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  • 1
    Online Resource
    Online Resource
    Canadian Science Publishing ; 2002
    In:  Canadian Journal of Forest Research Vol. 32, No. 6 ( 2002-06-01), p. 1057-1070
    In: Canadian Journal of Forest Research, Canadian Science Publishing, Vol. 32, No. 6 ( 2002-06-01), p. 1057-1070
    Abstract: The history of canopy disturbances over the lifetime of an old-growth Douglas-fir (Pseudotsuga menziesii (Mirb.) Franco) stand in the western Cascade Range of southern Washington was reconstructed using tree-ring records of cross-dated samples from a 3.3-ha mapped plot. The reconstruction detected pulses in which many western hemlock (Tsuga heterophylla (Raf.) Sarg.) synchronously experienced abrupt and sustained increases in ringwidth, i.e., "growth-increases", and focused on medium-sized or larger ([Formula: see text]0.8 ha) events. The results show that the stand experienced at least three canopy disturbances that each thinned, but did not clear, the canopy over areas [Formula: see text] 0.8 ha, occurring approximately in the late 1500s, the 1760s, and the 1930s. None of these promoted regeneration of the shade-intolerant Douglas-fir, all of which established 15001521. The disturbances may have promoted regeneration of western hemlock, but their strongest effect on tree dynamics was to elicit western hemlock growth-increases. Canopy disturbances are known to create patchiness, or horizontal heterogeneity, an important characteristic of old-growth forests. This reconstructed history provides one model for restoration strategies to create horizontal heterogeneity in young Douglas-fir stands, for example, by suggesting sizes of areas to thin in variable-density thinnings.
    Type of Medium: Online Resource
    ISSN: 0045-5067 , 1208-6037
    Language: English
    Publisher: Canadian Science Publishing
    Publication Date: 2002
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    SSG: 12
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  • 2
    Online Resource
    Online Resource
    Canadian Science Publishing ; 2002
    In:  Canadian Journal of Forest Research Vol. 32, No. 6 ( 2002-06-01), p. 1039-1056
    In: Canadian Journal of Forest Research, Canadian Science Publishing, Vol. 32, No. 6 ( 2002-06-01), p. 1039-1056
    Abstract: We used tree-ring records to reconstruct the stand initiation of an old-growth Douglas-fir (Pseudotsuga menziesii (Mirb.) Franco) stand in the western Cascade Range of southern Washington. All tree-ring samples were prepared and crossdated. Following a stand-replacing fire, the stand initiation period lasted from 1500 to 1540, with gradual filling-in of growing space over this period. All sampled Douglas-fir were initial colonizers, establishing (at stump-height) 15001521 under open conditions. A small number of the sampled western hemlock (Tsuga heterophylla (Raf.) Sarg.) were also initial colonizers. Growing space filled as tree crowns widened, and by 1540, closed forest conditions had developed. At this time, Douglas-fir were spaced about 3.5 m from equivalent competitors (ca. 800 trees/ha). In the centuries following canopy closure, considerable natural thinning of the initial colonizers occurred, but the canopy never opened enough again to allow further Douglas-fir establishment. Surviving Douglas-fir developed deep crowns despite the narrow initial spacing, and without epicormic branching from the bole. Most western hemlock that were canopy trees in 1992 established after 1540, originating in the understory. This reconstruction provides an example that may be useful where management policies emphasize the development of old-growth structures.
