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.2020 Jun 11;71(11):3254-3269.
doi: 10.1093/jxb/eraa007.

Evo-physio: on stress responses and the earliest land plants

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Evo-physio: on stress responses and the earliest land plants

Janine M R Fürst-Jansen et al. J Exp Bot..

Abstract

Embryophytes (land plants) can be found in almost any habitat on the Earth's surface. All of this ecologically diverse embryophytic flora arose from algae through a singular evolutionary event. Traits that were, by their nature, indispensable for the singular conquest of land by plants were those that are key for overcoming terrestrial stressors. Not surprisingly, the biology of land plant cells is shaped by a core signaling network that connects environmental cues, such as stressors, to the appropriate responses-which, thus, modulate growth and physiology. When did this network emerge? Was it already present when plant terrestrialization was in its infancy? A comparative approach between land plants and their algal relatives, the streptophyte algae, allows us to tackle such questions and resolve parts of the biology of the earliest land plants. Exploring the biology of the earliest land plants might shed light on exactly how they overcame the challenges of terrestrialization. Here, we outline the approaches and rationale underlying comparative analyses towards inferring the genetic toolkit for the stress response that aided the earliest land plants in their conquest of land.

Keywords: Charophytes; earliest land plants; exaptations; plant evolution; plant terrestrialization; streptophyte algae; stress physiology; terrestrial algae.

© The Author(s) 2020. Published by Oxford University Press on behalf of the Society for Experimental Biology.

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Figures

Fig. 1.
Fig. 1.
Terrestrial organisms are found across the green lineage. A cladogram shows the deep split of the green lineage into the clades Chlorophyta and Streptophyta. The Streptophyta are composed of the paraphylum streptophyte algae and the monophyletic Embryophyta (land plants). Streptophyte algae can be broken up into the paraphyla KCM (for Klebsormidiophyceae, Chlorokybophyceae, and Mesostigmatophyceae) and ZCC (for Zygnematophyceae, Coleochaetophyceae, and Charophyceae; de Vrieset al., 2016). ZCC streptophyte algae and land plants form the monophyletic clade Phragmoplastophyta. Taken in their entirety, Chlorophyta occur in habitats ranging from marine saltwater, to freshwater, to terrestrial (row of dots). Streptophyte algae mainly occur in freshwater and terrestrial environments; some Charophyceae live in a brackish habitat. While the Embryophyta are mainly terrestrial, some have secondarily moved back to a freshwater habitat; some have even conquered a new habitat: saltwater (e.g. sea grasses). Inset: the Zygnematophyceae are the closest algal relatives of land plants and they hence share with the clade of Embryophyta the last common ancestor of land plants and algae (yellow dot); along the trajectory from that last common ancestor of land plants and algae (yellow dot) to the last common ancestor of land plants (red dot) are the earliest land plants to be found (orange dot). Inferring the biology of the earliest land plants requires a subtraction of the traits (‘adaptations’) that were gained on land, that is en route to the last common ancestor of land plants (from the orange to the red dot; see also Fig. 2).
Fig. 2.
Fig. 2.
The earliest land plants: an evolutionary scenario for the conquest of land by streptophytes. Streptophyte algae are the only photosynthetic eukaryotes from which the macroscopic land flora evolved (red lines). That said, throughout the course of evolution, algae from various other lineages have colonized land (yellow lines)—but also streptophyte algae have continuously and independently made the wet to dry transition (convergence of red and yellow). Throughout history, numerous lineages have become extinct (‘x’ labels). Terrestrial algae of various taxonomic affiliations dwell on rock surfaces and form biological soil crusts. From the diversity of the paraphyletic streptophyte algae, however, did an organism whose descendants eventually conquered land on a global scale emerge: a likely branched filamentous—or even parenchymatous—organism that formed rhizoidal structures and experienced desiccation from time to time. From this ‘hypothetical hydro-terrestrial alga’, the lineages of Zygnematophyceae and embryophytes (land plants) arose. In its infancy, the trajectory leading to the embryophytes was represented by the—now extinct (see also Delauxet al., 2019)—earliest land plants. The earliest land plants probably interacted with beneficial substrate microbiota that aided them in obtaining nutrients from their substrate. Furthermore, the earliest land plants had to successfully overcome a barrage of terrestrial stressors (including UV and photosynthetically active irradiance, drought, drastic temperature shifts, etc.). They succeeded because they had the right set of traits—a mix of adaptations that were selected for in their hydro-terrestrial algal ancestors, exaptations, and the potential for co-option of a fortuitous set of genes and pathways. During the course of evolution, some members of the populations of the earliest land plants gained traits that are adaptive in terrestrial environments (such as some form of water conductance, stomata-like structures, embryos, etc.); eventually, the ‘hypothetical last common ancestor of land plants’ emerged. From this ancestor, the extant bryophytes and tracheophytes evolved. While the exact trait repertoire of the hypothetical last common ancestor of land plants is uncertain, it will certainly have entailed properties of vascular and non-vascular plants. What is also certain is that the last common ancestor of land plants had traits of algal ancestry. (All dating is roughly based on Morris et al. [2018])
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