Horizontal gene transfer (HGT) in bacteria occurs in the context of adaptive genome architecture. As a consequence, some chromosomal neighbourhoods are likely more permissive to HGT than others. Here, we investigate the chromosomal topology of horizontal gene flow into a clade of Bacillaceae that includes Geobacillus spp. Reconstructing HGT patterns using a phylogenetic approach coupled to model-based reconciliation, we discover three large contiguous chromosomal zones of HGT enrichment. These zones encompass and connect classically defined genomic islands. Analyzing topological and strand biases of recent and older transfer events, we show that restrictions on entry are rapidly enforced by selection and that restrictive and permissive zones have existed in their current locations for long periods of evolution. The largest zone, characterized by a high influx of metabolic genes, is centred on the terminus. The other two zones flank a narrow non-permissive zone around the origin of replication and extend to delimit the first third of the chromosome -the part of the chromosome that is confined to the forespore during early spore formation.Horizontal transfers into this area are biased towards functions classically controlled by the forespore-specific sigma factor σ F : signal transduction, transcription, and particularly membrane biogenesis. Similar enrichment patterns are present in spore-forming but absent in non-spore-forming Bacilli. Our results suggest that the topology of HGT in Geobacillus, and Bacilli more generally, reflects constraints imposed by chromosomal organization for fast and sporulation, as asymmetric chromosomal entrapment in the forespore during early spore formation restricts where HGT-driven innovation in sporulation can occur.