Abstract

Background and Aims Fluctuations in [CO2] have been widely studied as a potential driver of plant evolution; however, the role of a fluctuating [O2]:[CO2] ratio is often overlooked. The present study aimed to investigate the inherent physiological plasticity of early diverging, extant species following acclimation to an atmosphere similar to that across the Triassic–Jurassic mass extinction interval (TJB, approx. 200 Mya), a time of major ecological change. Methods Mature plants from two angiosperm (Drimys winteri and Chloranthus oldhamii), two monilophyte (Osmunda claytoniana and Cyathea australis) and one gymnosperm (Ginkgo biloba) species were grown for 2 months in replicated walk-in Conviron BDW40 chambers running at TJB treatment conditions of 16 % [O2]–1900 ppm [CO2] and ambient conditions of 21 % [O2]–400 ppm [CO2], and their physiological plasticity was assessed using gas exchange and chlorophyll fluorescence methods. Key Results TJB acclimation caused significant reductions in the maximum rate of carboxylation (VCmax) and the maximum electron flow supporting ribulose-1,5-bisphosphate regeneration (Jmax) in all species, yet this downregulation had little effect on their light-saturated photosynthetic rate (Asat). Ginkgo was found to photorespire heavily under ambient conditions, while growth in low [O2]:[CO2] resulted in increased heat dissipation per reaction centre (DIo/RC), severe photodamage, as revealed by the species’ decreased maximum efficiency of primary photochemistry (Fv/Fm) and decreased in situ photosynthetic electron flow (Jsitu). Conclusions It is argued that the observed photodamage reflects the inability of Ginkgo to divert excess photosynthetic electron flow to sinks other than the downregulated C3 and the diminished C2 cycles under low [O2]:[CO2]. This finding, coupled with the remarkable physiological plasticity of the ferns, provides insights into the underlying mechanism of Ginkgoales’ near extinction and ferns’ proliferation as atmospheric [CO2] increased to maximum levels across the TJB.

Highlights

  • The end of the Triassic marked the beginning of a period of geological and ecological upheaval known as the Triassic– Jurassic mass extinction event

  • Several studies have questioned the high rates (Hallam, 2002; Tanner et al, 2004) and sources (Bambach et al, 2004) of biodiversity loss across the Triassic–Jurassic boundary (TJB), it is widely considered as the third greatest mass extinction in the Phanerozoic (Benton, 1995; McElwain and Punyasena, 2007)

  • Even though the photosynthetic stimulation was statistically significant only in C. oldhamii, the two ferns and the two angiosperms increased their Asat by 13Á6–43Á0 % depending on the species, while the gymnosperm G. biloba displayed a small, non-significant decrease (6Á1 %)

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Summary

Introduction

The end of the Triassic marked the beginning of a period of geological and ecological upheaval known as the Triassic– Jurassic mass extinction event (approx. 200 Mya). Plant communities undergo structural reformation, which includes substantial changes of families’ relative abundances and distributions and/or in some cases the total loss of growth habits (McElwain et al, 2007, 2009; McElwain and Punyasena, 2007; Bonis and Kuerschner, 2012). In this context, differences in the physiological plasticity between species, families or reproductive groups are expected to play a role in shaping the composition of plant communities under changing environmental conditions. The present study aimed to investigate the inherent physiological plasticity of early diverging, extant species following acclimation to an atmosphere similar to that across the Triassic–Jurassic mass extinction interval (TJB, approx. 200 Mya), a time of major ecological change

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