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Morphometric and stable isotopic differentiation of Orbulina universa morphotypes from the Cariaco Basin, Venezuela

  • Author(s): Marshall, BJ
  • Thunell, RC
  • Spero, HJ
  • Henehan, MJ
  • Lorenzoni, L
  • Astor, Y
  • et al.
Abstract

© 2015 Elsevier B.V. Biometric characteristics of Orbulina universa (d'Orbigny) were used to differentiate two morphotypes present in sediment trap samples collected from the Cariaco Basin, Venezuela. Specifically, wall thickness and weight-area relationships were used to separate shells into thin (Mthin) and thick (Mthick) morphotypes. Mthick(mean thickness=19-41μm) comprises 75% of the total O. universa in these samples and has morphometric characteristics similar to that of the previously described Type I Caribbean genotype, whereas Mthin(mean thickness=6-22μm) is comparable to the Type III Mediterranean genotype. The flux of Mthickincreases during periods of upwelling, whereas Mthinflux shows no systematic relationship with changing hydrographic regimes in the basin. The δ18O and δ13C of Mthickare on average 0.34% higher and 0.38% lower, respectively, than those of Mthin, suggesting that they calcify their final spherical chamber at different depths in the water column and/or differ in their vital effects on shell geochemistry. Additionally, the absolute offset in the stable isotopic compositions of the two morphotypes varies as a function of surface ocean stratification. During periods of upwelling, the δ18O and δ13C absolute offsets between Mthinand Mthickare on average -0.15 and 0.25%, whereas average δ18O and δ13C absolute offsets between these two morphotypes increase to -0.54 and 0.41% during non-upwelling periods. We attribute the higher δ18O and δ13C offsets during non-upwelling periods to a difference in final chamber calcification depth and the combined effects of temperature (δ18O), δ13CDIC(δ13C), irradiance (δ13C) and [CO32-] (δ18O and δ13C). These data provide field evidence that thin and thick morphotypes of O. universa likely experience different environmental conditions during the formation of their final chamber and, therefore, should not be combined in geochemical analyses for reconstructing past surface ocean conditions. Finally, we introduce a new proxy for reconstructing past surface ocean stratification changes via the use of Mthinand Mthickδ18O and δ13C offsets.

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