I want to know the answer to the following question:
What was the result in the decline in sea level in the middle of the Carboniferous period?
All the background I'm provided with is that "A global drop in sea level at the end of the Devonian reversed early in the Carboniferous; this created the widespread epicontinental seas and carbonate deposition of the Mississippian.". Is that enough to answer the question?
Answer: no