n | Reference | source | date | set | rows |
---|---|---|---|---|---|
0 | not identified yet | 21 | |||
1 | Erba, E., 1992. Middle Cretaceous calcareous nannofossils from the western Pacific (Leg 129): evidence for paleoequatorial crossings. In Larson, R.L., Lancelot, Y., et al., Proc. ODP, Sci. Results, 129: College Station, TX (Ocean Drilling Program), 189–201. | prior to 2010 | 14 | 75 |
Age(Ma) | mbsf | 0 Discorhabdus rotatorius | 1 Watznaueria britannica | 2 Cyclagelosphaera margerelii | 3 Biscutum blackii | 4 Biscutum constans | 5 Watznaueria barnesae | 6 Discorhabdus rotatorius | 7 Cyclagelosphaera deflandrei | 8 Cretarhabdus conicus | 9 Diazomatolithus lehmanii | 10 Parhabdolithus embergeri | 11 Cruciellipsis chiastia | 12 Manivitella pemmatoidea | 13 Parhabdolithus asper | 14 Cretarhabdus surirellus | 15 Lithraphidites carniolensis | 16 Cretarhabdus angustiforatus | 17 Tegumentum stradneri | 18 Zygodiscus diplogrammus | 19 Zygodiscus elegans | 20 Chiastozygus litterarius | 21 Flabellites oblongus | 22 Rucinolithus irregularis | 23 Nannoconus truitti | 24 Parhabdolithus angustus | 25 Pervilithus varius | 26 Lithastrinus floralis | 27 Parhabdolithus achylostaurion | 28 Lithraphidites alatus | 29 Prediscosphaera columnata | 30 Tranolithus orionatus | 31 Cribrosphaerella ehrenbergii | 32 Eiffellithus turriseiffelii | 33 Prediscosphaera cretacea | 34 Lithraphidites pseudoquadratus | 35 Eiffellithus eximius | 36 Zygodiscus spiralis | 37 Watznaueria supracretacea | 38 Cretarhabdus sp. | 39 Nannoconus sp. | 40 Pervilithus varius | 41 Watznaueria supracretacea | sample | set |
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102.1 | 172.40 | A | R | R | R | F | 19_99_0.00cm | 14 | |||||||||||||||||||||||||||||||||||||
102.12 | 172.44 | C | R | 20_1_4.00cm | 14 | ||||||||||||||||||||||||||||||||||||||||
102.18 | 172.60 | R | 20_1_20.00cm | 14 | |||||||||||||||||||||||||||||||||||||||||
102.2 | 172.65 | A | R | R | F | F | 20_1_25.00cm | 14 | |||||||||||||||||||||||||||||||||||||
105.48 | 181.30 | R | R | R | R | F | 20_99_0.00cm | 14 | |||||||||||||||||||||||||||||||||||||
105.75 | 182.01 | R | RF | R | A | R | R | R | R | R | R | R | R | F | R | R | R | R | R | F | R | R | 21_1_71.00cm | 14 | |||||||||||||||||||||
105.96 | 182.57 | A | R | R | F | R | 21_1_127.00cm | 14 | |||||||||||||||||||||||||||||||||||||
105.97 | 182.60 | R | R | RF | R | A | R | R | R | R | R | R | R | R | R | R | R | R | RF | R | R | R | 21_1_130.00cm | 14 | |||||||||||||||||||||
106.06 | 182.83 | R | A | F | R | R | R | R | R | R | R | R | 21_2_3.00cm | 14 | |||||||||||||||||||||||||||||||
106.07 | 182.85 | R | R | R | R | A | R | R | F | R | R | R | R | R | R | R | R | R | 21_2_5.00cm | 14 | |||||||||||||||||||||||||
106.14 | 183.05 | R | R | R | R | 21_2_25.00cm | 14 | ||||||||||||||||||||||||||||||||||||||
108 | 191.00 | F | 21_99_0.00cm | 14 | |||||||||||||||||||||||||||||||||||||||||
108.13 | 191.56 | F | R | R | R | R | 22_1_56.00cm | 14 | |||||||||||||||||||||||||||||||||||||
110.22 | 200.50 | F | 22_99_0.00cm | 14 | |||||||||||||||||||||||||||||||||||||||||
110.27 | 200.71 | R | R | A | R | C | F | C | R | F | R | R | R | R | RF | R | 23_1_21.00cm | 14 |