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124 results for “shrubland”

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zenodo36/100

Data from: Diversity of Andean shrubland puna butterflies of the genus Punargentus (Nymphalidae, Satyrinae, Satyrini, Pronophilina) with the description of two new species and two new subspecies

<p>Two new species and two new subspecies of the satyrine butterfly genus&nbsp;<em>Punargentus&nbsp;</em>Heimlich &ndash;&nbsp;<em>P. atusparia&nbsp;</em>n. sp.,&nbsp;<em>P. heimlichi&nbsp;</em>n. sp.,&nbsp;<em>P. blanchardi libertas&nbsp;</em>n. ssp. and<em>&nbsp;P. atusparia yupania&nbsp;</em>n. ssp.<em>&nbsp;</em>&ndash; are described from north-central Peru (&Aacute;ncash, Hu&aacute;nuco and La Libertad). The affinities of the new taxa are evaluated based on molecular data obtained by target enrichment and COI barcoding.&nbsp;<em>Punargentus&nbsp;</em>is fully supported and divides into two branches,&nbsp;<em>P. lamna&nbsp;</em>clade with four species, and&nbsp;<em>P. blanchardi&nbsp;</em>clade with three species, two of which described here. The species of the&nbsp;<em>P. blanchardi&nbsp;</em>clade occur in Andean shrubland, at 2800-3600 m, whereas those of&nbsp;<em>P. lamna&nbsp;</em>clade are found in puna grassland at 3600-4600 m, with occasional overlapping. Considered their habitat preference, none of the newly described species requires immediate conservation measures.</p>

opencc-by-4.0Aug 2023View details →
dryad36/100

Areas of low natural regeneration potential post-fire in shrublands of southern California (selected years between 2008 and 2020)

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publicJan 2023View details →
dryad36/100

Shrubland vegetation topographic facets of Southern California

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publicJun 2021View details →
dryad36/100

Data from: Links between plant and fungal diversity in habitat fragments of coastal shrubland

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publicSep 2018View details →
dryad36/100

Data for: Extreme drought impacts have been underestimated in grasslands and shrublands globally

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publicNov 2025View details →
dryad36/100

Dataset on foraging ecology of shrubland bird community

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publicJun 2022View details →
dryad36/100

Data from: Competition suppresses shrubs during early, but not late, stages of arid grassland-shrubland state transition

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publicApr 2020View details →
dryad36/100

Can at-risk species serve as effective conservation surrogates? Case study in northeastern US shrublands

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publicFeb 2022View details →
dryad36/100

Data from: Climatic resilience after extreme drought in Mediterranean shrubland plant communities

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publicJun 2025View details →
dryad36/100

Data from: The importance of shrubland and local agroecological practices for pumpkin production in sub-Saharan smallholdings

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publicNov 2023View details →
dryad36/100

Episodic occurrence of favorable weather constrains recovery of a cold desert shrubland after fire

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publicMay 2021View details →
dryad36/100

The grass-layer (BGB) and shrub-layer (BGB) data across the northeast Tibetan Plateau shrublands

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publicJul 2025View details →
dryad36/100

Reduce revenue vs. increase expenditure: Fires and plant invasion drive soil carbon loss with different mechanisms in a Mediterranean shrubland

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publicJul 2025View details →
dryad36/100

Wildfire and extreme rainfall reduce soil carbon and nitrogen pools in a semiarid shrubland ecosystem

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publicDec 2025View details →
edi36/100

Phosphorus Fractions in Grassland and Shrubland Soils at the Sevilleta National Wildlife Refuge, New Mexico (1989)

This study examined concentrations of organic and inorganic phosphorus in surface soils of a Bouteloua gracilis-Bouteloua eriopoda grassland and a Larrea tridentata shrubland in the northern Chihuahuan Desert, New Mexico, USA. In this desert, where grassland vegetation has a uniform spatial distribution and individual shrubs have a patchy distribution, vegetation strongly influences the locations and concentrations of soil nutrients. Most studies of soil phosphorus (P) fractions in desert soils have focused on inorganic P fractions and have demonstrated the importance of geochemical controls on soil P cycling. This study addressed whether organic phosphorus, determined by the presence of different vegetation types, also contributes to soil P cycling. Within soils of similar age, topography, parent material, and climatic regime, samples were collected under and between vegetation and analyzed for P fractions following a modified sequential fractionation scheme.

openOpenJan 2020View details →
edi36/100

Soil Nutrient Distributions in Chihuahuan Desert Grasslands and Shrublands at the Sevilleta National Wildlife Refuge, New Mexico (1989)

