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Carl Wilhelm Scheele and Joseph Priestley independently prepared and investigated the gas now called oxygen; Antoine Lavoisier was central to interpreting it within a new account of combustion and chemical composition. Assigning a unique discoverer requires deciding whether discovery means first preparation, first public report, recognition of a distinct kind of gas, or a successful theoretical interpretation. The historical controversy is largely about why one of these achievements should be privileged over the others.

Carl Wilhelm Scheele's investigations, generally dated to the early 1770s, preceded publication of Chemical Treatise on Air and Fire by Carl Wilhelm Scheele in 1777. His work distinguished the component that sustained burning from the remainder of ordinary air. He obtained the active component through several chemical preparations, including heating suitable substances, and interpreted the results in terms of phlogiston. Delayed publication matters to public priority, but it does not show that the experimental work had not occurred. Equally, a publication date alone does not establish the precise date of every earlier trial.^[ref]

Joseph Priestley's 1775 account is unusually revealing because it records hesitation and revision. On 1 August 1774 he heated red mercury(II) oxide with a large burning lens and collected the released gas. A candle burned particularly strongly in it; later trials involving animals and comparison with nitric oxide helped him distinguish its properties from ordinary air. He initially lacked a settled understanding of what he had obtained. Calling the product dephlogisticated air eventually made it intelligible within his own framework: it had an unusually great capacity to accept the phlogiston supposedly released in burning and animal breathing.^[ref]

The modern chemical equation,is a useful reconstruction, but it must not be passed off as Joseph Priestley's own explanation. In modern terms, heating decomposes mercury(II) oxide into mercury and molecular oxygen. The eighteenth-century experimenter instead worked with such categories as calces and differently modified airs. The material operation can be recognized across the change in theory while the meaning of its product remains historically contested.

Antoine Lavoisier made a different contribution. His programme tracked what entered and left substances in calcination and combustion, placing gases within quantitative material balances. In the mercury experiment described in Elements of Chemistry by Antoine Lavoisier, a retort communicated with an enclosed supply of air over mercury. Prolonged heating formed a red calx and diminished the enclosed air. Stronger heating of the recovered calx released an especially combustion-supporting gas; adding it back to the residual air restored the properties of the original mixture. The persuasive feature was the linked decomposition and reconstruction, not just a single spectacular flame.^[ref]

That sequence supported the claim that air was a mixture and that calcination involved combining a metal with part of it. A metal could gain mass because material entered it from the air, without requiring an invisible substance to leave with anomalous properties. Conservation of mass made the weighing scale a constraint on the explanation. However, Antoine Lavoisier's entire system was not modern chemistry. He treated caloric as an explanatory principle and associated the newly named oxygen with the formation of all chemical acids. The latter universal claim is false: hydrochloric acid is an chemical acid whose solute, hydrogen chloride, contains hydrogen and chlorine but no oxygen. This concrete counterexample prevents us from defining discovery as possession of today's complete theory.^[ref]

There are consequently several legitimate allocations of credit. An investigator concerned with earliest preparation may emphasize Carl Wilhelm Scheele; one concerned with the well-documented 1774 experiment and its rapid communication may emphasize Joseph Priestley; one concerned with the explanatory reconstruction of combustion may emphasize Antoine Lavoisier. The last achievement depended on experimental results that the others had produced. Correct interpretation was neither a substitute for preparing the material nor an achievement wholly independent of communication between investigators.

Historians disagree because their accounts embody different pictures of scientific change. A simple accumulation story can make discovery look like identifying one additional item in a ready-made list of chemical elements. A conceptual-change story emphasizes that the list and its criteria were themselves changing: oxygen was not just another variety of modified air in the new chemistry. National priority narratives and the dramatic reputation of the Chemical Revolution can further encourage a single heroic winner. Yet replacing that winner with a collective label is insufficient unless the different experimental and theoretical contributions are explained.

The most defensible answer distributes credit while specifying the achievement. Carl Wilhelm Scheele and Joseph Priestley deserve independent experimental discovery credit; Antoine Lavoisier deserves central credit for the chemical interpretation and reorganization that gave oxygen its place in a new system. Discovery was a sequence of preparation, discrimination, communication and reinterpretation, rather than one instantaneous encounter with a theory-free fact.