The binodal of a boson square-well fluid is determined as a function of the particle mass through the newly devised quantum Gibbs ensemble Monte Carlo algorithm [R. Fantoni and S. Moroni, to be published]. In the infinite mass limit we recover the classical result. As the particle mass decreases the gas-liquid critical point moves at lower temperatures. We explicitely study the case of a quantum delocalization de Boer parameter close to the one of 4 He. For comparison we also determine the gas-liquid coexistence curve of 4 He for which we are able to observe the binodal anomaly below the λ-transition temperature. Soon after Feynman rewriting of quantum mechanics and quantum statistical physics in terms of the path integral [1,2] it was realized that the new mathematical object could be used as a powerful numerical instrument.The statistical physics community soon realized that a path integral could be calculated using the Monte Carlo method [3].Consider a fluid of N bosons at a given absolute temperature T = 1/k B β with k B Boltzmann constant. Let the system of particles have a HamiltonianĤsymmetric under particle exchange, with λ = 2 /2m, m the mass of the particles, and φ(|r i − r j |) the pair-potential of interaction between particle i at r i and particle j at r j . The many-particles system will have spatial configurations {R}, with R ≡ (r 1 , . . . , r N ) the coordinates of the N particles. The partition function of the fluid can be calculated [3] as a sum over the N ! possible particles permutations, P, of a path integral over closed many-particles paths X ≡ (R 0 , . . . , R P ) in the imaginary time interval τ ∈ [0, β = P ǫ], discretized into P intervals of equal length ǫ, the time-step, with R P = PR 0 the β-periodic boundary condition.More recently a grand canonical ensemble algorithm has been devised by Massimo Boninsegni et al. [4] for the path integral Monte Carlo method. This paved the way to the development of a quantum Gibbs ensemble Monte Carlo algorithm (QGEMC) to study the gas-liquid coexistence of a generic boson fluid [5]. This algorithm is the quantum analogue of Athanassios Panagiotopoulos [6] method which has now been successfully used for several decades to study first order phase transitions in classical fluids [7]. However, like simulations in the grandcanonical ensemble, the method does rely on a reasonable number of successful particle insertions to achieve compositional equilibrium. As a consequence, the Gibbs ensemble Monte Carlo method cannot be used to study equilibria involving very dense phases. Unlike previous extensions of Gibbs ensemble Monte Carlo to include quantum effects (some [8] only consider fluids with internal quantum states; others [9] successfully exploit the path integral Monte Carlo isomorphism between quantum particles and classical ring polymers, but lack the structure of particle exchanges which underlies Bose or Fermi statistics), the QGEMC scheme is viable even for systems with strong quantum delocalization in the degenerate regime of temperature. Details...