Seedling establishment in relation to microhabitat variation in a windthrow gap in a boreal Pinus sylvestris forest

Abstract. The characteristics of microhabitats of established Pinus sylvestris and Betula seedlings were studied in a small windthrow gap in a mature P. sylvestris-dominated forest in the Petkeljärvi National Park in eastern Finland. Seedlings were strongly clustered in disturbed microhabitats, particularly uprooting pits and mounds, formed by tree falls. They covered 3% of the 0.3.ha study area consisting of the gap and some of the forest edge. Although Betula occurred only as scattered individuals in the dominant canopy layer of the forest, it accounted for 30% of the seedlings found in the study area. Betula regeneration was almost completely restricted to pits and mounds, where 91% of the seedlings were found. Uprooting spots were also the most important regeneration microhabitats for Pinus, where 60% of the seedlings grew, even though the seedlings were found in other substrates as well, particularly on sufficiently decomposed coarse wood. Undisturbed field- and bottom-layer vegetation had effectively hindered tree seedling establishment, which emphasises the role of soil disturbance for regeneration. While the establishment of seedlings was found to be clearly determined by the availability of favourable regeneration microhabitats, the early growth of seedlings was affected by a complex interaction of environmental variables, including the type of microhabitat, radiation environment and interferences caused by competing seedlings and adjacent trees. In the most important regeneration microhabitats, i.e. in uprooting pits and on mounds, the distributions of the local elevations of Pinus and Betula seedlings were different. Pinus seedlings occurred closer to ground level, i.e. on the fringes of pits and lower on mounds, while Betula seedlings grew deeper in pits and higher on mounds. The position of the Betula seedlings indicate that they may have a competitive advantage over Pinus seedlings in the dense seedling groups occurring in uprooting spots. We suggest that this initial difference in Pinus and Betula establishment may affect the subsequent within-gap tree species succession and can, in part, explain the general occurrence of Betula in conifer-dominated boreal forests.     

Impacts of freeze-thaw processes on antioxidant activities and osmolyte contents of Syntrichia caninervis under different desert microhabitats

 齿肋赤藓(Syntrichia caninervis)作为典型的耐旱藓类, 广泛分布于世界干旱和半干旱荒漠地区, 是古尔班通古特沙漠生物土壤结皮中的优势藓类植物。该沙漠冬季具有稳定的降雪, 初春的积雪融化为植物的生长提供了良好的水热条件。荒漠藓类植物叶片仅具一层细胞, 对外界环境的变化十分敏感, 有关荒漠藓类植物在冬季和早春地表冻融交替过程中如何适应环境剧烈变化的研究鲜见报道。该研究探讨了生长于3种不同微生境(活灌丛、枯死灌丛和裸露地)下的齿肋赤藓, 经由冬季低温冻结到早春融雪复水再到春季中旬自然干燥过程中的生理生化变化特征。结果表明: 不同冻融期、微生境及二者的交互作用能够显著影响齿肋赤藓的渗透调节物质(游离脯氨酸、可溶性糖、可溶性蛋白)含量、丙二醛(MDA)含量、抗氧化酶活性(过氧化氢酶(CAT)、过氧化物酶(POD)和超氧化物歧化酶(SOD)活性)。冬季低温冻结期的极端低温和春季中旬的干燥环境使得齿肋赤藓可溶性糖和MDA含量, 以及3种抗氧化酶活性均显著高于早春融雪期, 可溶性蛋白含量显著低于融雪期。同时, 在融雪期灌丛遮阴所形成的“冷岛效应”使得生长于灌丛下的齿肋赤藓植株可溶性糖和MDA含量显著高于枯死灌丛和裸露地。但灌丛的存在也为春季中旬干旱无雨期齿肋赤藓提供了一个相对良好(含水量高)的生活环境, 其下齿肋赤藓的渗透调节物含量和抗氧化酶活性均显著低于其他两个生境。在整个冻融过程中裸露地齿肋赤藓的3种抗氧化酶活性均显著高于灌丛下, 这可能是由于生活于裸露地的苔藓有更强的耐胁迫特性。     

Long-term effects of nitrogen deposition on vegetation in a deciduous forest near Munich,Germany

Question: What are the main reasons for changes in the spatial distribution of vegetation types during the last four decades? Location: Isolated small deciduous forest; surrounded by farmland in the northeast of Munich (Germany). Methods: Based on sequential vegetation mapping from the last four decades the spatial development of the vegetation was analysed. Additionally, environmental parameters (soil parameters, PAR, N-deposition) have been analysed to describe the different vegetation types. Results: By linking the vegetation types to environmental parameters, it was possible to identify N-deposition as the most important factor for the changes. In the 1960s to 1980s the replacement of vegetation types adapted to N-poor conditions by N-rich vegetation was very fast. A vegetation type containing species signifying soil impoverishment vanished totally, another vegetation type indicating nutrient poor conditions decreased dramatically. However, since 1985 up to now the decrease of N-poor vegetation types has slowed, but is still ongoing. As a reason for the decreased rate of replacement, we stressed changes in the vertical structure: From 1961 to 1985 both N-deposition as well as changes in vertical vegetation structure seem to be important. Since 1985 up to now only minor changes in vertical structure could be found; changes are mainly due to N-availability. Conclusion: In this paper, the limitations of different methods to detect vegetation changes are discussed. We focus on the potentials of historical vegetation data and vegetation maps. It is shown that valuable information on N-induced vegetation changes can be retrieved from historical vegetation data.     

