学名(拉丁名) | Eupatorium japonicum |
中文名 | 白头婆 |
命名人 | Thunb. |
中文科名 | 菊科 |
拉丁属名 | Eupatorium |
类型 | species |
拉丁科名 | Compositae |
中文属名 | 泽兰属 |
学名(拉丁名) | Eupatorium japonicum |
中文名 | 白头婆 |
中文科名 | 菊科 |
拉丁属名 | Eupatorium |
类型 | species |
拉丁科名 | Compositae |
中文属名 | 泽兰属 |
学名(拉丁名) | Eupatorium japonicum |
命名人 | Thunb. (accepted name) |
拉丁属名 | Eupatorium |
类型 | species |
拉丁科名 | Asteraceae |
学名(拉丁名) | Eupatorium japonicum |
中文名 | 白头婆 |
拉丁属名 | Eupatorium |
类型 | species |
拉丁科名 | Asteraceae |
学名(拉丁名) | Eupatorium japonicum |
中文名 | 白头婆 |
中文科名 | 菊科 |
拉丁属名 | Eupatorium |
类型 | species |
拉丁科名 | Asteraceae |
中文属名 | 泽兰属 |
学名(拉丁名) | Eupatorium japonicum |
拉丁属名 | Eupatorium |
类型 | species |
拉丁科名 | Asteraceae |
Eupatorium chinense Linnaeus var. simplicifolium (Makino) Kitamura; E. chinense var. tozanense (Hayata) Kitamura; E. fortunei Turczaninow f. aureoreticulatum (Makino) Nakai; E. fortunei var. simplicifolium (Makino) Nakai; E. fortunei var. tripartitum (Makino) Nakai; E. japonicum f. aureoreticulatum Makino; E. japonicum var. dissectum Makino; E. japonicum var. simplicifolium Makino; E. japonicum var. tozanense (Hayata) Kitamura; E. japonicum var. tripartitum Makino; E. japonicum var. wallichii (Candolle) Yamamoto; E. tozanense Hayata; E. wallichii Candolle.
Herbs perennial, 50-200 cm tall. Rhizomes short, with numerous fibrous roots. Stems erect, purplish red, usually simple or corymbose synflorescence branched in upper part, white crisped-puberulent, more dense on synflorescence branches, glabrescent or sparsely hairy in lower part. Leaves opposite; petiole 0.5-2 cm, rather thick; median stem leaves elliptic, narrowly elliptic, ovate-elliptic, or lanceolate, 6-20 × 2-6.5 cm, pinnately veined, lateral veins 7-paired, abaxially prominent, base broadly or narrowly cuneate, margin sometimes 3-partite, apex acuminate; basal stem leaves withered by anthesis; upper leaves smaller, homomorphic with median leaves; both surfaces scabrid, crisped-villous or puberulent and yellow glandular, more densely hairy abaxially on veins and on petiole; margin coarsely or doubly serrate. Capitula apically densely corymbose, synflorescence usually 3-6 cm in diam., rarely forming a large compound corymbose synflorescence to 20 cm in diam. Involucre campanulate, 5-6 mm, 5-flowered; phyllaries imbricate, 3-seriate; outer phyllaries very short, lanceolate, 1-2 mm, median and inner phyllaries gradually longer, lanceolate, narrowly elliptic, or elliptic-lanceolate, 5-6 mm, green or purple-tinged, apex obtuse or rounded. Florets white, red-purple, or pink; corolla ca. 5 mm, with dense yellow glands. Achenes black-brown, elliptic, ca. 3.5 mm, 5-angled, with many yellow glands, glabrous. Pappus white, ca. 5 mm. Fl. and fr. Jun-Nov.
Grasslands on slopes, open forests, thickets, wet places, riverbanks; 100-3000 m. Anhui, Fujian, Guangdong, Guizhou, Hainan, Heilongjiang, Henan, Hubei, Jiangsu, Jiangxi, Jilin, Liaoning, Shaanxi, Shandong, Shanxi, Sichuan, Yunnan, Zhejiang [Japan, Korea].
