| 学名(拉丁名) | Phyllanthus |
| 中文名 | 叶下珠属 |
| 命名人 | Linn. |
| 中文科名 | 大戟科 |
| 类型 | genus |
| 拉丁科名 | Euphorbiaceae |
| 学名(拉丁名) | Phyllanthus |
| 中文名 | 叶下珠属 |
| 中文科名 | 大戟科 |
| 类型 | genus |
| 拉丁科名 | Euphorbiaceae |
| 学名(拉丁名) | Phyllanthus |
| 类型 | genus |
| 拉丁科名 | Phyllanthaceae |
| 学名(拉丁名) | Phyllanthus |
| 中文名 | 叶下珠属 |
| 类型 | genus |
| 拉丁科名 | Euphorbiaceae |
| 学名(拉丁名) | Phyllanthus |
| 中文名 | 叶下珠属 |
| 中文科名 | 大戟科 |
| 类型 | genus |
| 拉丁科名 | Euphorbiaceae |
| 学名(拉丁名) | Phyllanthus |
| 发表年份 | 1753(年) |
| 类型 | genus |
| 拉丁科名 | Phyllanthaceae |
| 学名(拉丁名) | Phyllanthus |
| 类型 | genus |
| 1 | 果实呈浆果状或核果状，干后不开裂，成熟后黑色。 (2) | |
| 1 | 果实为蒴果，干后开裂，成熟后褐色或淡棕色。 (7) | |
| 2 | 叶片基部两侧不对称；果实呈核果状；雄蕊3 (2.核果叶下珠亚属Subgen. Cicca (Linn.) Webster ) [3.余甘子组Sect. Emblica (Gaertn.) Baill.］。 | 余甘子 Phyllanthus emblica |
| 2 | 叶片基部两侧对称，果实呈浆果状；雄蕊5，稀3-4 (-6) (1.浆果叶下珠亚属Subgen. Kirganelia (Juss.) Webster)。 (3) | 浆果叶下珠亚属 Subgen. Kirganelia |
| 3 | 果4-12室[l. 异萼叶下珠组Sect. Anisonema (Juss.) Griseb.］。 (4) | 异萼叶下珠组 Sect. Anisonema |
| 3 | 果3室 (2. 白饭叶下珠组Sect. Flueggeopsis Muell. Arg.)。 (6) | 白饭叶下珠组 Sect. Flueggeopsis |
| 4 | 雄蕊3-5，花丝离生；果直径约8毫米，内有种子4颗。 | 少子叶下珠 Phyllanthus oligospermus |
| 4 | 雄蕊5，花丝3枚合生，2枚离生；果直径约6毫米，内有种子8-16颗。 (5) | 小果叶下珠 Phyllanthus reticulatus |
| 5 | 幼枝、叶和花梗均被短柔毛或微毛。 | 小果叶下珠（原变种） Phyllanthus reticulatus var. reticulatus |
| 5 | 幼枝、叶和花梗均无毛。 | 无毛小果叶下珠 Phyllanthus reticulatus var. glaher |
| 6 | 果时萼片宿存。 | 青灰叶下珠 Phyllanthus glaucus |
| 6 | 果时萼片脱落。 | 落萼叶下珠 Phyllanthus flexuosus |
| 7 | 花生于落叶的枝条中下部，1-2朵被苞片所包；苞片大于花；雄花萼片镊合状排列 (6.后生叶下珠亚属Subgen. Metaphyllanthus P. T. Li) 。 | 后生叶下珠 Phyllanthus dongfangensis |
| 7 | 花或花序生于叶腋，苞片远小于花；雄花萼片覆瓦状排列。 (8) | |
| 8 | 雄花萼片4-6，全缘。 (9) | |
| 8 | 雄花萼片4，边缘流苏状、齿状或啮蚀状［5.流萼叶下珠亚属Subgen. Eriococcus (Hassk.) Croiz. et Metc.］. (27) | 流萼叶下珠亚属 Subgen. Eriococcus |
| 9 | 雄蕊3，花丝离生 (3. 羽枝叶下珠亚属Subgen. lsocladus Webster)。 (10) | 羽枝叶下珠亚属 Subgen. lsocladus |
| 9 | 雄蕊2-4，2枚的花丝离生，3-4枚的花丝为合生 (4.叶下珠亚属Subgen. Phyllanthus)。 (12) | 叶下珠亚属 Subgen. Phyllanthus |
| 10 | 一年生草本；叶片线状披针形、长圆形或狭椭圆形，基部两侧不相等；子房有鳞片状凸起。 | 黄珠子草 Phyllanthus virgatus |
| 10 | 灌木；叶片倒卵形，间有椭圆形，基部两侧相等；子房平滑。 (11) | |
| 11 | 叶片长约2厘米；花簇生；花盘5裂，裂片近圆形。 | 麻德拉斯叶下珠 Phyllanthus maderaspatensis |
| 11 | 叶片长5-15毫米；花单生，花盘杯状，顶端浅波状。 | 滇藏叶下珠 Phyllanthus clarkei |
| 12 | 叶片下面边缘有1-3列短硬毛；子房和果有小疣状凸起 (4.叶下珠组Sect. Urinaria We. bster) 。 | 叶下珠 Phyllanthus urinaria |
| 12 | 叶片下面边缘无短硬毛；子房和果平滑。 (13) | |
| 13 | 雄花萼片5-6；雄蕊3 (5.珠子草组 Sect. Phvllanthus) (14) | 珠子草组 Sect. Phyllanthus |
| 13 | 雄花萼片4；雄蕊2。 (21) | |
| 14 | 灌木。 (15) | |
| 14 | 草本。 (19) | |
