Why do we study ocean biogeochemistry?
The ocean has a huge and diverse range of ecosystems, from shallow coastal waters to the vast open sea and the deep seafloor. Each one supports life that’s adapted to its own specific environment and food webs. Ultimately, at the base of almost all marine ecosystems are tiny, microscopic organisms: the phytoplankton.
Why Does the Ocean’s Carbon Cycle Matter?
The ocean plays a dominant role in the Earth’s carbon cycle. It holds more than 90% of the planet’s carbon and absorbs around 25% of our carbon dioxide (CO₂) emissions. This uptake reduces the amount of CO₂ left in the atmosphere to cause climate warming. Understanding how the ocean’s carbon cycle works is a critically important area of research.
Marine ecosystems play a significant part in the ocean’s natural carbon cycle by transporting carbon from the surface to the deep ocean. This process is known as the “biological carbon pump” (BCP). However, climate-driven changes in ocean temperature, circulation, and mixing are expected to reduce the supply of deep nutrients that fuel the BCP. This may disrupt its vital role in storing carbon.”
How Does Ocean Biogeochemistry Affect Human Communities?
Focusing more directly on human concerns, marine productivity is ultimately what provides us with resources like fisheries. Marine ecosystems support global fisheries, which collectively employ 62 million people and feed about 3.2 billion, sustaining regional economies.
In coastal areas, seaweeds provide ecosystem services like pollution remediation and have a natural value we can all appreciate. On top of that, the wider ocean carbon cycle could potentially be leveraged by marine carbon dioxide removal (mCDR) technologies. These aim to remove CO₂ from the atmosphere and eventually help reduce the extent of climate warming.
So, studying how marine ecosystems operate, and how they might change, is a major goal for our ecosystems modelling group.
What is MEDUSA?
MEDUSA (Model of Ecosystem Dynamics, nutrient Utilisation, Sequestration and Acidification) describes the surface ocean ecosystem with a simple, size-based model (nutrient-phytoplankton-zooplankton-detritus). It simulates the linked biogeochemical cycles of carbon, nitrogen, silicon, iron, and oxygen. We use MEDUSA in detailed, high-resolution simulations to help understand how human systems, including fisheries, may change in the future.
MEDUSA is typically run inside physical models of the ocean. This means its components respond to properties like temperature and salinity, and are transported around the ocean by currents. We can then compare the geographical and seasonal output from our models with observational data from ships, autonomous platforms, or satellites. This helps us work out how good a job the model is doing and how we can improve it.
How Does MEDUSA Contribute to Climate Research?
An important part of our work comes from MEDUSA serving as the marine biogeochemistry component of the UK’s state-of-the-art Earth system model, UKESM. Through UKESM, MEDUSA contributes to the international climate simulations that inform the Intergovernmental Panel on Climate Change (IPCC) Assessment Reports. This helps improve our global understanding of how the ocean influences climate.
Using UKESM also allows our group to better study the links between marine ecosystems and the wider atmosphere and land systems. This integrated approach lets us examine how changes in one part of the Earth system cascade through to affect others.
Why is the Research Important for the Future?
Ocean biogeochemistry is important for understanding the ocean’s carbon cycle and its ecosystems, so crucial for both tackling global-scale challenges such as climate change and knowing how we can mitigate these or adapt to them.
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National Oceanography Centre, 14 May 2026. More information.
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