Abstract

Abstract. Coccolithophores, a diverse group of phytoplankton, make important contributions to pelagic calcite production and export, yet the comparative biogeochemical role of species other than the ubiquitous Emiliania huxleyi is poorly understood. The contribution of different coccolithophore species to total calcite production is controlled by inter-species differences in cellular calcite, growth rate and relative abundance within a mixed community. In this study we examined the relative importance of E. huxleyi and two Coccolithus species in terms of daily calcite production. Culture experiments compared growth rates and cellular calcite content of E. huxleyi (Arctic and temperate strains), Coccolithus pelagicus (novel Arctic strain) and Coccolithus braarudii (temperate strain). Despite assumptions that E. huxleyi is a fast-growing species, growth rates between the three species were broadly comparable (0.16–0.85 d−1) under identical temperature and light conditions. Emiliania huxleyi grew only 12% faster on average than C. pelagicus, and 28% faster than C. braarudii. As the cellular calcite content of C. pelagicus and C. braarudii is typically 30–80 times greater than E. huxleyi, comparable growth rates suggest that Coccolithus species have the potential to be major calcite producers in mixed populations. To further explore these results we devised a simplistic model comparing daily calcite production from Coccolithus and E. huxleyi across a realistic range of relative abundances and a wide range of relative growth rates. Using the relative differences in growth rates from our culture studies, we found that C. pelagicus would be a larger source of calcite if abundances of E. huxleyi to C. pelagicus were below 34:1. Relative abundance data collected from North Atlantic field samples (spring and summer 2010) suggest that, with a relative growth rate of 88%, C. pelagicus dominated calcite production at 69% of the sites sampled. With a more extreme difference in growth rates, where C. pelagicus grows at 1/10th of the rate of E. huxleyi, C. pelagicus still dominated calcite production in 14% of the field. These results demonstrate the necessity of considering interactions between inter-species differences in growth rates, cellular calcite and relative abundances when evaluating the contribution of different coccolithophores to pelagic calcite production. In the case of C. pelagicus, we find that there is strong potential for this species to make major contributions to calcite production in the North Atlantic, although estimates of relative growth rates from the field are needed to confirm our conclusions.

Highlights

  • Coccolithophores are a diverse and biogeochemically important group of phytoplankton; through the production and subsequent export of their calcite coccoliths, they form a key component of the global carbon cycle (de Vargas et al, 2007)

  • We have modelled the effect of growth rate and relative abundance on the role of Coccolithus as a calcite producer, the relative calcite production of the two species in these models is highly dependent on the cellular calcite quotas attributed to both E. huxleyi and Coccolithus (Table 1), as calcite production is the product of growth rate and cellular calcite

  • The data we have presented show that, when grown in parallel under identical experimental conditions, the relative difference in growth rates between E. huxleyi and Coccolithus species was generally small (12 and 28 %, respectively, for C. pelagicus and C. braarudii), E. huxleyi generally grew significantly faster than both C. pelagicus and C. braarudii

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Summary

Introduction

Coccolithophores are a diverse and biogeochemically important group of phytoplankton; through the production and subsequent export of their calcite coccoliths, they form a key component of the global carbon cycle (de Vargas et al, 2007). Emiliania huxleyi is considered the keystone species of the coccolithophores due to its global dominance, propensity to form large-scale blooms and its perceived relatively fast growth rates (Paasche, 2002). Assumptions on the comparative physiology and ecology of the other ∼ 200 extant species are often poorly addressed, studies have examined intra- and inter-species differences in response to carbonate chemistry changes (Langer et al, 2006, 2009), photophysiological differences between haploid and diploid life. Daniels et al.: Biogeochemical implications of comparative growth rates

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