| 15 | 小枝圆柱形；雄花萼片和花盘腺体5。 | 瘤腺叶下珠 Phyllanthus myrtifolius |
| 15 | 小枝具棱；雄花萼片和花盘腺体6。 (16) | |
| 16 | 小枝常集生于茎顶或老枝条的上部；叶片基部偏斜；花丝仅基部合生。 | 水油甘 Phyllanthus parvifolius |
| 16 | 小枝均匀生于茎上或老枝条上；叶片基部两侧对称，花丝全部合生成柱状。 (17) | |
| 17 | 叶片长3-14厘米，宽1.5-3.5厘米；花组成总状或圆锥状聚伞花序，花序长2-10厘米；雌花花盘杯状，顶端多少撕裂。 | 崖县叶下珠 Phyllanthus annamensis |
| 17 | 叶片长2-20毫米，宽1-13毫米；花单生或簇生；雌花花盘坛状或盘状，顶端全缘。 (18) | |
| 18 | 叶片倒卵形或匙形，顶端钝或圆；侧脉不明显；托叶边缘有缘毛；苞片边缘撕裂；花通常单生。 | 越南叶下珠 Phyllanthus cochinchinensis |
| 18 | 叶片长圆形或披针形，顶端有尖头；侧脉明显；托叶边缘无毛；苞片边缘全缘；花4-6朵簇生。 | 西南叶下珠 Phyllanthus tsarongensis |
| 19 | 一年生草本；叶片长椭圆形；侧脉每边4-7条；萼片和雄花花盘腺体5。 | 珠子草 Phyllanthus niruri |
| 19 | 多年生草本；叶片椭圆形或倒卵形；侧脉每边约3条；萼片和雄花花盘腺体6。 (20) | 沙地叶下珠 Phyllanthus arenarius |
| 20 | 叶片近革质，长3-9毫米，宽2.5-4.5毫米。 | 沙地叶下珠（原变种） Phyllanthus arenarius var. arenarius |
| 20 | 叶片薄纸质，长1.5厘米，宽约1厘米。 | 云南沙地叶下珠 Phyllanthus arenarius var. yunnanensis |
| 21 | 子房4-6室[6. 红叶下珠组Sect. Nymphanthus (Lour.) Muell.-Arg. ]。 | 红叶下珠 Phyllanthus ruber |
| 21 | 子房3室 (7. 尖叶下珠组Sect. Eriococcoides Muell. Arg.) (22) | 尖叶下珠组 Sect. Eriococcoides |
| 22 | 一年生草本；花丝离生。 | 蜜甘草 Phyllanthus ussuriensis |
| 22 | 灌木；花丝合生。 (23) | |
| 23 | 叶片线状长圆形；花组成团伞花序。 | 落羽松叶下珠 Phyllanthus taxodiifolius |
| 23 | 叶片非线状长圆形；花单生或簇生。 (24) | |
| 24 | 叶片长4-5毫米，宽2毫米，基部偏斜；侧脉每边3条；花单生。 | 单花水油甘 Phyllanthus nanellus |
| 24 | 叶片长2-4.5厘米，宽0.7-1.7厘米，基部两侧对称；侧脉每边3-9条；花簇生。 (25) | |
| 25 | 小枝圆柱形；叶片椭圆形或卵形；侧脉每边6-9条；雄花花梗长5-7毫米。 | 隐脉叶下珠 Phyllanthus guangdongensis |
| 25 | 小枝具棱翅；叶片卵状披针形或披针形；侧脉每边3-5条；雄花花梗长1-8厘米。 (26) | |
| 26 | 花紫红色；雄花花梗长3-8厘米；雌花花梗长6-10毫米。 | 贵州叶下珠 Phyllanthus bodinieri |
| 26 | 花淡白色；雄花花梗长1-1.5厘米；雌花花梗长2-2.3厘米。 | 尖叶下珠 Phyllanthus fanchenensis |
| 27 | 雄蕊4。 (28) | |
| 27 | 雄蕊2。 (31) | |
| 28 | 子房密被皱波状或卷曲状长毛。 | 浙江叶下珠 Phyllanthus chekiangensis |
| 28 | 子房平滑或有小瘤状凸起。 (29) | |
| 29 | 枝条、叶下面、叶柄均无毛；叶片长5-17毫米，宽4-8毫米；花1-2朵腋生。 | 云泰叶下珠 Phyllanthus sootepensis |
| 29 | 枝条、叶下面、叶柄均被毛；叶片长2.5-12厘米，宽1.5-4.5厘米；花组成腋生聚伞花序。 (30) | |
| 30 | 叶片长圆形或长卵形，基部两侧略不对称；花梗被短柔毛；雄花花梗长1-1.5厘米；雌花萼片究雌花花盘与子房等高。 | 穗萼叶下珠 Phyllanthus fimbricalyx |
| 30 | 叶斜长圆状披针形，基部两侧对称；花梗无毛；雄花花梗长5毫米；雌花萼片6；雌花花盘仅达子房基部。 | 毛果叶下珠 Phyllanthus gracilipes |
| 31 | 叶片基部两侧对称；雌花花梗被短柔毛；子房和果密被柔软的皮刺。 | 刺果叶下珠 Phyllanthus forrestii |
| 31 | 叶片基部两侧不对称；雌花花梗无毛；子房和果平滑或有鳞片凸起。 (32) | |
| 32 | 花簇生；雌花萼片5；花丝基部合生。 | 海南叶下珠 Phyllanthus hainanensis |
| 32 | 花单生或组成腋生聚伞花序；雌花萼片6，花丝合生。 (33) | |
| 33 | 幼枝被微柔毛；小苞片边缘有缘毛；叶片长1.8-3厘米，宽0.8-1.3厘米；花组成聚伞花序。 | 云桂叶下珠 Phyllanthus pulcher |
| 33 | 小枝和小苞片无毛；叶片长3-13毫米，宽3-7毫米；花单生。 (34) | |
| 34 | 小枝圆柱状，通常1至数条自枝的小凸起处发出；花梗长2-8毫米；花柱基部合生。 | 云贵叶下珠 Phyllanthus franchetianus |
| 34 | 小枝具棱，均匀排成二列；花梗长1.5厘米；花柱分离。 | 细枝叶下珠 Phyllanthus leptoclados |
