Political Science homework help

Provide a 10 pages analysis while answering the following question: Hyper Thermal Events and Climate Change. Prepare this assignment according to the guidelines found in the APA Style Guide. An abstract is required. The essay introduces the Hyperthermal event such as the Paleocene-Eocene Thermal Maximum, Ordovician-Silurian extinction, The Pliocene, and climate change. Paleocene-Eocene Thermal Maximum, Ordovician-Silurian extinction, The Pliocene are the events used throughout the essay to represent many Hyperthermal events. Paleocene-Eocene Thermal Maximum, Ordovician-Silurian extinction, The Pliocene is the most common and impacted the ecosystem. The report evaluates the similarities and differences between Hyperthermal events and the present’s climate change (Kürschner, 2008). It further gives the advantages and disadvantages of using Hyperthermal events as analogs for the present climate change.Introduction&nbsp.&nbsp.&nbsp.&nbsp.&nbsp.&nbsp.&nbsp.&nbsp.&nbsp.&nbsp.&nbsp. The present climate change being experienced in different parts of the world results from global warming. Climate change results from the continuous emulsification of light carbon into the environment resulting from man and the environment’s interaction. Climate change is currently because of global warming (Pagani, 2010).&nbsp.&nbsp.&nbsp.&nbsp.&nbsp.&nbsp.&nbsp.&nbsp.&nbsp.&nbsp.&nbsp. Global warming has a definition as a rise in atmospheric temperatures because of increased greenhouse gases in the ozone layer. There are various causes of global warmings, such as carbon gases released in the manufacturing industry, wildfires, deforestation because of urbanization, and miss, ions from nuclear plants (Kürschner, 2008).The present climate change results from a gradual increase in the atmospheric temperatures, while aro. In contrast, five million years ago, climate change resulted from the rapid release of large carbon dioxide volumes into the atmosphere, leading to extreme temperatures (Pagani, 2010). This resulted from the hyperthermal events taking place in the ocean and the terrestrial parts of the earth. Hyperthermal activities such as the Paleocene-Eocene Thermal &nbsp.&nbsp.&nbsp.Maximum (PETM) resulted in increasing ease of global temperatures by approximately 5% and eight. In contrast, Ordovician-Silurian extinction, The Pliocene resulted from an extreme reduction in the atmospheric temperatures. Hyperthermal events lead to complete alteration of different weather, patterns which influenced a lot in the distribution of the animals across the world (Seki, 2010).&nbsp.&nbsp.&nbsp.&nbsp.&nbsp.&nbsp.&nbsp.&nbsp.&nbsp.&nbsp.&nbsp. The Paleocene-Eocene Thermal Maximum (PETM) was a duration in which h natural increase in atmospheric temperatures occurred because of the rapid release of carbon dioxide gas into the atmosphere. The Paleocene-Eocene Thermal Maximum occurred around fifty-five years ago.&nbsp.