Disturbance and Persistence of Sitka Spruce (Picea Sitchensis (Bong) Carr.) in Coastal Forests of the Pacific Northwest, North America
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Disturbance and Persistence of Sitka Spruce (Picea sitchensis (Bong) Carr.) in Coastal Forests of the Pacific Northwest, North America Alan H. Taylor Journal of Biogeography, Vol. 17, No. 1. (Jan., 1990), pp. 47-58. Stable URL: http://links.jstor.org/sici?sici=0305-0270%28199001%2917%3A1%3C47%3ADAPOSS%3E2.0.CO%3B2-3 Journal of Biogeography is currently published by Blackwell Publishing. Your use of the JSTOR archive indicates your acceptance of JSTOR's Terms and Conditions of Use, available at http://www.jstor.org/about/terms.html. JSTOR's Terms and Conditions of Use provides, in part, that unless you have obtained prior permission, you may not download an entire issue of a journal or multiple copies of articles, and you may use content in the JSTOR archive only for your personal, non-commercial use. Please contact the publisher regarding any further use of this work. Publisher contact information may be obtained at http://www.jstor.org/journals/black.html. Each copy of any part of a JSTOR transmission must contain the same copyright notice that appears on the screen or printed page of such transmission. JSTOR is an independent not-for-profit organization dedicated to and preserving a digital archive of scholarly journals. For more information regarding JSTOR, please contact [email protected]. http://www.jstor.org Thu Mar 29 13:19:38 2007 JO~rnalof Biogeograpky (1990)17,47-58 Disturbance and persistence of sitka spruce (Picea sitehensis (Bong) Carr.) in coastal forests of the Pacific Northwest, North America ALANH. TAYLORDepartment of Geograplzy, University of Maryland-Baltimore County, Baltimore, Maryland 21228, U.S.A. Abstract. Forests dominated by Picea sitchensis (Bong) and tree growth in gaps to determine if P. sitclzensis can Carr. and Tsuga lzeteroplzylla (Raf.) Sarg. occupy a narrow persist under a small gap disturbance regime. Tree replace- coastal strip along the Pacific Northwest coast of North ment models derived from tree replacement patterns in America. P. sitchensis is considered seral to T. heterophylla gaps were used to predict abundances of P. sitchensis and but descriptions of groups of P. sitchensis saplings and small T. heterophylla in the next generation. Tree replacement trees in light gaps created by small canopy disturbances models did not predict a decline in P. sitchensis abundance (<0.25 ha) suggest that P. sitchensis may persist by gap- in the next generation. Gaps of 800-1000 m2 appear large phase regeneration after small-scale disturbance. This enough for P. sitclzensis to persist in thesc: forests. study combines analyses of the disturbance regime (gap size distribution, gap age distribution, the spatial distribution of Key words. Disturbance, succession, forest dynamics, gaps, forest turnover time), patterns of tree regeneration Pacific Northwest, Picea sitchensis. INTRODUCTION Throughout most of its range Picea is considered seral to Tsuga. Catastrophic disturbances such as fire, windthrow, Natural disturbances are a common feature of forested landslides and insect attacks initiate secondary succession. landscapes that influence the spatial and temporal patterns Both species regenerate prolifically after catastrophic dis- of species abundance (Veblen & Ashton, 1978; White, turbance but as stands mature mixed forest is replaced by 1979; Runkle, 1981; Sousa, 1984). Infrequent catastrophic Tsuga (Franklin & Dyrness, 1973; Fonda, 1974; Ruth & fire, for example, is considered the most important disturb- Harris, 1979). Some sites deviate from this general pattern. ance affecting the distribution and abundance of some spe- Picea population structures in mixed forest on rnesic cies (e.g. Pseudotsuga menziesii (Mirb.) Franco) ill the alluvial flats in coastal valleys, and in the salt spray zone coniferous forests of the Pacific Northwest (Hemstroni & indicate that Picea will remain codominant with Tsuga Franklin, 1982). Pseudotsuga lnenziesii requires cata- (Cordes, 1972; Franklin & Dyrness, 1973; Kratz, 1975; strophic fire to regenerate and persist except as residual Mckee, LaRoi & Franklin, 1982). Picea reproduction in trees in old-growth forest (Franklin & Dyrness, 1973). Fre- mixed forest on typical sites is present, however, suggesting quent smaller-scale disturbances undoubtedly influence the that young Picea could replace canopy trees as they die composition, structure and community dynamics of con- (Hines, 1971; Juday, 1976; Quay, 1982; Greene, 1982; iferous forests in the Pacific Northwest but they have been Hemstrorn & Logan, 1986). Hines (1971), Juday (1976) and little studied. Quay (1982) observed groups of Picea saplings and small Coniferous forests dominated by Picea sitchensis (Bong.) trees beneath light gaps in the forest canopy inolder stands Carr. and Tsuga heterophylla (Raf.) Sarg. (referred to and speculated that Picea could persist by gap regeneration below as Tsuga and Picea, respectively) occupy a narrow in opening produced by death of small group of trees. Picea coastal