Brunner, Charlotte A; Andres, Miriam S; Holbourn, Ann E; Siedlecki, S; Brooks, Gregg R; Molina-Garza, Roberto S; Fuller, Michael D; Ladner, Bryan; Hine, Albert C; Li, Qianyu (2002): (Table T1) Depths and ages of datum levels at ODP Leg 182 sites [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.785925, Supplement to: Brunner, CA et al. (2002): Quaternary planktonic foraminiferal biostratigraphy, ODP Leg 182 sites. In: Hine, AC; Feary, DA; Malone, MJ (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 182, 1-16, https://doi.org/10.2973/odp.proc.sr.182.011.2002
Always quote citation above when using data! You can download the citation in several formats below.
Abstract:
The first and last appearances of Quaternary planktonic foraminifers in the Great Australian Bight were evaluated using datum levels from magnetostatigraphy, oxygen isotope stratigraphy, and calcareous nannofossil biostratigraphy to determine whether they were synchronous or diachronous with open-ocean biostratigraphic events. The first appearance of Globorotalia truncatulinoides is diachronous at 1.6-1.7 Ma at Site 1127 and 1.1-1.2 at Sites 1129 and 1132, similar to other local appearances in high latitudes. All other datum levels, however, are synchronous with open-ocean events, including the first appearance of Globorotalia hirsuta and the last appearances of Globorotalia tosaensis and pink Globigerinoides ruber in the Indo-Pacific region. A local reappearance of Gt. hirsuta at ~0.12 Ma and the disappearance of Globorotalia crassaformis at ~0.10 Ma were found to be useful for local biostratigraphy. Age control at the bottom of all of the sections is poor at this time, but results suggest that sedimentation recommenced starting at ~1.9 Ma above the regional unconformity that marks the base of seismostratigraphic Sequence 2. Sediment accumulation is distinctly reduced in the lower Pleistocene compared to the upper Pleistocene, perhaps in part because of processes associated with several omission surfaces.
Related to:
Berggren, William A; Kent, Dennis V; Swisher, Carl C, III; Aubry, Marie-Pierre (1995): A revised Cenozoic geochronology and chronostratigraphy. In: Berggren, W.A., Kent, D.V., Aubry, M.-P., Hardenbol, J. (eds.), Geochronology, time scales and global stratigraphic correlation. Special Publication - SEPM (Society for Sedimentary Geology), 54, 129-212, https://doi.org/10.2110/pec.95.04.0129
Project(s):
Ocean Drilling Program (ODP)
Coverage:
Median Latitude: -33.343304 * Median Longitude: 128.129662 * South-bound Latitude: -33.420180 * West-bound Longitude: 127.602200 * North-bound Latitude: -33.296560 * East-bound Longitude: 128.481300
Date/Time Start: 1998-10-30T21:30:00 * Date/Time End: 1998-11-26T18:30:00
Minimum DEPTH, sediment/rock: 3.50 m * Maximum DEPTH, sediment/rock: 556.70 m
Event(s):
182-1127B * Latitude: -33.357500 * Longitude: 128.481280 * Date/Time Start: 1998-10-30T21:30:00 * Date/Time End: 1998-11-03T01:45:00 * Elevation: -479.3 m * Penetration: 510.7 m * Recovery: 440.56 m * Location: Great Australian Bight * Campaign: Leg182 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 55 cores; 510.7 m cored; 0 m drilled; 86.3 % recovery
182-1129C * Latitude: -33.296560 * Longitude: 128.481300 * Date/Time Start: 1998-11-24T23:24:00 * Date/Time End: 1998-11-26T18:30:00 * Elevation: -202.4 m * Penetration: 451.6 m * Recovery: 322.89 m * Location: Great Australian Bight * Campaign: Leg182 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 48 cores; 451.6 m cored; 0 m drilled; 71.5 % recovery
182-1130A * Latitude: -33.420180 * Longitude: 127.602330 * Date/Time Start: 1998-11-11T22:07:00 * Date/Time End: 1998-11-13T18:15:00 * Elevation: -486.7 m * Penetration: 380.4 m * Recovery: 312.47 m * Location: Great Australian Bight * Campaign: Leg182 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 41 core; 380.4 m cored; 0 m drilled; 82.1 % recovery
Comment:
Sediment depth is given in mbsf. References used: 1 = Fuller et al. (2003, doi:10.1046/j.1440-0952.2003.01002.x), 2 = Andres and McKenzie (2000), 3 = Holbourn et al. (2002, doi:10.1029/2001PA000643), 4 = S. Siedlecki and G. Brooks (unpubl. data), 5 = Ladner (2002, doi:10.2973/odp.proc.sr.182.013.2002), 6 = Hine et al. (2002, doi:10.2973/odp.proc.sr.182.009.2002), 7 = Thompson et al. (1979, doi:10.1038/280554a0), 8 = Almond et al. (1993), 9 = Berggren et al. (1995a, doi:10.1130/0016-7606(1995)107<1272:LNCNPI>2.3.CO;2), 10 = Berggren et al. (1995b), 11 = Bassinot et al. (1994, doi:10.1016/0012-821X(94)90244-5), 12 = Sato and Kameo (1996, doi:10.2973/odp.proc.sr.151.112.1996).
