Difference between revisions of "Template:Graphical timeline/testcases"
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imported>Hike395 (correct Hangenberg) |
imported>Hike395 (test Echinoderms without right annotations) |
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| Line 988: | Line 988: | ||
|note4-remove-arrow=yes | |note4-remove-arrow=yes | ||
|note4-nudge-left=0.1 | |note4-nudge-left=0.1 | ||
| + | |caption=Axis scale: millions of years ago. | ||
| + | |||
| + | |bar24-from=-513 | ||
| + | |bar24-to=-501 | ||
| + | |bar24-left=0.81 | ||
| + | |bar24-right=0.83 | ||
| + | |bar24-colour=#13a | ||
| + | |bar25-from=-497 | ||
| + | |bar25-left=0.77 | ||
| + | |bar25-right=0.87 | ||
| + | |bar25-colour=#13a | ||
| + | |note5=[[Carpoid]]s | ||
| + | |note5-colour=#13a | ||
| + | |note5-at=-500 | ||
| + | |note5-remove-arrow=yes | ||
| + | |note5-nudge-left=5.5 | ||
| + | |||
| + | }} | ||
| + | {{clear}} | ||
| + | |||
| + | {{Test case|_format=columns|_collapsible=yes|_title=No right annotations| | ||
| + | |help=off | ||
| + | |link-to=Early_Echinoderms_graphical_timeline | ||
| + | |||
| + | |title=Early Echinoderms (?) | ||
| + | |||
| + | |from=-570 | ||
| + | |to=-498 | ||
| + | |height=28 | ||
| + | |width=7.8 | ||
| + | |scale-increment=5 | ||
| + | |||
| + | <!--Æons--> | ||
| + | |legend1=[[Neoproterozoic]] | ||
| + | :(last [[Era_%28geology%29{{!}}era]] of the [[Precambrian]]) | ||
| + | |legend1-colour={{period color|Neoproterozoic}} | ||
| + | |||
| + | |bar1-to=-542 | ||
| + | |bar1-left=.0 | ||
| + | |bar1-right=.1 | ||
| + | |bar1-colour={{period color|Neoproterozoic}} | ||
| + | |||
| + | |||
| + | |legend2=[[Palæozoic]] | ||
| + | :(first era of the [[Phanerozoic]]) | ||
| + | |legend2-colour={{period color|paleozoic}} | ||
| + | |bar2-from=-542 | ||
| + | |bar2-left=0 | ||
| + | |bar2-right=.1 | ||
| + | |bar2-colour={{period color|Palæozoic}} | ||
| + | |||
| + | |||
| + | <!--Periods--> | ||
| + | |||
| + | |bar3-to=-542 | ||
| + | |bar3-left=.1 | ||
| + | |bar3-colour={{period color|ediacaran}} | ||
| + | |bar3-border-width=.0 | ||
| + | |bar3-text='''[[Ediacaran]]''' | ||
| + | |bar3-nudge-down=2 | ||
| + | |||
| + | |bar4-text='''[[Cambrian]]''' | ||
| + | |bar4-from=-542 | ||
| + | |bar4-left=.1 | ||
| + | |bar4-colour={{period color|cambrian series 1}} | ||
| + | |bar4-border-width=0.1 | ||
| + | |||
| + | |bar5-from=-542 | ||
| + | |bar5-to=-513 | ||
| + | |bar5-left=0.1 | ||
| + | |bar5-colour= | ||
| + | |bar5-text='''L''' | ||
| + | |bar5-nudge-left=3 | ||
| + | |bar5-nudge-up=0.5 | ||
| + | |||
| + | |bar6-from=-513 | ||
| + | |bar6-to=-501 | ||
| + | |bar6-left=0.1 | ||
| + | |bar6-colour={{period color|cambrian series 2}} | ||
| + | |bar6-text='''M''' | ||
| + | |bar6-border-width=0.08 | ||
| + | |bar6-nudge-left=3 | ||
| + | |||
| + | |bar7-left=0.1 | ||
| + | |bar7-from=-501 | ||
| + | |bar7-colour={{period color|cambrian series 4}} | ||
| + | |bar7-text='''U''' | ||
| + | |bar7-nudge-left=3 | ||
| + | |||
| + | |bar9-left=.99 | ||
| + | |bar9-right=1 | ||
| + | |bar9-colour=#000000 | ||
| + | |||
| + | |bar10-left=.09 | ||
| + | |bar10-right=.1 | ||
| + | |bar10-colour=#000000 | ||
| + | |||
| + | <!--Events--> | ||
| + | |bar8-from=-530 | ||
| + | |bar8-to=-520 | ||
| + | |bar8-left=.95 | ||
| + | |bar8-right=1.05 | ||
| + | |bar8-colour=#dd0000 | ||
| + | |||
| + | <!--Organisms--> | ||
| + | |bar22-from=-513 | ||
| + | |bar22-to=-528 | ||
| + | |bar22-left=0.82 | ||
| + | |bar22-right=.92 | ||
| + | |bar22-colour=#770 | ||
| + | |note3=''[[Helicoplacus]]''<br>(approx.) | ||
| + | |note3-at=-530 | ||
| + | |note3-colour=#777700 | ||
| + | |note3-nudge-left=6.9 | ||
| + | |note3-remove-arrow=yes | ||
| + | |||
| + | |bar21-from=-560 | ||
| + | |bar21-to=-542 | ||
| + | |bar21-left=0.85 | ||
| + | |bar21-right=0.95 | ||
| + | |bar21-colour=#077 | ||
| + | |note2=''[[Arkarua]]''<br>(approx.) | ||
| + | |note2-at=-550 | ||
| + | |note2-colour=#077 | ||
| + | |note2-remove-arrow=yes | ||
| + | |note2-nudge-left=5.8 | ||
| + | |||
| + | |bar23-from=-558 | ||
| + | |bar23-to=-542 | ||
| + | |bar23-left=0.77 | ||
| + | |bar23-right=0.87 | ||
| + | |bar23-colour=#070 | ||
|caption=Axis scale: millions of years ago. | |caption=Axis scale: millions of years ago. | ||
Revision as of 21:36, 10 January 2021
| 42px | 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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| No right annotations | ||||
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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.