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- Table of Contents
BioMed Research International
Volume 2013 (2013), Article ID 407072, 18 pages
The Continuing Debate on Deep Molluscan Phylogeny: Evidence for Serialia (Mollusca, Monoplacophora + Polyplacophora)
1SNSB-Bavarian State Collection of Zoology, Münchhausenstraße 21, 81247 Munich, Germany
2Faculty of Biology, Department II, Ludwig-Maximilians-Universität München, Großhaderner Straße 2-4, 82152 Planegg-Martinsried, Germany
3Queen’s University Belfast, School of Biological Sciences, Marine Laboratory, 12-13 The Strand, Portaferry BT22 1PF, UK
4Department of Marine Ecosystems Dynamics, Atmosphere and Ocean Research Institute, University of Tokyo, 5-1-5 Kashiwanoha, Kashiwa, Chiba 277-8564, Japan
5Senckenberg Research Institute, German Centre for Marine Biodiversity Research (DZMB), Südstrand 44, 26382 Wilhelmshaven, Germany
6Museum of New Zealand Te Papa Tongarewa, P.O. Box 467, Wellington, New Zealand
Received 1 March 2013; Revised 8 August 2013; Accepted 23 August 2013
Academic Editor: Dietmar Quandt
Copyright © 2013 I. Stöger et al. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.
Molluscs are a diverse animal phylum with a formidable fossil record. Although there is little doubt about the monophyly of the eight extant classes, relationships between these groups are controversial. We analysed a comprehensive multilocus molecular data set for molluscs, the first to include multiple species from all classes, including five monoplacophorans in both extant families. Our analyses of five markers resolve two major clades: the first includes gastropods and bivalves sister to Serialia (monoplacophorans and chitons), and the second comprises scaphopods sister to aplacophorans and cephalopods. Traditional groupings such as Testaria, Aculifera, and Conchifera are rejected by our data with significant Approximately Unbiased (AU) test values. A new molecular clock indicates that molluscs had a terminal Precambrian origin with rapid divergence of all eight extant classes in the Cambrian. The recovery of Serialia as a derived, Late Cambrian clade is potentially in line with the stratigraphic chronology of morphologically heterogeneous early mollusc fossils. Serialia is in conflict with traditional molluscan classifications and recent phylogenomic data. Yet our hypothesis, as others from molecular data, implies frequent molluscan shell and body transformations by heterochronic shifts in development and multiple convergent adaptations, leading to the variable shells and body plans in extant lineages.
Molluscs are a morphologically megadiverse group of animals with expansive body plan modifications. There is no doubt about the monophyly of Mollusca as a whole or of any of the eight extant molluscan classes, based on strong morphoanatomical evidence and the consensus of molecular studies . Despite a number of important recent studies, resolving ingroup molluscan topology remains contentious (Figure 1(a)) and a major challenge of invertebrate evolution .
Other studies have not had access to suitable material for broad taxon sampling, in particular for monoplacophorans, a class of small deep-sea molluscs that still remain rare and largely inaccessible [3, 4]. Among several recent studies on molluscan phylogeny, most use a subset of classes [5–7]; only one phylogenomic study so far has included all eight classes .
Multigene studies on ribosomal proteins  and housekeeping genes  and two broad phylogenomic (EST-based) data sets [5, 8] supported a monophyletic clade Aculifera. This clade comprises those molluscs with a partial or entire body covered by a cuticle with calcareous spicules or scales and is composed of shell-less vermiform molluscs (aplacophoran) and shell-plate bearing Polyplacophora (chitons). The opposing clade Conchifera (incorporating the five classes with a “true” shell) remains controversial; phylogenomic studies recovered a monophyletic clade Conchifera [5, 8], but ribosomal protein multigene and housekeeping gene analyses showed paraphyletic Conchifera [6, 7].
A contradictory alternative hypothesis was proposed by earlier ribosomal RNA-dominated multilocus studies that included Monoplacophora and recovered this class as the sister to Polyplacophora [4, 9, 10]. This clade “Serialia” combines conchiferan and aculiferan members and is thus incompatible with results of recent molecular studies or the morphological Testaria (i.e., Conchifera + Polyplacophora) hypothesis (Figure 1). This result was widely criticised in the literature (e.g., ). Yet initial deficiencies  of the study by Giribet et al.  were addressed by Wilson et al.  and Serialia recovered again in a partially overlapping data set by Meyer et al.  and independently by Kano et al. .
The single phylogenomic data set with a monoplacophoran species also indicated some signal for Serialia, though weaker than that supporting a relationship of cephalopods and monoplacophorans within Conchifera . Phylogenomic data sets cannot yet cover the same density of taxon sampling relative to targeted gene approaches, and while systematic errors of phylogenomic analyses have been explored recently (e.g., [14–16]), there is already a suite of tools available for addressing well-known pitfalls of ribosomal RNA-based sequences (e.g., [17–20]). All data sets may still contribute to ongoing investigations of phylogeny if used and interpreted with care.
Where published topologies differ radically from concepts born from morphoanatomical hypotheses, these results have often been dismissed as artefacts even by the studies’ own authors. In addition to the “Serialia” concept, several studies over the last decade have repeatedly recovered Caudofoveata sister to Cephalopoda (e.g., [6, 9, 10, 21–23]). But this pattern has low support values [6, 12]. The position of scaphopods is also highly variable, sometimes in a clade with gastropods and bivalves [5, 7, 8] or sister to aplacophorans and cephalopods [9, 10, 21]. With only eight major clades to rearrange, it could be a serious handicap that many studies exploring molluscan topology have had to exclude one (e.g., [5, 7, 21]) to three (e.g., [4, 6]) classes, and all but one previous study  used single-taxon exemplars for at least one  to as many as three [7, 8] of those clades. More and better quality data from the monoplacophorans are necessary to resolve molluscan relationships and particularly the two mutually exclusive hypotheses Serialia and Aculifera. We assembled a large multilocus data set for molluscs, including novel sequences of three monoplacophoran species (added to previously published data for only two species, Veleropilina seisuimaruae and Laevipilina hyalina). To determine the plausibility of this new topology, we applied several tests for phylogenetic informativity, saturation of sites, and compositional heterogeneity within the molecular data sets and have also considered our results against other molecular, morphological, and fossil evidence. Finally we calculated a new time tree via a relaxed molecular clock approach, using multiple sets of fossil calibration points.
Applying carefully calibrated molecular clocks on broad extant taxon sets and reconstructing characters on dated ancient lineages are indispensable for interpretation of enigmatic key fossils such as Halkieria or Nectocaris that may form part of the early evolutionary history of the group (e.g., [24–27]). We present an alternative view on molluscan evolution that supports the Serialia hypothesis and demonstrates that the debate on pan-molluscan relationships is still in progress.
2. Material & Methods
2.1. DNA Extraction, PCR, and Sequencing
DNA from 12 molluscan taxa, including 3 previously unsampled monoplacophoran species, was extracted using the Qiagen Blood and Tissue Kit (Qiagen, Hilden) by following the manufacturer’s instructions. Amplifications of the four standard marker fragments, partial 16S, partial 18S, partial 28S, and complete H3, were carried out under PCR conditions and with primer pairs shown (see Supplementary Material available online at http://dx.doi.org/10.1155/2013/407072). Sequencing reactions were operated on an ABI 3730 48 capillary sequencer of the sequencing service of the Department of Biology of the LMU Munich by using the amplification primers. Newly generated sequences were edited in Sequencher version 4.7 (Gene Codes Inc., Ann Arbor, MI, USA).
2.2. Taxon and Gene Sampling
To compile a comprehensive and dense taxon sampling for resolving deep molluscan relationships, we expanded earlier published data sets [9, 10] by our own and archived (Genbank) data, including a broad selection of outgroups and initially including any molluscs with substantial sequence information available for five standard marker fragments (partial 16S rRNA, partial or complete 18S rRNA, partial 28S rRNA, complete H3, and partial COI). In some poorly sampled but significant ingroup clades we also included species with fragmentary sequence data. Previously unpublished, partial 16S, complete 18S and 28S, complete H3, and partial COI sequences of Veleropilina seisuimaruae were provided separately by one of the authors (YK). The total initial data set comprised 158 taxa (141 molluscan and 17 outgroup taxa; Suppl. Table 2).
2.3. Data Cleaning and Alignment
All the downloaded and new single sequences, including all 28S sequences, and all individual amplicons for 18S sequences in Solenogastres, were cross-checked against the nucleotide database of BLAST  by using the blastn algorithm. Potentially aberrant or problematic fragments were removed from the data sets (Suppl. Table 3A).
In some bivalve 28S sequences a dubious part of ca. 500 bp was detected in an otherwise homogeneous molluscan alignment. This portion differed substantially in most bivalve taxa but not in all and was highly heterogeneous also in closely related species. No pattern could be observed, so we removed the dubious region (Suppl. Table 3B).
The 18S sequences of Solenogastres were partially excluded due to contamination. Retained sequences of Epimenia species (E. sp., E. australis, and E. babai) were aligned separately with the first uncontaminated sequences of Meyer et al. , and resulting large gaps were cut by hand according to the template sequences of Micromenia fodiens, Simrothiella margaritacea and Wirenia argentea (Meyer sequences in ).
Patellogastropoda has aberrant 18S and 28S sequences with many indels causing highly incongruent alignments (own observations), leading to long branches and attraction artefacts in previous  and our own analyses. Patellogastropoda clustered with long branched Cephalopoda and Solenogastres under different regimes (Table 1). To verify the correct position of Patellogastropoda within or outside other Gastropoda a more focused data set was generated comprising only gastropod taxa plus some selected, short-branched outgroup taxa, that is, two bivalves, two polyplacophorans, one annelid, and one kamptozoan. This alignment is more homogeneous, and patellogastropods appear as a moderately long branch in a rather derived position within the Gastropoda (Suppl. Figure 2). So we confirm that patellogastropods show aberrant evolution leading to long branch attraction artefacts in broader data sets ; therefore we excluded this clade from the main analyses.