Parameter(s):
| # | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
|---|---|---|---|---|---|---|
| 1 | Event label | Event | ||||
| 2 | Latitude of event | Latitude | ||||
| 3 | Longitude of event | Longitude | ||||
| 4 | Elevation of event | Elevation | m | |||
| 5 | Ageprofile Datum Description | Ageprof dat des | Brunner, Charlotte A | T = top, B = bottom, o = onset, t = termination, Atl. = Atlantic Ocean, Ind. = Indian Ocean | ||
| 6 | Ageprofile Datum Type | Ageprof dat typ | Brunner, Charlotte A | |||
| 7 | Age model | Age model | ka | Brunner, Charlotte A | # = approximate | |
| 8 | Age model, optional | Age model opt | ka | Brunner, Charlotte A | estimated local age | |
| 9 | DEPTH, sediment/rock | Depth sed | m | Geocode | ||
| 10 | Error, absolute | Error a | ± | Brunner, Charlotte A | stratigraphic depth error in m | |
| 11 | Sample comment | Sample comment | Brunner, Charlotte A | |||
| 12 | Reference/source | Reference | Brunner, Charlotte A | see dataset comment for details |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
566 data points
Data
| 1 Event | 2 Latitude | 3 Longitude | 4 Elevation [m] | 5 Ageprof dat des | 6 Ageprof dat typ | 7 Age model [ka] | 8 Age model opt [ka] | 9 Depth sed [m] | 10 Error a [±] | 11 Sample comment | 12 Reference |
|---|---|---|---|---|---|---|---|---|---|---|---|
| 182-1127B | -33.3575 | 128.4813 | -479 | T Globorotalia crassaformis local disappearance | Planktonic foraminifer datum level | 100 | 58.45 | 1.50 | |||
| 182-1127B | -33.3575 | 128.4813 | -479 | T pink Gs. ruber | Planktonic foraminifer datum level | 120 | 120 | 60.71 | 0.75 | 7 | |
| 182-1127B | -33.3575 | 128.4813 | -479 | B reappearance Globorotalia hirsuta | Planktonic foraminifer datum level | #120 | 120 | 62.46 | 1.00 | 8 | |
| 182-1127B | -33.3575 | 128.4813 | -479 | T Globorotalia tosaensis | Planktonic foraminifer datum level | 650 | 680 | 317.25 | 1.80 | 9 | |
| 182-1127B | -33.3575 | 128.4813 | -479 | B Globorotalia truncatulinoides (Atl. and Ind.) | Planktonic foraminifer datum level | 2000 | 1700 | 418.71 | 0.75 | 9 | |
| 182-1127B | -33.3575 | 128.4813 | -479 | Brunhes (o) | Magnetostratigraphic boundaries | 780 | 343.40 | 1,10 | |||
| 182-1127B | -33.3575 | 128.4813 | -479 | Jaramillo (t) | Magnetostratigraphic boundaries | 990 | 380.70 | 1,10 | |||
| 182-1127B | -33.3575 | 128.4813 | -479 | Jaramillo (o) | Magnetostratigraphic boundaries | 1070 | 394.00 | 1.00 | 1,10 | ||
| 182-1127B | -33.3575 | 128.4813 | -479 | T MIS 2 | MIS boundaries | 11 | 9.20 | approximate depth | 2,3,4,11 | ||
| 182-1127B | -33.3575 | 128.4813 | -479 | T MIS 3 | MIS boundaries | 24 | 9.90 | approximate depth | 2,3,4,11 | ||
| 182-1127B | -33.3575 | 128.4813 | -479 | T MIS 4 | MIS boundaries | 57 | 34.50 | approximate depth | 2,3,4,11 | ||