| 1 | Plant dioecious, with either male or female flowers; leaf blade 1-10 cm | (2) |
| 1 + | Plant monoecious, with both male and female flowers; leaf blade often less than 1 cm | (3) |
| 2 (1) | Leaf blade 1-2 × 0.6-1.3 cm; inflorescences mostly 1-flowered; male sepals 6; female pedicel 2-3 mm. (24) | P. cochinchinensis |
| 2 (1) + | Leaf blade 2.5-10 × 1.5-4 cm; inflorescences many flowered; male sepals 4; female pedicel 10-15 mm. (9) | P. gracilipes |
| 3 (1) | Fruits indehiscent, fleshy | (4) |
| 3 (1) + | Fruit a dehiscent capsule, not fleshy, brown or brownish when mature | (9) |
| 4 (3) | Leaf base oblique; fruit a drupe, pale green or yellowish white, 10-13 mm in diam.; stamens 3 or 4 | (5) |
| 4 (3) + | Leaf base symmetrical; fruit a berry, purple-black when mature, 6-10 mm in diam.; stamens (3-)5(or 6) | (6) |
| 5 (4) | Leaves linear-oblong, 0.8-2.3 × 0.15-0.6 cm; stamens 3, fused. (1) | P. emblica |
| 5 (4) + | Leaves ovate or oblong-ovate, 2.4-10 × 1.9-4.5 cm; stamens 4, free. ..... P. acidus (see note above) | (4) |
| 6 (4) | Fruits 3-celled | (7) |
| 6 (4) + | Fruits 4-12-celled | (8) |
| 7 (6) | Fruiting sepals persistent; male sepals 6; fruit ca. 10 mm in diam.. (2) | P. glaucus |
| 7 (6) + | Fruiting sepals deciduous; male sepals 5; fruit ca. 6 mm in diam.. (3) | P. flexuosus |
| 8 (6) | Stamens 4 or 5(-7), filaments all free; fruit ca. 8 mm in diam., 4-seeded. (4) | P. oligospermus |
| 8 (6) + | Stamens 5, filaments 3 connate and 2 free; fruit ca. 6 mm in diam., 8-16-seeded. (5) | P. reticulatus |
| 9 (3) | Male sepal margins fimbriate, serrulate, or erose | (10) |
| 9 (3) + | Male sepal margins entire | (18) |
| 10 (9) | Ovary with dense, rugose-undulate or curved pubescence or densely setose | (11) |
| 10 (9) + | Ovary smooth or tuberculate | (12) |
| 11 (10) | Ovary with dense, rugose-undulate or curved pubescence; leaf blade 3-7 mm wide, base oblique. (6) | P. chekiangensis |
| 11 (10) + | Ovary and fruits with very dense, soft prickles; leaf blade 6-10 mm wide, base symmetrical. (10) | P. forrestii |
| 12 (10) | Female sepals 5 | (13) |
| 12 (10) + | Female sepals 6 | (14) |
| 13 (12) | Stipules 3-5 mm; female pedicel ca. 10 mm; stamens 4. (8) | P. fimbricalyx |
| 13 (12) + | Stipules 1-1.5 mm; female pedicel 20-35 mm; stamens 2. (11) | P. hainanensis |
| 14 (12) | Stamens 4 | (15) |
| 14 (12) + | Stamens 2 | (16) |
| 15 (14) | Branchlets glabrous; female sepals 1.2-2(-3.8) mm, obscurely erose or subentire; fruiting pedicel 1-1.5(-2.5) cm. (7) | P. sootepensis |
