Background

Flatworms are a phylum (Platyhelminthes) of largely parasitic animals of high importance for medicine, as they cause diseases in a variety of host animal groups, including domestic animals and humans. They also exhibit a broad range of parasitic strategies, including some lineages exhibiting remarkably high host-specificity [1,2,3]. As Platyhelminthes also comprises free-living lineages, these factors make Platyhelminthes a good phylogenetic system for studying the evolution of parasitism. The predominantly parasitic three classes of flatworms are classified together as the superclass Neodermata: Monogenea (primarily ectoparasitic), Trematoda (endoparasitic flukes), and Cestoda (endoparasitic tapeworms). Whereas the monophyly of Neodermata is relatively robust, the relationships among the above three main clades, as well their monophyly, remain debated [2,3,4,5,6]. Notably, there is evidence that Monogenea, which comprises a major part of the obligate parasitic flatworm diversity, might be paraphyletic, and split into two independent radiations (subclasses): Polyopisthocotylea and Monopisthocotylea [6, 7]. Mitogenomic nucleotide sequences and gene order rearrangements indicate that Polyopisthocotylea may even be a sister group to all other Neodermata [6, 8]. Another intriguing feature of this subclass is that it also exhibits mitogenomes with rearranged gene orders; this is uncommon within the Neodermata, which mostly exhibit a highly conserved architecture [6].

Along with the family Octomacridae, Diplozoidae are the only polyopisthocotyleans primarily parasitizing freshwater teleosts [9]. They are predominantly ectoparasites, commonly found on the gills of cyprinid and characid fishes, and they have a direct life-cycle (no intermediate host), which is typical for monogeneans. However, Diplozoidae are also characterised by a unique life history: two larvae (diporpae) permanently fuse into a pair, morphing into an X-shaped “Siamese” organism [9,10,11]. They are also important for aquaculture because they cause notable damage to the gill tissue of their hosts, which may cause secondary infections and mortality [11].

Taxonomy and phylogeny of diplozoids are mainly based on morphology (central hooks, clamps and spermatozoid ultrastructure) and host fishes, but reliance on these parameters often causes taxonomic and phylogenetic artefacts [11,12,13]. Therefore, the availability of molecular markers is a prerequisite for the reliable identification and phylogenetic and taxonomic studies of diplozoid parasites. Previous phylogenetic studies mostly relied on the 28S and ITS-2 rDNA (second internal transcribed spacer of ribosomal DNA) sequences, which often produce incongruent results between different datasets and methods [11, 13,14,15,16]. This lack of reliable phylogenetic marker results in multiple unresolved phylogenetic and taxonomic questions within the Diplozoidae and Monogenea [6, 13]. Mitochondrial genomes (mitogenomes) can provide a phylogenetic resolution superior to the traditionally used single-gene markers, so they are becoming an increasingly popular tool in evolutionary, population genetic, taxonomic, phylogenetic and diagnostic studies of Platyhelminthes [7, 11, 17, 18]. The only previous study that applied mitochondrial phylogenomics to Diplozoidae produced some novel family-level relationships, which indicates that the usefulness of mitogenomes for inferring the phylogeny of Polyopisthocotylea should be further explored [11, 13].

In most animal lineages, mitogenomes are circular molecules, ranging 13 ~ 16 kb in size, that encode 37 genes—13 protein-coding genes (PCGs), two ribosomal RNA genes, and 22 transfer RNA (tRNA) genes—but comparative mitogenomic architecture analyses (e.g., gene arrangement, base composition skews, etc.) often reveal lineages that exhibit intriguing patterns of mitogenomic evolution [19,20,21,22]. The only published study of Diplozoidae mitogenomes found unique base composition patterns and elevated evolution rates in comparison with other Monogenean mitogenomes [11]. As there are currently (Dec. 2021) only 12 sequenced and annotated complete mitogenomes for the Polyopisthocotylea, this scarcity of data hampers progress in the understanding of mitogenomic architecture evolution and phylogeny of Polyopisthocotylea and Monogenea. To address this dearth of data and further explore the unique base composition of diplozoid mitogenomes, we sequenced complete mitogenomes of two Diplozoidae species: Paradiplozoon homoion (Bychowsky & Nagibina, 1959) and a recently described [23] new species Paradiplozoon yarkandense (Arken et al. [23]).