Single alignments (per fragment) were created with Mafft version 6.847b  with the implemented E-INS-i algorithm. Alignments of 16S, 18S, and 28S rRNA were masked with Aliscore version 5.1 [17, 31] by running 10,000,000,000 replicates. All ambiguous positions were automatically cut with Alicut version 2.0 [17, 31] to remove highly variable positions that could lead to aberrant phylogenetic signals. The alignments of protein coding genes H3 and COI were manually checked for stop codons using MEGA5 . The single data sets were concatenated automatically using FASconCAT version 1.0 . This procedure resulted in a total alignment of 142 taxa with 8721 bp in length and a proportion of 60% gaps (Suppl. Table 5). Where taxon sampling had to be modified, for example, removing taxa or dubious gene fragments, this was done in the initial single data sets and the complete procedure of alignment, masking and concatenation was carried out again.
Final analyses were computed with the large data set excluding Patellogastropoda (142-taxon set), a targeted taxon subset (81-taxon set, alignment length 8367 bp, proportion of gaps 57%) after pruning fast-evolving species or derived members of densely sampled undisputed clades, and the gastropod data set (all gastropods including Patellogastropoda plus selected slowly evolving outgroups). Moreover, we generated and analysed diverse data sets for control reasons to test interclass topologies: the 142- and 81-taxon sets without Aplacophora, the 142-taxon set without long-branched Cephalopoda and Solenogastres, the 142-taxon set with COI and H3 coded as amino acids (142-taxon set amino acid), and one data set that comprises only 18S, 28S, and H3 fragments of the 142-taxon set (Suppl. Table 5). The concatenated sequence matrices of the two main analyses (142-taxon set and 81-taxon set) were deposited at TreeBase (http://purl.org/phylo/treebase/phylows/study/TB2:S14594). New sequences generated herein were deposited at Genbank (Suppl. Table 2).
2.4. Preanalyses of the Data
Since saturated sequences have minimal or no phylogenetic signal and could even lead to anomalous results, we measured substitution saturation of the protein coding genes, namely, H3 and COI, with Xia’s method implemented in DAMBE version 5.2.31 . We used default parameters, and the proportion of invariable sites was specified. The method was executed for all three codon positions together, for combined first and second codon positions, and for third codon position separately. In both cases, H3 and COI, the index of substitution saturation (Iss) values of all three codon positions in combination were significantly smaller than critical index of substitution saturation (Iss.c) values. This was also true for the alignments of first and second codon positions. This assumes that those positions conserve phylogenetic signal and are useful for further analyses. In the case of third codon positions only, substantial saturation could be observed (Iss significantly higher than Iss.c). All results are shown in Supplementary Table 6. Although substitution saturation was observed in third codon positions of H3 and COI, we ran additional analyses with the complete sequence information (1st, 2nd, and 3rd codon positions) to implement potential phylogenetic signal for lower taxonomic levels.
To crosscheck the phylogenetic results of the data sets with and without excluded third codon positions of protein coding genes we conducted the same analyses with all three codon positions included, using distinct models of evolution for the three different codon positions and without third codon positions of H3 and COI.
Testing the evolutionary models for all genes and in case of COI and H3 for every single codon position and for codon positions one and two versus position three was carried out with the programs Modeltest version 3.7  (for complete alignments) and MrModeltest version 2.3  (for codon positions) by the help of PAUP* version 4b10 for Windows . With the amino acid alignments of H3 and COI we additionally tested for the best fitting amino acid model of evolution using ProtTest version 2.4 . As RAxML provides only a part of the models that can potentially be tested by ProtTest we only selected those models in our ProtTest analysis (DAYHOFF, DCMUT, JTT, MTREV, WAG, RTREV, CPREV, VT, BLOSUM62, and MTMAM). The resulting best models for all genes (16S, 18S, 28S, H3, and COI), distinct codon positions of H3 and COI, and amino acid alignments of H3 and COI as well as the corresponding proportions of invariant sites and the gamma distribution shape parameters are shown in Supplementary Table 4.
2.5. Phylogenetic Analyses
Maximum Likelihood (ML) analyses for all data sets were executed using RAxML-HPC for Windows  and RAxML version 7.2.6  on the Linux cluster of the Leibniz Computer Centre. Parameters for the initial rearrangement settings and the rate categories were optimised under the GTRCAT model of evolution and a partition by genes (16S, 18S, and 28S) and codon positions (COI, H3) by conducting the hardway analysis described by Stamatakis .
First, a set of 10 randomised Maximum Parsimony (MP) starting trees was generated. Second, based on this set of starting trees, the ML trees with a specified setting of initial rearrangements (−i 10) and with an automatically determined initial rearrangement setting had to be inferred. Third, the number of rate categories was adjusted. Initial setting –c 10 was augmented by increments of 10 up to –c 50 for all MP starting trees. The fourth step was to execute 200 inferences on the original alignments. Finally, values of 1000 bootstrap topologies were mapped on the best-scoring ML tree.
Bayesian analyses for selected data sets were conducted with MrBayes v. 3.1.2 . Partitioning with corresponding models of evolution, substitution rates and nucleotide frequencies were applied according to the results of Modeltest , MrModeltest , and ProtTest . One tree was sampled every 1000 generations. If the average standard deviation of split frequencies declined 0.01 after 5 million generations the analysis was stopped. If not, analysis was continued with another 5 million generations. If the average standard deviation of split frequencies still did not decrease, the log likelihood values were examined with Tracer version 1.5 . If the run reached stationarity, the analysis was stopped. Burn-in was set to 2500 after 5 million generations and to 5000 after 10 million generations.
2.6. Molecular Clock Analyses
Time estimations were performed with the software package BEAST version 1.6.1 . The program is based on the Bayesian Markov Chain Monte Carlo (MCMC) method and therefore can take into account prior knowledge of the data. That is used when nodes in the topology are calibrated and the rate of molecular evolution along the branches is estimated.
We used nine fossil calibration points (Suppl. Table 7) with their corresponding prior distributions and assumed a relaxed clock with a lognormal distribution  of the rates for each branch (Suppl. Table 7). This setting is recommended because it additionally gives an indication of how clock-like the data are . Calibration points were set with a minimum bound according to Jörger et al. . To reduce computing time we used the targeted (81-taxa) data set for time estimations. The topology was constrained according to the resulting tree of the phylogenetic analyses.
An Xml-file with all information on data, calibration points, priors and the settings for the MCMC options was created with BEAUti version 1.4.7 . Gamma-shaped priors for all nine calibration points were used (Suppl. Table 7). We assumed that the lower bound of each calibration point is not more than 10% of its maximum age. In case that the next older fossil is within these 10% boundary we used the maximum age of that fossil as lower bound for the younger fossil .
Detailed partitioning of genes (16S, 18S, and 28S) and codon positions of COI and H3 and the constraint tree topology were added by hand to the Xml-file. The analysis was executed for 30 million generations, sampling one tree every 1000 generations on the Linux cluster of the Leibniz Computer Centre. The implemented program Tracer version 1.5  was used to confirm that posterior probabilities had reached stationarity. Burn-in was set to 25% (7500), so 22,500 trees were effectively analysed with TreeAnnotator version 1.6.1  to form the summary tree. Further, to check the reliability of our fossils, we repeated the same analysis several times and always omitted one calibration point (Table 2; Suppl. Table 7).
2.7. Testing Hypotheses
Several existing hypotheses about the molluscan interrelationships (Table 3) were tested by executing Approximately Unbiased tests (AU tests) implemented in Treefinder version of October 2008 . Therefore the input constraint trees were computed with RAxML-HPC  by using the –g-option and the associated partition by genes and codon positions. Those input tree topologies were tested in Treefinder with maximum number of replicates under the GTR model.
3. Results and Discussion
Analysing traditional multilocus markers for several large taxon sets with Maximum Likelihood and Bayesian methods under different alignment and masking regimes (Table 1, Suppl. Table 5), we recovered consistent phylogenetic trees (Figure 1(c)) with monophyletic Mollusca in contrast to other studies with similar markers [9, 10, 19, 21] and strong support for the monophyly of all molluscan classes, including Bivalvia (also in contrast to some earlier studies [9, 19, 21]).
Our approach included rigorously testing of all amplicons before and after alignment, which led to the exclusion of aberrant or problematic, previously published sequences from the data set (Suppl. Table 3). Criticism of previous accounts using the same set of markers has included the incomplete representation of taxa and the varying extant of missing data [12, 49]. Missing data is a common burden of multilocus studies and will be more severe for phylogenomic approaches [14, 15]. Our preanalyses showed that dubious sequences or ambiguous parts of alignments had much greater effect on the outcome than selecting taxa with the highest amount of data available. Rather than maximizing sequences per species, we concentrated on increasing taxon sampling to minimise potential branch lengths. Our quality controlled 158-taxon set includes 17 lophotrochozoan outgroups. Analytical trials on different subsets of nonmolluscan outgroups altered outgroup topology and support values of some basal ingroup nodes but did not change the ingroup topology (Figure 1).
Alignment issues involved in ribosomal RNA data were addressed by an array of measures proven to be beneficial (; see Section 2). Potential homoplasy in protein coding genes (especially the third codon positions) in our preferred multilocus analysis was addressed by additionally running the analysis with those fragments (COI and H3) encoded as amino acids. This had little effect on the topology but supported monophyletic Aplacophora. We applied a variety of alignment tools, including masking (Aliscore ) and refinement algorithms based on secondary structures (RNAsalsa ) and applied compartmentalised analyses of taxon clusters causing obvious alignment problems. Excluding patellogastropods (142-taxon set, Suppl. Figure 1; see Section 2) did not change our molluscan backbone topology (Figure 1(c)) but improved alignments. Separately analysing gastropods plus some slowly evolving outgroup taxa shows patellogastropods cluster with vetigastropods (Suppl. Figure 2). Our main aim was to elucidate molluscan relationships at the class level; thus we further pruned outgroups and fast-evolving members from more densely sampled ingroups (such as heterobranch gastropods) and used an 81-taxon set presented here in our main analysis (Figure 2).
