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Northern hardwood forests in lower mountain ranges could be eliminated if their zone shifts <br />upward too far. Those in higher ranges are unlikely to be eliminated, but their extent will become <br />more limited. Loss of lower elevation portions of patches will increase fragmentation to some <br />degree. Some patches that now are connected may become isolated if the lower elevation limit <br />rises. Patches in different mountain ranges are already naturally isolated by the warmer climate <br />at lower elevations. These communities were presumably shifted upward in elevation during the <br />Hypsithermal period, and those on lower ranges may have been eliminated then. There is likely to <br />be little additional wholesale loss of communities or species until the climate becomes warmer than <br />the Hypsithermal. The Hypsithermal was drier as well as warmer, and if our future climate is not <br />drier, the change may be less. However, having more severe drought and increased fire frequency <br />may be sufficient to cause substantial changes even if the average rainfall does not change. <br />Effects of reduced area and fragmentation may be significant, reducing some species populations <br />enough to cause demographic problems. Because the current area is limited, some species <br />populations are likely already small enough to be close to demographic problems. <br />Habitat Level Effects: <br />Natural Communities: <br />Third Approximation Name: Comments: <br />Boulderfield Forest Tied to distinctive sites, these communities will generally not be able <br />to migrate at all. A few new examples may develop, where bouldery <br />sites are currently covered with spruce -fir, as at Grandfather Mountain. <br />The distinctive boulderfield environment is occupied by the Boulderfield <br />Subtype of Rich Cove Forest at lower elevations, and this community <br />will spread into some of the lower elevation Boulderfield Forests. Some <br />Boulderfield Forests have substantial seepage. Droughts may be a <br />threat to seepage and disrupt the water- dependent component of the <br />community. <br />Northern Hardwood Forest (Beech Gap Subtype) Tied to distinctive microsites -- either high elevation gaps or high <br />elevation peaks that might otherwise have spruce -fir. Both may be <br />particularly vulnerable to warming climate. The most likely community <br />to develop in their place would be typic Northern Hardwood Forest. <br />Northern Hardwood Forest (Typic Subtype) Usually occurs in large patches. Patches will likely migrate uphill and <br />shrink but most are unlikely to be eliminated. <br />Appendix B 177 <br />