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52 results for “mountain ecosystems”

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zenodo36/100

Fig. 1 in Ashworthius sidemi Schulz, 1933 (Trichostrongylidae: Haemonchinae) in mountain ecosystems - a potential risk for the Tatra chamois Rupicapra rupicapra tatrica (Blahout, 1971/1972)

Fig. 1. Map of Tatras showing the geographical origin of the animals included in the study.

opencc-by-4.0Apr 2021View details →
zenodo36/100

Agreement of multiple night- and daytime filtering approaches of eddy covariance-derived net ecosystem CO2 exchange over a mountain forest. Reproducible workflow.

<p>Datasets and python scripts to reproduce results from the publication&nbsp;<em>Agreement of multiple night- and daytime filtering approaches of eddy covariance-derived net ecosystem CO2 exchange over a mountain forest.</em></p> <p>See README.txt for a description of the single files.</p>

opencc-by-4.0Jul 2024View details →
dryad36/100

The diversity of mycorrhiza-associated fungi and trees shape subtropical mountain forest ecosystem functioning

<p><span><strong>Aim</strong>: </span><span>Mycorrhiza play key roles in ecosystem structure and functioning in forests. However, how different mycorrhizal types influence mountain forest biodiversity-ecosystem functioning relationships is largely unknown. We evaluate how the diversity of distinct mycorrhiza-associated fungi and trees shape forest carbon storage along elevational gradients.</span></p> <p><span><strong>Location</strong>:</span><span> Gaoligong Mountains within Hengduan Mountains, Southwest China. </span></p> <p><span><strong>Taxon</strong>: </span><span>Seed plants and mycorrhizal fungi.</span></p> <p><span><strong>Methods</strong>: </span><span>We used the data from 31 subtropical forest plots along elevational gradients on two aspects (east and west) of the mountain. We quantified species richness of trees and symbiotic fungi and assigned both to their mycorrhizal type (arbuscular mycorrhiza (AM), ectomycorrhiza (EcM) and ericoid mycorrhiza (ErM)). We then examined the diversity effects of mycorrhiza-associated fungi and trees on above-ground carbon stored in trees and organic carbon stored in soils. </span></p> <p><span><strong>Results</strong>:</span><span> Species richness was highest for AM trees (79.5%), followed by ErM trees (13.4%) and then EcM trees (7.1%). Species richness of AM-associated trees and fungi decreased with increasing elevation, while ErM-associated trees and fungi showed an opposite trend. EcM-associated diversity followed a hump-shaped relationship with elevation. Positive relationships between diversity and above-ground carbon were detected in all three mycorrhizal associations, but despite low species number, canopy-dominating EcM trees comprised 64.4% of the amount of above-ground carbon. Furthermore, community-weighted means of height exhibited positive correlations with forest above-ground carbon, indicating that positive selection effects occur. Soil organic carbon was positively related to EcM-associated fungi diversity, above-ground carbon mass and soil nitrogen availability, with the latter having the strongest direct effects. </span></p> <p><span><strong>Main</strong> <strong>conclusions</strong>: </span><span>The distributions of forest biodiversity and carbon storage can be modulated by distinct mycorrhizal fungi and trees. Moreover, future global changes (e.g., climate warming, intensifying nitrogen deposition) could alter the mycorrhizal-mediated biodiversity-ecosystem functioning relationships in mountain forests.</span></p>

opencc-zeroDec 2022View details →
dryad36/100

Climate change accelerates ecosystem restoration in the mountain forests of Central Europe

