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473 results for “Soil temperatures”

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dryad32/100

Data from: Disentangling effects of air and soil temperature on C allocation in cold environments: a 14C pulse labelling study with two plant species

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publicMay 2019View details →
dryad32/100

Data from: Interactive effects of soil moisture, air temperature and litter nutrient diversity on soil microbial communities and Folsomia candida population

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publicApr 2024View details →
dryad32/100

Wetting‐induced soil CO2 emission pulses are driven by interactions among soil temperature, carbon, and nitrogen limitation in the Colorado Desert

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publicJul 2023View details →
dryad32/100

Data from: Water-conscious management strategies reduce per-yield irrigation and soil emissions of CO2, N2O, and NO in high-temperature forage cropping systems.

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publicJul 2023View details →
edi32/100

Hog Island Chronosequence Soil Eh, pH and Temperature 1991-1992

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openCustomDec 1997View details →
edi32/100

Temperature and Humidity at Soil Surface on Barro Colorado Island - OPEN 1

Patterns of biodiversity, such as the increase toward the tropics and the peaked curve during ecological succession, are fundamental phenomena for ecology. Such patterns have multiple, interacting causes, but temperature emerges as a dominant factor across organisms from microbes to trees and mammals, and across terrestrial, marine, and freshwater environments. However, there is little consensus on the underlying mechanisms, even as global temperatures increase and the need to predict their effects becomes more pressing. The purpose of this project is to generate and test theory for how temperature impacts biodiversity through its effect on biochemical processes and metabolic rate. A combination of standardized surveys in the field and controlled experiments in the field and laboratory measure diversity of three taxa -- trees, invertebrates, and microbes -- and key biogeochemical processes of decomposition in seven forests distributed along a geographic gradient of increasing temperature from cold temperate to warm tropical. This data is from a temperature humidity logger placed near the center of the Barro Colorado site macroplots array as part of a macrosystems biodiversity and latitude project supported by the National Science Foundation under Cooperative Agreement DEB#1065836. This data is associated with the project bento bags, but may be used as measures of the soil surface temperature for the dates represented.

openCustomDec 2013View details →
edi32/100

Macrosystems Soil Temperature and Soil Moisture at NWT, CWT, HFR, HJA, LUQ, and BCI - 2011-2013

Patterns of biodiversity, such as the increase toward the tropics and the peaked curve during ecological succession, are fundamental phenomena for ecology. Such patterns have multiple, interacting causes, but temperature emerges as a dominant factor across organisms from microbes to trees and mammals, and across terrestrial, marine, and freshwater environments. However, there is little consensus on the underlying mechanisms, even as global temperatures increase and the need to predict their effects becomes more pressing. The purpose of this project is to generate and test theory for how temperature impacts biodiversity through its effect on biochemical processes and metabolic rate. A combination of standardized surveys in the field and controlled experiments in the field and laboratory measure diversity of three taxa -- trees, invertebrates, and microbes -- and key biogeochemical processes of decomposition in seven forests distributed along a geographic gradient of increasing temperature from cold temperate to warm tropical. Readings of soil temperature and soil moisture were taken from all five Gentry tree plots at each of the six macrosystems project experimental sites (HJ Andrews, Coweeta, Harvard Forest, Luquillo, Niwot Ridge, and Barro Colorado Island), recorded by a HOBO device installed by the Enquist Lab (University of Arizona) as part of this macrosystems biodiversity and latitude project supported by the National Science Foundation under Cooperative Agreement DEB#1065836.

openCustomDec 2013View details →
edi32/100

Temperature and Humidity at Soil Surface on Barro Colorado Island - OPEN 2

Patterns of biodiversity, such as the increase toward the tropics and the peaked curve during ecological succession, are fundamental phenomena for ecology. Such patterns have multiple, interacting causes, but temperature emerges as a dominant factor across organisms from microbes to trees and mammals, and across terrestrial, marine, and freshwater environments. However, there is little consensus on the underlying mechanisms, even as global temperatures increase and the need to predict their effects becomes more pressing. The purpose of this project is to generate and test theory for how temperature impacts biodiversity through its effect on biochemical processes and metabolic rate. A combination of standardized surveys in the field and controlled experiments in the field and laboratory measure diversity of three taxa -- trees, invertebrates, and microbes -- and key biogeochemical processes of decomposition in seven forests distributed along a geographic gradient of increasing temperature from cold temperate to warm tropical. This data is from a temperature humidity logger placed near the center of the Barro Colorado site macroplots array as part of a macrosystems biodiversity and latitude project supported by the National Science Foundation under Cooperative Agreement DEB#1065836. This data is associated with the project bento bags, but may be used as measures of the soil surface temperature for the dates represented.