Methods

Paradiplozoon yarkandense was collected from the host Diptychus maculatus in the Taxkorgan river (a tributary of the Yarkand River) (37° 41′ 14″ N; 75° 18′ 9″ E), Xinjiang, China. Paradiplozoon homoion was collected from the host Leuciscus baicalensis in the Kelan River (a tributary of the Irtysh River) (47° 42′ 40″ N, 88° 13′ 25″ E). Xinjiang, China. Both species were morphologically identified according to our previous publications [23, 24] (Additional file 1: Text S1 and Figs. S1 to S5). DNA extraction, mitogenome amplification and sequencing, and sequence annotation and analyses were conducted exactly as described before [11]. The methodology only differed in selecting different reference mitogenomes: Polylabris halichoeres [25] and the three available Diplozoidae species [11] and different primers (Additional file 1: Tables S1 and S2). tRNAs were first identified using ARWEN [26] and MITOS [27] programs, and then R2DT [28] was further used to predict and visualise the secondary structure of selected tRNAs. ORF-Finder [29] was further used to search for genes resembling atp8 in large non-coding regions of both mitogenomes. Phylogenetic analysis was conducted on a dataset comprising all available Polyopisthocotylea mitogenomes (Additional file 2: Dataset S1). Following the evidence that using multiple outgroups produces better results than using a single outgroup [30], we used two different lineages as outgroups, two mitogenomes from the relatively closely related neodermatan clade, Monopisthocotylea: Gyrodactylus salaris (Gyrodactyloidea) [31] and Dactylogyrus lamellatus (Dactylogyridea) [32]; and two mitogenomes from Rhabditophora, belonging to the basal radiation of largely free-living flatworms [5]: Bipalium kewense [33] and Obrimoposthia wandeli [34]. PhyloSuite [35] was used to standardise annotation, extract data, and conduct phylogenetic analysis in the Flowchart mode using nucleotide sequences of 12 concatenated (but partitioned) PCGs with the help of several plug-in programs. Genes were aligned using the codon mode and the accurate G-INS-i strategy in MAFFT [36], concatenated using PhyloSuite, best-suited evolutionary models for partitions inferred using ModelFinder [37], and phylogeny was reconstructed using IQ-TREE [38] with 10,000 ultrafast bootstraps [39]. iTOL [40] was used to visualise the phylogeny and architecture using files generated by PhyloSuite. OGDRAW was used to create to-scale circular maps of the mitogenomic architecture [41].

Results

Phylogeny and identity

The ITS-2 sequence of the putative P. yarkandense exhibited 100% identity to a number of orthologous P. yarkandense sequences published in the original description study [23], whereas that of P. homoion exhibited a 100% identity to a P. homoion ITS-2 sequence sequenced by Benovics et al. [42] (Additional file 1: Figs. S5 and S6). The phylogenetic analysis resolved all major taxa, including the Diplozoidae, as monophyletic (Fig. 1). Statistical support for clades was very high (mostly over 90%). Mazocraeidea was split into two major clades; one comprising only Diplozoidae and the other containing all four remaining families included in the dataset (Diclidophoridae, Chauhaneidae, Mazocraeidae, and Microcotylidae). Within the Diplozoidae, however, the genus Paradiplozoon was paraphyletic: P. yarkandense formed a sister lineage with Paradiplozoon opsariichthydis, whereas P. homoion formed a sister lineage with Sindiplozoon sp. Eudiplozoon sp. was the sister group to the remaining four species.

Fig. 1
figure 1

The mitogenomic phylogeny of Polyopisthocotylea. Species names are followed by the GenBank accession number, statistical support is shown next to branches, and the tree scale is included in the figure. Yellow bars correspond to the A+T composition of entire mitogenomes, red bars correspond to the GC skew, and blue bars to the mitogenome length. Taxonomic identity is shown to the right: family and order (apart from Rhabditophora)

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Mitochondrial architecture and size

All genes are encoded on the same strand and the atp8 gene is missing from both newly sequenced mitogenomes (Fig. 2; Table 1). Both exhibit a gene order identical to that of Eudiplozoon sp. and Sindiplozoon sp. The only difference they exhibited was in the distribution of non-coding regions larger than 100 base pairs (bp) (Figs. 2 and 3), which is indicative of the fast evolution of non-coding sections. Both mitogenomes were the largest among the sequenced polyopisthocotylean mitogenomes: P. homoion was the largest with 17,321 bp and P. yarkandense was the second largest, with 16,816 bp (Fig. 1, Additional file 2: Dataset S1). Moreover, all other available mitogenomes were much smaller: 12,290 to 15,527 bp (some of the smallest mitogenomes were incomplete, so the lower end of the range is almost certainly a sequencing or assembly artefact). Aside from the outlier of P. halichoeres (Microcotylidae; 15,527 bp), the top five largest mitogenomes belonged to Diplozoidae. Aside from Eudiplozoon sp. (14,334 bp), all other Diplozoidae mitogenomes were larger than 15 kbp.

