Establishment of tree seedlings and water-soluble nutrients in coarse woody debris in an old-growth Picea-Abies forest in Hokkaido, northern Japan

2000 ◽  
Vol 30 (7) ◽  
pp. 1148-1155 ◽  
Author(s):  
Masamichi Takahashi ◽  
Yoshimi Sakai ◽  
Reiko Ootomo ◽  
Masao Shiozaki
Keyword(s):  
Picea Abies ◽  
Coarse Woody Debris ◽  
Forest Floor ◽  
Woody Debris ◽  
Tree Seedlings ◽  
Class Iii ◽  
Tree Seedling ◽  
Decay Class ◽  
Tree Seedling Establishment ◽  
Northern Japan

Forest floor microsite conditions and tree seedling establishment were studied at an old-growth Picea-Abies forest in Hokkaido Island, northern Japan. Tree seedlings were established abundantly on coarse woody debris (CWD) from decay class III, a class indicating moderate decay, to class V, the most advanced decay class. The height-class distribution of tree seedlings indicates that the recruitment of Picea glehnii (Fr. Schm.) Masters and Picea jezoensis (Sieb. et Zucc.) Carr. seedlings on CWD started on decay class II and was mostly restricted to CWD decay class III. Seedlings of Abies sachalinensis (Fr. Schm.) Masters also favored establishment on CWD but had a wide adaptability to most of the microsites. Although CWD functioned as a suitable seedbed, water extracts from CWD were acidic and had quite low mineral nutrient concentrations. Tree seedling establishment did not necessarily require high levels of nutrient content in microsites. Although the forest floor was largely covered by CWD, with 2056 m2·ha-1 of the total projected area covered by CWD, CWD decay class III covered only 366 m2·ha-1 of the forest floor, indicating that CWD as a functioning seedbed is limited by time and space on the forest floor.

Coarse woody debris and forest floor respiration in an old-growth coniferous forest on the Olympic Peninsula, Washington, USA

1994 ◽  
Vol 24 (9) ◽  
pp. 1811-1817 ◽  
Author(s):  
James L. Marra ◽  
Robert L. Edmonds
Keyword(s):  
Coarse Woody Debris ◽  
Forest Floor ◽  
Woody Debris ◽  
Large Diameter ◽  
Small Diameter ◽  
Douglas Fir ◽  
Western Hemlock ◽  
Respiration Rates ◽  
Decay Class ◽  
Class 1

Carbon dioxide evolution rates for downed logs (coarse woody debris) and the forest floor were measured in a temperate, old-growth rain forest in Olympic National Park, Washington, using the soda lime trap method. Measurements were taken every 4 weeks from October 22, 1991, to November 19, 1992. Respiration rates for Douglas-fir (Pseudotsugamenziesii (Mirb.) Franco) and western hemlock (Tsugaheterophylla (Raf.) Sarg.), logs were determined for decay classes 1–2, 3, and 5 in two diameter classes. Overall, western hemlock logs respired at a rate 35% higher (4.37 g CO2•m−2•day−1) than Douglas-fir logs (3.23 g CO2•m−2•day−1). Respiration rates for decay class 1–2 logs of both species were similar to decay class 5 logs (4.46 and 4.07 g CO2•m−2•day−1, respectively), but decay class 3 logs respired at a lower rate (3.23 g CO2•m−2•day−1). Seasonal patterns of respiration rates occurred, particularly for decay class 1 and 2 western hemlock logs where monthly averages ranged from a low of 2.67 g CO2•m−2•day−1 in February 1992 to a high of 8.30 g CO2•m−2•day−1 in September 1992. Rates for decay class 1–2 western hemlock logs were greater than those from the forest floor, which ranged from 3.42 to 7.13 g CO2•m−2•day−1. Respiration rates were depressed in late July and August compared with fall and spring owing to the summer drought characteristic of the Pacific Northwest. Large-diameter western hemlock logs in decay class 1–2 had higher respiration rates than small-diameter logs, whereas large-diameter decay class 3 western hemlock logs had lower respiration rates than small-diameter logs.

scholarly journals Patterns of laccase and peroxidases in coarse woody debris of Fagus sylvatica, Picea abies and Pinus sylvestris and their relation to different wood parameters