| 15 (14) + | Branchlets rufous puberulent; female sepals ca. 3.5 mm; fruiting pedicel ca. 5 cm. (9) | P. gracilipes |
| 16 (14) | Young branchlets puberulent; leaf blade 18-30 × 8-13 mm; inflorescence a bisexual axillary fascicle, usually with several male and 1 female flowers. (12) | P. pulcher |
| 16 (14) + | Branchlets glabrous; leaf blade 3-13 × 3-7 mm; inflorescence 1-flowered | (17) |
| 17 (16) | Branchlets terete, glabrous; pedicels 2-8 mm; styles connate at base. (13) | P. franchetianus |
| 17 (16) + | Branchlets angular, minutely papillate along upper side; pedicels 10-15 mm; styles free. (14) | P. leptoclados |
| 18 (9) | Stamens 3, filaments ± free | (19) |
| 18 (9) + | Stamens 2-4, filaments 2 free, others connate | (21) |
| 19 (18) | Shrubs; leaf blades thinly papery or membranous; male disk cup-shaped. (17) | P. clarkei |
| 19 (18) + | Herbs, branching mainly near base; leaf blades leathery or thinly leathery; male disk of separate glands | (20) |
| 20 (19) | Leaves ± distichous; stems usually ascending; female pedicel ca. 5 mm, disk orbicular, undivided; capsule with scalelike protuberances. (15) | P. virgatus |
| 20 (19) + | Leaves spiral; stems spreading; female pedicel 1.5-2 mm, disk of separate glands; capsule smooth. (16) | P. maderaspatensis |
| 21 (18) | Leaf blade margin hispidulous; ovary and fruits tuberculate. (18) | P. urinaria |
| 21 (18) + | Leaf blade not hispidulous; ovary and fruits smooth | (22) |
| 22 (21) | Male sepals 5 or 6; stamens 3 | (23) |
| 22 (21) + | Male sepals 4; stamens 2 | (29) |
| 23 (22) | Herbs | (24) |
| 23 (22) + | Shrubs | (25) |
| 24 (23) | Perennial herbs; leaf blade elliptic or obovate, lateral veins 3 pairs; male sepals and disk glands 6. (19) | P. arenarius |
| 24 (23) + | Annual herbs; leaf blade oblong-elliptic, lateral veins 4-7 pairs; male sepals and disk glands 5. (20) | P. amarus |
| 25 (23) | Branchlets terete; male sepals and disk glands 5. (21) | P. myrtifolius |
| 25 (23) + | Branchlets angular; male sepals and disk glands 6 | (26) |
| 26 (25) | Branchlets usually clustered at apex of erect main stem; leaf blade base oblique; filaments connate at base only. (22) | P. rheophyticus |
| 26 (25) + | Branchlets more evenly distributed along main stems; leaf blade base symmetrical; filaments connate into a column | (27) |
| 27 (26) | Leaf blade 3-14 × 1.5-3.5 cm; inflorescences on specialized racemelike leafless shoots, 2-10 cm; female disk cup-shaped, apex ± lacerate. (23) | P. pachyphyllus |
