1974
DOI: 10.1016/0033-5894(74)90006-4
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Late Quaternary Vegetational Changes on the East Side of Yellowstone Park, Wyoming

Abstract: A bog pond 4 km east of Yellowstone Lake has a pollen record starting with an Artemisia spruce assemblage, implying alpine vegetation. A layer of volcanic ash, dated as 14,360 ± 400 BP (probably Glacier Peak or Mt. St. Helens J), occurs within the zone, which terminates at 11,630 ± 180 BP. The rest of the pollen sequence is dominated by lodgepole pine, with reappearance of spruce pollen in modest quantities about 4500 BP, according to dating provided by a layer of Mt. Mazama ash (6600 BP). The present vegetati… Show more

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Cited by 88 publications
(71 citation statements)
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“…The name of each zone carries implications about the ecological conditions at the time of deposition. Similar zones appear in the core from Cub Creek pond (Waddington and Wright, 1970) and other cores (R. G. Baker, unpub.…”
Section: Quaternary Palynology Materials and Proceduresmentioning
confidence: 76%
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“…The name of each zone carries implications about the ecological conditions at the time of deposition. Similar zones appear in the core from Cub Creek pond (Waddington and Wright, 1970) and other cores (R. G. Baker, unpub.…”
Section: Quaternary Palynology Materials and Proceduresmentioning
confidence: 76%
“…18) is tentatively referred to this subzone on the basis of (1) presence of mixed alpine-and subalpine-plant macrofossils, (2) distribution of Betula glandulosa (bog bireh) fruits and catkin scales, and (3) rare presence of arboreal macrofossils. ·The Cub Creek pond sequence (Waddington and Wright, 1970) shows a similar Betula pollen peak at the base of the core.…”
Section: Betula Subzone (960 -875 Em)mentioning
confidence: 97%
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