Natural disturbance and tree species coexistence in an old-growth beech - dwarf bamboo forest,southwestern Japan

Abstract. The structure and composition of a cool-temperate old-growth beech (Fagus crenata) - dwarf bamboo (Sasa spp.) forest, partially affected by landslide disturbance, in the Daisen Forest Reserve of southwestern Japan, were investigated in relation to forest floor and canopy conditions. All stems ≥ 4 cm DBH were mapped on a 4-ha plot and analyses were made of population structure, spatial distribution and spatial association of major tree species. The dominant species, F. crenata, which had the maximum DBH among the species present, had the highest stem density. However, for other species, larger-sized species had lower stem density with few smaller stems or saplings, while smaller-sized species had higher stem density with many smaller stems or saplings. Canopy trees of F. crenata were distributed randomly in the plot, while its stems in the other layers and all other species were distributed patchily. Small patches represent gap-phase regeneration. Larger patches correlate with landslide disturbance, difference in soil age, or the presence/absence of Sasa. Cluster analysis for spatial associations among species and stems in the different layers revealed that the forest community consists of several groups. One main group was formed on sites not covered with Sasa. This group contained a successional subgroup (from Betula grossa to Acer mono and/or F. crenata) initiated by landslide disturbance and a subgroup of tree species that avoid Sasa. Another group was formed on sites with mature soils covered largely with Sasa. This contained associations of canopy trees of F. crenata and smaller-sized tree species such as Acanthopanax sciadophylloides and Acer japonicum. It is found that the community of this old-growth beech forest is largely organized by natural disturbance and heterogeneous conditions of the forest floor (difference in soil age and presence/absence of Sasa). The existence of these different factors and the different responses of species to them largely contribute to the maintenance of tree species diversity in this forest.; Keywords: Cluster analysis; Fagus crenata; Forest dynamics; Gap; Landslide; Spatial pattern.     

Spatiotemporal distribution of growth releases and suppressions along a landslide body

Our study analyzes the growth response (release or suppression) of Norway spruce trees growing along a landslide zone in eastern Czech Republic. A total of one hundred and eighty-six increment cores were extracted from Norway spruce (Picea abies (L.) Karst.) individuals, which were affected by two different disturbances, the Girová landslide in May 2010 and an anthropogenic cut-off in the neighborhood of the landslide later the same year. Growth changes were analysed in three zones that were defined according to the type of effect the disturbance had on the surrounding vegetation. The aims of our study are to (i) detect growth changes in trees that survived the disturbances in 2010, (ii) evaluate the delay time of the growth reaction to the disturbances, (iii) compare how growth changes differed in response to the two different disturbance types (natural landslide vs. anthropogenic harvesting and deforestation), and (iv) investigate spatio-temporal differences in the growth changes. Our results indicate that tree growth changed in response to the altered environmental conditions following the 2010 disturbances. The changes vary depending on the intensity of the disturbance and its effect on the forest stand. Trees in Zone 1 responded with a slight growth release (14.6 % of responding trees), which was strongest after 2013. However, growth suppression (85.4 %) was the dominant reaction in Zone 1; with the majority of trees showing growth suppression in 2014, four years after the events. The strongest and most abrupt growth release (66.1 %) occurred in Zone 2 in 2011, after a one-year delay. Since 2010, we have observed a trend of growth suppression (33.9 %) in this zone. In Zone 3, following a one-year delay, growth release has occurred gradually in about a third of the trees (37.0 %). The majority of trees in this zone have responded with growth suppression (63.0 %) in 2010 and with a three-year delay after 2013. We also found differences in how tree growth responds to anthropogenic and landslide disturbances, as well as spatio-temporal differences related to the extent of post-disturbance changes.     

Vegetation succession at the abandoned Ogushi sulfur mine, central Japan

We surveyed plant community development at the abandoned Ogushi sulfur mine. We found seven communities dominated by the following respective species: Deschampsia flexuosa, Miscanthus sinensis, shrub willow, Gaultheria miqueliana–Betula ermanii, Sasa senanensis–Betula ermanii, willow–Betula ermanii, and Sasa kurilensis–Abies veitchii. We examined the succession of these communities, in which younger communities of low height and ground cover contained seedlings of the successive communities that were taller and had higher ground cover. To understand the development of these different communities, we surveyed damage from mining pollution and effects of immature soils formed by landslides. The average pH (H₂O) was 4.12, and aluminum concentrations were not sufficiently high to damage plant growth, except in areas where sulfur had been mined. The organic carbon and nitrogen content in soil samples were very low because of a delay in soil development caused by a large landslide in 1937. Hence, succession was positively correlated with the soil development stage. The delay in soil development after a large landslide influenced the seven successional steps of the plant communities, but mineral poisons at the abandoned Ogushi sulfur mine had no effect on succession.     

Eco-environmental changes assessment at the Chiufenershan landslide area caused by catastrophic earthquake in Central Taiwan

A large-scale landslide, caused by the catastrophic earthquake on 21 September 1999, occurred at the Chiufenershan area in Central Taiwan. Multi-temporal SPOT satellite images coupled with a self-organizing map neural network, terrain analysis, Universal Soil Loss Equation, and landscape patch indicators were used to assess eco-environmental changes of the denudation sites, such as changes of the post-quake landslide, terrain displacement, soil erosion, and landscape ecology. The extracted area soon after the earthquake was 215.68 ha. From 1999 through 2006, the denudation area declined to 113.36 ha, which indicates that about 47.44% of the landslide has been restored. Based on terrain analysis for the denudation sites, the debris volumes at the collapsed and deposited areas are 31,896,667 m³ and 39,537,067 m³, respectively. The large amount of debris blocked two streams, the Satsikenghsi and the Chiutsaihuhsi, to form two landslide-dammed lakes. The annual erosion depth soon after the earthquake reached 22.07 mm, about 3.59 times as high as pre-quake. Without vegetation cover on the topsoil, the denudation sites became high-erosion areas during subsequent typhoon seasons. However, with landslide restoration, annual soil erosion depth prediction has reduced to 13.54 mm, about 2.21 times as high as pre-quake. In addition, the assessment of landscape patch indicators also points out the heterogeneity and the degree of richness of the landscape due to vegetation recovery at the landslide area. The analyzed results show that nature itself has a robust ability to restore its original landscape and mitigate disaster impacts for the destroyed eco-environment.     