6. 白头婆(长沙)泽兰 图版21: 1-3
Eupatorium japonicum Thunb., Fl. Jap. 307, 1784, DC., Prodr. 5: 180, 1836; Forbes et Hemsl. in Journ. Linn. Soc. Bot. 23: 403, 1888; Nakai, Fl. Koreana 2: 5, 1911; Kitam. in Act. Phytotax. Geobot. 1: 285, 1932 et in Mem. Coll. Sci. Kyoto Univ. Ser. B. 13: 284 1937; Ling in Contr. Inst. Bot. Nat. Acad. Peip. 1: 456, 1934; Hand. -Mazz., Symb. Sin. 7: 1086; 1936; Chang in Sunyats. 3: 279, 1937; 裴鉴、周太炎, 中国药用植物志 6: 图297, 1958; 裴鉴等, 江苏南部种子植物手册, 745, 1959; Ohwi, Fl. Jap. 867, 1965; S. Y. Hu in Quart. Journ. Taiwan Mus. 19: 257, 1966. ——Eupatorium wallichii DC., Prodr. 5: 179, 1836; Benth. Fl. Hongk., 172, 1861; Mattf. in Act. Hort. Gothob. 8: 78, 1933; Kitam. in Journ. Jap. Bot. 24: 79, 1949; S. Y. Hu in Quart. Journ. Taiwan Mus. 19: 259, 1966. ——Eupatorium japonicum var. simplicifolium Makino in Bot. Mag. Tokyo 23: 142, 1909. ——Eupatorium japonicum f. aureo-reticulatum Makino in Bot. Mag. 23: 90, 1909. ——Eupatorium fortunei var. simplicifolium (Makino) Nakai in Bot. Mag. Tokyo 41: 512, 1927. ——Eupatorium fortunei var. simplicifolium f. aureo-reticulatum (Makino) Nakai in Bot. Mag. Tokyo 41: 511, 1927. ——Eupatorium chinense L. var. simplicifolium (Makino) Kitam. in Journ. Jap. Bot. 24: 79, 1949; Ohwi, Fl. Jap. 867, 1956.——Eupatorium album auct. non L.: Thunb., Fl. Jap. 308, 1784. ——Eupatorium chinense auct. non L.: Komar., Fl. Manch. 3: 582, 1907.
白头婆(原变种)
var. japonicum
多年生草本,高50-200厘米。根茎短,有多数细长侧根。茎直立,下部或至中部或全部淡紫红色,基部径达1.5厘米,通常不分枝,或仅上部有伞房状花序分枝,全部茎枝被白色皱波状短柔毛,花序分枝上的毛较密,茎下部或全部花期脱毛或疏毛。叶对生,有叶柄,柄长1-2厘米,质地稍厚;中部茎叶椭圆形或长椭圆形或卵状长椭圆形或披针形,长6-20厘米,宽2-6.5厘米,基部宽或狭楔形,顶端渐尖,羽状脉,侧脉约7对,在下面突起;自中部向上及向下部的叶渐小,与茎中部叶同形,基部茎叶花期枯萎;全部茎叶两面粗涩,被皱波状长或短柔毛及黄色腺点,下面、下面沿脉及叶柄上的毛较密,边缘有粗或重粗锯齿。头状花序在茎顶或枝端排成紧密的伞房花序,花序径通常3-6厘米,少有大型复伞房花序而花序径达20厘米的。总苞钟状,长5-6毫米,含5个小花;总苞片覆瓦状排列,3层;外层极短,长1-2毫米,披针形;中层及内层苞片渐长,长5-6毫米,长椭圆形或长椭圆状披针形;全部苞片绿色或带紫红色,顶端钝或圆形。花白色或带红紫色或粉红色,花冠长5毫米,外面有较稠密的黄色腺点。瘦果淡黑褐色,椭圆状,长3.5毫米,5棱,被多数黄色腺点,无毛;冠毛白色,长约5毫米。花果期6-11月。海拔120-3000米。
产于黑龙江、吉林、辽宁、山东、山西、陕西、河南、江苏、浙江、湖北、湖南、安徽、江西、广东、四川、云南、贵州等地。生山坡草地、密疏林下、灌丛中、水湿地及河岸水旁。日本、朝鲜广为分布。
此种也有许多地方名,福建、湖南名孩儿菊,河南叫六月霜,江西叫六月雪、白花莲、麻杆消,湖北称麻婆娘。本种全草药用,性凉,消热消炎。
白头婆三裂叶变种
Eupatorium japonicum var. tripartitum Makino in Bot. Mag. Tokyo 23: 142, 1909; Kitam. in Mem. Coll. Sci. Kyoto Univ. Ser. B. 13: 285, 1937 et in Journ. Jap. Bot. 21: 51, 1947; S. Y. Hu, in Quart. Journ. Taiwan Mus. 19: 258, 1966. ——Eupatorium fortunei var. triparticum (Makino) Nakai. in Bot. Mag. Tokyo 41: 512, 1927.
