From Geoscience Australia
JSON format icon JSON RDF format icon RDF ISO19115-3 XML

d18O Seasonality of Planktonic Foraminifera from Southern Ocean Sediment Traps: Latitudinal Gradients and Implications for Paleoclimate Reconstructions

Created 17/10/2025

Updated 17/10/2025

JSON format icon JSON RDF format icon RDF ISO19115-3 XML

The oxygen isotopic record obtained from Globigerina bulloides, Globorotalia inflata, and Neogloboquadrina pachyderma (s.) was analysed for 5 sediment traps moored in the Southern Ocean and Southwest Pacific. The traps extend from Subtropical to the Polar Frontal environments, providing the first analysis of seasonal foraminiferal d18O records from these latitudes. Comparison between the foraminiferal records and various equations for predicted d18O of calcite reveals that the predicted d18O is best captured by the equations of Epstein et al. (1953) [Epstein, S., Buchsbaum, R., Lowenstam, H.A., Urey, H.C., 1953. Revised carbonate-water isotopic temperature scale. Geological Society of America Bulletin 64, 1315-1326.] and Kim and O'Neil (1997) [Kim, S.-T., O'Neil, J.R., 1997. Equilibrium and non-equilibrium oxygen isotope effects in synthetic carbonates. Geochimica et Cosmochimica Acta 61, 3461-3475.]. The Epstein equation shows a constant offset from the -18O of G. bulloides and N. pachyderma (s.) across the full range of latitudes. The seasonal range in -18O values for these two species implies a near-surface habitat across all sites, while G. inflata most likely dwells at 50 m depth. A significant finding in this study was that offsets from predicted -18O for G. bulloides do not correlate to changes in the carbonate ion concentration. This suggests that [CO32-] in and of itself may not capture the full range of carbonate chemistry conditions in the marine system. This sediment trap deployment also reveals distinct seasonal flux patterns for each species. Comparison between flux-weighted isotopic values calculated from the sediment traps and the isotopic composition of nearby surface sediments indicates that the sedimentary records retain this seasonal imprint. At the 51°S site, G. bulloides has a spring flux peak while N. pachyderma (s.) is dominated by summer production.

Files and APIs

Tags

Additional Info

Field Value
Title d18O Seasonality of Planktonic Foraminifera from Southern Ocean Sediment Traps: Latitudinal Gradients and Implications for Paleoclimate Reconstructions
Language eng
Licence Not Specified
Landing Page https://data.gov.au/data/dataset/59903543-1506-4d2e-8853-a7744e92888a
Contact Point
Geoscience Australia Data
clientservices@ga.gov.au
Reference Period 22/04/2018
Geospatial Coverage
Map data © OpenStreetMap contributors
{
  "coordinates": [
    [
      [
        120.0,
        -80.0
      ],
      [
        150.0,
        -80.0
      ],
      [
        150.0,
        -30.0
      ],
      [
        120.0,
        -30.0
      ],
      [
        120.0,
        -80.0
      ]
    ]
  ],
  "type": "Polygon"
}
Data Portal Geoscience Australia

Data Source

This dataset was originally found on Geoscience Australia "d18O Seasonality of Planktonic Foraminifera from Southern Ocean Sediment Traps: Latitudinal Gradients and Implications for Paleoclimate Reconstructions". Please visit the source to access the original metadata of the dataset:
https://ecat.ga.gov.au/geonetwork/srv/eng/csw/dataset/d18o-seasonality-of-planktonic-foraminifera-from-southern-ocean-sediment-traps-latitudinal-grad