openCustomNov 2014View details →
edi32/100

Temperature and Humidity at Soil Surface on Barro Colorado Island - CLOSED 1

Patterns of biodiversity, such as the increase toward the tropics and the peaked curve during ecological succession, are fundamental phenomena for ecology. Such patterns have multiple, interacting causes, but temperature emerges as a dominant factor across organisms from microbes to trees and mammals, and across terrestrial, marine, and freshwater environments. However, there is little consensus on the underlying mechanisms, even as global temperatures increase and the need to predict their effects becomes more pressing. The purpose of this project is to generate and test theory for how temperature impacts biodiversity through its effect on biochemical processes and metabolic rate. A combination of standardized surveys in the field and controlled experiments in the field and laboratory measure diversity of three taxa -- trees, invertebrates, and microbes -- and key biogeochemical processes of decomposition in seven forests distributed along a geographic gradient of increasing temperature from cold temperate to warm tropical. This data is from a temperature humidity logger placed near the center of the Barro Colorado site macroplots array as part of a macrosystems biodiversity and latitude project supported by the National Science Foundation under Cooperative Agreement DEB#1065836. This data is associated with the project bento bags, but may be used as measures of the soil surface temperature for the dates represented.

openCustomNov 2014View details →
edi32/100

Temperature and Humidity at Soil Surface on Barro Colorado Island - CLOSED 2

Patterns of biodiversity, such as the increase toward the tropics and the peaked curve during ecological succession, are fundamental phenomena for ecology. Such patterns have multiple, interacting causes, but temperature emerges as a dominant factor across organisms from microbes to trees and mammals, and across terrestrial, marine, and freshwater environments. However, there is little consensus on the underlying mechanisms, even as global temperatures increase and the need to predict their effects becomes more pressing. The purpose of this project is to generate and test theory for how temperature impacts biodiversity through its effect on biochemical processes and metabolic rate. A combination of standardized surveys in the field and controlled experiments in the field and laboratory measure diversity of three taxa -- trees, invertebrates, and microbes -- and key biogeochemical processes of decomposition in seven forests distributed along a geographic gradient of increasing temperature from cold temperate to warm tropical. This data is from a temperature humidity logger placed near the center of the Barro Colorado site macroplots array as part of a macrosystems biodiversity and latitude project supported by the National Science Foundation under Cooperative Agreement DEB#1065836. This data is associated with the project bento bags, but may be used as measures of the soil surface temperature for the dates represented.

openCustomNov 2014View details →
zenodo28/100

In situ temperature and brGDGTs measurements in soils from the Tropical Andes of Colombia and a tropical soil brGDGT compilation dataset

<p>This dataset contain:</p> <p>Table S1. Air and soil mean monthly temperatures from the new 16 sites in the Eastern Cordillera of Colombia with data presented in this study.<br> Table S3. Soil Branched glycerol dialkyl glycerol tetraethers (brGDGTs) from&nbsp;the Eastern Cordillera of Colombia and data compilation from the tropics.<br> Table S4.&nbsp;nonlinear brGDGTs predictors for the tropical compilation data.</p> <p>&nbsp;</p>

opencc-by-4.0Jul 2020View details →
dryad28/100

Data from: Increased soil temperature and decreased precipitation during early plant life stages constrain grass seedling recruitment in cold desert restoration

1. Seed-based restoration is one of the most difficult challenges for dryland restoration. Identifying environmental conditions that drive variation in seed and seedling mortality across similar restoration efforts could increase understanding of when and where restoration outcomes are likely to be favorable and identify new tools and strategies to improve outcomes. 2. We asked how variation in a suite of environmental predictors influenced germination, emergence, seedling establishment, and juvenile survival of four commonly sown perennial grass species across 33 seeding experiments distributed over a ~160,000-km2 area of the Great Basin, a cold desert system in the western United States. 3. Across experiments, we observed wide variation in the rates of four demographic transitions and wide variation in environmental conditions experienced by plants at each stage. For all species, higher precipitation during the first 30 days following seeding was associated with an increase in germination. Conversely, higher soil temperature over this same time period was associated with a significant decrease in germination and emergence and soil temperature was associated with a substantial portion of the variation in germination and emergence probabilities observed across our seeding experiments. 4. Within the range of precipitation variation observed, we were unable to detect a significant relationship between seedling establishment the first growing season and cumulative precipitation the first year, precipitation during the first spring growing season, or annual climatic water deficit (CWD) the first year. Higher CWD the second growing season reduced seedling survival over that time period. 5. Synthesis and application. Our results show higher soil temperature negatively impacts grass seedling recruitment. Our results can be combined with seasonal and subseasonal temperature forecasts to improve restoration decision-making. These results also suggest climate warming will make restoration even more difficult, with our model estimates suggesting the 2°C increase in temperature expected in the Great Basin over the coming decades will decease germination and emergence by about 30%. Lastly, while our field-based approach provided insight into short-term drivers of mortality, it did not provide insight into drivers of longer-term survival, suggesting a need to develop process-based approaches for predicting long-term restoration outcomes.29-Aug-2019

opencc-zeroSep 2020View details →
zenodo28/100

Dataset for: Short-term temperature history affects mineralization of fresh litter and extant soil organic matter, irrespective of agricultural management

