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Visits

1. Interactions between Ediacaran animals and microbial mats: Insight.. [1264]
2. A uniquely preserved Ediacaran fossil with direct evidence for a q.. [1127]
3. Ediacaran seawater temperature: Evidence from inclusions of Sinian.. [700]
4. 国际地层指南― 地层分类、术语和程序(第二版) (译著) [529]
5. Diverse small spinose acritarchs from the Ediacaran Doushantuo For.. [516]
6. 蓝田生物群:一个认识多细胞生物起源和早期演化的新窗口 [483]
7. The oldest known dinoflagellates: Morphological and molecular evid.. [482]
8. 陡山沱期生物群-早期动物辐射前夕的生命 [413]
9. Palaeoceanographic redox environments for the lower Cambrian Hetan.. [392]
10. Three-dimensional phosphatic preservation of giant acritarchs from.. [390]
11. (17)O-depleted barite from two Marinoan cap dolostone sections, So.. [376]
12. Integrated chemostratigraphy of the Doushantuo Formation at the no.. [370]
13. 华南扬子地台埃迪卡拉纪中早期古海洋的演化——基于深水相沉积柱的证据 [369]
14. 皖南地区埃迪卡拉系皮园村组微体和宏体化石——兼论埃迪卡拉纪-寒武纪.. [367]
15. Carbon, sulfur, and oxygen isotope evidence for a strong depth gra.. [363]
16. A pronounced negative delta C-13 excursion in an Ediacaran success.. [359]
17. Timing the deposition of (17)O-depleted barite at the aftermath of.. [353]
18. 元古代刘老碑组Leiosphaeridia asperata膜壁的超微结构及其亲缘关系探.. [346]
19. Stratification and mixing of a post-glacial Neoproterozoic ocean: .. [337]
20. Pulsed oxidation and bioloical evolution in the Ediacaran Doushant.. [337]
21. The Neoproterozoic Quruqtagh Group in eastern Chinese Tianshan: ev.. [327]
22. Chuaria的解剖结构及其植物属性 [327]
23. Cell wall ultrastructures of the Proterozoic acritarch Leiosphaeri.. [316]
24. Ediacaran Acanthomorphic Acritarchs and Other Microfossils From Ch.. [316]
25. 华南埃迪卡拉系底部钾质斑脱岩的岩石地球化学特征及其地质意义 [315]
26. 古元古代冰期事件:山西五台地区滹沱群的碳同位素证据 [313]
27. 迄今最古老的多细胞宏体生物化石——“蓝田生物群” [304]
28. Anatomy and plant affinity of Chuaria [303]
29. 浙西北上奥陶统文昌组和堰口组沉积特征及其意义 [302]
30. Oxygen isotope composition of meltwater from a Neoproterozoic glac.. [299]
31. SHRIMP zircon U-Pb age constraints on Neoproterozoic Quruqtagh dia.. [297]
32. Carbon and sulfur isotope chemostratigraphy of the Neoproterozoic .. [292]
33. 扬子区早寒武世早期磷质小壳化石的再沉积和地层对比问题 [288]
34. 皖南早寒武世荷塘组海绵动物群 [284]
35. 华南埃迪卡拉纪陡山沱海洋中无机碳同位素组成变化 [283]
36. An O-17 record of late Neoproterozoic glaciation in the Kimberley .. [283]
37. An early Ediacaran assemblage of macroscopic and morphologically d.. [280]
38. 江西上饶朝阳磷矿新元古代晚期陡山沱组微体化石新材料 [276]
39. BASAL CAMBRIAN MICROFOSSILS FROM THE YANGTZE GORGES AREA (SOUTH CH.. [274]
40. Ediacaran delta C-13 chemostratigraphy of South China [272]
41. Repositioning the Great Unconformity at the southeastern margin of.. [272]
42. Triple oxygen isotope evidence for elevated CO(2) levels after a N.. [271]
43. 蓝田生物群 [268]
44. Systematic description and phylogenetic affinity of tubular microf.. [266]
45. The diversification and extinction of Doushantuo-Pertatataka acrit.. [265]
46. 华南埃迪卡拉纪化石保存方式及其时空分布 [262]
