Difference between revisions of "Template:Geologic time scale"

From blackwiki
Jump to navigation Jump to search
imported>Thomas-1770
m (Very minor edit. Just like the last one, I noticed that a space was missing after many links, also. All edits are of the type: "linkword" changed to "link word".)
imported>Thomas-1770
m (Found a few more missing spaces. Type: "link,link" changed to "link, link".)
Line 79: Line 79:
 
|rowspan="4" style="background:#eaad43"| [[Eocene]]
 
|rowspan="4" style="background:#eaad43"| [[Eocene]]
 
| [[Priabonian]]
 
| [[Priabonian]]
|rowspan="4"| [[Greenhouse and Icehouse Earth|Moderate, cooling climate]].  Archaic [[mammal]]s (e.g. [[Creodont]]s, [[Condylarth]]s,[[Uintatheriidae|Uintatheres]], etc) flourish and continue to develop during the epoch. Appearance of several "modern" mammal families. Primitive [[Cetacea|whales]] diversify.  First [[grass]]es. Reglaciation of Antarctica and formation of its [[ice cap]]; [[Azolla event]] triggers [[ice age]], and the [[Greenhouse and Icehouse Earth|Icehouse Earth]] climate that would follow it to this day, from the settlement and decay of [[seafloor]] [[algae]] drawing in massive amounts of atmospheric [[carbon dioxide]]<ref name="atmospheric-carbon-dioxide" />, lowering it from 3800 [[parts per million|ppmv]] down to 650 ppmv. End of [[Laramide Orogeny|Laramide]] and [[Sevier orogeny|Sevier Orogenies]] of the [[Rocky Mountains]] in North America. [[Orogeny]] of the [[Alps]] in Europe begins. [[Hellenic Orogeny]] begins in Greece and [[Aegean Sea]].
+
|rowspan="4"| [[Greenhouse and Icehouse Earth|Moderate, cooling climate]].  Archaic [[mammal]]s (e.g. [[Creodont]]s, [[Condylarth]]s, [[Uintatheriidae|Uintatheres]], etc) flourish and continue to develop during the epoch. Appearance of several "modern" mammal families. Primitive [[Cetacea|whales]] diversify.  First [[grass]]es. Reglaciation of Antarctica and formation of its [[ice cap]]; [[Azolla event]] triggers [[ice age]], and the [[Greenhouse and Icehouse Earth|Icehouse Earth]] climate that would follow it to this day, from the settlement and decay of [[seafloor]] [[algae]] drawing in massive amounts of atmospheric [[carbon dioxide]]<ref name="atmospheric-carbon-dioxide" />, lowering it from 3800 [[parts per million|ppmv]] down to 650 ppmv. End of [[Laramide Orogeny|Laramide]] and [[Sevier orogeny|Sevier Orogenies]] of the [[Rocky Mountains]] in North America. [[Orogeny]] of the [[Alps]] in Europe begins. [[Hellenic Orogeny]] begins in Greece and [[Aegean Sea]].
 
|style="background:#eaad43"| 38.0
 
|style="background:#eaad43"| 38.0
 
|-
 
|-
Line 330: Line 330:
 
|rowspan="3" style="background:#fbb4bd"| [[Late Ordovician|Upper]]
 
|rowspan="3" style="background:#fbb4bd"| [[Late Ordovician|Upper]]
 
| [[Hirnantian]]
 
| [[Hirnantian]]
|rowspan="7"| [[Invertebrate]]s diversify into many new types (e.g., long [[orthoconic|straight-shelled]] [[orthocerida|cephalopods]]). Early [[coral]]s, articulate [[brachiopod]]s (''Orthida'', ''Strophomenida'', etc.), [[Bivalvia|bivalves]], [[nautiloid]]s, [[trilobite]]s,[[ostracod]]s, [[bryozoa]], many types of [[echinoderms]] ([[crinoid]]s, [[Cystoidea|cystoids]], [[Asteroidea|starfish]], etc.), branched [[graptolite]]s, and other taxa all common. [[Conodont]]s (early [[plankton]]ic [[vertebrate]]s) appear. First [[Embryophyte|green plant]]s and [[fungus|fungi]] on land. Ice age at end of period.
+
|rowspan="7"| [[Invertebrate]]s diversify into many new types (e.g., long [[orthoconic|straight-shelled]] [[orthocerida|cephalopods]]). Early [[coral]]s, articulate [[brachiopod]]s (''Orthida'', ''Strophomenida'', etc.), [[Bivalvia|bivalves]], [[nautiloid]]s, [[trilobite]]s, [[ostracod]]s, [[bryozoa]], many types of [[echinoderms]] ([[crinoid]]s, [[Cystoidea|cystoids]], [[Asteroidea|starfish]], etc.), branched [[graptolite]]s, and other taxa all common. [[Conodont]]s (early [[plankton]]ic [[vertebrate]]s) appear. First [[Embryophyte|green plant]]s and [[fungus|fungi]] on land. Ice age at end of period.
 