2015 ◽  
Vol 135 (1) ◽  
pp. 109-124 ◽  
Author(s):  
Tobias Arnstadt ◽  
Björn Hoppe ◽  
Tiemo Kahl ◽  
Harald Kellner ◽  
Dirk Krüger ◽  
...  
Keyword(s):  
Picea Abies ◽  
Pinus Sylvestris ◽  
Fagus Sylvatica ◽  
Coarse Woody Debris ◽  
Woody Debris

Short-term effect of thinning on carbon storage in soil, forest floor and coarse woody debris ofQuercusspp. stand in Hoengseong, Gangwon-do, Korea

2011 ◽  
Vol 7 (4) ◽  
pp. 168-173 ◽  
Author(s):  
A-Ram Yang ◽  
Nam Jin Noh ◽  
Sue Kyoung Lee ◽  
Tae Kyung Yoon ◽  
Choonsig Kim ◽  
...  
Keyword(s):  
Carbon Storage ◽  
Coarse Woody Debris ◽  
Forest Floor ◽  
Woody Debris ◽  
Term Effect ◽  
Short Term ◽  
Short Term Effect

scholarly journals Potentials of Natural Tree Regeneration after Clearcutting in Subalpine Forests

2008 ◽  
Vol 23 (1) ◽  
pp. 46-52 ◽  
Author(s):  
Juergen Kreyling ◽  
Andreas Schmiedinger ◽  
Ellen Macdonald ◽  
Carl Beiekuhnlein
Keyword(s):  
Natural Regeneration ◽  
Pinus Contorta ◽  
Woody Debris ◽  
Negative Relationship ◽  
Forest Edge ◽  
Tree Regeneration ◽  
Tree Seedlings ◽  
Tree Seedling ◽  
Engelmann Spruce ◽  
Understory Plant

Abstract Regeneration of interior mountain forests still is not adequately understood, although these forests are subject to intensified use over the last decades. We examined factors influencing the success of natural tree regeneration after harvesting in the Engelmann spruce–subalpine fir zone of the Monashee Mountains, British Columbia, Canada. Distance from the forest edge was an important factor for regeneration; at distances exceeding 70 m from the forest edge only 50% of plots showed sufficient natural regeneration to meet stocking targets compared with 90% of plots closer to forest edges. Seedling density and growth were superior in the more protected southern portions of clearcuts. Seedling growth was less in plots containing high cover of downed woody debris. There was no relationship between understory plant diversity or composition and tree seedling regeneration. However, cover of fireweed (Epilobium angustifolium) had a significant negative relationship with density but not growth of tree seedlings, particularly for lodgepole pine (Pinus contorta var. latifolia). Cover of fireweed decline substantially within the first 10 years after clearcutting. We conclude that natural regeneration of trees has potential to help achieve stocking targets and also to maintain natural diversity of tree species if spatial constraints, especially thresholds in clearcut size, are considered.

scholarly journals Epixylic vegetation abundance, diversity, and composition vary with coarse woody debris decay class and substrate species in boreal forest

2018 ◽  
Vol 48 (4) ◽  
pp. 399-411 ◽  
Author(s):  
Praveen Kumar ◽  
Han Y.H. Chen ◽  
Sean C. Thomas ◽  
Chander Shahi
Keyword(s):  
Species Richness ◽  
Species Diversity ◽  
Boreal Forest ◽  
Plant Communities ◽  
Coarse Woody Debris ◽  
Woody Debris ◽  
Percent Cover ◽  
Diverse Range ◽  
Decay Class ◽  
Wide Range

Although the importance of coarse woody debris (CWD) to understory species diversity has been recognized, the combined effects of CWD decay and substrate species on abundance and species diversity of epixylic vegetation have received little attention. We sampled a wide range of CWD substrate species and decay classes, as well as forest floors in fire-origin boreal forest stands. Percent cover, species richness, and evenness of epixylic vegetation differed significantly with both CWD decay class and substrate species. Trends in cover, species richness, and evenness differed significantly between nonvascular and vascular taxa. Cover, species richness, and species evenness of nonvascular species were higher on CWD, whereas those of vascular plants were higher on the forest floor. Epixylic species composition also varied significantly with stand ages, overstory compositions, decay classes, substrate species, and their interactions. Our findings highlight strong interactive influences of decay class and substrate species on epixylic plant communities and suggest that conservation of epixylic diversity would require forest managers to maintain a diverse range of CWD decay classes and substrate species. Because stand development and overstory compositions influence CWD decay classes and substrate species, as well as colonization time and environmental conditions in the understory, our results indicate that managed boreal landscapes should consist of a mosaic of different successional stages and a broad suite of overstory types to support diverse understory plant communities.

