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Bluefish Caves (Figure 1), located 54 km southwest of the village of Old Crow in northern Yukon has yielded evidence of episodic human activity from about 25,000 to 12,000 BP (radiocarbon years before present). It may be the most significant of Late Pleistocene Eastern Beringian and Canadian cave faunas because the caves contain: (1) in situ evidence for the earliest people in North America; (2) a well-marked transition between Pleistocene (approximately 2 million to 10,000 years ago) and Holocene (about the last 10,000 years) sediments, flora and fauna; and (3) remains of a substantial variety of both smaller and larger mammals adapted to northern conditions, as well as migratory birds, that lived during the last...
An ecological assessment of the Sambaa K'e Candidate Protected Area (SKCPA) and vicinity is required as part of the Northwest Territories Protected Area Strategy. This report presents the results of an aerial survey that was conducted in March 2009 as part of the Phase 2 ecological assessment. It includes observations of moose, boreal caribou, beaver, wolf, and wolverine.--Includes text from document.
Bluefish Caves (Figure 1), located 54 km southwest of the village of Old Crow in northern Yukon has yielded evidence of episodic human activity from about 25,000 to 12,000 BP (radiocarbon years before present). It may be the most significant of Late Pleistocene Eastern Beringian and Canadian cave faunas because the caves contain: (1) in situ evidence for the earliest people in North America; (2) a well-marked transition between Pleistocene (approximately 2 million to 10,000 years ago) and Holocene (about the last 10,000 years) sediments, flora and fauna; and (3) remains of a substantial variety of both smaller and larger mammals adapted to northern conditions, as well as migratory birds, that lived during the last...
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Tags: M1-Changes in Plant and Animal Distributon,
M1-Fauna
Bluefish Caves (Figure 1), located 54 km southwest of the village of Old Crow in northern Yukon has yielded evidence of episodic human activity from about 25,000 to 12,000 BP (radiocarbon years before present). It may be the most significant of Late Pleistocene Eastern Beringian and Canadian cave faunas because the caves contain: (1) in situ evidence for the earliest people in North America; (2) a well-marked transition between Pleistocene (approximately 2 million to 10,000 years ago) and Holocene (about the last 10,000 years) sediments, flora and fauna; and (3) remains of a substantial variety of both smaller and larger mammals adapted to northern conditions, as well as migratory birds, that lived during the last...
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