|
Hole,
core, section,
interval (cm) |
Depth
(mbsf) |
Event
type
|
Species
|
Age
(Ka) |
Ericson
zone
|
|---|---|---|---|---|---|
| 1002C-1H-4, 17 | 4.67 | AS | Globorotalia menardii/tumida | 9 | Y/Z |
| 1002C-3H-3, 75 | 21.64 | AS | Pulleniatina obliquiloculata | ~40 | YP.obliq |
| 1002C-4H-5, 72 | 34.32 | AS/LO | Globorotalia menardii/tumida/flexuosa | 80 | X/Y |
| 1002C-5H-6, 75 | 45.22 | AS | Globorotalia menardii/tumida | 130 | W/X |
| 1002C-6H-7, 79 | 55.05 | AS | Globorotalia menardii/tumida | 165 | V/W |
| 1002D-9H-8, 77 | 82.15 | FO | Emiliania huxleyi | 248 | |
| 1002C-13H-6, 72 | 120.73 | AS | Globorotalia menardii/tumida | 425 | U/V |
| 1002C-14H-CC | 133.15 | LO | Pseudoemiliania lacunosa | 458 |
Notes: AS = abundance
shift, FO = first occurrence, LO = last occurrence. Age estimates presented here
were used to help constrain the 
18O
stratigraphy for this site but were not used as tie points in the age model
applied to Figure 6. Reported depths are in original mbsf and are not corrected
for gas expansion. Ericson zones are after Ericson et al. (1961) and Ericson and
Wollin (1968).