Table T10. Distribution of planktonic foraminifers, Hole U1314C.
| Core | Abundance | Preservation | Fill level in PF vial before splitting (mm) | Globigerinella aequilateralis | Globigerina bulloides | Globigerina falconensis | Globigerinella calida | Globigerinita glutinata | Neogloboquadrina pachyderma (d) | Neogloboquadrina pachyderma (s) | Neogloboquadrina dutertrei | Neogloboquadrina atlantica (s) | Neogloboquadrina atlantica (d) | Turborotalita quinqueloba | Globigerinoides ruber white/pink | Orbulina universa | Globorotalia scitula (s) | Globorotalia scitula (d) | Globorotalia hirsuta | Globorotalia inflata | Globorotalia crassaformis | Globorotalia truncatulinoides (s) | Globorotalia truncatulinoides (d) | Globorotalia puncticulata | Ostracodes | Other species and observations | Stratigraphic event |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 306-U1314C- | |||||||||||||||||||||||||||
| 1H, top | A | M | — | D | F | F | D | F | C | P | Washout and some Holocene sediments, abundant diatoms | ||||||||||||||||
| 1H-CC | D | VG | 4 | A | F | A | A | A | F | R | R | P | Few IRD | ||||||||||||||
| 2H-CC | D | VG | 11 | R | A | R | A | A | A | R | F | F | R | R | P | Beella digitata, few IRD including tephra | |||||||||||
| 3H-CC | D | VG | 3 | R | A | R | R | A | F | F | R | C | A | F | R | P | B. digitata | ||||||||||
| 4H-CC | D | VG | 17 | R | F | D | R | R | R | R | Abundant IRD (also gravel sized) including tephra | ||||||||||||||||
| 5H-CC | D | G | 7 | R | C | R | F | A | F | F | A | F | F | C | P | ||||||||||||
| 6H-CC | D | G | 20 | C | R | F | C | D | C | R | C | R | R | P | IRD including tephra | ||||||||||||
| 7H-CC | D | G | 18 | R | C | R | A | A | A | R | C | Some IRD including tephra and stained quartz | |||||||||||||||
| 8H-CC | A | G | 22 | R | C | R | F | A | A | R | F | R | R | F | F | F | R | P | Abundant IRD including stained quartz and abundant tephra | ||||||||
| 9H-CC | D | G | 30 | R | A | F | F | A | F | F | R | A | F | Some IRD | |||||||||||||
| 10H-CC | D | G | 9 | F | C | R | F | A | R | R | F | R | A | F | P | Abundant sponge spicules | |||||||||||
| 11H-CC | D | G | 30 | R | C | R | R | F | A | A | R | F | R | R | A | R | R | P | Rare IRD (quartz) | ||||||||
| 12H-CC | A | M | — | F | F | D | D | F | R | F | Aggregates, IRD including tephra and stained quartz | ||||||||||||||||
| 13H-CC | D | G | 3 | A | A | R | A | R | R | R | Abundant IRD | ||||||||||||||||
| 14H-CC | D | G | 14 | F | F | A | A | F | R | R | C | ||||||||||||||||
| 15H-CC | F | G | 8 | F | F | D | F | C | R | Abundant IRD particles, quartz, muscovite, rock fragments | FaO N. pachyderma (s) (1.78 Ma) | ||||||||||||||||
| 16H-CC | D | G | 13 | F | F | D | F | C | |||||||||||||||||||
| 17H-CC | D | G | 6 | C | F | D | F | F | F | C | P | ||||||||||||||||
| 18H-CC | D | G | 10 | C | F | A | F | F | C | FO G. inflata (2.09 Ma) | |||||||||||||||||
| 19H-CC | D | G | 12 | C | F | A | F | F | R | C | |||||||||||||||||
| 20H-CC | D | G | 24 | C | F | A | F | F | R | A | R | ||||||||||||||||
| 21H-CC | D | G | 25 | C | F | A | F | F | R | F | F | Abundant quartz, dominant aggregates | |||||||||||||||
| 22H-CC | D | G | 14 | C | F | F | A | F | F | P | LO N. atlantica (s) (2.41 Ma) | ||||||||||||||||
Notes: Abundance: D = dominant, A = abundant, C = common, F = few, R = rare. Preservation: VG = very good, G = good, M = moderate. See “Foraminifers” in the “Site U1312–U1315 methods” chapter. PF = planktonic foraminifers. d = dextral, s = sinistral. P in ostracodes column = presence of valves. IRD = ice-rafted debris, FO = first occurrence, FaO = first abundant occurrence, LO = last occurrence.
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