A bit more information you asked for about the burrow systems:
You have picked up a nodule of Flint, which is a form of cryptocrystalline quartz and occurs naturally where chalk is the local bedrock.. Flint formed soon after deposition of the Chalk (around 80-90 million years ago), a metre or more below the sea-floor. The silica was derived mainly from the dissolved skeletal elements of hard sponges, in the generally alkaline environment that existed below the sea floor.. When organic matter rots, it sometimes can create local acidic conditions. The silica can no longer remain in solution in these conditions and reprecipitates as a form of silica gel initially, while the chalk (calcium carbonate) dissolves instead. This process occurred preferentially in more permeable parts of the sediment, such as horizontal galleries of burrows (probably excavated by shrimps for feeding or shelter). Consequently, most flints are replacements of the chalk in and around burrows, and the shape of a flint nodule generally reflects the original burrow morphology. Yours is a piece of one of these "Nodular Flints", which has grown even bigger into quite a large irregular mass. Sometimes, they were so abundant that they coalesced into a more or less continuous bed, forming a so-called "Tabular Flint".
So, while this is not exactly the dinosaur you hoped for, it is the direct result of animal activity in the Cretaceous Period which has been preserved and is called a Trace Fossil.