Related Experiment Video
Updated: Jul 14, 2026

05:00
Measuring Dissolved Methane in Aquatic Ecosystems Using An Optical Spectroscopy Gas Analyzer
Published on: July 26, 2024
Trace gas emissions from the marine biosphere.
1School of Environmental Sciences, University of East Anglia, Norwich, UK. p.liss@uea.ac.uk
Summary
Marine biological and photochemical processes produce trace gases that often transfer to the atmosphere, impacting air chemistry, climate, and human health through oxidation and particle formation.
Area of Science:
- Biogeochemistry
- Atmospheric Chemistry
- Climate Science
Background:
- Marine waters are sources of various trace gases formed through biological and photochemical reactions.
- These gases, often supersaturated in water, flux to the atmosphere, influencing atmospheric composition.
Purpose of the Study:
- To provide a brief update on recent advances in marine trace gas biogeochemistry.
- To discuss the impacts of marine-derived trace gases on atmospheric chemistry, climate, and human health.
Main Methods:
- Review of recent literature and research findings on marine trace gases.
- Discussion of specific trace gases (e.g., dimethyl sulphide, organohalogens, nitrous oxide) and their atmospheric fates.
Main Results:
- Trace gases released from the ocean are oxidized in the atmosphere, affecting air's oxidizing capacity.
- These gases contribute to new particle formation and growth, influencing aerosol effects on climate.
- The cycles of these gases have implications for atmospheric chemistry, climate regulation, and human health.
Conclusions:
- Marine trace gases play a significant role in atmospheric processes and climate.
- Understanding these biogeochemical cycles is crucial for assessing their broader environmental impacts.
Related Concept Videos
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 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...
Bioremediation
Bioremediation is the use of prokaryotes, fungi, or plants to remove pollutants from the environment. This process has been used to remove harmful toxins in groundwater as a byproduct of agricultural run-off and also to clean up oil spills.
The Sulfur Cycle
Sulfur, an important element in the chemical makeup of proteins, is recycled through the atmosphere and aquatic and terrestrial environments. Found in the atmosphere as sulfur dioxide (SO2), sulfur is released by decaying organisms, weathered rocks, geothermal vents, volcanos, and burning fossil fuels. It is deposited into the ecosystem, cycled through the biotic community, and either released back into the atmosphere as gas or deposited in marine sediment for long-term storage and eventual...
Deep Sea Microbial Ecology
The deep ocean and its underlying sediments represent vast, largely unexplored microbial habitats that extend far beyond the sunlit photic zone. The photic (euphotic) zone typically spans the upper ~100–200 meters of pelagic waters in the open ocean, but its depth varies geographically and seasonally, where sufficient light supports photosynthetic life. Below this lies the deep sea, spanning roughly 1000–6000 meters (bathypelagic to abyssal zones), with deeper hadal trenches extending beyond...
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.

