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Related Concept Videos

Primary Production01:06

Primary Production

The total amount of energy acquired by primary producers in an ecosystem is called gross primary production (GPP). However, of this energy, producers use some for metabolic processes, and some is lost as heat, decreasing the amount of energy available to the next trophic level. The remaining usable amount of energy is called the net primary productivity (NPP). In terrestrial ecosystems, NPP is driven by climate, while light penetration and nutrient availability drive NPP in aquatic ecosystems.
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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...
Marine Microbial Ecology01:30

Marine Microbial Ecology

Marine microbial ecosystems are shaped by distinct physicochemical limits, including high salinity, low nutrient availability, and fluctuating oxygen levels. These conditions favor smaller microbial cell sizes, which maximize their surface-to-volume ratio for efficient nutrient uptake.Microbial activity and community composition are closely linked to biogeochemical cycles, particularly in dynamic environments like estuaries, where halotolerant microbes thrive in response to variable salinity...
Freshwater Microbial Ecology01:24

Freshwater Microbial Ecology

Freshwater systems such as streams, rivers, and lakes exhibit distinct physical and biological characteristics that influence their microbial communities. These environments are broadly categorized into lotic systems—those with flowing waters like streams and most rivers—and lentic systems, which include still or slow-moving waters such as lakes, ponds, and marshes.In lentic systems, phytoplankton drive primary production, generating autochthonous organic carbon. In contrast, lotic systems...
Microbial Interactions: Predation01:28

Microbial Interactions: Predation

Microbial predation refers to the process by which one microorganism kills and consumes another to obtain nutrients and energy. It encompasses both bacterial and protozoan predators. This interaction plays a crucial role in shaping microbial communities and regulating nutrient cycling.Bacterial Predators: Epibiotic vs. EndobioticBacterial predators are classified based on their mode of attack as either epibiotic or endobiotic. Epibiotic predators, such as Vampirococcus, attach to the surface of...
Microbial Mats01:25

Microbial Mats

Microbial communities forming biofilms and mats represent complex, spatially structured ecosystems where metabolic processes are stratified according to light, oxygen, and nutrient gradients. Biofilms are initial colonization stages, only a few millimeters thick, while mature microbial mats can reach centimeter-scale thickness and display intricate vertical organization. Their structural and functional heterogeneity allows microorganisms to occupy distinct ecological niches within a few...

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Ocean acidification and rising temperatures may increase biofilm primary productivity but decrease grazer

Bayden D Russell1, Sean D Connell, Helen S Findlay

  • 1Southern Seas Ecology Laboratories, School of Earth and Environmental Sciences, University of Adelaide, South Australia 5005, Australia. bayden.russell@adelaide.edu.au

Philosophical Transactions of the Royal Society of London. Series B, Biological Sciences
|August 28, 2013
PubMed
Summary
This summary is machine-generated.

Climate change impacts on intertidal ecosystems are complex. Short-term experiments may not predict long-term effects due to organism acclimation to elevated CO2 and temperature.

Keywords:
biofilmclimate changegrazingocean acidificationphysiological performanceprimary productivity

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Area of Science:

  • Marine Ecology
  • Climate Change Biology
  • Ecosystem Dynamics

Background:

  • Climate change, driven by increasing atmospheric CO2 and temperatures, can restructure ecosystems.
  • Intertidal zones are particularly vulnerable to these changes, affecting primary producers and consumers.
  • Organismal responses to environmental stressors can vary based on exposure duration.

Purpose of the Study:

  • To investigate the combined effects of elevated CO2 and temperature on UK intertidal biofilms and their consumers, Littorina littorea.
  • To assess how pre-exposure duration (two weeks vs. five months) influences the response of L. littorea to climate change conditions.
  • To evaluate the predictability of ecosystem responses using short-term laboratory experiments versus long-term acclimation.

Main Methods:

  • Controlled microcosm experiment simulating elevated CO2 and temperature.
  • Investigation of biofilms (primary producers) and Littorina littorea (consumers).
  • Comparative analysis of L. littorea grazing rates and biofilm abundance after short-term (five weeks) and long-term (five months) pre-exposure.

Main Results:

  • Elevated CO2 and temperature decreased grazer consumption of primary productivity over five weeks, increasing biofilm abundance.
  • Long-term pre-exposure (five months) resulted in higher grazing rates in L. littorea compared to short-term exposure.
  • Short-term experiments may overestimate negative impacts of climate change due to lack of organismal acclimation.

Conclusions:

  • Ecosystem responses to climate change may not be accurately predicted by short-term laboratory studies alone.
  • Prolonged exposure allows organisms to acclimate, altering their physiological and consumptive responses.
  • Predicting future ecosystem structures requires integrating laboratory data with long-term, large-scale ecosystem experiments.