Michael Wagreich

Earth and Planetary Sciences

1. Campanian 100%
2. Anthropocene 79%
3. Miocene 76%
4. Upper Cretaceous 67%
5. Late Cretaceous 58%
6. Subsidence 57%
7. Nannofossil 46%
8. Sea Level 45%
9. Tectonics 43%
10. Santonian 37%
11. Biostratigraphy 33%
12. Maastrichtian 31%
13. Holocene 31%
14. Paleoclimate 31%
15. Sandstone 31%
16. Sea Level Change 30%
17. Organic Carbon 28%
18. Paleogene 27%
19. Coniacian 26%
20. Heavy Mineral 25%
21. Flysch 24%
22. Paleoenvironment 22%
23. Paleogeography 21%
24. Stable Isotope 21%
25. Planktonic foraminifera 21%
26. Basin Evolution 21%
27. Turonian 21%
28. Pleistocene 20%
29. Eocene 20%
30. Trace Element 18%
31. Ostracod 18%
32. Cenomanian 18%
33. Red Bed 17%
34. Mudstone 16%
35. Porosity 16%
36. Carbon 14 16%
37. Depositional Environment 16%
38. Dinoflagellate Cyst 15%
39. Sedimentary Basin 14%
40. Deep Water 13%
41. Badenian 13%
42. Calcite 13%
43. Stratotype 13%
44. Turbidite 12%
45. Carbonate Platform 12%
46. Geological Time 11%
47. Climate Change 11%
48. Synclines 11%
49. Paratethys 11%
50. Trace Metal 10%