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  • 182-1127B; 182-1129C; 182-1130A; 182-1131A; 182-1132B; Age model; Age model, optional; Ageprofile Datum Description; Ageprofile Datum Type; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Elevation of event; Error, absolute; Event label; Great Australian Bight; Joides Resolution; Latitude of event; Leg182; Longitude of event; Ocean Drilling Program; ODP; Reference/source; Sample comment  (1)
  • 2000-2004  (1)
  • 1975-1979
Collection
Keywords
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  • 2000-2004  (1)
  • 1975-1979
Year
  • 1
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    PANGAEA
    In:  Supplement to: 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): 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
    Publication Date: 2024-01-09
    Description: 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.
    Keywords: 182-1127B; 182-1129C; 182-1130A; 182-1131A; 182-1132B; Age model; Age model, optional; Ageprofile Datum Description; Ageprofile Datum Type; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Elevation of event; Error, absolute; Event label; Great Australian Bight; Joides Resolution; Latitude of event; Leg182; Longitude of event; Ocean Drilling Program; ODP; Reference/source; Sample comment
    Type: Dataset
    Format: text/tab-separated-values, 566 data points
    Location Call Number Expected Availability
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