Literature DB >> 30165616

Mobile Elements Shape Plastome Evolution in Ferns.

Tanner A Robison1, Amanda L Grusz2,3, Paul G Wolf1, Jeffrey P Mower4, Blake D Fauskee2, Karla Sosa5, Eric Schuettpelz3.   

Abstract

Plastid genomes display remarkable organizational stability over evolutionary time. From green algae to angiosperms, most plastid genomes are largely collinear, with only a few cases of inversion, gene loss, or, in extremely rare cases, gene addition. These plastome insertions are mostly clade-specific and are typically of nuclear or mitochondrial origin. Here, we expand on these findings and present the first family-level survey of plastome evolution in ferns, revealing a novel suite of dynamic mobile elements. Comparative plastome analyses of the Pteridaceae expose several mobile open reading frames that vary in sequence length, insertion site, and configuration among sampled taxa. Even between close relatives, the presence and location of these elements is widely variable when viewed in a phylogenetic context. We characterize these elements and refer to them collectively as Mobile Open Reading Frames in Fern Organelles (MORFFO). We further note that the presence of MORFFO is not restricted to Pteridaceae, but is found across ferns and other plant clades. MORFFO elements are regularly associated with inversions, intergenic expansions, and changes to the inverted repeats. They likewise appear to be present in mitochondrial and nuclear genomes of ferns, indicating that they can move between genomic compartments with relative ease. The origins and functions of these mobile elements are unknown, but MORFFO appears to be a major driver of structural genome evolution in the plastomes of ferns, and possibly other groups of plants.

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Year:  2018        PMID: 30165616      PMCID: PMC6166771          DOI: 10.1093/gbe/evy189

Source DB:  PubMed          Journal:  Genome Biol Evol        ISSN: 1759-6653            Impact factor:   3.416


Introduction

Plastid genomes (plastomes) are a rich source of molecular sequence data and have proved to be especially useful in explorations of plant evolutionary history. From single-gene analyses to full plastome phylogenomics, important evolutionary insights can be gleaned from these relatively small, highly conserved, and minimally repetitive chromosomes (Taberlet et al. 1991; Chaw et al. 2004; Pryer et al. 2004; Yoon et al. 2004; Shaw et al. 2005; Givnish et al. 2010; Moore et al. 2010; Leliaert et al. 2012; Ruhfel et al. 2014; Gitzendanner et al. 2018). Plastomes contain high proportions of protein coding genes compared with plant nuclear genomes, with many of these genes being essential to photosynthesis (Wicke et al. 2011). Consequently, plastomes experience relatively low nucleotide substitution rates, especially in the inverted repeats (IRs), making them extremely stable over evolutionary time (Wolfe et al. 1987; Li et al. 2016; Zhu et al. 2016). The plastomes of land plants seem to be especially resistant to changes in gene content, which, along with gene order, generally varies little between distantly related lineages—even after hundreds of millions of years (Palmer 1985). Relatively few plastome genes have been lost, except in heterotrophic lineages in which photosynthetic genes are typically not required for survival (Bungard 2004). Even rarer is the acquisition of new genes (Timmis et al. 2004). Since the gain of ycf1 and ycf2 in the algal ancestors, very few new genes have been incorporated into land plant plastomes (Timmis et al. 2004; de Vries et al. 2015). However, some groups do show exceptional variability in plastome structure, even among closely related taxa (Chumley et al. 2006; Cai et al. 2008; Haberle et al. 2008; Hirao et al. 2008; Guisinger et al. 2011). Notable among these exceptional lineages is Campanulaceae, within which a prolific group of inserted open reading frames (ORFs) appear to have driven over 125 large inversions across the family (Knox 2014). Overall stability in plastome structure across land plants contrasts, strikingly, with punctuated and/or persistent genomic rearrangements that are apparent in certain lineages (Chumley et al. 2006; Cai et al. 2008; Haberle et al. 2008; Hirao et al. 2008; Guisinger et al. 2011; Mower and Vickrey 2018). Ferns are among these, showing evidence of multiple genomic inversions since their initial diversification (Stein et al. 1992; Wolf et al. 2015; Zhu et al. 2016; Labiak and Karol 2017). An increasing number of fern plastome sequences are beginning to reveal a dynamic organellar genome, shaped in large part by structural inversions and/or shifts in gene content from single copy regions into the IR (Wolf et al. 2010). Genomic inversions like these have been associated with shifts in molecular evolutionary rate (Blazier et al. 2016; Li et al. 2016; Zhu et al. 2016) and may be moderated by selective constraints related to gene synteny and gene expression (Cui et al. 2006; Wicke et al. 2011). Despite the great strides that have been made in our understanding of plastome evolution in ferns over the last decade (Mower and Vickrey 2018), dense taxonomic sampling is almost always lacking. Instead, studies of plastome evolution in ferns have focused on disparate groups of deeply divergent taxa (Gao et al. 2011; Wei et al. 2017), or on comparisons of only a few closely related species (Labiak and Karol 2017). Here, we aim to bridge this gap with the first family-scale comparative analysis of plastome structure and content in ferns. Our focus is on Pteridaceae, an early-diverging family of polypod ferns that comprises roughly 1,200 species and accounts for well over 10% of extant fern diversity (PPG I 2016). The family is cosmopolitan in distribution and occupies a wide array of niches, from shaded forests to xeric and even aquatic habitats (Tryon 1990). Members exhibit a range of reproductive modes and some groups are noteworthy for undergoing frequent whole genome duplication. Among the most striking evolutionary patterns in the family is a dramatic shift in molecular evolutionary rate that has been documented across plastid and nuclear genomes of the so-called “vittarioid” ferns (Rothfels and Schuettpelz 2014; Grusz et al. 2016). In this study, we leverage genome skimming data to assemble and analyze 27 new plastomes from across the Pteridaceae in an effort to: 1) examine plastome variation in Pteridaceae; 2) gain insight into genomic shifts within members of the Vittarioideae; and 3) reevaluate the phylogenetic relationships among major lineages comprising the family. Our data expose a massive plastome inversion and a group of mobile elements—newly characterized here—that appear to be a particularly dynamic component of fern plastomes, as evidenced from within Pteridaceae and beyond.