<ol> <li>Restoring degraded forest ecosystems is an important element in the ongoing challenge to sustain the integrity and functioning of the biosphere. However, the evaluation of restoration success is hampered by long lead times of management measures in forests. Moreover, forest change is accelerating in the absence of management because of ongoing climate change. Yet, because a counterfactual is frequently missing, it remains unclear whether restoration measures are aided or impeded by climate change. </li> <li>Here, we analyzed the pace and success of forest restoration under climate change, combining field data and simulation modelling. We focused on the management zone of Berchtesgaden National Park (BGNP), Germany, where restoration aims to restore homogeneous Norway spruce (<em>Picea abies</em>) forests to structurally diverse mixed mountain forests. We evaluated three alternative restoration strategies: Two active strategies focused on planting the currently underrepresented silver fir (<em>Abies alba</em>) and European beech (<em>Fagus</em> <em>sylvatica</em>) but differing in the creation of gap-cuts, and a third passive restoration strategy without interventions. Strategies were simulated with the forest landscape model iLand from 2020 to 2100 under different climate scenarios (historic, RCP 2.6, 4.5, and 8.5).</li> <li>The forests of BGNP developed into structurally diverse and mixed forests under all evaluated management strategies, and differences between active and passive restoration were generally small. While restoration goals for forest structure were largely met by 2100, forest composition remained far from target in all strategies. Climate change aided restoration by significantly increasing the prevalence of silver fir and European beech (+104.2 % to +258.6 %). Field data on short-term restoration effects were in line with simulated long-term trajectories.</li> <li> <em>Synthesis and applications</em>. We here show that forest restoration efforts in Central European mountain forests will likely be accelerated by climate change. Nonetheless, the slow pace of restoration underscores the need for taking action. Our study highlights that active restoration measures such as tree planting can bring the system closer to restoration targets. However, it also demonstrates that passive restoration (no intervention) is a viable option for management, highlighting the need to evaluate restoration measures against the counterfactual of a no-intervention strategy.</li> </ol>

opencc-zeroOct 2023View details →
dryad36/100

Data from: Beyond the trail: understanding non-native plant invasions in mountain ecosystems

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publicOct 2025View details →
dryad36/100

Riparian ecosystem collapse in Rocky Mountain National Park

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publicApr 2025View details →
dryad36/100

The diversity of mycorrhiza-associated fungi and trees shape subtropical mountain forest ecosystem functioning

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publicDec 2022View details →
dryad36/100

Effects of species richness and turnover on ecosystem functioning in heterogeneous environments of two tropical mountains

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publicOct 2025View details →
dryad36/100

Data from: Testing the ectomycorrhizal dominance hypothesis for ecosystem multifunctionality in a subtropical mountain forest

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publicJul 2024View details →
dryad36/100

Climate change accelerates ecosystem restoration in the mountain forests of Central Europe

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publicApr 2024View details →
dryad36/100

Citizen science data reveal altitudinal movement and seasonal ecosystem use by hummingbirds in the Andes Mountains

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publicNov 2023View details →
dryad32/100

Mountain biodiversity and ecosystem functions: Interplay between geology and contemporary environments

<p><span>Although biodiversity and ecosystem functions are strongly shaped by contemporary environments such as climate and local biotic and abiotic attributes, relatively little is known about how they depend on long-term geological processes. Here, along a 3000-m elevational gradient with tectonic faults on the Tibetan Plateau, we studied the joint effects of geological and contemporary environments on biological communities<i>, </i>such as the diversity and community composition of plants and soil bacteria,<i> </i>and ecosystem functions<i>.</i> We found that these biological communities and ecosystem functions generally show consistent elevational breakpoints at 2000–2800 m, which coincide with Indus-Yalu suture zone fault and are similar to the elevational breakpoints of soil bacteria on another mountain range 1000 km away. Mean annual temperature, soil pH and moisture were the primary contemporary determinants of biodiversity and ecosystem functions, which supports previous findings. However, compared to the models excluding geological processes, inclusion of geological effects, including parent rock and weathering, increased 67.9% and 35.9% of the explained variations in plant and bacterial communities, respectively. Such inclusion increased 27.6% of the explained variations in ecosystem functions. The geological processes thus provide additional links to ecosystem properties, which are prominent but show divergent effects on biodiversity and ecosystem functions: parent rock and weathering exert considerable direct effects on biodiversity, whereas indirectly influence ecosystem functions via interactions with biodiversity and contemporary environments. Thus, the integration of geological processes with environmental gradients could enhance our understanding of biodiversity and, ultimately, ecosystem functioning across different climatic zones.</span></p>

opencc-zeroAug 2020View details →
dryad32/100

Using proxies of microbial community‐weighted means traits to explain the cascading effect of management intensity, soil and plant traits on ecosystem resilience in mountain grasslands