| 182-1127B | -33.3575 | 128.4813 | -479 | T MIS 5 | MIS boundaries | 71 | 40.50 | approximate depth | 2,3,4,11 | ||
| 182-1127B | -33.3575 | 128.4813 | -479 | MIS 5.1 | MIS boundaries | 79 | 41.00 | approximate depth | 2,3,4,11 | ||
| 182-1127B | -33.3575 | 128.4813 | -479 | MIS 5.2 | MIS boundaries | 86 | 44.00 | approximate depth | 2,3,4,11 | ||
| 182-1127B | -33.3575 | 128.4813 | -479 | MIS 5.3 | MIS boundaries | 97 | 46.00 | approximate depth | 2,3,4,11 | ||
| 182-1127B | -33.3575 | 128.4813 | -479 | MIS 5.4 | MIS boundaries | 106 | 50.00 | approximate depth | 2,3,4,11 | ||
| 182-1127B | -33.3575 | 128.4813 | -479 | MIS 5.5 | MIS boundaries | 122 | 62.50 | approximate depth | 2,3,4,11 | ||
| 182-1127B | -33.3575 | 128.4813 | -479 | T MIS 6 | MIS boundaries | 129 | 65.50 | approximate depth | 2,3,4,11 | ||
| 182-1127B | -33.3575 | 128.4813 | -479 | T MIS 7 | MIS boundaries | 186 | 83.00 | approximate depth | 2,3,4,11 | ||
| 182-1127B | -33.3575 | 128.4813 | -479 | T MIS 8 | MIS boundaries | 242 | 125.00 | approximate depth | 2,3,4,11 | ||
| 182-1127B | -33.3575 | 128.4813 | -479 | T MIS 9 | MIS boundaries | 301 | 140.00 | approximate depth | 2,3,4,11 | ||
| 182-1127B | -33.3575 | 128.4813 | -479 | T MIS 10 | MIS boundaries | 334 | 167.00 | approximate depth | 2,3,4,11 | ||
| 182-1127B | -33.3575 | 128.4813 | -479 | T MIS 11 | MIS boundaries | 364 | 185.00 | approximate depth | 2,3,4,11 | ||
| 182-1127B | -33.3575 | 128.4813 | -479 | T MIS 12 | MIS boundaries | 427 | 212.00 | approximate depth | 2,3,4,11 | ||
| 182-1127B | -33.3575 | 128.4813 | -479 | T MIS 13 | MIS boundaries | 474 | 223.00 | approximate depth | 2,3,4,11 | ||
| 182-1127B | -33.3575 | 128.4813 | -479 | T MIS 14 | MIS boundaries | 528 | 243.00 | approximate depth | 2,3,4,11 | ||
| 182-1127B | -33.3575 | 128.4813 | -479 | T MIS 15 | MIS boundaries | 568 | 256.00 | approximate depth | 2,3,4,11 | ||
| 182-1127B | -33.3575 | 128.4813 | -479 | T MIS 16 | MIS boundaries | 621 | 292.00 | approximate depth | 2,3,4,11 | ||
| 182-1127B | -33.3575 | 128.4813 | -479 | T MIS 17 | MIS boundaries | 659 | 312.00 | approximate depth | 2,3,4,11 | ||
| 182-1127B | -33.3575 | 128.4813 | -479 | T MIS 18 | MIS boundaries | 712 | 325.00 | approximate depth | 2,3,4,11 | ||
| 182-1127B | -33.3575 | 128.4813 | -479 | T MIS 19 | MIS boundaries | 760 | 334.00 | approximate depth | 2,3,4,11 | ||
| 182-1127B | -33.3575 | 128.4813 | -479 | T MIS 20 | MIS boundaries | 787 | 347.00 | approximate depth | 2,3,4,11 | ||
| 182-1127B | -33.3575 | 128.4813 | -479 | Emiliania huxleyi Acme | Nannofossil datum level | 85 | 26.10 | 5,9 | |||
| 182-1127B | -33.3575 | 128.4813 | -479 | B Emiliania huxleyi | Nannofossil datum level | 240 | 137.71 | 5,12 | |||
| 182-1127B | -33.3575 | 128.4813 | -479 | T Pseudoemiliania lacunosa | Nannofossil datum level | 420 | 233.10 | 5,12 | |||