47. 扬子区晚震旦世动物化石新材料 [261]
48. 新元古代陡山沱期真核生物的辐射 [260]
49. Cellular and subcellular structure of neoproterozoic animal embryo.. [258]
50. 蓟县铁岭组底部硅质褐铁矿屑砂岩的地质意义 [257]
51. Rare earth elements and carbon isotope geochemistry of the Doushan.. [257]
52. 皖南新元古代两次冰期事件 [256]
53. Towards an Ediacaran Time Scale: Problems, Protocols, and Prospect.. [256]
54. New constraints on the ages of neoproterozoic glaciations in south.. [254]
55. 贵州瓮安—开阳地区陡山沱期含磷岩系的大型球形绿藻化石 [253]
56. 南沱冰期锰矿的起源和时代 [252]
57. 宜昌峡东地区埃迪卡拉系陡山沱组疑源类化石新材料及其生物地层学意义 [251]
58. 湘鄂西奥陶纪宝塔组灰岩网纹构造成因及沉积环境探讨 [248]
59. Carbon isotope profiles and their correlation across the Neoproter.. [248]
60. Towering sponges in an Early Cambrian Lagerstatte: Disparity betwe.. [247]
61. New Ediacara fossils preserved in marine limestone and their ecolo.. [247]
62. 湖北南漳地区晚震旦世高家山期微化石的新发现——兼论南江上升运动的地.. [245]
63. Sponge fossil assemblage from the Early Cambrian Hetang Formation .. [244]
64. 最古老的沟鞭藻:来自山西永济中元古代晚期的化石和分子生物学证据 [244]
65. Carbon Isotope Development in the Ordovician of the Yangtze Gorges.. [243]
66. The stratigraphic complexity of the middle Ediacaran carbon isotop.. [242]
67. Paleoproterozoic glaciation: Evidence from carbon isotope record o.. [239]
68. 湖北宜昌埃迪卡拉系陡山沱组天柱山卵囊胞——Tianzhushania的新认识 [239]
69. Sedimentary constraints on the duration of the Marinoan Oxygen-17 .. [238]
70. YANGTZIRAMULUS ZHANGI NEW GENUS AND SPECIES, A CARBONATE-HOSTED MA.. [236]
71. 中国埃迪卡拉纪综合地层和时间框架 [234]
72. 滇东早寒武世梅树村期浅色粘土岩层的地球化学特征和地质意义 [233]
73. Comment on "Fossilized Nuclei and Germination Structures Identify .. [233]
74. An Integrated carbon, oxygen, and strontium isotopic studies of th.. [233]
75. Phosphatized acanthomorphic acritarchs and related microfossils fr.. [231]
76. 湖北保康陡山沱组磷酸盐化微体化石组合 [230]
77. 瓮安生物群 [230]
78. Late Proterozoic tubular fossils from the Doushantuo Formation of .. [229]
79. 湘西王村剖面寒武系花桥组浊积岩特征及其大地构造意义 [227]
80. 湖北峡东地区九龙湾剖面震旦系陡山沱组微体化石的新发现 [227]
81. 新元古代“雪球事件”和早期真核生物辐射 [227]
82. Palaeontology - Undressing and redressing Ediacaran embryos [226]
83. Exceptional preservation of macrofossils from the Ediacaran Lantia.. [225]
84. 蓝田生物群不同保存形态丘尔藻化石的成因探究 [223]
85. Transient marine euxinia at the end of the terminal Cryogenian gla.. [223]
86. Cambrian sections at dadoushan near duibian, jiangshan, western Zh.. [222]
87. Quantitative evaluation of the biostratigraphic distribution of ac.. [221]
88. 湖北宜昌樟村坪陡山沱组微体化石新资料 [221]
89. Controls on fossil pyritization: Redox conditions, sedimentary org.. [221]
90. Cell differentiation and germ-soma separation in Ediacaran animal .. [218]
91. Methane-derived authigenic carbonate from the lower Doushantuo For.. [218]
92. 新元古代大塘坡组黑色页岩中的甲藻甾烷及其生物学意义(英文) [215]
93. Was the Ediacaran Shuram Excursion a globally synchronized early d.. [215]
94. Phosphatized biotas from the Neoproterozoic Doushantuo Formation o.. [214]
95. 扬子地台新元古代陡山沱期磷酸盐化生物群 [214]
96. The Weng’an biota and the Ediacaran radiation of multicellular eu.. [214]
