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From: on behalf of Panel Registry Subject: FW: TNG registration of ...
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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 />
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