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    Mountain Ecosystems as Natural Laboratories for Climate Change Experiments
    (Frontiers Media S.A., 2020-03-31)
    Experimental studies are needed to empirically examine the effects of climate change on terrestrial organisms and to serve as the basis for predictions and management practices. As such, designing and implementing experimental systems that can simulate complex changes in the natural environment is currently a major area of interest of climate change science. Most climate change experiments (e.g., infrared heaters, open-top chambers) are typically performed within small, controlled environments and often manipulate just temperature and/or CO2 concentration. Other factors are more difficult to control (e.g., wind speed, soil moisture) or are frequently ignored (e.g., biotic interactions), leading to uncertainties in the results and limiting our ability to make realistic predictions about species’ responses to future environmental changes. We examined the natural variation of abiotic and biotic factors along mountain elevational gradients in order to highlight the potential for using these systems as natural laboratories for climate change research and experiments. The high variability of different abiotic and biotic factors along elevational gradients provides a good opportunity to carry out field transplant/translocation experiments aimed at answering some critical questions, including: How will new biotic assemblages affect key interactions and processes? What are the factors that influence species assemblages under novel climates? How do local abiotic factors influence the establishment of species migrating into novel and climatically suitable habitats? Based on empirical evidence, we strongly encourage researchers to take advantage of the natural environmental gradients found in mountains to study the potential direct and indirect impacts of climate change on species, communities and biodiversity as a whole.
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    Carbon footprint, sustainability and anesthesia. We are beginning to learn
    (Sociedad de Anestesiologia de Chile, 2022-01-01)
    Human health has been negatively impacted by the difficult environmental conditions produced by climate change. The health industry, paradoxically, generates a carbon footprint (CF) that drives climate change and represents 9.8% of the greenhouse gas (GHG) emissions in the United States (2013) and 6.3% of CF in England (2017). A considerable portion of these emissions comes from the clinical practice of anesthesia. Anesthetic gases present global warming potentials (GWPs) of up to 3,714 times higher than CO 2 throughout their life cycles, from their manufacture and use to their disposal. In this context, this review compiled and assessed the environmental impacts of the anesthetic strategy in clinical practice, making use of the life cycle analysis tool. This review describes how the anesthetic technique has a major impact on CF, through the emission of GHG expressed through tools such as the GWP 100 . As an example, at the manufacturing stage, the GWP of halogenated gases is up to 2,540 kg CO 2 eq versus 21 kg CO 2 eq for Propofol. This and other variables determine the contribution of the anesthetic technique in the emission of GHG. Finally, this review aims to help health care providers make informed decisions when considering the CH and sustainability of each anesthetic technique.
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    5R and hospital sustainability: Our contribution in the climate emergency. Part II. Rethink and research
    (Sociedad de Anestesiologia de Chile, 2022-01-01)
    Introduction: Climate change is a health problem and, at the same time, health systems are important contributors. Hospitals stand out due to their high rates of energy consumption, resources and waste generation. The purpose of the study is to know and identify the determinants of sanitary waste and the measures that can be implemented that allow reducing the production of hospital waste, seeking to achieve a general and updated appreciation of this phenomenon and taking into account hospital sustainability. Method: A bibliographic search was carried out in pubmed that included keywords related to the concepts of carbon footprint, recycling and hospital waste. The screening yielded a total of 37 articles and later 12 publications founded from references (or that were previously known by the authors) were added. Results: The results are presented into 5 points known as the “5 Rs”, named below. “Reduce” (through adequate segregation of waste, correct management of effluents and energy, significant reduction of excesses and automatic administration of anesthetic gases), “Reuse” (through device reprocessing, reusable material and donation), “Recycle”, “Rethink” (with examples such as selection of less polluting gases, selective use of containers, staff education) and “Investigate” through different models. Discussion: Several of the recognized measures could have an application in many hospital areas despite the fact that most of the available evidence refers to the operating room. The organization and education of the personnel is important in order to implement the measures found.
      1
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    5R and hospital sustainability: Our contribution in the climate emergency. Part I. Reduce, reuse and recycle
    (Sociedad de Anestesiologia de Chile, 2022-01-01)
    Introduction: Climate change is a health problem and, at the same time, health systems are important contributors. Hospitals stand out due to their high rates of energy consumption, resources and waste generation. The purpose of the study is to know and identify the determinants of sanitary waste and the measures that can be implemented that allow reducing the production of hospital waste, seeking to achieve a general and updated appreciation of this phenomenon and taking into account hospital sustainability. Method: A bibliographic search was carried out in pubmed that included keywords related to the concepts of carbon footprint, recycling and hospital waste. The screening yielded a total of 37 articles and later 12 publications founded from references (or that were previously known by the authors) were added. Results: The results are presented into 5 points known as the “5 Rs”, named below. “Reduce” (through adequate segregation of waste, correct management of effluents and energy, significant reduction of excesses and automatic administration of anesthetic gases), “Reuse” (through device reprocessing, reusable material and donation), “Recycle”, “Rethink” (with examples such as selection of less polluting gases, selective use of containers, staff education) and “Investigate” through different models. Discussion: Several of the recognized measures could have an application in many hospital areas despite the fact that most of the available evidence refers to the operating room. The organization and education of the personnel is important in order to implement the measures found.
