Matches in SemOpenAlex for { <https://semopenalex.org/work/W2006661008> ?p ?o ?g. }
- W2006661008 endingPage "121" @default.
- W2006661008 startingPage "105" @default.
- W2006661008 abstract "Pollen analysis of radiocarbon-dated lake sediment from northern Vancouver Island, southwest British Columbia reveals regional changes in forest vegetation over the last 12,200 14C yr (14,900 cal yr). Between at least 12,200 and 11,700 14C yr BP (14,900–13,930 cal yr BP), open woodlands were dominated by Pinus contorta, Alnus crispa, and various ferns. As P. contorta decreased in abundance, Alnus rubra and more shade-tolerant conifers (i.e., Picea and Tsuga mertensiana) increased. Increases in T. mertensiana, P. contorta, and A. crispa pollen accumulation rates (PARs) between 10,600 and 10,400 14C yr BP (11,660–11,480 cal yr BP) reflect a cool and moist climate during the Younger Dryas chronozone. Orbitally induced warming around 10,000 14C yr BP (11,090 cal yr BP) allowed the northward extension of Pseudotsuga menziesii, although Picea, Tsuga heterophylla, and A. rubra dominated early Holocene forests. By 7500 14C yr BP (8215 cal yr BP), shade-tolerant T. heterophylla was the dominant forest tree. Cupressaceae (Thuja plicata and Chamaecyparis nootkatensis) was present by 7500 14C yr BP but reached its maximum after 3500 14C yr BP (3600 cal yr BP), when a cooler and wetter regional climate facilitated the development of temperate rainforest. The highest rates of vegetation change are associated with Lateglacial climate change and species with rapid growth rates and short life spans." @default.
- W2006661008 created "2016-06-24" @default.
- W2006661008 creator A5027557227 @default.
- W2006661008 date "2005-01-01" @default.
- W2006661008 modified "2023-10-09" @default.
- W2006661008 title "Late Quaternary dynamics of forest vegetation on northern Vancouver Island, British Columbia, Canada" @default.
- W2006661008 cites W1620829297 @default.
- W2006661008 cites W1654234791 @default.
- W2006661008 cites W1881638488 @default.
- W2006661008 cites W1927648166 @default.
- W2006661008 cites W1949467692 @default.
- W2006661008 cites W1966081590 @default.
- W2006661008 cites W1967868821 @default.
- W2006661008 cites W1970033143 @default.
- W2006661008 cites W1970389511 @default.
- W2006661008 cites W1973186833 @default.
- W2006661008 cites W1975131719 @default.
- W2006661008 cites W1976469911 @default.
- W2006661008 cites W1976909126 @default.
- W2006661008 cites W1978569501 @default.
- W2006661008 cites W1979011093 @default.
- W2006661008 cites W1984767443 @default.
- W2006661008 cites W1992058642 @default.
- W2006661008 cites W1993603888 @default.
- W2006661008 cites W1999080586 @default.
- W2006661008 cites W1999431839 @default.
- W2006661008 cites W2005896816 @default.
- W2006661008 cites W2006817468 @default.
- W2006661008 cites W2007098296 @default.
- W2006661008 cites W2008423436 @default.
- W2006661008 cites W2015753881 @default.
- W2006661008 cites W2016184904 @default.
- W2006661008 cites W2018126594 @default.
- W2006661008 cites W2019558782 @default.
- W2006661008 cites W2021408360 @default.
- W2006661008 cites W2022005640 @default.
- W2006661008 cites W2023726252 @default.
- W2006661008 cites W2025864350 @default.
- W2006661008 cites W2035217747 @default.
- W2006661008 cites W2037055413 @default.
- W2006661008 cites W2039593896 @default.
- W2006661008 cites W2040389720 @default.
- W2006661008 cites W2040611564 @default.
- W2006661008 cites W2040706704 @default.
- W2006661008 cites W2049214105 @default.
- W2006661008 cites W2051087039 @default.
- W2006661008 cites W2052823227 @default.
- W2006661008 cites W2052869621 @default.
- W2006661008 cites W2055683676 @default.
- W2006661008 cites W2056530892 @default.
- W2006661008 cites W2057727628 @default.
- W2006661008 cites W2062137846 @default.
- W2006661008 cites W2065976365 @default.
- W2006661008 cites W2067242307 @default.
- W2006661008 cites W2068028745 @default.
- W2006661008 cites W2068219607 @default.
- W2006661008 cites W2071185249 @default.
- W2006661008 cites W2076332631 @default.
- W2006661008 cites W2078999606 @default.
- W2006661008 cites W2083072147 @default.
- W2006661008 cites W2085648853 @default.
- W2006661008 cites W2089039533 @default.
- W2006661008 cites W2091569024 @default.
- W2006661008 cites W2091630640 @default.
- W2006661008 cites W2094476767 @default.
- W2006661008 cites W2094829689 @default.
- W2006661008 cites W2098151891 @default.
- W2006661008 cites W2104437475 @default.
- W2006661008 cites W2105988999 @default.
- W2006661008 cites W2108273792 @default.
- W2006661008 cites W2114319241 @default.
- W2006661008 cites W2123836780 @default.
- W2006661008 cites W2126497987 @default.
- W2006661008 cites W2132058438 @default.
- W2006661008 cites W2139427406 @default.
- W2006661008 cites W2141459972 @default.
- W2006661008 cites W2147359762 @default.
- W2006661008 cites W2148654450 @default.
- W2006661008 cites W2157464420 @default.
- W2006661008 cites W2157855454 @default.
- W2006661008 cites W2159678538 @default.
- W2006661008 cites W2171715479 @default.
- W2006661008 cites W2280624662 @default.
- W2006661008 cites W2329745432 @default.
- W2006661008 doi "https://doi.org/10.1016/j.quascirev.2004.05.008" @default.
- W2006661008 hasPublicationYear "2005" @default.
- W2006661008 type Work @default.
- W2006661008 sameAs 2006661008 @default.
- W2006661008 citedByCount "48" @default.
- W2006661008 countsByYear W20066610082012 @default.
- W2006661008 countsByYear W20066610082013 @default.
- W2006661008 countsByYear W20066610082015 @default.
- W2006661008 countsByYear W20066610082016 @default.
- W2006661008 countsByYear W20066610082017 @default.
- W2006661008 countsByYear W20066610082018 @default.
- W2006661008 countsByYear W20066610082019 @default.
- W2006661008 countsByYear W20066610082020 @default.
- W2006661008 countsByYear W20066610082022 @default.