Erika J. Edwards

The Origins of C4 Grasslands: Integrating Evolutionary and Ecosystem Science

Grassland Emergence The evolution of the C4 photosynthetic pathway from the ancestral C3 pathway in grasses led to the establishment of grasslands in warm climates during the Late Miocene (8 to 3 million years ago). This was a major event in plant evolutionary history, and their high rates of foliage production sustained high levels of herbivore consumption. The past decade has seen significant advances in understanding C4 grassland ecosystem ecology, and now a wealth of data on the geological history of these ecosystems has accumulated and the phylogeny of grasses is much better known. Edwards et al. (p. 587) review this multidisciplinary research area and attempt to synthesize emerging knowledge about the evolution of grass species within the context of plant and ecosystem ecology. The evolution of grasses using C4 photosynthesis and their sudden rise to ecological dominance 3 to 8 million years ago is among the most dramatic examples of biome assembly in the geological record. A growing body of work suggests that the patterns and drivers of C4 grassland expansion were considerably more complex than originally assumed. Previous research has benefited substantially from dialog between geologists and ecologists, but current research must now integrate fully with phylogenetics. A synthesis of grass evolutionary biology with grassland ecosystem science will further our knowledge of the evolution of traits that promote dominance in grassland systems and will provide a new context in which to evaluate the relative importance of C4 photosynthesis in transforming ecosystems across large regions of Earth.

The C4 plant lineages of planet Earth

Using isotopic screens, phylogenetic assessments, and 45 years of physiological data, it is now possible to identify most of the evolutionary lineages expressing the C(4) photosynthetic pathway. Here, 62 recognizable lineages of C(4) photosynthesis are listed. Thirty-six lineages (60%) occur in the eudicots. Monocots account for 26 lineages, with a minimum of 18 lineages being present in the grass family and six in the sedge family. Species exhibiting the C(3)-C(4) intermediate type of photosynthesis correspond to 21 lineages. Of these, 9 are not immediately associated with any C(4) lineage, indicating that they did not share common C(3)-C(4) ancestors with C(4) species and are instead an independent line. The geographic centre of origin for 47 of the lineages could be estimated. These centres tend to cluster in areas corresponding to what are now arid to semi-arid regions of southwestern North America, south-central South America, central Asia, northeastern and southern Africa, and inland Australia. With 62 independent lineages, C(4) photosynthesis has to be considered one of the most convergent of the complex evolutionary phenomena on planet Earth, and is thus an outstanding system to study the mechanisms of evolutionary adaptation.

Contemporaneous and recent radiations of the world's major succulent plant lineages.

The cacti are one of the most celebrated radiations of succulent plants. There has been much speculation about their age, but progress in dating cactus origins has been hindered by the lack of fossil data for cacti or their close relatives. Using a hybrid phylogenomic approach, we estimated that the cactus lineage diverged from its closest relatives ≈35 million years ago (Ma). However, major diversification events in cacti were more recent, with most species-rich clades originating in the late Miocene, ≈10–5 Ma. Diversification rates of several cactus lineages rival other estimates of extremely rapid speciation in plants. Major cactus radiations were contemporaneous with those of South African ice plants and North American agaves, revealing a simultaneous diversification of several of the worlds major succulent plant lineages across multiple continents. This short geological time period also harbored the majority of origins of C4 photosynthesis and the global rise of C4 grasslands. A global expansion of arid environments during this time could have provided new ecological opportunity for both succulent and C4 plant syndromes. Alternatively, recent work has identified a substantial decline in atmospheric CO2 ≈15–8 Ma, which would have strongly favored C4 evolution and expansion of C4-dominated grasslands. Lowered atmospheric CO2 would also substantially exacerbate plant water stress in marginally arid environments, providing preadapted succulent plants with a sharp advantage in a broader set of ecological conditions and promoting their rapid diversification across the landscape.