Fig. 2
figure 2

To-scale circular architectural maps of mitogenomes of P. homoion and P. yarkandense. The transcription direction is clockwise

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Table 1 The comparative table of mitogenomic architectures of P. yarkandense (left) and P. homoion (right)
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Fig. 3
figure 3

Gene orders in Polyopisthocotylea. Species names are followed by GenBank accession numbers. The two newly sequenced species are shaded yellow. Family-level taxonomic identity is shown to the right. Partial mitogenomes are labelled with the letter P

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Base composition and skews

The A+T-base content was high in the polyopisthocotylid mitogenomes: 65.6–72.7% (Fig. 1, Fig. 4, Additional file 2: Dataset S1). However, Diplozoidae exhibited the three lowest values in the dataset. This was particularly strongly pronounced in the P. homoion mitogenome, which shared the lowest AT content of 65.6% with Paradiplozoon hemiculteri. The elevated AT content in the dataset was largely driven by the high T-base content (39.2–50.7%). Somewhat surprisingly, the six Diplozoidae were among the top seven taxa with the highest T-content (45.2–50.7%), along with the Polystomatidae species, Diplorchis hangzhouensis (49.7%). Therefore, the reduced AT content in Diplozoidae was driven solely by the strongly reduced A-content (18.6–20.4%) in all Diplozoidae aside from Eudiplozoon sp. (23.6%) in comparison with other polyopisthocotylids (22.5–29.9%). The C-content was strongly reduced in all species (7.3–12.1%), but Diplozoidae were not consistently different from the rest of the dataset; the only minor exception was the newly sequenced P. homoion with the highest C-content in the dataset (12.1%). In terms of the G-content, Diplozoidae on average exhibited comparatively reduced values (five out of seven lowest values).

Fig. 4
figure 4

The base composition of mitogenomes of Polyopisthocotylea

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The unusual base composition was also reflected in base composition skews (Fig. 1, Fig. 5, Additional file 2: Dataset S1). Diplozoidae had much higher AT skews (−0.34 to −0.45) than the rest of the dataset (−0.15 to −0.22). The only other species that had skews comparable to Diplozoidae was D. hangzhouensis (−0.38). As regards GC skews, a majority of Diplozoidae grouped in the upper end of the range (0.358 to 0.454), but the highest value was exhibited by D. hangzhouensis (0.479), and P. homoion exhibited a low value of 0.294 (the overall range: 0.25 to 0.48).

Fig. 5
figure 5

AT and GC skews in mitogenomes of Polyopisthocotylea

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Gene comparison

For nominally congeneric species, the two newly sequenced Paradiplozoon species exhibited remarkably low identity values between genes (Fig. 6). Only three tRNA genes exhibited similarity values larger than 75%: trnF (79), trnI (77), and trnC (75). The two species also exhibited surprisingly divergent start and stop codons (Table 1). Otherwise, start/stop codons were standard for polyopisthocotyleans (Additional file 2: Dataset S2).