Materials and Methods

Taxon Sampling

Taxonomic sampling included 29 ingroup species, representing all major clades within the Pteridaceae (Schuettpelz et al. 2007), as well as three outgroup taxa (Table 1). Increased sampling from within subfamily Vittarioideae was undertaken in an effort to better understand the molecular evolutionary rate heterogeneity between the two main subclades therein, Adiantum and the vittarioid ferns.
Table 1

Taxonomic Sampling and Voucher Information for Samples Used in This Study

TaxonVoucher or CitationGenbank Accession
Adiantum aleuticum (Rupr.) C. A. ParisRothfels 4097 (DUKE)MH173079
Adiantum capillus-veneris L.Wolf et al. (2004)NC004766
Adiantum tricholepis FéeRothfels 08-094 (DUKE)MH173071
Antrophyum semicostatum BlumeSchuettpelz 1561 (BO)MH173087
Bommeria hispida (Mett. ex Kuhn) Underw.Beck 1130 (DUKE)MH173074
Calciphilopteris ludens (Wall. ex Hook.) Yesilyurt & H. Schneid.Huiet s.n. (DUKE)MH173084
Ceratopteris cornuta (P. Beauv.) Lepr.Rothfels 4298 (DUKE)MH173082
Ceratopteris richardii Brongn.Marchant et al. unpub.KM052729
Cheilanthes bolborrhiza Mickel & BeitelRothfels 3294 (DUKE)MH173073
Cheilanthes micropteris Sw.Prado 2132 (DUKE)MH173078
Cryptogramma acrostichoides R. Br.Rothfels 4195 (DUKE)MH173081
Cystopteris chinensis (Ching) X. C. Zhang & R. WeiWei et al. (2017)KY427337
Dryopteris decipiens (Hook.) KunzeWei et al. (2017)KY427348
Gastoniella chaerophylla (Desv.) Li Bing Zhang & Liang ZhangPrado 2178 (SP)MH173080
Haplopteris elongata (Sw.) E. H. CraneSchuettpelz 1559 (BO)MH173086
Hemionitis subcordata (D. C. Eaton ex Davenp.) MickelRothfels 3163 (DUKE)MH173072
Jamesonia brasiliensis ChristSchuettpelz 1444 (SP)MH173077
Llavea cordifolia Lag.Schuettpelz 1744 (US)MH173088
Myriopteris covillei (Maxon) Á. Löve & D. LöveSchuettpelz 443 (DUKE)MG953517
Myriopteris lindheimeri (Hook.) J. Sm.Schuettpelz 450 (DUKE)NC014592
Myriopteris scabra (C. Chr.) Grusz & WindhamWindham 3495 (DUKE)MH173083
Notholaena standleyi MaxonSchuettpelz 435 (DUKE)MH173067
Onychium japonicum (Thunb.) KunzeSchuettpelz 1057 (DUKE)MH173069
Pellaea truncata Goodd.Schuettpelz 430 (DUKE)MH173066
Pentagramma triangularis (Kaulf.) Yatsk., Windham & E. Wollenw.Schuettpelz 1332 (DUKE)MH173070
Pityrogramma trifoliata (L.) R. M. TryonRothfels 3658 (DUKE)MH173075
Pteridium aquilinum (L.) Koon.Der et al. unpub.NC014348
Pteris vittata L.Schuettpelz 893 (DUKE)MH173068
Scoliosorus ensiformis (Hook.) T. MooreSchuettpelz 1782 (US)MH173090
Tryonia myriophylla (Sw.) Schuettp., J. Prado & A. T. CochranSchuettpelz 1434 (SP)MH173076
Vaginularia trichoidea FéeSchuettpelz 1553 (BO)MH173085
Vittaria appalachiana Farrar & MickelStevens OH-p1-s11 (PUR)MH173091
Taxonomic Sampling and Voucher Information for Samples Used in This Study

DNA Extraction, Library Prep, and Sequencing

Whole genomic DNA for all newly sampled ingroup taxa (27 total) was extracted from silica-dried leaf tissue using the Qiagen DNeasy Plant Mini Kit (Germantown, Maryland) following the manufacturer’s protocol. Whole genomic DNA for 26 samples (all except Vittaria appalachiana) was sent to the Duke University Center for Genomic and Computational Biology for in-house library preparation and sequencing. There, individual genomic libraries (∼300 bp) were prepared using the Kappa Hyper Prep Kit (Wilmington, Massachusetts). In total, 32 samples (26 included in this study) were multiplexed and pooled over one complete flowcell (8 lanes) on the Illumina HiSeq 2000/2500 platform for 125 bp paired-end sequencing. The V. appalachiana DNA was sent to BGI (Shenzhen, China) and sequenced on the Illumina HiSeq 2000 platform, generating 5 Gb of 100 bp paired-end reads from an ∼800 bp library.

