Rippert, Nadine; Nürnberg, Dirk; Raddatz, Jacek; Maier, Edith; Hathorne, Ed C; Bijma, Jelle; Tiedemann, Ralf (2016): Multinet and water column properties of station SO225-21. PANGAEA, https://doi.org/10.1594/PANGAEA.864455, Supplement to: Rippert, N et al. (2016): Constraining foraminiferal calcification depths in the western Pacific warm pool. Marine Micropaleontology, 128, 14-27, https://doi.org/10.1016/j.marmicro.2016.08.004
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Insight into past changes of upper ocean stratification, circulation, and nutrient signatures rely on our knowledge of the apparent calcification depth (ACD) and ecology of planktonic foraminifera, which serve as archives for paleoceanographic relevant geochemical signals. The ACD of different species varies strongly between ocean basins, but also regionally. We constrained foraminiferal ACDs in the western Pacific warm pool (Manihiki Plateau) by comparing stable oxygen and carbon isotopes (d18Ocalcite, d13Ccalcite) as well as Mg/Ca ratios from living planktonic foraminifera to in-situ physical and chemical water mass properties (temperature, salinity, d18Oseawater, d13CDIC). Our analyses point to Globigerinoides ruber as the shallowest dweller, followed by Globigerinoides sacculifer, Neogloboquadrina dutertrei, Pulleniatina obliquiloculata and Globotaloides hexagonus inhabiting increasingly greater depths. These findings are consistent with other ocean basins; however, absolute ACDs differ from other studies. The uppermost mixed-layer species G. ruber and G. sacculifer denote mean calcification depths of ~95 m and ~120 m, respectively. These Western Pacific ACDs are much deeper than in most other studies and most likely relate to the thick surface mixed layer and the deep chlorophyll maximum in this region. Our results indicate that N. dutertrei appears to be influenced by mixing waters from the Pacific equatorial divergence, while P. obliquiloculata with an ACD of ~160 m is more suitable for thermocline reconstructions. ACDs of G. hexagonus reveal a deep calcification depth of ~450 m in oxygen-depleted, but nutrient-rich water masses, consistent to other studies. As the d13C of G. hexagonus is in near-equilibrium with ambient seawater, we suggest this species is suitable for tracing nutrient conditions in equatorial water masses originating in extra-topical regions.
Median Latitude: -3.037917 * Median Longitude: -165.034300 * South-bound Latitude: -3.050000 * West-bound Longitude: -165.057333 * North-bound Latitude: -3.001667 * East-bound Longitude: -164.967500
Date/Time Start: 2012-12-07T16:45:00 * Date/Time End: 2012-12-08T18:12:00
Datasets listed in this publication series
- Rippert, N; Nürnberg, D; Raddatz, J et al. (2016): Abundance of planktic foraminifera measured on multinet samples at station SO225_21. https://doi.org/10.1594/PANGAEA.864438
- Rippert, N; Nürnberg, D; Raddatz, J et al. (2016): Physical oceanography at station SO225_21. https://doi.org/10.1594/PANGAEA.864435
- Rippert, N; Nürnberg, D; Raddatz, J et al. (2016): Stable isotopes and Mg/Ca measured on multinet samples at station SO225_21. https://doi.org/10.1594/PANGAEA.864437
- Rippert, N; Nürnberg, D; Raddatz, J et al. (2016): Stable isotopes measured on water bottle samples at station SO225_21. https://doi.org/10.1594/PANGAEA.864436