Articles | Volume 44, issue 2
https://doi.org/10.5194/jm-44-601-2025
https://doi.org/10.5194/jm-44-601-2025
Research article
 | 
02 Dec 2025
Research article |  | 02 Dec 2025

Low-latitude biostratigraphy and diversity of planktonic foraminifera from the middle Eocene to early Oligocene

Adam Woodhouse, Bridget S. Wade, Tom Dunkley Jones, Carina Hoorn, and Kirsty M. Edgar

Related authors

IODP3 Expedition 505S “ENIGMA: ExploratioN Into a Global early Miocene Anomaly” Scientific Prospectus
Adam Woodhouse and Jennifer Kasbohm
Proc. Int. Ocean Drill. Prog., 505S, 1, https://doi.org/10.5194/piodp-505S-1-2026,https://doi.org/10.5194/piodp-505S-1-2026, 2026
Short summary

Cited articles

Agnini, C., Fornaciari, E., Giusberti, L., Grandesso, P., Lanci, L., Luciani, V., Muttoni, G., Pälike, H., Rio, D., Spofforth, D. J., and Stefani, C.: Integrated biomagnetostratigraphy of the Alano section (NE Italy): A proposal for defining the middle-late Eocene boundary, Bulletin, 123, 841–872, https://doi.org/10.1130/B30158.1, 2011. 
Agnini, C., Fornaciari, E., Raffi, I., Catanzariti, R., Pälike, H., Backman, J., and Rio, D.: Biozonation and biochronology of Paleogene calcareous nannofossils from low and middle latitudes, Newslett. Stratigr., 47, 131–181, 2014. 
Aljahdali, M. H., Elhag, M., Mufrreh, Y., Memesh, A., Alsoubhi, S., and Zalmout, I. S.: Upper Eocene calcareous nannofossil biostratigraphy: a new preliminary priabonian record from northern Saudi Arabia, Applied Ecology and Environmental Research, 18, https://doi.org/10.15666/aeer/1804_56075625, 2020. 
Al-Sabouni, N., Kucera, M., and Schmidt, D. N.: Vertical niche separation control of diversity and size disparity in planktonic foraminifera, Mar. Micropaleontol., 63, 75–90, 2007. 
Anagnostou, E., John, E. H., Edgar, K. M., Foster, G. L., Ridgwell, A., Inglis, G. N., Pancost, R. D., Lunt, D. J., and Pearson, P. N.: Changing atmospheric CO2 concentration was the primary driver of early Cenozoic climate, Nature, 533, 380–384, https://doi.org/10.1038/nature17423, 2016. 
Download
Short summary
Between 44–34 million years ago, Earth's climate substantially cooled, leading to permanent Antarctic glaciation and major ocean changes. This caused high extinction rates amongst marine organisms, including the planktonic foraminifera. New data from the western Atlantic Ocean highlight how these organisms responded, where surface species declined and deeper species increased in abundance, reflecting shifts in vertical ocean structure during this key climate transition.
Share