Genome Assembly and Annotation

Raw sequence reads from V. appalachiana were assembled using Velvet version 1.2.03 (Zerbino and Birney 2008) according to previously described procedures (Guo et al. 2014; Sigmon et al. 2017). Genome assembly for all other ingroup taxa was performed using NOVOPlasty (Dierckxsens et al. 2017). NOVOPlasty implements a seed-based, de novo genome assembly, which can lessen structural assembly biases that may otherwise mask inferred rearrangements. NOVOPlasty employs the seed to retrieve a given sequence from the target genome, which is then extended and circularized (Dierckxsens et al. 2017). In most cases, the rbcL gene from Adiantum capillus-veneris (NC_004766; Table 1) was used as a seed sequence, but in select cases, if rbcL had inadequate coverage, the entire plastome of A. capillus-veneris was used instead. Raw, unfiltered Illumina reads were subsampled to ≤30 million reads to reduce memory requirements. The default k-mer of 39 was used unless there was low organellar genome coverage (<1%), in which case the k-mer was reduced to 23–30. In cases involving long repetitive regions, higher k-mers of 45–55 were used. For Jamesonia brasiliensis and Cheilanthes bolborrhiza, complete assembly of plastomes was not possible, but we were able to get contigs of considerable size, which have been included in this study. Following assembly, genomes were annotated in Geneious 11.1 (Kearse et al. 2012), using the gene sequences of A. capillus-veneris as a reference. Putative RNA editing sites were annotated to retain conserved ORFs (Wolf et al. 2003, 2004). Intergenic sequences that differed dramatically from A. capillus-veneris were queried against the NCBI Nucleotide database using BLAST (Altschul et al. 1990) to ensure that they did not result from the false assembly of mitochondrial or nuclear sequences. Assembly errors were further assessed by mapping raw reads to the newly assembled genome using Bowtie2 (Langmead and Salzberg 2012), looking for dips in read depth. Additionally, overall plastome assembly quality was assessed for each sample using Pilon (Walker et al. 2014). In all cases, changes proposed by Pilon were relatively minor (<10 nucleotides) suggesting that the quality and accuracy from NOVOPlasty assembly was high.

Plastome Phylogenomic Analyses

In total, 32 plastomes were included in our phylogenomic analyses; 26 were new to this study and the remaining 6 were obtained from Genbank (Table 1). Each annotated plastome was opened in Geneious and all CDS/gene regions were extracted in FASTA format. Using these taxon-specific FASTA files, containing all CDS/gene regions, we then compiled a FASTA file for each locus. Sequences for each region were aligned using MAFFT 7.394 (Kuraku et al. 2013; Katoh et al. 2017) and alignments of all loci concatenated using Sequence Matrix (Vaidya et al. 2011). The resulting concatenated matrix, comprising 76 loci and 68,047 nucleotide sites, partitioned by gene, was processed through PartitionFinder2 (Lanfear et al. 2012, 2017) on the CIPRES Science Gateway version 3.3 (Miller et al. 2010) using the following settings: Branchlengths = linked, models = GTR, GTR + G, GTR + I + G, and model_selection = AICc. PartitionFinder2 identified 36 unique model partitions spanning the concatenated matrix. Phylogenomic analyses of the concatenated, partitioned data set were implemented using maximum likelihood (ML) and Bayesian optimality criteria on the CIPRES Science Gateway version 3.3 (Miller et al. 2010). ML searches were conducted in RAxML V.8 using multiparametric bootstrapping (−b; 1,000 replicates) and our previously described partitioned model (−q). Bayesian inference was performed using MrBayes 3.2.6 and comprised four independent runs, each with four chains (one cold, three heated) and otherwise default (i.e., flat) priors, with the exception that rates of evolution were allowed to vary among loci (ratepr = variable). Chains were run for 10 million generations and trees were sampled from the cold chain every 1,000 generations. To determine at which point the analysis had reached stationarity, the standard deviation of split frequencies among the independent runs (as calculated by MrBayes) was examined and the output parameter estimates were plotted using Tracer v1.6 (Rambaut et al. 2014). Based on convergence diagnostics, the first 2.5 million generations were excluded before obtaining a consensus phylogeny and clade posterior probabilities with the “sumt” command (contype = allcompat).

Characterizing MORFFO Elements

To search for MORFFO-like sequences in GenBank, all MORFFO insertions found in Pteridaceae were aligned using Geneious, and a consensus sequence was generated. All BLAST (Altschul et al. 1990; Madden 2013) queries for MORFFO were performed using this consensus sequence. This consensus sequence was also used when querying both VecScreen (NCBI Resource Coordinators 2017) and RepeatMasker (Smit et al. 2013). Three main search strategies were employed when using NCBI Nucleotide BLAST. Initial queries for MORFFO-like sequences were performed with BLASTN using the default parameters. Then, BLASTX and TBLASTN searches were performed using the default parameters and a word size of 3. Additional searches using specific MORFFO sequences rather than a consensus returned equivalent results. To evaluate the level of selective constraint on the three MORFFO genes, estimates of dN/dS were calculated for five species that contained all three MORFFO genes (Bommeria hispida, Hemionitis subcordata, Notholaena standleyi, Tryonia myriophylla, and Vaginularia trichoidea). First, codon-based alignments were generated using the ClustalW-Codons option in MEGA version 7.0.18 (Kumar et al. 2016). Alignments were trimmed using Gblocks version 0.91b (Castresana 2000) in codon mode with a relaxed set of parameters (t = c, b2 = 3, b5 = half). For each trimmed gene alignment, branch wise estimates of dN/dS were calculated for each species using the GA-branch model (Kosakovsky Pond and Frost 2005), which uses a genetic algorithm to optimize the number of dN/dS rate classes across the tree and ML to optimize branch lengths and substitution rates, as implemented on the Datamonkey web server (Delport et al. 2010). For the analysis, the HKY rate matrix was chosen as the substitution rate model based on the Datamonkey model selection tool. To evaluate the influence of the tree topology on dN/dS estimates, the analysis was run using either a NJ tree or a user-defined tree that matched organismal relationships shown in figure 1.
. 1.

—Distribution of MORFFO elements across the Pteridaceae phylogeny. Topology results from ML analysis of plastome data (−ln L=609991.403586); thickened branches indicate bootstrap/posterior probability support=100/1.0. Symbols highlight shared insertion sites, with empty squares signifying evident lack of a MORFFO insertion. Short arrows flanking morffo1 indicate short inverted repeats. Novel insertions and losses, as inferred by maximum parsimony, are depicted as arrows or crossed-out circles, respectively.

