Paleocene Ipomoea (Convolvulaceae) from India with implications for an East Gondwana origin of Convolvulaceae

The chloroplast genome sequences of Ipomoea alba and I. obscura (Convolvulaceae): genome comparison and phylogenetic analysis

Ipomoea species have diverse uses as ornamentals, food, and medicine. However, their genomic information is limited; I. alba and I. obscura were sequenced and assembled. Their chloroplast genomes were 161,353 bp and 159,691 bp, respectively. Both genomes exhibited a quadripartite structure, consisting of a pair of inverted repeat (IR) regions, which are separated by the large single-copy (LSC) and small single-copy (SSC) regions. The overall GC content was 37.5% for both genomes. A total of 104 and 93 simple sequence repeats, 50 large repeats, and 30 and 22 short tandem repeats were identified in the two chloroplast genomes, respectively. G and T were more preferred than C and A at the third base position based on the Parity Rule 2 plot analysis, and the neutrality plot revealed correlation coefficients of 0.126 and 0.105, indicating the influence of natural selection in shaping the codon usage bias in most protein-coding genes (CDS). Genome comparative analyses using 31 selected Ipomoea taxa from Thailand showed that their chloroplast genomes are rather conserved, but the presence of expansion or contraction of the IR region was identified in some of these Ipomoea taxa. A total of five highly divergent regions were identified, including the CDS genes accD, ndhA, and ndhF, as well as the intergenic spacer regions psbI-atpA and rpl32-ccsA. Phylogenetic analysis based on both the complete chloroplast genome sequence and CDS datasets of 31 Ipomoea taxa showed that I. alba is resolved as a group member for series (ser.) Quamoclit, which contains seven other taxa, including I. hederacea, I. imperati, I. indica, I. nil, I. purpurea, I. quamoclit, and I. × sloteri, while I. obscura is grouped with I. tiliifolia, both of which are under ser. Obscura, and is closely related to I. biflora of ser. Pes-tigridis. Divergence time estimation using the complete chloroplast genome sequence dataset indicated that the mean age of the divergence for Ipomoeeae, Argyreiinae, and Astripomoeinae, was approximately 29.99 Mya, 19.81 Mya, and 13.40 Mya, respectively. The node indicating the divergence of I. alba from the other members of Ipomoea was around 10.06 Mya, and the split between I. obscura and I. tiliifolia is thought to have happened around 17.13 Mya. The split between the I. obscura accessions from Thailand and Taiwan is thought to have taken place around 0.86 Mya.

Variations and reduction of plastome are associated with the evolution of parasitism in Convolvulaceae

Parasitic lifestyle can often relax the constraint on the plastome, leading to gene pseudogenization and loss, and resulting in diverse genomic structures and rampant genome degradation. Although several plastomes of parasitic Cuscuta have  been reported, the evolution of parasitism in the family Convolvulaceae which is linked to structural variations and reduction of plastome has not been well investigated. In this study, we assembled and collected 40 plastid genomes belonging to 23 species representing four subgenera of Cuscuta and ten species of autotrophic Convolvulaceae. Our findings revealed nine types of structural variations and six types of inverted repeat (IR) boundary variations in the plastome of Convolvulaceae spp. These structural variations were associated with the shift of parasitic lifestyle, and IR boundary shift, as well as the abundance of long repeats. Overall, the degradation of Cuscuta plastome proceeded gradually, with one clade exhibiting an accelerated degradation rate. We observed five stages of gene loss in Cuscuta, including NAD(P)H complex → PEP complex → Photosynthesis-related → Ribosomal protein subunits → ATP synthase complex. Based on our results, we speculated that the shift of parasitic lifestyle in early divergent time promoted relaxed selection on plastomes, leading to the accumulation of microvariations, which ultimately resulted in the plastome reduction. This study provides new evidence towards a better understanding of plastomic evolution, variation, and reduction in the genus Cuscuta.

