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• Effects <strong>of</strong> climate change: Kinnikinnick is likely at low risk to climate change as it is<br />

adapted to droughty sites across BECs. However, it is sensitive to moderate and severe<br />

fires.<br />

Sheperdia Canadensis (soapberry)<br />

• Ecology: Sheperdia is widespread<br />

in dry to moist openings and clearings<br />

• Effects <strong>of</strong> climate change: Sheperdia<br />

will likely expand into areas as they get drier.<br />

Veratrum virid e (Indian Hellebore)<br />

• Ecology: Hellebore is wide spread and most abundant subalpine elevati<strong>on</strong>s <strong>on</strong> wet seepage<br />

sites.<br />

• Effects <strong>of</strong> climate change: Hellebore is at risk as it has a preference for wet seepage sites<br />

with cold air drainage.<br />

Ledum groenlandicum (Labrador tea) and Ledum glandulosum (Trapper tea)<br />

• Ecology: Most comm<strong>on</strong> in colder mid to high elevati<strong>on</strong>s in the Chilcotin. Often dominating<br />

bogs and cold wetland fringes. Absent in hot arid climates.<br />

• Effects <strong>of</strong> climate change: At risk as climate becomes warmer and drier. Persistence may<br />

depends <strong>on</strong> what BEC it is in, i.e. the colder (higher) and wetter the ecosystem is now the<br />

l<strong>on</strong>ger it will persist.<br />

5.3. Wildlife & Wild Horses<br />

This secti<strong>on</strong> provides a summary <strong>of</strong> the larger Study Background Report <strong>on</strong> wildlife and wild horses<br />

prepared by Wayne McCrory, RPBio. For the full report, please see Annex 3.<br />

Past and present exogenous and climate­related impacts <strong>on</strong> wildlife and wild horse habitats<br />

Impact <strong>of</strong> climate change <strong>on</strong> wildlife is not a new phenomen<strong>on</strong>. Indeed, the effects <strong>of</strong> l<strong>on</strong>g‐term<br />

climate variati<strong>on</strong>s can be observed dating back to the last Ice Age <strong>on</strong> three <strong>of</strong> the indicator species<br />

that are currently found in the XGCA: (i) the mountain goat; (ii) the wild horse; and (iii) moose.<br />

• Mountain Goat ­ Until about 8,000 years ago, there were mountain goats <strong>on</strong> Vancouver Island.<br />

Yet, they went extinct at that time, apparently because <strong>of</strong> global warming (temperatures<br />

higher than today), which caused fragmentati<strong>on</strong> and loss <strong>of</strong> the goats’ alpine habitat, which, in<br />

turn, was a result <strong>of</strong> the treeline expanding upward in elevati<strong>on</strong>.<br />

• Wild Horses ‐ The horse species, which evolved in North America (and even existed <strong>on</strong><br />

Vancouver Island) also went extinct about 8,000 years ago, but for unknown reas<strong>on</strong>s. It was<br />

later re‐introduced by the Spaniards to the Americas in the 1500s, and was brought<br />

northward by First Nati<strong>on</strong>s. As a result, it arrived in the XGCA before the Europeans did, about<br />

200+ years ago.<br />

• Moose ­ The moose did not arrive in the Chilcotins until about 90 years ago as a result <strong>of</strong> a<br />

gradual, southward range expansi<strong>on</strong> from refugia in the Yuk<strong>on</strong> during the last Ice Age.<br />

In more recent time (the past couple <strong>of</strong> decades), the wildlife and wild horse habitats within the<br />

XGCA have been negatively impacted by a range <strong>of</strong> factors, including both exogenous and climate‐<br />

related <strong>on</strong>es. The most significant climate‐related factors have been massive pine beetle<br />

40

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