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Table T8. Relative abundances of planktonic foraminifers, Hole U1322B.

Core, section, interval (cm) Depth (mbsf) Sample code Zone Age Preparation
Preservation
Group abundance
Bolliella calida Globigerina bulloides Globigerina falconensis Globigerina quinqueloba Globigerinella calida Globigerinella siphonifera Globigerinita glutinata Globigerinoides conglobatus Globigerinoides ruber (pink) Globigerinoides ruber (white) Globigerinoides sacculifer Globorotalia crassaformis Globorotalia flexuosa Globorotalia inflata Globorotalia menardii Globorotalia scitula Globorotalia truncatulinoides Globorotalia tumida Hastigerina pelagica Neogloboquadrina dutertrei Orbulina universa Pulleniatina obliquiloculata Sphaeroidinella dehiscens Comments
308-U1322B-
1H-CC, 0–10 4 PAL Z Pleistocene >63 M C     R R   R T T F F R R B T T   R B B R R R B G. inflata reworked
2H-CC, 17–27 14 PAL Y1   VG F   T F R   R T   F R R F   R     R     R R      
3H-CC, 6–16 22 PAL   VG C T T R R T F T   C C R F   R     R     R R      
4H-CC, 29–34 33 PAL Y2   G F   T F F   R     F F   R   F     R       R      
5H-CC, 24–29 42 PAL   G R     R R   R R   R F       F     T     T R      
6H-CC, 41–46 51 PAL   G R     R R   R T   F R   R   R     T     R        
7H-CC, 22–27 61 PAL   G R     R R   R T   R R   R   R     T     R R      
8H-CC, 25–30 71 PAL   G VR     R T     T   R R   R   R             T     Some charcoal
9H-CC, 45–50 80 PAL   G R   T R F   F R   R R R R   R   T R     R R     Some charcoal
10H-CC, 29–34 90 PAL   G R   T R R   R R   R R F T   R   T T     R R      
11H-CC, 56–61 98 PAL   G R     T T   R     R R R     R     R     R F      
12H-CC, 28–33 108 PAL   G R     T T   R     R R T     F     R       R      
13H-CC, 63–68 116 PAL   G F     F R   R     R R F R   R   T R       R      
14H-CC, 43–48 125 PAL Y3   G F   T R R   R     R R T     F     R     R R     Abundant charcoal
15H-1, 95–99 126 PAL   G R   T F R   R R   F R       R     T       R     Rare
15H-CC, 47–52 135 PAL   VG F     R R   R T   R R R     R   R F     T R     Abundant charcoal
16H-CC, 41–46 142 PAL   G C   R F R     T   F R T F   R     F     F R     Mica
17H-CC, 40–45 150 PAL   VG C   R F R   T     C F T F   R   R R     F R R   Mica + charcoal
18H-CC, 31–36 158 PAL   VG C T   R R T F     C F R R   R   R R     R R R   Charcoal +
19H-CC, 28–33 167 PAL   G R     R R   R     C C R F   R   T R     F R R   Charcoal +
20H-CC, 46–51 174 PAL   G A   T R R T T     R R T T   R     T     R T     Silt sand
21H-CC, 24–29 182 PAL Y5   G VR   R T     R     C C F F   R   R F     F R     Charcoal
22H-CC, 33–38 189 PAL Y6   M R     T       T   T T T     F     T             Silt sand
23H-CC, 37–42 199 PAL   M R   R R     T       R       F                   Mica + silt
24H-CC, 18–23 202 PAL   M R   T T           F R       F           T R     Silt + many sea urchin spines
25H-CC, 33–38 210 PAL   M R   R T     T     R R       R     R     R R     Silt + mica
26H-CC, 21–26 214 PAL   M R   T T           R R       T     T     T T     Silt + mica
27H-CC, 23–28 220 PAL   M R   T T     T     R R       R     T     R T     Mica + silt + charcoal
28H-CC, 33–38 227 PAL   M R   R R     R R   F F       F   R         R     Charcoal
29H-CC, 39–44 234 PAL   M R     R T   T T   F F       F             T     Charcoal

Notes: Abundance: A = abundant, C = common, F = frequent, R = rare, VR = very rare, T = trace, B = barren. Preservation: VG = very good, G = good, M = moderate. PAL = paleontological sample.

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