Multiple Scales of Temporal Variability in Ecosystem Metabolism Rates: Results from 2 Years of Continuous Monitoring in a Forested Headwater Stream

Headwater streams are key sites of nutrient and organic matter processing and retention, but little is known about temporal variability in gross primary production (GPP) and ecosystem respiration (ER) rates as a result of the short duration of most metabolism measurements in lotic ecosystems. We examined temporal variability and controls on ecosystem metabolism by measuring daily rates continuously for 2 years in Walker Branch, a first-order deciduous forest stream. Four important scales of temporal variability in ecosystem metabolism rates were identified: (1) seasonal, (2) day-to-day, (3) episodic (storm-related), and (4) inter-annual. Seasonal patterns were largely controlled by the leaf phenology and productivity of the deciduous riparian forest. Walker Branch was strongly net heterotrophic throughout the year with the exception of the open-canopy spring when GPP and ER rates were co-equal. Day-to-day variability in weather conditions influenced light reaching the streambed, resulting in high day-to-day variability in GPP particularly during spring (daily light levels explained 84% of the variance in daily GPP in April). Episodic storms depressed GPP for several days in spring, but increased GPP in autumn by removing leaves shading the streambed. Storms depressed ER initially, but then stimulated ER to 2–3 times pre-storm levels for several days. Walker Branch was strongly net heterotrophic in both years of the study, with annual GPP being similar (488 and 519 g O₂ m⁻² y⁻¹ or 183 and 195 g C m⁻² y⁻¹) but annual ER being higher in 2004 than 2005 (−1,645 vs. −1,292 g O₂ m⁻² y⁻¹ or −617 and −485 g C m⁻² y⁻¹). Inter-annual variability in ecosystem metabolism (assessed by comparing 2004 and 2005 rates with previous measurements) was the result of the storm frequency and timing and the size of the spring macroalgal bloom. Changes in local climate can have substantial impacts on stream ecosystem metabolism rates and ultimately influence the carbon source and sink properties of these important ecosystems.     

Climate‐induced warming imposes a threat to north European spring ecosystems

Interest in climate change effects on groundwater has increased dramatically during the last decade. The mechanisms of climate‐related groundwater depletion have been thoroughly reviewed, but the influence of global warming on groundwater‐dependent ecosystems (GDEs) remains poorly known. Here we report long‐term water temperature trends in 66 northern European cold‐water springs. A vast majority of the springs (82%) exhibited a significant increase in water temperature during 1968–2012. Mean spring water temperatures were closely related to regional air temperature and global radiative forcing of the corresponding year. Based on three alternative climate scenarios representing low (RCP2.6), intermediate (RCP6) and high‐emission scenarios (RCP8.5), we estimate that increase in mean spring water temperature in the region is likely to range from 0.67 °C (RCP2.6) to 5.94 °C (RCP8.5) by 2086. According to the worst‐case scenario, water temperature of these originally cold‐water ecosystems (regional mean in the late 1970s: 4.7 °C) may exceed 12 °C by the end of this century. We used bryophyte and macroinvertebrate species data from Finnish springs and spring‐fed streams to assess ecological impacts of the predicted warming. An increase in spring water temperature by several degrees will likely have substantial biodiversity impacts, causing regional extinction of native, cold‐stenothermal spring specialists, whereas species diversity of headwater generalists is likely to increase. Even a slight (by 1 °C) increase in water temperature may eliminate endemic spring species, thus altering bryophyte and macroinvertebrate assemblages of spring‐fed streams. Climate change‐induced warming of northern regions may thus alter species composition of the spring biota and cause regional homogenization of biodiversity in headwater ecosystems.     

