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Abbravation: Quaternary Research

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Cambridge University Press

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DOI

10.1016/0377-2217(82)90028-5

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1096-0287

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Fire and Vegetation History from the Coastal Rain

Authors: Colin J Long Cathy Whitlock
Publish Date: 2002/11
Volume: 58, Issue: 3, Pages: 215-225
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Abstract

Highresolution charcoal and pollen analyses were used to reconstruct a 4600yrlong history of fire and vegetation near Taylor Lake in the wettest forests of coastal Oregon Today fires in these forests are rare because the season of ignition does not coincide with months of dry fuels From ca 4600 to 2700 cal yr BP fire episodes occurred at intervals of 140±30 yr while forest vegetation was dominated by disturbanceadapted taxa such as Alnus rubra From ca 2700 cal yr BP to the present fire episodes have become less common occurring at intervals of 240±30 yr and firesensitive forest taxa such as Tsuga heterophylla and Picea sitchensis have become more prominent Fire occurrence during the midHolocene was similar to that of the more xeric forests in the eastern Coast Range and suggests that summer drought was widespread After ca 2700 cal yr BP a decrease in fire episode frequency suggests that cooler conditions and possibly increased summer fog allowed the establishment of presentday Picea sitchensis forests within the watershed These results provide evidence that fire has been an important disturbance agent in the Coast Range of Oregon and variations in fire frequency and climate have led to the establishment of presentday forests


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References

citation title=A comparative review of forest dynamics and disturbance in the temperate rain forests of North and South America citation author=Veblen T T citation author=Alaback P B citation author=Lawford P B citation publication date=1996 citation firstpage=173 citation lastpage=213


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  1. Ice-Sheet Glaciation of the Puget Lowland, Washington, during the Vashon Stade (Late Pleistocene) 1
  2. The Timing of Late Pleistocene Mammalian Extinctions in North America
  3. An Altitudinal Cline in Tropical African Grass Floras and Its Paleoecological Significance
  4. Glaciations of the West Coast Range, Tasmania
  5. Tephrochronology of Late Wisconsin Deglaciation and Holocene Glacier Fluctuations Near Glacier Peak, North Cascade Range, Washington
  6. Determining the Exposure Age of a Karst Landscape
  7. Stable Isotope Stratigraphy of a Late Last Interglacial Speleothem from Rana, Northern Norway
  8. Holocene Paleoenvironmental Change in the Kenyan Central Rift as Indicated by Micromammals from Enkapune Ya Muto Rockshelter
  9. Paleoecological Studies at Lake Patzcuaro on the West-Central Mexican Plateau and at Chalco in the Basin of Mexico 1
  10. Some Effects of Partial Recrystallisation on 14 C dating Late Pleistocene Corals and Molluscs
  11. Some Effects of Partial Recrystallisation on 14 C dating Late Pleistocene Corals and Molluscs
  12. Climate Variation and the Rise and Fall of an Andean Civilization
  13. Saharan Dust Transport and High-Latitude Glacial Climatic Variability: The Alboran Sea Record
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