Phylogenetic analyses reveal the shady history of C4 grasses

Grasslands cover more than 20% of the Earths terrestrial surface, and their rise to dominance is one of the most dramatic events of biome evolution in Earth history. Grasses possess two main photosynthetic pathways: the C3 pathway that is typical of most plants and a specialized C4 pathway that minimizes photorespiration and thus increases photosynthetic performance in high-temperature and/or low-CO2 environments. C4 grasses dominate tropical and subtropical grasslands and savannas, and C3 grasses dominate the worlds cooler temperate grassland regions. This striking pattern has been attributed to C4 physiology, with the implication that the evolution of the pathway enabled C4 grasses to persist in warmer climates than their C3 relatives. We combined geospatial and molecular sequence data from two public archives to produce a 1,230-taxon phylogeny of the grasses with accompanying climate data for all species, extracted from more than 1.1 million herbarium specimens. Here we show that grasses are ancestrally a warm-adapted clade and that C4 evolution was not correlated with shifts between temperate and tropical biomes. Instead, 18 of 20 inferred C4 origins were correlated with marked reductions in mean annual precipitation. These changes are consistent with a shift out of tropical forest environments and into tropical woodland/savanna systems. We conclude that C4 evolution in grasses coincided largely with migration out of the understory and into open-canopy environments. Furthermore, we argue that the evolution of cold tolerance in certain C3 lineages is an overlooked innovation that has profoundly influenced the patterning of grassland communities across the globe.

Anatomical enablers and the evolution of C4 photosynthesis in grasses

C4 photosynthesis is a series of anatomical and biochemical modifications to the typical C3 pathway that increases the productivity of plants in warm, sunny, and dry conditions. Despite its complexity, it evolved more than 62 times independently in flowering plants. However, C4 origins are absent from most plant lineages and clustered in others, suggesting that some characteristics increase C4 evolvability in certain phylogenetic groups. The C4 trait has evolved 22–24 times in grasses, and all origins occurred within the PACMAD clade, whereas the similarly sized BEP clade contains only C3 taxa. Here, multiple foliar anatomy traits of 157 species from both BEP and PACMAD clades are quantified and analyzed in a phylogenetic framework. Statistical modeling indicates that C4 evolvability strongly increases when the proportion of vascular bundle sheath (BS) tissue is higher than 15%, which results from a combination of short distance between BS and large BS cells. A reduction in the distance between BS occurred before the split of the BEP and PACMAD clades, but a decrease in BS cell size later occurred in BEP taxa. Therefore, when environmental changes promoted C4 evolution, suitable anatomy was present only in members of the PACMAD clade, explaining the clustering of C4 origins in this lineage. These results show that key alterations of foliar anatomy occurring in a C3 context and preceding the emergence of the C4 syndrome by millions of years facilitated the repeated evolution of one of the most successful physiological innovations in angiosperm history.

COMPLEX EVOLUTIONARY TRANSITIONS AND THE SIGNIFICANCE OF C3–C4 INTERMEDIATE FORMS OF PHOTOSYNTHESIS IN MOLLUGINACEAE

C4 photosynthesis is a series of biochemical and structural modifications to C3 photosynthesis that has evolved numerous times in flowering plants, despite requiring modification of up to hundreds of genes. To study the origin of C4 photosynthesis, we reconstructed and dated the phylogeny of Molluginaceae, and identified C4 taxa in the family. Two C4 species, and three clades with traits intermediate between C3 and C4 plants were observed in Molluginaceae. C3–C4 intermediacy evolved at least twice, and in at least one lineage was maintained for several million years. Analyses of the genes for phosphoenolpyruvate carboxylase, a key C4 enzyme, indicate two independent origins of fully developed C4 photosynthesis in the past 10 million years, both within what was previously classified as a single species, Mollugo cerviana. The propensity of Molluginaceae to evolve C3–C4 and C4 photosynthesis is likely due to several traits that acted as developmental enablers. Enlarged bundle sheath cells predisposed some lineages for the evolution of C3–C4 intermediacy and the C4 biochemistry emerged via co‐option of photorespiratory recycling in C3–C4 intermediates. These evolutionarily stable transitional stages likely increased the evolvability of C4 photosynthesis under selection environments brought on by climate and atmospheric change in recent geological time.

Molecular Dating, Evolutionary Rates, and the Age of the Grasses

Many questions in evolutionary biology require an estimate of divergence times but, for groups with a sparse fossil record, such estimates rely heavily on molecular dating methods. The accuracy of these methods depends on both an adequate underlying model and the appropriate implementation of fossil evidence as calibration points. We explore the effect of these in Poaceae (grasses), a diverse plant lineage with a very limited fossil record, focusing particularly on dating the early divergences in the group. We show that molecular dating based on a data set of plastid markers is strongly dependent on the model assumptions. In particular, an acceleration of evolutionary rates at the base of Poaceae followed by a deceleration in the descendants strongly biases methods that assume an autocorrelation of rates. This problem can be circumvented by using markers that have lower rate variation, and we show that phylogenetic markers extracted from complete nuclear genomes can be a useful complement to the more commonly used plastid markers. However, estimates of divergence times remain strongly affected by different implementations of fossil calibration points. Analyses calibrated with only macrofossils lead to estimates for the age of core Poaceae ∼51-55 Ma, but the inclusion of microfossil evidence pushes this age to 74-82 Ma and leads to lower estimated evolutionary rates in grasses. These results emphasize the importance of considering markers from multiple genomes and alternative fossil placements when addressing evolutionary issues that depend on ages estimated for important groups.

