ALICE is the LHC experiment devoted to the study of heavy-ion collisions. While results from Pb-Pb collisions at √ sNN = 2.76 TeV provide insight on the properties of the plasma of quarks and gluons, formed in nucleus-nucleus interactions, the study of p-Pb collisions at √ sNN = 5.02 TeV allows a deeper understanding of cold nuclear matter effects. Therefore, p-Pb results turn out to be a powerful tool to provide a baseline for Pb-Pb, to correctly quantify how the various observables are affected by genuine hot medium effects. In this proceeding, a selection of the most recent ALICE results on the medium global properties and on heavy-flavour and quarkonium production will be discussed. ALICE (A Large Ion Collider Experiment) is one of the four large LHC experiments and its main objective is the study of the properties of the QGP. The ALICE experiment complements the experi- mental heavy-ion program, started about thirty years ago at the Brookhaven Alternating Gradient Syn- chrotron (AGS) and continued at the CERN Super Proton Synchrotron (SPS) up to √ sNN =20 GeV and finally at the Brookhaven Relativistic Heavy-Ion collider (RHIC) up to √ sNN =200 GeV. In the last five years ALICE has collected a large wealth of data, studying Pb-Pb collisions at √ sNN = 2.76 TeV and to complement its heavy-ion program, also p-A and pp interactions, to be used as references, have been investigated. In particular, since in the simpler p-A collision system the conditions which should lead to the formation of the QGP are not fullfilled, hot matter related effects are not expected to set in. Therefore, the study of the behaviour of several probes in the cold nuclear matter provides a fundamental reference to understand the Pb-Pb results, where hot matter effects are present on top of the cold matter ones. One way to investigate the global properties of the QCD medium is via the collective behaviour of the bulk of particles produced in the collisions. In the hot and strongly interacting medium collective behaviours can arise and flow of particles, generated by the presence of pressure gradients, can be
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