Related Experiment Video
Updated: May 9, 2026

06:10
Using Generative Art to Convey Past and Future Climate Transitions
Published on: March 31, 2023
Climate change and the oceans--what does the future hold?
Jelle Bijma1, Hans-O Pörtner, Chris Yesson
1Alfred-Wegener Institute for Polar and Marine Research, Bremerhaven, Germany.
Marine Pollution Bulletin
|August 13, 2013
Summary
The ocean absorbs CO2, leading to acidification and warming, which harms marine life. Urgent emission cuts are needed to prevent irreversible ecosystem damage and extinctions.
Area of Science:
- Marine Biology
- Oceanography
- Climate Science
Background:
- Oceans mitigate climate change by absorbing atmospheric CO2.
- Ocean CO2 absorption causes acidification (lowering pH).
- Ocean warming, freshening, and deoxygenation impact marine ecosystems.
Purpose of the Study:
- To review observed impacts of ocean warming, acidification, and deoxygenation.
- To analyze historical parallels of these stressors.
- To project future ocean ecosystem changes under continued emissions.
Main Methods:
- Literature review of observed oceanographic and ecological changes.
- Analysis of paleoceanographic data and past extinction events.
- Synthesis of current trends to predict future impacts.
Main Results:
- Combined effects of warming, acidification, and deoxygenation severely impact marine flora and fauna.
- Distribution shifts and population declines are widespread.
- Synergistic effects with pollution, eutrophication, and overfishing exacerbate damage.
Conclusions:
- The "deadly trio" of ocean stressors mirrors past events linked to mass extinctions.
- Without significant and immediate carbon emission reductions, severe future impacts on marine biodiversity are projected.
- Urgent climate action is critical to prevent catastrophic marine ecosystem collapse.
Related Concept Videos
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.
What is Climate?
Climate refers to the prevailing weather conditions in a specific area over an extended period. As the saying goes, “Climate is what you expect. Weather is what you get.” Climate is influenced by geographic factors, such as latitude, terrain, and proximity to bodies of water.
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...
What is Weather?
Overview
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.

