Brown Moss of breeding birds at the site and many visitors, including wetland birds, such as Canada goose, mallard and great crested grebe. During the summer, froglets and dragonflies are found around water and woodland edges. Brown Moss is a flat site that was created at the end of the last Ice Age, over 10,000 years ago. As glaciers retreated, pools were formed by the stranded ice rocks, forming kettle holes Peat is still being created and Sphagnum moss – which is very important for the creation of peat – is found in abundance. This site contains a number of circular walks
Moss Antarctica and Russia, and a case is put forwards for Carboniferous mosses. It has further been claimed that tube-like fossils from the Silurian are the macerated remains of moss calyptræ. Mosses also appear to evolve 2–3 times slower than ferns, gymnosperms and angiosperms. Recent research show that ancient moss could explain why the Ordovician ice ages occurred. When the ancestors of today's moss started to spread on land 470 million years ago, they absorbed CO from the atmosphere and extracted minerals by secreting organic acids that dissolved the rocks they were growing on. These chemically altered rocks in turn reacted