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37 results for “thermal gradient”

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dryad32/100

Data from: Hindered and constrained: limited potential for thermal adaptation in post-metamorphic and adult Rana temporaria along elevational gradients

Adaptation to warming climates could counteract the effects of global warming. Thus, understanding how species cope with contrasting climates may inform us about their potential for thermal adaptation and which processes may hamper that ability (e.g. evolutionary trade-offs, phenology, or behavioural thermoregulation). In addition to temperature, time constraints may also exert important selective pressures. Here we compare the thermal sensitivity of locomotion of metamorphic and adult European common frogs (Rana temporaria) originating from populations along an elevational gradient. We employed the template mode of variation (TMV) analysis to decompose the thermal sensitivity of locomotion and explore the existence of trade-offs ('hotter is better' and 'specialist-generalist') and the degree of local adaptation. To that end, we studied the relationship between TMV parameters and local environmental conditions. Further, we compared preferred temperatures to assess whether behavioral thermoregulation could dampen the effects of thermal variation, reducing the intensity of selection and limiting thermal adaptation (i.e. 'Bogert effect'). We suggest that behavioral thermoregulation has promoted the conservatism of thermal sensitivity in R. temporaria. Yet, we observed a trend towards narrower thermal niches shifted towards warmer temperature in populations with severe temporal constraints, conforming to the 'generalist-specialist' trade-off. Apparently, this enables time-constrained populations – especially in the case of metamorphs – to effectively exploit resources during the warmest periods. The limited potential of R. temporaria for thermal adaptation suggests that forecasts of global warming should incorporate thermoregulation and explore its potential to buffer species from rising temperatures.

opencc-zeroDec 2017View details →
dryad32/100

Data from: Hindered and constrained: limited potential for thermal adaptation in post-metamorphic and adult Rana temporaria along elevational gradients

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publicSep 2018View details →
dryad32/100

Data from: Variation in thermal niche of a declining river-breeding frog: from counter-gradient responses to population distribution patterns

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publicApr 2018View details →
dryad32/100

Data from: Nonlinear thermal gradients shape broad-scale patterns in geographic range size and can reverse Rapoport’s rule

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publicAug 2015View details →
dryad32/100

Data from: Adaptation to a latitudinal thermal gradient within a widespread copepod species: the contributions of genetic divergence and phenotypic plasticity

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publicMar 2017View details →
dryad32/100

Thermal performance curves dataset based on <em>Littorina littorea</em> from different locations along a latitudinal gradient: Physiological and life history traits

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publicDec 2025View details →
dryad32/100

Data from: Thermal regime drives a latitudinal gradient in morphology and life history in a livebearing fish

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publicJul 2018View details →
dryad32/100

Data from: Variation in thermal biology of three closely related lizard species across an elevation gradient

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publicMar 2019View details →
dryad32/100

Data from: Consumer trait responses track change in resource supply along replicated thermal gradients

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publicDec 2021View details →
dryad28/100

Thermal tolerance of Lasius americanus across urbanization and geographical gradients

<p class="CxSpFirst"><span>Cities are emerging as a new venue to overcome the challenges of obtaining data on compensatory responses to climatic warming through phenotypic plasticity and evolutionary change. In this review, we highlight how cities can be used to explore physiological trait responses to experimental warming and also how cities can be used as human-made space-for-time substitutions. We synthesized the current literature and found evidence for significant plasticity and evolution in thermal tolerance trait responses to urban heat islands. For those studies that reported both plastic and evolved components of thermal tolerance, we found evidence that both mechanisms contributed to phenotypic shifts in thermal tolerance, rather than plastic responses precluding or limiting evolved responses. Interestingly though, for a broader range of studies, we found that the magnitude of evolved shifts in thermal tolerance was not significantly different from the magnitude of shift in those studies that only reported phenotypic results, which could be a product of evolution, plasticity, or both. Regardless, the magnitude of shifts in urban thermal tolerance phenotypes was comparable to more traditional space-for-time substitutions across latitudinal and altitudinal clines in environmental temperature. We conclude by considering how urban-derived estimates of plasticity and evolution of thermal tolerance traits can be used to improve forecasting methods including macrophysiological models and species distribution modelling approaches. Finally, we consider areas for further exploration including sub-lethal performance traits and thermal performance curves, assessing the adaptive nature of trait shifts, and taking more full advantage of the environmental thermal variation that cities generate.</span></p>

opencc-zeroNov 2020View details →
zenodo28/100

Data and Drawing Project for [A Method for Nonlinear Electric-thermal Coupling Calculations of Bushings Based on Unbiased Gradient-free Smooth Domains]