3.2. The Basal Molluscan Dichotomy
In our new tree, the phylum Mollusca is divided into two clades (Figure 1(c), Figure 2, Suppl. Figure 1). The first clade is composed of Gastropoda sister to a clade of Bivalvia and Serialia (Monoplacophora + Polyplacophora). For convenience we will refer to this clade as “Dorsoconcha”; the name refers to the (plesiomorphic) presence of a dorsal shell for members of this clade, though modified to two lateral valves in bivalves and to (7-)8 dorsal plates in chitons, and the shell internalised or lost multiple times especially among gastropods.
Gastropods, bivalves, and monoplacophorans are commonly considered to be united by their single shell (secondarily split in bivalves) built by a shell gland at the mantle border (and by the entire mantle roof secreting organic matrix and calcareous layers letting the shell grow thicker, or repair damage). Chitons are traditionally excluded from the hypothetical clade “Conchifera” on the basis of their eight shell plates. The chiton girdle is also covered by a cuticle with embedded calcareous and organic sclerites, similar to the body cuticle of the shell-less aplacophorans, but according to our results, this is convergent and may reflect the different, single versus multicellular spicule formation in these taxa . That chitons cluster with monoplacophorans rather than aplacophorans is congruent to previous molecular approaches that included monoplacophoran exemplars [4, 9, 10, 13]. The exception is the phylogenomic study by Smith et al. , in which a single monoplacophoran, Laevipilina hyalina, robustly clustered with cephalopods in the main analyses, though parts of the genes used also showed signal supporting an association with chitons.
In the second major molluscan clade, Scaphopoda are sister to a clade of vermiform Caudofoveata and Solenogastres, plus Cephalopoda. Herein we will call this clade “Variopoda,” referring to the various derived foot attributes of its members: the digging foot in Scaphopoda, reduced narrow gliding sole or completely lost in (adult) aplacophorans, and transformed in cephalopods possibly building parts of tentacles and funnel. Dorsoconcha appears as a monophyletic group although bootstrap support is low (60%), and the Variopoda is strongly supported in all Maximum Likelihood analyses; Bayesian posterior probabilities are high for both nodes (Figure 2, Suppl. Figure 1).
The placement of aplacophorans within Variopoda is unconventional, but a sister relationship between Scaphopoda and Cephalopoda has been previously put forward [51, 52]. Previous multilocus approaches with broad taxon sampling (i.e., more than one exemplar of each aplacophoran class) are actually not in general disagreement with Variopoda, since contaminated aplacophoran sequences may account for occasionally aberrant topologies [9, 10, 13]. Inner scaphopod topology resolves the two currently recognised groups Dentaliida and Gadilida, as does Cephalopoda splitting into modern Nautilida and Coleoidea, and is congruent with previous classifications .
We calculated time trees with a Bayesian molecular clock approach (Figure 3) using a mix of younger and older calibration points (Suppl. Table 7). We also tested sets of calibrations successively excluding each single calibration point used (Table 2) to minimise circularity involved by calculating individual node times . All our time trees confirm a Precambrian origin of Mollusca (Table 2, Suppl. Table 8) in agreement with previous studies , and 95% confidence time bars of all our time trees allow for a Cambrian origin of those classes with a reliable fossil record (Figure 3). As a further sensitivity test we also calculated a time tree from a data set excluding aplacophorans; the topologies are congruent and node ages almost identical, confirming general time estimates (not shown).
Molluscan diversification occurred at an extremely rapid pace after the initial origination of the shell (Figure 3). Short branches at the base of the ingroup can be artefacts of signal erosion in deep nodes , but as we discuss below, the rapid early evolution of Mollusca is also supported by the fossil record. Our molecular clock indicates a potential time frame of only around 20–40 million years from the first shelled molluscs (ca. 560–540 Ma) to the presence of differentiated variopod, dorsoconch, gastropod, bivalve, and serialian stem lineages (ca. 520 Ma). The shell was central for rapid evolutionary success of molluscs, and shell modification and divergence are correlated with adaptive radiations during this early period.
3.3. Evaluating Molecular Data Sets
All recent multigene and phylogenomic studies [5–8] have tested the effects of gene sampling, analytical methods, and inference programs; like our results, their topologies were more or less robust, also against varying outgroup selection. Sensitivity analyses do not attribute the major split into Variopoda (or parts thereof) and Dorsoconcha or the recovery of Serialia to LBA effects. Yet our multilocus study uses fewer markers and nucleotides than “next-generation sequencing” studies [5–8], so it may be more prone to inadequate signal of certain markers or stochastic errors.
Split decomposition analyses of an earlier multilocus set  usually recovered the single monoplacophoran species among bivalves , consistent with a Dorsoconcha clade. Splitstree analyses (not shown) of our improved data set still show overall polytomy and some individual taxa are clearly misplaced in the network (e.g., the gastropod Crepidula clusters with cephalopods). Overall, most dorsoconch terminals are separated from variopods. Within Dorsoconcha, monoplacophorans cluster with chitons and bivalves. A lack of tree-like structure and a priori split support, especially in a large and heterogeneous taxon set, may not necessarily mean that there is too little signal for phylogenetic analyses; it just means that there is conflict that may or may not be resolved applying current models of sequence evolution.
Nuclear ribosomal RNA genes were shown to be informative even on deeper levels than basal molluscs, if treated adequately . Other, supposedly faster-evolving mitochondrial markers (partial COI, 16S) were stringently masked herein, partitioned when necessary or excluded when saturated (Suppl. Tables 4–6). Combined analysis incorporates multiple tempos of evolution experienced by the different loci and is therefore more representative of deep evolutionary patterns. Our backbone topology is robust against varying the taxon and marker sets, masking and partitioning regimes, models of evolution, and methods of analyses (Table 1, Suppl. Tables 4 and 5).
3.4. Evaluating Alternative Morphological and Molecular Concepts
We directly evaluated the statistical fit of major competing morphology- or molecular-based concepts constraining our topologies and calculating their likeliness according to our data set. Using our preferred 81-taxon set with all markers, but also under most other schemes, the AU test rejects all the higher molluscan textbook concepts : the Testaria, Aculifera, Conchifera, Cyrtosoma, and Diasoma hypotheses, with the highest possible statistical support; the same AU tests do not reject Dorsoconcha nor Variopoda (Table 3). We also tested our data against three new molecular concepts (Figure 1(b)): Pleistomollusca (Bivalvia + Gastropoda) established by Kocot et al.  and the clades of Monoplacophora and Cephalopoda  versus other conchiferans (Scaphopoda, Gastropoda, and Bivalvia) [5, 8]. Only the clade of Monoplacophora and Cephalopoda was not rejected with significant support in any of the main analyses, but all these groups received much lower AU values than our unconstrained topology.
While several recent phylogenomic studies recover Aculifera [5, 7, 8], the Serialia concept has been tested only by Smith et al. , by inclusion of a single monoplacophoran species. Though association with cephalopods is preferred, there is a weaker signal also for Serialia . Kano et al.  recovered Serialia but did not include any aplacophoran taxa in their data set. The Serialia as a concept cannot be dismissed yet, and our dense taxon sampling herein, though based on far fewer sequences than recent phylogenomic approaches [5, 8], still may allow for a more differentiated and perhaps more correct view on molluscan interclass relationships.
The association of cephalopods and aplacophorans has been recovered previously but dismissed as an artefact of high substitution rates in rRNA genes [6, 13, 21]. But our results cannot easily be explained by long branch attraction (LBA) effects (contra ). Branch lengths of scaphopods and caudofoveates are moderate, and the variopod node is stable against removal of putative long branched taxa showing accelerated evolutionary rates or biased base compositions , such as the branches of Solenogastres or Cephalopoda or both (trees not shown).
Molluscan evolution, whatever the underlying tree, is known to be laden with convergence at all taxon levels, including morphological features previously suspected to be informative for deep phylogeny (e.g., [56–58]). Conclusions derived from single organ systems, or the shell alone, are not able to exclude alternative interpretations. Coding hypothetical bauplans rather than existing representatives has been criticised [59, 60] and may lead to erroneous assumptions especially in groups with uncertain internal topology such as gastropods or aplacophorans. Morphocladistic approaches to date (e.g., [61–63]) all recovered Testaria, but this hypothesis is not supported by any molecular approaches.
Our proposed topology and any other nontestarian hypothesis imply that ancestral molluscs were complex rather than simple. This means that many anatomical characters inherited by descendants may be plesiomorphic and thus not informative, or could have been reduced or lost repeatedly, implying a high level of homoplasy. In fact, early molluscan phylogeny may have been shaped by habitat-induced selective pressure combined with heterochronic processes (e.g., ). This combination may lead to concerted morphological parallelisms powerful enough to obfuscate any phylogenetic signal, which has been found to be the case in heterobranch gastropods (e.g., [47, 65, 66]). It is possible to disentangle even highly homoplastic and heterochronic groups (e.g., [67–69]) if detailed and reliable microanatomical data are available on a dense ingroup taxon sampling, which is, however, not yet available for most molluscs. Unfortunately none of the many competing morphology-based hypotheses on molluscan class interrelationships available at present appears to represent a reliable benchmark for evaluating molecular topologies.
