Difference between revisions of "Template:Graphical timeline/testcases"
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imported>Hike395 (canidae test case) |
imported>Hike395 (Paleogene test case) |
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|caption='''An approximate timescale of key Triassic events.'''<br>'''Axis scale: millions of years ago.'''<br>(NOTE: The white links are for readability only. They are still clickable.)<br> | |caption='''An approximate timescale of key Triassic events.'''<br>'''Axis scale: millions of years ago.'''<br>(NOTE: The white links are for readability only. They are still clickable.)<br> | ||
}} | }} | ||
| + | {{clear}} | ||
| + | {{Test case|_format=columns|_collapsible=yes|_title=Paleogene graphical timeline| | ||
{{clear}} | {{clear}} | ||
| + | |help=off | ||
| + | |||
| + | | link-to=Paleogene_graphical_timeline | ||
| + | | title=Key events in the Paleogene | ||
| + | |title-colour={{period color|Paleogene}} | ||
| + | |||
| + | |from=-68.85 | ||
| + | |to=-20.18 | ||
| + | |height=45 | ||
| + | |width=7.5 | ||
| + | |plot-colour=#000000 | ||
| + | |||
| + | <!--Eras--> | ||
| + | |||
| + | |bar1-to=-66 | ||
| + | |bar1-text=<span style="line-height:10px;display:block;">'''[[Mesozoic|M<br/>Z]]'''</span> | ||
| + | |bar1-nudge-down=0.3 | ||
| + | |bar1-right=.1 | ||
| + | |bar1-colour={{period color|mesozoic}} | ||
| + | |||
| + | |bar2-from=-66 | ||
| + | |bar2-text=<span style="line-height:16px;display:block;">'''[[Cenozoic|C<br/>e<br/>n<br/>o<br/>z<br/>o<br/>i<br/>c]]'''</span> | ||
| + | |bar2-nudge-down=-5 | ||
| + | |bar2-right=.1 | ||
| + | |bar2-colour={{period color|Cenozoic}} | ||
| + | |||
| + | <!--Periods--> | ||
| + | |||
| + | |bar3-to=-66 | ||
| + | |bar3-left=.11 | ||
| + | |bar3-colour={{period color|Cretaceous}} | ||
| + | |bar3-border-width=.0 | ||
| + | |bar3-text='''[[Cretaceous]]''' | ||
| + | |bar3-nudge-down=0 | ||
| + | |||
| + | |bar4-from=-66 | ||
| + | |bar4-to=-23.03 | ||
| + | |bar4-left=.11 | ||
| + | |bar4-right=.22 | ||
| + | |bar4-colour={{period color|paleogene}} | ||
| + | |bar4-border-width=.05 | ||
| + | |bar4-text=<span style="line-height:16px;display:block;">'''[[Paleogene|P<br>a<br>l<br>e<br>o<br>g<br>e<br>n<br>e]]'''</span> | ||
| + | |bar4-nudge-down=-7 | ||
| + | |||
| + | |bar5-from=-23.03 | ||
| + | |bar5-left=.11 | ||
| + | |bar5-colour={{period color|Neogene}} | ||
| + | |bar5-border-width=.0 | ||
| + | |bar5-text='''[[Neogene]]''' | ||
| + | |||
| + | <!--Series--> | ||
| + | |||
| + | |bar7-from=-66 | ||
| + | |bar7-to=-56 | ||
| + | |bar7-left=.23 | ||
| + | |bar7-right=.34 | ||
| + | |bar7-colour={{period color|paleocene}} | ||
| + | |bar7-border-width=.05 | ||
| + | |bar7-text=<span style="line-height:12px;display:block;">[[Paleocene|P<br/>a<br/>l<br/>e<br/>o<br>c<br>e<br>n<br>e]]<br/><br/></span> | ||
| + | |bar7-nudge-down=-3.5 | ||
| + | |||
| + | |bar8-from=-56 | ||
| + | |bar8-to=-33.9 | ||
| + | |bar8-left=.23 | ||
| + | |bar8-right=.34 | ||
| + | |bar8-colour={{period color|eocene}} | ||
| + | |bar8-border-width=.0 | ||
| + | |bar8-text=<span style="line-height:14px;display:block;">[[Eocene|E<br/>o<br/>c<br/>e<br/>n<br/>e]]</span> | ||
| + | |bar8-nudge-down=-3 | ||
| + | |||
| + | |bar9-from=-33.9 | ||
| + | |bar9-to=-23.03 | ||
| + | |bar9-left=.23 | ||
| + | |bar9-right=.34 | ||
| + | |bar9-colour={{period color|oligocene}} | ||
| + | |bar9-border-width=.05 | ||
| + | |bar9-text=<span style="line-height:12px;display:block;">[[Oligocene|O<br/>l<br/>i<br/>g<br>o<br>c<br>e<br>n<br>e]]</span> | ||
| + | |bar9-nudge-down=-3.1 | ||
| + | |||
| + | <!-- stages --> | ||
| + | |||
| + | |bar10-from=-66 | ||
| + | |bar10-to=-61.6 | ||
| + | |bar10-left=.35 | ||
| + | |bar10-colour={{period color|Danian}} | ||
| + | |bar10-border-width=.05 | ||
| + | |bar10-text=<span style="font-size:90%">[[Danian]]</span> | ||
