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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 [489]
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 [377]
3. 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 [319]
4. 华南埃迪卡拉纪陡山沱海洋中无机碳同位素组成变化 [289]
5. 蓝田生物群 [274]
6. 皖南新元古代冰期地层再认识 [272]
7. 华南埃迪卡拉纪化石保存方式及其时空分布 [272]
8. 埃迪卡拉纪蓝田生物群和埃迪卡拉生物群中的Flabellophyton [261]
9. Quantitative Analysis of Flabellophyton from the Ediacaran Lantian.. [258]
10. 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 [257]
11. New Ediacara fossils preserved in marine limestone and their ecolo.. [250]
12. The stratigraphic complexity of the middle Ediacaran carbon isotop.. [250]
13. 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 [246]
14. An Integrated carbon, oxygen, and strontium isotopic studies of th.. [239]
15. Controls on fossil pyritization: Redox conditions, sedimentary org.. [237]
16. Methane-derived authigenic carbonate from the lower Doushantuo For.. [230]
17. Exceptional preservation of macrofossils from the Ediacaran Lantia.. [229]
18. 蓝田生物群不同保存形态丘尔藻化石的成因探究 [227]
19. Integrated carbon, sulfur, and nitrogen isotope chemostratigraphy .. [221]
20. Distribution of Ediacaran acanthomorphic acritarchs in the lower D.. [220]
21. SYSTEMATIC DESCRIPTION OF PUTATIVE ANIMAL FOSSILS FROM THE EARLY E.. [213]
22. Acanthomorphic acritarchs of the Doushantuo Formation from an uppe.. [213]
23. Orbisiana linearis from the early Ediacaran Lantian Formation of S.. [205]
24. The Lantian biota: A new window onto the origin and early evolutio.. [202]
25. 皖南埃迪卡拉系蓝田组地球化学研究及其环境意义 [197]
26. A new SIMS zircon U-Pb date from the Ediacaran Doushantuo Formatio.. [197]
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 [186]
28. Recovery of lacustrine ecosystems after the end-Permian mass extin.. [178]
29. Fluctuation of shelf basin redox conditions in the early Ediacaran.. [177]
30. A tale of three taphonomic modes: The Ediacaran fossil Flabellophy.. [175]
31. Composition and pore characteristics of black shales from the Edia.. [171]
32. Evolution of Holdfast Diversity and Attachment Strategies of Ediac.. [135]
33. Revisiting Ediacaran sulfur isotope chemostratigraphy with in situ.. [124]
34. 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 [114]
35. 宜昌埃迪卡拉系陡山沱组中—下部旋回地层学研究 [97]
36. Dynamic interplay of biogeochemical C, S and Ba cycles in response.. [97]
37. Influence of a chromium reduction treatment in the analysis of org.. [90]
38. Implications for Ediacaran biological evolution from the ca. 602 M.. [90]
39. Low marine sulfate levels during the initiation of the Cryogenian .. [72]
40. Quantitative Analysis of Flabellophyton from the Ediacaran Lantian.. [71]
41. Integrated study of the Doushantuo Formation in northwestern Hunan.. [59]
42. Taphonomic study of Chuaria fossils from the Ediacaran Lantian bio.. [32]

Downloads

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 [27]
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 [13]
9. 皖南新元古代冰期地层再认识 [12]
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.. [8]
12. New Ediacara fossils preserved in marine limestone and their ecolo.. [7]
13. 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]
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. Integrated carbon, sulfur, and nitrogen isotope chemostratigraphy .. [6]
18. Quantitative Analysis of Flabellophyton from the Ediacaran Lantian.. [5]
19. Orbisiana linearis from the early Ediacaran Lantian Formation of S.. [5]
20. Exceptional preservation of macrofossils from the Ediacaran Lantia.. [5]
21. 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 [5]
22. The stratigraphic complexity of the middle Ediacaran carbon isotop.. [5]
23. Acanthomorphic acritarchs of the Doushantuo Formation from an uppe.. [5]
24. Fluctuation of shelf basin redox conditions in the early Ediacaran.. [3]
25. Methane-derived authigenic carbonate from the lower Doushantuo For.. [3]
26. SYSTEMATIC DESCRIPTION OF PUTATIVE ANIMAL FOSSILS FROM THE EARLY E.. [2]
27. A new SIMS zircon U-Pb date from the Ediacaran Doushantuo Formatio.. [2]
28. Recovery of lacustrine ecosystems after the end-Permian mass extin.. [2]
29. Distribution of Ediacaran acanthomorphic acritarchs in the lower D.. [2]
30. Composition and pore characteristics of black shales from the Edia.. [1]
31. Revisiting Ediacaran sulfur isotope chemostratigraphy with in situ.. [1]
32. Dynamic interplay of biogeochemical C, S and Ba cycles in response.. [1]
33. Taphonomic study of Chuaria fossils from the Ediacaran Lantian bio.. [1]