Pfuhl, Helen A; McCave, I Nick (2003): (Table T1) Fossil, magnetic reversal, and additional datums of ODP Leg 189 sites [dataset]. PANGAEA, https://doi.org/10.1594/PANGAEA.780220, Supplement to: Pfuhl, HA; McCave, IN (2003): Integrated age models for the early Oligocene-early Miocene, Sites 1168 and 1170-1172. In: Exon, NF; Kennett, JP; Malone, MJ (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 189, 1-21, https://doi.org/10.2973/odp.proc.sr.189.108.2003
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Abstract:
The aim of this study is to assess the viability of age models based on shipboard and postcruise bio- and magnetostratigraphic datums, as of August 2002, using independently derived control points. The control points are based on matching between-site trends in stable isotope records, carbonate content, and weight percent sand. Site 1170 on the western South Tasman Rise has a good record of magnetic reversals, which suggests a hiatus prior to ~30 Ma (early Oligocene) relating to the Marshall Paraconformity, followed by strongly reduced sedimentation in the late Oligocene. Preservation of the Mi-1 event at this site is evidence for continued sedimentation across the Oligocene/Miocene boundary. Correlation of the Mi-1a event to the record at Site 1090 on the Agulhas Ridge confirms the usefulness of the magnetostratigraphic record at this site. However, the timing of the Mi-1 event at Site 1170 appears different from that at Site 1090, but is constrained by four magnetic reversals. At Site 1171 additional control points are consistent with biostratigraphic datums. Site 1172 is marked by the lowest sedimentation rates of all sites. Additional control points before 22 Ma are more consistent with the biostratigraphy than with the magnetostratigraphy. At Site 1168 we suggest that the magnetic reversal record MR1 provides the best match with the biostratigraphy and additional control points, as well as changes in the biogenic and lithogenic composition of the sedimentary record.
The late Eocene/early Oligocene Marshall Paraconformity (base = ~33 Ma at the type location) is evident at Sites 1170-1172, and low sedimentation rates occur at the two eastern sites (1171 and 1172) in the early Oligocene. A change in sedimentation just after the early-late Oligocene transition appears to reduce rates at Site 1170 and strongly affect the biogenic composition of sediments at Site 1168, which is less exposed to the flow of the Antarctic Circumpolar Current. The Oligocene-Miocene transition finally is marked by reduced sedimentation at Sites 1170-1172, but a relatively stronger decrease is noticeable at Site 1168. Above this boundary sedimentation rates are identical at Sites 1168 and 1170 above 21.5 Ma and at Sites 1171 and 1172 above 17 Ma.
Project(s):
Ocean Drilling Program (ODP)
Coverage:
Median Latitude: -45.554837 * Median Longitude: 147.375642 * South-bound Latitude: -48.499900 * West-bound Longitude: 144.412683 * North-bound Latitude: -42.609467 * East-bound Longitude: 149.928433
Date/Time Start: 2000-02-29T00:00:00 * Date/Time End: 2000-04-22T00:00:00
Minimum DEPTH, sediment/rock: 159.35 m * Maximum DEPTH, sediment/rock: 740.00 m
Event(s):
189-1168 * Latitude: -42.609467 * Longitude: 144.412683 * Date/Time: 2000-02-29T00:00:00 * Elevation: -2463.6 m * Penetration: 1282.4 m * Recovery: 1191.5 m * Location: Indian Ocean * Campaign: Leg189 * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE) * Comment: 138 cores; 1282.4 m cored; 0 m drilled; 92.9% recovery
189-1170 * Latitude: -47.150467 * Longitude: 146.049767 * Date/Time: 2000-03-31T00:00:00 * Elevation: -2704.4 m * Penetration: 1600 m * Recovery: 1026.6 m * Location: Indian Ocean * Campaign: Leg189 * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE) * Comment: 128 cores; 1175 m cored; 425 m drilled; 87.4% recovery
189-1171 * Latitude: -48.499900 * Longitude: 149.111683 * Date/Time: 2000-04-11T00:00:00 * Elevation: -2147.9 m * Penetration: 1466.8 m * Recovery: 995.2 m * Location: South Pacific Ocean * Campaign: Leg189 * Basis: Joides Resolution * Method/Device: Composite Core (COMPCORE) * Comment: 132 cores; 1219.2 m cored; 247.6 m drilled; 81.6% recovery
Comment:
Sediment depth is given in mbsf. Ages are based on Cande and Kent (1992, doi:10.1029/92JB01202; 1995, doi:10.1029/94JB03098) .
