Bush, Leslie (Glenn A. Black Laboratory of Archaeology, Indiana
University, Bloomington)


PLANT USE BY THE OLIVER PHASE PEOPLE; PRELIMINARY RESULTS FROM
THE CLAMPITT SITE


Little is known about the paleoethnobotany of Oliver Phase sites, but it is hoped that research undertaken this summer at the Clampitt site (12 Lr 329) will help fill that gap. This paper presents preliminary data from plant remains recovered primarily through flotation, with comments on historically documented uses of those plants and a comparison of Clampitt plant remains to those at a similar site of the Fort Ancient Anderson Phase.

A total of 31 flotation samples were obtained from 24 features, ranging in volume from 12.5 liters to 22.0 liters. Samples were processed in a machine-assisted flotation device, the Indiana Machine, which had been updated and improved by Bret Ruby. The extremely sandy soil at the Clampitt site necessitated use of a 1.0 mm heavy fraction screen in the flotation device, even though a screen of less than 0.5 mm is standard. While this does not affect the light fractions in any way, some charred remains less than 1.0 mm in diameter may have been lost from the heavy fractions during flotation.

Preliminary analysis of the recovered remains was carried out using on procedures adapted from Mollie Toll. All samples were sifted through geologic screen to separate them into four size categories. Remains greater than 2.0 mm were completely sorted by hand under an illuminated magnifying glass. In this size category, as in all others, uncharred remains were rejected as modern contaminants. Size categories between 1.0 mm and 2.0 mm and between 0.5 mm and 1.0 mm were scanned under a light microscope for 10 minutes each and all charred seeds, rind, and nutshell removed. This process has been completed for 29 of the light fractions (representing 536 liters of soil) and the data presented here come from these light fractions.

Before turning to the results of the analysis, some cautions are in order: First, these are preliminary data. While the range of plant types identified is not expected to increase greatly -- if at all -- during further investigations, some changes in distribution are to be expected. For this reason, I felt it preliminary to calculate wood/nut and nutshell/seed ratios at this time.

Second, with few exceptions, plant types have been identified to the genus level only, as Deborah Pearsall and others caution against over-specific identification.

Third and most importantly, the range of plant remains found though flotation represents only what was available to the Oliver Phase people and not necessarily what they used or the proportions in which they used them. Accidental deposition, food preparation and disposal techniques, and differential preservation bias the botanical record.

As shown in Figure 3, 24 genera of plants were recovered through flotation. While woods and nutshell have not yet been analyzed, it appears that wood is dominated by hardwoods. Nutshell remains include hickory, walnut, and acorn.

Tropical cultigens clearly dominate the plant remains. Maize (Zea mays) is the most common of the tropical cultigens on the site -- both in terms of number of pieces found and ubiquity. Only one corn cob was found; it appears to be an eight-rowed specimen. Beans (Phaseolus), though not as numerous as maize, are well distributed throughout the site.

Five of the other plant types found on the site are generally thought to have been cultigens or quasi-cultigens at some point during prehistoric times. They are: goosefoot (Chenopodium), knotweed (Polygonum), pigweed (Amaranthus), little barley (Hordeum), and maygrass or canarygrass (Phalaris).

Wild plant types recovered are: sumac (Rhus), purslane (Portulaca), pokeweed (Phytolacca), blueberry (Vaccinium), blackberry (Rubus), catchfly (Silene), bedstraw or goosegrass (Galium), panicgrass or witchgrass (Panicum), grape (Vitis), wild black cherry (Prunus serotina), wild plum (P. americana), honeylocust (Gleditsia triacanthos), pawpaw (Asimina triloba), carpetweed (Mollugo), winterberry (Ilex), ragweed (Ambrosia), and copperleaf (Acalypha).

The range of species found at the Clampitt site provide limited information about seasonality: Almost all of the seeds mature in late summer through late fall. However greens are available in the early to late spring, indicating that the recovered botanical remains were harvested between early spring and late fall. It should be remembered that this scenario assumes that most plant remains found were deliberately introduced to the site. Another complicating factor is that the season of harvest is not necessarily the same as season of use and deposition.

In general, botanical data provide support for recent work by Bob McCullough and Brian Redmond showing that the Oliver phase people lived in ways similar to the better-known Fort Ancient peoples. An Anderson Phase Ft. Ancient site, the Incinerator site (also called "Sunwatch Village") served as a conceptual model for students during the field school. Because of this, and because Gail Wagner has recently analyzed the botanical remains from that site, it serves as the basis for comparison here.

The botanical profiles of the two sites are very similar. Both are dominated by maize and beans, and both share a similar range of smaller seeds. The three most common smaller seeds at both sites are: goosefoot, purslane, and sumac. The primary differences are the presence of blueberry and catchfly at the Clampitt site and nightshade at the Incinerator site. A simple regression analysis of the small seeds gives an r-squared value of 0.75. A second regression analysis was performed after removing genera for which a total of five or fewer seeds were recovered from both sites to eliminate undue influence from seeds present in such small numbers that they are likely to have been introduced accidentally. The r-squared value for that second correlation is still 0.71, indicating a strong correlation between the types and relative amounts of seeds on the sites.

Even though the tropical cultigens are clearly the most numerous plant types found at both sites, some interesting differences emerge. Maize was found in all Incinerator trash pits, yet it appeared in only 71% of Clampitt features. In contrast, beans were found in more of the Clampitt features. Possibly, this represents functional differentiation of middens at the Incinerator Site, or a difference in food preparation and/or disposal techniques at the two sites. But it also may represent a real difference in the amount of maize and beans consumed at the two sites.

In sum, botanical remains from the Clampitt site reveal a typical Fort Ancient susistence pattern -- exactly as one would expect from an Oliver phase site. But they also show some interesting divergences from the pattern at the very similar Incinerator site which warrant further investigation.

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Created: July 25, 1996
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Copyright 1996, Glenn Black Laboratory of Archaeology and The Trustees of Indiana University
Last updated: September 15, 2003