Abstract

Rubisco assimilates CO2 to form the sugars that fuel life on earth. Correlations between rubisco kinetic traits across species have led to the proposition that rubisco adaptation is highly constrained by catalytic trade-offs. However, these analyses did not consider the phylogenetic context of the enzymes that were analyzed. Thus, it is possible that the correlations observed were an artefact of the presence of phylogenetic signal in rubisco kinetics and the phylogenetic relationship between the species that were sampled. Here, we conducted a phylogenetically resolved analysis of rubisco kinetics and show that there is a significant phylogenetic signal in rubisco kinetic traits. We re-evaluated the extent of catalytic trade-offs accounting for this phylogenetic signal and found that all were attenuated. Following phylogenetic correction, the largest catalytic trade-offs were observed between the Michaelis constant for CO2 and carboxylase turnover (∼21–37%), and between the Michaelis constants for CO2 and O2 (∼9–19%), respectively. All other catalytic trade-offs were substantially attenuated such that they were marginal (<9%) or non-significant. This phylogenetically resolved analysis of rubisco kinetic evolution also identified kinetic changes that occur concomitant with the evolution of C4 photosynthesis. Finally, we show that phylogenetic constraints have played a larger role than catalytic trade-offs in limiting the evolution of rubisco kinetics. Thus, although there is strong evidence for some catalytic trade-offs, rubisco adaptation has been more limited by phylogenetic constraint than by the combined action of all catalytic trade-offs.

Highlights

  • IntroductionThe vast majority of organic carbon on Earth entered the biosphere via the catalytic pocket of rubisco (ribulose-1,5bisphosphate [RuBP] carboxylase/oxygenase) (Beer et al 2010)

  • The vast majority of organic carbon on Earth entered the biosphere via the catalytic pocket of rubisco (Beer et al 2010)

  • In support of this hypothesis, antagonistic correlations between rubisco kinetic traits inferred from studies comparing limited numbers of species are commonly cited (Tcherkez et al 2006; Savir et al 2010)

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Summary

Introduction

The vast majority of organic carbon on Earth entered the biosphere via the catalytic pocket of rubisco (ribulose-1,5bisphosphate [RuBP] carboxylase/oxygenase) (Beer et al 2010). Form I rubisco contains two subunits, only the large subunit is essential for catalysis (Andrews 1988; Lee and Tabita 1990; Whitney et al.2011), whereas the small subunit has an indirect effect on catalytic properties and activity (Andrews 1988; Lee and Tabita 1990; Lee et al 1991; Read and Tabita 1992a, 1992b; Spreitzer et al 2005; Ishikawa et al 2011; Joshi et al 2015; Fukayama et al 2019; Martin-Avila et al 2020)

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