Table T4. Planktonic foraminifer range chart, Holes U1339A, U1339B, U1339C, and U1339D. (See table notes.)
|
Core, section |
Abundance |
Preservation |
Globigerina bulloides |
Globigerina umbilicata |
Neogloboquadrina pachyderma (dex) |
Neogloboquadrina pachyderma (sin) |
Turborotalia quinqueloba |
Other observations |
|---|---|---|---|---|---|---|---|---|
| 323-U1339A- | ||||||||
| Mudline | F | |||||||
| 1H-CC | D | G | R | R | D | Abundant siliciclastics | ||
| 2H-CC | A | G | R | A | Abundant siliciclastics | |||
| 3H-CC | P | G | P | Few siliciclastics | ||||
| 4H-CC | F | G | P | F | Dominant siliciclastics | |||
| 323-U1339B- | ||||||||
| Mudline | B | |||||||
| 1H-CC | A | G | D | F | P | Abundant siliciclastics | ||
| 2H-CC | R | G | R | Abundant siliciclastics | ||||
| 3H-CC | A | G | A | R | Few siliciclastics | |||
| 4H-CC | A | G | A | F | P | P | Abundant siliciclastics | |
| 5H-CC | A | G | D | P | R | P | Abundant siliciclastics. Tests are yellow, Fe coated? | |
| 6H-CC | P | G | P | Few siliciclastics | ||||
| 7H-CC | F | G | F | P | Few siliciclastics | |||
| 8H-CC | P | G | P | Abundant siliciclastics | ||||
| 9H-CC | B | Abundant siliciclastics | ||||||
| 10H-CC | R | G | R | P | P | Dominant siliciclastics. Rock fragment >1 cm | ||
| 11H-CC | P | G | P | P | Abundant siliciclastics | |||
| 12H-CC | A | G | A | P | P | Few siliciclastics | ||
| 13H-CC | R | G | R | Abundant siliciclastics | ||||
| 14H-CC | P | G | P | P | P | Abundant siliciclastics | ||
| 15H-CC | P | G | P | P | Dominant siliciclastics | |||
| 16H-CC | B | Dominant siliciclastics | ||||||
| 17H-CC | A | G | A | F | P | Abundant siliciclastics | ||
| 18H-CC | A | G | F | A | P | Dominant siliciclastics | ||
| 19H-CC | A | G | A | P | P | Dominant siliciclastics | ||
| 20H-CC | P | G | P | P | P | Dominant siliciclastics | ||
| 21H-CC | P | G | P | P | Dominant siliciclastics | |||
| 22H-CC | B | Dominant siliciclastics | ||||||
| 323-U1339C- | ||||||||
| Mudline | B | |||||||
| 1H-CC | A | G | A | F | F | Few siliciclastics | ||
| 2H-CC | A | G | A | F | R | Abundant siliciclastics | ||
| 3H-CC | R | G | R | P | Abundant siliciclastics | |||
| 4H-CC | F | G | F | P | Dominant siliciclastics | |||
| 5H-CC | A | G | A | F | Dominant siliciclastics | |||
| 6H-CC | A | G | A | R | Dominant siliciclastics | |||
| 7H-CC | A | G | A | R | Dominant siliciclastics | |||
| 8H-CC | P | G | P | Abundant siliciclastics | ||||
| 9H-CC | A | G | P | A | P | Few siliciclastics | ||
| 10H-CC | A | G | A | R | Abundant siliciclastics | |||
| 11H-CC | A | G | A | F | P | Abundant siliciclastics | ||
| 12H-CC | B | Abundant siliciclastics | ||||||
| 13H-CC | A | G | A | P | Abundant siliciclastics | |||
| 14H-CC | R | G | R | Abundant siliciclastics | ||||
| 15H-CC | A | G | A | P | P | Abundant siliciclastics | ||
| 16H-CC | P | P | P | P | Abundant siliciclastics | |||
| 17H-CC | D | G | D | R | Dominant siliciclastics | |||
| 18H-CC | R | G | R | Dominant siliciclastics | ||||
| 19H-CC | A | G | F | A | R | Few siliciclastics | ||
| 20H-CC | A | G | A | A | A | Abundant siliciclastics | ||
| 21H-CC | A | G | P | A | R | Few siliciclastics | ||
| 323-U1339D- | ||||||||
| Mudline | A | G | A | F | R | Dominant siliciclastics | ||
| 1H-CC | A | G | A | F | F | Dominant siliciclastics | ||
| 2H-CC | A | G | A | R | Dominant siliciclastics | |||
| 3H-CC | F | G | F | P | Dominant siliciclastics | |||
| 4H-CC | A | G | A | F | Dominant siliciclastics | |||
| 5H-CC | R | G | R | Dominant siliciclastics | ||||
| 6H-CC | D | G | D | F | P | Dominant siliciclastics | ||
| 7H-CC | F | G | F | R | Dominant siliciclastics | |||
| 8H-CC | A | G | A | F | R | Dominant siliciclastics | ||
| 9H-CC | B | Dominant siliciclastics | ||||||
| 10H-CC | F | M | F | Few siliciclastics | ||||
| 11H-CC | B | Few siliciclastics | ||||||
| 12H-CC | P | M | P | P | Few siliciclastics | |||
| 13H-CC | A | G | A | P | Abundant siliciclastics | |||
| 14H-CC | A | G | A | P | Abundant siliciclastics | |||
| 15H-CC | A | G | P | A | R | P | Abundant siliciclastics | |
| 16H-CC | A | G | D | F | P | Dominant siliciclastics | ||
| 17H-CC | R | M | R | R | Dominant siliciclastics | |||
| 18H-CC | A | M | R | A | F | R | Dominant siliciclastics | |
| 19H-CC | A | G | R | A | R | R | Dominant siliciclastics | |
| 20H-CC | B | Dominant siliciclastics | ||||||
| 21H-CC | R | M | R | R | R | P | Dominant siliciclastics | |
| 22H-CC | R | M | P | R | Abundant siliciclastics | |||
Notes: Abundance: D = dominant, A = abundant, F = few, R = rare, P = present, B = barren. Preservation: VG = very good, G = good, M = moderate, P = poor. Dex = dextral, sin = sinistral.
Previous | Close | Next | Top of page