Difference between revisions of "Template:Geologic time scale"

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imported>Art Carlson
m (just a comma to remove ambiguity)
imported>The Banner
m (WPCleaner (v1.10) Repaired link to disambiguation page - (You can help) - Appalachian)
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|rowspan="2" style="background:#b3e3ee"| [[Lopingian]]
 
|rowspan="2" style="background:#b3e3ee"| [[Lopingian]]
 
| [[Changhsingian]]
 
| [[Changhsingian]]
|rowspan="9"| [[Landmass]]es unite into [[supercontinent]] [[Pangaea]], creating the [[Appalachian]]s. End of Permo-Carboniferous glaciation. [[Synapsida|Synapsid]] [[Reptilia|reptile]]s ([[pelycosaur]]s and [[therapsid]]s) become plentiful, while [[parareptile]]s and [[temnospondyli|temnospondyl]] [[Amphibia|amphibian]]s remain common. In the mid-Permian, [[coal]]-age flora are replaced by [[Conifer cone|cone]]-bearing [[gymnosperm]]s (the first true [[seed plants]]) and by the first true [[moss]]es. [[Beetles]] and [[Fly|flies]] evolve. Marine life flourishes in warm shallow reefs; [[Productida|productid]] and [[Spiriferida|spiriferid]] brachiopods, bivalves, [[foraminifera|foram]]s, and [[orthocerid|ammonoid]]s all abundant. [[Permian-Triassic extinction event]] occurs 251 [[Year#SI_prefix_multipliers|Ma]]: 95% of life on Earth becomes extinct, including all [[trilobite]]s, [[graptolite]]s, and [[blastoid]]s. [[Ouachita Orogeny|Ouachita]] and [[Innuitian orogeny|Innuitian orogenies]] in North America. [[Uralian orogeny]] in Europe/Asia tapers off. [[Altai Mountains|Altaid]] orogeny in Asia. [[Hunter-Bowen Orogeny]] on [[Australia (Continent)|Australian Continent]] begins (c. 260–225 [[Year#SI_prefix_multipliers|Ma]]), forming the [[MacDonnell Ranges]].
+
|rowspan="9"| [[Landmass]]es unite into [[supercontinent]] [[Pangaea]], creating the [[Appalachian Mountains|Appalachian]]s. End of Permo-Carboniferous glaciation. [[Synapsida|Synapsid]] [[Reptilia|reptile]]s ([[pelycosaur]]s and [[therapsid]]s) become plentiful, while [[parareptile]]s and [[temnospondyli|temnospondyl]] [[Amphibia|amphibian]]s remain common. In the mid-Permian, [[coal]]-age flora are replaced by [[Conifer cone|cone]]-bearing [[gymnosperm]]s (the first true [[seed plants]]) and by the first true [[moss]]es. [[Beetles]] and [[Fly|flies]] evolve. Marine life flourishes in warm shallow reefs; [[Productida|productid]] and [[Spiriferida|spiriferid]] brachiopods, bivalves, [[foraminifera|foram]]s, and [[orthocerid|ammonoid]]s all abundant. [[Permian-Triassic extinction event]] occurs 251 [[Year#SI_prefix_multipliers|Ma]]: 95% of life on Earth becomes extinct, including all [[trilobite]]s, [[graptolite]]s, and [[blastoid]]s. [[Ouachita Orogeny|Ouachita]] and [[Innuitian orogeny|Innuitian orogenies]] in North America. [[Uralian orogeny]] in Europe/Asia tapers off. [[Altai Mountains|Altaid]] orogeny in Asia. [[Hunter-Bowen Orogeny]] on [[Australia (Continent)|Australian Continent]] begins (c. 260–225 [[Year#SI_prefix_multipliers|Ma]]), forming the [[MacDonnell Ranges]].
 
|style="background:#b3e3ee"| 253.8 ±&nbsp;0.7<sup>*</sup>
 
|style="background:#b3e3ee"| 253.8 ±&nbsp;0.7<sup>*</sup>
 
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Revision as of 04:44, 14 February 2012

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