叶三全裂,中裂片大,椭圆形或椭圆状披针形;产于安徽、四川。
泽兰是一个分布广变异大的一个种;日本分类学家根据日本的标本,分出了若干类群(变种与变型);在台湾的标本中,曾将叶顶端长渐尖,边缘有圆锯齿的一类分立为独立的一群(土场白头婆或白头婆土场变种 Eupatorium japonicum var. tozanense (Hayata) Kitam. in Mem. Coll. Sci. Kyoto Univ. Ser. B. 13: 286, 1937——Eupatorium tozanense Hayata, Ic. Pl. Formos. 8: 44, 1919.
Eupatorium japonicum | |||
Family Name: | Compositae | Genera name: | Eupatorium |
Species name: | japonicum | Genera status: | |
NLR: | Comments: | ||
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Sample Name: | Reuver | Formation: | |
Age: | Epoch (to): | Pliocene~ | |
Stage: | Reuverian~ | Contributer: | |
Ecology: | Climate: | ||
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locality name: | Reuver | Province/State: | Limburg |
Continents: | Europe | county: | |
country: | Netherland | longitude-decimal degrees: | 6.1 |
latitude-decimal degrees: | 51.35 | elevation [m]: | 35 |
Notes: |
Netherland-Reid and Reid, 1915 | |||
title: | THE PLIOCENE FLORAS OF THE DUTCH PRUSSIAN BORDER | ||
Year: | 1915 | Type: | |
Volume: | Issue: | ||
Pages: | Publisher: | ||
Location of publisher: | General: | ||
Authors: | CLEMENT REID, ELEANOR M. REID |
Phanerozoic |
Proterozoic |
Archean |
Hadean (informal) |
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Permian |
Carboniferous |
Devonian |
Silurian |
Ordovician |
Cambrian |
Ediacaran |
Cryogenian |
Tonian |
Stenian |
Ectasian |
Calymmian |
Statherian |
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Rhyacian |
Siderian |
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Paleocene |
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Lower |
Upper |
Middle |
Lower |
Lopingian |
Guadalupian |
Cisuralian |
Pennsylvanian-Upper |
Pennsylvanian-Middle |
Pennsylvanian-Lower |
Mississippian-Upper |
Mississippian-Middle |
Mississippian-Lower |
Upper |
Middle |
Lower |
Pridoli |
Ludlow |
Wenlock |
Llandovery |
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Middle |
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Furongian |
Series 3 |
Series 2 |
Terreneuvian |
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Upper |
"lonia" |
Calabrian |
Gelasian |
Piacenzian |
Zanclean |
Messinian |
Tortonian |
Serravallian |
Langhian |
Burdigalian |
Chattian |
Aquitanian |
Rupelian |
Priabonian |
Bartonian |
Lutetian |
Ypresian |
Thanetian |
Selandian |
Danian |
Maastrichtian |
Campanian |
