Articles | Volume 19, issue 3
https://doi.org/10.5194/bg-19-743-2022
https://doi.org/10.5194/bg-19-743-2022
Research article
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08 Feb 2022
Research article | Highlight paper |  | 08 Feb 2022

Late Neogene evolution of modern deep-dwelling plankton

Flavia Boscolo-Galazzo, Amy Jones, Tom Dunkley Jones, Katherine A. Crichton, Bridget S. Wade, and Paul N. Pearson

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Cited articles

Ando, A., Huber, B. T., and MacLeod, K. G.: Depth-habitat reorganization of planktonic foraminifera across the Albian/Cenomanian boundary, Paleobiology, 36, 357–373, 2010. 
Aze, T., Ezard, T. H. G., Purvis, A., Coxall, H. K., Stewart, D. R. M., Wade, B. S., and Pearson, P. N.: A phylogeny of Cenozoic macroperforate planktonic foraminifera from fossil data, Biol. Rev., 86, 900–927, 2011. 
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Bergen, J. A., de Kaenel, E., Blair, S. A., Boesiger, T. M., and Browning, E.: Oligocene–Pliocene taxonomy and stratigraphy of the genus Sphenolithus in the circum North Atlantic Basin: Gulf of Mexico and ODP Leg 154, J. Nannoplankton Res., 37, 77–112, 2017. 
Berggren, W. A.: Late Neogene planktonic foraminiferal biostratigraphy of the Rio Grande Rise (South Atlantic), Mar. Micropaleontol., 2, 265–313, 1977. 
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Deep-living organisms are a major yet poorly known component of ocean biomass. Here we reconstruct the evolution of deep-living zooplankton and phytoplankton. Deep-dwelling zooplankton and phytoplankton did not occur 15 Myr ago, when the ocean was several degrees warmer than today. Deep-dwelling species first evolve around 7.5 Myr ago, following global climate cooling. Their evolution was driven by colder ocean temperatures allowing more food, oxygen, and light at depth.
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