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Oxygen isotope composition of the final chamber of planktic foraminifera provides evidence of vertical migration and depth-integrated growth

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Academic year: 2021

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Figure 1. Schematic to show the competing individual and population dynamics that may contribute to the variance within the δ 18 O of a population
Figure 2. Representatives of species used within this study. Light microscope from core top location and scanning electron microscope (SEM) images used to highlight particular features were collected using plankton tows and plankton pumps from the Arabian
Figure 3. Location Map of RETRO multi-core GS07-150-24 plotted on a basemap of sea surface δ 18 O eq seasonality
Figure 4. Physical properties of T. sacculifer. (a) Size vs. weight of T. sacculifer; the data are overlaid on a theoretical calculation of what the shell weight would be of a spherical hollow foraminifer with consistent porosity, assuming the density of c
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