Distribution and abundance of coarse woody debris in a managed forest landscape of the central Appalachians

1994 ◽  
Vol 24 (7) ◽  
pp. 1317-1329 ◽  
Author(s):  
Brian C. McCarthy ◽  
Ronald R. Bailey
Keyword(s):  
Coarse Woody Debris ◽  
Forest Floor ◽  
Woody Debris ◽  
Small Diameter ◽  
Stem Density ◽  
Moderate Amount ◽  
Clear Cutting ◽  
Central Appalachians ◽  
Management Regime ◽  
Commercial Thinning

Coarse woody debris (CWD) is integral to the functioning and productivity of forested ecosystems. Standing snags and large logs on the forest floor affect soil processes, soil fertility, hydrology, and wildlife microhabitat. Few data are available pertaining to the distribution and abundance of CWD in the managed hardwood forests of the central Appalachians. We surveyed 11 stands, at various stages of development (succession) after clear-cutting (<2, 15–25, 65–90, >100 years old), to evaluate the density, volume, and biomass of trees, snags, and logs under the local forest management regime. As expected, density, volume, and biomass of CWD (stems ≥2.5 cm diameter) were greatest in young stands (<2 years old) immediately following clear-cutting; the vast majority of CWD existed as relatively labile, small-diameter, low decay state logging slash. Young stands retained a few large logs in advanced decay states but observations suggest that these elements were often disturbed (i.e., crushed) by logging equipment during the harvest process. Crushed logs do not function ecologically in the same capacity as large intact logs. A marked decline in CWD was observed in young pole stands (15–25 years old) as slash decomposed. These stands were characterized by a high density of young hardwood stump sprouts in the overstory while maintaining a moderate amount of CWD in middle size and decay states on the forest floor. More mature hardwood stands (65–90 years old) generally exhibited a decrease in live-stem density and an increase in basal area, accompanied by a slight increase in CWD. Commercial thinning presumably limits the contribution of large CWD to the forest floor. This was most clearly evident in the oldest stands (>100 years old) where large CWD was not widely observed. A striking feature across all stands was the near absence of logs in large size classes (>65 cm diameter) and a paucity of logs in mid to late decay stages. We discuss our data in the context of hardwood forest structure and management in the central Appalachians.

Suillus tomentosus tuberculate ectomycorrhizal abundance and distribution in Pinus contorta woody debris

2006 ◽  
Vol 36 (2) ◽  
pp. 460-466 ◽  
Author(s):  
Leslie R Paul ◽  
Bill K Chapman ◽  
Christopher P Chanway
Keyword(s):  
Coarse Woody Debris ◽  
Forest Floor ◽  
Pinus Contorta ◽  
Woody Debris ◽  
Soil Characteristics ◽  
Stand Age ◽  
Nitrogen Economy ◽  
Basaltic Soils ◽  
Abundance And Distribution

Tuberculate ectomycorrhizae (TEM) have been observed in decaying coarse woody debris (CWD) and may play a role in the nitrogen economy of forests. This study evaluates the occurrence of Suillus tomentosus (Kauff.) Singer, Snell and Dick TEM within CWD in Pinus contorta Dougl. ex Loud. var. latifolia Engelm. stands and relates their occurrence to CWD and soil characteristics as well as stand age. TEM were more abundant in the basal end of CWD incorporated in the forest floor than in the middle and top portions. Tubercle abundance was positively correlated with moisture and texture of CWD, degree of incorporation of CWD into the forest floor, and the amount of roots within CWD. There were significantly more TEM in CWD in young stands than in old stands and on sites with granitic soils than on sites with basaltic soils. Highly degraded CWD that is well incorporated in the forest floor appears to be an important microhabitat for the formation and occurrence of TEM.

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