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访问统计


  总访问量
 848
  访问来源
    内部： 0
    外部： 848
    国内： 643
    国外： 205

  年访问量
 94
  访问来源
    内部： 0
    外部： 94
    国内： 79
    国外： 15

  月访问量
 30
  访问来源
    内部： 0
    外部： 30
    国内： 27
    国外： 3

访问量

访问量

1. 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 [587]
2. 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 [473]
3. Distribution of Ediacaran acanthomorphic acritarchs in the lower D.. [422]
4. 皖南新元古代冰期地层再认识 [390]
5. 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 [390]
6. 华南埃迪卡拉纪陡山沱海洋中无机碳同位素组成变化 [382]
7. 华南埃迪卡拉纪化石保存方式及其时空分布 [380]
8. Controls on fossil pyritization: Redox conditions, sedimentary org.. [378]
9. The stratigraphic complexity of the middle Ediacaran carbon isotop.. [372]
10. 蓝田生物群 [355]
11. Acanthomorphic acritarchs of the Doushantuo Formation from an uppe.. [343]
12. 埃迪卡拉纪早期“蓝田生物群”中可能的后生动物化石的系统描述 [331]
13. 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 [323]
14. Methane-derived authigenic carbonate from the lower Doushantuo For.. [323]
15. 蓝田生物群不同保存形态丘尔藻化石的成因探究 [322]
16. 埃迪卡拉纪蓝田生物群和埃迪卡拉生物群中的Flabellophyton [322]
17. Recovery of lacustrine ecosystems after the end-Permian mass extin.. [311]
18. A tale of three taphonomic modes: The Ediacaran fossil Flabellophy.. [311]
19. Evolution of Holdfast Diversity and Attachment Strategies of Ediac.. [306]
20. Integrated carbon, sulfur, and nitrogen isotope chemostratigraphy .. [302]
21. Revisiting Ediacaran sulfur isotope chemostratigraphy with in situ.. [299]
22. Quantitative Analysis of Flabellophyton from the Ediacaran Lantian.. [298]
23. A new SIMS zircon U-Pb date from the Ediacaran Doushantuo Formatio.. [295]
24. An Integrated carbon, oxygen, and strontium isotopic studies of th.. [289]
25. New Ediacara fossils preserved in marine limestone and their ecolo.. [288]
26. SYSTEMATIC DESCRIPTION OF PUTATIVE ANIMAL FOSSILS FROM THE EARLY E.. [287]
27. 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 [283]
28. Integrated study of the Doushantuo Formation in northwestern Hunan.. [279]
29. Composition and pore characteristics of black shales from the Edia.. [272]
30. Dynamic interplay of biogeochemical C, S and Ba cycles in response.. [269]
31. 皖南埃迪卡拉系蓝田组地球化学研究及其环境意义 [265]
32. Exceptional preservation of macrofossils from the Ediacaran Lantia.. [263]
33. Orbisiana linearis from the early Ediacaran Lantian Formation of S.. [246]
34. Low marine sulfate levels during the initiation of the Cryogenian .. [243]
35. The Lantian biota: A new window onto the origin and early evolutio.. [241]
36. Influence of a chromium reduction treatment in the analysis of org.. [237]
37. Taphonomic study of Chuaria fossils from the Ediacaran Lantian bio.. [228]
38. Implications for Ediacaran biological evolution from the ca. 602 M.. [216]
39. Fluctuation of shelf basin redox conditions in the early Ediacaran.. [209]
40. 复杂生物的起源和早期演化 [209]
41. 浙西邵家山埃迪卡拉纪地层的碳同位素特征及其地层对比意义 [204]
42. 宜昌埃迪卡拉系陡山沱组中—下部旋回地层学研究 [201]
43. 中国埃迪卡拉纪岩石地层划分和对比 [153]
44. A new phosphate purification method for igneous weathering profile.. [93]

下载量

1. 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]
2. 蓝田生物群 [28]
3. 华南埃迪卡拉纪陡山沱海洋中无机碳同位素组成变化 [24]
4. 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]
5. 埃迪卡拉纪蓝田生物群和埃迪卡拉生物群中的Flabellophyton [24]
6. 蓝田生物群不同保存形态丘尔藻化石的成因探究 [18]
7. 埃迪卡拉纪早期“蓝田生物群”中可能的后生动物化石的系统描述 [18]
8. 华南埃迪卡拉纪化石保存方式及其时空分布 [14]
9. 皖南新元古代冰期地层再认识 [13]
10. 皖南埃迪卡拉系蓝田组地球化学研究及其环境意义 [10]
11. Controls on fossil pyritization: Redox conditions, sedimentary org.. [9]
12. 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 [8]
13. New Ediacara fossils preserved in marine limestone and their ecolo.. [7]
14. The Lantian biota: A new window onto the origin and early evolutio.. [6]
15. 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]
16. An Integrated carbon, oxygen, and strontium isotopic studies of th.. [6]
17. 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 [6]
18. The stratigraphic complexity of the middle Ediacaran carbon isotop.. [6]
19. Acanthomorphic acritarchs of the Doushantuo Formation from an uppe.. [6]
20. Integrated carbon, sulfur, and nitrogen isotope chemostratigraphy .. [6]
21. Quantitative Analysis of Flabellophyton from the Ediacaran Lantian.. [5]
22. Orbisiana linearis from the early Ediacaran Lantian Formation of S.. [5]
23. Exceptional preservation of macrofossils from the Ediacaran Lantia.. [5]
24. Taphonomic study of Chuaria fossils from the Ediacaran Lantian bio.. [4]
25. 中国埃迪卡拉纪岩石地层划分和对比 [4]
26. 复杂生物的起源和早期演化 [4]
27. Fluctuation of shelf basin redox conditions in the early Ediacaran.. [3]
28. Methane-derived authigenic carbonate from the lower Doushantuo For.. [3]
29. Revisiting Ediacaran sulfur isotope chemostratigraphy with in situ.. [3]
30. SYSTEMATIC DESCRIPTION OF PUTATIVE ANIMAL FOSSILS FROM THE EARLY E.. [2]
31. A new SIMS zircon U-Pb date from the Ediacaran Doushantuo Formatio.. [2]
32. Recovery of lacustrine ecosystems after the end-Permian mass extin.. [2]
33. Distribution of Ediacaran acanthomorphic acritarchs in the lower D.. [2]
34. Dynamic interplay of biogeochemical C, S and Ba cycles in response.. [2]
35. Composition and pore characteristics of black shales from the Edia.. [1]
36. A tale of three taphonomic modes: The Ediacaran fossil Flabellophy.. [1]
37. 浙西邵家山埃迪卡拉纪地层的碳同位素特征及其地层对比意义 [1]
38. 宜昌埃迪卡拉系陡山沱组中—下部旋回地层学研究 [1]
39. Evolution of Holdfast Diversity and Attachment Strategies of Ediac.. [1]
40. Implications for Ediacaran biological evolution from the ca. 602 M.. [1]
41. Integrated study of the Doushantuo Formation in northwestern Hunan.. [1]
42. A new phosphate purification method for igneous weathering profile.. [1]