Santonian |
Coniacian |
Turonian |
Cenomanian |
Albian |
Aptian |
Barremian |
Hauterivian |
Valanginian |
Berriasian |
Tithonian |
Kimmeridgian |
Oxfordian |
Callovian |
Bathonian |
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Aalenian |
Toarcian |
Pliensbachian |
Sinemurian |
Hettangian |
Rhaetian |
Norian |
Carnian |
Ladinian |
Anisian |
Olenekian |
Induan |
Changhsingian |
Wuchiapingian |
Capitanian |
Wordian |
Roadian |
Kungurian |
Artinskian |
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Asselian |
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Kasimovian |
Moscovian |
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Visean |
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Eifelian |
Emsian |
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Lochkovian |
Ludfordian |
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Telychian |
Aeronian |
Rhuddanian |
Hirnantian |
Katian |
Sandbian |
Darriwilian |
Dapingian |
Floian |
Tremadocian |
Stage 10 |
Stage 9 |
Paibian |
Guzhangian |
Drumian |
Stage 5 |
Stage 4 |
Stage 3 |
Stage 2 |
Fortunian |
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0 | 0.0117 | 0.126 | 0.781 | 1.806 | 2.588 | 3.6 | 5.332 | 7.246 | 11.608 | 13.82 | 15.97 | 20.43 | 23.03 | 28.4 ±0.1 | 33.9 ±0.1 | 37.2 ±0.1 | 40.4 ±0.2 | 48.6 ±0.2 | 55.8 ±0.2 | 58.7 ±0.2 | 61.1 | 65.5 ±0.3 | 70.6 ±0.6 | 83.5 ±0.7 | 85.8 ±0.7 | 88.6 | 93.6 ±0.8 | 99.6 ±0.9 | 112.0 ±1.0 | 125.0 ±1.0 | 130.0 ±1.5 | 133.9 | 140.2 ±3.0 | 145.5 ±4.0 | 150.8 ±4.0 | 155.6 | 161.2 ±4.0 | 164.7 ±4.0 | 167.7 ±3.5 | 171.6 ±3.0 | 175.6 ±2.0 | 183.0 ±1.5 | 189.6 ±1.5 | 196.5 ±1.0 | 199.6 ±0.6 | 203.6 ±1.5 | 216.5 ±2.0 | 228.7 | 237.0 ±2.0 | 245.9 | 249.5 | 251.0 ±0.4 | 253.8 ±0.7 | 260.4 ±0.7 | 265.8 ±0.7 | 268.0 ±0.7 | 270.6 ±0.7 | 275.6 ±0.7 | 284.4 ±0.7 | 294.6 ±0.8 | 299.0 ±0.8 | 303.4 ±0.9 | 307.2 ±1.0 | 311.7 ±1.1 | 318.1 ±1.3 | 328.3 ±1.6 | 345.3 ±2.1 | 359.2 ±2.5 | 374.5 ±2.6 | 385.3 ±2.6 | 391.8 ±2.7 | 397.5 ±2.7 | 407.0 ±2.8 | 411.2 ±2.8 | 416.0 ±2.8 | 418.7 ±2.7 | 421.3 ±2.6 | 422.9 ±2.5 | 426.2 ±2.4 | 428.2 ±2.3 | 436.0 ±1.9 | 439.0 ±1.8 | 443.7 ±1.5 | 445.6 ±1.5 | 455.8 ±1.6 | 460.9 ±1.6 | 468.1 ±1.6 | 471.8 ±1.6 | 478.6 ±1.7 | 488.3 ±1.7 | 492 | 496 | 499 | 503 | 506.5 | 510 | 515 | 521 | 528 | 542.0 ±1.0 | 635 | 850 | 1000 | 1200 | 1400 | 1600 | 1800 | 2050 | 2300 | 2500 | 2800 | 3200 | 3600 | 4000 | 4600 |