    Type of Medium: Online Resource
    ISSN: 0045-5067 , 1208-6037
    Language: English
    Publisher: Canadian Science Publishing
    Publication Date: 2002
    detail.hit.zdb_id: 1473096-0
    SSG: 23
    SSG: 12
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  • 3
    Online Resource
    Online Resource
    Springer Science and Business Media LLC ; 1986
    In:  Vegetatio Vol. 67, No. 2 ( 1986-10), p. 119-130
    In: Vegetatio, Springer Science and Business Media LLC, Vol. 67, No. 2 ( 1986-10), p. 119-130
    Type of Medium: Online Resource
    ISSN: 0042-3106 , 1573-5052
    RVK:
    Language: English
    Publisher: Springer Science and Business Media LLC
    Publication Date: 1986
    detail.hit.zdb_id: 201543-2
    detail.hit.zdb_id: 1364679-5
    detail.hit.zdb_id: 1479167-5
    SSG: 12
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  • 4
    Online Resource
    Online Resource
    Cambridge University Press (CUP) ; 2002
    In:  Quaternary Research Vol. 57, No. 3 ( 2002-05), p. 325-333
    In: Quaternary Research, Cambridge University Press (CUP), Vol. 57, No. 3 ( 2002-05), p. 325-333
    Abstract: A sediment core from Smorodinovoye Lake (SML), northeastern Siberia (area to the east of the Verkhoyansk Range) spanning the last 24,000 14 C yr indicates that vegetational and climatic changes in the upper Indigirka basin resemble those in eastern Siberia (Lena basin and westward). For example, maximum postglacial summer temperatures at SML probably occurred 6000–4000 14 C yr B.P., an age more in accordance with eastern than northeastern records. Larix arrived near the lake by 9600 14 C yr B.P., approximately when forests expanded in the east but ca. 1500 14 C yr later than forests were established in the neighboring upper Kolyma basin. Paleobotanical data further suggest that Larix possibly migrated southward from populations in the arctic lowlands of eastern Siberia and did not originate from interior refugia of the upper Kolyma basin. Although a Younger Dryas cooling has been noted in eastern Siberia, SML provides the first evidence from the northeast for a similar climatic reversal. Climatic variations seemingly have persisted between the Indigirka and Kolyma basins over at least the last 11,000 14 C yr, despite the proximity of the two drainages and the occurrence of major changes in boundary conditions (e.g., seasonal insolation, sea levels) that have influenced other regional climatic patterns.
    Type of Medium: Online Resource
    ISSN: 0033-5894 , 1096-0287
    RVK:
    Language: English
    Publisher: Cambridge University Press (CUP)
    Publication Date: 2002
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    SSG: 14
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  • 5
    Online Resource
    Online Resource
    Cambridge University Press (CUP) ; 1994
    In:  Quaternary Research Vol. 41, No. 3 ( 1994-05), p. 306-315
    In: Quaternary Research, Cambridge University Press (CUP), Vol. 41, No. 3 ( 1994-05), p. 306-315
    Abstract: Pollen analysis of a new core from Joe Lake indicates that the late Quaternary vegetation of northwestern Alaska was characterized by four tundra and two forest-tundra types. These vegetation types were differentiated by combining quantitative comparisons of fossil and modern pollen assemblages with traditional, qualitative approaches for inferring past vegetation, such as the use of indicator species. Although imprecisely dated, the core probably spans at least the past 40,000 yr. A graminoid- Salix tundra dominated during the later and early portions of the glacial record. The middle glacial interval and the transition from glacial to interglacial conditions are characterized by a graminoid- Betula-Salix tundra. A Populus forest- Betula shrub tundra existed during the middle potion of this transition, being replaced in the early Holocene by a Betula-Alnus shrub tundra. The modern Picea forest-shrub tundra was established by the middle Holocene. These results suggest that the composition of modem tundra communities in northwestern Alaska developed relatively recently and that throughout much of the late Quaternary, tundra communities were unlike the predominant types found today in northern North America. Although descriptions of vegetation variations within the tundra will always be restricted by the innate taxonomic limitations of their herb-dominated pollen spectra, the application of multiple interpretive approaches improves the ability to reconstruct the historical development of this vegetation type.