Fig. 6
figure 6

Gene identity (%) values between the genes of P. yarkandense and P. homoion

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This rapid sequence evolution was reflected in a high number of insertions, deletions, and in general poorly aligned gene segments within the Polyopisthocotylea dataset. For example, nad6 exhibited a 3′ elongation in P. homoion, which caused a 7-bp overlap with the downstream trnY (Table 1, Additional file 1: Fig. S8). Nad5 and nad3 were highly divergent among the available species, with few universally conserved sites, and 5′ and 3′ ends exhibiting many insertions and deletions. Nad1, nad2 and nad4 were relatively conserved, aside from their highly divergent 5′ ends. Maybe it should be noted that nad2 in D. hangzhouensis had a 3′ extension unmatched in the dataset, so we hypothesise that this is most probably an artefact. Somewhat surprisingly, nad4L was relatively conserved within the dataset. As regards cytb, 5′ and 3′ ends were highly divergent in the dataset, but the rest was conserved. cox3 was relatively poorly conserved, with insertions and deletions throughout the sequences, but also with some universally conserved sites. Start codons for this gene were perfectly conserved among all species, but the two newly sequenced species exhibited a 3′ elongation of 6 to 10 bases. Cox2 was more conserved, with fewer insertions and deletions. In P. homoion, cox2 exhibited a 3′ end elongation of 12 bases. This occurred due to a loss of the T base, which changed the stop codon TAG into –AG and caused a frameshift mutation. As a consequence, there may exist a 15 bp overlap with the downstream trM (discussed above). We sequenced this segment twice to confirm this, and found no indications of an annotation artefact. The central part of cox1 was highly conserved, higher than any other gene, but both 5′ and 3′ ends were remarkably divergent, at least for this usually highly conserved gene [43]. Paradiplozoon homoion exhibited an elongation of 15 bp at the 5′ end as compared with P. yarkandense and several other species, but these were not the only species that exhibited a 5′ elongation. Paradiplozoon homoion exhibited a slightly truncated 3′ end in comparison with most other species (but the 3′ end was not conserved among species so there is no reliable benchmark to compare it with), whereas P. yarkandense exhibited a slightly elongated 3′ end. As 3′ was highly divergent in the dataset, we have no reason to suspect sequencing or annotation artefacts. Atp6 was generally very poorly conserved, with only a few globally conserved sites and highly divergent 3′ end. Py exhibited a large insertion, which resulted in a slightly increased size in comparison with available orthologues (636 bp; compared with 556 in P. homoion).

Gene overlaps

Locations and sizes of intergenic regions and gene overlaps were also remarkably divergent for nominal congenerics (Table 1). Furthermore, several overlaps were very large. Accordingly, in the two studied species, most gene overlaps involved a tRNA gene, but we also identified some overlaps between two PCGs. A relatively large putative overlap between cytb and nad4L was conserved in both species: P. yarkandense = 10 bp, P. homoion = 16 bp (Table 1). There was also a putative remarkably large overlap of 49 bases between nad4 and nad4L genes in P. homoion. Equally surprisingly, these two genes had 59 bases of intergenic space in P. yarkandense. Although nad4L exhibited only a handful of universally conserved amino acids in the alignment of polyopisthocotylean orthologues (Additional file 1: Fig. S9), the P. yarkandense and P. homoion orthologues exhibited the identity of 60% (Fig. 6), which was an average similarity value for PCGs.

Other overlaps involved tRNA genes. In P. yarkandense, trnI exhibited a large overlap of 19 bases with the downstream nad3. The alignment of trnI genes of Polyopisthocotylea indicated that only the 3′ was not highly conserved, and the P. yarkandense orthologue was remarkably similar to other genes (Additional file 1: Fig. S10), as additionally indicated by some of the highest identity levels between the two newly sequenced species of almost 78% (Fig. 6). Notably, this gene was annotated by MITOS, whereas ARWEN and R2DT failed to fold it into a cloverleaf structure. The trnI of P. homoion was successfully folded into a standard structure (Additional file 1: Fig. S11). It is unclear whether this is an indication of an algorithm artefact, posttranslational editing [44], or non-functionality. trnG of P. yarkandense overlapped by 18 bases with the upstream cox1. This gene was less conserved than trnI (Additional file 1: Fig. S12), but it was successfully recognised as a tRNA by all three algorithms employed. It could be folded into a cloverleaf structure, but its T-arm appeared rather crippled (Fig. 7a) as compared with the P. homoion orthologue (Fig. 7b) and other polyopisthocotylean orthologues [11]. In P. homoion, trnM overlapped by 15 bases with the upstream cox2. Its 3′ end was rather poorly conserved among the orthologues (Additional file 1: Fig. S13). Structurally, it was successfully folded into a perfectly standard cloverleaf structure, apart from its 3′ end (acceptor stem), which was truncated (Fig. 7c and d).