显生宇 |
元古宇 |
太古宇 |
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侏罗系 |
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石炭系 |
泥盆系 |
志留系 |
奥陶系 |
寒武系 |
埃迪卡拉系 |
成冰系 |
拉伸系 |
狭带系 |
延展系 |
盖层系 |
固结系 |
造山系 |
层侵系 |
成铁系 |
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始新统 |
古新统 |
上白垩统 |
下白垩统 |
上侏罗统 |
中侏罗统 |
下侏罗统 |
上三叠统 |
中三叠统 |
下三叠统 |
乐平统 |
瓜德鲁普统 |
乌拉尔统 |
宾夕法尼亚亚系-上 |
宾夕法尼亚亚系-中 |
宾夕法尼亚亚系-下 |
密西西比亚系-上 |
密西西比亚系-中 |
密西西比亚系-下 |
上泥盆统 |
中泥盆统 |
下泥盆统 |
普里道利统 |
罗德洛统 |
文洛克统 |
兰多维列统 |
上奥陶统 |
中奥陶统 |
下奥陶统 |
芙蓉统 |
第三统 |
第二统 |
纽芬兰统 |
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上更新统 |
“伊奥尼雅阶” |
卡拉布里雅阶 |
格拉斯阶 |
皮亚琴察阶 |
赞克尔阶 |
梅辛阶 |
托尔通阶 |
塞拉瓦尔阶 |
兰哥阶 |
布尔迪加尔阶 |
阿启坦阶 |
夏特阶 |
鲁培尔阶 |
普利亚本阶 |
巴尔通阶 |
鲁帝特阶 |
伊普里斯阶 |
坦尼特阶 |
赛兰特阶 |
丹尼阶 |
马斯特里赫特阶 |
坎潘阶 |
三冬阶 |
康尼亚克阶 |
土伦阶 |
赛诺曼阶 |
阿尔布阶 |
阿普特阶 |
巴雷姆阶 |
欧特里夫阶 |
凡兰吟阶 |
贝利阿斯阶 |
提塘阶 |
基末利阶 |
牛津阶 |
卡洛夫阶 |
巴通阶 |
巴柔阶 |
阿林阶 |
土阿辛阶 |
普林斯巴阶 |
辛涅缪尔阶 |
赫塘阶 |
瑞替阶 |
诺利阶 |
卡尼阶 |
拉丁阶 |
安尼阶 |
奥伦尼克阶 |
印度阶 |
长兴阶 |
吴家坪阶 |
卡匹敦阶 |
沃德阶 |
罗德阶 |
空谷阶 |
亚丁斯克阶 |
萨克马尔阶 |
阿瑟尔阶 |
格舍尔阶 |
卡西莫夫阶 |
莫斯科阶 |
巴什基尔阶 |
谢尔普霍夫阶 |
维宪阶 |
杜内阶 |
法门阶 |
弗拉阶 |
吉维特阶 |
艾菲尔阶 |
埃姆斯阶 |
布拉格阶 |
洛霍考夫阶 |
卢德福特阶 |
高斯特阶 |
侯墨阶 |
申伍德阶 |
特列奇阶 |
埃隆阶 |
鲁丹阶 |
赫南特阶 |
凯迪阶 |
桑比阶 |
达瑞威尔阶 |
大坪阶 |
弗洛阶 |
特马豆克阶 |
第十阶 |
第九阶 |
排碧阶 |
古丈阶 |
鼓山阶 |
第五阶 |
第四阶 |
第三阶 |
第二阶 |
幸运阶 |
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0 | 0.0117 | 0.126 | 0.781 | 1.806 | 2.588 | 3.6 | 5.332 | 7.246 | 11.608 | 13.82 | 15.97 | 20.43 | 23.03 | 28.4 ±0.1 | 33.9 ±0.1 | 37.2 ±0.1 | 40.4 ±0.2 | 48.6 ±0.2 | 55.8 ±0.2 | 58.7 ±0.2 | 61.1 | 65.5 ±0.3 | 70.6 ±0.6 | 83.5 ±0.7 | 85.8 ±0.7 | 88.6 | 93.6 ±0.8 | 99.6 ±0.9 | 112.0 ±1.0 | 125.0 ±1.0 | 130.0 ±1.5 | 133.9 | 140.2 ±3.0 | 145.5 ±4.0 | 150.8 ±4.0 | 155.6 | 161.2 ±4.0 | 164.7 ±4.0 | 167.7 ±3.5 | 171.6 ±3.0 | 175.6 ±2.0 | 183.0 ±1.5 | 189.6 ±1.5 | 196.5 ±1.0 | 199.6 ±0.6 | 203.6 ±1.5 | 216.5 ±2.0 | 228.7 | 237.0 ±2.0 | 245.9 | 249.5 | 251.0 ±0.4 | 253.8 ±0.7 | 260.4 ±0.7 | 265.8 ±0.7 | 268.0 ±0.7 | 270.6 ±0.7 | 275.6 ±0.7 | 284.4 ±0.7 | 294.6 ±0.8 | 299.0 ±0.8 | 303.4 ±0.9 | 307.2 ±1.0 | 311.7 ±1.1 | 318.1 ±1.3 | 328.3 ±1.6 | 345.3 ±2.1 | 359.2 ±2.5 | 374.5 ±2.6 | 385.3 ±2.6 | 391.8 ±2.7 | 397.5 ±2.7 | 407.0 ±2.8 | 411.2 ±2.8 | 416.0 ±2.8 | 418.7 ±2.7 | 421.3 ±2.6 | 422.9 ±2.5 | 426.2 ±2.4 | 428.2 ±2.3 | 436.0 ±1.9 | 439.0 ±1.8 | 443.7 ±1.5 | 445.6 ±1.5 | 455.8 ±1.6 | 460.9 ±1.6 | 468.1 ±1.6 | 471.8 ±1.6 | 478.6 ±1.7 | 488.3 ±1.7 | 492 | 496 | 499 | 503 | 506.5 | 510 | 515 | 521 | 528 | 542.0 ±1.0 | 635 | 850 | 1000 | 1200 | 1400 | 1600 | 1800 | 2050 | 2300 | 2500 | 2800 | 3200 | 3600 | 4000 | 4600 |