—Distribution of MORFFO elements across the Pteridaceae phylogeny. Topology results from ML analysis of plastome data (−ln L=609991.403586); thickened branches indicate bootstrap/posterior probability support=100/1.0. Symbols highlight shared insertion sites, with empty squares signifying evident lack of a MORFFO insertion. Short arrows flanking morffo1 indicate short inverted repeats. Novel insertions and losses, as inferred by maximum parsimony, are depicted as arrows or crossed-out circles, respectively. Phylogenetic relationships among MORFFO sequences were estimated using ML best tree and bootstrap searches, implemented in RAxML V.8 (Stamatakis 2014) with multiparametric bootstrapping (−b; 1,000 replicates).

Results

We assembled and annotated 25 complete plastomes from previously unsampled species, representing all major clades within Pteridaceae (Schuettpelz et al. 2007), plus 2 partial plastome sequences for J. brasiliensis and C. bolborrhiza (139,531 and 39,380 bp, respectively). The average length of complete plastid genome sequences was 153,153 bp (range 145,327–165,631 bp) with an average GC content of 41.46% (range 36.7%–45.3%; Table 2). Gene content remained largely stable across samples, with no losses of protein coding genes relative to A. capillus-veneris. We did, however, detect a loss of trnT in all vittarioid ferns sampled (Fig. 1), as well as a loss of trnV in Onychium japonicum, Ceratopteris cornuta, plus all vittarioids with the exception of Haplopteris elongata. Across all samples, there were 82 protein coding genes, 33–35 tRNA genes and 4 rRNA genes. Gene order was unchanged across the family—with the exception of a 7,000 bp genomic inversion within the IRs of all vittarioid species except V.trichoidea.
Table 2

Summary of Basic Genomic Features of Plastomes Used in This Study

SpeciesIR Size (bp)LSC Size (bp)Genome Size (bp)SSC Size (bp)%GCMORFFO
Adiantum aleuticum26,28983,345157,51921,596451, 2
Adiantum capillus-veneris23,44882,282150,56821,39041Absent
Adiantum tricholepis23,23382,740150,66721,46142Absent
Antrophyum semicostatum20,97787,492150,27420,828401, 3
Bommeria hispida23,14282,491156,74927,974431, 2, 3
Calciphilopteris ludens26,58582,423157,06821,475431, 2
Ceratopteris cornuta22,28783,623149,42421,22737Absent
Ceratopteris richardii22,02083,178148,44421,22635Absent
Cheilanthes bolborrhiza∼25,000na39,380*Na441, 2
Cheilanthes micropteris23,30688,393157,56722,562411, 3
Cryptogramma acrostichoides22,65283,690150,16221,16842Absent
Cystopteris chinensis26,67183,429*131,808*21,708*40Absent
Dryopteris decipiens23,45682,462150,97821,60442Absent
Gastoniella chaerophylla22,65781,918148,09920,867402
Haplopteris elongata27,18880,810156,00220,816411, 2
Hemionitis subcordata30,92182,607165,63121,182431, 2, 3
Jamesonia brasiliensis27,704na139,531*20,941411
Llavea cordifolia23,20881,944149,38721,02742Absent
Myriopteris covillei25,56783,093155,54821,321422
Myriopteris lindheimeri25,69483,059155,77021,323422
Myriopteris scabra27,11582,874162,05124,947421
Notholaena standleyi27,26183,769159,55621,265421, 2, 3
Onychium japonicum23,41982,289150,15621,02941Absent
Pellaea truncata23,24082,865150,71321,36842Absent
Pentagramma triangularis23,37885,675153,44521,014421, 3
Pityrogramma trifoliata22,46582,321148,15620,90540Absent
Pteridium aquilinum23,38484,335152,36221,259412
Pteris vittata25,27582,604154,10820,954422
Scoliosorus ensiformis21,07882,358145,32720,81340Absent
Tryonia myriophylla24,14187,238156,32720,807401, 2, 3
Vaginularia trichoidea21,61884,026147,19219,930391, 2, 3
Vittaria appalachiana22,18584,330149,53120,831401
Vittaria graminifolia22,06686,058151,03520,845401, 2

* signifies that the genome was only a partial assembly and therefore the genome size is prone to error.

IR=inverted repeat; LSC=large single copy; SSC=small single copy.

Summary of Basic Genomic Features of Plastomes Used in This Study * signifies that the genome was only a partial assembly and therefore the genome size is prone to error. IR=inverted repeat; LSC=large single copy; SSC=small single copy. Several plastid DNA insertions were recovered from multiple clades within Pteridaceae. The most prominent of these comprised a suite of genomic insertions, here referred to as Mobile Open Reading Frames in Fern Organelles (MORFFO), that were detected in most of the plastomes sampled. These MORFFO clusters are characterized by three large and distinct ORFs that are variably absent, or present in a number of different arrangements (fig. 1). One ∼1,300 bp ORF (morffo1) is flanked by inverted repeat (IRs) of ∼40 bp that are often in the motif TGT CGA TAG, repeated 3–5 times. The amino acid sequences of morffo1 do not bear similarity to any characterized proteins in GenBank, but do bear similarity to a hypothetical protein found in the fern Mankuya chejuensis and the green alga Roya anglica (table 3). A larger ORF (morffo2) of ∼1,700 bp has domains similar to primases associated with mobile elements in cyanobacteria and archaea (DN_5 superfamily) when queried using BLASTX (Altschul et al. 1990; table 3). A smaller ORF (morffo3) of ∼630 bp has no significant similarity to any known genes or proteins; it is found less frequently than the 2 larger ORFs, but is still prevalent. Often, but not always, morffo1 is found inserted in frame with morffo2 to form a larger ORF of ∼3,500 bp. Importantly, morffo1, morffo2, and morffo3 can be found in a variety of different arrangements, but when present they are always found immediately adjacent to one another (fig. 1).
Table 3

