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ecords.<br />

Vegetation Rscard.<br />

Grass (Graminellel pollen constitutes cs. 601 <strong>of</strong> the Renews<br />

1660-1680 occupation period pallen spectra that were calculated<br />

from the <strong>total</strong> pollen sun (solid bar histogram) and up to 838 <strong>of</strong><br />

the spectra calculated from non-arboreal pollen <strong>only</strong> (bollor bar<br />

histogram). Sorrel-typ (RmY aCet08ellalacero~a-type), at up to<br />

15% <strong>of</strong> the <strong>total</strong> sun, is the second most prominent type. pine<br />

(ELwsJ, at lo% <strong>of</strong> the <strong>total</strong> nun in the exterlor sample (ps 1). is<br />

the third <strong>be</strong>st represented type, and it is followed by dandeliontype<br />

ILiguliflorael, white spruce (Pisaa olauca-type), barel<br />

(-1, and alder (&h&s), at ca. 7%. At least two <strong>of</strong> the<br />

relatively prominent types, dandelion-type and sorrel-type, are <strong>of</strong><br />

European origin.<br />

Herb pollen starts out st a lover altitude than tree pollen.<br />

Wind velocities are lower in this near-ground zone, and the chance<br />

<strong>of</strong> pollen loss from the wind stream thmugh impact with vegetation<br />

IS hlgher. Herb pollen does not, as a consequence, travel as far cia<br />

tree pollen and rends to doninate locally produced pollen spectra<br />

an open spacer (~ansren 1973:33). Graon pollen. moreover, is a good<br />

indicator <strong>of</strong> relative boll stability, <strong>be</strong>cause the perreoiating<br />

organs <strong>of</strong> grasses are destroyed by plavinq and other extensive sail<br />

dlsturbanctls (8ehre 1983:227). Herb pollen, dominated by grass, is<br />

clearly more important than tree pollen in the Renews spectra,<br />

indicating that the area around the site vae relatively open and<br />

roils were relatively stabls during deposition <strong>of</strong> the 17th century<br />

matrices. The extent to which thls varies from the natural, precontact<br />

condition <strong>of</strong> the locality or the normal situation during<br />

the hrstorlcal era cannot <strong>be</strong> determined from the pollen data<br />

without a canpararive roil pr<strong>of</strong>ile.<br />

The historical era spectra in a pollen sequence from a pond on<br />

cape Breton Island (Livingstone and Livingstone 1958:Fiqre 1) have<br />

larger percentages <strong>of</strong> grass, ragweed-type (--type), and<br />

dock/sorrel-type pollen, than the prehistoric counts. This raisss<br />

the possibility rhat the domination <strong>of</strong> the Renews pollen spectra Ly<br />

grass pollen nay <strong>be</strong> at least partially cultural in origin. ~hio is<br />

certainly true <strong>of</strong> the =xoticr, such as sorrel-type and dandelion<br />

type, but most <strong>of</strong> the herbs are more characteristic <strong>of</strong> waste ground<br />

than <strong>of</strong> actively distur<strong>be</strong>d soils. and it is probable rhat the<br />

gmundcover around the Renews structure was relatively continuous.<br />

~01Ian sample 1 from outside the house sontamed 28% arboreal<br />

(tree) pollen vhlle the interior samples 2. 3, and 4 had 11.258,<br />

16.3%, and 98, respectively. Thin contrast <strong>be</strong>tween the exterior<br />

sanple and the interlor samples is large enough to <strong>be</strong> siymificlmt.<br />

There are also differences in the dandelion-type, goldonrod-type,<br />

sorrel-type, red baneterry (u-type Ranunculoceae), and heath<br />

family (Ericaceae) counts <strong>of</strong> the exterlar and interior sampleathat<br />

appear to <strong>be</strong> sysrenaric. Possible explanations are: different<br />

reasons <strong>of</strong> deposition, different activities inside the house than<br />

Outside, different sources far the matrix, different exposure to<br />

the atmosphere, different sedimentation rates (more or less years<br />

'<br />

!<br />

I

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