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Pollen studies show a regressive loss of rainforest plants and an increase in grassland species, maize, and weeds from the time of Maya occupation to about AD 1000.[167] Additional evidence comes from studies of lake-bottom sediments, which show that sedimentation rates increased greatly during the Classic Maya Period, and the character of the sediments indicates that they resulted from erosion caused by deforestation.[168] Regeneration of the forests would have been inhibited if, as some studies suggest, the climate in this period was unusually dry.[169] Recent studies, however, have not found archaeological evidence for drought in the southern lowland Maya heartland.[170] The forests were largely gone by the Late Classic Period