Think about the energy for a particle of mass $m$ in a uniform gravitational field,
$$E=\frac{1}{2}mv^{2}+mgz.$$
This energy is conserved, because it does not depend explicitly on $t$. That essentially just means that $t$ does not appear in the mathematical expression. However, if the mass were changing (if, say, it was being eroded by wind), making the mass a function of $t$—something like $m(t)=m_{0}e^{-t/T}$, for some constants $m_{0}$ and $T$, then the energy
$$E(t)=\frac{1}{2}m_{0}e^{t/T}v^{2}+m_{0}e^{t/T}gz$$
is clearly not going to be constant in time. The energy will decay along with the mass of the object.
This should all be fairly straightforward. The confusing bit of terminology appears because, the energy $E$ is defined in terms of other dynamical quantities (in this case, the velocity $v$ and the vertical position $z$). And both of these are going to be functions of time in the usual way:
$$v(t)=v_{0}-gt\\
z(t)=z_{0}+v_{0}t-\frac{1}{2}gt^{2}.$$
So you could still consider $E$ as a function of $t$, through its dependence on $v$ and $z$, as in
$$E(t)=\frac{1}{2}m\left[v(t)\right]^{2}+mgz(t).$$
What the statement of the book is trying to convey is that when the time dependence of the energy $E$ is only of this form—only implicit, through the time dependences of the position and velocity—then the total energy is conserved. In fact, if you calculate the derivative $dE/dt$ from the above equation, using the multivariable chain rule, you will get an expression that is zero if you plug in the $v(t)$ and $z(t)$ that obey the equations of motion.
Having a usual kinetic term $\frac{1}{2}mv^{2}$ and a potential energy $V(x)$ is one way to get a time-independent (and thus conserved) $E$. However, the statement that if $E$ has no explicit time dependence, then it is conserved, is more somewhat more general.