    Type of Medium: Online Resource
    ISSN: 0033-5894 , 1096-0287
    RVK:
    Language: English
    Publisher: Cambridge University Press (CUP)
    Publication Date: 1994
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    SSG: 13
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  • 6
    Online Resource
    Online Resource
    Cambridge University Press (CUP) ; 1983
    In:  Quaternary Research Vol. 20, No. 2 ( 1983-09), p. 194-214
    In: Quaternary Research, Cambridge University Press (CUP), Vol. 20, No. 2 ( 1983-09), p. 194-214
    Abstract: Five pollen diagrams reveal late Wisconsin and Holocene vegetation changes in the Walker Lake/Alatna Valley region of the central Brooks Range, approximately 100 km west of the area studied by D. A. Livingstone (1955, Ecology 36, 587–600). New insights into the vegetation history of this region are provided by calculations of pollen influx and by the use of linear discriminant analysis to separate Picea glauca and P. mariana pollen. Three major pollen zones are identified: (1) a basal herb zone, characterized by high percentages of Cyperaceae, Gramineae, Salix , and Artemisia , and low total pollen influx; (2) a shrub Betula zone with increased total pollen influx and very high percentages of Betula pollen, predominantly in the size range of B. nana and B. glandulosa ; and (3) and Alnus zone dominated by Alnus pollen. Lakes currently within the boreal forest or near tree line show relatively high percentages of Picea pollen in the Alnus zone. Several striking vegetation changes occurred between ca. 10,000 and 7000 yr B.P. Between ca. 11,000 and 10,000 yr B.P., Populus balsamifera pollen percentages as great as 30% indicate that this species was present at low-elevation sites near Walker Lake. These populations declined abruptly ca. 10,000 yr ago and have never regained prominence. About 8500 yr B.P., Picea glauca pollen reached 10–15%, indicating the arrival of P. glauca in or near the study area. P. glauca populations evidently decreased ca. 8000 yr ago, when Picea pollen percentages and influx fell to low values. About 7000 yr B.P., Alnus pollen percentages and influx rose sharply as alder shrubs became established widely. Picea once more expanded ca. 5000 yr ago, but these populations were dominated by P. mariana rather than P. glauca , which increased slowly at this time and may still be advancing northward. Some vegetation changes have been remarkably synchronous over wide areas of interior Alaska, and probably reflect responses of in situ vegetation to environmental changes, but others may reflect the lagged responses of species migrating into new areas.
    Type of Medium: Online Resource
    ISSN: 0033-5894 , 1096-0287
    RVK:
    Language: English
    Publisher: Cambridge University Press (CUP)
    Publication Date: 1983
    detail.hit.zdb_id: 1471589-2
    detail.hit.zdb_id: 205711-6
    SSG: 13
    SSG: 14
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  • 7
    Online Resource
    Online Resource
    Elsevier BV ; 1986
    In:  Review of Palaeobotany and Palynology Vol. 46, No. 3-4 ( 1986-01), p. 273-291
    In: Review of Palaeobotany and Palynology, Elsevier BV, Vol. 46, No. 3-4 ( 1986-01), p. 273-291
    Type of Medium: Online Resource
    ISSN: 0034-6667
    Language: English
    Publisher: Elsevier BV
    Publication Date: 1986
    detail.hit.zdb_id: 1497512-9
    detail.hit.zdb_id: 209897-0
    SSG: 13
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  • 8
    Online Resource
    Online Resource
    Wiley ; 2013
    In:  Ecological Monographs Vol. 83, No. 4 ( 2013-11), p. 471-489
    In: Ecological Monographs, Wiley, Vol. 83, No. 4 ( 2013-11), p. 471-489
    Type of Medium: Online Resource
    ISSN: 0012-9615
    Language: English
    Publisher: Wiley
    Publication Date: 2013
    detail.hit.zdb_id: 2010129-6
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  • 9
    Online Resource
    Online Resource
    Wiley ; 1989
    In:  Ecology Vol. 70, No. 2 ( 1989-04), p. 405-410
    In: Ecology, Wiley, Vol. 70, No. 2 ( 1989-04), p. 405-410
    Type of Medium: Online Resource
    ISSN: 0012-9658
    RVK:
    Language: English
    Publisher: Wiley
    Publication Date: 1989
    detail.hit.zdb_id: 1797-8
    detail.hit.zdb_id: 2010140-5
    SSG: 12
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  • 10
    Online Resource
    Online Resource
    Wiley ; 2005
    In:  Ecology Vol. 86, No. 7 ( 2005-07), p. 1667-1668
    In: Ecology, Wiley, Vol. 86, No. 7 ( 2005-07), p. 1667-1668
    Type of Medium: Online Resource
    ISSN: 0012-9658
    RVK:
    Language: English
    Publisher: Wiley
    Publication Date: 2005
    detail.hit.zdb_id: 1797-8
    detail.hit.zdb_id: 2010140-5
    SSG: 12
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