83 citations as recorded by crossref.

1. High‐Resolution Coccolithophore Morphological Changes in Response to Orbital Forcings During the Early Oligocene R. Ma et al. 10.1029/2022GC010746
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3. No detectable effect of CO2 on elemental stoichiometry of Emiliania huxleyi in nutrient-limited, acclimated continuous cultures A. Engel et al. 10.3354/meps10824
4. Coccolithophore growth and calcification in a changing ocean K. Krumhardt et al. 10.1016/j.pocean.2017.10.007
5. Nannoplankton malformation during the Paleocene-Eocene Thermal Maximum and its paleoecological and paleoceanographic significance T. Bralower & J. Self-Trail 10.1002/2016PA002980
6. Environmental controls on the <i>Emiliania huxleyi</i> calcite mass M. Horigome et al. 10.5194/bg-11-2295-2014
7. Decrease in coccolithophore calcification and CO2 since the middle Miocene C. Bolton et al. 10.1038/ncomms10284
8. Morphology, phylogenetic position, and ecophysiological features of the coccolithophore Chrysotila dentata (Prymnesiophyceae) isolated from the Bohai Sea, China H. Liu et al. 10.1080/00318884.2019.1644477
9. Physiological responses of coccolithophores to abrupt exposure of naturally low pH deep seawater M. Iglesias-Rodriguez et al. 10.1371/journal.pone.0181713
10. Late Quaternary coccolith weight variations in the northern South China Sea and their environmental controls X. Su et al. 10.1016/j.marmicro.2019.101798
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12. 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
13. A unifying concept of coccolithophore sensitivity to changing carbonate chemistry embedded in an ecological framework L. Bach et al. 10.1016/j.pocean.2015.04.012
14. Responses of marine primary producers to interactions between ocean acidification, solar radiation, and warming K. Gao et al. 10.3354/meps10043
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18. Short-term effects of winter warming and acidification on phytoplankton growth and mortality: more losers than winners in a temperate coastal lagoon R. Domingues et al. 10.1007/s10750-021-04672-0
19. Do marine phytoplankton follow Bergmann's rule sensu lato? U. Sommer et al. 10.1111/brv.12266
20. Reduced growth with increased quotas of particulate organic and inorganic carbon in the coccolithophore <i>Emiliania huxleyi</i> under future ocean climate change conditions Y. Zhang et al. 10.5194/bg-17-6357-2020
21. Adaptations of Coccolithophore Size to Selective Pressures During the Oligocene to Early Miocene High CO2 World J. Guitián et al. 10.1029/2020PA003918
22. Covariation of metabolic rates and cell size in coccolithophores G. Aloisi 10.5194/bg-12-4665-2015
23. Diurnally fluctuatingpCO2 enhances growth of a coastal strain ofEmiliania huxleyiunder future-projected ocean acidification conditions F. Li et al. 10.1093/icesjms/fsab036
24. Temperature affects the morphology and calcification of <i>Emiliania huxleyi</i> strains A. Rosas-Navarro et al. 10.5194/bg-13-2913-2016
25. Influence of temperature and elevated carbon dioxide on the production of dimethylsulfoniopropionate and glycine betaine by marine phytoplankton A. Spielmeyer & G. Pohnert 10.1016/j.marenvres.2011.11.002
26. Individual and interactive effects of ocean acidification, global warming, and UV radiation on phytoplankton K. Gao et al. 10.1007/s10811-017-1329-6
27. Biogeochemistry and carbon mass balance of a coccolithophore bloom in the northern Bay of Biscay (June 2006) J. Harlay et al. 10.1016/j.dsr.2010.11.005
28. Influence of CO<sub>2</sub> and nitrogen limitation on the coccolith volume of <I>Emiliania huxleyi</I> (Haptophyta) M. Müller et al. 10.5194/bg-9-4155-2012
29. Ocean Acidification Affects Redox-Balance and Ion-Homeostasis in the Life-Cycle Stages of Emiliania huxleyi S. Rokitta et al. 10.1371/journal.pone.0052212
30. Changes in calcification of coccoliths under stable atmospheric CO<sub>2</sub> C. Berger et al. 10.5194/bg-11-929-2014
31. Strain-specific morphological response of the dominant calcifying phytoplankton species Emiliania huxleyi to salinity change C. Gebühr et al. 10.1371/journal.pone.0246745