97. Problematic macrofossils from Ediacaran successions in the North C.. [213]
98. Integrated carbon, sulfur, and nitrogen isotope chemostratigraphy .. [212]
99. 通过C_(27)/C_(29)甾烷和有机碳同位素来判断早古生代和前寒武纪的烃源.. [211]
100. Late Ediacaran trackways produced by bilaterian animals with paire.. [211]

Downloads

1. A uniquely preserved Ediacaran fossil with direct evidence for a q.. [177]
2. The oldest known dinoflagellates: Morphological and molecular evid.. [56]
3. Diverse small spinose acritarchs from the Ediacaran Doushantuo For.. [56]
4. 国际地层指南― 地层分类、术语和程序(第二版) (译著) [51]
5. Palaeoceanographic redox environments for the lower Cambrian Hetan.. [48]
6. Three-dimensional phosphatic preservation of giant acritarchs from.. [44]
7. Towering sponges in an Early Cambrian Lagerstatte: Disparity betwe.. [43]
8. Triple oxygen isotope evidence for elevated CO(2) levels after a N.. [42]
9. Systematic description and phylogenetic affinity of tubular microf.. [42]
10. 华南扬子地台埃迪卡拉纪中早期古海洋的演化——基于深水相沉积柱的证据 [40]
11. Sponge fossil assemblage from the Early Cambrian Hetang Formation .. [39]
12. 扬子区早寒武世早期磷质小壳化石的再沉积和地层对比问题 [39]
13. The Neoproterozoic Quruqtagh Group in eastern Chinese Tianshan: ev.. [38]
14. 古元古代冰期事件:山西五台地区滹沱群的碳同位素证据 [37]
15. The diversification and extinction of Doushantuo-Pertatataka acrit.. [35]
16. Ediacaran seawater temperature: Evidence from inclusions of Sinian.. [35]
17. (17)O-depleted barite from two Marinoan cap dolostone sections, So.. [34]
18. New constraints on the ages of neoproterozoic glaciations in south.. [34]
19. Tube structure and original composition of Sinotubulites: shelly f.. [31]
20. 元古代刘老碑组Leiosphaeridia asperata膜壁的超微结构及其亲缘关系探.. [30]
21. Ediacaran delta C-13 chemostratigraphy of South China [29]
22. Cell wall ultrastructures of the Proterozoic acritarch Leiosphaeri.. [29]
23. 皖南新元古代两次冰期事件 [29]
24. 湖北峡东地区九龙湾剖面震旦系陡山沱组微体化石的新发现 [29]
25. SHRIMP zircon U-Pb age constraints on Neoproterozoic Quruqtagh dia.. [28]
26. 扬子区晚震旦世动物化石新材料 [27]
27. A pronounced negative delta C-13 excursion in an Ediacaran success.. [27]
28. 蓝田生物群 [27]
29. Cellular and subcellular structure of neoproterozoic animal embryo.. [26]
30. Chuaria的解剖结构及其植物属性 [26]
31. 皖南早寒武世荷塘组海绵动物群 [26]
32. Rare helical spheroidal fossils from the Doushantuo Lagerstatte: E.. [25]
33. 湘鄂西奥陶纪宝塔组灰岩网纹构造成因及沉积环境探讨 [25]
34. 湖北宜昌埃迪卡拉系陡山沱组天柱山卵囊胞——Tianzhushania的新认识 [25]
35. Stratification and mixing of a post-glacial Neoproterozoic ocean: .. [24]
36. 华南埃迪卡拉纪陡山沱海洋中无机碳同位素组成变化 [24]
37. 瓮安陡山沱组磷块岩中球状绿藻化石繁殖机制的发现(英文) [24]
38. 蓝田生物群:一个认识多细胞生物起源和早期演化的新窗口 [24]
39. 湖北保康陡山沱组磷酸盐化微体化石组合 [23]
40. 湖北南漳地区晚震旦世高家山期微化石的新发现——兼论南江上升运动的地.. [23]
41. 通过C_(27)/C_(29)甾烷和有机碳同位素来判断早古生代和前寒武纪的烃源.. [23]
42. Carbon Isotope Development in the Ordovician of the Yangtze Gorges.. [22]
43. Anatomy and plant affinity of Chuaria [22]
44. 江西上饶朝阳磷矿新元古代晚期陡山沱组微体化石新材料 [22]
45. 扬子地台新元古代陡山沱期磷酸盐化生物群 [22]
46. 皖南地区埃迪卡拉系皮园村组微体和宏体化石——兼论埃迪卡拉纪-寒武纪.. [22]
