Vertical distribution of living planktonic foraminifera in the seas around Japan

By A. Kuroyanagi, H. Kawahata. 2004

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Predicting the global distribution of planktonic foraminifera using a dynamic ecosystem model (2008, background): “…Biogeosciences, 5, 891–911, 2008 Biogeosciences, 5, 891–911, 2008 www.biogeosciences.net/5/891/2008/ www.biogeosciences.net/5/891/2008/ Biogeosciences, 5, 891–911, 2008 Kuroyanagi and Kawahata, 2004), or that they are expatriated specimens from the upwelling region.”
Modelling planktic foraminifer growth and distribution using an ecophysiological multi-species approach (2011, methodology): “These plankton tows were obtained with mesh size from 63 μm (Kuroyanagi and Kawahata, 2004; Watkins et al., 1996, 1998) to 100 μm (Schiebel et al.”
Pelagic functional group modeling: Progress, challenges and prospects (2006, unknown): “Even if heterotrophic production of CaCO3 is taken into account, variability in the relative abundance of autotrophic and heterotrophic calcifying species (Eguchi et al., 2003; Kuroyanagi and Kawahata, 2004) argues against the use of a single PIC/POC ratio for the oceans.”
Modelling the temperature dependent growth rates of planktic foraminifera (2009, background): “This could originate from their adaptation to a sub-surface habitat if sea surface temperature is too high and sufficient food is available (Kuroyanagi and Kawahata, 2004), although part of that discrepancy may also be derived from a higher culture stress near the upper temperature limits for these ”