User:Benniboi01/testcases

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Cambrian

{{User:Benniboi01 |after=[[Ordovician]] |before=[[Ediacaran]] |captionpaleo=A map of the world as it appeared during the Stage 2 epoch of the mid-Cambrian. (520 ma) |celestialbody=earth |co2=4500 |containedin=*[[Paleozoic]] 
*[[Phanerozoic]] |longrange=yes |lowerdef=Appearance of the [[Trace fossil|Ichnofossil]] ''[[Treptichnus pedum]]'' |lowergsspacceptdate=1992 |lowergssplocation=<span class="geo-inline"><span class="plainlinks nourlexpansion load-gadget" data-gadget="WikiMiniAtlas">[https://geohack.toolforge.org/geohack.php?pagename=User:Benniboi01/testcases&params=47.0762_N_55.8310_W_ <span class="geo-nondefault"><span class="geo-dms" title="Maps, aerial photos, and other data for this location"><span class="latitude">47°04′34″N</span> <span class="longitude">55°49′52″W</span></span></span><span class="geo-multi-punct">&#xfeff; / &#xfeff;</span><span class="geo-default"><span class="geo-dec" title="Maps, aerial photos, and other data for this location">47.0762°N 55.8310°W</span><span style="display:none">&#xfeff; / <span class="geo">47.0762; -55.8310</span></span></span>]</span></span> |mappaleo=File:Scotese 520 ma.png |name=Cambrian |nameacceptdate=1994 |o2=12.5 |proposedby=[[Adam Sedgwick]], 1835 |rockunit=system |sealevel=Rising steadily from 4m to 90m^[1] |setabovecolor=Cambrian |status=Accepted by the ICS |stratotype=[[Fortune Head|Fortune Head section]], [[Newfoundland]], [[Canada]] |subdivisions=[[#Subdivisions|See Text]] |temp=21 |timeend=485.4 |timeinterval=period |timeline=Cambrian |timestart=538.8 |upperdef=First appearance of the [[conodont]] species ''[[Iapetognathus fluctivagus]]'' |uppergsspacceptdate=2000 |uppergssplocation=<span class="geo-inline"><span class="plainlinks nourlexpansion load-gadget" data-gadget="WikiMiniAtlas">[https://geohack.toolforge.org/geohack.php?pagename=User:Benniboi01/testcases&params=49.6829_N_57.9653_W_ <span class="geo-nondefault"><span class="geo-dms" title="Maps, aerial photos, and other data for this location"><span class="latitude">49°40′58″N</span> <span class="longitude">57°57′55″W</span></span></span><span class="geo-multi-punct">&#xfeff; / &#xfeff;</span><span class="geo-default"><span class="geo-dec" title="Maps, aerial photos, and other data for this location">49.6829°N 57.9653°W</span><span style="display:none">&#xfeff; / <span class="geo">49.6829; -57.9653</span></span></span>]</span></span> |usage=Global ([[International Commission on Stratigraphy|ICS]])}}

Paleogeography in the Ediacaran was dominated by the final stages of the breakup of the Supercontinent Rodinia, and saw the assembly of a new supercontinent, Gondwana, at its end. While it is generally agreed that these events occurred during this time, specifics pertaining to the location of continental fragments and the timing of certain events in relation to each other vary wildly depending upon the model used, due to lacking paleomagnetic data. The opening of the Iapetus Ocean began around 610 Ma^[2]

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Official ICS Subdivisions of geologic time.
Axis scale: millions of years ago.

Arenig

{{User:Benniboi01 |celestialbody=earth |lowerdef=First appearance of ''[[Tetragraptus approximatus]]'' |name=Arenig |proposedby=[[Adam Sedgwick]], 1847 |rockunit=stage |timeend=471.8 |timeinterval=age |timestart=478.6 |usage=Regional |usedby=<span class="flagicon">[[File:Flag of the United Kingdom.svg|23x15px|border |alt=|link=]]</span>[[United Kingdom]]}}

Paleogeography in the Ediacaran was dominated by the final stages of the breakup of the Supercontinent Rodinia, and saw the assembly of a new supercontinent, Gondwana, at its end. While it is generally agreed that these events occurred during this time, specifics pertaining to the location of continental fragments and the timing of certain events in relation to each other vary wildly depending upon the model used, due to lacking paleomagnetic data. The opening of the Iapetus Ocean began around 610 Ma^[3]

User:Benniboi01/testcases

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Palaeontology

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Official ICS Subdivisions of geologic time.
Axis scale: millions of years ago.

Chaotian

{{User:Benniboi01 |name=Chaotian |proposedby=C., Zahnle, K. J., Sleep, N. H., and Nisbet, E. G., 2010 |rockunit=erathem |timeend=4404 |timeinterval=era |timeline=Eons |timestart=4568 |topbartype=long |usage=Proposed subdivision of the [[Hadean]] [[Eon]]}}

Paleogeography in the Ediacaran was dominated by the final stages of the breakup of the Supercontinent Rodinia, and saw the assembly of a new supercontinent, Gondwana, at its end. While it is generally agreed that these events occurred during this time, specifics pertaining to the location of continental fragments and the timing of certain events in relation to each other vary wildly depending upon the model used, due to lacking paleomagnetic data. The opening of the Iapetus Ocean began around 610 Ma^[4]

User:Benniboi01/testcases

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Palaeontology

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Official ICS Subdivisions of geologic time.
Axis scale: millions of years ago.

