In this previous answer to Life on a molten world, I provided several biochemical regimes dependent upon temperature.
At 400+ C, Fluorosilicones (silicon based macromolecule)
Each of the suggested biochemical regimes includes carbon as the backbone molecule for the chemical chain, except that of the highest temperature which is Fluorosilicone chemical chains dissolved in fluorosilicone solvent (our chemistry is proteins [carbon chains] dissolved in water) for temperatures in the 400 C - 500 C range.
$$\begin{array}{|c|c|}
\hline \text{Temp Range} & \text{Macromolecule in Solvent} \\
\hline \text{400° C to 500°? C} & \text{Fluorosilicones in Fluorosilicones} \\
\hline \text{113° C to 445° C } & \text{Fluorocarbons in molten Sulfur} \\
\hline \text{0° C to 100° C} & \text{Proteins in Water} \\
\hline \text{-77.7° C to -33.4° C} & \text{Proteins in Liquid Ammonia} \\
\hline \text{-183.6° C to -161.6° C} & \text{Lipids in Liquid Methane} \\
\hline \text{-253° C to -240° C} & \text{Lipids in Liquid Hydrogen} \\
\hline
\end{array}$$
This table suggests that our familiar protein in water form of life is only appropriate for a certain range of temperatures. When you develop worlds in other temperature ranges, native life will develop for the temperature range of that planet.
e.g. Mars (average temperature of -65 C) might require proteins in liquid ammonia while Titan (average temperature -180 C) might require life using lipids in liquid methane.