32. Carbon assimilation and losses during an ocean acidification mesocosm experiment, with special reference to algal blooms N. Liu et al. 10.1016/j.marenvres.2017.05.003
33. Ocean warming modulates the effects of acidification on Emiliania huxleyi calcification and sinking S. Milner et al. 10.1002/lno.10292
34. Reviews and Syntheses: Responses of coccolithophores to ocean acidification: a meta-analysis J. Meyer & U. Riebesell 10.5194/bg-12-1671-2015
35. Increased CO2 and iron availability effects on carbon assimilation and calcification on the formation of Emiliania huxleyi blooms in a coastal phytoplankton community M. Rosario Lorenzo et al. 10.1016/j.envexpbot.2017.12.003
36. Seasonal variability of the carbonate system and coccolithophore Emiliania huxleyi at a Scottish Coastal Observatory monitoring site P. León et al. 10.1016/j.ecss.2018.01.011
37. A three-dimensional niche comparison of <i>Emiliania huxleyi</i> and <i>Gephyrocapsa oceanica</i>: reconciling observations with projections N. Gafar & K. Schulz 10.5194/bg-15-3541-2018
38. Impacts of nitrogen limitation on the sinking rate of the coccolithophoridEmiliania huxleyi(Prymnesiophyceae) A. Pantorno et al. 10.2216/12-064.1
39. CO2‐concentrating mechanisms in three southern hemisphere strains of Emiliania huxleyi S. Stojkovic et al. 10.1111/jpy.12074
40. Differing responses of three Southern Ocean Emiliania huxleyi ecotypes to changing seawater carbonate chemistry M. Müller et al. 10.3354/meps11309
41. Phenotypic Variability in the Coccolithophore Emiliania huxleyi S. Blanco-Ameijeiras et al. 10.1371/journal.pone.0157697
42. The role of coccoliths in protecting <i>Emiliania huxleyi</i> against stressful light and UV radiation J. Xu et al. 10.5194/bg-13-4637-2016
43. Effects of elevated CO2 partial pressure and temperature on the coccolithophore Syracosphaera pulchra S. Fiorini et al. 10.3354/ame01520
44. Reduction in size of the calcifying phytoplankton Calcidiscus leptoporus to environmental changes between the Holocene and modern Subantarctic Southern Ocean A. Rigual-Hernández et al. 10.3389/fmars.2023.1159884
45. The cellular response to ocean warming in Emiliania huxleyi C. Dedman et al. 10.3389/fmicb.2023.1177349
46. Photosynthetic responses of <i>Emiliania huxleyi</i> to UV radiation and elevated temperature: roles of calcified coccoliths K. Xu et al. 10.5194/bg-8-1441-2011
47. Diverse trends in shell weight of three Southern Ocean pteropod taxa collected with Polar Frontal Zone sediment traps from 1997 to 2007 D. Roberts et al. 10.1007/s00300-014-1534-6
48. Simultaneous shifts in elemental stoichiometry and fatty acids of <i>Emiliania huxleyi</i> in response to environmental changes R. Bi et al. 10.5194/bg-15-1029-2018
49. Variations and controlling factors of the coccolith weight in the Western Pacific Warm Pool over the last 200 ka D. Liang & C. Liu 10.1007/s11802-016-3088-4
50. High-CO2 Levels Rather than Acidification Restrict Emiliania huxleyi Growth and Performance V. Vázquez et al. 10.1007/s00248-022-02035-3
51. Temperature Modulates Coccolithophorid Sensitivity of Growth, Photosynthesis and Calcification to Increasing Seawater pCO2 S. Sett et al. 10.1371/journal.pone.0088308
52. Intraspecific Differences in Biogeochemical Responses to Thermal Change in the Coccolithophore Emiliania huxleyi P. Matson et al. 10.1371/journal.pone.0162313
53. Ocean acidification reduces hardness and stiffness of the Portuguese oyster shell with impaired microstructure: a hierarchical analysis Y. Meng et al. 10.5194/bg-15-6833-2018
54. Coccolithophore community response to ocean acidification and warming in the Eastern Mediterranean Sea: results from a mesocosm experiment B. D’Amario et al. 10.1038/s41598-020-69519-5
55. Predominance of heavily calcified coccolithophores at low CaCO 3 saturation during winter in the Bay of Biscay H. Smith et al. 10.1073/pnas.1117508109
56. Coccolith mass and morphology of different Emiliania huxleyi morphotypes: A critical examination using Canary Islands material S. Linge Johnsen et al. 10.1371/journal.pone.0230569
57. EVOLUTIONARY RESPONSES OF A COCCOLITHOPHORIDGEPHYROCAPSA OCEANICATO OCEAN ACIDIFICATION P. Jin et al. 10.1111/evo.12112
