Late-Holocene climate variability and ecosystem responses in Alaska inferred from high-resolution multiproxy sediment analyses at Grizzly Lake

Willy Tinner, Ruth Beer, Christian Bigler, Benjamin Frank Clegg, Richard T. Jones, Petra Kaltenrieder, Ulrike J. van Raden, Adrian Gilli, Feng Sheng Hu

Research output: Contribution to journalArticle

Abstract

The late-Holocene shift from Picea glauca (white spruce) to Picea mariana (black spruce) forests marked the establishment of modern boreal forests in Alaska. To understand the patterns and drivers of this vegetational change and the associated late-Holocene environmental dynamics, we analyzed radiocarbon-dated sediments from Grizzly Lake for chironomids, diatoms, pollen, macrofossils, charcoal, element composition, particle size, and magnetic properties for the period 4100-1800 cal BP. Chironomid assemblages reveal two episodes of decreased July temperature, at ca. 3300-3150 (ca -1 °C) and 2900-2550 cal BP (ca -2 °C). These episodes coincided with climate change elsewhere in the Northern Hemisphere, atmospheric reorganization, and low solar activity. Diatom-inferred lake levels dropped by ca. 5 m at 3200 cal BP, suggesting dry conditions during the period 3200-1800 cal BP. P. glauca declined and P. mariana expanded at ca. 3200 cal BP; this vegetational change was linked to diatom-inferred low lake levels and thus decreased moisture availability. Forest cover declined at 3300-3100, 2800-2500 and 2300-2100 cal BP and soil erosion as inferred from increased values of Al, K, Si, Ti, and Ca intensified, when solar irradiance was low. Plant taxa adapted to disturbance and cold climate (e.g. Alnus viridis, shrub Betula, Epilobium) expanded during these periods of reduced forest cover. This open vegetation type was associated with high fire activity that peaked at 2800 cal BP, when climatic conditions were particularly cold and dry. Forest recovery lagged behind subsequent climate warming (≤+3 °C) by ca. 75-225 years. Our multiproxy data set suggests that P. glauca was dominant under warm-moist climatic conditions, whereas P. mariana prevailed under cold-dry and warm-dry conditions. This pattern implies that climatic warming, as anticipated for this century, may promote P. glauca expansions, if moisture availability will be sufficiently high, while P. mariana may expand under dry conditions, possibly exacerbating climate impacts on the fire regime.

Original languageEnglish (US)
Pages (from-to)41-56
Number of pages16
JournalQuaternary Science Reviews
Volume126
DOIs
StatePublished - Oct 15 2015

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ecosystem response
Picea glauca
Picea mariana
diatom
Holocene
climate
Bacillariophyceae
lake level
forest cover
lakes
sediments
ecosystems
lake
warming
moisture
sediment
Chironomidae
global warming
climate effect
magnetic property

Keywords

  • 2.8 ka event
  • 2800 event
  • Boreal
  • Climate change
  • Erosion
  • Fire
  • Paleoecology
  • Vegetation

ASJC Scopus subject areas

  • Global and Planetary Change
  • Ecology, Evolution, Behavior and Systematics
  • Archaeology
  • Archaeology
  • Geology

Cite this

Late-Holocene climate variability and ecosystem responses in Alaska inferred from high-resolution multiproxy sediment analyses at Grizzly Lake. / Tinner, Willy; Beer, Ruth; Bigler, Christian; Clegg, Benjamin Frank; Jones, Richard T.; Kaltenrieder, Petra; van Raden, Ulrike J.; Gilli, Adrian; Hu, Feng Sheng.

In: Quaternary Science Reviews, Vol. 126, 15.10.2015, p. 41-56.

Research output: Contribution to journalArticle

Tinner, Willy ; Beer, Ruth ; Bigler, Christian ; Clegg, Benjamin Frank ; Jones, Richard T. ; Kaltenrieder, Petra ; van Raden, Ulrike J. ; Gilli, Adrian ; Hu, Feng Sheng. / Late-Holocene climate variability and ecosystem responses in Alaska inferred from high-resolution multiproxy sediment analyses at Grizzly Lake. In: Quaternary Science Reviews. 2015 ; Vol. 126. pp. 41-56.
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AU - Jones, Richard T.

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AU - van Raden, Ulrike J.

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AU - Hu, Feng Sheng

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