| 27 (26) + | Leaf blade 0.2-2 × 0.1-1.3 mm; inflorescence 1-flowered or a 4-6-flowered fascicle, subtended by normal leaves; female disk urceolate or disk-shaped, apex entire | (28) |
| 28 (27) | Leaf blade obovate or spatulate, apex obtuse or rounded, lateral veins obscure; stipule margins ciliate; bract margins lacerate; flowers usually solitary. (24) | P. cochinchinensis |
| 28 (27) + | Leaf blade oblong or lanceolate, apex apiculate, lateral veins prominent; stipule margins glabrous; bract margins entire; flowers 4-6-fascicled. (25) | P. tsarongensis |
| 29 (22) | Branchlets, petioles, ovary, and fruits with stellate tufts of brown hairs; ovary 4-6-celled. (26) | P. tsiangii |
| 29 (22) + | Branchlets, petioles, ovary, and fruits glabrous; ovary 3-celled | (30) |
| 30 (29) | Annual herbs; stamen filaments free. (27) | P. ussuriensis |
| 30 (29) + | Shrubs; stamen filaments connate | (31) |
| 31 (30) | Leaf blade linear-oblong; flowers in glomerules. (28) | P. taxodiifolius |
| 31 (30) + | Leaf blade not linear-oblong; flowers solitary or fascicled | (32) |
| 32 (31) | Leaf blade 4-5 × ca. 2 mm, base oblique; flowers solitary. (29) | P. nanellus |
| 32 (31) + | Leaf blade 20-45 × 7-17 mm, base symmetrical; flowers fascicled | (33) |
| 33 (32) | Branchlets terete; leaf blade elliptic-ovate, lateral veins 6-9 pairs; male pedicels 5-7 mm. (30) | P. guangdongensis |
| 33 (32) + | Branchlets angular-winged; leaf blade ovate-lanceolate or lanceolate, lateral veins 3-5 pairs; male pedicels 1-8 cm | (34) |
| 34 (33) | Sepals purple; male pedicels 0.3-0.8 cm; female pedicels 0.6-1 cm. (31) | P. bodinieri |
| 34 (33) + | Sepals whitish; male pedicels 1-1.5 cm; female pedicels 2-2.3 cm. (32) | P. fangchengensis |
一年至多年生草木，灌木，少数为乔木；无乳汁。单叶，互生，通常在小枝上排成2列，呈羽状复叶状，全缘，羽状脉，具短柄；托叶2枚，小，着生于叶柄基部两侧，常早落。花通常小、单性，雌雄同株或异株，单生、簇生或组成聚伞、团伞、总状或圆锥花序；花梗纤细；无花瓣；雄花：萼片（2-）3-6，离生，1-2轮，覆瓦状排列；花盘通常分裂为离生且与萼片互生的腺体3-6枚；雄蕊2-6，花丝离生或合生成柱状，花药2室，外向，药室平行、基部叉开或完全分离，纵裂或横裂，药隔不明显；无退化雌蕊；雌花：萼片与雄花的同数或较多；花盘腺体通常小，离生或合生呈环状或坛状，围绕子房；子房通常3室，稀4-12室，每室有胚珠2颗，花柱与子房室同数，分离或合生，顶端全缘或2裂，直立、伸展或下弯。蒴果，稀浆果或核果状，通常扁球形，成熟后常开裂3个2裂的分果爿；种子三棱形，种皮平滑或有网纹，无假种皮和种阜。染色体基数x＝13。约600种，主要分布于世界热带及亚热带地区，少数为北温带地区。我国有33种，4变种；云南产20种，1变种。本属被很多学者认为是一个不自然的类群，Brunel 把它分为13个亚属，Holm-Nielsen 将它分为10个亚属。近年国外有的学者将珠子木属 Phyllanthodendron 及一些曾是单立的类群并入本属，广义的叶下珠属则有约833种。
11.叶下珠属*——Phyllanthus Linn.
Linn. Sp. Pl. 1981. 1753; Muell. Arg. in DC. Prodr. 15 (2): 274. 1866; emend. ——Niruri Adans. Fam. Pl. 2: 356. 1763.——Urinaria Medic. M alvenlam. 80. 1787. ——Diasperus Kuntze, Rev. Gen. 2: 596. 1891.
