Mesoproterozoic
Template:Short description Template:Distinguish Template:Infobox geologic timespan The Mesoproterozoic EraTemplate:Refn is a geologic era that occurred from Template:Ma. The Mesoproterozoic was the first era of Earth's history for which a fairly definitive geological record survives. Continents existed during the preceding era (the Paleoproterozoic), but little is known about them. The continental masses of the Mesoproterozoic were more or less the same ones that exist today, although their arrangement on the Earth's surface was different.
Major events and characteristicsEdit
The major events of this era are the breakup of the Columbia supercontinent, the formation of the Rodinia supercontinent,<ref name=ZhaoEtal2004>Template:Cite journal</ref> and the evolution of sexual reproduction.<ref name="PB-2000">Template:Cite journal</ref>
This era is marked by the further development of continental plates and plate tectonics. The supercontinent of Columbia broke up between 1500 and 1350 million years ago,<ref name=ZhaoEtal2004/> and the fragments reassembled into the supercontinent of Rodinia around 1100 to 900 million years ago, on the time boundary between the Mesoproterozoic and the subsequent Neoproterozoic.<ref name=LiEtal2008>Template:Cite journal</ref> These tectonic events were accompanied by numerous orogenies (episodes of mountain building) that included the Kibaran orogeny in Africa;<ref>Template:Cite journal</ref> the Late Ruker orogeny in Antarctica;<ref>Template:Cite news</ref> the Gothian<ref>Template:Cite book</ref> and Sveconorwegian orogenies in Europe;<ref name=Andessonetal2008>Template:Cite conference</ref> and the Picuris and Grenville orogenies in North America.<ref name="wk2007">Template:Cite journal</ref>
The era saw the development of sexual reproduction, which greatly increased the complexity of life to come and signified the start of development of true multicellular organisms.<ref name="PB-2000"/><ref name="Bai2015">Template:Cite journal</ref> Though the biota of the era was once thought to be exclusively microbial, recent finds have shown multicellular life did exist during the Mesoproterozoic.<ref>Template:Cite journal</ref><ref name="PB-2000"/> This era was also the high point of the stromatolites before they declined in the Neoproterozoic.<ref name=Allwood2009>Template:Cite journal</ref>
SubdivisionsEdit
The subdivisions of the Mesoproterozoic are arbitrary divisions based on time. They are not geostratigraphic or biostratigraphic units. The decision to base the Precambrian time scale on radiometric dating reflects the sparse nature of the fossil record, and Precambrian subdivisions of geologic time roughly reflect major tectonic cycles. It is possible that future revisions to the time scale will reflect more "natural" boundaries based on correlative geologic events.<ref name=Ogg2004>Template:Cite journal</ref>
The Mesoproterozoic is presently divided into the Calymmian (1600 to 1400 Mya) and the Ectasian (1400 to 1200 Mya), and the Stenian (1200 to 1000 Mya). The Calymmian and Ectasian were characterized by stabilization and expansion of cratonic covers and the Stenian by formation of orogenic belts.<ref name=Ogg2004/>
The time period from 1780 Ma to 850 Ma, an unofficial period based on stratigraphy rather than chronometry, named the Rodinian, is described in the geological timescale review 2012 edited by Gradstein et al.,<ref name="Gradstein_et_al_2012">Template:Cite book</ref> but Template:As of, this has not yet been officially adopted by the International Union of Geological Sciences (IUGS).