The surprising discovery of tripling the superconducting critical temperature of KFe2As2 at high pressures issued an intriguing question of how the superconductivity in the collapsed tetragonal phase differs from that in the non-collapsed phases of Fe-based superconductors. Here we report 89 Y nuclear magnetic resonance study of YFe2GexSi2−x compounds whose electronic structure is similar to that of iron-pnictide collapsed tetragonal phases already at ambient pressure. Fe(Ge,Si) layers show strong ferromagnetic spin fluctuations whereas layers are coupled antiferromagnetically -both positioning the studied family close to a quantum critical point. Next, localized moments attributed either to Fe interstitial or antisite defects may account for magnetic impurity pair-breaking effects thus explaining the substantial variation of superconductivity among different YFe2Ge2 samples. The collapsed tetragonal phase (CTP) found in the family of AFe 2 As 2 (A = Ba, Ca, Eu, Sr, K) at high pressures has been considered as a non-superconducting phase [1], because the formation of interlayer As-As bonds triggers topological change of the Fermi surface thus removing for the superconductivity important nesting conditions [2]. This notion has suddenly changed by the recent discovery of tripling the superconducting critical temperature T c in KFe 2 As 2 at pressures higher than ∼ 15 GPa when CTP is formed [3,4]. The strong electron correlations [4] or almost perfectly nested electron and hole pockets found for KFe 2 As 2 in CTP [5] were both put forward to explain the surprising enhancement of T c . Thus, to what degree the superconducting pairing mechanism of CTP differs from that of the non-collapsed layered Fe-based phases [6] remains at present unclear.Rare earth iron silicides and germanides of the RFe 2 X 2 type (R = rare earth element, X = Ge, Si) have been studied since the 1970's for their magnetic propertiesvarious probes showed no long-range magnetic order in this family of materials [7,8].