Preprints
https://doi.org/10.5194/egusphere-2025-555
https://doi.org/10.5194/egusphere-2025-555
17 Feb 2025
 | 17 Feb 2025

Increasing opal productivity in the late Eocene Southern Ocean: Evidence for increased carbon export preceding the Eocene-Oligocene glaciation

Volkan Özen, David Lazarus, Johan Renaudie, and Gabrielle Rodrigues de Faria

Abstract. The Eocene/Oligocene Transition represents a period of profound changes in diatom productivity and evolutionary history within the Cenozoic era. Unraveling how these changes correlate with climatic shifts during this transition is crucial for understanding the potential role of diatoms in the cooling trends observed at the Eocene/Oligocene boundary (~33.9 Ma). Current research predominantly relies on bulk opal accumulation measurements to assess productivity dynamics, which fails to distinguish the contribution of different biosiliceous (e.g., diatom versus radiolarian) plankton to total biogenic silica productivity. Furthermore, despite the fundamental role of community composition and diversity in diatom productivity and carbon sequestration, these factors are often not incorporated in existing studies focusing on the late Paleogene diatom productivity. The main objective of our work is to explore the potential roles of diatom communities in the late Eocene climatic changes by focusing on diatom- and radiolarian-specific productivity across multiple Southern Ocean sites, rather than bulk opal measurements, and by incorporating total diatom abundance into the analysis of diatom diversity evolution throughout the Eocene/Oligocene transition. By quantifying diatom and radiolarian abundances across four Southern Ocean sites in the Atlantic and Indian Ocean sectors, and analyzing diatom productivity through recent reconstructions of diatom diversity from approximately 40–30 Ma interval, our findings reveal a significant increase in diatom abundance coupled with notable shifts in community diversity. These changes suggest a potential ecological shift, likely associated with the development of stronger circum-Antarctic currents in the late Eocene. Such shifts could have influenced the efficiency of the biological carbon pump by enhancing organic carbon export to the deep ocean and thus potentially contributing to reduced atmospheric CO2 levels. While our findings indicate that the expansion of diatoms may have been a part of the mechanisms underlying the late Eocene cooling, they also highlight the importance of integrating diatom diversity and community evolution into diatom productivity research. Furthermore, our results offer valuable insights into the complex relationship between diatom abundance and diversity in the geological record, reflecting the intricate interplay of environmental and climatic factors.

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Volkan Özen, David Lazarus, Johan Renaudie, and Gabrielle Rodrigues de Faria

Status: final response (author comments only)

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on egusphere-2025-555', Anonymous Referee #1, 11 Mar 2025
    • AC2: 'Reply on RC1', Volkan Özen, 29 Apr 2025
  • RC2: 'Comment on egusphere-2025-555', Anonymous Referee #2, 12 Mar 2025
    • AC3: 'Reply on RC2', Volkan Özen, 29 Apr 2025
  • RC3: 'Comment on egusphere-2025-555', Anonymous Referee #3, 14 Mar 2025
    • AC4: 'Reply on RC3', Volkan Özen, 29 Apr 2025
  • AC1: 'Comment on egusphere-2025-555', Volkan Özen, 09 Apr 2025
Volkan Özen, David Lazarus, Johan Renaudie, and Gabrielle Rodrigues de Faria
Volkan Özen, David Lazarus, Johan Renaudie, and Gabrielle Rodrigues de Faria

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Latest update: 09 Sep 2025
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Short summary
We studied diatom fossils from the Southern Ocean to understand how ocean productivity changed ~40–30 million years ago during a major climate shift marked by the onset of permanent Antarctic glaciation and global cooling. We found striking shifts in diatom productivity, revealing critical changes in ocean circulation and nutrient supply. Our results show how these microscopic organisms may have influenced climate, acting as a geological force that shaped global climate over time.
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