Formation and maintenance of community boundaries in a sub‐alpine forest landscape in northern Japan

Abstract. We focused on community boundaries in a sub‐alpine forest landscape in the Shiretoko Peninsula, northern Japan. Gradient‐directed transects were conducted on the northwestern slope (ranging 500–600 m a.s.l.) of Mount On'nebetsu (1331 m), where complex topography was formed by past landslides. Pioneer Picea glehnii made up a mosaic of pure stands related to landslides. Structural and compositional changes from P. glehnii pure stands to P. glehnii and Abies sachalinensis mixed stands were characterized by ca. 20 m transitional zones over the landscape. Stand density of the species changed across boundaries. A. sachalinensis preferred less undulated slopes with deep soil and P. glehnii preferred undulated rocky sites. Positive spatial associations between overstorey‐understorey P. glehnii were found at undulated core parts of P. glehnii pure stands. Short‐lived A. sachalinensis grew faster to the smaller maximum size than long‐lived P. glehnii. Undulated topography controlled the increase of A. sachalinensis and provided regeneration sites for P. glehnii, which prevented the general trend of canopy replacement from P. glehnii to late‐successional A. sachalinensis. However, the locations of current boundaries were not accordant with the topographic changes in the meso‐scale landscape. Initial P. glehnii pure stands would extend to larger areas if current patterns reflect vegetation recovery since the last landslide. P. glehnii pure stands with accurate boundaries were not maintained by topographic complexity, but were dynamically arranged by the one‐sided canopy replacements from P. glehnii to A. sachalinensis at less undulated slopes in the sub‐alpine forest landscape.     

Earthquake impacts in old‐growth Nothofagus forests in New Zealand

Abstract. Six stands located on different land forms in mixed old‐growth Nothofagus forests in the Matiri Valley (northwest of South Island, New Zealand) were sampled to examine the effects of two recent large earthquakes on tree establishment and tree‐ring growth, and how these varied across land forms. 50 trees were cored in each stand to determine age structure and the cores were cross‐dated to precisely date unusual periods of radial growth. The 1968 earthquake (M = 7.1, epicentre 35 km from the study area) had no discernible impact on the sampled stands. The impact of the 1929 earthquake (M = 7.7, epicentre 20 km from the study area) varied between stands, depending on whether or not they had been damaged by soil or rock movement. In all stands, the age structures showed a pulse of N. fusca establishment following the 1929 earthquake, with this species dominating establishment in large gaps created by landslides. Smaller gaps, created by branch or tree death, were closed by both N. fusca and N. menziesii. The long period of releases (1929–1945) indicates that direct earthquake damage was not the only cause of tree death, and that many trees died subsequently most likely of pathogen attack or a drought in the early 1930s. The impacts of the 1929 earthquake are compared to a storm in 1905 and a drought in 1974–1978 which also affected forests in the region. Our results confirm that earthquakes are an important factor driving forest dynamics in this tectonically active region, and that the diversity of earthquake impacts is a major source of heterogeneity in forest structure and regeneration.     

Patterns of restoration of soil physciochemical properties and microbial biomass in different landslide sites in the sal forest ecosystem of Nepal Himalaya

The pattern of natural restoration in soil components and processes was documented in five landslide-damaged (1–58-year-old) sites in the moist tropical sal (Shorea robusta) forest ecosystem of Nepal Himalaya. Comparisons were made with an undisturbed forest site in the same region. Concentrations of soil organic C, total N, total P and extractable nutrients (Ca, Mg and K) increased with the age of sites. The 58-year-old site showed concentrations of soil organic C, total N and total P that were 75–89% of concentrations in the undisturbed sal forest. The soil microbial biomass, the active fraction of soil organic matter, showed similar seasonal variations at all sites. The amount of mean microbial biomass (expressed as C, N and P contents) increased 4–5 times at the 58-year-old site relative to the 1-year-old site, and the bulk increase occurred within the initial 15 year. The increase in the C/N ratio of soil microbial biomass with age (9.4–11.6 years) reflected change in its composition. Although the net N-mineralization rate increased consistently until 58 years of age, the proportion of nitrification rate relative to ammonification rate distinctly decreased beyond 40 years. On the other hand, the soil available-N (both NO₃⁻ and NH₄⁺) concentrations increased from 1 to 40 year and then declined; with age the proportion of NH₄⁺ increased, however. Rates of restoration in soil properties were faster in the early successional stages (1–15 year) than late stages. Among different soil properties the restoration of soil microbial biomass (C and N) was faster than soil organic C and total N. Best fit power function models showed that the estimated times for the 58-year-old site to reach the level of the undisturbed, mature sal forest would be about 30–35 year for microbial biomass (C and N) and about 100–150 year for organic C and total N. Higher accumulation of soil microbial biomass and high N-mineralization rate at late successional stages indicated the re-establishment of enriched soil and restitution of nutrient cycling during the course of ecosystem restoration.