Parameter(s):
# | Name | Short Name | Unit | Principal Investigator | Method/Device | Comment |
---|---|---|---|---|---|---|
1 | Event label | Event | ||||
2 | Age model | Age model | ka | Pfuhl, Helen A | ||
3 | Ageprofile Datum Description | Ageprof dat des | Pfuhl, Helen A | FO = first occurrence, LO = last occurrence; D = diatom, DF = dinocyst, NF = nannofossil, PF = planktonic foraminifer, RD = radiolarian; MR = magnetic reversal; MPC = Marshall Paraconformity | ||
4 | DEPTH, sediment/rock | Depth sed | m | Geocode |
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
202 data points
Data
1 Event | 2 Age model [ka] | 3 Ageprof dat des | 4 Depth sed [m] |
---|---|---|---|
189-1170 | 14076 | MR-Onset C5ACn | 283.50 |
189-1170 | 14178 | MR-Termination C5ADn | 286.00 |
189-1170 | 14380 | D-FO Actinocyclus ingens var. nodus | 291.42 |
189-1170 | 14612 | MR-Onset C5ADn | 292.00 |
189-1170 | 14800 | MR-Termination C5Bn.1n | 294.00 |
189-1170 | 14888 | MR-Onset C5Bn.1n | 296.00 |
189-1170 | 15034 | MR-Termination C5Bn.2n | 297.50 |
189-1170 | 16014 | MR-Termination C5Cn.1n | 308.00 |
189-1170 | 16293 | MR-Onset C5Cn.1n | 310.50 |
189-1170 | 16327 | MR-Termination C5Cn.2n | 311.00 |
189-1170 | 16488 | MR-Onset C5Cn.2n | 312.00 |
189-1170 | 17615 | MR-Onset C5Dn | 323.00 |
189-1170 | 18781 | MR-Onset C5En | 338.00 |
189-1170 | 19048 | MR-Termination C6n | 341.00 |
189-1170 | 21634 | 1090 Mi-1a | 365.76 |
189-1170 | 21700 | 1090 Mi-1a | 366.59 |
189-1170 | 21859 | MR-Onset C6AAn | 370.50 |
189-1170 | 22151 | MR-Termination C6AAr.1n | 372.20 |
189-1170 | 22459 | MR-Termination C6AAr.2n | 374.90 |
189-1170 | 22493 | MR-Onset C6AAr.2n | 375.40 |
189-1170 | 22588 | MR-Termination C6Bn.1n | 375.80 |
189-1170 | 22804 | MR-Termination C6Bn.2n-bottom of gap | 377.40 |
189-1170 | 23535 | MR-Onset C6Cn.1n | 380.00 |
189-1170 | 23677 | MR-Termination C6Cn.2n | 382.00 |
189-1170 | 23800 | MR-Onset C6Cn.2n | 382.90 |
189-1170 | 24118 | MR-Onset C6Cn.3n | 386.00 |
189-1170 | 24730 | MR-Termination C7n.1n | 393.40 |
189-1170 | 24781 | MR-Onset C7n.1n | 394.00 |
189-1170 | 25496 | MR-Termination C7An | 395.00 |
189-1170 | 25648 | MR-Onset C7An | 396.20 |
189-1170 | 25823 | MR-Termination C8n.1n | 397.00 |
189-1170 | 26100 | NF-LO Chiasmolithus altus | 397.46 |
189-1170 | 26554 | MR-Onset C8n.2n | 398.60 |
189-1170 | 27027 | MR-Termination C9n | 402.00 |
189-1170 | 27972 | MR-Onset C9n | 403.00 |
189-1170 | 28283 | MR-Termination C10n.1n | 406.50 |
189-1170 | 29401 | MR-Termination C11n.1n | 440.00 |
189-1170 | 30240 | D-FO Rocella vigilans - ~top MPC | 458.55 |
189-1171 | 14076 | MR-Onset C5ACn | 159.35 |
189-1171 | 14178 | MR-Termination C5ADn | 161.30 |
189-1171 | 14612 | MR-Onset C5ADn | 167.20 |
189-1171 | 19048 | MR-Termination C6n | 207.20 |
189-1171 | 20131 | MR-Onset C6n | 223.50 |
189-1171 | 21700 | 1170-benthic d13C | 240.23 |