strip from near Coos Bay Oregon to Prince William clearly persists at landscape scales by regenerating after sound in Alaska (Fig. 1) (Ruth & Harris, 1979). The dis- catastrophic disturbance but smaller disturbances too may tribution of Picea, which defines the range of this forest provide an opportunity for Picea to regenerate and persist type, is associated with a mild mesic maritime climate at stand scales. (Fowells, 1965; Franklin & Dyrness, 1973; Ruth & Harris, The objectives of this study were to: (1) identify patterns 1979). Picea declines in importance away from the coastal of regeneration in small (<0.25 ha) canopy opening pro- zone and other conifers become major associates of Tsuga duced by death of one or a few canopy trees; (2) determine (Franklin & Dyrness, 1973; Ruth & Harris, 1979). if a disturbance regime characterized by treefall gaps is 48 Alan H. Taylor / Picea sitchensis - Tsuaa heterophvlla - ---L - - - J Forest type L 0 300 60C krr \ i do'- 1 - CALIFORNIA ( \ I \ FIG. 1. Distribution of the Piceu sitchensis (Bong) Carr.-Tsugu heterophyllri (Raf.) Sarg. forest type in the Pacific Northwest (adapted from Ruth & Harris, 1979). adequate for Picea regeneration; and (3) predict future tems are shallow and rarely penetrate below 1 m in depth forest composition from tree replacement patterns in gaps. (Harmon, 1986). Study areas. Forests at two sites, Cascade Head and Cape The forest canopy is dominated by Picea and Tsuga and Lookout, both on the northern Oregon coast, were selected there is a well-developed shrub-forb-moss understorey. for sampling. These sites were chosen for the following Important shrubs include Rubus spectabilis Pursh, Vac- reasons: (1) previous descriptions of their forest structure ciniumparvifolium Smith, V.ovalifolium Smith, Sambucus suggested that Picea might persist by gap-phase regenera- racemosa L. var. arborescens (T. & G.) Gray, Menziesia tion; (2) reconnaissance showed gaps to be common at both ferruginea Smith and Oplopanax horrirluln (J. E. Smith) sites; and (3) stands were undisturbed by recent human Miq. The most common forbs are Oxalis oregana Nutt. ex activity. T. & G., Polysticum munituln (Kaulf.) Presl. and Montia Cascade Head. Sampling was conducted in the Neskowin siberica (L.) How. (Quay, 1982). Much of the forest estab- Crest Research Natural Area (Greene, 1982). Cascade lished after a human-set conflagration in the mid-nine- Head is a deeply dissected headland composed primarily of teenthcentury (Morris, 1934; Muliger, 1944; Gr&ne, 1982; marine tuffaceous sandstone overlying volcanics (Baldwin, Harcornbe, 1986) but there are groups of trees scattered 1964; Greene, 1982). Altitudes vary between sea level and throughout the area that did not burn in this fire. 400 m. Soils are strongly acidic, high in nitrogen and organic Cape Lookout. Cape Lookout is a long (4 km) narrow matter, and vary in texture from silt loam to silty clay loam (=I km) peninsula that juts into the Pacific Ocean. Parent and are moderately well drained (Grier, 1978). Root sys- material consists primarily of basaltic deposits and soils Gap regeneration of Picea sitchensis 49 vary in texture from loam to silty clay loam and may exceed mineral soil) of each seedling, sapling or tree were 1 m in depth (Quay, 1982). Altitudes vary from sea level to recorded. Additional detail on rooting substrates were 100 m and overall the topography is less rugged than that at obtained by classifying each log by decomposition class Cascade Head. (sensu Fogel, Ogawas & Trappe, 1972). The tallest tree Picea-Tsuga forests on Cape Lookout apparently did not (>5.0 cm dbh) in a quadrant was designated as the suc- originate after the mid-nineteenth century fire that burned cessor tree, or tree most likely to fill the gap quadrant (sensu forests on Cascade Head. Various stand ages were present Barden, 1981). No successor tree was designated for a of Cape Lookout including young, mature and old-growth quadrant if no sterns were 35.0 cm dbh. Four successor suggesting that stand initiating disturbances have been trees could be designated per gap. All trees within a gap cornmon over the last 200 years. The forest understorey is were cored 30 cm above the base and their age was esti- similar to that at Cascade Head but the shrubs R. spectabilis mated by counting annual growth rings. and Gaultheria shallon Pursh. and the forbs Blechnum spi- The relationship between age and dbh of canopy trees cant (L.) Roth and Maianthemum dilatatuln (Wood) Nels. was determined using least squares regression for a sample & Macbr. are more common (Quay, 1982). of at least five trees of each species in 10 cm cbh classes Climate. The climate at both sites is strongly influenced beginning at 5.0 cm and ending at 85 cm dbh, at each site. by proximity to the Pacific Ocean. Conditions are mild and Gap age, gap expansion, tree growth rates, canopy dis- moist. Average annual precipitation at a representative turbance. Ages of canopy gaps were estimated in one of two station (Otis, Oregon, altitude=60 m) is about 250 cm with ways: (1) by dating the oldest sudden increase in annual tree little falling between June and August (16 cm).