EGU21-15795
https://doi.org/10.5194/egusphere-egu21-15795
EGU General Assembly 2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.

Tracking the South Pacific convergence zone variability and recent acidification reconstructed from tropical corals

Sara Todorović1,2, Henry C. Wu1, Braddock Linsley3, Delphine Dissard4, Henning Kuhnert5, Albert Benthien6, Klaus-Uwe Richter6, Markus Raitzsch5,6, and Jelle Bijma6
Sara Todorović et al.
  • 1Leibniz Centre for Tropical Marine Research, Biogeochemistry and Geology, Germany (sara.todorovic@leibniz-zmt.de)
  • 2Faculty of Geosciences, University of Bremen, Bremen, Germany
  • 3Lamont-Doherty Earth Observatory of Columbia University, Palisades, NY, USA
  • 4IRD-Sorbonne Universités, UPMC, Univ Paris 06-CNRS-MNHN, LOCEAN, Paris, France
  • 5MARUM – Center for Marine Environmental Sciences, University of Bremen, Bremen, Germany
  • 6Alfred Wegener Institute – Helmholz Centre for Polar and Marine Research (AWI), Bremerhaven, Germany

Massive tropical corals represent one of the most important natural archives of modern climate change. Coral based reconstructions give us the possibility to extend the instrumental oceanographic records and observe hydrographic variability on seasonal to interdecadal scales in tropical oceans. South Pacific convergence zone (SPCZ) variability, Interdecadal Pacific Oscillation (IPO) and El Niño-Southern Oscillation (ENSO) events are major drivers of global climate and may exert control on regional CO2 absorption, outgassing and pH variability.

Porites sp. corals from Tonga and Rotuma (Fijian dependency) are being analyzed for multi-proxy (e.g. Sr/Ca, δ18O, δ13C, δ11B, B/Ca) reconstructions of sea surface temperature and salinity (SST, SSS) and carbonate chemistry, on a monthly to annual resolution. Preliminary data of the Rotuma Porites sp. coral shows δ18O has been decreasing by 0.004 ‰ per year at the end of the 20th century, suggesting freshening and/or warming of the surface water. In the same period, we observe a δ13C decrease of 0.017 ‰ per year in-line with the anthropogenic CO2 driven Suess effect. Initial results of the δ11B Tonga Porites sp. show high interannual variability, and a strong trend of decrease of -0.0626 ‰ per year in the last five decades of the record (1949-2004) suggesting acidification. The results are in agreement with published coral-based reconstructions from the region.

When completed, the new records will facilitate exploring the effects of modern anthropogenic influence on ocean carbonate system and pH variation, and the relationship between them and interannual and decadal-interdecadal climatic fluctuations.

How to cite: Todorović, S., C. Wu, H., Linsley, B., Dissard, D., Kuhnert, H., Benthien, A., Richter, K.-U., Raitzsch, M., and Bijma, J.: Tracking the South Pacific convergence zone variability and recent acidification reconstructed from tropical corals, EGU General Assembly 2021, online, 19–30 Apr 2021, EGU21-15795, https://doi.org/10.5194/egusphere-egu21-15795, 2021.

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