Abstract

Emiliania huxleyi (Lohmann) evolved from the genus Gephyrocapsa Kamptner (Prymneosiophyceae) of the coccolithophore family Naёlaerhadaceae. Over the past 100 thousand years E. huxleyi has acquired the status of the most ecologically predominant coccolithophore due to its remarkable adaptability to a variety of environmental conditions and interspecific competitiveness. E. huxleyi plays an important role in both the marine carbon system and carbon cycling between the atmosphere and ocean due to its ability to produce organic and inorganic carbon as well as to form massive blooms throughout the world ocean. This study examines both older information and recent findings to shed light on the current tendencies in the two-way interactions between E. huxleyi blooms and the immediate and global environment under conditions of climate change. The assembled knowledge has emerged from laboratory and mesocosm instrumental investigations, retrievals of satellite remote sensing data, machine learning/statistical analyses, and numerical simulations. Special attention is given to both the quantitative data reported over the last two decades on such interactions, and the only very recently appearing mid-term projections of E. huxleyi bloom dynamics across the world ocean. These blooms strongly affect the atmosphere and ocean carbon cycles. They reduce CO2 fluxes from by ~50% to ~150% as is documented for the North Atlantic, and on the global scale release particulate inorganic carbon as calcium calcite in the amounts assessed at 0.4 to 4.8 PgC/yr. At the same time, they are also sensitive to the atmospheric and oceanic state. This results in E. huxleyi blooms having an increased impact on the environment in response to ongoing global warming.

Highlights

  • E. huxleyi contribute to marine sulphur cycles by producing a precursor of dimethylsulphide (DMS), the latter being a precursor for the generation of maritime aerosol

  • These properties are consequential as E. huxleyi is able to form extensive and intensive blooms throughout the world ocean

  • Analysis of the reviewed publications suggests that all major and basic aspects of the E. huxleyi cell composition and functioning have been clarified to a large extent, and that this alga is one of the best-studied marine organisms

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Summary

INTRODUCTION

E. huxleyi contribute to marine sulphur cycles by producing a precursor of dimethylsulphide (DMS), the latter being a precursor for the generation of maritime aerosol These properties are consequential as E. huxleyi is able to form extensive and intensive blooms throughout the world ocean. No single review is able to cover all aspects of the knowledge that has emerged on E.huxleyi In this manuscript we chose to concentrate on the ecology of this alga and its influence on the atmosphere and ocean, as well as the vice versa influence on this alga of the changing climatic conditions of the recent past and near future. Our review explores some «old knowledge», since the basic accomplishments in E. huxleyi-related research continue to be fundamental for our understanding of the phenomena related to this remarkable marine organism

A HISTORIC OVERVIEW OF ORIGIN AND DEVELOPMENT
Findings
CONCLUDING REMARKS
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