* The melting parameterisations used in **meltPT**, via **pyMelt**, use a
quadratic function for the solidus, so that for large potential temperatures
no melting path can be calculated. To avoid optimisation algorithms
attempting to test such high potential temperatures, we included an
arbritrary upper bound on potential temperature. In this new version, rather
than being set abritrarily, the upper bound is chosen based on the properties
of the mantle object passed to the optimisation routine.
* A bug has been fixed which caused sample-composition backtracking with a
constant value for the partition coefficient to fail in verbose mode.
* A discrepency between the script Examples/Tutorials/Tutorial_1.py and the
version rendered in the documentation has been fixed.