Fig. 7
figure 7

Secondary structures of tRNA genes. a P. yarkandense trnG. b P. homoion trnG. c P. homoion trnM. (d) P. yarkandense trnM

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Discussion

Phylogenetic analysis of Polyopisthocotylea resolved all major taxa as monophyletic, and Mazocraeidea was split into two major clades: (Diplozoidae) + (all four remaining families: Diclidophoridae, Chauhaneidae, Mazocraeidae and Microcotylidae). It also provided further confirmation that the genus Paradiplozoon Akhmerov, 1974 is paraphyletic and requires a taxonomic revision. The paraphyly of Paradiplozoon is a recognised scientific fact [13, 16, 23, 42, 45]. In the study that described P. yarkandense, the ITS-2 sequence grouped it with Paradiplozoon bingolense and Paradiplozoon krugerense [23]. This clade was recognised as “Genus 3” in a recent review of diplozoid phylogeny [13]. No other species nominally included in the “Genus 3” were available for our analysis, so P. yarkandense clustered with the only available “Genus 2” species—P. opsariichthydis. This is in agreement with the proposed sister group relationship of “Genus 2” (Paradiplozoon) and “Genus 3”, which together form the Clade2 [13]. Clade 1 comprised a number of different genera: Eudiplozoon, Sindiplozoon, Inustiatus and Genus 1. The Genus 1 clade comprised Diplozoon and some Paradiplozoon species, including the P. homoion complex [13]. Sindiplozoon sp. and P. homoion forming a separate clade in our analysis supports the above topology, as they correspond to the above described “Clade 1”. The authors proposed that the “Genus 1” clade should revert to the type genus Diplozoon von Nordmann, 1832 [13]. Following this proposal, which is also supported by our study, the species currently denominated P. homoion may have to be renamed Diplozoon homoion. Remarkably, “Genus 3” contains species from Africa, Turkey and an unidentified sequence from China [13]. Our findings provide an additional indirect indication that this may be a unique genus, sufficiently evolutionarily old to have such a wide distribution (alternatively the distribution may be of a recent origin due to global trade, but in that case, this should show as a poorly resolved topology). The authors also proposed that the appropriate designation for Genus 3 may be Indodiplozoon, given that all specimens were collected from river systems that eventually enter the Indian Ocean, which may indicate that members of this proposed genus have an Indo-Pacific ancestor [13]. Accordingly, P. yarkandense may have to be renamed Indodiplozoon yarkandense. This taxonomic revision is further supported by remarkably low identity values between genes of nominally congeneric P. yarkandense and P. homoion. Additionally, the geographic distribution of the genus Indodiplozoon indicates that it may be evolutionarily rather old. In this light, it should be noted that the species inhabits the endorheic Tarim Basin in Xinjiang, China. However, a number of rivers from Xinjiang and geographically close Tibet and Qinghai empty into the Indian Ocean, so this finding may not directly contradict the above hypothesis. We should note that the accuracy of taxonomic revision is affected by a limited number of morphological parameters useful for the identification and classification of these species, as well as insufficiently detailed previous morphological descriptions and unavailability of sufficiently detailed and complete morphological maps [12, 13]. As a result, currently we do not have morphological comparative data that perfectly support the molecular results, or we even have conflicting signals from molecular and morphological data. For example, molecular data indicate that Paradiplozoon homoion should be assigned to the genus Diplozoon, but morphologically this species better resembles the classical Paradiplozoon features: the anterior part of the body between the opisthaptor and the area of the reproductive organs does not have a prominent disc dilation [46, 47] (more details in Additional file 1: Text S1 and Figs. S1 to S5). Similarly, the three Diplozoon species that putatively belong to the Genus 3 (Indodiplozoon) also share the basic characteristics of the genus Diplozoon (a prominent disc dilation in the anterior part of the body) [47]. Therefore, in cases where morphological data do not directly support the molecular data, we should seek agreement between both mitochondrial DNA (mtDNA) and nuclear DNA (nucDNA) data before going forth with taxonomic revision.

Unfortunately, in some cases, mtDNA and nucDNA data sometimes also produce contradictory results. For example, Eudiplozoon forming a sister group to all other available Diplozoidae is in disagreement with the topology produced by the ITS-2 sequences, which indicates that more studies with new molecular data are needed to resolve the phylogeny of Diplozoidae. It may also be important to note that a study based on nuclear 18S and 28S genes found that Mazocraeidae was the only polyopisthocotylean family that exhibited an elevated evolutionary rate [9], but mitogenomic sequences do not follow this pattern: Diplozoidae exhibited the longest branches in the dataset. Although our results provide further indications that mitogenomes may be a useful tool in the phylogenetics of Diplozoidae and Polyopisthocotylea, there are currently too few mitogenomic sequences available to conclude this with confidence.