| + | |bar10-nudge-down=-0.1 | ||
| + | |||
| + | |bar11-from=-61.6 | ||
| + | |bar11-to=-59.2 | ||
| + | |bar11-left=.35 | ||
| + | |bar11-colour={{period color|Selandian}} | ||
| + | |bar11-border-width=0 | ||
| + | |bar11-text=<span style="font-size:90%">[[Selandian]]<br/></span> | ||
| + | |||
| + | |bar12-from=-59.2 | ||
| + | |bar12-to=-56 | ||
| + | |bar12-left=.35 | ||
| + | |bar12-colour={{period color|Thanetian}} | ||
| + | |bar12-border-width=.05 | ||
| + | |bar12-text=<span style="font-size:90%">[[Thanetian]]</span> | ||
| + | |||
| + | |bar13-from=-56 | ||
| + | |bar13-to=-47.8 | ||
| + | |bar13-left=.35 | ||
| + | |bar13-colour={{period color|Ypresian}} | ||
| + | |bar13-border-width=.0 | ||
| + | |bar13-text=<span style="font-size:90%">[[Ypresian]]</span> | ||
| + | |||
| + | |bar14-from=-47.8 | ||
| + | |bar14-to=-41.3 | ||
| + | |bar14-left=.35 | ||
| + | |bar14-colour={{period color|Lutetian}} | ||
| + | |bar14-border-width=.05 | ||
| + | |bar14-text=<span style="font-size:90%">[[Lutetian]]</span> | ||
| + | |||
| + | |bar15-from=-41.3 | ||
| + | |bar15-to=-38 | ||
| + | |bar15-text=<span style="font-size:90%">[[Bartonian]]</span> | ||
| + | |bar15-border-width=0.0 | ||
| + | |bar15-left=0.35 | ||
| + | |bar15-colour={{period color|Bartonian}} | ||
| + | |||
| + | |bar16-from=-38 | ||
| + | |bar16-to=-33.9 | ||
| + | |bar16-text=<span style="font-size:90%">[[Priabonian]]</span> | ||
| + | |bar16-border-width=0.0 | ||
| + | |bar16-left=0.35 | ||
| + | |bar16-colour={{period color|Priabonian}} | ||
| + | |||
| + | |bar17-from=-33.9 | ||
| + | |bar17-to=-28.1 | ||
| + | |bar17-text=<span style="font-size:90%">[[Rupelian]]</span> | ||
| + | |bar17-border-width=0.05 | ||
| + | |bar17-left=0.35 | ||
| + | |bar17-colour={{period color|Rupelian}} | ||
| + | |||
| + | |bar18-from=-28.1 | ||
| + | |bar18-to=-23.03 | ||
| + | |bar18-text=<span style="font-size:90%">[[Chattian]]</span> | ||
| + | |bar18-border-width=0.0 | ||
| + | |bar18-left=0.35 | ||
| + | |bar18-colour={{period color|Chattian}} | ||
| + | |||
| + | <!--Lines--> | ||
| + | |||
| + | |bar19-left=.99 | ||
| + | |bar19-right=1 | ||
| + | |bar19-colour=#000000 | ||
| + | |||
| + | |bar28-from=-66 | ||
| + | |bar28-to=-65.9 | ||
| + | |bar28-colour=#000000 | ||
| + | |||
| + | |bar29-from=-37.9 | ||
| + | |bar29-to=-37.8 | ||
| + | |bar29-left=.34 | ||
| + | |bar29-colour=#000000 | ||
| + | |||
| + | |bar30-from=-23.08 | ||
| + | |bar30-to=-23.03 | ||
| + | |bar30-left=.11 | ||
| + | |bar30-colour=#000000 | ||
| + | |||
| + | <!--Notes--> | ||
| + | |||
| + | <!--Notes--> | ||
| + | |note1=[[Paleocene–Eocene Thermal Maximum|PETM]] | ||
| + | |note1-at=-56 | ||
| + | |note1-size=75% | ||
| + | |||
| + | |note3-at=-33.9 | ||
| + | |note3=<span style="line-height:10px; display:block;">First Antarctic [[ice-sheet|permanent ice-sheets]]<ref name=Zachos2k5>{{cite journal | ||
| + | | author1 = Zachos, J. C. | ||
| + | | author2 = Kump, L. R. | ||
| + | | year = 2005 | ||
| + | | title = Carbon cycle feedbacks and the initiation of Antarctic glaciation in the earliest Oligocene | ||
| + | | journal = Global and Planetary Change | ||
| + | | volume = 47 | ||
| + | | issue = 1 | ||
| + | | pages = 51–66 | ||
| + | | doi=10.1016/j.gloplacha.2005.01.001 | ||
| + | | bibcode=2005GPC....47...51Z | ||
| + | }}</ref></span> | ||
| + | |note3-size=75% | ||
| + | |||
| + | |note4=<span style="line-height:10px;display:block;">[[Cretaceous–Paleogene extinction event|K-Pg mass<br>extinction]]</span> | ||
| + | |note4-at=-65.8 | ||
| + | |note4-size=75% | ||
| + | |caption=An approximate timescale of key Paleogene events<br>Axis scale: millions of years ago<br> | ||
| + | }} | ||
{{Test case|_format=columns|_collapsible=yes|_title=Burgsvik beds graphical timeline| | {{Test case|_format=columns|_collapsible=yes|_title=Burgsvik beds graphical timeline| | ||