<p>Dataset for the article:</p> <p>Mason-Jones, K., Vrehen, P, Koper, K., Wang, J., van der Putten, W.H., Veen, G.F. 2020. Short-term temperature history affects mineralization of fresh litter and extant soil organic matter, irrespective of agricultural management. Soil Biology and Biochemistry, 150, 107985.</p> <p>Article DOI: 10.1016/j.soilbio.2020.107985</p>

opencc-by-4.0Dec 2019View details →
dryad28/100

Multiscale legacy responses of soil gas concentrations to soil moisture and temperature fluctuations

<p>The sensitivity of soil carbon dynamics to climate change is a major uncertainty in carbon cycle models. Of particular interest is the response of soil biogeochemical cycles to variability in hydroclimatic states and the related quantification of soil memory. Toward this goal, the power spectra of soil hydrologic and biogeochemical states were analyzed using measurements of soil temperature, moisture, oxygen, and carbon dioxide at two sites. Power spectra indicated multiscale power law scaling across sub-hourly to annual timescales. Precipitation fluctuations were most strongly expressed in the soil biogeochemical signals at monthly to annual timescales. Soil moisture and temperature fluctuations were comparable in strength at one site, while temperature was dominant at the other. The effect of soil hydrologic, thermal, and biogeochemical processes on gas concentration variability was evidenced by low spectral entropy relative to the white noise character of precipitation. A full mass balance model was unable to capture high-frequency soil temperature influence, indicating a gap in commonly used model assumptions. A linearized model was shown to capture the main features of the observed and modeled gas concentration spectra and demonstrated how the means and variances of soil moisture and temperature interact to produce the gas concentration spectra. Breakpoints in the spectra corresponded to the mean rate of gas efflux, providing a first-order estimate of the soil biogeochemical integral timescale ($\sim 1$ minute). These methods can be used to identify biogeochemical system dynamics to develop robust, process-based soil biogeochemistry models that capture variability in addition to long-term mean values.</p>

opencc-zeroDec 2020View details →
zenodo28/100

Effect of earth-air and temperature variation on the concentration of CO2 in the soil in extremely arid regions

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opencc-by-4.0Jun 2024View details →
zenodo28/100

Fig. 2. Soil temperature changes from July 2003 in Trigonopeltastes delta (Coleoptera: Scarabaeidae: Cetoniinae) Larva Developing in a Bromeliad Terrarium

Fig. 2. Soil temperature changes from July 2003 to June 2004 at Wuhan, P. R. China.

opennotspecifiedDec 2005View details →
zenodo28/100

Fig. 2. Soil temperature changes from July 2003 in The Morphology and Temperature-dependent Development of Mylabris phalerata Pallas (Coleoptera: Meloidae)

Fig. 2. Soil temperature changes from July 2003 to June 2004 at Wuhan, P. R. China.

opennotspecifiedDec 2005View details →
zenodo28/100

Database for the article "Acclimation of fine root systems to soil warming: comparison of an experimental setup and a natural soil temperature gradient", published in Ecosystems

<p>The database contains measurements of fine root biomass, absorptive fine root biomass, absorptive root morphology (diameter, specific root length, specific root area, root tissue density, root tip length, root tip weight and branching per length and weight) and identifications and sequences of root-colonizing ectomycorrhizal fungi.</p>

opencc-by-nc-4.0Dec 2017View details →
dryad28/100

Tree identity and diversity directly affect soil moisture and temperature but not soil carbon ten years after planting

<p>1. Soil C is the largest C pool in forest ecosystems that contributes to C sequestration and mitigates climate change. Tree diversity enhances forest productivity, so diversifying the tree species composition, notably in managed forests, could increase the quantity of organic matter being transferred to soils, and alter other soil properties relevant to the C cycle.</p> <p>2. A ten-year-old tree diversity experiment was used to study the effects of tree identity and diversity (functional and taxonomic) on soils. Surface (0-10 cm) mineral soil was repeatedly measured for soil C concentration, C:N ratio, pH, moisture and temperature in twenty-four tree species mixtures and twelve corresponding monocultures (replicated in four blocks).</p> <p>3. Soil pH, moisture and temperature responded to tree diversity and identity. Greater productivity in above- and below-ground tree components did not increase soil C concentration. Soil pH increased and soil moisture decreased with functional diversity, more specifically, when species had different growth strategies and shade tolerances. Functional identity affected soil moisture and temperature, such that tree communities with more slow-growing and shade-tolerant species had greater soil moisture and temperature. Higher temperature was measured in communities with broadleaf-deciduous species compared to communities with coniferous-evergreen species.</p> <p>4. We conclude that long-term soil C cycling in forest plantations will likely respond to changes in soil pH, moisture and temperature that is mediated by tree species composition, since tree species affect these soil properties through their litter quality, water uptake and physical control of soil microclimates.</p>

opencc-zeroJan 2023View details →
dryad28/100

Data from: Increased soil temperature and decreased precipitation during early life stages constrain grass seedling recruitment in cold desert restoration

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publicOct 2019View details →

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