189-1171 | 22400 | 1170-benthic d18O | 249.36 |
189-1171 | 22800 | 1170-bulk d13C | 251.00 |
189-1171 | 23150 | 1170-benthic d13C | 251.90 |
189-1171 | 23880 | 1170-benthic d18O | 258.56 |
189-1171 | 26400 | 1170-bulk d13C | 268.76 |
189-1171 | 26900 | 1170-benthic d13C | 269.26 |
189-1171 | 30240 | D-FO Rocella vigilans-~top MPC | 272.90 |
189-1172 | 14076 | MR-Onset C5ACn | 285.20 |
189-1172 | 14178 | MR-Termination C5ADn | 287.30 |
189-1172 | 14612 | MR-Onset C5ADn | 291.90 |
189-1172 | 14800 | MR-Termination C5Bn.1n | 293.30 |
189-1172 | 14888 | MR-Onset C5Bn.1n | 293.90 |
189-1172 | 15034 | MR-Termination C5Bn.2n | 296.30 |
189-1172 | 15155 | MR-Onset C5Bn.2n | 298.80 |
189-1172 | 16014 | MR-Termination C5Cn.1n | 302.30 |
189-1172 | 16726 | MR-Onset C5Cn.3n | 314.10 |
189-1172 | 17277 | MR-Termination C5Dn | 316.90 |
189-1172 | 18281 | MR-Termination C5En | 320.20 |
189-1172 | 18781 | MR-Onset C5En | 324.00 |
189-1172 | 19048 | MR-Termination C6n | 325.80 |
189-1172 | 20131 | MR-Onset C6n | 333.10 |
189-1172 | 21790 | 1170-bulk d13C | 339.86 |
189-1172 | 22490 | 1170-benthic d13C | 342.51 |
189-1172 | 22810 | 1170-bulk d13C | 342.86 |
189-1172 | 23150 | 1170-benthic d13C | 343.26 |
189-1172 | 23950 | 1170-benthic d18O | 344.37 |
189-1172 | 26340 | 1170-bulk d13C | 347.31 |
189-1172 | 29401 | MR-Termination C11n.1n | 356.10 |
189-1172 | 29662 | MR-Onset C11n.1n | 356.80 |
189-1172 | 29765 | MR-Termination C11n.2n | 357.30 |
189-1172 | 30098 | MR-Onset C11n.2n-~top MPC | 358.60 |
189-1168 | 14000 | NF-FO Triquetrorhabdulus rugosus | 244.30 |
189-1168 | 15100 | PF-FO Orbulina suturalis | 255.26 |
189-1168 | 16300 | PF- FO Praeorbulina curva | 264.90 |
189-1168 | 17400 | NF-FO Calcidiscus premacintyrei | 280.35 |
189-1168 | 18200 | NF-FO Sphenolithus heteromorphus | 293.80 |
189-1168 | 18300 | NF-LO Sphenolithus belemnos | 299.55 |
189-1168 | 19200 | NF-FO Sphenolithus belemnos | 313.90 |
189-1168 | 21400 | PF-LO Tenuitella munda | 341.10 |
189-1168 | 22600 | PF-FO Globoturborotalita woodi | 373.97 |
189-1168 | 23200 | PF-FO Globoquadrina dehiscens | 407.64 |
189-1168 | 23750 | 1170-Mi1 peaks | 414.00 |
189-1168 | 23900 | 1170-Mi1 peaks | 420.00 |
189-1168 | 24730 | MR-1-Termination C7n.1n | 428.05 |
189-1168 | 25183 | MR-1-Onset C7n.2n | 462.65 |
189-1168 | 25496 | MR-1-Termination C7An | 472.00 |
189-1168 | 27027 | MR-1-Termination C9n | 509.35 |
189-1168 | 27972 | MR-1-Onset C9n | 546.20 |
189-1168 | 28283 | MR-1-Termination C10n.1n | 572.90 |
189-1168 | 28512 | MR-1-Onset C10n.1n | 597.80 |
189-1168 | 28578 | MR-1-Termination C10n.2n | 602.45 |
189-1168 | 29401 | MR-1-Termination C11n.1n | 706.10 |
189-1168 | 29662 | MR-1-Onset C11n.1n | 716.70 |
189-1168 | 29765 | MR-1-Termination C11n.2n | 718.48 |
189-1168 | 30098 | MR-1-Onset C11n.2n | 729.90 |
189-1168 | 30479 | MR-1-Termination C12n | 733.95 |
189-1168 | 30939 | MR-1-Onset C12n | 740.00 |