Summary of Hits to MORFFO Sequences in NCBI Blast, Using Either BLASTX or TBLASTN

SpeciesOrganism Group and Genome CompartmentSearch StrategyMORFFO MatchLength of Match (aa)% IdentityAccession Number
Actinostachys pennulaFern plastomeTBLASTNmorffo223134KU764518.1
Alsophila spinulosaFern plastomeTBLASTNmorffo27844FJ556581.1
Angiopteris angustifoliaFern plastomeTBLASTNmorffo233249KP099647
Angiopteris evectaFern plastomeTBLASTNmorffo233147DQ821119.1
Asplenium nidusFern mitochondrial genomeTBLASTNmorffo126052AM600641.1
Asplenium prolongatumFern plastomeTBLASTNmorffo2110/5977/64KY427332.1
ChondrocystisaCyanobacterium plasmidTBLASTNmorffo223327AP018284.1
Crocosphaera watsoniiaCyanobacteriumBLASTXmorffo236543WP_007310072.1
Dryopteris fragransFern plastomeTBLASTNmorffo1/morffo2323/35546/49KX418656.2
Helminthostachys zeylanicaFern plastomeTBLASTNmorffo222670KM817788.2
Huperzia lucidulaLycopod plastomeTBLASTNmorffo211435AY660566.1
Huperzia serrataLycopod plastomeTBLASTNmorffo211435KX426071.1
Lepisorus clathratusFern plastomeTBLASTNmorffo1/morffo2183/20850/56KY419704.1
Lygodium japonicumFern plastomeTBLASTNmorffo215236HM021803.1
Myxosarcina sp.aGreen alga plastomeBLASTXmorffo249727WP_052055951.1
Nostoc punctiformeaCyanobacteriumTBLASTNmorffo224528CP001037.1
Ophioglossum californicumFern plastomeTBLASTNmorffo1/morffo2/morffo3120/169/6556/41/42KC117178.1
Polypodium glycyrrhizaFern plastomeTBLASTNmorffo316253KP136832
Prasiola crispaGreen alga plastomeTBLASTNmorffo241625KR017750.1
Roya anglicaGreen alga plastomeTBLASTNmorffo120230NC_024168
Roya obtusaGreen alga plastomeTBLASTNmorffo120230KU646496.1
Volvox carteriGreen alga plastomeTBLASTNmorffo1/morffo2200/30328/25EU755299.1
Woodwardia unigemmataFern plastomeTBLASTNmorffo1/morffo2247/10551/77KT599101.1

Putative DN_5 superfamily conserved domain.

Summary of Hits to MORFFO Sequences in NCBI Blast, Using Either BLASTX or TBLASTN Putative DN_5 superfamily conserved domain. The location of MORFFO elements varied across the genomes sampled, being included in the large single copy (LSC), the IR, or the small single copy (SSC) regions (fig. 2). As a whole, MORFFO sequences (morffo1, morffo2, and morffo3) were similar among species, ranging from 92% to 45% sequence identity (table 4). For those species with a full set of three MORFFO sequences, the genes appear to encode functional proteins. The coding sequences are intact (no internal stop codons or frameshifting indels) and exhibit nonsynonymous (dN) to synonymous (dS) substitution rate ratios that are consistent with selective constraint (dN/dS ≪ 1, ranging from 0.17 to 0.43), with the exception of morffo1 from T.myriophylla, which has at least two frameshifting indels and a dN/dS approaching 1 (supplementary table S1, Supplementary Material online). A weak association was observed between the genomic location of MORFFO elements and phylogenetic position among species sampled (table 4).
. 2.

—Detected insertion sites in plastomes of Pteridaceae, relative to Adiantum capillus-veneris. Light gray bar denotes inverted repeat region.

Table 4

Summary of Matches for MORFFO Sequences Within Ferns, Using BLASTN

SpeciesMORFFO PresentLength of Match (bp)% IdentityRegionAccession Number
Adiantum aleuticummorffo1/morffo21316/ 185188/67IRMH173079
Alsophila podophyllamorffo1/morffo2/morffo31250/1778/63178/76/81IRMG262389
Antrophyum semicostatummorffo1/ morffo31323/ 62953/ 57LSCMH173087
Asplenium prolongatummorffo226581IRKY427332
Bommeria hispidamorffo1/ morffo2/ morffo31296/ 1708/ 170889/ 87/ 84SSCMH173074
Calciphilopteris ludensmorffo1/ morffo2 (truncated)1324/ 92878/ 51IRMH173084
Cheilanthes bolborrhizamorffo1/ morffo21304/ 185992/ 90IRMH173073
Cheilanthes micropterismorffo1/ morffo31292/ 63050/ 50LSCMH173078
Cibotium barometzmorffo1/ morffo21296/185077/50IRNC_037893
Dicksonia squarrosamorffo1132150IRKJ569698
Diplopterygium glaucummorffo363955LSCKF225594
Drynaria roosiimorffo1131451LSCKY075853
Haplopteris elongatamorffo1/ morffo21336/ 185956/ 55IRMH173086
Hemionitis subcordatamorffo1/ morffo2/ morffo31296/ 1863/ 66591/ 75/ 92IRMH173072
Hymenasplenium unilateralemorffo1/morffo3252/ 64365/61IR/LSCKY427350
Jamesonia brasiliensismorffo1131051IRMH173077
Mankyua chejuensismorffo1/ morffo2193/18668/67IRKP205433
Myriopteris covilleimorffo2188649IRMG953517
Myriopteris lindheimerimorffo285267IRHM778032
Myriopteris scabramorffo1131098IRMH173083
Notholaena standleyimorffo1/ morffo2/ morffo31312/ 1866/ 64089/ 86/ 91IRMH173067
Pentagramma triangularismorffo2/ morffo31860/ 63083/ 84LSCMH173070
Plagiogyria glaucamorffo1130549LSCKP136831
Plagiogyria glaucamorffo2185646MitoWolf et al. (2015)
Plagiogyria japonicamorffo2129550LSCHQ658099
Pteridium aquilinummorffo228065LSCHM535629.1
Pteris vittatamorffo2117280LSCMH173068
Rhachidosorus consimilismorffo243070IRKY427356
Tryonia myriophyllamorffo1/ morffo2/ morffo31326/ 1854/ 64189/ 84/ 86LSCMH173076
Vaginularia trichoideamorffo1/ morffo2/ morffo31315/ 1836/ 63053/ 52/ 62LSCMH173085
Vittaria appalachianamorffo1131668LSCMH173091