Eupatorium japonicum | |||
Family Name: | Compositae | Genera name: | Eupatorium |
Species name: | japonicum | Genera status: | |
NLR: | Comments: | ||
|
Sample Name: | Swalmen | Formation: | |
Age: | Epoch (to): | Pliocene~ | |
Stage: | Reuverian~ | Contributer: | |
Ecology: | Climate: | ||
|
locality name: | Swalmen | Province/State: | Limburg |
Continents: | Europe | county: | |
country: | Netherland | longitude-decimal degrees: | 6.03 |
latitude-decimal degrees: | 51.22 | elevation [m]: | 23 |
Notes: |
Netherland-Reid and Reid, 1915 | |||
title: | THE PLIOCENE FLORAS OF THE DUTCH PRUSSIAN BORDER | ||
Year: | 1915 | Type: | |
Volume: | Issue: | ||
Pages: | Publisher: | ||
Location of publisher: | General: | ||
Authors: | CLEMENT REID, ELEANOR M. REID |
Phanerozoic |
Proterozoic |
Archean |
Hadean (informal) |
||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
Cenozoic |
Mesozoic |
Paleozoic |
Neoproterozoic |
Mesoproterozoic |
Paleoproterozoic |
Neoarchean |
Mesoarchean |
Paleoarchean |
Eoarchean |
||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
Quaternary |
Neogene |
Paleogene |
Cretaceous |
Jurassic |
Triassic |
Permian |
Carboniferous |
Devonian |
Silurian |
Ordovician |
Cambrian |
Ediacaran |
Cryogenian |
Tonian |
Stenian |
Ectasian |
Calymmian |
Statherian |
Orosirian |
Rhyacian |
Siderian |
||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
Holocene |
Pleistocene |
Pliocene |
Miocene |
Oligocene |
Eocene |
Paleocene |
Upper |
Lower |
Upper |
Middle |
Lower |
Upper |
Middle |
Lower |
Lopingian |
Guadalupian |
Cisuralian |
Pennsylvanian-Upper |
Pennsylvanian-Middle |
Pennsylvanian-Lower |
Mississippian-Upper |
Mississippian-Middle |
Mississippian-Lower |
Upper |
Middle |
Lower |
Pridoli |
Ludlow |
Wenlock |
Llandovery |
Upper |
Middle |
Lower |
Furongian |
Series 3 |
Series 2 |
Terreneuvian |
||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
Upper |
"lonia" |
Calabrian |
Gelasian |
Piacenzian |
Zanclean |
Messinian |
Tortonian |
Serravallian |
Langhian |
Burdigalian |
Chattian |
Aquitanian |
Rupelian |
Priabonian |
Bartonian |
Lutetian |
Ypresian |
Thanetian |
Selandian |
Danian |
Maastrichtian |
Campanian |
Santonian |
Coniacian |
Turonian |
