CPAWS CANADIAN PARKS AND WILDERNESS SOCIETY YUKON CHAPTER THE PEEL RIVER WATERSHED: ECOLOGICAL CROSSROADS AND BERINGIAN HOTSPOT OF ARCTIC AND BOREAL This report was produced BIODIVERSITY by the Yukon Chapter of the Canadian Parks & Wilderness Society with the support and participation of the Yellowstone to Yukon Conservation Initiative. Jedediah F. Brodie11,, JoelJoel BergerBerger22 1David H. Smith Conservation Research Fellow Faculty Affiliate, Wildlife Biology Program University of Montana Missoula, MT 59801, USA
[email protected] 2John J. Craighead Chair and Professor of Wildlife Biology Division of Biological Sciences University of Montana Missoula, MT 59801, USA [
[email protected] ] [ Grizzly bears feeding. Photo: Peter Mather ] TABLE OF CONTENTS Summary 1 Part I: Nexus of floral and faunal interchange 4 Preface Beringia 4 The ice-free corridor 8 Current biota of the Peel River watershed 11 Part II: Biogeographically unique organisms of the Peel 13 Habitat features 14 Fish 14 Terrestrial vertebrates 16 Invertebrates 17 Plants 18 Fungi 19 Part III: Conclusions 21 Acknowledgements 22 Table 23 Literature Cited 27 ii SUMMARY The Peel River watershed of … the only large the Yukon Territory is a hotspot tracts of the ancient of arctic and boreal biodiversity realm of Beringia to in Canada. Essentially the be found in Canada only large tracts of the ancient are in the upper Peel realm of Beringia to be found River drainage and in Canada are in the upper surrounding areas Peel River drainage and such as the surrounding areas such as the [ Porcupine Basin. ] Porcupine Basin. During the Pleistocene glaciations, the steppes of Beringia stretched contiguously from Ice dams formed during the Pleistocene blocked the flow of the Peel River on several occasions, causing it to switch its flow to drain west into the Yukon River.