| 182-1127B | -33.3575 | 128.4813 | -479 | B Helicosphaera inversa | Nannofossil datum level | 510 | 262.00 | 5,12 | |||
| 182-1127B | -33.3575 | 128.4813 | -479 | T Reticulofenestra asanoi | Nannofossil datum level | 850 | 358.20 | 5,12 | |||
| 182-1127B | -33.3575 | 128.4813 | -479 | T small Gephyrocapsa spp. | Nannofossil datum level | 950 | 377.40 | 5,12 | |||
| 182-1127B | -33.3575 | 128.4813 | -479 | B Reticulofenestra asanoi | Nannofossil datum level | 1160 | 406.01 | 5,12 | |||
| 182-1127B | -33.3575 | 128.4813 | -479 | T Calcidiscus macintyrei | Nannofossil datum level | 1590 | 412.01 | 5,9 | |||
| 182-1127B | -33.3575 | 128.4813 | -479 | B. bigelowii acme | Nannofossil datum level | 456.00 | 5 | ||||
| 182-1127B | -33.3575 | 128.4813 | -479 | T Discoaster brouweri | Nannofossil datum level | 1950 | 469.70 | 5,12 | |||
| 182-1127B | -33.3575 | 128.4813 | -479 | Omission surface | Breaks in sedimentation | 313.00 | |||||
| 182-1127B | -33.3575 | 128.4813 | -479 | Omission surface | Breaks in sedimentation | 414.35 | |||||
| 182-1127B | -33.3575 | 128.4813 | -479 | Unconformable base of Sequence | 1950 | 463.28 | 3.66 | 2 | |||
| 182-1131A | -33.3261 | 128.4812 | -333 | T Globorotalia crassaformis local disappearance | Planktonic foraminifer datum level | 26.32 | 1.50 | ||||
| 182-1131A | -33.3261 | 128.4812 | -333 | B reappearance Globorotalia hirsuta | Planktonic foraminifer datum level | #120 | 29.32 | 1.50 | 8 | ||
| 182-1131A | -33.3261 | 128.4812 | -333 | B Globorotalia truncatulinoides (Atl. and Ind.) | Planktonic foraminifer datum level | 2000 | 517.26 | 4.76 | 9 | ||
| 182-1131A | -33.3261 | 128.4812 | -333 | Brunhes (o) | Magnetostratigraphic boundaries | 780 | 293.45 | 8.45 | 1,10 | ||
| 182-1131A | -33.3261 | 128.4812 | -333 | Jaramillo (t) | Magnetostratigraphic boundaries | 990 | 308.00 | 1,10 | |||
| 182-1131A | -33.3261 | 128.4812 | -333 | T MIS 2 | MIS boundaries | 11 | 3.50 | approximate depth | 2,3,4,11 | ||
| 182-1131A | -33.3261 | 128.4812 | -333 | T MIS 3 | MIS boundaries | 24 | 12.00 | approximate depth | 2,3,4,11 | ||
| 182-1131A | -33.3261 | 128.4812 | -333 | T MIS 4 | MIS boundaries | 57 | 19.00 | approximate depth | 2,3,4,11 | ||
| 182-1131A | -33.3261 | 128.4812 | -333 | T MIS 5 | MIS boundaries | 71 | 26.00 | approximate depth | 2,3,4,11 | ||
| 182-1131A | -33.3261 | 128.4812 | -333 | T MIS 6 | MIS boundaries | 129 | 36.00 | approximate depth | 2,3,4,11 | ||
| 182-1131A | -33.3261 | 128.4812 | -333 | B. bigelowii acme | Nannofossil datum level | 522.00 | 5 | ||||
| 182-1131A | -33.3261 | 128.4812 | -333 | Omission surface | Breaks in sedimentation | 463.30 | |||||
| 182-1131A | -33.3261 | 128.4812 | -333 | Unconformable base of Sequence | 531.49 | 2 | |||||
