Coal forms from the remains of seedless plants that grew in forests during the Carboniferous period. These early forests helped convert rocks into soil and paved the way for larger plants to evolve. Today, 10 plant phyla survive, including non-vascular bryophytes like mosses and liverworts, as well as vascular tracheophytes. All plants undergo alternation of generations, alternating between multicellular haploid and diploid stages.