Abstract

Abstract. Coccolithophores are globally important marine calcifying phytoplankton that utilize a haplo-diplontic life cycle. The haplo-diplontic life cycle allows coccolithophores to divide in both life cycle phases and potentially expands coccolithophore niche volume. Research has, however, to date largely overlooked the life cycle of coccolithophores and has instead focused on the diploid life cycle phase of coccolithophores. Through the synthesis and analysis of global scanning electron microscopy (SEM) coccolithophore abundance data (n=2534), we find that calcified haploid coccolithophores generally constitute a minor component of the total coccolithophore abundance (≈ 2 %–15 % depending on season). However, using case studies in the Atlantic Ocean and Mediterranean Sea, we show that, depending on environmental conditions, calcifying haploid coccolithophores can be significant contributors to the coccolithophore standing stock (up to ≈30 %). Furthermore, using hypervolumes to quantify the niche of coccolithophores, we illustrate that the haploid and diploid life cycle phases inhabit contrasting niches and that on average this allows coccolithophores to expand their niche by ≈18.8 %, with a range of 3 %–76 % for individual species. Our results highlight that future coccolithophore research should consider both life cycle stages, as omission of the haploid life cycle phase in current research limits our understanding of coccolithophore ecology. Our results furthermore suggest a different response to nutrient limitation and stratification, which may be of relevance for further climate scenarios. Our compilation highlights the spatial and temporal sparsity of SEM measurements and the need for new molecular techniques to identify uncalcified haploid coccolithophores. Our work also emphasizes the need for further work on the carbonate chemistry niche of the coccolithophore life cycle.

Highlights

  • Coccolithophores are marine phytoplankton that produce calcium carbonate platelets, called “coccoliths”, which can be seen from space when coccolithophores bloom

  • Through the synthesis and analysis of global scanning electron microscopy (SEM) coccolithophore abundance data (n = 2534), we find that calcified haploid coccolithophores generally constitute a minor component of the total coccolithophore abundance (≈ 2 %–15 % depending on season)

  • Our meta-analysis shows that holococcolithophores are a minor contributor to coccolithophore abundance in the modern ocean, contributing between ≈ 2 %–15 % to the total coccolithophore abundance and between ≈ 5 %–30 % of the total paired coccolithophore abundance depending on season

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Summary

Introduction

Coccolithophores are marine phytoplankton that produce calcium carbonate platelets, called “coccoliths”, which can be seen from space when coccolithophores bloom. Through the production of coccoliths, coccolithophores produce ≈ 1.5 Pg of inorganic carbon per year (Hopkins and Balch, 2018; Krumhardt et al, 2019) and subsequently account for 30 % to 90 % of carbonate in sediments J. de Vries et al.: Haplo-diplontic life cycle expands coccolithophore niche and Clark, 2009), highlighting the importance of coccolithophores in calcium carbonate burial. In addition to the carbonate pump, coccolithophores contribute to the organic carbon pump, accounting for 1 %–40 % of marine primary production depending on habitat (Poulton et al, 2007, 2013). Because of involvement in the ocean carbon pumps and food web, coccolithophores play an important role in the ocean on regional to global spatial scales and seasonal to geological timescales

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