Sensitivity of planktic foraminifera to sea surface temperature and export production as derived from sediment trap data

By S. Zarić, B. Donner, G. Fischer, S. Mulitza, G. Wefer. 2005

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Modelling the temperature dependent growth rates of planktic foraminifera (2009, background): “(2005) In addition, and despite the fact that populations observed in sediment traps certainly depends on other parameters than just individual growth rate, the asymmetrical growth pattern we observe seems to correspond to the asymmetrical pattern in abundance observed in sediment traps in response ”
Modelling planktic foraminifer growth and distribution using an ecophysiological multi-species approach (2011, background): “…◦C, food concentration, and light availability) whereas other parameters can act on foraminifer abundance such as the salinity (Bijma et al., 1990, Siccha et al., 2009), the depth of the mixed layer (̌Zarić et al., 2005) or the phase in the lunar cycle (Erez et al., 1991; Schiebel et al., 1997).”
Global analysis of seasonality in the shell flux of extant planktonic foraminifera (2015, background): “Reproductive success would then simply follow temperature, leading to the observed seasonality in the shell fluxes (e.g. Lombard et al., 2011; Zaric et al., 2005).”
Calcium isotopic composition of high-latitude proxy carrier Neogloboquadrina pachyderma (sin.) (2007, background): “AlthoughN. pachyderma(sin.) andG. sacculiferhave different ecologies demonstrated particularly in opposite temperature preferences (Zaric et al., 2005), the occurrence of both species is restricted to narrow temperature habitats (Fig.”