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Northeast Subsistence-Settlement Change: A.D. 700 –1300

Northeast Subsistence-Settlement Change: A.D. 700 –1300

Northeast Subsistence-Settlement Change: A.D. 700 –1300

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or earlier in interior southwestern Maine in the Saco<br />

River Valley. In Figure 13.5, the data point for maize<br />

(0.01 frags. >2 mm/g) at 810 B.P. at the Little Ossipee<br />

North site represents a mean date; a direct date for<br />

maize at that site was 570 B.P. for a fragment found in<br />

a feature dating to 1010 B.P. A greater quantity and<br />

variety of seeds is generally recovered from Maine<br />

sites after about 1000 B.P., which is an indication that<br />

the activities associated with agriculture had an effect<br />

on the surrounding plant communities (Asch Sidell<br />

1999d).<br />

Indicator species that may be associated with maize<br />

agriculture are considered in more detail in the<br />

Memorial Park site and Tracy Farm site discussions<br />

below.<br />

EVIDENCE OF ANTHROPOGENESIS<br />

Many archaeological sites provide evidence of<br />

anthropogenesis, since plant foods tend to be most<br />

concentrated and most easily collected from open or<br />

disturbed areas. Focusing upon changes that may<br />

have occurred with the adoption of maize agriculture,<br />

there are certain indicator species that are associated<br />

with maize at the Memorial Park and Tracy Farm<br />

sites. Selected data are also presented from two sites<br />

in southcentral New York, for which there is possible<br />

evidence of landscape alteration by the use of fire.<br />

Memorial Park Site<br />

The clearest evidence of anthropogenesis is found<br />

at the deeply stratified Memorial Park site in<br />

Pennsylvania, where a large increase in seed density<br />

is associated with the presence of maize agriculture<br />

and the growing of some species of the Eastern<br />

Agricultural Complex (Figure 13.5). Of the Late<br />

Woodland (A.D. 760-1385) seeds, two-thirds were<br />

those of native cultivated plants, including little barley,<br />

two domesticated forms of Chenopodium<br />

berlandieri, tobacco, and possibly sunflower, although<br />

the single sunflower kernel was wild-sized.<br />

Altogether 64 percent of the identifiable seeds were<br />

little barley (Hordeum pusillum), which occurred in<br />

more than half of the 46 samples containing seeds.<br />

Among the fleshy fruits and berries was black nightshade<br />

(Solanum americanum). Black nightshade was<br />

associated with a period of intensive agriculture in<br />

westcentral Illinois and the American Bottom (D. Asch<br />

and N. Asch 1985a:388-389). Since it has not been<br />

recorded from Archaic sites, it is presumed that disturbances<br />

associated with prehistoric agriculture permitted<br />

an increase in the abundance of black nightshade.<br />

Today, black nightshade is widely distributed in open<br />

and disturbed habitats (Magee and Ahles 1999). At the<br />

Memorial Park site, black nightshade represented 52<br />

percent of the fruit and berry seeds in the Late<br />

Woodland features.<br />

Another possible indicator of anthropogenesis at<br />

the Memorial Park site is a substantial increase in the<br />

percentage of oak and hickory wood charcoal coincident<br />

with the appearance of maize agriculture.<br />

Sample size is not equal for each data point in Figure<br />

13.5. The largest samples of wood charcoal are 605 fragments<br />

for the Terminal Archaic Canfield (2100-1640<br />

B.C.) component and 150 fragments for the Early<br />

Clemson Island (A.D. 760-830) component. The<br />

amount of oak and hickory wood charcoal for these<br />

components is 47.93 percent and 88.33 percent, respectively.<br />

The increase in oak and hickory wood is accompanied<br />

by an increase in the nutshell index from 2.05 in<br />

the Terminal Archaic Canfield to 5.61 in the Early<br />

Clemson Island, as predicted by the nut tree–nutshell<br />

model presented earlier. There was also an increase in<br />

the seed index from 0.03 to 2.12 seeds per gram of charcoal,<br />

indicating more open habitat for seed collection in<br />

the Early Clemson Island occupation.<br />

Tracy Farm Site<br />

In Maine, the Norridgewock Mission study compared<br />

archaeobotanical evidence with historic<br />

accounts of plant use to serve as a baseline for assessing<br />

prehistoric plant assemblages (Asch Sidell 1996a).<br />

At the Tracy Farm site across the river from<br />

Norridgewock Mission, there were differences in the<br />

plant remains through time (Asch Sidell 2000d).<br />

Among the three features that were unquestionably<br />

attributed to the Middle Woodland (200 B.C.-A.D.<br />

600) 2 occupation, there was a lack of nutshell, seeds,<br />

and domesticated plants. However, because of collection<br />

techniques, only one of the samples could have<br />

been expected to contain seeds or nuts. Most of the<br />

Late Woodland/Contact (A.D. 1300-1690) 2 features at<br />

the Tracy Farm site contained a mixture of various<br />

seeds and nutshell. All types of nuts that grew in the<br />

area were recovered in small quantities from the Late<br />

Woodland and/or Contact occupations of the Tracy<br />

Farm site, and the nutshell occurred ubiquitously in<br />

81 percent of the features. Of 32 Late Woodland or<br />

Contact features, 21 (or two-thirds) contained maize,<br />

5 had squash/pumpkin rind, 3 had wheat, and 1 contained<br />

bean. One wild-sized sunflower seed was also<br />

250 Sidell

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