| 182-1129C | -33.2966 | 128.4813 | -202 | T Globorotalia crassaformis local disappearance | Planktonic foraminifer datum level | 39.72 | 1.50 | ||||
| 182-1129C | -33.2966 | 128.4813 | -202 | B reappearance Globorotalia hirsuta | Planktonic foraminifer datum level | #120 | 39.72 | 1.50 | 8 | ||
| 182-1129C | -33.2966 | 128.4813 | -202 | B Globorotalia truncatulinoides (Atl. and Ind.) | Planktonic foraminifer datum level | 2000 | 1100 | 413.80 | 9.31 | 9 | |
| 182-1129C | -33.2966 | 128.4813 | -202 | Brunhes (o) | Magnetostratigraphic boundaries | 780 | 343.00 | 4.20 | 1,10 | ||
| 182-1129C | -33.2966 | 128.4813 | -202 | Jaramillo (t) | Magnetostratigraphic boundaries | 990 | 397.90 | 5.00 | 1,10 | ||
| 182-1129C | -33.2966 | 128.4813 | -202 | Jaramillo (o) | Magnetostratigraphic boundaries | 1070 | 440.00 | 5.00 | 1,10 | ||
| 182-1129C | -33.2966 | 128.4813 | -202 | Olduvai (t) | Magnetostratigraphic boundaries | 1770 | 540.00 | 1,10 | |||
| 182-1129C | -33.2966 | 128.4813 | -202 | T MIS 2 | MIS boundaries | 11 | 5.00 | approximate depth | 2,3,4,11 | ||
| 182-1129C | -33.2966 | 128.4813 | -202 | T MIS 3 | MIS boundaries | 24 | 9.00 | approximate depth | 2,3,4,11 | ||
| 182-1129C | -33.2966 | 128.4813 | -202 | T MIS 4 | MIS boundaries | 57 | 30.00 | approximate depth | 2,3,4,11 | ||
| 182-1129C | -33.2966 | 128.4813 | -202 | T MIS 5 | MIS boundaries | 71 | 36.00 | approximate depth | 2,3,4,11 | ||
| 182-1129C | -33.2966 | 128.4813 | -202 | T MIS 6 | MIS boundaries | 129 | 41.00 | approximate depth | 2,3,4,11 | ||
| 182-1129C | -33.2966 | 128.4813 | -202 | T MIS 7 | MIS boundaries | 186 | 50.00 | approximate depth | 2,3,4,11 | ||
| 182-1129C | -33.2966 | 128.4813 | -202 | T MIS 8 | MIS boundaries | 242 | 83.00 | approximate depth | 2,3,4,11 | ||
| 182-1129C | -33.2966 | 128.4813 | -202 | T MIS 9 | MIS boundaries | 301 | 91.00 | approximate depth | 2,3,4,11 | ||
| 182-1129C | -33.2966 | 128.4813 | -202 | T MIS 10 | MIS boundaries | 334 | 97.00 | approximate depth | 2,3,4,11 | ||
| 182-1129C | -33.2966 | 128.4813 | -202 | T MIS 11 | MIS boundaries | 364 | 101.00 | approximate depth | 2,3,4,11 | ||
| 182-1129C | -33.2966 | 128.4813 | -202 | T MIS 12 | MIS boundaries | 427 | 127.00 | approximate depth | 2,3,4,11 | ||
| 182-1129C | -33.2966 | 128.4813 | -202 | T MIS 13 | MIS boundaries | 474 | 140.00 | approximate depth | 2,3,4,11 | ||
| 182-1129C | -33.2966 | 128.4813 | -202 | Unconformable base of Sequence | 1890 | 556.70 | 2 | ||||
| 182-1130A | -33.4202 | 127.6023 | -487 | T Globorotalia crassaformis local disappearance | Planktonic foraminifer datum level | 34.40 | 1.50 | ||||
| 182-1130A | -33.4202 | 127.6023 | -487 | B reappearance Globorotalia hirsuta | Planktonic foraminifer datum level | #120 | 50.46 | 1.50 | 8 | ||
| 182-1130A | -33.4202 | 127.6023 | -487 | T Globorotalia tosaensis | Planktonic foraminifer datum level | 650 | 179.70 | 1.50 | 9 | ||
