26 citations as recorded by crossref.

1. Different photosynthetic responses of haploid and diploid Emiliania huxleyi (Prymnesiophyceae) to high light and ultraviolet radiation Z. Ruan et al. 10.1186/s40643-023-00660-5
2. Calcification Moderates the Increased Susceptibility to UV Radiation of the Coccolithophorid Gephryocapsa oceanica Grown under Elevated CO2 Concentration: Evidence Based on Calcified and Non‐calcified Cells H. Miao et al. 10.1111/php.12928
3. Lower Salinity Leads to Improved Physiological Performance in the Coccolithophorid Emiliania huxleyi, Which Partly Ameliorates the Effects of Ocean Acidification J. Xu et al. 10.3389/fmars.2020.00704
4. The requirement for calcification differs between ecologically important coccolithophore species C. Walker et al. 10.1111/nph.15272
5. The Possession of Coccoliths Fails to Deter Microzooplankton Grazers K. Mayers et al. 10.3389/fmars.2020.569896
6. Physiological and biochemical responses of Emiliania huxleyi to ocean acidification and warming are modulated by UV radiation S. Tong et al. 10.5194/bg-16-561-2019
7. Optical Properties of Nanostructured Silica Structures From Marine Organisms A. Mcheik et al. 10.3389/fmars.2018.00123
8. Fungal-type carbohydrate binding modules from the coccolithophore Emiliania huxleyi show binding affinity to cellulose and chitin B. Rooijakkers et al. 10.1371/journal.pone.0197875
9. The Ecology, Biogeochemistry, and Optical Properties of Coccolithophores W. Balch 10.1146/annurev-marine-121916-063319
10. Light and photosynthetic microalgae: A review of cellular- and molecular-scale optical processes A. Lehmuskero et al. 10.1016/j.pocean.2018.09.002
11. Ocean acidification affects physiology of coccolithophore Emiliania huxleyi and weakens its mechanical resistance to copepods H. Xu et al. 10.1016/j.marenvres.2023.106232
12. Calcification increases carbon supply, photosynthesis, and growth in a globally distributed coccolithophore A. Grubb et al. 10.1002/lno.12656
13. Extremely strong coccolithophore blooms in the Black Sea: The decisive role of winter vertical entrainment of deep water A. Kubryakov et al. 10.1016/j.dsr.2021.103554
14. Extreme Ozone Loss Following Nuclear War Results in Enhanced Surface Ultraviolet Radiation C. Bardeen et al. 10.1029/2021JD035079
15. Diurnally fluctuatingpCO2 enhances growth of a coastal strain ofEmiliania huxleyiunder future-projected ocean acidification conditions F. Li et al. 10.1093/icesjms/fsab036
16. Phyletic evolution of calcareous nannofossil species Reticulofenestra oamaruensis: An example of microevolution preserved at IODP Site U1553 (Southern Pacific Ocean) V. Catelli et al. 10.1016/j.marmicro.2025.102452
17. Haplo-diplontic life cycle expands coccolithophore niche J. de Vries et al. 10.5194/bg-18-1161-2021
18. Hard shell, soft blue-green core: Ecology, processes, and modern applications of calcification in terrestrial cyanobacteria P. Jung et al. 10.1016/j.isci.2024.111280
19. Interannual variability of Emiliania huxleyi blooms in the Barents Sea: In situ data 2014–2018 V. Silkin et al. 10.1016/j.marpolbul.2020.111392
20. Summer and winter coccolithophore blooms in the Black Sea and their impact on production of dissolved organic matter from Bio-Argo data A. Kubryakov et al. 10.1016/j.jmarsys.2019.103220
21. Coccolithophore growth and calcification in a changing ocean K. Krumhardt et al. 10.1016/j.pocean.2017.10.007
22. Adsorptive exchange of coccolith biominerals facilitates viral infection C. Johns et al. 10.1126/sciadv.adc8728
23. Effects of elevated CO2 on growth, calcification, and spectral dependence of photoinhibition in the coccolithophore Emiliania huxleyi (Prymnesiophyceae)1 M. Lorenzo et al. 10.1111/jpy.12885
24. Coccolith volume of the Southern Ocean coccolithophore Emiliania huxleyi as a possible indicator for palaeo‐cell volume M. Müller et al. 10.1111/gbi.12414
25. Calcification moderates the biochemical responses of Gephyrocapsa oceanica to ocean acidification X. Shi et al. 10.1080/17451000.2021.2016841
26. High light stress reduces dinoflagellate predation on phytoplankton through both direct and indirect responses S. Strom et al. 10.3354/ame01924