Oxygen from Water: How Plants Build It Brick by Brick express

Original: "New water oxidation mechanism in Photosystem II resolves major experimental controversies"
· Yulia Pushkar
arXiv:2601.14273 · 2026-01-09 · CC BY 4.0 · 2 min
Scientists have figured out how the photosynthesis protein joins two oxygen atoms into one molecule.

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In every leaf, in the light, a factory works that splits water into oxygen and hydrogen. The oxygen goes into the air we breathe, and the plant uses the hydrogen for food. The heart of this factory is a protein complex with four manganese atoms and one calcium atom. It's there that water loses electrons and becomes oxygen.

For a long time, researchers couldn't figure out how two oxygen atoms that were previously in different water molecules end up next to each other and bond. New work proposes this scenario. One oxygen atom (let's call it O3) comes from a water molecule and sits next to manganese. The second atom (O6) is already held ready by the protein. When light arrives, electrons jump, and the atoms come closer. The bond between them forms like a zipper: two halves come together, and the teeth catch each other.

The protein doesn't just bring atoms together. It controls their charges through weak interactions, like a conductor who doesn't play himself but decides when each instrument should come in.

This pathway of bonding turns out to be energetically more favorable than the one previously considered dominant. Instead of waiting for two oxygen atoms to find each other in a crowded room, the protein guides one of them to the right spot and holds it until the second arrives. It's like assembling furniture: first you place a piece into the groove, then you screw in the second one.

The researchers noticed a similarity with hemoglobin — the protein that carries oxygen in blood. There, too, there's a "pocket" that holds oxygen until it's needed. Nature often uses the same tricks.

Understanding this mechanism is important for creating artificial systems that will produce oxygen or clean fuel from water and sunlight. If we learn to replicate this trick, we could build factories that mimic a leaf but are even more efficient.

Original abstract

as written by the authors arXiv:2601.14273

Light driven oxygen formation in Photosystem II protein is a fundamental process that sustains our biosphere and serves as a blue print to future clean energy solutions due to its high energy conversion efficiency. Last decade of intense research by advanced physical techniques delivered new insights on the structure and function of the Mn4CaO5 cluster a center of the oxygen evolving complex (OEC). However, discrepancies in experimental observations and computational models persist impeding the understanding of the O-O bond formation and the role of the protein environment in the process. Here we show that i) assignment of the OEC unique oxygen O3 ligated by histidine (His337) via dynamic H-bond as a slow exchanging substrate and ii) its coupling with O6 oxygen generated at Mn1 in the S2 to S3 transition give the O-O bond formation mechanism most consistent with all currently available experimental data. Proposal shows how protein environment can steer the O-O bond formation by charge control via H-bond and open coordination of Mn1. Obtained O3-O6 peroxide is at lower energy than peroxides in the most studied O5-O6 bond formation pathway. His337 appears to be similar to distal His in globins used for management of the O2 and H2O2 intermediates. The new mechanism breaks the prior impasse and will undoubtedly invigorate future detailed studies uncovering its further details.

Each year, plants produce about 300 billion tons of oxygen. That's roughly the weight of all humans on Earth multiplied by 40.

Scientists
William Lawrence BraggDaniel BernoulliLeonhard EulerArchimedesFred HoyleMargaret Burbidge
Concepts
water splitting photosynthesis hydrogen bond oxygen photochemistry chlorophyll hydrocarbon energy extraction hydrogen production carbon monoxide helium burning atmospheric chemistry calcium titanium oxide lithium niobate hydrogen carbon dioxide triple-alpha process (Hoyle process) hydrogen atmosphere sulfur dioxide