|style="background:#fbb4bd"| 445.2&nbsp;±&nbsp;1.4<sup>*</sup>
 
|style="background:#fbb4bd"| 445.2&nbsp;±&nbsp;1.4<sup>*</sup>
 
|-
 
|-
Line 423: Line 423:
 
|-
 
|-
 
|style="background:#b3b25e"| [[Orosirian]]
 
|style="background:#b3b25e"| [[Orosirian]]
|colspan="3"| The [[Earth's atmosphere|atmosphere]] becomes [[oxygen]]ic. [[Vredefort crater|Vredefort]] and [[Sudbury Basin]] asteroid impacts. Much [[orogeny]]. [[Penokean orogeny|Penokean]] and [[Trans-Hudsonian Orogeny|Trans-Hudsonian Orogenies]] in North America. Early Ruker Orogeny in Antarctica, 2000 - 1700 [[Year#SI_prefix_multipliers|Ma]]. Glenburgh Orogeny, [[Gascoyne Complex|Glenburgh Terrane]],[[Australia (Continent)|Australian Continent]] [[circa|c.]] 2005–1920 [[Year#SI prefix multipliers|Ma]]. Kimban Orogeny, [[Gawler craton]] in Australian Continent begins.
+
|colspan="3"| The [[Earth's atmosphere|atmosphere]] becomes [[oxygen]]ic. [[Vredefort crater|Vredefort]] and [[Sudbury Basin]] asteroid impacts. Much [[orogeny]]. [[Penokean orogeny|Penokean]] and [[Trans-Hudsonian Orogeny|Trans-Hudsonian Orogenies]] in North America. Early Ruker Orogeny in Antarctica, 2000 - 1700 [[Year#SI_prefix_multipliers|Ma]]. Glenburgh Orogeny, [[Gascoyne Complex|Glenburgh Terrane]], [[Australia (Continent)|Australian Continent]] [[circa|c.]] 2005–1920 [[Year#SI prefix multipliers|Ma]]. Kimban Orogeny, [[Gawler craton]] in Australian Continent begins.
 
|style="background:#b3b25e"| 2050<ref name="absolute-age" />
 
|style="background:#b3b25e"| 2050<ref name="absolute-age" />
 
|-
 
|-
Line 431: Line 431:
 
|-
 
|-
 
|style="background:#b3b25e"| [[Siderian]]
 
|style="background:#b3b25e"| [[Siderian]]
|colspan="3"| [[Oxygen catastrophe]]: [[banded iron formation]]s forms. Sleaford Orogeny on [[Australia (Continent)|Australian Continent]],[[Gawler Craton]] 2440&ndash;2420 [[Year#SI_prefix_multipliers|Ma]].
+
|colspan="3"| [[Oxygen catastrophe]]: [[banded iron formation]]s forms. Sleaford Orogeny on [[Australia (Continent)|Australian Continent]], [[Gawler Craton]] 2440&ndash;2420 [[Year#SI_prefix_multipliers|Ma]].
 
|style="background:#b3b25e"| 2500<ref name="absolute-age" />
 
|style="background:#b3b25e"| 2500<ref name="absolute-age" />
 
|-
 
|-

Revision as of 16:37, 13 March 2013

ar:قالب:المقياس الزمني الجيولوجي es:Plantilla:Escala temporal geológica hi:भूवैज्ञानिक समय-मान pt:Predefinição:Tempo geológico zh:Template:Geologic time scale