3.5. Topologies Tested against the Fossil Record
Molluscan diversification has been widely assumed to originate from a basal “monoplacophoran” bauplan , although early single shelled molluscs cannot be reliable separated from gastropods or any nonmonoplacophoran univalve . The earliest calcareous molluscan-like shells, including undisputed molluscs, appear in the uppermost Precambrian, in the late Nemakit-Daldynian ca. 543 Ma . Polyplacophoran shell plates first appear in the Late Cambrian, almost 50 My later [7, 71]. This does not support the Testaria hypothesis that would suggest that chitons evolved before the invention of a true “conchiferan” shell. There are dubious disarticulated microscopic chiton-like plates  from the early Meishuchunian (likely Early Tommotian) of China, but these still appeared later rather than earlier than the very first undisputed conchiferan shells. The Aculifera concept with monoplacophorans sister to other members of Conchifera or our molecular basal dichotomy are both fully compatible with the origin of molluscan shells latest at the Precambrian/Cambrian boundary.
The earliest tryblidian monoplacophorans are recorded from the Late Cambrian . Older, nontryblidian “monoplacophorans” do not show serialised muscle scars and thus cannot be considered part of the crown-group. Yet the earliest reliable bivalves with elaborated hinge and ligament (Fordilla, Pojetaia) appear earlier, in the Early Tommotian (; ca. 535 Ma). Both Aculifera and our basal dichotomy are not contradicted by the early appearance of bivalves. Under an Aculifera topology, chiton-like stem members could appear soon after a terminal Precambrian split separating Aculifera and Conchifera. Interpreting Early to Middle Cambrian sachitids (halwaxiids) as stem aculiferans would help fill this gap , but these taxa show a chronological sequence of shell plate loss rather than acquisition, which may be contrary to a progressive transition to chitons. The mosaic taxon Phthipodochiton, which has been proposed as a stem aplacophoran, does not appear until the Ordovician [75, 76]; other fossils from the Silurian, combining aplacophoran and polyplacophoran features with some soft tissue preservation, have also been used to support the Aculifera hypothesis . These could also simply represent further disparity in extinct Polyplacophora. Regardless, there is compelling evidence from molecular systematics as well as fossil evidence that aplacophorans lost their ancestral shell (or shell plates) secondarily, and many other groups show repeated shell-loss or evolution to a vermiform body plan.
The topologies recovered by Vinther et al.  and Kocot et al.  support Aculifera but also imply that cephalopods are sister to Aculifera  or represent the earliest-diverging conchiferans  (excluding monoplacophorans from the analysis). However, there is no evidence for cephalopod-like fossils appearing earlier than, for example, bivalves. Similarly, bivalves are derived within Conchifera in the topology of Smith et al. , which is contradicted by the early fossil record of bivalves. In contrast, our basal dichotomy could fit with the many univalve small shelly fossils occurring earlier in the fossil record than bivalves, and both monoplacophorans and polyplacophorans appear later, actually at a similar time in the Latest Cambrian, and as predicted by a split of Serialia into Monoplacophora and Polyplacophora.
3.6. The Timing of Early Molluscan Evolution
The molluscan stem is Precambrian according to all our molecular time trees. The Vendian (555 Ma) body fossil Kimberella was discussed as a mollusc , but not widely accepted as such, and rather treated as lophotrochozoan stem member or “no more specifically than as a bilaterian” . According to previous constrained (e.g., ) and our less constrained time trees (Table 2, Suppl. Table 8), however, Kimberella appears late enough in the fossil record to be considered as a potential stem mollusc. The other recent molecular clock for Mollusca puts the stem Mollusca even deeper , but Kimberella is within the 95% HPD interval for the split of the basal dichotomy also recovered herein. Having confirmed the conceptual basis of our proposed topology is not rejected by evidence in the fossil record, we further consider the timing of the radiation of specific clades proposed by our molecular clock analyses (Figure 3).
Cap-shaped Helcionellidae from the terminal Precambrian (e.g., Latouchella) are putative monoplacophorans according to the seminal study by Runnegar and Pojeta  or a separate molluscan class  or, based on nonserial muscle scars, gastropods . Our time tree suggests that Nemakit-Daldynian and Earliest Tommotian molluscs with symmetrical cap-shaped shells with large openings are stem molluscs (or in the stem of one part of the basal dichotomy). In contrast, helicoid shells from the same period such as Aldanellidae (e.g., ) could well be gastropods, whether or not the animal was torted [70, 82].
Early Tommotian Watsonella, formerly known as Heraultipegma (the putatively earliest rostroconch), is a laterally compressed, bivalve-like univalve , possibly with dorsomedially decalcified or even bivalved shell . This and other laterally compressed Watsonellidae may pre-date the first reliable Bivalvia (Early to Middle Tommotian Fordilla;  versus ) by some million years and thus could well be stem bivalves (or offshoots of the dorsoconch stem) according to our time tree (Figure 3).
It is important to note that neither reliable Monoplacophora (sensu Tryblidia) nor reliable Polyplacophora (i.e., Paleoloricata) are known before Late Cambrian, and this is confirmed in our chronograms (Figure 3). Yu  interpreted the Early Cambrian Merismoconchia as having eight pairs of muscles on a pseudometameric shell, linking 8-plated chitons with single shelled monoplacophorans in a transitional row of shell fusion. The similarity of merismoconchs with both serialian classes is curious, and their early occurrence in the pretrilobite Meishucun Stage suggests they could be early stem Serialia. The microscopic merismoconchs with their ventrally still connected shell segments and seven observed pairs of muscle scars may have been a transitional stage in how to make a foot efficient for sucking and a shell more flexible to adapt to uneven hard substrates. According to our time tree (Figure 3), chiton-like shell “fragmentation” into fully separated plates occurred much later, after splitting from single-shelled monoplacophoran-like ancestors.
The Cambrian (Atdabanian) Halkieria and related Middle Cambrian halwaxiids could also be interpreted as stem Serialia (Figure 3). A role as ancestral lophotrochozoans for halwaxiids as suggested by Edgecombe et al.  is not supported by our analysis.
According to our time tree (Figure 3), Yochelcionellidae, conspicuous Tommotian to Middle Cambrian shells that have a “snorkel,” could be part of the gastropod radiation as suggested by Parkhaev , or members of the dorsoconch stem lineage, or variopod stem members. The latter possibility is especially intriguing, since Yochelcionellidae evolved a “flow-through” water system with two shell openings; a dorsal shell elongates laterally and fuses ventrally, and the body axis shifts towards anterior growth extending head and foot out of a now tube-like shell. This condition is displayed by living and fossil variopods (i.e., scaphopods, cephalopods, and nonwatsonellid Rostroconchia).
Our results show that scaphopods could have split off from the variopod stem earlier, that is, in the Early Cambrian, but the oldest potential scaphopods in the familiar modern tusk-like shape are from the Ordovician  or even post-Devonian . There is a vast record of Middle Cambrian tube-like shells that may be unrecognised parts of the early scaphopod diversification that started much earlier and morphologically less constrained than previously expected .
Knightoconus, a Middle to Late Cambrian large “monoplacophoran” conical shell with internal septa but no siphuncle , was described as a stem cephalopod  but subsequently questioned (e.g., ) and ultimately suspected to be a brachiopod . Knightoconus could fit stratigraphically with stem cephalopods based on our evidence (Figure 3), but its morphological interpretation remains in doubt. The earliest reliable cephalopod fossils are the small bodied, septate, and siphuncle-bearing Plectronoceras from the Late Cambrian. Some versions of our analysis used Plectronoceras as a soft bound calibration point; by not using Plectronoceras, the origin of cephalopods shifts considerably towards the Silurian (Table 2).
Recently, shell-less and coleoid-shaped Lower Cambrian Nectocaris pteryx was regarded as a cephalopod , but this was immediately rejected on several lines of argument [91, 92]. Other putative Early Cambrian nectocaridids such as Vetustovermis  are superficially similar to Nectocaris in having a pair of long cephalic tentacles and stalked eyes but show a ventral foot separated from the supposedly wing-like mantle. Interpreting Nectocaris as having an axial cavity with gills and a funnel would provide synapomorphies for interpreting Nectocarididae as stem cephalopods [24, 94]. Molecular clock estimates can provide further insight to such contentious interpretations; according to our time estimates (which excluded nectocaridids as potential calibration points), Nectocaris is too ancient to be a cephalopod (Figure 3). If Nectocaris could be accepted as molluscan based on its contentious morphological interpretation, our time trees would be compatible with the idea that nectocaridids are stem variopods or within the stem of an aplacophoran/cephalopod or aplacophoran clade. Nectocaridid features with superficial similarities to coleoid cephalopods [24, 94] instead could be ancestral attributes of variopods: an anteriorly elongated body with head, long and flexible head tentacles, putative preoral hood, and a more or less reduced foot.
The fossil record offers shells and body fossils which, by their occurrence and morphology, at least hypothetically fill our time tree with life. The topology and timing of our hypothesis of early molluscan evolution is not rejected by fossil evidence.
Molecular, morphological, and palaeontological evidence support (or fail to reject) our basal molluscan dichotomy. The clade Dorsoconcha includes most shelled molluscs and 98% of living species in four classes: Gastropoda, Bivalvia, Polyplacophora, and Monoplacophora.
We note two inferred potential morphological synapomorphies of Dorsoconcha, both relating to the digestive system and both somewhat ambiguous: the intestine is surrounded by the pericardium in basal lineages of gastropods, bivalves, and in monoplacophorans and may be positionally homologous in chitons (Figure 1(c) character 7) and a rotating enzymatic crystalline style (or protostyle; Figure 1(c) character 9). Many basal, noncarnivorous molluscs have a more or less well-developed stomach separated into sorting zones, but only dorsoconchs (and a family of caudofoveates ) have the complex style; this was secondarily lost in chitons, which have a derived position in our proposed topology.