<p>1. Trait-based approaches provide a framework to understand the role of functional biodiversity on ecosystem functioning under global change. While plant traits have been reported as potential drivers of soil microbial community composition and resilience, studies directly assessing microbial traits are scarce, limiting our mechanistic understanding of ecosystem functioning.</p> <p>2. We used microbial biomass and enzyme stoichiometry, and mass-specific enzymes activity as proxies of microbial community-weighted mean (CWM) traits, to infer trade-offs in microbial strategies of resource use with cascading effects on ecosystem resilience. We simulated a drought event on intact plant-soil mesocosms extracted from mountain grasslands along a management intensity gradient. Ecosystem processes and properties related to nitrogen cycling were quantified before, during and after drought to characterize ecosystem resilience.</p> <p>3. Soil microbial CWM traits and ecosystem resilience to drought were strongly influenced by grassland type. Structural equation modelling revealed a cascading effect from management to ecosystem resilience through modifications in soil nutrients, and plant and microbial CWM traits. Overall, our results depict a shift from high investment in extracellular enzymes in nutrient poor soils (oligotrophic strategy), to a copiotrophic strategy with low microbial biomass N:P and low investment in extracellular enzymes associated with exploitative plant traits in nutrient rich soils.</p> <p>4. Microbial CWM traits responses to management intensity were highly related to ecosystem resilience. Microbial communities with a copiotrophic strategy had lower resistance but higher recovery to drought, while microbial communities with an oligotrophic strategy showed the opposite responses. The unexpected trade-off between plant and microbial resistance suggested that the lower resistance of copiotrophic microbial communities enabled plant resistance to drought.</p> <p>5. Synthesis Grassland management has cascading effects on ecosystem resilience through its combined effects on soil nutrients and plant traits propagating to microbial traits and resilience. We suggest that intensification of permanent grassland management and associated increases in soil nutrient availability decreased plant-microbe competition for N under drought through the selection of drought-sensitive microbial communities with a copiotrophic strategy that promoted plant resistance. Including proxies of microbial CWM traits into the functional trait framework will strengthen our understanding of soil ecosystem functioning under global change.</p>

opencc-zeroNov 2019View details →
dryad32/100

Data from: Resilience and regime change in a southern Rocky Mountain ecosystem during the past 17000 years

Paleoecological records indicate that subalpine forests in western North America have been resilient in response to multiple influences, including severe droughts, insect outbreaks, and widely varying fire regimes, over many millennia. One hypothesis for explaining this ecosystem resilience centers on the disruption of forest dynamics by frequent disturbance and climatic variability, and the resulting development of non- steady-state regimes dominated by early-succession conifers with broad climatic tolerances, such as lodgepole pine (Pinus contorta var. latifolia Engelm. ex Wats.). To evaluate this hypothesis, we independently reconstructed the vegetation, fire, and effective-moisture histories of a small, forested watershed at 2890-m elevation in southeastern Wyoming, using sedimentary pollen and charcoal counts in conjunction with sedimentary lake-level indicators. The data indicate that prominent vegetation shifts (from sagebrush steppe to spruce-fir parkland at ca. 10.7 ka and spruce-fir parkland to pine-dominated forest at ca. 8.5 ka) coincided with changes in effective moisture. However, after lodgepole pine forests established at ca. 8.5 ka, similar hydroclimatic changes did not produce detectable vegetation responses. Fire history data show that other aspects of the ecosystem were responsive to changes in effective moisture at centennial timescales with prolonged fire-free episodes coinciding with periods of low effective moisture ca. 7.2-5.6 and 3.7-1.6 ka. Throughout our record, the ratio of ecosystem perturbation time (i.e., fire frequency and changes in effective moisture) to recovery time (assuming 200-600 year successional processes) falls within estimates of the ratio for non-steady state ecosystems. Frequent perturbations, therefore, may have prevented this ecosystem from reaching compositional equilibrium with the varied climatic conditions over the past 8.5 ka. Equilibrium states could have included more abundant spruce (Picea spp.) and fir (Abies spp.) than presently observed based on brief increases in pollen abundances of these taxa during prolonged dry, fire-free intervals. Our results show that although current climate changes favor widespread disturbance in Rocky Mountain forests, the composition of these ecosystems could be highly resilient and recover through successional dynamics over the next few decades to centuries.

opencc-zeroDec 2011View details →
zenodo32/100

Data for evaluating ecosystem protection and fragmentation of the world's major mountain regions

<p>Data developed in support of the manuscript: evaluating ecosystem protection and fragmentation of the world's major mountain regions.</p><p>Major mountain regions and their file abbreviations include: Alb=Albertine Rift; Alp=Alps; And=Andes; EaR=Great Eastern Ranges; Him=Himalayas; and Y2Y: Yellowstone to Yukon.</p><p>Files:</p><p>GlobalMountain_ecosystems.zip - spatial dataset (TIFF)&nbsp;with unique integer values encoded as: (landform * 10000) + (biome ID * 100) + (climate region ID).</p><p>GlobalMountain_humanmod.zip -&nbsp;&nbsp;spatial dataset (TIFF)&nbsp;with values ranging 0.0 (not human modified) to 1.0 (human modified).</p><p>GlobalMountain_protectedareas.zip - spatial dataset (TIFF) with integer values of 1 representing protected areas (IUCN categories I-IV).</p><p>GlobalMountain_regions.zip - spatial datasets (shapefiles) of the regions with 0, 10, and 30 km buffer.</p><p>GlobalMountain_samples.zip - tabular datasets (*.csv) of random samples within each region containing variables on: protected area, human modification, distance from ecosystem edge, ecosystem ID.</p><p>Google Earth Engine code.</p>