IR=inverted repeat; LSC=large single copy; SSC=small single copy.

Summary of Matches for MORFFO Sequences Within Ferns, Using BLASTN IR=inverted repeat; LSC=large single copy; SSC=small single copy. —Detected insertion sites in plastomes of Pteridaceae, relative to Adiantum capillus-veneris. Light gray bar denotes inverted repeat region. Chromosome-wide read depth analyses revealed no shifts in coverage spanning MORFFO insertions or insertion boundaries, indicating that these inserts are not an artifact of genomic library preparation or genome misassembly. Furthermore, MORFFO insertions were detected in V.appalachiana, which was sequenced and assembled in a separate lab, using an alternative assembly protocol. We also examined each member of the MORFFO cluster using VecScreen (NCBI Resource Coordinators 2017) and RepeatMasker (Smit et al. 2013), neither of which yielded matches to any known vectors nor transposable elements. We searched for MORFFO sequences against current draft assemblies of nuclear genomes of the ferns Azolla and Salvinia on FernBase (Li et al. 2018) as well as scaffolds for the draft genomes of Ceratopteris, and whereas they were not detected in Azolla or Salvinia, we did observe the presence of morffo1 in Ceratopteris scaffolds. In addition, we searched for the presence of MORFFO in available transcriptomes from members of Pteridaceae in the 1 kp project (Johnson et al. 2012; Matasci et al. 2014; Wickett et al. 2014; Xie et al. 2014), and found no evidence of transcription of MORFFO. To test whether MORFFO elements could be of mitochondrial origin, we filtered plastid reads using the mitochondrial option in NOVOPlasty (Dierckxsens et al. 2017), and then assembled the remaining reads using morffo1 as a seed. This did not generate an assembly of any known mitochondrial sequence. Instead, a seemingly circular 2,139 bp contig was inferred in Adiantum tricholepis, containing morffo1 and morffo2, but no known mitochondrial sequences. Furthermore, this contig lacked the flanking inverted repeat normally associated with morffo1. A control assembly using the mitochondrial genes atp1 and cox1 as seed sequences was also generated using nonplastid raw reads from this species. The assemblies based on mitochondrial genes had markedly lower average coverage depth (86.5) than that of the morffo1 based assembly (556) and the plastome (359), suggesting that the MORFFO cluster in A.tricholepis exists as an independent mobile element that is not an integrated component of the mitochondrial genome. Where this element resides within the cell is unclear. Relationships among MORFFO sequences were estimated using an ML optimality criterion and 1,000 bootstrap replicates. Each MORFFO element—morffo1, morffo2, morffo3—comprises a monophyletic clade, within which some sequences are united with moderate to high bootstrap support (supplementary fig. S1, Supplementary Material online). However, relationships among sequences within each MORFFO clade were not congruent with the accepted species tree. Our final, concatenated plastome alignment included 68,047 sites spanning 76 plastid loci for 31 taxa, including three outgroups. PartitionFinder2 returned a most favorable partition model with 36 subsets (AICc: 1211937.74576), from which partition blocks were assigned in RAxML (Stamatakis 2014) and MrBayes (Ronquist et al. 2012). Trees inferred using ML and Bayesian optimality criteria were in full topological agreement with maximum support on all branches, with the exception of the branch subtending O.japonicum, T.myriophylla, J.brasiliensis, Gastionella chaerophylla, and Pityrogramma trifoliata, which was supported by an ML bootstrap of 95 and a posterior probability of 1.0 (fig. 1).

Discussion

Comparative analyses of plastomes over the past two decades have dramatically improved our understanding of their evolution across land plants. Early data painted a picture of structural and organizational stability among deeply divergent embryophyte plastomes, punctuated by relatively few large-scale inversions (Ogihara et al. 1988; Hoot and Palmer 1994; Wolf et al. 2010). Recent evidence, however, has begun to expose the plastome as a dynamic molecule that in some lineages undergoes frequent changes in DNA content and structure (Guisinger et al. 2011; Lin et al. 2012; Knox 2014; Cremen et al. 2018). As more information has come to light, many highly rearranged plastomes have also been found to host sizeable insertions, occasionally including ORFs of unknown homology (Knox 2014; Cremen et al. 2018). In some cases, these inserted ORFs appear to encode functional proteins, whereas in others they resemble conserved domains that have undergone extensive rearrangements and/or pseudogenization, comparable to what has been observed within some plastid genes (e.g., ndhK, clpP, and ycf2; Haberle et al. 2008; Lin et al. 2012; Smith 2014; Sun et al. 2016). Several studies have determined that similar, undescribed plastid ORFs are the result of horizontal transfer from mitochondria to plastids (Goremykin et al. 2009; Iorizzo et al. 2012; Ma et al. 2015; Burke et al. 2016; Rabah et al. 2017). Plastome ORF insertions like these—with no known sequence homology—have not been characterized in ferns, although previous authors have reported large intergenic expansions and insertions in some taxa (Gao et al. 2011; Logacheva et al. 2017). It was speculated that some of these intergenic expansions originated via intracellular transfer from the mitochondrion (Logacheva et al. 2017), but until now, limited sampling in previous studies has obscured the highly mobile nature of these peculiar sequences. Here, we take a focused phylogenetic approach, targeting the fern family Pteridaceae, to reveal a suite of highly mobile ORFs (MORFFO) within a broad sampling of plastomes from across the family. Preliminary analyses indicate that MORFFO elements, which are frequently associated with extensive genomic rearrangements, may be present in lineages well-removed from ferns.