Most previous studies on the phylogeny of molluscs have been driven by the Conchifera concept [1, 95] and emphasised the opinion that Serialia violates putative conchiferan synapomorphies . Such features all are plesiomorphic for dorsoconchs in our topology (Figure 1(c)). We note several potential apomorphies for Serialia (Figure 1(c)): the serial (seven or) eightfold (octoserial) dorsoventral pairs of muscle bundles, with two pairs of intertwined muscle bundles in chitons and also partly present in large Neopilina [95, 96]; serial gills in a circumpedal mantle cavity; a highly similar cerebral nerve cord; and a longitudinal elongation of the dorsoventrally flattened body, to mention just some (Figure 1(c)). The most prominent feature of Serialia, serial paired foot retractors, is also present in bivalves, but octoserial retractors appear in Ordovician Babinka and not in the earliest known bivalves in the Cambrian  (Figure 1(c) character 10). While head and buccal apparatus are reduced almost completely in bivalves, Serialia elaborated the buccal mass evolving highly similar radulae and the radula bolster. Similar foot and radula structures in patellogastropod limpets  could be either plesiomorphic or convergent, because Patellogastropoda are either an isolated early-diverging gastropod group or relatively recently derived within Vetigastropoda [98, 99].
From this topological result and the available fossil evidence, we propose that the last common ancestor of monoplacophorans and chitons was cap-shelled and adapted to epibenthic life in shallow waters, rasping algae or other microorganisms from rocky substrates (Figure 1). In this scenario, chitons are not primitive molluscs but rather a derived group, potentially adapted to high-energy marine shores. Monoplacophorans initially also were shallow water dwellers  but could have colonised deeper waters during the Palaeozoic, where modern monoplacophorans still occur . The Cenozoic or Late Cretaceous molecular dating of the diversification of living monoplacophorans and their short inner branches (, Figure 3) are compatible with earlier assumptions of pronounced anagenetic changes in the long stem line of these so-called “living fossils” [4, 100].
The clade Variopoda (Figure 1(c)) groups the scaphopods, aplacophorans, and cephalopods together in all our analyses, and it is very well supported. We infer several features of variopods, including an apparent propensity for habitat-induced transformations (noted in the taxon epithet; Figure 1(c) character 2). Some other roughly hypothesised apomorphies may refer to a clade of scaphopods and cephalopods only, that is, to variopods only under the assumption that aplacophorans represent highly paedomorphic and thus aberrant offshoots (see below): lateral extension of a primitively dorsal cap-like shell forming a tube; twisting the growth axis during ontogeny from initial dorsoventral to an anterior body extension, translocating head foot and mantle cavity with anal opening anteriorly; formation of a ring-like dorsoventral muscle insertion; multiplication of cephalic tentacles into prey-capturing feeding tentacles; and at least partly using muscle antagonist rather than merely hydrostatic systems in these tentacles (convergently in gastropod cephalic sensory tentacles); a hood is formed anterior to the mouth; and muscular retraction of the foot is used to pump water, waste, and gametes through/out the mantle cavity.
A clade of scaphopods and cephalopods repeatedly has been proposed based on morphological data, sometimes with one or the other or both together allied with gastropods , and was recovered by molecular data  and broadly within some pan-molluscan molecular phylogenies [10, 21]. In contrast, morphocladistic neontological  and palaeontological studies (e.g., [80, 102]) advocated the Diasoma concept suggesting scaphopods as sister to bivalves with a rostroconch ancestor. Developmental data showing different ontogeny of shells have not supported the latter opinion . Diasoma has been equivocally recovered within one mitogenomic analysis (, but see  for limitations of protein coding mitochondrial genes), and in one supplementary analysis of transcriptome data . Similar features such as a digging foot could be interpreted as convergent adaptations to infaunal life.
The two aplacophoran classes Caudofoveata and Solenogastres have never been associated with either scaphopods or cephalopods in morphological studies. In our analyses aplacophorans are usually paraphyletic, but some permutations, in particular when excluding (the faster-evolving, but stringently masked) COI and 16S markers, recover a clade Aplacophora sister to Cephalopoda. Aplacophora as a clade is not rejected by AU analyses of the combined 5-marker set either (Table 3). A single origin of vermiform body plans in the cephalopod stem lineage could arguably be more parsimonious than arising twice independently. Monophyly of Aplacophora is indicated by all recent studies using multiple nuclear protein coding genes and phylogenomic data sets ([5, 7, 8]; Figure 1(b)) but not neuroanatomy .
Aplacophorans may share an inferred tendency of modifying the ancestral foot, they have an elongated body with a foot (or head) shield with strong retractor muscle in caudofoveates, and the atrial cavity especially in Solenogastres could be interpreted as a modified preoral hood, as remnants of a hypothesised variopod body plan. Yet there is no morphological indication for a specifically aplacophoran-cephalopod clade. Interpretation of the vermiform molluscan morphology as progenetically derived rather than reflecting a basal molluscan condition (also assumed under the Aculifera concept) actually allows for hypotheses that resolve them at any position in the molluscan tree (or makes their position impossible to recover using currently available anatomical data). Assuming that aplacophorans (once or twice independently) initially evolved into interstitial secondary worms could be correlated with precerebral ganglia present in caudofoveates ; these transformations have evolved many times independently in interstitial worm-like gastropod groups, which are likely progenetic . Calcareous spicules also evolved many times convergently in different interstitial shell-less gastropod lineages  and a protective dorsal cuticle covering the body evolved within progenetic corambid sea slugs [67, 68]. “Regressive” [sensu ] traits in aplacophorans such as miniaturisation, losses of shell, tentacles, and cephalisation have been attributed to progenesis . The serial dorsoventral muscle grid of aplacophorans resembles early ontogenetic stages observed in other molluscs  and could be paedomorphic, but it is still an adaptive innovation for nonlarval stages. The narrow bipartite radulae of aplacophorans are specialised tools for microcarnivory but also resemble some stem molluscan radula types ; evidence from Cambrian fossils is more congruent with an ancestral unipartite radula .
Our topology places aplacophorans in an unconvential position; however, there is consensus among all recent molecular studies that aplacophorans represent derived rather than plesiomorphic members of Mollusca (Figure 1). These notes on the specific feature of aplacophorans therefore are of general interest to resolving the pattern and tempo of molluscan evolution, regardless of differences between our new topology and other studies.
3.9. Molluscan Ancestors
The origin of molluscs is a long-standing question, and speculations on the “hypothetical ancestral mollusk” depend on character-polarity and even topological assumptions [1, 59]. Broad genomic analyses (e.g., [14–16, 22]) recovered molluscs as an early-derived offshoot of Lophotrochozoa (Spiralia), as had been proposed on morphological grounds . Modern morphological studies suggest entoprocts as sister to molluscs , a view supported by mitochondrial genomics . MicroRNA data  suggest Annelida is the sister to Mollusca, as recovered (but never robustly supported) by most of our analyses with a large outgroup taxon set (Suppl. Figure 1A). Our analyses did not resolve a consistent sister group to Mollusca. Yet permutations and pruning of our outgroup sampling did not affect ingroup topologies. We regard the molluscan sister group as an unanswered question, but not necessarily problematic to the question of internal molluscan phylogeny (if ingroup taxon sampling is sufficiently dense).
Our initial morphological character mapping (Figure 1(c)) suggests that the last common ancestor of living molluscs (“LAM”) was a single-shelled conchiferan with a complex body, single (or few) paired shell retractors, single paired gills in a circumpedal mantle cavity, and an elaborated (cephalised) anterior body portion. There is little reason to assume that this hypothetical LAM resembled a chiton or monoplacophoran (e.g., ) or to suspect a segmented body organisation (e.g., ). Instead, the LAM may have resembled an untorted gastropod with a cap-like shell, perhaps similar to Latouchella, as assumed by morphologists before the discovery of the supposedly “living fossil” Neopilina and still advocated by some palaeontologists .
Our assessment of potential morphological apomorphies (Figure 1(c)) and the molecular clock results (Figure 3) would suggest that the Vendian (555 Ma) Kimberella  is a candidate stem-group mollusc appearing before the evolution of a dorsal shell field. The interpretation of Kimberella is controversial , but the true stem molluscs probably did have a large, bilaterally symmetrical body with subapical mouth on a snout with a likely bipartite radula , a broad ventral foot, many dorsoventral muscle bundles, and a dorsal mantle covered with a resistant dorsal cuticle with mineralised spicules, which are all molluscan features, but lacking a shell [115, 116]. During the latest Precambrian rise of predators and successive development of sediment bottoms , molluscan larvae or early juveniles may have calcified their plesiomorphic cap-shaped mantle cuticle for protective reasons. Answering Yochelson , the mollusc made a shell, but then the shell made the molluscs.
Only one (if any) of the dozens of proposed hypotheses on molluscan phylogeny reflects the true tree. Both the traditional palaeontological concept, with monoplacophorans giving rise to all other molluscan lineages, and the widely accepted morphocladistic Testaria hypothesis, with progressive evolution from vermiform molluscs to chitons and conchiferans [62, 118], are not supported by molecular evidence and are apparently incompatible with the chronological appearance of reliable fossils representing major molluscan lineages.
The Aculifera concept has been supported by phylogenomic results [2, 119], whose dichotomy is not inherently contradicted by the available fossil record if the last common molluscan ancestor was small and complex and had a shell (i.e., was conchiferan rather than chiton-like). Yet the branching patterns of living clades in available phylogenomic topologies appear to be incongruent with stratigraphic evidence. The debate on molluscan phylogeny can only be progressed using all available evidence, integrating morphological, fossil, and molecular data. To provide meaningful insights, molecular approaches must include all eight molluscan classes and cover the well-known diversity of living taxa.
Our results, despite using traditional markers that cover arguably less data than next-generation approaches, are based on a comprehensive taxon set with data quality checked exhaustively at all levels. Topologies recovered still may suffer from poor sampling especially of aplacophoran lineages and from heterogeneous evolution of ingroup clades such as cephalopods or patellogastropods. The data available, while extensive and of high quality, are small in comparison to the total genetic diversity of the phylum under study.
