The idempotents elements of the magma monoid \((\mathcal {M}(S), \triangleleft )\) are characterized. The characterization is used to determine, when S has n elements, the number of idempotents in \(\mathcal {M}(S)\) (also called \(\mathcal {M}(n)\) ). A combinatorial argument is inferred and then this generalized principle is used in a larger setting, that is, analogs to the magma monoid are introduced for s-ary operations, and the generalized combinatorial principle is used to determine the number of idempotent elements in those new monomials.In addition, the kernel-cokernel decomposition of idempotents in the binary magma monoid is analyzed and its properties and relations with anticommutative and pseudo-anticommutative operations are established.