Characterization of MORFFO Elements

Logacheva et al. (2017) established that “hypervariable” sequences of significant length are found in the IR of Woodwardia unigemmata as well as the LSC of Plagiogyria. Our results are consistent with their findings, and further expose the dynamic nature of these sequences (MORFFO) among a collection of closely related fern plastomes. Searches for MORFFO-like sequences outside of Pteridaceae returned similar, putatively homologous regions in many ferns (tables 3 and 4), but not in seed plants. Significantly, an 8 kb region in the plastome of the fern M.chejuensis (Ophioglossaceae) contains an expanded complement of the MORFFO cluster. Additional searches for MORFFO-like sequences outside of vascular plants revealed similar conserved domains in several cyanobacteria plastomes (table 3), as well as domains in the plastomes of the green algae Prasiola crispa, Roya obtusa, and R.anglica (table 3). Within ferns, we note that MORFFO elements are frequently found adjacent to inferred sites of genomic inversion. For example: 1) morffo1 is found adjacent to the border of one of two hypothesized inversions in the region spanning rpoB-psbZ which occurred in a common ancestor of the core leptosporangiates (fig. 3; PPG I 2016); 2) morffo3 is found within a 9.7 kb inversion that characterizes leptosporangiate ferns (Kim et al. 2014); 3) morffo1 and morffo2 are found inserted adjacent to the 7 kb inversion seen in the plastomes of vittarioid ferns; 4) and morffo1 and morffo2 also appear adjacent to an inversion described in filmy ferns (fig. 3; Gao et al. 2011; Wolf et al. 2011; Kim et al. 2014; Kuo et al. 2018). Although MORFFO insertions are frequently associated with inversions, we are unsure why. One possibility is that MORFFO may target nucleotide sites that are prone to inversion. Conversely, the insertion of MORFFO could be directly influencing inversion events. In several taxa, we observe a proliferation of the inverted repeats flanking morffo1, possibly caused by replication slippage, or possibly by the repeated insertion and excision of morffo1. In other groups, plastome reorganization has been similarly associated with the presence of small dispersed repeats like these (Wicke et al. 2011). Likewise, the relationship between MORFFO insertion sites and inversions is not unlike the insertions seen in other dynamic embryophyte plastomes (Knox 2014).
. 3.

—Major inversion events uncovered in fern plastomes. (A) Depiction of the two inversion events necessary to explain gene order differences between Angiopteris and Adiantum and their relationship to morffo1. (B) Depiction of the inversion events seen in early leptosporangiate and vittarioid ferns, highlighting relationship of morffo1 to the event.

—Major inversion events uncovered in fern plastomes. (A) Depiction of the two inversion events necessary to explain gene order differences between Angiopteris and Adiantum and their relationship to morffo1. (B) Depiction of the inversion events seen in early leptosporangiate and vittarioid ferns, highlighting relationship of morffo1 to the event. The variable presence, location, and configuration of MORFFO observed in a phylogenetic context suggests that these ORFs are mobile elements. With a few notable exceptions, plastid genes are not frequently gained or lost, yet our results indicate that MORFFO moves into, out of, and across the plastome in relatively short evolutionary timescales. Although MORFFO sequences have been observed in mitochondrial contigs (Logacheva et al. 2017), it is important to note that they are not found in either of the currently available complete mitochondrial genomes of ferns (Guo et al. 2017). Additionally, the location of these insertions in mitochondrial genomes seems to vary as much as in those of plastids, making it difficult to pinpoint a potential mitochondrial origin. Furthermore, we have also noted the presence of MORFFO in the nuclear genome of Ceratopteris. Thus, MORFFO appears to be moving across genomes as readily as within them. However, this does not explain the origin of the elements or the mechanisms of their movement. Plasmid-like sequences have been observed in the plastomes of diatoms, green algae, dinoflagellates, and red algae (Zhang et al. 1999; La Claire and Wang 2000; Ruck et al. 2014; Lee et al. 2016; Cremen et al. 2018). Although we are not aware of previous work describing chloroplast plasmids in land plants, this is a plausible mechanism to explain the variable presence and location of MORFFO elements. It would also explain the variability in order and direction of MORFFO insertions (fig. 1). As noted above (see Results section), we were able to assemble a circular sequence containing morffo1 and morffo2 from A.tricholepis, which did not have the MORFFO insert in its plastome. The coverage analysis for this sequence indicates that MORFFO is likely a high copy-number sequence that is independent of both the plastome and the mitochondrial genome. This, combined with the fact that morffo2 has regions that share similarity to conserved domains (DN_5 superfamily) associated with primase genes found in mobile elements of cyanobacteria, strongly suggests that these sequences could be of plasmid origin, possibly from a plastid plasmid. Alternatively, MORFFO elements could be of viral origin. In addition to being similar to plasmid primases, the conserved domain found in morffo2 also resembles primase genes found in phages. Viral origins could explain why MORFFO is found frequently but irregularly in fern plastomes. Likewise, many of the above arguments in favor of a plasmid or plasmid-like origin for MORFFO sequences can also be attributed to viral origin. The structural similarities that morffo1 shares with bacterial insertion sequences is noteworthy, especially because insertion sequences are known to cause inversions (Darmon and Leach 2014). This, along with the clear mobility of these sequences strongly suggests that morffo1 could be a previously undescribed insertion sequence. The case for morffo1 being an insertion sequence is made stronger by the fact that of all the MORFFO sequences, it appears to display the most independence. In nonplastid DNA, it is almost always found without the other MORFFO sequences. It is also more frequently seen independent of additional MORFFO sequences in the plastomes of ferns outside of Pteridaceae. Furthermore, copies of morffo1 were detected in the nuclear genome of Ceratopteris and the mitochondrial genome of Asplenium nidus, suggesting that it may be a particularly promiscuous mobile element. The relationship of morffo2 and morffo3 to morffo1, however, remains unclear. If morffo1 is an independent insertion sequence, then how are morffo2 and morffo3 inserted? Phylogenetic analysis of MORFFO elements reveals three strongly supported, monophyletic groups made up of morffo1, morffo2, and morffo3 elements. Relationships within each MORFFO clade do not reflect the accepted species phylogeny, but phylogenetic similarity across clades may reflect shared histories of degradation among MORFFO elements (supplementary fig. S1, Supplementary Material online). We also note that whereas MORFFO elements are pervasive in Pteridaceae, they appear to be less common in most other groups of ferns. In part, this may be an artifact of the historical reliance on reference-based assemblies, which can be biased toward assembling genomes that appear more similar to their reference, thus reducing the likelihood of detecting significant rearrangements. Based on the few sequences available in GenBank, MORFFO elements may be prevalent in Plagiogyria and Ophioglossaceae; however, it remains to be determined how widespread this cluster of ORFs is among other lineages of ferns. More studies at the family level are needed to understand the extent to which MORFFO sequences are moving throughout fern genome space. The current paucity of fern nuclear and mitochondrial genomes makes it difficult to determine the source of these inserts. At the time of writing there were only two fern mitochondrial sequences (Guo et al. 2017) available in GenBank, and no nuclear genomes, although several were in preparation. As more genomes are published in the coming years, the reservoir from which MORFFO clusters are migrating should become clear.

