Carbon Isotopic Fractionation of Alkenones and Gephyrocapsa Coccoliths Over the Late Quaternary (Marine Isotope Stages 12–9) Glacial‐Interglacial Cycles at the Western Tropical Atlantic. Issue 8 (28th July 2021)

• Record Type: Journal Article
• Authors: González‐Lanchas, A.; Hernández‐Alméida, I.; Flores, J.‐A.; Sierro, F. J.; Guitian, J.; Stoll, H. M.
• Is Part Of: Paleoceanography and paleoclimatology. Volume 36:Issue 8(2021)
• Page Start: n/a
• Page End: n/a
• Publication Date: 2021-07-28
• Subjects: coccolithophores -- alkenones -- photosynthetic carbon isotopic fractionation -- CO2 -- multiproxy -- stable isotope vital effects; Paleoceanography -- Periodicals; Paleoclimatology -- Periodicals; 551.46
• DOI: 10.1029/2020PA004175
• Languages: English
• ISSNs: 2572-4517

Abstract

Abstract: The sensitivity of coccolithophores to changing CO2 and its role modulating cellular photosynthetic carbon isotopic fractionation (εp ) is crucial to understand the future adaptation of these organisms to higher CO2 world and to assess the reliability of εp for past CO2 estimation. Here, we present εp measured on natural fossil samples across the glacial‐interglacial (G‐I) CO2 variations of marine isotope stages 12 to 9 interval (454–334 ka) at the western tropical Atlantic Ocean Drilling Program Site 925 together with a set of organic and inorganic geochemical, micropaleontological and morphometrical data from Gephyrocapsa coccoliths in the same samples. The ∼2‰ variation in εp is significantly correlated with the CO2 [aq] concentrations calculated from assumption of air‐sea equilibrium with measured ice core p CO2 concentrations. The sensitivity of εp to CO2 [aq] is similar to that derived from a multiple regression model of culture observations and is not well simulated with the classical purely diffusive model of algal CO2 acquisition. The measured range of Gephyrocapsa cell sizes is insufficient to explain the non‐CO2 effects on εp at this location, via either direct size effect or growth rate correlated to cell size. Primary productivity, potentially triggered by shifting growth rates and light levels, may also affect εp. Proposed productivity proxies % Florisphaera profunda and the ratio between the C37 to C38.et alkenone (C37/C38.et ratio) both correlates modestly with the non‐CO2 effects on εp . When the observed G‐I εp to CO2 sensitivity at this site is used to estimate p CO2 from εp since the Miocene, the inferred p CO2 declines are larger in amplitude compared to that calculated from a theoretical εp diffusive model. We find that oxygen and carbon stable isotope vital effects in the near monogeneric‐separated Gephyrocapsa coccoliths (respectively Δδ 18 O Gephyrocapsa–Trilobatus sacculifer and εcoccolith ) are coupled through the time series, but the origins of these vital effects are not readily explained by existing models. Key Points: Coccolithophore εp sensitivity to CO2 [aq] is consistent with that observed in cultures but contrasts with predictions of classical diffusive models of CO2 acquisition Geochemical, micropaleontological, and morphometrical proxies are assessed as indicators of the non‐CO2 effects on εp Gephyrocapsa coccoliths show coupled variations in oxygen and carbon isotope vital effects over the time series