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Atomism

Natural philosophy holding that the world comprises fundamental indivisible components

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Through Principle, India and Buddhists

The concept of atomism appeared in both ancient Greek and ancient Indian philosophical traditions. Atomism in multiple different forms appeared in ancient Greece. Leucippus is the earliest figure whose commitment to Greek atomism is well attested and is usually credited with inventing Greek atomism. He and other ancient Greek atomists argued that nature consists of two fundamental principles: atom and void. Clusters of different shapes, arrangements, and positions give rise to the various macroscopic substances in the world. A similar idea was developed by Kanāda of the Vaiśeṣika school, who proposed indivisible particles (paramāṇu). Indian Buddhists, such as Dharmakirti (fl. c. 6th or 7th century) and others, developed distinctive theories of atomism, for example, involving momentary (instantaneous) atoms (kalapas) that flash in and out of existence.

The particles of chemical matter for which chemists and other natural philosophers of the early 19th century found experimental evidence were thought to be indivisible, and therefore were given by John Dalton the name "atom", long used by the atomist philosophy. Although the connection to historical atomism is at best tenuous, elementary particles have become a modern analogue of philosophical atoms.

Reductionism

Philosophical atomism is a reductive argument, proposing not only that everything is composed of atoms and void, but that nothing they compose really exists: the only things that really exist are atoms ricocheting off each other mechanistically in an otherwise empty void. One proponent of this theory was the Greek philosopher Democritus.

By convention sweet is sweet, by convention bitter is bitter, by convention hot is hot, by convention cold is cold, by convention color is color. But in reality there are atoms and the void.

Atomism stands in contrast to a substance theory wherein a prime material continuum remains qualitatively invariant under division (for example, the ratio of the four classical elements would be the same in any portion of a homogeneous material).

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