Nevertheless, our data sets, regimes, and analyses support and refine the Serialia hypothesis . The topological results inferred herein cannot be refuted by recent research on shell building gene expression and mollusc palaeontology. In many well-studied molluscan taxa, shells are reduced or duplicated, bodies adapted to different environments and life styles such as benthic, interstitial, or pelagic realms, and features such as mantle cavities and radulae repeatedly were transformed, often drastically and rapidly. Heterochronic processes could already have occurred in the Palaeozoic, which would be consistent with the disparity known in living molluscs but which could also obscure deeper phylogenetic signal in morphological analyses. Ultimately, such complex diversification could have led to the fossil and extant molluscs that stand apart from other (noninsect) animals in terms of species diversity, body disparity, and variation of life traits. The true reconstruction of the early radiation of molluscs still is one of the major unresolved issues in evolutionary biology. Independent molecular evidence, such as microRNAs or phylogenomic data on a similarly comprehensive and dense taxon sampling as used herein, will be needed to further test these hypotheses.
I. Stöger carried out the molecular genetic studies, performed the sequence alignments and the phylogenetic analyses, and drafted the paper. J. D. Sigwart participated in the design of the study and contributed to writing the paper; Y. Kano participated in original fieldwork and in the molecular genetic studies; T. Knebelsberger participated in the molecular genetic studies; B. A. Marshall carried out original fieldwork and helped draft the paper; E. Schwabe participated in original fieldwork and helped draft the paper; M. Schrödl conceived and designed the study, participated in original fieldwork, contributed to molecular genetic studies, and contributed to writing the paper.
Monoplacophoran material was collected during the expedition ANDEEP SYSTCO, from commercial fisheries bycatch, and by Taeko and Shoichi Kimura. Dirk Metzler (Munich) helped with molecular clocks, Patrick Kück (Bonn) performed some of the analyses with removed putative long branched molluscan classes by the help of a bioinformatic pipeline, Korbinian Trumpp provided computational support, and Gerhard Haszprunar (Munich) is thanked for critical discussions. Anonymous referees on a previous, short version of this paper greatly contributed to improve analyses and interpretations. The authors are grateful for additional comments from David Lindberg (Berkeley) and an anonymous reviewer. This study was funded by the Deep Metazoan Priority Programme of the German Research Foundation (DFG667/9-1 to MS). Further support came from the GeoBioCenter LMU and the Leibniz Computer Centre (both Munich).
- G. Haszprunar, C. Schander, and K. M. Halanych, “Relationships of higher taxa,” in Phylogeny and Evolution of the Mollusca, W. F. Ponder and D. R. Lindberg, Eds., pp. 19–32, University of California Press, Berkeley, Calif, USA, 2008.
- M. J. Telford and G. E. Budd, “Invertebrate evolution: bringing order to the molluscan chaos,” Current Biology, vol. 21, no. 23, pp. R964–R966, 2011.
- N. G. Wilson, D. Huang, M. C. Goldstein, H. Cha, G. Giribet, and G. W. Rouse, “Field collection of Laevipilina hyalina McLean, 1979 from southern California, the most accessible living monoplacophoran,” Journal of Molluscan Studies, vol. 75, no. 2, pp. 195–197, 2009.
- Y. Kano, S. Kimura, Y. Kimura, and A. Warén, “Living Monoplacophora: morphological conservatism or recent diversification?” Zoologica Scripta, vol. 41, no. 5, pp. 471–488, 2012.
- K. M. Kocot, J. T. Cannon, C. Todt et al., “Phylogenomics reveals deep molluscan relationships,” Nature, vol. 477, no. 7365, pp. 452–456, 2011.
- A. Meyer, A. Witek, and B. Lieb, “Selecting ribosomal protein genes for invertebrate phylogenetic inferences: how many genes to resolve the Mollusca?” Methods in Ecology and Evolution, vol. 2, no. 1, pp. 34–42, 2011.
- J. Vinther, E. A. Sperling, D. E. G. Briggs, and K. J. Peterson, “A molecular palaeobiological hypothesis for the origin of aplacophoran molluscs and their derivation from chiton-like ancestors,” Proceedings of the Royal Society B, vol. 279, no. 1732, pp. 1259–1268, 2012.
- S. A. Smith, N. G. Wilson, F. E. Goetz et al., “Resolving the evolutionary relationships of molluscs with phylogenomic tools,” Nature, vol. 480, no. 7377, pp. 364–367, 2011.
- G. Giribet, A. Okusu, A. R. Lindgren, S. W. Huff, M. Schrödl, and M. K. Nishiguchi, “Evidence for a clade composed of molluscs with serially repeated structures: monoplacophorans are related to chitons,” Proceedings of the National Academy of Sciences of the United States of America, vol. 103, no. 20, pp. 7723–7728, 2006.
- N. G. Wilson, G. W. Rouse, and G. Giribet, “Assessing the molluscan hypothesis Serialia (Monoplacophora + Polyplacophora) using novel molecular data,” Molecular Phylogenetics and Evolution, vol. 54, no. 1, pp. 187–193, 2010.
- C. Nielsen, G. Haszprunar, B. Ruthensteiner, and A. Wanninger, “Early development of the aplacophoran mollusc Chaetoderma,” Acta Zoologica, vol. 88, no. 3, pp. 231–247, 2007.
- J. W. Wägele, H. Letsch, A. Klussmann-Kolb, C. Mayer, B. Misof, and H. Wägele, “Phylogenetic support values are not necessarily informative: the case of the Serialia hypothesis (a mollusk phylogeny),” Frontiers in Zoology, vol. 6, no. 1, p. 12, 2009.
- A. Meyer, C. Todt, N. T. Mikkelsen, and B. Lieb, “Fast evolving 18S rRNA sequences from Solenogastres (Mollusca) resist standard PCR amplification and give new insights into mollusk substitution rate heterogeneity,” BMC Evolutionary Biology, vol. 10, no. 1, p. 70, 2010.
- H. Philippe, H. Brinkmann, D. V. Lavrov et al., “Resolving difficult phylogenetic questions: why more sequences are not enough,” PLoS Biology, vol. 9, no. 3, Article ID e1000602, 2011.
- H. Philippe, H. Brinkmann, R. R. Copley et al., “Acoelomorph flatworms are deuterostomes related to Xenoturbella,” Nature, vol. 470, no. 7333, pp. 255–260, 2011.
- K. S. Pick, H. Philippe, F. Schreiber et al., “Improved phylogenomic taxon sampling noticeably affects nonbilaterian relationships,” Molecular Biology and Evolution, vol. 27, no. 9, pp. 1983–1987, 2010.
- B. Misof and K. Misof, “A Monte Carlo approach successfully identifies randomness in multiple sequence alignments: a more objective means of data exclusion,” Systematic Biology, vol. 58, no. 1, pp. 21–34, 2009.
- R. R. Stocsits, H. Letsch, J. Hertel, B. Misof, and P. F. Stadler, “Accurate and efficient reconstruction of deep phylogenies from structured RNAs,” Nucleic Acids Research, vol. 37, no. 18, pp. 6184–6193, 2009.
- J. Mallatt, C. W. Craig, and M. J. Yoder, “Nearly complete rRNA genes assembled from across the metazoan animals: effects of more taxa, a structure-based alignment, and paired-sites evolutionary models on phylogeny reconstruction,” Molecular Phylogenetics and Evolution, vol. 55, no. 1, pp. 1–17, 2010.
- J. Paps, J. Baguñà, and M. Riutort, “Lophotrochozoa internal phylogeny: new insights from an up-to-date analysis of nuclear ribosomal genes,” Proceedings of the Royal Society B, vol. 276, no. 1660, pp. 1245–1254, 2009.
- Y. J. Passamaneck, C. Schander, and K. M. Halanych, “Investigation of molluscan phylogeny using large-subunit and small-subunit nuclear rRNA sequences,” Molecular Phylogenetics and Evolution, vol. 32, no. 1, pp. 25–38, 2004.
- C. W. Dunn, A. Hejnol, D. Q. Matus et al., “Broad phylogenomic sampling improves resolution of the animal tree of life,” Nature, vol. 452, no. 7188, pp. 745–749, 2008.
- A. Hejnol, M. Obst, A. Stamatakis et al., “Assessing the root of bilaterian animals with scalable phylogenomic methods,” Proceedings of the Royal Society B, vol. 276, no. 1677, pp. 4261–4270, 2009.
- M. R. Smith and J.-B. Caron, “Primitive soft-bodied cephalopods from the Cambrian,” Nature, vol. 465, no. 7297, pp. 469–472, 2010.
- J.-B. Caron, A. H. Scheltema, C. Schander, and D. Rudkin, “A soft-bodied mollusc with radula from the Middle Cambrian Burgess Shale,” Nature, vol. 442, no. 7099, pp. 159–163, 2006.
- J. Vinther and C. Nielsen, “The early Cambrian Halkieria is a mollusc,” Zoologica Scripta, vol. 34, no. 1, pp. 81–89, 2005.
- S. C. Morris and J.-B. Caron, “Halwaxiids and the early evolution of the lophotrochozoans,” Science, vol. 315, no. 5816, pp. 1255–1258, 2007.
- A. Stamatakis, “RAxML-VI-HPC: maximum likelihood-based phylogenetic analyses with thousands of taxa and mixed models,” Bioinformatics, vol. 22, no. 21, pp. 2688–2690, 2006.
- S. F. Altschul, W. Gish, W. Miller, E. W. Myers, and D. J. Lipman, “Basic local alignment search tool,” Journal of Molecular Biology, vol. 215, no. 3, pp. 403–410, 1990.
- K. Katoh, G. Asimenos, and H. Toh, “Multiple alignment of DNA sequences with MAFFT,” Methods in Molecular Biology, vol. 537, pp. 39–64, 2009.