Nectarian

{{User:Benniboi01 |accessible=yes |celestialbody=moon |manualabovecolor=rgb(228, 83, 18) |name=Nectarian |rockunit=system |timeend=3850 |timeinterval=period |timeline=Lunar periods |timestart=3920 |topbartype=lunar}}

Paleogeography in the Ediacaran was dominated by the final stages of the breakup of the Supercontinent Rodinia, and saw the assembly of a new supercontinent, Gondwana, at its end. While it is generally agreed that these events occurred during this time, specifics pertaining to the location of continental fragments and the timing of certain events in relation to each other vary wildly depending upon the model used, due to lacking paleomagnetic data. The opening of the Iapetus Ocean began around 610 Ma^[5]

User:Benniboi01/testcases

This user is a participant in
WikiProject Geology.

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This user is interested in
Palaeontology

All Geologic Time

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Official ICS Subdivisions of geologic time.
Axis scale: millions of years ago.

Hadean

{{User:Benniboi01 |accessible=yes |captionreconstruction=Artist's impression of a Hadean landscape |celestialbody=earth |lowerdef=Formation of the [[Earth]] |name=Hadean |proposedby=[[Preston Cloud]], 1972 |proposedsubdivisions=* |reconstruction=File:Hadean.png |rockunit=eonothem |setabovecolor=Hadean |status=Informal |stratotype=None |synonym1='''Pre-Archean''' |synonym2='''Priscoan Period''' |synonym2ref=[[W. Brian Harland|Harland]] et al., 1989 |timeend=4031 |timeinterval=eon |timeline=eons |timestart=4567.3 |topbartype=long |upperdef=Defined chronometrically |usage=Global ([[International Commission on Stratigraphy|ICS]])}}

Paleogeography in the Ediacaran was dominated by the final stages of the breakup of the Supercontinent Rodinia, and saw the assembly of a new supercontinent, Gondwana, at its end. While it is generally agreed that these events occurred during this time, specifics pertaining to the location of continental fragments and the timing of certain events in relation to each other vary wildly depending upon the model used, due to lacking paleomagnetic data. The opening of the Iapetus Ocean began around 610 Ma^[6]

User:Benniboi01/testcases

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Ediacaran

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Official ICS Subdivisions of geologic time.
Axis scale: millions of years ago.

^ Haq, B. U.; Schutter, SR (2008). "A Chronology of Paleozoic Sea-Level Changes". Science. 322 (5898): 64–8. Bibcode:2008Sci...322...64H. doi:10.1126/science.1161648. PMID 18832639.
^ O'Brien, Tim; van der Pluijm, Ben (May 2012). "Timing of Iapetus Ocean rifting from ar geochronology of pseudotachylytes in the St. Lawrence rift system of southern Quebec". Geology. 40 (5): 443–446. doi:10.1130/G32691.1. Retrieved 2 April 2022.
^ O'Brien, Tim; van der Pluijm, Ben (May 2012). "Timing of Iapetus Ocean rifting from ar geochronology of pseudotachylytes in the St. Lawrence rift system of southern Quebec". Geology. 40 (5): 443–446. doi:10.1130/G32691.1. Retrieved 2 April 2022.
^ O'Brien, Tim; van der Pluijm, Ben (May 2012). "Timing of Iapetus Ocean rifting from ar geochronology of pseudotachylytes in the St. Lawrence rift system of southern Quebec". Geology. 40 (5): 443–446. doi:10.1130/G32691.1. Retrieved 2 April 2022.
^ O'Brien, Tim; van der Pluijm, Ben (May 2012). "Timing of Iapetus Ocean rifting from ar geochronology of pseudotachylytes in the St. Lawrence rift system of southern Quebec". Geology. 40 (5): 443–446. doi:10.1130/G32691.1. Retrieved 2 April 2022.
^ O'Brien, Tim; van der Pluijm, Ben (May 2012). "Timing of Iapetus Ocean rifting from ar geochronology of pseudotachylytes in the St. Lawrence rift system of southern Quebec". Geology. 40 (5): 443–446. doi:10.1130/G32691.1. Retrieved 2 April 2022.

[1] Haq, B. U.; Schutter, SR (2008). "A Chronology of Paleozoic Sea-Level Changes". Science. 322 (5898): 64–8. Bibcode:2008Sci...322...64H. doi:10.1126/science.1161648. PMID 18832639.

[2] O'Brien, Tim; van der Pluijm, Ben (May 2012). "Timing of Iapetus Ocean rifting from ar geochronology of pseudotachylytes in the St. Lawrence rift system of southern Quebec". Geology. 40 (5): 443–446. doi:10.1130/G32691.1. Retrieved 2 April 2022.

[3] O'Brien, Tim; van der Pluijm, Ben (May 2012). "Timing of Iapetus Ocean rifting from ar geochronology of pseudotachylytes in the St. Lawrence rift system of southern Quebec". Geology. 40 (5): 443–446. doi:10.1130/G32691.1. Retrieved 2 April 2022.

[4] O'Brien, Tim; van der Pluijm, Ben (May 2012). "Timing of Iapetus Ocean rifting from ar geochronology of pseudotachylytes in the St. Lawrence rift system of southern Quebec". Geology. 40 (5): 443–446. doi:10.1130/G32691.1. Retrieved 2 April 2022.

[5] O'Brien, Tim; van der Pluijm, Ben (May 2012). "Timing of Iapetus Ocean rifting from ar geochronology of pseudotachylytes in the St. Lawrence rift system of southern Quebec". Geology. 40 (5): 443–446. doi:10.1130/G32691.1. Retrieved 2 April 2022.

[6] O'Brien, Tim; van der Pluijm, Ben (May 2012). "Timing of Iapetus Ocean rifting from ar geochronology of pseudotachylytes in the St. Lawrence rift system of southern Quebec". Geology. 40 (5): 443–446. doi:10.1130/G32691.1. Retrieved 2 April 2022.

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