Our study provides further evidence that mitogenomes of Diplozoidae are evolving at elevated rates within the polyopisthocotylean dataset. This was reflected in their exceptionally long branches, large sizes, unique base composition, large base composition skews, and very low gene sequence similarity levels between the two newly sequenced species. As an example, even the normally highly conserved cox1 gene [43] exhibited an identity value of only 71.67%, which is exceptionally low for metazoans on average, but not uncommon in Platyhelminthes [48]. Similar values were also observed in the previous Diplozoidae analysis [11]. Unique base composition and increased skews in Diplozoidae were also observed in the previous study [11]. Increased skews might be reflective of reduced purifying selection pressures [49], which would also explain long branches. The A+T-base content is commonly high in monogenean mitogenomes [2, 31, 32]. Remarkably, the elevated AT content in the Polyopisthocotylea is largely driven by the high T-base content, whereas the reduced AT content in Diplozoidae was driven solely by the strongly reduced A-content in comparison with other polyopisthocotylids. As their reduced A+T-base composition bias is reflective of their faster, and not slower, evolution, this indicates that the AT content of Diplozoidae might be evolving in the opposite direction of most other Monogenean mitogenomes, towards lower values. In some other aspects, the two newly sequenced mitogenomes possessed typical general characteristics of most flatworm and all neodermatan mitogenomes; e.g. all genes are transcribed from the same strand and the atp8 gene could not be identified [8, 11, 50, 51]. It should be noted that we identified a number of putative ORFs in both large NCRs, but comparison with previously annotated flatworm atp8 genes did not reveal any similarity. Without gene and protein expression data, it remains impossible to assess whether these putative ORFs are expressed and functional. The gene order exhibited by Eudiplozoon sp. and Sindiplozoon sp. was previously recognised as the ancestral architecture for the Diplozoidae, and putatively even for Polyopisthocotylea [11]. Our study offers further support for this hypothesis, as both newly sequenced mitogenomes exhibit the putative ancestral gene order.

We identified remarkably large overlaps between genes. Usually, overlaps in metazoan mitogenomes involve tRNA genes, which is believed to be a consequence of lesser evolutionary constraints on tRNA sequences [44]. The overlaps between atp6/atp8 and nad4/nad4L are common in a broad range of metazoan lineages, perhaps due to their evolutionary conserved translation from a bicistronic mRNA [19, 52,53,54,55,56,57] and the fact that atp8 and nad4L are small genes that appear to evolve under relaxed evolutionary constraints, as evidenced by the absence of atp8 from several major metazoan lineages [19]. Overlaps between PCGs of less than 10 bp have been experimentally confirmed in a nematode species [58], but the exceptionally large overlap between cox1 and nad4L observed here appears to be very rare. Much larger overlaps involving tRNA genes have been observed and experimentally confirmed in Armadillidium vulgare (Arthropoda: Isopoda) [44]. However, this was explained by the apparent existence of strong evolutionary pressure for a reduced mitogenomic size [44], which does not appear to be the case in the newly sequenced Diplozoidae species, as they possess larger than average mitogenomes. While relaxed purifying selection pressures may also be a putative explanation for the existence of unusually large overlaps, their existence remains an evolutionary puzzle. Finally, although we did our best to confirm these overlaps by conducting detailed comparative analyses and considering alternative start and stop codons, without the transcriptomic data, we cannot be 100% confident that these are not annotation artefacts.

Conclusions

Due to their comparative advantages, mitogenomic sequences are a popular marker for phylogenetic studies, but their applicability is still somewhat curbed by the fact that many taxonomic categories remain poorly or not at all represented. Furthermore, multiple studies have indicated that in some cases, mitogenomes may also produce artefactual relationships [59,60,61]. Although our initial findings are promising, future studies should be very cautious in this aspect, and seek agreement between the topology produced by mitogenomic, nuclear, and ideally morphological data, to assess whether mitogenomic data can be used with confidence to conduct a thorough revision of the taxonomy and phylogeny of Diplozoidae. Furthermore, as the reasons for their elevated evolutionary rates remain unknown, Diplozoidae are a remarkably interesting lineage for other types of evolutionary mitogenomic studies.