Understanding CO₂ fixations in oceans

Marine algae play a critical role in global CO₂ fixation, and they play an important role in the oceans uptake of anthropogenic CO₂. Because their photosynthetic enzymes evolved when the atmospheric CO₂ concentration was much higher over a billion years ago, today most algae invest a large amount of energy to transport carbon and elevate the concentration of CO₂ at the active site of the enzymes. It is thought that rising atmospheric CO₂ levels might reduce the need for such a large energy investment and might benefit algal productivity in some areas of the ocean. But because this system of carbon concentration takes place deep in the cell and is largely unobservable, we don’t have a good grasp of how extensively it is used in populations in different parts of the ocean today, where the cells must balance their energy allocation to deal with multiple challenges.

In a recently published study in the Proceedings of the National Academy of Sciences (PNAS) scientists from the Geological Institute of ETH Zurich were looking to decode a chemical indicator – the relative abundance of two stable isotopes of hydrogen in algal lipids – so that they can use this indicator to better understand the efficiency of photosynthesis in other settings where they cannot easily manipulate or probe algae in the way they do in lab experiments. They were working with the hydrogen isotope ratio of lipids produced by the algae, because these lipids can easily be extracted from natural populations of algae in aquaculture, in the ocean, and these lipids are even accumulated at the seafloor after the algae have died so they can investigate even the behavior of photosynthetic processes in the past under different environmental conditions.

Previously, there has been wide interest in using the ratio of two hydrogen isotopes (²H/¹H) in algal lipids, as a passive indicator of the ²H/¹H ratio of the ocean. The hydrogen isotope ratio in the ocean is controlled by the balance of evaporation from and precipitation to, seawater in a given region and varies with salinity. This interest was focused on using lipids from fossil algae to estimate the past changes in salinity of different regions of the ocean to better understand the freshwater cycle in different climates. However, that interpretive framework kept producing paradoxes of really different responses in algal lipids collected from natural ocean populations, compared to laboratory cultures where a single environmental variable like salinity was manipulated.

To better decode this indicator, the researchers grew the algae under carefully controlled conditions in the laboratory and for the first time evaluated how the CO₂ concentration affected the hydrogen isotope ratio. In a second phase of the study, they developed a comprehensive new model of the cellular conversions of hydrogen in different parts of the photosynthetic cycle, and how these would affect the hydrogen isotope ratio. This new model allowed them to diagnose the biochemical variables encoded in the chemical indicator and show that it is very sensitive to the concentration of CO₂ achieved at the site of the photosynthetic enzyme Rubisco.

In a next step it will be important to investigate if the regulation of the carbon concentrating mechanism is similar in other types of marine phytoplankton.