Table T9. Distribution of planktonic foraminifers, Hole U1314B.
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Core
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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
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Stratigraphic event
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|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
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306-U1314B- |
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| 1H, top | F | G | — | P | P |
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P | P |
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P |
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P |
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>150 µm; mainly diatoms, only presence (P) of species noted |
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| 1H-CC | D | VG | 14 |
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A |
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F |
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A | R |
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C |
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R |
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R |
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R |
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P | IRD including tephra and stained quartz |
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| 2H-CC | D | G | 12 |
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D |
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F | C | C |
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F |
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R | R | A |
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F |
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P | Few IRD including tephra and stained quartz |
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| 3H-CC | D | G | 9 | R | A |
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R | F | D |
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C |
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R | F |
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A |
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P | IRD |
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| 4H-CC | D | G | 9 | R | A |
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F | A |
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R |
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C |
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A | R | R | F |
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P |
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| 5H-CC | D | G | 12 | R | A |
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R | F | A |
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A |
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R |
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F |
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A |
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P | Abundant IRD including tephra and stained quartz |
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| 6H-CC | A | G | 11 | R | C |
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F | C | D |
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F |
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F |
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R |
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A |
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P | Abundant IRD including tephra and stained quartz |
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| 7H-CC | D | G | 14 | R | A |
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F | R | A | F | F |
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A |
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F | F | F |
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A | R |
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P | Few IRD |
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| 8H-CC | D | M | 8 |
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C |
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F | A | A |
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F |
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F |
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A | F |
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In-flow! IRD including tephra and stained quartz |
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| 9H-CC | D | G | 18 | R | C |
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R | A | A |
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R | R |
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R |
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C | A | R |
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P | Abundant radiolarians |
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| 10H-CC | D | G | 23 | R | A |
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F | F | A | R |
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C |
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R | F |
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A | F |
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P | Few IRD |
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| 11H-CC | D | G | 16 | F | A |
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R | A | R | R |
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F |
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R |
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A | F |
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P |
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| 12H-CC | D | G | 7 |
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A |
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R | R | A | A |
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F |
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A | A |
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| 13H-CC | A | M | 13 |
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D | F |
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A | F | A |
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C |
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C |
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Aggregates |
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| 14H-CC | D | G | 12 |
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R |
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R | C | A | A |
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C |
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R | C |
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A | F |
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P |
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| 15H-CC | D | G | 8 |
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C |
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F | C | A |
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R |
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F |
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A |
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FaO N. pachyderma (s) (1.78 Ma) |
| 16H-CC | D | G | 6 | R | C |
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F | D | R |
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F |
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F |
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C | R |
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| 17H-CC | D | G | 10 | F | F |
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F | D |
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C |
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R | F |
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C |
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P |
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| 18H-CC | D | G | 11 |
|
C |
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C | A |
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C |
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C |
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C |
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P |
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FO G. inflata (2.09 Ma) |
| 19H-CC | D | G | 4 |
|
F |
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F | D | R |
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F |
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F | F |
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P |
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| 20H-CC | D | G | 14 |
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C |
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F | D | R |
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R | R | C |
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F |
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| 21H-CC | D | G | 7 |
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F |
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F | D | R |
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F |
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R |
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F |
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| 22H-CC | D | G | 5 |
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C |
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F | D | R |
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R |
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R |
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F |
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| 23H-CC | D | G | 14 |
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C |
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F | A | R |
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C |
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F |
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R | F |
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F |
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F |
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LO G. puncticulata, N. atlantica (s) (2.41 Ma) |
| 24H-CC | D | M | 8 |
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A |
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F | C |
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C |
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F |
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F |
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F |
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F |
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F |
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| 25H-CC | D | M | 10 |
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F |
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F |
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D |
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F |
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Full of aggregates, high fragmentation |
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| 26H-CC | D | G | 11 |
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A |
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R | F |
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A |
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R |
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Full of aggregates, high fragmentation |
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| 27H-CC | D | M |
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C |
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D | R |
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R |
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R |
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Full of aggregates, high fragmentation |
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| 28H-CC | D | M | 9 |
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F |
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F |
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D | R |
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F |
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F |
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Full of aggregates, high fragmentation |
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| 29H-CC | D | G | 4 |
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C |
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F | A |
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C | R | F |
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F |
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F |
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R |
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F |
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| 30H-CC | D | G | 3 | R | F |
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C | A | F |
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C |
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F |
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F |
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C |
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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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