模板:Geologic time scale
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这是使用{{navbox}}创建的导航模板,可以在条目附录末尾使用{{Geologic time scale}}将其嵌入包含于页面中,以便为读者提供相关条目之导览。
显示状态
- 如何控制本模板的显示状态
- 使用
{{Geologic time scale|state=collapsed}}使本模板显示为折叠(隐藏)状态。 - 使用
{{Geologic time scale|state=expanded}}使本模板显示为展开(显示)状态。 - 使用
{{Geologic time scale|state=autocollapse}}使本模板仅在页面上有其他相同类型的模板时,显示为折叠(隐藏)状态。 expanded已被设为默认状态。
模板数据
<templatedata> { "params": { "state": { "label": "State", "description": "导航框的默认显示状态", "suggestedvalues": [ "collapsed", "expanded", "autocollapse" ], "suggested": true, "type": "string" } }, "description": "可放置于条目底部的导航框。" } </templatedata>
嵌入状况
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参考资料
- ↑ Paleontologists often refer to faunal stages rather than geologic (geological) periods. The stage nomenclature is quite complex. For an excellent time-ordered list of faunal stages, see The Paleobiology Database. [2006-03-19].
- ↑ 2.0 2.1 所有全球年代地层单位均由其底界的全球界线层型剖面和点位(GSSP)界定,包括长期由全球标准地层年龄(GSSA)界定的太古宇和元古宇各单位。斜体代表非正式名称或尚未命名单位的临时名称。图件及已批准GSSP的详情参见国际地层委员会官网。GSSP被标记为*,而GSSA被标记为+。
年龄值仍在不断修订;显生宇和埃迪卡拉系的单位不能由年龄界定,而只能由GSSP界定。显生宇中没有确定GSSP或精确年龄值的单位,则标注了近似年龄值(~)。 - ↑ References to the "Post-Cambrian Supereon" are not universally accepted, and therefore must be considered unofficial.
- ↑ Historically, the 新生代 has been divided up into the 第四纪 and 第三纪 sub-eras, as well as the 新近纪 and 古近纪 periods. The 2009 version of the ICS time chart recognizes a slightly extended Quaternary as well as the Paleogene and a truncated Neogene, the Tertiary having been demoted to informal status.
- ↑ 5.0 5.1 5.2 5.3 5.4 5.5 For more information on this, see the following articles: 地球大气层, 二氧化碳, Carbon dioxide in the Earth's atmosphere, global warming, 气候变迁, Image:Phanerozoic_Carbon_Dioxide.png, Image:65 Myr Climate Change.png, Image:Five Myr Climate Change.png, and Template:DF temperature
- ↑ 6.0 6.1 在北美,石炭纪被细分为 密士西必纪与宾夕法尼亚纪。
- ↑ 7.0 7.1 上石炭纪地质在欧美及中国均以盛产煤炭著名,因此便以石炭纪为此时代地层的名称,但在美国则以密士西必纪作为下石炭纪,另以宾夕法尼亚纪称上部石炭纪。[1]
- ↑ The Precambrian is also known as Cryptozoic.
- ↑ 9.0 9.1 9.2 9.3 9.4 9.5 9.6 9.7 The Proterozoic, Archean and Hadean are often collectively referred to as the Precambrian Time or sometimes, also the Cryptozoic.
- ↑ The age of the oldest measurable craton, or continental crust, is dated to 3600–3800 Ma
- ↑ Geology.wisc.edu
- ↑ Bowring, Samuel A.; Williams, Ian S. Priscoan (4.00–4.03 Ga) orthogneisses from northwestern Canada. Contributions to Mineralogy and Petrology. 1999, 134 (1): 3. Bibcode:1999CoMP..134....3B. doi:10.1007/s004100050465. The oldest rock on Earth is the Acasta Gneiss, and it dates to 4.03 Ga, located in the Northwest Territories of Canada.