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Evidence of current impact of climate change on life: a walk from genes to the biosphere

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TLDR
The evidence of how organisms and populations are currently responding to climate change through phenotypic plasticity, genotypic evolution, changes in distribution and, in some cases, local extinction is reviewed.
Abstract
We review the evidence of how organisms and populations are currently responding to climate change through phenotypic plasticity, genotypic evolution, changes in distribution and, in some cases, local extinction. Organisms alter their gene expression and metabolism to increase the concentrations of several antistress compounds and to change their physiology, phenology, growth and reproduction in response to climate change. Rapid adaptation and microevolution occur at the population level. Together with these phenotypic and genotypic adaptations, the movement of organisms and the turnover of populations can lead to migration toward habitats with better conditions unless hindered by barriers. Both migration and local extinction of populations have occurred. However, many unknowns for all these processes remain. The roles of phenotypic plasticity and genotypic evolution and their possible trade-offs and links with population structure warrant further research. The application of omic techniques to ecological studies will greatly favor this research. It remains poorly understood how climate change will result in asymmetrical responses of species and how it will interact with other increasing global impacts, such as N eutrophication, changes in environmental N : P ratios and species invasion, among many others. The biogeochemical and biophysical feedbacks on climate of all these changes in vegetation are also poorly understood. We here review the evidence of responses to climate change and discuss the perspectives for increasing our knowledge of the interactions between climate change and life.

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Truncation of thermal tolerance niches among Australian plants

TL;DR: A widespread disparity between realized and potential thermal limits may have significant implications for species' capacity to persist in situ with a changing climate and may potentially improve the reliability of model projections under climate change.
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The interaction between drought and elevated CO2 in water relations in two grassland species is species-specific.

TL;DR: Elevated CO2 partially mitigated the negative impact of drought on turgor potential in Trifolium pratense through a higher osmotic adjustment and root to shoot ratio and in Agrostis capillaris through aHigher leaf relative water content caused by higher hydraulic conductance, but the impact ofrought was not mitigated in either species by higher soil water conservation.
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Exploring interactive effects of climate change and exotic pathogens on Quercus suber performance: Damage caused by Phytophthora cinnamomi varies across contrasting scenarios of soil moisture

TL;DR: The results suggest that an average drier climate might imply sub-optimal conditions for P. cinnamomi infections allowing for a slower advance of the disease in invaded areas, but this effect will be modulated by the also predicted more frequent extreme climatic events.
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Asymmetric warming significantly affects net primary production, but not ecosystem carbon balances of forest and grassland ecosystems in northern China

TL;DR: Analysis of covariance shows that NPP is significant greater at most ecosystems under the various environmental change scenarios once temperature asymmetries are taken into consideration, which indicates that asymmetry in climate change does not result in significant alterations of the overall carbon balance in the dominating forest or grassland ecosystems.
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Thermal Characterization of European Ant Communities Along Thermal Gradients and Its Implications for Community Resilience to Temperature Variability

TL;DR: In this paper, the authors characterized the thermal niches of 147 ant species from 342 communities found along broad temperature gradients in western Europe and found that community thermal resilience was negatively and positively correlated with mean temperature and temperature seasonality, respectively.
References
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Climate change 2007: the physical science basis

TL;DR: The first volume of the IPCC's Fourth Assessment Report as mentioned in this paper was published in 2007 and covers several topics including the extensive range of observations now available for the atmosphere and surface, changes in sea level, assesses the paleoclimatic perspective, climate change causes both natural and anthropogenic, and climate models for projections of global climate.
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A globally coherent fingerprint of climate change impacts across natural systems

TL;DR: A diagnostic fingerprint of temporal and spatial ‘sign-switching’ responses uniquely predicted by twentieth century climate trends is defined and generates ‘very high confidence’ (as laid down by the IPCC) that climate change is already affecting living systems.
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Climate change 2007: the physical science basis

TL;DR: In this article, Chen et al. present a survey of the state of the art in the field of computer vision and artificial intelligence, including a discussion of the role of the human brain in computer vision.

Climate and atmospheric history of the past 420,000 years from the Vostok ice core, Antarctica

TL;DR: The recent completion of drilling at Vostok station in East Antarctica has allowed the extension of the ice record of atmospheric composition and climate to the past four glacial-interglacial cycles.
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Trending Questions (2)
Disuss the impact of global climate change as a evidence today?

Organisms exhibit phenotypic plasticity, genotypic evolution, distribution shifts, and local extinctions in response to current climate change, highlighting its significant impact on life today.

What are the current scientific consensus and evidence on the existence and impact of climate change?

Current evidence shows organisms respond to climate change through phenotypic plasticity, genotypic evolution, distribution changes, and local extinction. However, uncertainties remain regarding asymmetrical species responses and interactions with other global impacts.