| 182-1130A | -33.4202 | 127.6023 | -487 | B Globorotalia truncatulinoides (Atl. and Ind.) | Planktonic foraminifer datum level | 2000 | 229.30 | 1.50 | 9 | ||
| 182-1130A | -33.4202 | 127.6023 | -487 | Brunhes (o) | Magnetostratigraphic boundaries | 780 | 200.00 | 1,10 | |||
| 182-1130A | -33.4202 | 127.6023 | -487 | Jaramillo (t) | Magnetostratigraphic boundaries | 990 | 215.00 | 1,10 | |||
| 182-1130A | -33.4202 | 127.6023 | -487 | T MIS 6 | MIS boundaries | 129 | 47.73 | approximate depth | 2,3,4,11 | ||
| 182-1130A | -33.4202 | 127.6023 | -487 | T MIS 7 | MIS boundaries | 186 | 62.45 | approximate depth | 2,3,4,11 | ||
| 182-1130A | -33.4202 | 127.6023 | -487 | T MIS 8 | MIS boundaries | 242 | 83.38 | approximate depth | 2,3,4,11 | ||
| 182-1130A | -33.4202 | 127.6023 | -487 | T MIS 9 | MIS boundaries | 301 | 92.45 | approximate depth | 2,3,4,11 | ||
| 182-1130A | -33.4202 | 127.6023 | -487 | T MIS 10 | MIS boundaries | 334 | 115.10 | approximate depth | 2,3,4,11 | ||
| 182-1130A | -33.4202 | 127.6023 | -487 | T MIS 12 | MIS boundaries | 427 | 136.95 | approximate depth | 2,3,4,11 | ||
| 182-1130A | -33.4202 | 127.6023 | -487 | T MIS 13 | MIS boundaries | 474 | 149.21 | approximate depth | 2,3,4,11 | ||
| 182-1130A | -33.4202 | 127.6023 | -487 | T MIS 15 | MIS boundaries | 568 | 164.73 | approximate depth | 2,3,4,11 | ||
| 182-1130A | -33.4202 | 127.6023 | -487 | B. bigelowii acme | Nannofossil datum level | 234.34 | 5 | ||||
| 182-1130A | -33.4202 | 127.6023 | -487 | Omission surface | Breaks in sedimentation | 222.30 | |||||
| 182-1130A | -33.4202 | 127.6023 | -487 | Omission surface | Breaks in sedimentation | 229.80 | |||||
| 182-1130A | -33.4202 | 127.6023 | -487 | Omission surface | Breaks in sedimentation | 238.80 | |||||
| 182-1130A | -33.4202 | 127.6023 | -487 | Unconformable base of Sequence | 259.25 | 2 | |||||
| 182-1130A | -33.4202 | 127.6023 | -487 | 2.73 mbsf | Radiocarbon dates | 13.30 | 0.09 | 6 | |||
| 182-1130A | -33.4202 | 127.6023 | -487 | 2.73 mbsf | Radiocarbon dates | 13.60 | 0.15 | 6 | |||
| 182-1130A | -33.4202 | 127.6023 | -487 | 5.73 mbsf | Radiocarbon dates | 19.00 | 0.15 | 6 | |||
| 182-1130A | -33.4202 | 127.6023 | -487 | 5.73 mbsf | Radiocarbon dates | 24.50 | 0.30 | 6 | |||
| 182-1130A | -33.4202 | 127.6023 | -487 | 10.45 mbsf | Radiocarbon dates | 26.90 | 0.19 | 6 | |||
| 182-1130A | -33.4202 | 127.6023 | -487 | 10.45 mbsf | Radiocarbon dates | 27.70 | 0.36 | 6 | |||
| 182-1130A | -33.4202 | 127.6023 | -487 | 16.47 mbsf | Radiocarbon dates | 38.40 | 0.39 | 6 | |||
| 182-1132B | -33.3162 | 127.6022 | -218 | T Globorotalia crassaformis local disappearance | Planktonic foraminifer datum level | 130 | 39.98 | 0.74 | |||
| 182-1132B | -33.3162 | 127.6022 | -218 | B reappearance Globorotalia hirsuta | Planktonic foraminifer datum level | #120 | 130 | 41.48 | 0.76 | 8 | |
