Sunday, March 24, 2019
Evolution of Land Mammals :: essays research papers
Evolution of fetch animals THE LARGEST genetic study ever per organise to diddle when degrade full treatments and fungi first appeared on the realm has revealed a glib biological cause for two major climate events the snowball existence eras, when ice periodically covered the globe, and the era called the Cambrian Explosion, which produced the first fossils of most all major categories of animals living today. According to the authors of the study, Science, plants paved the way for the phylogeny of land animals by simultaneously increasing the percentage of oxygen in the Earths atmosphere and decreasing the percentage of carbon dioxide, a powerful glasshouse gas. "Our research shows that land plants and fungi evolved much in front than previously thought--in the beginning the Snowball Earth and Cambrian Explosion events--suggesting their presence could have had a cloggy effect on the climate and the evolution of life on Earth," says Blair Hedges, an evolutionary biologist and leader of the Penn State research team that performed the study. The researchers found that land plants had evolved on Earth by about 700 gazillion years agone and land fungi by about 1,300 million years ago--much earlier than previous estimates of around 480 million years ago, which were based on the earlier fossils of those organisms. Prior to this study, it was believed that Earths landscape at that time was covered with barren rocks harboring secret code more than some bacteria and possibly some algae. No unquestioned fossils of the earliest land plants and fungi have been found in rocks formed during the Precambrian period, says Hedges, possibly because their primitive bodies were too soft to turn into fossils.The early appearing on the land of fungi and plants suggests their plausible role in some(prenominal) the mysterious lowering of the Earths surface temperature during the series of Snowball Earth events roughly 750 million to 580 million years ago and the sudden appearance of more spic-and-span species of fossil animals during the Cambrian Explosion era roughly 530 million years ago. "Both the lowering of the Earths surface temperature and the evolution of many new types of animals could result from a decrease in atmospheric carbon dioxide and a rise in oxygen caused by presence on land of lichen fungi and plants at this time, which our research suggests," Hedges says. "An increase in land plant abundance may have occurred at the time just before the period known as the Cambrian Explosion, when the next Snowball Earth period failed to occur because temperatures did not get quite cold enough," Hedges says.
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