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Related Concept Videos

Microbes and Climate Change01:27

Microbes and Climate Change

Microorganisms are pivotal agents in Earth's biogeochemical cycles, significantly influencing climate dynamics through their metabolic activities. These microbes modulate the levels of key greenhouse gases by both contributing to and helping mitigate climate change.Microbial Contributions to Greenhouse Gas EmissionsRising global temperatures accelerate microbial metabolism, which, in turn, speeds up the decomposition of organic matter. This process releases carbon dioxide (CO₂) through...
Microbes and the Carbon Cycle01:24

Microbes and the Carbon Cycle

The carbon cycle is a fundamental Earth process involving the transfer of carbon among the biosphere, lithosphere, atmosphere, and hydrosphere. It plays a critical role in regulating the planet’s climate and supporting life by cycling carbon through various chemical forms and reservoirs. Carbon primarily circulates as carbon dioxide (CO₂), representing its oxidized form, while reduced forms such as methane (CH₄) and organic compounds also play essential roles.Microbial activity is central to...
Global Climate Change01:50

Global Climate Change

Throughout its ~4.5 billion year history, the Earth has experienced periods of warming and cooling. However, the current drastic increase in global temperatures is well outside of the Earth’s cyclic norms, and evidence for human-caused global climate change is compelling. Paleoclimatology, the study of ancient climate conditions, provides ample evidence for human-caused global climate change by comparing recent conditions with those in the past.
The Carbon Cycle01:14

The Carbon Cycle

Carbon is the basis of all organic matter on Earth, and is recycled through the ecosystem in two primary processes: one in which carbon is exchanged among living organisms, and one in which carbon is cycled over long periods of time through fossilized organic remains, weathering of rocks, and volcanic activity. Human activities, including increased agricultural practices and the burning of fossil fuels, has greatly affected the balance of the natural carbon cycle.
Microbes and the Sulfur Cycle01:29

Microbes and the Sulfur Cycle

Sulfur is a vital element in Earth's biogeochemical systems. It transitions through various inorganic states, including sulfate (SO₄²⁻), elemental sulfur (S⁰), and sulfide (S²⁻). Abiotic and biological mechanisms across oxic and anoxic environments intricately mediate these transformations. Sulfate, the most oxidized form of sulfur, is predominantly stored in rocks, marine sediments, and oceanic waters, acting as a long-term reservoir in the global sulfur cycle.In oxic environments,...
Microbes and Methanogenesis01:26

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Methanogenesis is a critical microbial process in anaerobic ecosystems responsible for the biological production of methane, a potent greenhouse gas and valuable biofuel. This metabolic pathway is primarily facilitated by methanogenic archaea, which thrive in anoxic environments such as wetlands, sediments, and animal gastrointestinal tracts. The absence of oxygen in these habitats prevents aerobic respiration, thereby favoring alternative biochemical pathways for organic matter degradation.In...

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Visualizing Methane-Cycling Microbial Dynamics in Coastal Wetlands
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Microbial contributions to climate change through carbon cycle feedbacks.

Richard D Bardgett1, Chris Freeman, Nicholas J Ostle

  • 1Soil and Ecosystem Ecology, Lancaster University, Lancaster, UK. r.bardgett@lancaster.ac.uk

The ISME Journal
|July 11, 2008
PubMed
Summary

Understanding soil microbes is key to predicting climate change impacts on carbon exchange. Research must consider direct and indirect climate effects on soil microorganisms and their interactions with plants and the environment.

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Area of Science:

  • Soil science
  • Microbial ecology
  • Climate change research

Background:

  • Terrestrial carbon cycle-climate feedbacks are crucial for understanding global warming.
  • Soil microbial communities play a central role in regulating land-atmosphere carbon exchange.
  • The complexity of soil microbial responses to climate change hinders definitive conclusions.

Purpose of the Study:

  • To emphasize the need for explicit consideration of direct and indirect climate change impacts on soil microbes.
  • To highlight the importance of interactions between microbes, plants, and the environment in climate change.
  • To identify challenges and the urgent need for research on soil microbial ecology and carbon cycle feedbacks.

Main Methods:

  • Review and synthesis of current understanding of soil microbial ecology and climate change.
  • Argument for a multifactor experimental approach.
  • Focus on direct and indirect impacts of climate change on microorganisms.

Main Results:

  • Soil microbial ecology is central to assessing terrestrial carbon cycle-climate feedbacks.
  • Climate change effects on soil microbes are complex, involving direct and indirect impacts.
  • Interactions between microbes, plants, and the environment amplify climate-driven effects.

Conclusions:

  • A comprehensive understanding of soil microbial ecology is urgently needed to predict land-atmosphere carbon exchange under climate change.
  • Multifactor experimental approaches are essential to unravel the responses of soil microbes to climate change.
  • Future research must address the complex interactions and feedbacks within soil ecosystems to accurately assess carbon cycle consequences.