灌木或草本，少数为乔木；无乳汁。单叶，互生，通常在侧枝上排成2例，呈羽状复叶状，全缘；羽状脉；具短柄；托叶2，小，着生于叶柄基部两侧，常早落。花通常小、单性，雌雄同株或异株，单生、簇生或组成聚伞、团伞、总状或圆锥花序；花梗纤细；无花瓣；雄花：萼片（2-) 3-6，离生，1-2轮，覆瓦状排列；花盘通常分裂为离生，且与萼片互生的腺体3-6枚；雄蕊2-6，花丝离生或合生成柱状，花药2室，外向，药室平行、基部叉开或完全分离，纵裂、斜裂或横裂，药隔不明显；无退化雌蕊；雌花：萼片与雄花的同数或较多；花盘腺体通常小，离生或合生呈环状或坛状，围绕子房；子房通常3室，稀4-12室，每室有胚珠2颗，花柱与子房室同数，分离或合生，顶端全缘或2裂，直立、伸展或下弯。蒴果，通常基顶压扁呈扁球形，成熟后常开裂3个2裂的分果爿，中轴通常宿存；种子三棱形，种皮平滑或有网纹，无假种皮和种阜。染色体基数x＝13。
约600种，主要分布于世界热带及亚热带地区，少数为北温带地区。我国产33种，4变种，主要分布于长江以南各省区。
本属模式种：珠子草 PhyIIanthus niruri Linn。
本属花粉形态多样，有3-5孔沟型、多孔沟型、多合沟孔型及散孔型等，萌发孔的形状，与构造、位置、数目等均有差异。
| Sample Name: | Bitterfeld_Hauptflöz(F) | Formation: | |
| Age: | Epoch (to): | Miocene~ | |
| Stage: | ~ | Contributer: | |
| Ecology: | Climate: | ||
|
|
|||
| locality name: | Bitterfeld_Hauptflöz(F) | Province/State: | |
| Continents: | county: | ||
| country: | Germany | longitude-decimal degrees: | |
| latitude-decimal degrees: | elevation [m]: | ||
| Notes: | |||
| Bitterfeld_Hauptflöz(F)-Mai and Walther, 1991 | |||
| title: | Die oligozänen und untermiozänen Floren Nordwest-Sachsens und des Bitterfelder Raumes. | ||
| Year: | 1991 | Type: | |
| Volume: | 38 | Issue: | |
| Pages: | 201p | Publisher: | |
| Location of publisher: | General: | ||
| Authors: | Mai, H.D. and Walther, H | ||
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) |
||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
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 |
||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
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 |
| Sample Name: | Chernoluch, lignite | Formation: | |
| Age: | Epoch (to): | Miocene~Miocene | |
| Stage: | ~ | Contributer: | |
| Ecology: | Climate: | ||
|
|
|||
| locality name: | Chernoluch | Province/State: | Omsk |
| Continents: | Europe | county: | Irtysh River |
| country: | Russian Federation | longitude-decimal degrees: | 73.016667 |
| latitude-decimal degrees: | 55.216667 | elevation [m]: | |
| Notes: | |||
| Western Siberia-Dorofeev, 1963 | |||
| title: | Tretichnye Flory Zapadnoi Sibiri (Tertiary Floras of Western Siberia) | ||
| Year: | 1963 | Type: | book |
| Volume: | Issue: | ||
| Pages: | 1-343 | Publisher: | |
| Location of publisher: | General: | ||
| Authors: | P. I. Dorofeev | ||
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) |
||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
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 |
||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
