Answer:Paleoclimatic evidence that supports the idea of the late Paleozoic supercontinent in the southern hemisphere includes the distribution of glacial deposits and the presence of coal deposits. During the late Paleozoic era, the southern hemisphere was covered in ice sheets, which left behind glacial deposits. These deposits are found in South America, Africa, India, and Australia, which suggests that these continents were once connected. Additionally, coal deposits are found in these same continents, which indicates that these areas were once covered in lush, swampy forests. These forests likely grew in the warm, humid climate that existed in the late Paleozoic era, which would have been possible if these continents were connected. The distribution of glacial and coal deposits in the southern hemisphere provides strong evidence for the existence of a late Paleozoic supercontinent in the southern hemisphere.
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