12 citations as recorded by crossref.

1. Ocean kinetic energy and photosynthetic biomass are important drivers of planktonic foraminifera diversity in the Atlantic Ocean M. Rufino et al. 10.3389/fmars.2022.887346
2. Strong temperature gradients in the ice age North Atlantic Ocean revealed by plankton biogeography L. Jonkers et al. 10.1038/s41561-023-01328-7
3. Towards spatio-temporal comparison of simulated and reconstructed sea surface temperatures for the last deglaciation N. Weitzel et al. 10.5194/cp-20-865-2024
4. Coupled Coccolith-Based Temperature and Productivity High-Resolution Reconstructions in the Eastern Equatorial Pacific During the Last Deglaciation and the Holocene M. Saavedra-Pellitero et al. 10.3389/fmars.2022.865846
5. The return of the Iváň Canyon, a large Neogene canyon in the Alpine-Carpathian Foredeep S. Nehyba et al. 10.1016/j.marpetgeo.2022.105808
6. Technical note: Considerations on using uncertain proxies in the analogue method for spatiotemporal reconstructions of millennial-scale climate O. Bothe & E. Zorita 10.5194/cp-17-721-2021
7. Nutrients and hydrography explain the composition of recent Mediterranean planktonic foraminiferal assemblages L. Azibeiro et al. 10.1016/j.marmicro.2022.102201
8. Relative sea-level reconstructions by using foraminiferal transfer functions Y. Milker 10.1016/j.marmicro.2024.102410
9. Are Past Sea-Ice Reconstructions Based on Planktonic Foraminifera Realistic? Study of the Last 50 ka as a Test to Validate Reconstructed Paleohydrography Derived from Transfer Functions Applied to Their Fossil Assemblages F. Eynaud et al. 10.3390/geosciences11100409
10. The Foraminiferal Response to Climate Stressors Project: Tracking the Community Response of Planktonic Foraminifera to Historical Climate Change T. de Garidel-Thoron et al. 10.3389/fmars.2022.827962
11. Preface: Advances in paleoclimate data synthesis and analysis of associated uncertainty: towards data–model integration to understand the climate L. Jonkers et al. 10.5194/cp-17-2577-2021
12. Micropaleontological and Isotopic Perspective of Surface Water Mass Variability in the NE Atlantic from MIS 6 to 5e (188 to 115 ka) H. Rashid et al. 10.3390/geosciences13050149