#365papers for May 5, 2017
What’s it about?
Many hypotheses have been put forward to explain global glaciation that happened toward the end of the Paleozoic (started around 340-330 million years ago and ended around 290 million years ago). This paper explores the hypothesis that uplift and subsequent erosion of the ancient Hercynian orogeny (mountain belt) which once straddled the equator may have played an important role.Continue reading “Rock Weathering and its Influence on Climate – #365papers – 2017 – 125”