Marginal leaf galls on Pliocene leaves from India indicate mutualistic behavior between Ipomoea plants and Eriophyidae mites

We report a new type of fossil margin galls arranged in a linear series on dicot leaf impressions from the latest Neogene (Pliocene) sediments of the Chotanagpur Plateau, Jharkhand, eastern India. We collected ca. 1500 impression and compression leaf fossils, of which 1080 samples bear arthropod damage referable to 37 different damage types (DT) in the 'Guide to Insect (and Other) Damage Types in Compressed Plant Fossils'. A few leaf samples identified as Ipomoea L. (Convolvulaceae) have specific margin galls that do not match any galling DT previously described. This type of galling is characterized by small, linearly arranged, irregular, sessile, sub-globose, solitary, indehiscent, solid pouch-galls with irregular ostioles. The probable damage inducers of the present galling of the foliar margin might be members of Eriophyidae (Acari). The new type of gall suggests that marginal gall-inducing mites on leaves of Ipomoea did not change their host preference at the genus level since the Pliocene. The development of marginal leaf galling in Ipomoea is linked to extrafloral nectaries that do not offer protection against arthropod galling but indirectly protect the plant against herbivory from large mammals.

Legumes from the Paleocene sediments of India and their ecological significance

During the early Paleogene, greenhouse gases created warm global climates. These warm climates redistributed the habitat of marine and terrestrial biota globally. Understanding the ecology of biotas under extremely warm climates is important to decipher their behavior in future climate warming. Here we report two new legume fossils (Leguminocarpum meghalayensis Bhatia, Srivastava et Mehrotra sp. nov., and Parvileguminophyllum damalgiriensis Bhatia, Srivastava et Mehrotra sp. nov.) from the late Paleocene sediments of Tura Formation of Meghalaya, northeast India. Globally, the Paleocene legume fossil records indicate that legumes most likely immigrated to India from Africa via the Ladakh-Kohistan Arc during the early Paleogene. Moreover, previously reconstructed climate data from the Tura Formation indicate that legumes were well adapted to a warm seasonal climate with monsoon rains.

The temporal dynamics of evolutionary diversification in Ipomoea

Molecular phylogenies are used as a basis for making inferences about macroevolutionary history. However, a robust phylogeny does not contain the information that is necessary to make many of these inferences. Complex methodologies that incorporate important assumptions about the nature of evolutionary history are therefore required. Here, we explore the implications of these assumptions for making inferences about the macroevolutionary history of Ipomoea - a large pantropical genus of flowering plants that contains the sweet potato (Ipomoea batatas), a crop of global economic importance. We focus on assumptions that underlie inferences of divergence times, and diversification parameters (speciation rates, extinction rates, and net diversification rates). These are among the most fundamental variables in macroevolutionary research. We use a series of novel approaches to explore the implications of these assumptions for inferring the age of Ipomoea, the ages of major clades within Ipomoea, whether there are significant differences in diversification parameters among clades within Ipomoea, and whether the storage root of I. batatas evolved in pre-human times. We show that inferring an age estimate for Ipomoea and major clades within Ipomoea is highly problematic. Inferred divergence times are sensitive to uncertain fossil calibrations and differing assumptions about among-branch-substitution-rate-variation. Despite this uncertainty, we are able to make robust inferences about patterns of variation in diversification parameters within Ipomoea, and that the storage root of I. batatas evolved in pre-human times. Taken together, this study presents novel and generalizable insights into the implications of methodological assumptions for making inferences about macroevolutionary history. Further, by presenting novel findings relating to the temporal dynamics of evolution in Ipomoea, as well as more specifically to I. batatas, this study makes a valuable contribution to our understanding of tropical plant evolution, and the evolutionary context in which economically important crops evolve.

Insights from Empirical Analyses and Simulations on Using Multiple Fossil Calibrations with Relaxed Clocks to Estimate Divergence Times

Relaxed clock methods account for among-branch-rate-variation when estimating divergence times by inferring different rates for individual branches. In order to infer different rates for individual branches, important assumptions are required. This is because molecular sequence data do not provide direct information about rates but instead provide direct information about the total number of substitutions along any branch, which is a product of the rate and time for that branch. Often, the assumptions required for estimating rates for individual branches depend heavily on the implementation of multiple fossil calibrations in a single phylogeny. Here, we show that the basis of these assumptions is often critically undermined. First, we highlight that the temporal distribution of the fossil record often violates key assumptions of methods that use multiple fossil calibrations with relaxed clocks. With respect to “node calibration” methods, this conclusion is based on our inference that different fossil calibrations are unlikely to reflect the relative ages of different clades. With respect to the fossilized birth–death process, this conclusion is based on our inference that the fossil recovery rate is often highly heterogeneous. We then demonstrate that methods of divergence time estimation that use multiple fossil calibrations are highly sensitive to assumptions about the fossil record and among-branch-rate-variation. Given the problems associated with these assumptions, our results highlight that using multiple fossil calibrations with relaxed clocks often does little to improve the accuracy of divergence time estimates.