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 |
| Sample Name: | Chernoluch, Miocene Sands | Formation: | |
| Age: | Epoch (to): | Miocene~Miocene | |
| Stage: | ~ | Contributer: | |
| Ecology: | Climate: | ||
|
|
|||
| locality name: | Chernoluch | Province/State: | Omsk |
| Continents: | Europe | county: | Irtysh River |
| country: | Russian Federation | longitude-decimal degrees: | 73.016667 |
| latitude-decimal degrees: | 55.216667 | elevation [m]: | |
| Notes: | |||
| Western Siberia-Dorofeev, 1963 | |||
| title: | Tretichnye Flory Zapadnoi Sibiri (Tertiary Floras of Western Siberia) | ||
| Year: | 1963 | Type: | book |
| Volume: | Issue: | ||
| Pages: | 1-343 | Publisher: | |
| Location of publisher: | General: | ||
| Authors: | P. I. Dorofeev | ||
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) |
||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
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 |
||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
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 |
| Sample Name: | Compass Forest, Tym River, Sample 3 | Formation: | |
| Age: | Epoch (to): | Oligocene~ | |
| Stage: | Chattian~ | Contributer: | |
| Ecology: | Climate: | ||
|
|
|||
| locality name: | Compass Forest | Province/State: | Tomsk |
| Continents: | county: | ||
| country: | Russian Federation | longitude-decimal degrees: | 81 |
| latitude-decimal degrees: | 59.05 | elevation [m]: | |
| Notes: | |||
| Western Siberia-Dorofeev, 1963 | |||
| title: | Tretichnye Flory Zapadnoi Sibiri (Tertiary Floras of Western Siberia) | ||
| Year: | 1963 | Type: | book |
| Volume: | Issue: | ||
| Pages: | 1-343 | Publisher: | |
| Location of publisher: | General: | ||
| Authors: | P. I. Dorofeev | ||
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) |
||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
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 |
||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||||
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 |
| Sample Name: | Compass Forest, Tym River, Sample 4 | Formation: | |
| Age: | Epoch (to): | Oligocene~ | |
| Stage: | Chattian~ | Contributer: | |
| Ecology: | Climate: | ||
|
|
|||
| locality name: | Compass Forest | Province/State: | Tomsk |
| Continents: | county: | ||
| country: | Russian Federation | longitude-decimal degrees: | 81 |
| latitude-decimal degrees: | 59.05 | elevation [m]: | |
| Notes: | |||
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