There's some substructure in EEFs. There are two main clades of EEFs, which are Iberian EEFs and Danubian EEFs. The main difference between them are the presence or absence of Neolithic Iranian ancestry (which seems closest to IRN_Wezmeh_N), yet there are some EEFs in Central and Eastern Europe lacking that ancestry. Chief among the latter group is UKR_N_o:I3719, especially since it's the easternmost EEF sample known (at least of its time) and representative of an EEF population that contributed ancestry to Steppe groups. Then, there's variation in the amount of what looks like CHG ancestry, along with variable amounts of Natufian ancestry. Plus, there's local HG admixture, whose amount and nature varies on location and time period. Notably, variations in Neolithic Iranian, CHG, and Natufian admixtures are already seen in Neolithic Anatolia, with TUR_Barcin_N:I1096 as the only known Ceramic Neolithic-period ANF lacking Neolithic Iranian ancestry. The substructures in the founding ANF populations and their EEF descendants could explain the differences between Iberian and Danubian EEFs (besides different HG admixtures), the extra Neolithic Iranian ancestry in Italian EEFs, and the lack of it in some Central and Eastern European EEFs.