example the ramon or breadnut, Brosimum alicastrum),
large fruits or other fleshy plant organs. These will not be considered
further.
sample categories of parenchymatous tissue
no. 1 2 3
4415 + - -
4440 + + -
4448 + - +
4457 + + +
4458 + - +
4490 + + -
1 = unidentifiable remains
2 = cf. Xanthosoma sp.
3 = Manihot esculenta
TABLE 1. Occurrence of different categories of parenchymatous plant tissues
recovered from samples at Cuello.
Partially vesicularized parenchymatous tissue with approximately
one-third recognizable cellular tissue. Vascular tissue is in small
amphivasal concentric to possible collateral bundles with breakdown of
phloem to solid carbon. Tissue preservation and its organization is very
similar to Araceous tissues recovered from the Pacific (Hather &
Hunt, forthcoming) and to modern reference material of Xanthosoma
(FIGURES 1 (archaeological) & 2 (modern)).
Well preserved narrow lengths of root tissue with epidermis. The
anatomical structure of these fragments indicated a root structure with
characters of both the secondary xylem (largely parenchymatous) and
phloem well preserved. Morphological and anatomical characters identify
them as parts of narrow roots attaching the root tubers of Manihot
esculenta to the main axis of the plant. Interestingly, this part would
naturally be discarded in preparing the tuber for cooking (FIGURES 3
(archaeological) & 4 (modern)).
Of these identifications that of Xanthosoma is the less certain.
Characters of its anatomy suggest this identification, but whether it
was cultivated (and inferentially domesticated?) or collected cannot be
determined. As other Araceous taxa that exist in the wild in the Cuello
area have not been examined as reference material, identification stands
as a possibility rather than a certainty. The identification of Manihot
esculenta is of greater certainty, because the tissues are better
preserved and more complete. Marcus (1982, citing Rogers 1963) states
that Manihot esculenta does not occur in its wild form in the Maya area.
If that is correct, this identification must perforce document
cultivation of manioc by the Preclassic Maya.
Six samples included unidentifiable tissues; three yielded the
remains of the possible Xanthosoma and three those of Manihot esculenta;
one sample yielded unidentifiable tissues only, and one sample yielded
both of the identified categories; maize was recovered at Cuello at an
82% ubiquity, though from a much larger range of samples (Miksicek
1991). The remains under discussion here were derived from a relatively
small sample size and therefore the comparison of ubiquity is not
statistically viable, but indications are that root and tuber ubiquity
is approximately two thirds that of maize remains.
One sample of Manioc was submitted to the Oxford University
Accelerator Unit for AMS dating with the following result: 2450[+ or
-]70 b.p. (OXA-4452) which at 0.77 probability lies between 700 BC and
531 BC at 1[Sigma] level (0.23 probability for 800-753 BC); and with
0.94 probability between 808 and 475 BC at 2[Sigma] level (R. Housley
pers. comm). These determinations are compatible with other AMS dates
from occupation material and burials from the Middle Preclassic period
at Cuello.
Conclusions
This analysis of plant remains from Cuello was directed at the
recovery and identification of root and tuber tissues with direct
reference to the question of whether Classic Maya subsistence economy
could have been, at least partially, based on root crops. We have found
Cuello assemblages to contain tissues derived from roots and tubers
including one and perhaps two of the four root crops identified by
Bronson (1966) in his model of Classic Maya subsistence economy. The
relative importance of root and tuber foods and of maize cannot easily
be determined from such archaeological data. Use of foods in the past
will have altered from year to year, depending on crop success and minor
variations in cultural preference. The accuracy of the archaeological
record in representing the past depends on factors of preservation and
post-depositional taphonomy. The comparison of such data quantified in
terms other than that of ubiquity poses an enormous problem to
archaeobotanists.
The nature of the involvement of roots and tubers in past subsistence
patterns in the lowland Maya area depends on the particular species
grown. Pachyrrhizus erosus, Ipomoea batatas and Xanthosoma spp. may be
grown in gardens with other crops such as maize, and the yield of either
would only increase proportionately to the area of land devoted to their
cultivation if grown as a monocrop. Manihot esculenta, a large bushy
crop commonly grown on relatively poorly prepared ground, is unlikely to
have been grown in a multi-cropping system. In this respect manioc is
likely to have been grown in rotation with other crops either following
a fallow period and prior to a maize crop, or following maize and prior
to fallow. A subsistence system relying on a variety of root crops and
maize, beans and squash would probably be based on both relatively
permanent house gardens growing a wide variety of crops possibly
including Xanthosoma spp., Ipomoea batatas and Pachyrrhizus erosus, as
well as manioc and maize rotating in milpa swidden fields.
Acknowledgements. Funding for this study was provided by the Science
and Engineering Research Council, Institute of Archaeology, University
College London, and Boston University. The Cuello excavations were
funded principally by the National Geographic Society and Boston
University. We thank Amanda Clarke, site director at Cuello in 1992, and
David R. Harris, Director of the Institute of Archaeolog}, for practical
and fiscal assistance, and Rupert Housley and Robert Hedges of the
Oxford University Radiocarbon Accelerator Unit for AMS dating.
References
BRONSON, B. 1966. Roots and the subsistence of the ancient Maya,
Southwestern Journal of Anthropology 22: 251-79.
CARR, R.F. and J.E. HAZARD. 1961. Map of the ruins of Tikal, El
Peten, Guatemala. Philadelphia (PA): University of Pennsylvania Museum.
Tikal Report 11.
HAMMOND, N. (ed.). 1991. Cuello: an early Maya community in Belize.
Cambridge: Cambridge University Press.
HATHER, J.G. 1991. The identification of charred archaeological
remains of vegetative parenchymatous tissues, Journal of Archaeological
Science 18: 661-75.
1993. An archaeobotanical guide to root and tuber identification 1:
Europe and South West Asia. Oxford: Oxbow. Monographs in Archaeology 28.
HATHER, J.G. & T. HUNT. Forthcoming. Prehistoric taro (Colocasia
esculenta) from Hawaii.
HATHER, J.G. & P.V. KIRCH 1992. Prehistoric sweet potato (Ipomoea
batatas) from Mangaia Island, Central Polynesia, Antiquity 65: 887-93.
MARCUS, J. 1982. The plant world of the 16th- and 17th-century Maya,
in K.V. Flannery (ed.), Maya subsistence: studies in memory of Dennis E.
Puleston: 239-67. New York (NY): Academic Press.
MIKSICEK, C.H. 1991. The ecology and economy of Cuello I: the natural
and cultural landscape of Preclassic Cuello, in Hammond (1991): 70-84.
MIKSICEK, C.H., R.M BIRD, B. PICKERSGILL, S. DONAGHEY, J. CARTWRIGHT
& N. HAMMOND. 1981. Preclassic lowland maize from Cuello, Belize,
Nature 289: 56-9.
MORLEY, S.G. 1946. The ancient Maya. Stanford (CA): Stanford
University Press.
ROGERS, D.J. 1963. Studies of Manihot esculenti Crantz, and related
species, Bulletin of the Torrey Botanical Club 90: 43-54.
ROSENDAHL, P & D.E. YEN. 1972. Fossil sweet potato remains from
Hawaii, Journal of the Polynesian Society 80: 379-85.