- P. Kück, K. Meusemann, J. Dambach et al., “Parametric and non-parametric masking of randomness in sequence alignments can be improved and leads to better resolved trees,” Frontiers in Zoology, vol. 7, p. 10, 2010.
- K. Tamura, D. Peterson, N. Peterson, G. Stecher, M. Nei, and S. Kumar, “MEGA5: molecular evolutionary genetics analysis using maximum likelihood, evolutionary distance, and maximum parsimony methods,” Molecular Biology and Evolution, vol. 28, no. 10, pp. 2731–2739, 2011.
- P. Kück and K. Meusemann, FASconCAT, Version 1. 0. Zool, Forschungsmuseum A. Koenig, Bonn, Germany, 2010.
- A. J. Drummond and A. Rambaut, “BEAST: bayesian evolutionary analysis by sampling trees,” BMC Evolutionary Biology, vol. 7, no. 1, pp. 754–755, 2007.
- J. Castresana, “Selection of conserved blocks from multiple alignments for their use in phylogenetic analysis,” Molecular Biology and Evolution, vol. 17, no. 4, pp. 540–552, 2000.
- G. Jobb, A. Von Haeseler, and K. Strimmer, “TREEFINDER: a powerful graphical analysis environment for molecular phylogenetics,” BMC Evolutionary Biology, vol. 4, p. 18, 2004.
- X. Xia and Z. Xie, “DAMBE: software package for data analysis in molecular biology and evolution,” Journal of Heredity, vol. 92, no. 4, pp. 371–373, 2001.
- D. Posada and K. A. Crandall, “MODELTEST: testing the model of DNA substitution,” Bioinformatics, vol. 14, no. 9, pp. 817–818, 1998.
- J. A. A. Nylander, MrModeltest V2. 3. Program Distributed by the Author, Evolutionary Biology Centre, Uppsala University, Uppsala, Sweden, 2008.
- D. L. Swofford, PAUP. Phylogenetic Analysis Using Parsimony (and Other Methods). Version 4, Sinauer Associates, Sunderland, Mass, USA, 2003.
- F. Abascal, R. Zardoya, and D. Posada, “ProtTest: selection of best-fit models of protein evolution,” Bioinformatics, vol. 21, no. 9, pp. 2104–2105, 2005.
- A. Stamatakis, The RAxML 7.0.4 Manual. Department of Computer Science, Ludwig-Maximilian-Universität München, Germany.
- J. P. Huelsenbeck and F. Ronquist, “MRBAYES: bayesian inference of phylogenetic trees,” Bioinformatics, vol. 17, no. 8, pp. 754–755, 2001.
- A. Rambaut and A. J. Drummond, “Tracer v1. 4,” 2007, http://tree.bio.ed.ac.uk/software/tracer/.
- A. J. Drummond, S. Y. W. Ho, M. J. Phillips, and A. Rambaut, “Relaxed phylogenetics and dating with confidence,” PLoS Biology, vol. 4, no. 5, p. e88, 2006.
- A. J. Drummond, S. Y. W. Ho, N. Rawlence, and A. Rambaut, A Rough Guide to BEAST 1.4, 2007.
- K. M. Jörger, I. Stöger, Y. Kano, H. Fukuda, T. Knebelsberger, and M. Schrödl, “On the origin of Acochlidia and other enigmatic euthyneuran gastropods, with implications for the systematics of Heterobranchia,” BMC Evolutionary Biology, vol. 10, no. 1, p. 323, 2010.
- C. A. Hipsley, L. Himmelmann, D. Metzler, and J. Müller, “Integration of bayesian molecular clock methods and fossil-based soft bounds reveals early cenozoic origin of African lacertid lizards,” BMC Evolutionary Biology, vol. 9, no. 1, p. 151, 2009.
- J. W. Wägele and C. Mayer, “Visualizing differences in phylogenetic information content of alignments and distinction of three classes of long-branch effects,” BMC Evolutionary Biology, vol. 7, p. 147, 2007.
- T. Furuhashi, C. Schwarzinger, I. Miksik, M. Smrz, and A. Beran, “Molluscan shell evolution with review of shell calcification hypothesis,” Comparative Biochemistry and Physiology B, vol. 154, no. 3, pp. 351–371, 2009.
- T. R. Waller, “Origin of the molluscan class Bivalvia and a phylogeny of major groups,” in Bivalves: An Eon of Evolution, P. A. Johnston and J. W. Haggard, Eds., pp. 1–45, University of Calgary Press, Calgary, Canada, 1998.
- G. Steiner and H. Dreyer, “Molecular phylogeny of Scaphopoda (Mollusca) inferred from 18s rDNA sequences: support for a Scaphopoda-Cephalopoda clade,” Zoologica Scripta, vol. 32, no. 4, pp. 343–356, 2003.
- W. F. Ponder and D. R. Lindberg, Phylogeny and Evolution of the Mollusca, University of California Press, Berkeley, Calif, USA, 2008.
- P. C. E. Donoghue and M. J. Benton, “Rocks and clocks: calibrating the Tree of Life using fossils and molecules,” Trends in Ecology and Evolution, vol. 22, no. 8, pp. 424–431, 2007.
- E. Mossel and M. Steel, “How much can evolved characters tell us about the tree that generated them?” in Mathematics of Evolution and Phylogeny, O. Gascuel, Ed., pp. 384–412, Oxford University Press, Oxford, UK, 2005.
- A. H. Scheltema, K. Kerth, and A. M. Kuzirian, “Original molluscan radula: comparisons among Aplacophora, Polyplacophora, Gastropoda, and the Cambrian fossil Wiwaxia corrugata,” Journal of Morphology, vol. 257, no. 2, pp. 219–244, 2003.
- S. Shigeno, T. Sasaki, and G. Haszprunar, “Central nervous system of Chaetoderma japonicum (Caudofoveata, Aplacophora): implications for diversified ganglionic plans in early molluscan evolution,” Biological Bulletin, vol. 213, no. 2, pp. 122–134, 2007.
- K. Lundin, C. Schander, and C. Todt, “Ultrastructure of epidermal cilia and ciliary rootlets in Scaphopoda,” Journal of Molluscan Studies, vol. 75, no. 1, pp. 69–73, 2009.
- D. R. Lindberg and M. T. Ghiselin :, “Fact, theory and tradition in the study of molluscan origins,” Proceedings of the California Academy of Sciences, vol. 54, pp. 663–686, 2003.
- L. Prendini, “Species or supraspecific taxa as terminals in Cladistic analysis? groundplans versus exemplars revisited,” Systematic Biology, vol. 50, no. 2, pp. 290–300, 2001.
- G. Haszprunar, “Is the Aplacophora monophyletic? A cladistic point of view,” American Malacological Bulletin, vol. 15, no. 2, pp. 115–130, 2000.
- G. Haszprunar and A. Wanninger, “Molluscs,” Current Biology, vol. 22, no. 13, pp. R510–R514, 2012.
- L. Salvini-Plawen and G. Steiner, “Synapomorphies and plesiomorphies in higher classification of Mollusca,” in Origin and Evolutionary Radiation of the Mollusca, J. Taylor, Ed., pp. 29–51, Oxford University Press, Oxford, UK, 1996.
- A. H. Scheltema, “Phylogenetic position of Sipuncula, Mollusca and the progenetic Aplacophora,” in Origin and Evolutionary Radiation of the Mollusca, J. Taylor, Ed., pp. 53–58, Oxford University Press, Oxford, UK, 1996.
- M. Schrödl, K. M. Jörger, A. Klussmann-Kolb, and N. G. Wilson, “Bye bye “Opisthobranchia”! a review on the contribution of mesopsammic sea slugs to euthyneuran systematics,” Thalassas, vol. 27, no. 2, pp. 101–112, 2011.
- M. Schrödl, K. M. Jörger, and N. G. Wilson, “A reply to Medina et al. (2011): crawling through time: transition of snails to slugs dating back to the Paleozoic based on mitochondrial phylogenomics,” Marine Genomics, vol. 4, no. 4, pp. 301–303, 2011.
- A. Martynov, B. Brenzinger, Y. Hooker, and M. Schrödl, “3D-anatomy of a new tropical Peruvian nudibranch gastropod species, Corambe mancorensis, and novel hypotheses on dorid gill ontogeny and evolution,” Journal of Molluscan Studies, vol. 77, no. 2, pp. 129–141, 2011.
- A. Martynov and M. Schrödl, “Phylogeny and evolution of corambid nudibranchs (Mollusca: Gastropoda),” Zoological Journal of the Linnean Society, vol. 163, no. 2, pp. 585–604, 2011.
- M. Schrödl and T. P. Neusser, “Towards a phylogeny and evolution of Acochlidia (Mollusca: Gastropoda: Opisthobranchia),” Zoological Journal of the Linnean Society, vol. 158, no. 1, pp. 124–154, 2010.
- P. Y. Parkhaev, “The early molluscan radiation,” in Phylogeny and Evolution of the Mollusca, W. F. Ponder and D. R. Lindberg, Eds., pp. 33–69, University of California Press, Berkeley, Calif, USA, 2008.
- A. G. Smith, “Amphineura,” in Treatise on Invertebrate Palaeontology, Part 1: Mollusca 1, R. C. Moore, Ed., pp. 141–176, Geological Society of America, New York, NY, USA, 1960.
- W. Yu, “Yangtze micromolluscan fauna in Yangtze region of China with notes on Precambrian-Cambrian boundary,” in Stratigraphy and Palaeontology Boundary in China Precambrian-Cambrian Boundary, vol. 1, pp. 19–275, Nanjing Institute of Geology and Palaeontology Academia Sinica, Nanjing University, Jiangsu, China, 1987.
- D. R. Lindberg, “Monoplacophorans and the origin and relationships of mollusks,” Evolution, vol. 2, no. 2, pp. 191–203, 2009.