Chapter 4 - The Ecological Water-Use Strategies of Succulent Plants

Abstract Plants with pronounced succulent tissues present considerable morphological and phylogenetic diversity. One way to make sense of this diversity is to recognise the common elements comprising ecological strategies shared by diverse taxa and forms. We review two broad plant ecological strategies often accompanied by pronounced tissue succulence, drought avoidance and salt tolerance, and identify common elements and variations within each. Drought-avoiding succulence typically involves high-capacitance water storage tissues, which buffer the transpiration stream and extend carbon uptake during drought. In contrast, water storage in salt-tolerant succulence is thought to be largely a by-product of massive ionic accumulation in vacuoles, and we show preliminary results indicating that succulence in halophytes is not closely linked to tissue capacitance. We review the relationship between crassulacean acid metabolism (CAM) photosynthesis and succulence, identifying putative anatomical features that may explain the frequent association of these two traits. Furthermore, although a high adaptive value of CAM has been proposed for halophytes, it is infrequent in these plants, possibly because of conflict between malate and salt storage functions in vacuoles. This may explain the surprising rarity of evolutionary transitions between drought-avoiding and halophytic succulence. We also discuss the exceptional case of the Aizoaceae, a mostly drought-avoiding group that appears to have evolved a high degree of salt tolerance, possibly multiple times. Finally, we discuss the need for a widely applicable method of quantifying succulence as a continuous trait.

Adaptive Evolution of C4 Photosynthesis through Recurrent Lateral Gene Transfer

C(4) photosynthesis is a complex trait that confers higher productivity under warm and arid conditions. It has evolved more than 60 times via the co-option of genes present in C(3) ancestors followed by alteration of the patterns and levels of expression and adaptive changes in the coding sequences, but the evolutionary path to C(4) photosynthesis is still poorly understood. The grass lineage Alloteropsis offers unparalleled opportunities for studying C(4) evolution, because it includes a C(3) taxon and five C(4) species that vary significantly in C(4) anatomy and biochemistry. Using phylogenetic analyses of nuclear genes and leaf transcriptomes, we show that fundamental elements of the C(4) pathway in the grass lineage Alloteropsis were acquired via a minimum of four independent lateral gene transfers from C(4) taxa that diverged from this group more than 20 million years ago. The transfer of genes that were already fully adapted for C(4) function has occurred periodically over at least the last 10 million years and has been a recurrent source for the optimization of the C(4) pathway. This report shows that plant-plant lateral nuclear gene transfers can be a potent source of genetic novelty and adaptation in flowering plants.

C4 eudicots are not younger than C4 monocots

C(4) photosynthesis is a plant adaptation to high levels of photorespiration. Physiological models predict that atmospheric CO(2) concentration selected for C(4) grasses only after it dropped below a critical threshold during the Oligocene (∼30 Ma), a hypothesis supported by phylogenetic and molecular dating analyses. However the same models predict that CO(2) should have reached much lower levels before selecting for C(4) eudicots, making C(4) eudicots younger than C(4) grasses. In this study, different phylogenetic datasets were combined in order to conduct the first comparative analysis of the age of C(4) origins in eudicots. Our results suggested that all lineages of C(4) eudicots arose during the last 30 million years, with the earliest before 22 Ma in Chenopodiaceae and Aizoaceae, and the latest probably after 2 Ma in Flaveria. C(4) eudicots are thus not globally younger than C(4) monocots. All lineages of C(4) plants evolved in a similar low CO(2) atmosphere that predominated during the last 30 million years. Independent C(4) origins were probably driven by different combinations of specific factors, including local ecological characteristics such as habitat openness, aridity, and salinity, as well as the speciation and dispersal history of each clade. Neither the lower number of C(4) species nor the frequency of C(3)-C(4) intermediates in eudicots can be attributed to a more recent origin, but probably result from variation in diversification and evolutionary rates among the different groups that evolved the C(4) pathway.