      1
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    Amazonian and Andean tree communities are not tracking current climate warming
    (EarthArXiv, 2024-12-18)
    Climate change is shifting species distributions, leading to changes in community composition and novel species assemblages worldwide. However, the responses of tropical forests to climate change across large-scale environmental gradients remain largely unexplored. Using long-term data over 66,000 trees of more than 2,500 species occurring over 3,500 m elevation along the hyperdiverse Amazon-to-Andes elevational gradient, we assessed community-level shifts in species composition through a 44-year time span. We tested for the predicted increase in relative abundances of species from warmer climates (thermophilization) along the Amazon-to-Andes elevational gradients in Peru and Bolivia. Additionally, we examined the relative contributions of tree mortality, recruitment, and growth to observed compositional changes. Mean thermophilization rates across the Amazon-to-Andes gradient were slow relative to concordant changes in regional temperatures. Thermophilization rates were positive and more variable among Andean forest plots compared to Amazonian plots but were fastest at mid-elevations around the cloud base. Across all elevations, thermophilization rates were driven primarily by tree mortality and decreased growth of highland species rather than an influx of lowland species with higher thermal optima. Given the high variability of community-level responses to warming along the elevational gradients and the generally slower-than-warming rates of compositional change, we conclude that most tropical tree species, and especially Amazonian tree species, will not be able to escape current or future climate change through upward range shifts.
      1
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    Amazonian and Andean tree communities are not tracking current climate warming
    (National Academy of Sciences, 2025)
    Climate change is shifting species distributions, leading to changes in community composition and novel species assemblages worldwide. However, the responses of tropical forests to climate change across large-scale environmental gradients remain largely unexplored. Using long-term data over 66,000 trees of more than 2,500 species occurring over 3,500 m elevation along the hyperdiverse Amazon-to-Andes elevational gradients in Peru and Bolivia, we assessed community-level shifts in species composition over a 40+ y time span. We tested the thermophilization hypothesis, which predicts an increase in the relative abundances of species from warmer climates through time. Additionally, we examined the relative contributions of tree mortality, recruitment, and growth to the observed compositional changes. Mean thermophilization rates (TR) across the Amazon-to-Andes gradient were slow relative to regional temperature change. TR were positive and more variable among Andean forest plots compared to Amazonian plots but were highest at midelevations around the cloud base. Across all elevations, TR were driven primarily by tree mortality and decreased growth of highland (cool-adapted) species rather than an influx of lowland species with higher thermal optima. Given the high variability of community-level responses to warming along the elevational gradients, the high tree mortality, and the slower-than-warming rates of compositional change, we conclude that most tropical tree species, and especially lowland Amazonian tree species, will not be able to escape current or future climate change through upward range shifts, causing fundamental changes to composition and function in Earth’s highest diversity forests.
      2
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    Microbial death in the Andes: necromass declines despite growth and carbon-use-efficiency increases with decadal soil warming
    (Elsevier, 2026)
    The growth and death of soil microbes are important drivers of soil carbon formation. A warming climate is predicted to affect both the production of microbial biomass and the stability of microbial residues (necromass) held in soils. However, we have very little information on how warming in tropical soils will affect these processes, and on the effect of temperature on microbial production and turnover over different time-scales. To address this, we studied temperature effects on microbial-mediated C cycling across two different time-scales, using a 20 ⁰C mean annual temperature gradient in the Peruvian Andes (long-term effects) and decadal experimental-warming via soil translocation (11-years of temperature effects). At long-term timescales, a legacy of warmer temperatures decreased microbial carbon use efficiency (CUE), microbial biomass C, and decreased fungal and bacterial necromass concentration in soils. At decadal timescales, experimental warming increased CUE, microbial production and microbial biomass concentration (likely the result of concomitant changes in substrate availability). However, this did not translate into increased microbial necromass concentration, which generally declined with warming across all temporal scales. Together, we show that warmer temperatures over decadal (11-year) timescales affect soil microbial processes to potentially increase their C input to soil (increased CUE, microbial production, and biomass) but we find no evidence that this C became stabilized as the necromass C pool decreased. Our results indicate that warming can alter microbial community metabolism to potentially increase necromass C inputs to soil, although we find no evidence to show that this offset overall soil C loss with warming.
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