Boreal ecosystem development in the Northwestern Alaska range since 11,000 yr B.P.

Feng Sheng Hu, Linda B. Brubaker, Patricia M. Anderson

Research output: Contribution to journalArticle

Abstract

Analyses of pollen, plant macrofossils, macroscopic charcoal, mollusks, magnetic susceptibility, and geochemical content of a sediment core from Farewell Lake yield a 11,000-yr record of terrestrial and aquatic ecosystem changes in the northwestern foot-hills of the Alaska Range. Between 11,000 and 8500 yr B.P., the regional landscape was dominated by a Betula shrub tundra, in which Populus-Salix communities were common. Abundant charcoal in sediments indicates that fires were common in the lake catchment during this period, and high mineral accumulation rates, allogenic elemental content, and magnetic susceptibility suggest intense soil erosion. In addition, mollusks, pollen and macrofossils of aquatic macrophytes, and biogenic silica provide evidence that the lake was substantially shallower and more productive 11,000-8500 yr B.P. than later. Low lake level and high aquatic productivity might have been caused by warm and dry summers associated with early postglacial insolation maximum in northern high latitudes. About 8000 yr B.P., Picea glauca arrived within the lake catchment, forming a forest tundra association until ca. 6000 yr B.P. Alnus shrub thickets established in the region ca. 6500 yr B.P., and Betula papyrifera arrived ca. 6000 yr B.P. Closed P. glauca forests developed ca. 6000 yr B.P. Picea mariana became important subsequently and replaced P. glauca as the dominant tree species in the region ca. 4000 yr B.P. An increase in authigenic Fe/Mn ratios suggests that the development of waterlogged soils accompanied this vegetation change. Fires increased in importance at this time and might have accelerated soil erosion. The establishment of P. mariana forests probably reflected complex responses of forest ecosystems to the onset of cooler and wetter climate conditions during the late Holocene.

Original languageEnglish (US)
Pages (from-to)188-201
Number of pages14
JournalQuaternary Research
Volume45
Issue number2
DOIs
StatePublished - Mar 1996

Fingerprint

ecosystem
lake
magnetic susceptibility
tundra
charcoal
soil erosion
shrub
pollen
catchment
lake level
insolation
climate conditions
terrestrial ecosystem
Postglacial
accumulation rate
aquatic ecosystem
forest ecosystem
sediment core
silica
Holocene

ASJC Scopus subject areas

  • Arts and Humanities (miscellaneous)
  • Earth-Surface Processes
  • Earth and Planetary Sciences(all)

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Boreal ecosystem development in the Northwestern Alaska range since 11,000 yr B.P. / Hu, Feng Sheng; Brubaker, Linda B.; Anderson, Patricia M.

In: Quaternary Research, Vol. 45, No. 2, 03.1996, p. 188-201.

Research output: Contribution to journalArticle

Hu, Feng Sheng ; Brubaker, Linda B. ; Anderson, Patricia M. / Boreal ecosystem development in the Northwestern Alaska range since 11,000 yr B.P. In: Quaternary Research. 1996 ; Vol. 45, No. 2. pp. 188-201.
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