| 182-1132B | -33.3162 | 127.6022 | -218 | B Globorotalia hirsuta | Planktonic foraminifer datum level | 450 | 137.22 | 1.50 | 9 | ||
| 182-1132B | -33.3162 | 127.6022 | -218 | T Globorotalia tosaensis | Planktonic foraminifer datum level | 650 | 159.22 | 2.00 | 9 | ||
| 182-1132B | -33.3162 | 127.6022 | -218 | B Globorotalia truncatulinoides (Atl. and Ind.) | Planktonic foraminifer datum level | 2000 | 1180 | 197.89 | 1.20 | 9 | |
| 182-1132B | -33.3162 | 127.6022 | -218 | Brunhes (o) | Magnetostratigraphic boundaries | 780 | 175.50 | 5.50 | 1,10 | ||
| 182-1132B | -33.3162 | 127.6022 | -218 | Jaramillo (t) | Magnetostratigraphic boundaries | 990 | 186.00 | highly speculative assignment of reversals to chron boundaries (M. Fuller, pers. comm.) | 1,10 | ||
| 182-1132B | -33.3162 | 127.6022 | -218 | Jaramillo (o) | Magnetostratigraphic boundaries | 1070 | 193.00 | highly speculative assignment of reversals to chron boundaries (M. Fuller, pers. comm.) | 1,10 | ||
| 182-1132B | -33.3162 | 127.6022 | -218 | Olduvai (t) | Magnetostratigraphic boundaries | 1770 | 225.50 | highly speculative assignment of reversals to chron boundaries (M. Fuller, pers. comm.) | 1,10 | ||
| 182-1132B | -33.3162 | 127.6022 | -218 | T MIS 3 | MIS boundaries | 24 | 4.00 | approximate depth | 2,3,4,11 | ||
| 182-1132B | -33.3162 | 127.6022 | -218 | T MIS 6 | MIS boundaries | 129 | 41.50 | approximate depth | 2,3,4,11 | ||
| 182-1132B | -33.3162 | 127.6022 | -218 | T MIS 7 | MIS boundaries | 186 | 52.00 | approximate depth | 2,3,4,11 | ||
| 182-1132B | -33.3162 | 127.6022 | -218 | T MIS 8 | MIS boundaries | 242 | 83.00 | approximate depth | 2,3,4,11 | ||
| 182-1132B | -33.3162 | 127.6022 | -218 | T MIS 9 | MIS boundaries | 301 | 92.00 | approximate depth | 2,3,4,11 | ||
| 182-1132B | -33.3162 | 127.6022 | -218 | T MIS 10 | MIS boundaries | 334 | 107.00 | approximate depth | 2,3,4,11 | ||
| 182-1132B | -33.3162 | 127.6022 | -218 | T MIS 11 | MIS boundaries | 364 | 115.00 | approximate depth | 2,3,4,11 | ||
| 182-1132B | -33.3162 | 127.6022 | -218 | T MIS 12 | MIS boundaries | 427 | 136.00 | approximate depth | 2,3,4,11 | ||
| 182-1132B | -33.3162 | 127.6022 | -218 | T MIS 13 | MIS boundaries | 474 | 145.00 | approximate depth | 2,3,4,11 | ||
| 182-1132B | -33.3162 | 127.6022 | -218 | B. bigelowii acme | Nannofossil datum level | 222.91 | 5 | ||||
| 182-1132B | -33.3162 | 127.6022 | -218 | Omission surface | Breaks in sedimentation | 158.48 | |||||
| 182-1132B | -33.3162 | 127.6022 | -218 | Omission surface | Breaks in sedimentation | 163.41 | |||||
| 182-1132B | -33.3162 | 127.6022 | -218 | Omission surface | Breaks in sedimentation | 188.09 | |||||
| 182-1132B | -33.3162 | 127.6022 | -218 | Unconformable base of Sequence | 2000 | 236.30 | 2 |