- J. Pojeta Jr., “Cambrian Pelecypoda (Mollusca),” American Malacological Bulletin, vol. 15, no. 2, pp. 157–166, 2000.
- J. D. Sigwart and M. D. Sutton, “Deep molluscan phylogeny: synthesis of palaeontological and neontological data,” Proceedings of the Royal Society B, vol. 274, no. 1624, pp. 2413–2419, 2007.
- M. D. Sutton and J. D. Sigwart, “A chiton without a foot,” Palaeontology, vol. 55, no. 2, pp. 401–411, 2012.
- M. D. Sutton, D. E. G. Briggs, D. J. Siveter, D. J. Siveter, and J. D. Sigwart, “A Silurian armoured aplacophoran and implications for molluscan phylogeny,” Nature, vol. 490, pp. 94–97, 2012.
- M. A. Fedonkin and B. M. Waggoner, “The late Precambrian fossil Kimberella is a mollusc-like bilaterian organism,” Nature, vol. 388, no. 6645, pp. 868–871, 1997.
- G. D. Edgecombe, G. Giribet, C. W. Dunn et al., “Higher-level metazoan relationships: recent progress and remaining questions,” Organisms Diversity and Evolution, vol. 11, no. 2, pp. 151–172, 2011.
- B. Runnegar and J. Pojeta Jr., “Molluscan phylogeny: the paleontological viewpoint,” Science, vol. 186, no. 4161, pp. 311–317, 1974.
- E. L. Yochelson, “An alternative approach to the interpretation of the phylogeny of ancient molluscs,” Malacologia, vol. 17, pp. 185–191, 1978.
- J. A. Harper and H. B. Rollins, “The bellerophont controversy revisited,” American Malacological Bulletin, vol. 15, no. 2, pp. 147–156, 2000.
- J. Dzik, “Evolution of “small shelly fossils” assemblages of the early Paleozoic,” Acta Palaeontologica Polonica, vol. 39, no. 3, pp. 247–313, 1994.
- W. Yu, “On merismoconchids,” Acta Oceanologica Sinica, vol. 23, pp. 432–446, 1983.
- A. P. Gubanov and J. S. Peel, “Cambrian monoplacophoran molluscs (Class Helcionelloida),” American Malacological Bulletin, vol. 15, no. 2, pp. 139–145, 2000.
- E. L. Yochelson and C. H. Holland, “Dentalium saturni Goldfuss, 1841 (Eifelian: Mollusca): complex issues from a simple fossil,” Paläontologische Zeitschrift, vol. 78, no. 1, pp. 97–102, 2004.
- J. S. Peel, “Pinnocaris and the origin of scaphopods,” Acta Palaeontologica Polonica, vol. 49, no. 4, pp. 543–550, 2004.
- E. Yochelson, R. H. Flower, and G. F. Webers, “The bearing of new Late Cambrian monoplacophoran genus Knightoconus upon the origin of Cephalopoda,” Lethaia, vol. 6, no. 3, pp. 275–309, 1973.
- G. F. Webers and E. L. Yochelson, “Carboniferous Scaphopoda (Mollusca) and non-scaphopods from Scotland,” Scottish Journal of Geology, vol. 47, no. 1, pp. 67–79, 2011.
- J. Dzik, “Brachiopod identity of the alleged monoplacophoran ancestors of cephalopods,” Malacologia, vol. 52, no. 1, pp. 97–113, 2010.
- B. Kröger, J. Vinther, and D. Fuchs, “Cephalopod origin and evolution: a congruent picture emerging from fossils, development and molecules: extant cephalopods are younger than previously realised and were under major selection to become agile, shell-less predators,” BioEssays, vol. 33, no. 8, pp. 602–613, 2011.
- D. Mazurek and M. Zatoń, “Is Nectocaris pteryx a cephalopod?” Lethaia, vol. 44, no. 1, pp. 2–4, 2011.
- J.-Y. Chen, D.-Y. Huang, and D. J. Bottjer, “An Early Cambrian problematic fossil: Vetustovermis and its possible affinities,” Proceedings of the Royal Society B, vol. 272, no. 1576, pp. 2003–2007, 2005.
- M. R. Smith and J.-B. Caron, “Nectocaris and early cephalopod evolution: reply to Mazurek & Zatoń,” Lethaia, vol. 44, no. 4, pp. 369–372, 2011.
- L. Salvini-Plawen, The Significance of the Placophora for Molluscan Phylogeny, vol. 65, Venus, Elko, Nev, USA, 2006.
- K. G. Wingstrand, “On the anatomy and relationships of recent Monoplacophora,” Galathea Report, vol. 16, pp. 7–94, 1985.
- G. Giribet, “Bivalvia,” in Phylogeny and Evolution of the Mollusca, W. F. Ponder and D. R. Lindberg, Eds., pp. 105–141, University of California Press, Berkeley, Calif, USA, 2008.
- S. W. Aktipis and G. Giribet, “A phylogeny of Vetigastropoda and other “archaeogastropods”: re-organizing old gastropod clades,” Invertebrate Biology, vol. 129, no. 3, pp. 220–240, 2010.
- S. W. Aktipis and G. Giribet, “Testing relationships among the vetigastropod taxa: a molecular approach,” Journal of Molluscan Studies, vol. 78, no. 1, pp. 12–27, 2012.
- G. Haszprunar, “Monoplacophora (Tryblidia),” in Phylogeny and Evolution of the Mollusca, W. F. Ponder and D. R. Lindberg, Eds., pp. 97–104, University of California Press, Berkeley, Calif, USA, 2008.
- L. R. L. Simone, “Comparative morphology among representatives of main taxa of Scaphopoda and basal protobranch Bivalvia (Mollusca),” Papeis Avulsos de Zoologia, vol. 49, no. 32, pp. 405–457, 2009.
- J. Pojeta and B. Runnegar, “The paleontology of rostroconch mollusks and the early history of the phylum Mollusca,” U.S. Geological Survey Professional Paper, vol. 986, pp. 1–88, 1976.
- A. Wanninger and G. Haszprunar, “The expression of an engrailed protein during embryonic shell formation of the tusk-shell, Antalis entalis (Mollusca, Scaphopoda),” Evolution and Development, vol. 3, no. 5, pp. 312–321, 2001.
- S.-I. Yokobori, T. Iseto, S. Asakawa et al., “Complete nucleotide sequences of mitochondrial genomes of two solitary entoprocts, Loxocorone allax and Loxosomella aloxiata: implications for lophotrochozoan phylogeny,” Molecular Phylogenetics and Evolution, vol. 47, no. 2, pp. 612–628, 2008.
- I. Stöger and M. Schrödl, “Mitogenomics does not resolve deep molluscan relationships (yet?),” Molecular Phylogenetics and Evolution, vol. 69, no. 2, pp. 376–392, 2013.
- S. Faller, B. H. Rothe, C. Todt, A. Schmidt-Rhaesa, and R. Loesel, “Comparative neuroanatomy of Caudofoveata, Solenogastres, Polyplacophora, and Scaphopoda (Mollusca) and its phylogenetic implications,” Zoomorphology, pp. 1–22, 2012.
- M. P. Pelseneer, “Sur le quatrième orifice palléal des Pélécypodes,” Comptes Rendus Hebdonnaires des Séances de l’Académie des Sciences, vol. 110, pp. 154–156, 1890.
- A. Wanninger and G. Haszprunar, “Chiton myogenesis: perspectives for the development and evolution of larval and adult muscle systems in molluscs,” Journal of Morphology, vol. 251, no. 2, pp. 103–113, 2002.
- M. R. Smith, “Mouthparts of the Burgess Shale fossils Odontogriphus and Wiwaxia: implications for the ancestral molluscan radula,” Proceedings of the Royal Society B, vol. 279, no. 1745, pp. 4287–4295, 2012.
- L. Salvini-Plawen, Origin, Phylogeny and Classification of the Phylum Mollusca, vol. 9, Iberus, Madrid, Spain, 1990.
- B. M. Wheeler, A. M. Heimberg, V. N. Moy et al., “The deep evolution of metazoan microRNAs,” Evolution and Development, vol. 11, no. 1, pp. 50–68, 2009.
- R. D. Hoare, “Considerations on Paleozoic Polyplacophora including the description of Plasiochiton curiosus n. gen. and sp.,” American Malacological Bulletin, vol. 15, no. 2, pp. 131–137, 2000.
- A. Y. Ivantsov, “Paleontological evidence for the supposed Precambrian occurrence of mollusks,” Paleontological Journal, vol. 44, no. 12, pp. 1552–1559, 2010.
- A. Seilacher and J. W. Hagadorn, “Early molluscan evolution: evidence from the trace fossil record,” Palaios, vol. 25, no. 9, pp. 565–575, 2010.
- M. A. Fedonkin, A. Simonetta, and A. Y. Ivantsov, “New data on Kimberella, the Vendian mollusc-like organism (White Sea region, Russia): palaeoecological and evolutionary implications,” Geological Society Special Publication, no. 286, pp. 157–179, 2007.
- A. Y. Ivantsov, “New reconstruction of Kimberella, problematic Vendian metazoan,” Paleontological Journal, vol. 43, no. 6, pp. 601–611, 2009.
- E. L. Yochelson, “Concerning the concept of extinct classes of Mollusca: or what may/may not be a class of mollusks,” American Malacological Bulletin, vol. 15, no. 2, pp. 195–202, 2000.
- G. Haszprunar and B. Ruthensteiner, “Monoplacophora (Tryblidia)-some unanswered questions,” American Malacological Bulletin, vol. 31, no. 1, pp. 189–194, 2013.
- K. Kocot, “Recent advances and unanswered questions in deep molluscan phylogenetics,” American Malacological Bulletin, vol. 31, no. 1, pp. 195–208, 2013.