Cenomanian |
Albian |
Aptian |
Barremian |
Hauterivian |
Valanginian |
Berriasian |
Tithonian |
Kimmeridgian |
Oxfordian |
Callovian |
Bathonian |
Bajocian |
Aalenian |
Toarcian |
Pliensbachian |
Sinemurian |
Hettangian |
Rhaetian |
Norian |
Carnian |
Ladinian |
Anisian |
Olenekian |
Induan |
Changhsingian |
Wuchiapingian |
Capitanian |
Wordian |
Roadian |
Kungurian |
Artinskian |
Sakmarian |
Asselian |
Gzhelian |
Kasimovian |
Moscovian |
Bashkirian |
Serpukhovian |
Visean |
Tournaisian |
Famennian |
Frasnian |
Givetian |
Eifelian |
Emsian |
Pragian |
Lochkovian |
Ludfordian |
Gorstian |
Homerian |
Sheinwoodian |
Telychian |
Aeronian |
Rhuddanian |
Hirnantian |
Katian |
Sandbian |
Darriwilian |
Dapingian |
Floian |
Tremadocian |
Stage 10 |
Stage 9 |
Paibian |
Guzhangian |
Drumian |
Stage 5 |
Stage 4 |
Stage 3 |
Stage 2 |
Fortunian |
||||||||||||||||||
0 | 0.0117 | 0.126 | 0.781 | 1.806 | 2.588 | 3.6 | 5.332 | 7.246 | 11.608 | 13.82 | 15.97 | 20.43 | 23.03 | 28.4 ±0.1 | 33.9 ±0.1 | 37.2 ±0.1 | 40.4 ±0.2 | 48.6 ±0.2 | 55.8 ±0.2 | 58.7 ±0.2 | 61.1 | 65.5 ±0.3 | 70.6 ±0.6 | 83.5 ±0.7 | 85.8 ±0.7 | 88.6 | 93.6 ±0.8 | 99.6 ±0.9 | 112.0 ±1.0 | 125.0 ±1.0 | 130.0 ±1.5 | 133.9 | 140.2 ±3.0 | 145.5 ±4.0 | 150.8 ±4.0 | 155.6 | 161.2 ±4.0 | 164.7 ±4.0 | 167.7 ±3.5 | 171.6 ±3.0 | 175.6 ±2.0 | 183.0 ±1.5 | 189.6 ±1.5 | 196.5 ±1.0 | 199.6 ±0.6 | 203.6 ±1.5 | 216.5 ±2.0 | 228.7 | 237.0 ±2.0 | 245.9 | 249.5 | 251.0 ±0.4 | 253.8 ±0.7 | 260.4 ±0.7 | 265.8 ±0.7 | 268.0 ±0.7 | 270.6 ±0.7 | 275.6 ±0.7 | 284.4 ±0.7 | 294.6 ±0.8 | 299.0 ±0.8 | 303.4 ±0.9 | 307.2 ±1.0 | 311.7 ±1.1 | 318.1 ±1.3 | 328.3 ±1.6 | 345.3 ±2.1 | 359.2 ±2.5 | 374.5 ±2.6 | 385.3 ±2.6 | 391.8 ±2.7 | 397.5 ±2.7 | 407.0 ±2.8 | 411.2 ±2.8 | 416.0 ±2.8 | 418.7 ±2.7 | 421.3 ±2.6 | 422.9 ±2.5 | 426.2 ±2.4 | 428.2 ±2.3 | 436.0 ±1.9 | 439.0 ±1.8 | 443.7 ±1.5 | 445.6 ±1.5 | 455.8 ±1.6 | 460.9 ±1.6 | 468.1 ±1.6 | 471.8 ±1.6 | 478.6 ±1.7 | 488.3 ±1.7 | 492 | 496 | 499 | 503 | 506.5 | 510 | 515 | 521 | 528 | 542.0 ±1.0 | 635 | 850 | 1000 | 1200 | 1400 | 1600 | 1800 | 2050 | 2300 | 2500 | 2800 | 3200 | 3600 | 4000 | 4600 |
显生宇 |
元古宇 |
太古宇 |
冥古宇 (非正式) |
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新生界 |
中生界 |
古生界 |
新元古界 |
中元古界 |
古元古界 |
新太古界 |
中太古界 |
古太古界 |
始太古界 |
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第四系 |
新近系 |
古近系 |
白垩系 |
侏罗系 |
三叠系 |
三叠系 |
石炭系 |
泥盆系 |
志留系 |
奥陶系 |
寒武系 |
埃迪卡拉系 |
