User talk:EmilyJadeski/sandbox

I plan to add more detail and more specific events to the paleocontinent page. I also plan to add how the movement of continents in Earth's past effects the global climate.

Lead:

A paleocontinent or palaeocontinent is a distinct area of continental crust that existed as a major landmass in the geological past. There have been many different landmasses throughout Earth’s time. They range in sizes, some are just a collection of small microcontinents while others are large conglomerates of crust. As time progresses and sea levels rise and fall more crust can be exposed making way for larger landmasses. The continents of the past shaped the evolution of organisms on Earth and contributed to the climate of the globe as well. As land masses break apart species are separated and that were once the same now have evolved to their new climate. The constant movement of these landmasses greatly determines the distribution of organisms on the Earth’s surface. This is evident with how similar fossils are found on completely separate continents. Also, as continents move, mountain building events (orogeny’s) occur, causing a shift in the global climate as new rock is exposed and then there is more exposed rock at higher elevations. This causes glacial ice expansion and an overall cooler global climate. Which effects the overall global climate trend of the Earth. The movement of the continents greatly changes and effects the overall dispersion of organisms throughout the world and the trend in climate throughout the Earth’s history. Examples include Laurentia, Baltica and Avalonia, which collided together during the Caledonian orogeny to form the Old Red Sandstone paleocontinent of Laurussia. This event, along with others similar to it created mountains that would soon be the foundation of glacier formation. Another example includes a collision that occurred during the late Pennsylvanian and early Permian time when there was a collision between the two continents of Tarimsky and Kirghiz-Kazakh. This collision was caused because of their askew convergence when the paleoceanic basin closed.

Peer Review
This draft lead looks solid, and the narrative is easy to follow. The 1st and 4th sources look to be the same article, however, and the 5th source appears as a directory location, which is something I've never seen here. The only other suggestion I really have is to break up the paragraph at a logical point, just for ease of reading. Otherwise, it seems like a good introduction to the topic. Jmead2 (talk) 21:40, 12 May 2017 (UTC) It’s a great start with many resources to include in the article. It would be really nice if you can have headings and sub headings for the topic that will be more effective and easy to manageJamilabaig (talk) 21:42, 17 May 2017 (UTC)

comments
This is a good topic that is also only patchily covered on wikipedia as far as I can tell. Jamila has good comments about breaking up the article into subsections (simply adding sections into existing articles. I see two places to add your work: Geologic history of Earth or Palaeography.  The Palaeography page would be the best place to discuss methods to reconstruct palaeocontinents.  The Geological history of Earth article already has a lot of specifics on paleocontinents and it may be difficult to add to that.  Answer.to.the.rock (talk) 13:09, 25 May 2017 (UTC)