A layered double hydroxides (LDH) hydrotalcite-pyroaurite solid solution series (Mg 1−x Fe(II) x ) 3 Al 1 Cl 1 · nH 2 O with variable xFe solid = Fe 2+ /(Fe 2+ + Mg 2+ ) iron mole fractions were studied in co-precipitation experiments at T = 25, 40, 45, 50, 55 and 60 • C and pH = 10.00 ± 0.05. The compositions of the solids and reaction solutions were determined using ICP-OES, EDX (Mg, Al, Fe) and TGA techniques (Cl − , OH − , H 2 O). Powder X-ray diffraction was applied for phase identification and determination of unit-cell parameters a o = b o and c o from Bragg evaluation. Syntheses products containing xFe solid > 0.13 display additional X-ray patterns attributed to the mixture of iron oxides and hydroxides. On the other side, precipitates with 0 ≤ xFe solid ≤ 0.13 show only X-ray reflexes typical for pure LDH compositions. Moreover, in this case unit-cell parameters a o = b o as a function of xFe solid follow Vegard's law corroborating the existence of a continuous solid solution series. TGA data demonstrated the temperatures at which interlayer H 2 O molecules and Cl − -anions are lost, and at which temperatures dehydroxylation of brucite-like layer occurs. Based on detailed analyses of TGA curves it was established that the increase of xFe solid does not result in a visible change of the thermal stability of hydrotalcite-pyroaurite solids. From the chemical analyses of both the solids and the reaction solutions after syntheses, preliminary Gibbs free energies of formation were estimated by using GEMS-PSI code package. Values of G • f (Hydrotalcite) = −3619.04 ± 15.27 kJ/mol and G • f (Pyroaurite) = −2703.61 ± 191.93 kJ/mol were found at 298.15 K. A comparison of our estimate with G • f value −3746.90 ± 11.00 kJ/mol for CO 3 2− -bearing hydrotalcite presented in our previous studies, denotes the effect of intercalated anion on the aqueous solubilities of LDH when Cl-containing solids have to be more soluble than CO 3 2− -bearing substances. Estimation of the standard molar entropy of the hydrotalcite end-member by applying Helgeson's methods and using results of co-precipitation experiments at variable temperatures let us to conclude that derivation of more precise S • f values would require calorimetric measurements.