成冰系 |
拉伸系 |
狭带系 |
延展系 |
盖层系 |
固结系 |
造山系 |
层侵系 |
成铁系 |
||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
全新统 |
更新统 |
上新统 |
中新统 |
渐新统 |
始新统 |
古新统 |
上白垩统 |
下白垩统 |
上侏罗统 |
中侏罗统 |
下侏罗统 |
上三叠统 |
中三叠统 |
下三叠统 |
乐平统 |
瓜德鲁普统 |
乌拉尔统 |
宾夕法尼亚亚系-上 |
宾夕法尼亚亚系-中 |
宾夕法尼亚亚系-下 |
密西西比亚系-上 |
密西西比亚系-中 |
密西西比亚系-下 |
上泥盆统 |
中泥盆统 |
下泥盆统 |
普里道利统 |
罗德洛统 |
文洛克统 |
兰多维列统 |
上奥陶统 |
中奥陶统 |
下奥陶统 |
芙蓉统 |
第三统 |
第二统 |
纽芬兰统 |
||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
上更新统 |
“伊奥尼雅阶” |
卡拉布里雅阶 |
格拉斯阶 |
皮亚琴察阶 |
赞克尔阶 |
梅辛阶 |
托尔通阶 |
塞拉瓦尔阶 |
兰哥阶 |
布尔迪加尔阶 |
阿启坦阶 |
夏特阶 |
鲁培尔阶 |
普利亚本阶 |
巴尔通阶 |
鲁帝特阶 |
伊普里斯阶 |
坦尼特阶 |
赛兰特阶 |
丹尼阶 |
马斯特里赫特阶 |
坎潘阶 |
三冬阶 |
康尼亚克阶 |
土伦阶 |
赛诺曼阶 |
阿尔布阶 |
阿普特阶 |
巴雷姆阶 |
欧特里夫阶 |
凡兰吟阶 |
贝利阿斯阶 |
提塘阶 |
基末利阶 |
牛津阶 |
卡洛夫阶 |
巴通阶 |
巴柔阶 |
阿林阶 |
土阿辛阶 |
普林斯巴阶 |
辛涅缪尔阶 |
赫塘阶 |
瑞替阶 |
诺利阶 |
卡尼阶 |
拉丁阶 |
安尼阶 |
奥伦尼克阶 |
印度阶 |
长兴阶 |
吴家坪阶 |
卡匹敦阶 |
沃德阶 |
罗德阶 |
空谷阶 |
亚丁斯克阶 |
萨克马尔阶 |
阿瑟尔阶 |
格舍尔阶 |
卡西莫夫阶 |
莫斯科阶 |
巴什基尔阶 |
谢尔普霍夫阶 |
维宪阶 |
杜内阶 |
法门阶 |
弗拉阶 |
吉维特阶 |
艾菲尔阶 |
埃姆斯阶 |
布拉格阶 |
洛霍考夫阶 |
卢德福特阶 |
高斯特阶 |
侯墨阶 |
申伍德阶 |
特列奇阶 |
埃隆阶 |
鲁丹阶 |
赫南特阶 |
凯迪阶 |
桑比阶 |
达瑞威尔阶 |
大坪阶 |
弗洛阶 |
特马豆克阶 |
第十阶 |
第九阶 |
排碧阶 |
古丈阶 |
鼓山阶 |
第五阶 |
第四阶 |
第三阶 |
第二阶 |
幸运阶 |
||||||||||||||||||
0 | 0.0117 | 0.126 | 0.781 | 1.806 | 2.588 | 3.6 | 5.332 | 7.246 | 11.608 | 13.82 | 15.97 | 20.43 | 23.03 | 28.4 ±0.1 | 33.9 ±0.1 | 37.2 ±0.1 | 40.4 ±0.2 | 48.6 ±0.2 | 55.8 ±0.2 | 58.7 ±0.2 | 61.1 | 65.5 ±0.3 | 70.6 ±0.6 | 83.5 ±0.7 | 85.8 ±0.7 | 88.6 | 93.6 ±0.8 | 99.6 ±0.9 | 112.0 ±1.0 | 125.0 ±1.0 | 130.0 ±1.5 | 133.9 | 140.2 ±3.0 | 145.5 ±4.0 | 150.8 ±4.0 | 155.6 | 161.2 ±4.0 | 164.7 ±4.0 | 167.7 ±3.5 | 171.6 ±3.0 | 175.6 ±2.0 | 183.0 ±1.5 | 189.6 ±1.5 | 196.5 ±1.0 | 199.6 ±0.6 | 203.6 ±1.5 | 216.5 ±2.0 | 228.7 | 237.0 ±2.0 | 245.9 | 249.5 | 251.0 ±0.4 | 253.8 ±0.7 | 260.4 ±0.7 | 265.8 ±0.7 | 268.0 ±0.7 | 270.6 ±0.7 | 275.6 ±0.7 | 284.4 ±0.7 | 294.6 ±0.8 | 299.0 ±0.8 | 303.4 ±0.9 | 307.2 ±1.0 | 311.7 ±1.1 | 318.1 ±1.3 | 328.3 ±1.6 | 345.3 ±2.1 | 359.2 ±2.5 | 374.5 ±2.6 | 385.3 ±2.6 | 391.8 ±2.7 | 397.5 ±2.7 | 407.0 ±2.8 | 411.2 ±2.8 | 416.0 ±2.8 | 418.7 ±2.7 | 421.3 ±2.6 | 422.9 ±2.5 | 426.2 ±2.4 | 428.2 ±2.3 | 436.0 ±1.9 | 439.0 ±1.8 | 443.7 ±1.5 | 445.6 ±1.5 | 455.8 ±1.6 | 460.9 ±1.6 | 468.1 ±1.6 | 471.8 ±1.6 | 478.6 ±1.7 | 488.3 ±1.7 | 492 | 496 | 499 | 503 | 506.5 | 510 | 515 | 521 | 528 | 542.0 ±1.0 | 635 | 850 | 1000 | 1200 | 1400 | 1600 | 1800 | 2050 | 2300 | 2500 | 2800 | 3200 | 3600 | 4000 | 4600 |