Development of oxygenic photosynthesis provided the primeval reducing atmosphere with oxygen that is essential for all presently existing higher forms of heterotrophic life including human beings. Oxygenic photosynthesis is initiated at photosystem II (PSII), a multi‐subunit protein complex that is decorated with various cofactors and located in the thylakoid membrane of cyanobacteria, algae and higher plants. PSII captures sunlight with its antenna proteins and converts it to chemical energy by catalyzing water oxidation to atmospheric oxygen, protons and electrons. The reducing electrons are exploited in subsequent steps in the formation of reduced nicotinamide adenine dinucleotide phosphate (NADPH) used to reduce CO
2
to carbohydrates.
We discuss here the presently most complete structure of cyanobacterial PSII that includes 35 chlorophyll
a
, 11 carotenoids, 2 pheophytins
a
, 2 plastoquinones, 2 hemes, bicarbonate, 14 lipids, 3 detergent molecules (
n
‐dodecyl‐β‐
D
‐maltoside), 4 Mn‐atoms, 2 Ca
2+
, and Fe
2+
that are embedded within 19 protein subunits per monomer. Water oxidation takes place at a redox‐active metal cluster that is composed of 4 Mn‐cations and 1 Ca
2+
cation. The arrangement, geometry and coordination of the metal ions in the Mn
4
Ca‐cluster provide information essential for understanding mechanistic aspects of water oxidation.