Plastome Variation Across Pteridaceae

Pteridaceae is an ecologically and morphologically diverse family comprising more than 10% of extant fern species (Schuettpelz et al. 2007). Within this group, subfamily Vittarioideae, comprising the genus Adiantum and the so-called vittarioid ferns, is especially noteworthy. High levels of molecular substitution rate heterogeneity have been detected between members of the genus Adiantum and the vittarioid ferns, in both plastid and nuclear DNA sequences (Rothfels and Schuettpelz 2014; Grusz et al. 2016). As noted above, we also find variation in plastome structure across the family, with MORFFO elements (morffo1, morffo2, and morffo3) being repeatedly gained, lost, and/or rearranged, even among closely related taxa (fig. 1). The physical position of MORFFO cluster insertions is relatively conserved within the five major clades comprising Pteridaceae (fig. 1), but in some cases the location and composition of these clusters varies widely, even between congeneric relatives (e.g., Myriopteris lindheimeri vs. M. scabra and V.appalachiana vs. V. graminifolia; fig. 1). Based on our sampling, we find no evidence of MORFFO elements within Cryptogrammoideae or Parkerioideae. However, unique insertions of MORFFO sequences have taken place in some members of the Pteridoideae, including J.brasiliensis (between trnN and ycf2), T.myriophylla (between trnD and trnY), and Pteris vittata (between psbM and petN). MORFFO elements were notably absent in the species of Gastoniella, Pityrogramma, and Onychium sampled (fig. 1). Compared with the Pteridoideae, subfamilies Vittarioideae and Cheilanthoideae exhibit relative stability in their MORFFO insertion sites (fig. 1). Altogether, we find at least nine unique MORFFO cluster insertions across the Pteridaceae (there are almost certainly more), not including a multitude of species-specific rearrangements, gains, and losses of individual MORFFO elements (morffo1, morffo2, and morffo3) following cluster insertions. Within each independent MORFFO cluster insertion, the presence and position of morffo1, morffo2, and morffo3 are highly variable among species sampled. For example, a variety of insertions, rearrangements, and losses of all three elements can be found in the MORFFO cluster found between rpoB and trnD within subfamily Vittarioideae (fig. 1). Likewise, the MORFFO cluster between rps12 and rrn16 in Cheilanthoideae shows insertions and losses of all three MORFFO elements, including a duplication of morffo2 in H.subcordata (fig. 1). Interestingly, vittarioid ferns do not appear to have experienced expansion or contraction of the IR, which have been associated with extensive genomic rearrangements, gene loss, and the proliferation of repetitive regions in other groups (Zhu et al. 2016). In addition to the variable presence of MORFFO elements, we find that their insertion into the ancestral vittarioid IR (fig. 1) may have also coincided with a loss of trnT. Most vittarioid ferns share an additional gene loss (trnV)—with the exception of Haplopteris elongata, in which trnV is found intact. Given that V.trichoidea and H. elongata are inferred to be successively sister to the remaining vittarioid ferns sampled (fig. 1; Schuettpelz et al. 2016), this topology implies the gain of trnV into the plastome of H. elongata. Nevertheless, a shared ∼7 kb inversion between rrn16 and rrn5 in all vittarioid ferns except V. trichoidea further supports our phylogenetic inferences based on DNA sequence data (figs. 1 and 3). The vittarioid ferns are characterized by high levels of plastome rearrangement, elevated molecular substitution rates, a shift to epiphytism, morphological reduction, and shared ancestral whole genome duplication (Pryer et al. 2016). This array of shared traits leads one to ask which (if any) might have driven these changes in vittariod plastome structure and expression. Similarly, frequent rearrangements, insertions, and losses of the MORFFO suite within the plastomes of subfamily Cheilanthoideae coincide with adaptations to extreme xeric environments, extensive whole genome duplications, hybridization, and apomixis—any of which may relate to the changes we detect in plastome structure across this subfamily. Click here for additional data file.
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