As the second most-abundant chemical element in the universe, helium makes up a large fraction of giant gaseous planets, including Jupiter, Saturn, and most extrasolar planets discovered to date. Using first-principles molecular dynamics simulations, we find that fluid helium undergoes temperature-induced metallization at high pressures. The electronic energy gap (band gap) closes at 20,000 K at a density half that of zero-temperature metallization, resulting in electrical conductivities greater than the minimum metallic value. Gap closure is achieved by a broadening of the valence band via increased s-p hydridization with increasing temperature, and this influences the equation of state: The Grü neisen parameter, which determines the adiabatic temperature-depth gradient inside a planet, changes only modestly, decreasing with compression up to the high-temperature metallization and then increasing upon further compression. The change in electronic structure of He at elevated pressures and temperatures has important implications for the miscibility of helium in hydrogen and for understanding the thermal histories of giant planets.high pressure ͉ metallization ͉ giant planets ͉ gap closure ͉ hybridization H elium is known to be an electrical insulator at low pressure, with a wide energy gap (19.8 eV) between occupied and unoccupied electron orbitals; it exhibits almost no chemical bonding (1). Under compression, however, helium is predicted to metallize via closure of the energy gap at Ϸ100 Mbar (10 TPa) (2), a pressure greater than that at Jupiter's center (3). Thus, one might expect helium to be insulating at giant-planetary conditions, for its solubility in metallic hydrogen to be limited and for addition of helium to limit the electrical conductivity of the gaseous envelope (4).However, recent high-pressure results have revealed the role of temperature in metallization, particularly in the fluid state. Fluid hydrogen becomes metallic at 1.4 Mbar at high temperature (Ͼ10 3 K) along the shock-wave Hugoniot (5), whereas at low temperature (Յ300 K) crystalline hydrogen is expected to metallize only Ͼ4 Mbar (6). In a sense, hydrogen at elevated pressures resembles other materials that undergo insulator-tometal transitions upon melting, such as silicon and carbon, in which the liquid has a more densely-packed structure than the solid phase. Yet the metallization of fluid hydrogen may also be related to changes in the fluid, from dominantly molecular (H 2 ) at lower pressures to dominantly atomic (H) at higher pressures (7). That ionization and dissociation of the molecule take place across overlapping regimes of density and pressure is a complication that has confounded a full understanding of the metallization of hydrogen. The case of helium is thus revealing in that it effectively isolates the influences of temperature and density on the development of metallic bonding, because both liquid and solid are monatomic and close packed at high pressure.We performed first-principles molecular dynamics simulations and fou...