Articles | Volume 19, issue 3
https://doi.org/10.5194/bg-19-743-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/bg-19-743-2022
© Author(s) 2022. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| Highlight paper
| 
08 Feb 2022
Research article | Highlight paper |
| 08 Feb 2022
| 08 Feb 2022
Late Neogene evolution of modern deep-dwelling plankton
Flavia Boscolo-Galazzo
CORRESPONDING AUTHOR
School of Earth and Environmental Sciences, Cardiff University, Cardiff, UK
now at: Department of Earth Science, Bergen University, Bergen, Norway
now at: Bjerknes Center for Climate Research, Bergen, Norway
Amy Jones
School of Geography, Earth and Environmental Sciences, Birmingham University, Birmingham, UK
Tom Dunkley Jones
School of Geography, Earth and Environmental Sciences, Birmingham University, Birmingham, UK
Katherine A. Crichton
School of Earth and Environmental Sciences, Cardiff University, Cardiff, UK
now at: Department of Geography, Exeter University, Exeter, UK
Bridget S. Wade
Department of Earth Sciences, University College London, London, UK
Paul N. Pearson
School of Earth and Environmental Sciences, Cardiff University, Cardiff, UK
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Cited
14 citations as recorded by crossref.
- The Late Neogene to Quaternary Surface Water Changes as Responses from Planktonic Foraminifera at the Transitional Subantarctic Zone B. Nirmal & K. Mohan 10.2139/ssrn.4133351
- Origination of the modern-style diversity gradient 15 million years ago I. Fenton et al. 10.1038/s41586-023-05712-6
- Biochronology and evolution of Pulleniatina (planktonic foraminifera) P. Pearson et al. 10.5194/jm-42-211-2023
- Alternating regimes of shallow and deep-sea diversification explain a species-richness paradox in marine fishes E. Miller et al. 10.1073/pnas.2123544119
- Paleoecology and evolutionary response of planktonic foraminifera to the mid-Pliocene Warm Period and Plio-Pleistocene bipolar ice sheet expansion A. Woodhouse et al. 10.5194/bg-20-121-2023
- What the geological past can tell us about the future of the ocean’s twilight zone K. Crichton et al. 10.1038/s41467-023-37781-6
- Globorotalia truncatulinoides in the Mediterranean Basin during the Middle–Late Holocene: Bio-Chronological and Oceanographic Indicator G. Margaritelli et al. 10.3390/geosciences12060244
- The late Neogene to Quaternary surface water changes as responses from planktonic foraminifera at the transitional Subantarctic Zone B. Nirmal & K. Mohan 10.1016/j.palaeo.2022.111183
- Biogeographic response of marine plankton to Cenozoic environmental changes A. Swain et al. 10.1038/s41586-024-07337-9
- A Replacement Neotype for Globigerina Crassaformis Galloway & Wissler, 1927 G. Scott 10.61551/gsjfr.53.4.397
- A Replacement Neotype for Globigerina Crassaformis Galloway & Wissler, 1927 G. Scott 10.2113/gsjfr.53.4.397
- Diachroneity Rules the Mid-Latitudes: A Test Case Using Late Neogene Planktic Foraminifera across the Western Pacific A. Lam et al. 10.3390/geosciences12050190
- Late Cenozoic cooling restructured global marine plankton communities A. Woodhouse et al. 10.1038/s41586-023-05694-5
- The chronology of mysticete diversification (Mammalia, Cetacea, Mysticeti): Body size, morphological evolution and global change M. Bisconti et al. 10.1016/j.earscirev.2023.104373
14 citations as recorded by crossref.
- The Late Neogene to Quaternary Surface Water Changes as Responses from Planktonic Foraminifera at the Transitional Subantarctic Zone B. Nirmal & K. Mohan 10.2139/ssrn.4133351
- Origination of the modern-style diversity gradient 15 million years ago I. Fenton et al. 10.1038/s41586-023-05712-6
- Biochronology and evolution of Pulleniatina (planktonic foraminifera) P. Pearson et al. 10.5194/jm-42-211-2023
- Alternating regimes of shallow and deep-sea diversification explain a species-richness paradox in marine fishes E. Miller et al. 10.1073/pnas.2123544119
- Paleoecology and evolutionary response of planktonic foraminifera to the mid-Pliocene Warm Period and Plio-Pleistocene bipolar ice sheet expansion A. Woodhouse et al. 10.5194/bg-20-121-2023
- What the geological past can tell us about the future of the ocean’s twilight zone K. Crichton et al. 10.1038/s41467-023-37781-6
- Globorotalia truncatulinoides in the Mediterranean Basin during the Middle–Late Holocene: Bio-Chronological and Oceanographic Indicator G. Margaritelli et al. 10.3390/geosciences12060244
- The late Neogene to Quaternary surface water changes as responses from planktonic foraminifera at the transitional Subantarctic Zone B. Nirmal & K. Mohan 10.1016/j.palaeo.2022.111183
- Biogeographic response of marine plankton to Cenozoic environmental changes A. Swain et al. 10.1038/s41586-024-07337-9
- A Replacement Neotype for Globigerina Crassaformis Galloway & Wissler, 1927 G. Scott 10.61551/gsjfr.53.4.397
- A Replacement Neotype for Globigerina Crassaformis Galloway & Wissler, 1927 G. Scott 10.2113/gsjfr.53.4.397
- Diachroneity Rules the Mid-Latitudes: A Test Case Using Late Neogene Planktic Foraminifera across the Western Pacific A. Lam et al. 10.3390/geosciences12050190
- Late Cenozoic cooling restructured global marine plankton communities A. Woodhouse et al. 10.1038/s41586-023-05694-5
- The chronology of mysticete diversification (Mammalia, Cetacea, Mysticeti): Body size, morphological evolution and global change M. Bisconti et al. 10.1016/j.earscirev.2023.104373
Latest update: 25 Apr 2024
Short summary
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.
Deep-living organisms are a major yet poorly known component of ocean biomass. Here we...
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