58. Evolutionary driven of Gephyrocapsa coccolith isotopic vital effects over the past 400 ka X. Jin et al. 10.1016/j.epsl.2018.09.010
59. Cellular morphological trait dataset for extant coccolithophores from the Atlantic Ocean R. Sheward et al. 10.1038/s41597-024-03544-1
60. Effect of ocean acidification on marine phytoplankton and biogeochemical cycles K. Sugie & T. Yoshimura 10.5928/kaiyou.20.5_101
61. Environmental controls on coccolithophore calcification J. Raven & K. Crawfurd 10.3354/meps09993
62. Predicting coccolithophore rain ratio responses to calcite saturation state S. Fielding 10.3354/meps10657
63. Emiliania huxleyi increases calcification but not expression of calcification-related genes in long-term exposure to elevated temperature and p CO 2 I. Benner et al. 10.1098/rstb.2013.0049
64. Ocean acidification effects on haploid and diploid Emiliania huxleyi strains: Why changes in cell size matter M. Brady Olson et al. 10.1016/j.jembe.2016.12.008
65. Microorganisms and ocean global change D. Hutchins & F. Fu 10.1038/nmicrobiol.2017.58
66. Environmental controls on the growth, photosynthetic and calcification rates of a Southern Hemisphere strain of the coccolithophore Emiliania huxleyi Y. Feng et al. 10.1002/lno.10442
67. Contrasting species-specific stress response to environmental pH determines the fate of coccolithophores in future oceans N. Chauhan et al. 10.1016/j.marpolbul.2024.117136
68. Dissolved inorganic carbon dynamics and air‐sea carbon dioxide fluxes during coccolithophore blooms in the northwest European continental margin (northern Bay of Biscay) K. Suykens et al. 10.1029/2009GB003730
69. Nitrogen source and pCO2 synergistically affect carbon allocation, growth and morphology of the coccolithophore Emiliania huxleyi: potential implications of ocean acidification for the carbon cycle S. Lefebvre et al. 10.1111/j.1365-2486.2011.02575.x
70. Adaptive evolution in the coccolithophore Gephyrocapsa oceanica following 1,000 generations of selection under elevated CO2 S. Tong et al. 10.1111/gcb.14065
71. Effects of Elevated Temperature and Carbon Dioxide on the Growth and Survival of Larvae and Juveniles of Three Species of Northwest Atlantic Bivalves S. Talmage et al. 10.1371/journal.pone.0026941
72. Phosphorus limitation and heat stress decrease calcification in <i>Emiliania huxleyi</i> A. Gerecht et al. 10.5194/bg-15-833-2018
73. Physiological responses of a coccolithophore to multiple environmental drivers P. Jin et al. 10.1016/j.marpolbul.2019.06.032
74. Biological responses of the marine diatom Chaetoceros socialis to changing environmental conditions: A laboratory experiment X. Li et al. 10.1371/journal.pone.0188615
75. Increasing coccolith calcification during CO2 rise of the penultimate deglaciation (Termination II) K. Meier et al. 10.1016/j.marmicro.2014.07.001
76. How will the key marine calcifier <i>Emiliania huxleyi</i> respond to a warmer and more thermally variable ocean? X. Wang et al. 10.5194/bg-16-4393-2019
77. Extreme pH Conditions at a Natural CO2 Vent System (Italy) Affect Growth, and Survival of Juvenile Pen Shells (Pinna nobilis) L. Basso et al. 10.1007/s12237-014-9936-9
78. Interactive effects of temperature, CO2 and nitrogen source on a coastal California diatom assemblage A. Tatters et al. 10.1093/plankt/fbx074
79. The role of ocean acidification in <i>Emiliania huxleyi</i> coccolith thinning in the Mediterranean Sea K. Meier et al. 10.5194/bg-11-2857-2014
80. Calcareous Nannofossil Size and Abundance Response to the Messinian Salinity Crisis Onset and Paleoenvironmental Dynamics A. Mancini et al. 10.1029/2020PA004155
81. Resilience of Emiliania huxleyi to future changes in subantarctic waters E. Armstrong et al. 10.1371/journal.pone.0284415
82. Pedogenic carbonates and carbon pools in gypsiferous soils of a semiarid Mediterranean environment in south Italy V. Laudicina et al. 10.1016/j.geoderma.2012.07.015
83. Calcareous nannofossil changes linked to climate deterioration during the Paleocene–Eocene thermal maximum in Tarim Basin, NW China W. Cao et al. 10.1016/j.gsf.2018.04.002