苔藓植物对贵州丹寨汞矿区汞污染的生态监测

采用野外生态学系统取样方法和室内理化分析方法相结合,分别从苔藓植物地球化学特征、物种丰富度、群落类型、群落的结构等生物学特征上,探讨苔藓植物对丹寨汞矿区汞污染的生态监测。丹寨汞矿区苔藓植物共20个科,34属85种;真藓科和丛藓科占优势。在汞污染程度不同的4种生境梯度中,汞含量均超出国家土壤环境质量三级土标准的10倍以上。各研究生境梯度真藓(Bryum argenteum),丛生真藓(Bryum caespiticium)和狭叶小羽藓(Haplocladium angustifolium)体内的汞含量与其生境基质(土壤)的汞含量在P＜0.01水平上呈显著的正相关;且信度系数R均大于0.9,表明被测苔藓植物在地球化学特征上具有监测环境汞污染的生态功能。物种丰富度特征方面,汞污染严重区域物种丰富度较低;而污染程度相对较轻区域物种丰富度则较大;表明了该区苔藓植物丰富度总体上可以作为环境中汞污染的监测指标之一。群落学特征方面,群落类型丰富度在汞污染较重的区域丰富度较低;而苔藓植物群落结构方面,在汞污染较重区域过渡到汞污染相对较轻区域,纯群落数在逐渐减少,但3种及3种以上组成的群落数却有所增加。表现了苔藓群落结构组成越简单则该区汞污染较严重,苔藓植物结构组成越复杂则该区的汞污染程度相对较轻。这说明了苔藓植物群落特征也较适合作为汞矿区生态监测的指标。在汞污染区过渡到相对清洁区的污染过渡带,苔藓物种多样性和群落类型趋于多样化,产生了较明显群落边缘效应。     

Phyllosphere nitrogen relations: reciprocal transfer of nitrogen between epiphyllous liverworts and host plants in the understorey of a lowland tropical wet forest in Costa Rica

Epiphyllous bryophytes on tropical rainforest plants acquire nutrients from throughfall and free-living N2-fixing organisms, but may also depend directly on host leaf leachates. By contrast, after drying events bryophytes lose significant quantities of nutrients through leaching that can be taken up by host leaves. To assess a potential nutritional interdependency, nitrogen fluxes between epiphyllous liverworts and their host leaves (Carludovica drudei, Costus laevis, Dieffenbachia concinna, Pentagonia wendlandii) were quantified by in situ15N-labelling techniques in a lowland rainforest, Piedras Blancas National Park, Costa Rica. Depending on host species, epiphyllous bryophytes met between 1 and 57% of their N demand from host leaf leachates. Externally supplied 15N was taken up both by epiphylls and host leaves, but N from epiphyll leachates accounted for < 2.5% of host leaf N after 14 d. Long-term observations (180 d) demonstrated the highly dynamic nature of phyllosphere N of the investigated tropical rainforest understorey and an intermittent sink capacity of epiphyllous bryophytes.     

Understory Vegetation Dynamics of North American Boreal Forests

Understory vegetation is the most diverse and least understood component of North American boreal forests. Understory communities are important as they act as drivers of overstory succession and nutrient cycling. The objective of this review was to examine how understory vegetation abundance, composition, and diversity change with stand development after a major stand replacing disturbance. Understory vegetation abundance and diversity increase rapidly after fire, in response to abundant resources and an influx of disturbance adapted species. The highest diversity occurs within the first 40 years following fire, and declines indefinitely thereafter as a result of decreasing productivity and increased dominance of a small number of late successional feather mosses and woody plant species. Vascular plant and bryophyte/lichen communities undergo very different successional changes. Vascular plant communities are dynamic and change more dramatically with time after fire, whereas bryophyte and lichen communities are much slower to establish and change over time. Considerable variations in these processes exist depending on canopy composition, site condition, regional climate, and frequently occurring non-stand-replacing disturbances. Forest management practices represent a unique disturbance process and can result in different understory vegetation communities from those observed for natural processes, with potential implications for overstory succession and long-term productivity. Because of the importance of understory vegetation on nutrient cycling and overstory composition, post-harvest treatments emulating stand-replacing fire are required to maintain understory diversity, composition, and promote stand productivity in boreal forests.     

Nitrogen deposition enhances moss growth,but leads to an overall decline in habitat condition of mountain moss‐sedge heath

Ecosystems are subject to multiple, natural and anthropogenic environmental influences, including nitrogen (N) deposition, land use and climate. Assessment of the relative importance of these influences on biodiversity and ecosystem functioning is crucial for guiding policy and management decisions to mitigate global change; yet, few studies consider multiple drivers. In the UK, ongoing loss of the internationally important arctic/alpine moss‐sedge community, Racomitrium heath, has been linked to elevated N deposition, high grazing pressures and their combination; however, the relative importance of these drivers remains unclear. We used environmental gradients across the habitat's European distribution (UK, Faroes, Norway and Iceland) to investigate the relative impact of N deposition and grazing pressure, as well as climate, on the condition of the dominant moss species, Racomitrium lanuginosum. Key variables including tissue chemistry, growth and cover were measured at 36 sites, and multiple linear regressions were used to examine the relative importance of the drivers across sites. Our results clearly show that regional variation in the condition of R. lanuginosum across Europe is primarily associated with the impacts of N deposition, with climate (air temperature) and grazing pressure playing secondary roles. In contrast to previous experimental studies, we found moss growth to be stimulated by elevated N deposition; this apparent discrepancy may result from the use of artificially high N concentrations in many experiments. Despite increased growth rates, we found that moss mat depth and cover declined in response to N deposition. Our results suggest that this is due to increased decomposition of material in the moss mat, which ultimately leads to loss of moss cover and habitat degradation. This study clearly demonstrates both the key role of N deposition in degradation of Racomitrium heath and the importance of observational studies along natural gradients for testing predictions from experimental studies in the real world.