opencc-by-4.0Nov 2023View details →
dryad32/100

Influence of biomimicry structures on ecosystem function in a Rocky Mountain incised stream

<p>Rising levels of stream degradation have motivated a boom in restoration projects across the globe. However, post-restoration monitoring is still frequently lacking and does not always incorporate biotic responses to changes in the physical template. Beaver mimicry structures (BMS) are becoming a popular tool to restore degraded streams throughout the American West, but relatively little is known about how these installations influence both biotic and abiotic factors, with consequences for ecosystem functioning. We monitored basal resources, organic and inorganic material standing stocks, and macroinvertebrate density, biomass, and production to quantify functional responses to BMS installation. We compared conditions at BMS sites to naturally occurring beaver dam and reference riffle sites in a low-gradient stream in southwest Montana, USA. Thermal ranges were contracted, and daily maximum temperatures were higher, in the BMS treatment compared to the reference riffle treatment. Fine sediment standing stock and basal resources were similar in beaver and BMS treatments, and both treatments were higher than reference riffles. All treatments differed in macroinvertebrate density, which was highest in the Beaver treatment, followed by Mimic and then Reference treatment. Biomass and secondary production were higher in Beaver and BMS treatments compared to the Reference treatment, but only Beaver and Reference treatments differed significantly, likely due to differences in physical habitat and basal resource availability. Consequently, production of collector-gatherers in the BMS treatment and shredders in the beaver treatment was higher than in reference riffles. Changes to local hydrology and sediment dynamics resulting from BMS influence biotic functional responses like organic material standing stock and secondary production, creating habitat and ecosystem function distinct from riffles and similar to target conditions of natural beaver dams. To continue to improve BMS as a standard restoration practice, future research could consider the extent of degradation, increasing temporal scale of monitoring. alterations to aquatic-terrestrial subsidies and impacts to fishes.</p>

opencc-zeroNov 2021View details →
dryad32/100

Data from: Resilience and regime change in a southern Rocky Mountain ecosystem during the past 17000 years

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publicFeb 2012View details →
dryad32/100

Data from: Future ecosystem services from European mountain forests under climate change

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publicAug 2017View details →
dryad32/100

Using proxies of microbial community‐weighted means traits to explain the cascading effect of management intensity, soil and plant traits on ecosystem resilience in mountain grasslands

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publicNov 2019View details →
dryad32/100

Mountain biodiversity and ecosystem functions: Interplay between geology and contemporary environments

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publicAug 2020View details →

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Allen Brain Atlas

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allen-brain-atlas
neuroscienceopenDocumentation, web resources, and API references are available online.
Last verified 2026-04-30Open record

Annotated Behaviour and Observability Dataset (ABODe)

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abode-home-cage
behavioral-neuroscienceopenThe DataShare record exposes download links for annotations, documentation, license text, and the zipped per-snippet data directory.
Last verified 2026-04-30Open record

DANDI Archive for NWB datasets

DANDI is a BRAIN Initiative archive for publishing and sharing neurophysiology data, including electrophysiology, optophysiology, and behavioral data packaged as NWB and related standards.

dandi-nwb
electrophysiologyopenPublished Dandiset metadata and archive endpoints are available through the production DANDI API.
Last verified 2026-04-30Open record

International Brain Laboratory public data

The International Brain Laboratory public data releases expose standardized mouse decision-making experiments, including Neuropixels recordings, widefield calcium imaging, behavior, and session metadata accessed through the ONE API.

ibl
behavioral-neuroscienceopenPublic sessions can be searched and loaded from the IBL public data server through ONE.
Last verified 2026-04-29Open record

OpenNeuro

OpenNeuro is a free, open platform for sharing neuroimaging datasets, with public search, dataset pages, and download paths for web, S3, DataLad, and the OpenNeuro CLI.

openneuro
neuroscienceopenPublished datasets are available on demand over the internet.
Last verified 2026-04-29Open record