globalchange  > 过去全球变化的重建
DOI: 10.1016/j.quascirev.2014.05.030
Scopus记录号: 2-s2.0-84902511641
论文题名:
Inferring local to regional changes in forest composition from Holocene macrofossils and pollen of a small lake in central Upper Michigan
作者: Jackson S.T.; Booth R.K.; Reeves K.; Andersen J.J.; Minckley T.A.; Jones R.A.
刊名: Quaternary Science Reviews
ISSN: 2773791
出版年: 2014
卷: 98
起始页码: 60
结束页码: 73
语种: 英语
英文关键词: Forest history ; Holocene ; Michigan ; North America ; Paleoecology ; Plant macrofossils ; Pollen ; Scale ; Vegetation
Scopus关键词: Dynamics ; Lakes ; Vegetation ; Forest history ; Holocenes ; Michigan ; North America ; Paleoecology ; Plant macrofossils ; Pollen ; Scale ; Forestry ; climate effect ; community dynamics ; forest dynamics ; fossil record ; Holocene ; lacustrine deposit ; landscape ecology ; paleoecology ; pollen ; vegetation dynamics ; vegetation history ; Ecology ; Lakes ; Michigan ; North America ; Plants ; Pollen ; Michigan ; North America ; United States
英文摘要: Vegetational response to climatic change involves processes of population and community dynamics within local stands, which scale up to landscape-level changes in vegetation composition and broad-scale changes in species distributions. Understanding these dynamics poses a critical challenge to paleoecological explanation, because of the broad range of scales at which these dynamics take place and interact. We present an 8600-year paleoecological record of local and regional changes in forest composition from a small (2.6ha) lake in central Upper Michigan. Plant macrofossils provide a spatially precise record of local forest composition, while pollen data provide a spatially integrated record of regional vegetational changes. Temporal patterns among different macrofossil types within species show overall coherence, indicating that changes in macrofossil abundance generally record changes in local tree abundance. Temporal patterns in macrofossil sequences correspond to patterns in pollen sequences, indicating that local changes contributed to the large-scale changes in the surrounding region. The pollen and macrofossil records show nearly continuous turnover in vegetation composition throughout the past 8600 years; the longest period without major compositional change was ca1600 years, and dynamics at multidecadal to multicentennial scales are observed during many periods. Coordinated application of temporally precise sequences of pollen and macrofossil data at multiple sites can support inferences concerning vegetation dynamics at multiple spatial and temporal scales, and test mechanistic hypotheses. © 2014.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/60202
Appears in Collections:过去全球变化的重建

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作者单位: Department of Botany, University of Wyoming, 3165, 1000 E. University Ave., Laramie, WY 82071, United States; Program in Ecology, University of Wyoming, Laramie, WY 82071, United States; Department of Earth and Environmental Sciences, Lehigh University, 31 Williams Drive, Bethlehem, PA 18015, United States; Metro Regional Center, 600 NE Grand Ave., Portland, OR 97232, United States; Department of Geography, University of Wyoming, Laramie, WY 82071, United States; Department of Geosciences, University of Arizona, Tucson, AZ 85721, United States

Recommended Citation:
Jackson S.T.,Booth R.K.,Reeves K.,et al. Inferring local to regional changes in forest composition from Holocene macrofossils and pollen of a small lake in central Upper Michigan[J]. Quaternary Science Reviews,2014-01-01,98
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