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Alexander, Ian T; Kroon, Dick; Thompson, Roy (1993): Sedimentology, mineral magnetism, andoxygen isotope stratigraphy of ODP Hole 133-819A [dataset publication series]. PANGAEA, https://doi.org/10.1594/PANGAEA.785608, Supplement to: Alexander, IT et al. (1993): Late Quaternary paleoenvironmental change on the northeast Australian Margin as evidenced in oxygen isotope stratigraphy, mineral magnetism, and sedimentology. In: McKenzie, JA; Davies, PJ; Palmer-Julson, A; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 133, 129-161, https://doi.org/10.2973/odp.proc.sr.133.224.1993

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Abstract:
To investigate late Quaternary paleoclimatic and paleoceanographic change in the sedimentary record, preserved on the Australian Continental Margin during the late Quaternary, core material was collected from Ocean Drilling Program, Leg 133, Site 819. An expanded sequence of late Quaternary, rhythmically bedded, predominantly hemipelagic sediments were recovered from Hole 819A. The foraminiferal d18O record preserved at Hole 819A suggests that the late Quaternary section is incomplete. Both benthic and planktonic d18O stratigraphies can be traced tentatively downcore to stage 6 at about 32.5 mbsf, where a major hiatus occurs. At this level, a slump detachment surface has been identified (Shipboard Scientific Party, 1991). This slump has removed marine oxygen isotope stages 7 to 13. Below 32.5 mbsf, continuous correlation can be achieved in the planktonic d18O curve, with existing deep-sea foraminiferal oxygen isotope stratigraphies from stage 14 through stage 28.
The major hiatus at 32.5 mbsf marks the position of a significant change in the character of the sedimentation at Site 819. Sediments below 32.5 mbsf, relative to those above 32.5 mbsf, are characterized by less variation in mean particle size; lower percentages of carbonate content in the coarse fraction (>63 µm); a stronger relationship between the percentage of fine fraction and magnetic mineral concentration, and lower foraminiferal abundances. Above the hiatus, large fluctuations in mean particle size occurred, which have been interpreted to be the result of high foraminiferal abundances. Early highstands show high terrigenous influx in the fine fraction above the hiatus. This is the opposite of the general idea of high terrigenous influx during lowstands of sea level on siliciclastic dominated continental margins. We are far from understanding the origin of this material and further investigation will be required (see also Glenn et al., this volume).
All our records, except the planktonic foraminiferal oxygen isotope record, indicate that the major hiatus marks the position of a significant change in the environment at Site 819. The planktonic foraminiferal d18O record suggests that environmental change occurred prior to the formation of the hiatus (i.e., near the Brunhes/Matuyama [B/M] boundary). The interval between the B/M boundary and the hiatus represents a transitional period between two different patterns of ocean circulation.
Throughout most of the lower part of the sequence, Site 819 was at a shallow-water depth and local oceanographic conditions were dominated by sluggish Subtropical Central Water (SCW) flow. However, near the B/M boundary, ocean circulation patterns intensified, reflecting a worldwide change in paleoenvironment. Enhanced ocean circulation patterns were possibly aided by tectonic subsidence. During this period Site 819 became progressively more under the influence of Antarctic Intermediate Water (AAIW), than SCW.
In the upper part of the sequence at Hole 819 A, we see a continuation of the pattern of oceanographic reorganization suggested during stages 21 through 14. Intensification of the subsurface oceanographic circulation was also accompanied by the progressive wedging southward of surface waters associated with the East Australian Current (EAC).
The change in the nature of the records in the lower and upper parts of the sequence at Site 819 are thought to reflect perturbations by the orbital eccentricity cycle.
Project(s):
Ocean Drilling Program (ODP)
Coverage:
Latitude: -16.624000 * Longitude: 146.324700
Date/Time Start: 1990-09-10T01:24:00 * Date/Time End: 1990-09-12T06:50:00
Event(s):
133-819A * Latitude: -16.624000 * Longitude: 146.324700 * Date/Time Start: 1990-09-10T01:24:00 * Date/Time End: 1990-09-12T06:50:00 * Elevation: -577.0 m * Penetration: 400 m * Recovery: 339.52 m * Location: Coral Sea * Campaign: Leg133 * Basis: Joides Resolution * Method/Device: Drilling/drill rig (DRILL) * Comment: 44 cores; 400 m cored; 0 m drilled; 84.9 % recovery
License:
Creative Commons Attribution 3.0 Unported (CC-BY-3.0)
Size:
4 datasets

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Datasets listed in this publication series

  1. Alexander, IT; Kroon, D; Thompson, R (1993): (Table 4) Carbonate content in ODP Hole 133-819A. https://doi.org/10.1594/PANGAEA.785606
  2. Alexander, IT; Kroon, D; Thompson, R (1993): (Table 2) Stable oxygen isotope record of foraminifera of ODP Hole 133-819A. https://doi.org/10.1594/PANGAEA.785599
  3. Alexander, IT; Kroon, D; Thompson, R (1993): (Table 1) Magnetic susceptibility and laboratory-imparted magnetization at ODP Hole 133-819A. https://doi.org/10.1594/PANGAEA.785596
  4. Alexander, IT; Kroon, D; Thompson, R (1993): (Table 3) Particle size distribution in ODP Hole 133-819A. https://doi.org/10.1594/PANGAEA.785604