(a) If the Aα are non-zero, A is non-zero. (b) If the Aα are integral domains, A is an integral domain. (c) If the Aα are fields, A is a field.
Let 0α,1α be the zero and unit of Aα and 0, 1 the zero and unit of A. There exists α∈I such that fα(0α)=0,fα(1α)=1. If 0=1, there exists β≥α such that fβα(0α)=fβα(1α), that is 0β=1β. This proves (a).
Suppose that Aα are integral domains. Then A is commutative and non-zero by (a). Let x,y be elements of A such that xy=0. There exists α∈I and xα,yα∈Aα such that x=fα(xα),y=fα(yα). Then fα(xαyα)=xy=0=fα(0α). Hence there exists β≥α such that fβα(xαyα)=fβα(0α). As Aβ is an integral domain, it follows that fβα(xα)=0β or fβα(yα)=0β, hence x=0 or y=0. This proves (b).
Suppose that the Aα are fields. Then A={0} by (a). Let x be a non-zero element of A. There exist α∈I and xα∈Aα such that x=fα(xα). Then xα=0 and fα(xα−1) is the inverse of x in A. This proves (c).
Let E=(Eα,fβα) and E′=(Eα′,fβα′) be two direct systems of magmas (resp. monoids, groups, rings). A homomorphism of E into E′ is a direct system (uα)α∈I of mappings uα:Eα→Eα′ such that each uα is a homomorphism. Under these conditions, the mapping u=limuα from E=limEα to E′=limEα′ is a homomorphism (cf. Set Theory, III, § 7, no. 6).
Bourbaki puts the proof directly after the statement, so what is above is the statement and its proof together.
Nothing.