Spatial dynamics of coccolithophore assemblages in the Equatorial Western-Central Pacific Ocean

By K. Hagino, H. Okada, H. Matsuoka. 2000

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Coccolithophore assemblages and morphotypes of Emiliania huxleyi in the boundary zone between the cold Oyashio and warm Kuroshio currents off the coast of Japan (2005, background): “Higher sea surface temperatures (>28˚C) caused a change in the flora from an assemblage in which E. huxleyi was common to an assemblage in which G. oceanica was common, regardless of nutrient concentration (Hagino et al., 2000; Hagino and Okada, 2004).”
Coccolithophore ecology in the tropical and subtropical Atlantic Ocean: New perspectives from the Atlantic Meridional Transect (AMT) programme (2017, background): “Both latitudinal biogeographical and floral depth zones have been recognised on the basis of characteristic coccolithophore species assemblages (e.g., McIntyre and Be, 1967; Okada and McIntyre, 1977; Winter et al., 1994); with further work in the Atlantic (Kinkel et al., 2000; Haidar and Thierstein,”
Relating coccolithophore calcification rates to phytoplankton community dynamics: Regional differences and implications for carbon export (2007, background): “, 2003), deeper in the water column (50–100m) in association with the nutricline (Hagino et al., 2000; Jordan and Winter, 2000; Cortes et al., 2001; Haider and Thierstein, 2001), or may be evenly distributed over the euphotic zone (Reid, 1980; Jordan and Winter, 2000).”