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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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Among the food plants listed above, Canada plum<br />

(Prunus nigra) may be of particular importance. It<br />

grows wild throughout the province, but is most<br />

densely clustered along the upper Saint John and<br />

Restigouche Rivers, the mouth of the St. Croix River,<br />

and along the lower portion of the Miramichi River<br />

(Gorham 1943:44). The common occurrence of plum<br />

trees at Native sites and the recovery of charred plum<br />

pits at Meductic led Gorham (1943) to suggest that the<br />

prehistoric Native peoples of New Brunswick were<br />

intentionally planting this species around their campsites.<br />

Leonard (1996) recently recovered plum pits<br />

from a Late Prehistoric burial at Skull Island site,<br />

Shediac Bay, and has revived Gorham’s theory concerning<br />

Native arboriculture. Additional evidence for<br />

possible plum arboriculture comes from the discovery<br />

of nine plum pits in a leather pouch that accompanied<br />

a Protohistoric female burial from Northport, Nova<br />

Scotia (Whitehead 1993:45). The Skull Island site also<br />

produced 75 gm of charred groundnut (Apios americana)<br />

tubers (Leonard 1996:144-152). This species was<br />

an important food resource in the Early Historic period<br />

and very likely represents a form of pre-Contact<br />

plant use. Leonard (1996:150-152) presents evidence<br />

that indicates that the groundnut may actually have<br />

been introduced into the Maritimes during prehistoric<br />

times.<br />

Leonard (1995, 1996:168-186) also reviews the evidence<br />

for possible Mi’kmaq horticulture during the<br />

Protohistoric period. He cites Lescarbot’s assertion<br />

that the Mi’kmaq once cultivated corn, beans, and<br />

squashes, only to abandon the practice when they<br />

began to acquire foodstuffs through trade with the<br />

French (Leonard 1996:176). Leonard also cites Pierre<br />

Arsenault’s 1714 account of Mi’kmaq gardens of corn<br />

at Shediac and Richibucto, and John Giles late seventeenth<br />

century account of Maliseet gardens of corn<br />

and storage practices at Meductic (1996:177-180). As<br />

Leonard points out (1996:176), both of these areas had<br />

suitable climatic conditions for corn horticulture,<br />

along with portions of southwestern New Brunswick.<br />

Historic accounts also indicate that the Mi’kmaq were<br />

growing tobacco (probably Nicotiana rustica) during<br />

the early seventeenth century (Leonard 1996:168-174).<br />

Monckton (1997) recently identified corn kernel and<br />

cupule (Zea mays) fragments, and a single possible<br />

tobacco seed from the Jemseg site. Unfortunately, the<br />

cultural context for these specimens is presently<br />

unclear (Susan Blair 2000, pers. comm.), and other<br />

specimens of uncharred squash seeds (Cucurbita pepo)<br />

and a single charred barley seed (Hordeum sp.) are<br />

believed to date to the period of European settlement.<br />

Leonard’s (1996) study provides a provocative<br />

model of Late Prehistoric-Protohistoric plant use. It<br />

begins with a Late Prehistoric hunting and fishing subsistence<br />

strategy, supplemented by the collection of<br />

edible berries, nuts, and roots. This much is consistent<br />

with existing paleoethnobotanical evidence. Some time<br />

during the Late Prehistoric period, plum arboriculture<br />

and tuber management were introduced from outside<br />

the region. This rudimentary form of horticulture prepared<br />

them for the adoption of tobacco, and later, corn<br />

(maize) cultivation. The latter most likely took place<br />

between A.D. 1350 and 1550, in areas suitable for corn<br />

cultivation (Leonard 1996:185). As the volume of<br />

European foodstuffs including peas, beans, biscuits,<br />

and prunes increased, attempts at corn horticulture,<br />

along with plum arboriculture, were abandoned. This<br />

model is very compelling, but much more archaeological<br />

evidence is needed, especially in areas of possible<br />

corn cultivation.<br />

Faunal Resources<br />

Faunal resources utilized by the Late Prehistoric<br />

peoples of New Brunswick include a variety of land<br />

and marine mammals, birds, freshwater and marine<br />

fish, and shellfish. Today, the diversity and richness of<br />

faunal resources varies considerably by ecological<br />

zone within the province. Although the archaeological<br />

record for faunal resources in this province is far<br />

from complete, it demonstrates that this situation also<br />

existed in the Late Prehistoric period when it affected<br />

local patterns of resource exploitation (e.g., Burley<br />

1981:206). There have been over one hundred zooarchaeological<br />

reports written for the Maritime<br />

Provinces (Murphy and Black 1996). These reports<br />

tend to be short research papers, often unpublished,<br />

concerning faunal assemblages from single sites, but<br />

together they give us a glimpse of prehistoric animal<br />

use. Stewart (1989) provides one of the few published<br />

overview papers for this region.<br />

It should be noted that the preservation of archaeological<br />

specimens varies considerably between coastal<br />

and interior locations. Large quantities of shell in<br />

coastal midden sites counteract the acidity of midden<br />

sediments and allow the preservation of a wider<br />

range of organic materials, including mammal, bird,<br />

and fish bones. Bones do not survive well at interior<br />

sites unless they have been exposed to fire. Even then,<br />

some denser bone, such as beaver, survive charring<br />

better than bones of other species (Knight 1985; Spiess<br />

1992), thus influencing the interpretation of faunal<br />

assemblages at interior sites. Evidence of interior<br />

Chapter 17 Aboriginal Land and Resource Use in New Brunswick During the Late Prehistoric and Early Contact Periods 325

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