47. 南沱冰期锰矿的起源和时代 [21]
48. 湘西王村剖面寒武系花桥组浊积岩特征及其大地构造意义 [21]
49. An early Ediacaran assemblage of macroscopic and morphologically d.. [20]
50. 新元古代大塘坡组黑色页岩中的甲藻甾烷及其生物学意义(英文) [20]
51. 蓟县铁岭组底部硅质褐铁矿屑砂岩的地质意义 [20]
52. 湖北宜昌樟村坪陡山沱组微体化石新资料 [19]
53. Comment on "Fossilized Nuclei and Germination Structures Identify .. [19]
54. Carbon isotope development in the Ordovician of the Yangtze Gorges.. [19]
55. BASAL CAMBRIAN MICROFOSSILS FROM THE YANGTZE GORGES AREA (SOUTH CH.. [18]
56. An O-17 record of late Neoproterozoic glaciation in the Kimberley .. [18]
57. Integrated chemostratigraphy of the Doushantuo Formation at the no.. [18]
58. 蓝田生物群不同保存形态丘尔藻化石的成因探究 [18]
59. Rare earth elements and carbon isotope geochemistry of the Doushan.. [17]
60. Remnants of early Archean (circa 3.5 GA) seawater in BIF from Caoz.. [16]
61. 最古老的沟鞭藻:来自山西永济中元古代晚期的化石和分子生物学证据 [16]
62. 陡山沱期生物群-早期动物辐射前夕的生命 [16]
63. Timing the deposition of (17)O-depleted barite at the aftermath of.. [15]
64. Carbon, sulfur, and oxygen isotope evidence for a strong depth gra.. [15]
65. “动物胚胎”——对瓮安地区陡山沱组微体化石的错误解释 [15]
66. 浙西北上奥陶统文昌组和堰口组沉积特征及其意义 [15]
67. Paleoproterozoic glaciation: Evidence from carbon isotope record o.. [14]
68. 贵州瓮安上震旦统陡山沱组骨针状假化石 [14]
69. 云南永善肖滩早寒武世早期碳氧同位素记录 [14]
70. 贵州瓮安地区晚震旦世陡山沱期成磷事件 [14]
71. 中国震旦纪冰期和磷酸盐化化石库研究 [14]
72. 贵州瓮安—开阳地区陡山沱期含磷岩系的大型球形绿藻化石 [14]
73. Palaeontology - Undressing and redressing Ediacaran embryos [13]
74. Carbon and sulfur isotope chemostratigraphy of the Neoproterozoic .. [13]
75. Phosphatized biotas from the Neoproterozoic Doushantuo Formation o.. [13]
76. 贵州瓮安地区上震旦统碳同位素特征 [13]
77. 贵州瓮安上震旦统陡山沱组磷质似红藻石 [13]
78. 华南埃迪卡拉纪化石保存方式及其时空分布 [13]
79. Carbon isotope profiles and their correlation across the Neoproter.. [13]
80. Pulsed oxidation and bioloical evolution in the Ediacaran Doushant.. [12]
81. Quantitative evaluation of the biostratigraphic distribution of ac.. [12]
82. Late Proterozoic tubular fossils from the Doushantuo Formation of .. [12]
83. Problematic macrofossils from Ediacaran successions in the North C.. [11]
84. 贵州瓮安磷矿上震旦统陡山沱组地层和沉积环境 [11]
85. 贵州瓮安磷矿新元古代微体生物化石 [10]
86. YANGTZIRAMULUS ZHANGI NEW GENUS AND SPECIES, A CARBONATE-HOSTED MA.. [9]
87. 滇东下寒武统含磷岩系底部火山喷发事件沉积及其意义 [9]
88. 滇东早寒武世梅树村期浅色粘土岩层的地球化学特征和地质意义 [8]
89. 新元古代陡山沱期真核生物的辐射 [8]
90. Controls on fossil pyritization: Redox conditions, sedimentary org.. [8]
91. Potential global standard stratotype-sections (GSSPs) at Luoyixi, .. [8]
92. 同步辐射X射线荧光微探针技术测定太古宙条带状硅铁建造中硅质条带及包.. [7]
93. 湘鄂地区晚寒武世末至早奥陶世特马道克期层序地层与岩相古地理 [7]
94. 迄今最古老的多细胞宏体生物化石——“蓝田生物群” [7]
95. New Ediacara fossils preserved in marine limestone and their ecolo.. [7]
96. 皖南埃迪卡拉系蓝田组页岩的有机质富集与孔隙发育特征 [7]
97. The Lantian biota: A new window onto the origin and early evolutio.. [6]
98. 华南埃迪卡拉系底部钾质斑脱岩的岩石地球化学特征及其地质意义 [6]
99. An Integrated carbon, oxygen, and strontium isotopic studies of th.. [6]
100. Integrated carbon, sulfur, and nitrogen isotope chemostratigraphy .. [6]