| help=off | | help=off | ||
Revision as of 03:49, 9 December 2020
| This is the template test cases page for the sandbox of Template:Graphical timeline. Script error: No such module "Purge". to update the examples. If there are many examples of a complicated template, later ones may break due to limits in MediaWiki, see the HTML comment "NewPP limit report" in the rendered page. You can also use Special:ExpandTemplates to examine the results of template uses. You can test how this page looks in the different skins with these links: |
| Devonian graphical timeline | ||||
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| Triassic graphical timeline | ||||
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| Paleogene graphical timeline | ||||
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| Burgsvik beds graphical timeline | ||||
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| Early Echinoderms graphical timeline | ||||
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| Canidae graphical timeline | ||||
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References
- ↑ Jeppsson, L.; Calner, M. (2007). "The Silurian Mulde Event and a scenario for secundo—secundo events". Earth and Environmental Science Transactions of the Royal Society of Edinburgh. 93 (02): 135–154. doi:10.1017/S0263593300000377.
- ↑ Munnecke, A.; Samtleben, C.; Bickert, T. (2003). "The Ireviken Event in the lower Silurian of Gotland, Sweden-relation to similar Palaeozoic and Proterozoic events". Palaeogeography, Palaeoclimatology, Palaeoecology. 195 (1): 99–124. doi:10.1016/S0031-0182(03)00304-3.
- ↑ Parry, S. F.; Noble, S. R.; Crowley, Q. G.; Wellman, C. H. (2011). "A high-precision U–Pb age constraint on the Rhynie Chert Konservat-Lagerstätte: time scale and other implications". Journal of the Geological Society. London: Geological Society. 168 (4): 863–872. doi:10.1144/0016-76492010-043.
- ↑ Kaufmann, B.; Trapp, E.; Mezger, K. (2004). "The numerical age of the Upper Frasnian (Upper Devonian) Kellwasser horizons: A new U-Pb zircon date from Steinbruch Schmidt(Kellerwald, Germany)". The Journal of Geology. 112 (4): 495–501. Bibcode:2004JG....112..495K. doi:10.1086/421077.
- ↑ Algeo, T. J. (1998). "Terrestrial-marine teleconnections in the Devonian: links between the evolution of land plants, weathering processes, and marine anoxic events". Philosophical Transactions of the Royal Society B: Biological Sciences. 353 (1365): 113–130. doi:10.1098/rstb.1998.0195.
- ↑ Widmann, Philipp; Bucher, Hugo; Leu, Marc; Vennemann, Torsten; Bagherpour, Borhan; Schneebeli-Hermann, Elke; Goudemand, Nicolas; Schaltegger, Urs (2020). "Dynamics of the Largest Carbon Isotope Excursion During the Early Triassic Biotic Recovery". Frontiers in Earth Science. 8 (196): 1–16. doi:10.3389/feart.2020.00196.
- ↑ McElwain, J. C.; Punyasena, S. W. (2007). "Mass extinction events and the plant fossil record". Trends in Ecology & Evolution. 22 (10): 548–557. doi:10.1016/j.tree.2007.09.003. PMID 17919771.
- ↑ |note5-nudge-down=1 Retallack, G. J.; Veevers, J.; Morante, R. (1996). "Global coal gap between Permian–Triassic extinctions and middle Triassic recovery of peat forming plants". GSA Bulletin. 108 (2): 195–207. doi:10.1130/0016-7606(1996)108<0195:GCGBPT>2.3.CO;2. Retrieved 2007-09-29.
- ↑ Payne, J. L.; Lehrmann, D. J.; Wei, J.; Orchard, M. J.; Schrag, D. P.; Knoll, A. H. (2004). "Large Perturbations of the Carbon Cycle During Recovery from the End-Permian Extinction". Science. 305 (5683): 506–9. doi:10.1126/science.1097023. PMID 15273391.
- ↑ Zachos, J. C.; Kump, L. R. (2005). "Carbon cycle feedbacks and the initiation of Antarctic glaciation in the earliest Oligocene". Global and Planetary Change. 47 (1): 51–66. Bibcode:2005GPC....47...51Z. doi:10.1016/j.gloplacha.2005.01.001.