Vegetation throughout the southwestern United States has changed from perennial grassland to woody shrubland over the past century. Previous studies on the development of 'islands of fertility' focused primarily on only the most limiting, plant-essential element, soil nitrogen (N). The research presented here addressed the question of whether other plant-essential elements, namely phosphorus (P) and potassium (K), showed similar concentration gradients under the desert shrub Larrea tridentata (creosotebush). It also examined whether the spatial distribution of N, P, and K differed from that of essential, but non-limiting nutrients, namely calcium (Ca), magnesium (Mg), and sulfur (S), and non-essential elements, namely sodium (Na), chloride (Cl), and fluoride (F). Within adjacent grassland and shrubland plots, surface soils were collected under and between vegetation and analyzed for a suite of soil nutrients. Soil nutrient distribution followed a uniform pattern that mirrored the spatial homogeneity of bunchgrasses in the grassland, but followed a patchy distribution that mirrored the spatial heterogeneity of individual shrubs in the shrubland. The main differences were that in the grassland, all elements were uniformly distributed, but in the shrubland the plant-essential elements, nitrogen, phosphorus, and potassium, were concentrated under the shrub canopy, and the non-limiting and non-essential elements were either concentrated in the intershrub spaces or were equally concentrated under shrubs and in the interspaces. Our results show how vegetation shifts from grassland to shrubland contribute to long-term, widespread change in the structure and function of desert ecosystems.

openOpenJan 2020View details →
edi36/100

15N Tracer Study in Grassland and Shrubland at the Sevilleta National Wildlife Refuge, New Mexico (1989-2002)

Because grasses and shrubs may induce different spatial distributions of nutrients in desert soils, this study was initiated to examine the redistribution of nitrogen in grassland and shrubland soils over a long time period. The stable isotope N15 was applied to plots in grassland and shrubland, and the plots were measured annually from 1989-1993 and again in 1999, 2001, and 2002.

openOpenSep 2010View details →
edi36/100

Bird Community Assessment in Grassland, Shrubland, and Woodland Habitats at the Sevilleta National Wildlife Refuge, New Mexico (1991-1997)

This project was designed to sample the richness and abundance of birds on the Sevilleta National Wildlife Refuge. Three types of habitat were surveyed: grassland, creosote shrubland and pinyon-juniper woodland.

openOpenSep 2010View details →
edi36/100

Small Mammal Exclosure Study (SMES) Rabbit Feces Data from Chihuahuan Desert Grassland and Shrubland at the Sevilleta National Wildlife Refuge, New Mexico (1995-2005)

The purpose of this study is to determine whether or not the activities of small mammals regulate plant community structure, plant species diversity, and spatial vegetation patterns in Chihuahuan Desert shrublands and grasslands. What role if any do indigenous small mammal consumers have in maintaining desertified landscapes in the Chihuahuan Desert? Additionally, how do the effects of small mammals interact with changing climate to affect vegetation patterns over time? This is data for numbers rabbit fecal pellets counted on each of the Small Mammal Exclosure Study (SMES) plots. Rabbit fecal pellets were counted from each of the 36 one-meter2 quadrats twice each year when vegetation was measured.

openOpenMar 2016View details →
dryad32/100

Data from: Differential impacts of nitrogen addition on rhizosphere and bulk-soil carbon sequestration in an alpine shrubland

<p><span><span>1. Due to complex root-soil interactions, the responses of carbon (C) dynamics in the rhizosphere to elevated nitrogen (N) deposition may be different from those in bulk soil. However, the potentially different response of C dynamics in the rhizosphere and bulk soils and their contributions to soil C sequestration under N deposition is still not elucidated.</span></span></p> <p><span><span>2. We conducted an N addition experiment in an alpine shrubland dominated by <i>Sibiraea angustata</i> located on the eastern Qinghai-Tibet Plateau (QTP). We measured the soil organic C (SOC) contents and density fractions in the rhizosphere and bulk soils in the top 15 cm of mineral soil and then employed a numerical model based on the rhizosphere extent to evaluate how the rhizosphere modulates soil C sequestration under N addition. We also measured the microbial gene abundance and C-acquisition enzyme activities to assess microbial community responses to N addition.</span></span></p> <p><span><span>3. The results showed that nitrogen addition had opposite effects on the rhizosphere and bulk-soil C stocks. Specifically, N addition decreased the rhizosphere SOC content through increasing bacterial abundance, β-glucosidase activity, and thus accelerating the loss of free light fraction C (FLF-C). However, N addition increased the bulk-soil C content, which was corresponding with the reduced oxidase activities and the accelerated accumulation of heavy fraction C (HF-C) under N addition. Numerical model analysis showed that the decrease induced by N addition in rhizosphere SOC stock ranged from 0.11 to 3.01 kg C m<sup>-2</sup> as root exudation diffusion distance extended from 0.5 mm to 2 mm, while the corresponding increase in the bulk-soil C stock ranged from 1.91 to 4.08 kg C m<sup>-2</sup>. By synthesizing the dynamics of the SOC stocks in these two soil compartments under N addition, the SOC stock at the ecosystem level exhibited an increase in range of 0.73-2.44 kg C m<sup>-2</sup>.</span></span></p> <p><span><span>4. <i>Synthesis</i> Our results suggest that alpine shrublands on the eastern QTP have great potential for soil C sequestration under N deposition, and the magnitude of the sequestration would depend closely on the responses of rhizosphere microbial C processes and the rhizosphere extent. Our results highlight the importance of integrating rhizosphere processes into land surface models to accurately predict ecosystem functions in the background of elevated N deposition.</span></span></p>

opencc-zeroJul 2020View details →

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Allen Brain Atlas

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Last verified 2026-04-30Open record

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DANDI Archive for NWB datasets

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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.

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Last verified 2026-04-29Open record

OpenNeuro

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openneuro
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Last verified 2026-04-29Open record