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opencc-by-4.0Apr 2024View details →
dryad28/100

Data from: Divergence of thermal physiological traits in terrestrial breeding frogs along a tropical elevational gradient

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publicMar 2018View details →
dryad28/100

Phenotypic plasticity can reverse the relative extent of intra and interspecific variability across a thermal gradient

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publicJun 2021View details →
dryad28/100

Thermal tolerance of Lasius americanus across urbanization and geographical gradients

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publicDec 2020View details →
zenodo12/100

Soil thermal gradient at Solfatara during 2020-2021 (Campi Flegrei, south Italy)

<p>The monitoring of energy fluxes associated with diffuse degassing may bean important tool in the surveillance of volcanic activity. In a purely conductive regime, the heat flux is a linear function of the soil thermal gradient with a slope proportional to the thermal conductivity of the medium.</p> <p>For that reason, soil temperatures were continuously measured during two years (2020 and 2021) within the crater of Solfatara using an automatic station. The station was equipped with a Gigalog mod.F data logger that acquires, at 1-hour time intervals, the soil temperature along a vertical profile&nbsp;at 0.1, 0.2, 0.3 and 0.4 m depth,&nbsp;</p> <p>The measurements, expressed in degrees centrigade, made with n.4 Resistance Temperature Detector &quot;RTD&quot; PT100 in platinum class B with a tolerance of &plusmn;0.3 &deg;C at 0&deg;C.</p> <p>The coordinates of the instrument are 33T 427461.48m E 4520150.14m N</p>

restrictedApr 2022View details →
zenodo12/100

Soil thermal gradient at Solfatara during 2018-2019 (Campi Flegrei, south Italy)

<p>The monitoring of energy fluxes associated with diffuse degassing may bean important tool in the surveillance of volcanic activity. In a purely conductive regime, the heat flux is a linear function of the soil thermal gradient with a slope proportional to the thermal conductivity of the medium.</p> <p>For that reason, soil temperatures were continuously measured during two years (2018 and 2019) within the crater of Solfatara using an automatic station. The station was equipped with a Gigalog mod.F data logger that acquires, at 1-hour time intervals, the soil temperature along a vertical profile&nbsp;at 0.1, 0.2, 0.3 and 0.4 m depth,&nbsp;</p> <p>The measurements, expressed in degrees centrigade, made with n.4 Resistance Temperature Detector &quot;RTD&quot; PT100 in platinum class B with a tolerance of &plusmn;0.3 &deg;C at 0&deg;C.</p> <p>The coordinates of the instrument are 33T 427461.48m E 4520150.14m N</p>

restrictedApr 2022View details →
zenodo12/100

Soil thermal gradient at Solfatara during 2016-2017 (Campi Flegrei, south Italy)

<p>The monitoring of energy fluxes associated with diffuse degassing may bean important tool in the surveillance of volcanic activity. In a purely conductive regime, the heat flux is a linear function of the soil thermal gradient with a slope proportional to the thermal conductivity of the medium.</p> <p>For that reason, soil temperatures were continuously measured during two years (january 2016 to january 2018) within the crater of Solfatara using an automatic station. The station was equipped with a Gigalog mod.F data logger that acquires, at 1-hour time intervals, the soil temperature along a vertical profile&nbsp;at 0.1, 0.2, 0.3 and 0.4 m depth,&nbsp;</p> <p>The measurements, expressed in degrees centrigade, made with n.4 Resistance Temperature Detector &quot;RTD&quot; PT100 in platinum class B with a tolerance of &plusmn;0.3 &deg;C at 0&deg;C.</p> <p>The coordinates of the instrument are 33T 427461.48m E 4520150.14m N<br> &nbsp;</p>

restrictedApr 2022View details →

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