The pollen analysis of two sediment cores from Oil Lake, in the eastern foothills of the Brooks Range, and Feniak Lake, in the Noatak River drainage, reveal late Wisconsin and Holocene vegetation changes. These cores exhibit alternative trends in the development of the modern tundra biome. At Oil Lake, a long birch/herb zone with little fluctuation is followed by a rapid rise in sedge, which is then followed by a birch zone and an alder zone. There is a drop in birch pollen at the late glacial/Holocene boundary, with a rise in sedge and Nymphaea, an indication of the increase in moisture at the end of the late glacial. Feniak Lake yields a detailed history of Holocene vegetation change that includes an early Alnus pollen rise during the Birch Zone, indicating local expansion of alder in the Noatak River region.
Late Quaternary Pollen Records from Oil Lake and Feniak Lake, Alaska, U.S.A.
Published 1992 in Arctic and Alpine Research
ABSTRACT
PUBLICATION RECORD
- Publication year
1992
- Venue
Arctic and Alpine Research
- Publication date
1992-02-01
- Fields of study
Geology, Environmental Science
- Identifiers
- External record
- Source metadata
Semantic Scholar
CITATION MAP
EXTRACTION MAP
CLAIMS
CONCEPTS
- alder pollen
Pollen produced by alder, identified in the record as Alnus pollen.
Aliases: Alnus pollen
- birch pollen
Pollen produced by birch taxa and used as a vegetation indicator in the cores.
- feniak lake
A lake in the Noatak River drainage that provided the other analyzed sediment core.
- late glacial/holocene boundary
The transition interval between the late glacial and Holocene portions of the sediment records.
- modern tundra biome
The present-day tundra vegetation regime reconstructed from the lake pollen sequences.
- nymphaea
A water-lily genus whose pollen in the cores marks wetter, more open-water conditions.
- oil lake
A lake in the eastern foothills of the Brooks Range that provided one of the analyzed sediment cores.
- sedge
Sedge vegetation represented in the pollen record, used as an indicator of tundra or wetland conditions.
REFERENCES
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CITED BY
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