We present evidence that the single representative of the crustacean order Amphionidacea is a decapod shrimp and not a distinct order. After reviewing available morphological evidence, it is concluded that Amphionides is a larval form, but with an as yet unknown parentage. Although the most likely adult form is in the family Pandalidae, the limited molecular data available cannot fully resolve its affinity. We therefore propose to treat Amphionides reynaudii as incertae sedis within Caridea, rather than a separate family. In view of the large scale, tropical and subtropical distribution of the taxon, the possibility is discussed that Amphionides is more likely to be a composite taxon at generic level, rather than larvae of a single shrimp species.
In the traditional classification scheme of crustaceans1, the crustacean superorder Eucarida comprises three orders, Euphausiacea, Amphionidacea and Decapoda, although the relationship of euphausiids to decapods remains unclear2. Amphionides, the sole genus in the order Amphionidacea is typically planktonic, and found in all subtropical-tropical oceans3, with presumed larval specimens usually collected at depths less than 100 m, whilst metamorphosed specimens are mostly found below 700 m. Historically, four larval nominal taxa were recognised in the genus, as well as an additional metamorphosed nominal taxon. However, these have all been considered to be synonyms of each other since 19694, and currently only one species is recognised in the order. The majority of specimens were collected during major historical oceanographic expeditions, such as the Dana expedition4 and the International Indian Ocean Expedition5, with very few specimens recorded since 19733. Most specimens are rather damaged (Fig. 1), with no supposed intact adult specimen ever collected.
The order Amphionidacea was erected in 19735 and is currently assumed to consist of only a single species, Amphionides reynaudii (H. Milne Edwards, 1833), but a separate ordinal status has been controversial for many decades. Although large-scale compilations and summaries of crustacean systematics have followed Williamson’s concept1,3,6,7, Richter & Scholtz2 mentioned briefly that the order should be included in the Decapoda, a view shared by many of the earlier crustacean workers. Koeppel in 1902 saw affinities with larvae of the Sergestidae8, whilst even earlier in 1888 Spence Bate9 considered it closely related to the larval genus Eretmocaris (now considered to be the larvae of the caridean genus Lysmata). Gurney, who was an expert in the morphology of larval Decapoda, considered the genus to be clearly based within Caridea10 and in 1942 placed the genus in its own family, Amphionidae (recte Amphionididae)11. Based on an exhaustive study of the Dana expedition material Heegaard4, whilst maintaining the family, placed it as the sole member of the sub-tribe Amphionidea within the tribe Caridea, although indicating that it may well constitute a tribe on its own.
Despite the interesting morphology of the group, the position of Amphionides has only been scrutinised three times within an analytical framework; all have been based on morphology as to date no material suitable for genetics has come to light. In an early cladistic analysis of Eucarida, Amphionidacea was resolved as the sister-group to Decapoda12, a relationship that was resolved also in an expanded analysis of Malacostraca2. However, the latter study in a summary of evolutionary relationships suggested that ‘the Decapoda should also comprise the Amphionidacea’. In a more recent, exhaustive analysis of recent and fossil Arthropoda, the same sister-relationship was recovered13.
Recently freshly-collected material of A. reynaudii from the Canary Islands (Atlantic Ocean) has become available, and we are now able to elucidate the phylogenetic position of the taxon on the basis of four molecular markers. DNA analysis has in recent years proved to be a powerful tool for linking enigmatic larval or planktonic forms to adult taxa, especially in decapod species with unknown larval taxa, an area where morphology often fails to correctly link both taxa. For example, the enigmatic deep-sea taxon, Galatheacaris abyssalis (previously placed in its own family and superfamily within Caridea14) represents the decapodid stage of Eugonatonotus chacei15. In a similar way, phylogenetics demonstrated that the armoured, pelagic taxon, Cerataspis monstrosa is a larval form of the wide-spread dendrobranchiate shrimp, Plesiopenaeus armatus16.
The final four- and two-marker datasets comprise 59 species each with 3884 bp and 205 species each with 2234 bp, respectively (Supplementary Figure S1 and Supplementary Table S2). A total of 95 species and 190 gene sequences (excluding A. reynaudii) are added to an existing two-marker dataset17. The optimal models for 16 S and 18 S alignments of the two-marker dataset assessed are all with gamma-distributed (G) and invariant sites (I). Tree topologies from ML and BI analyses are generally similar and the BI phylogram is presented to show the phylogenetic relationship of A. reynaudii in both the four- and two-marker results (Figs. 2 and 3).
Using Euphausiacea and Stomatopoda as non-decapod outgroups and including all the suborders and infraorders of decapods, as well as 19 species of carideans from nine families, the four-gene phylogenetic tree (Fig. 2) reveals that Amphionides is nested inside the carideans and sister to Pandalus montagui of the family Pandalidae (Pp = 1.0, MLb = 99), The nodal support for the major groups of decapod crustaceans is generally strong and similar to a previous analysis18. The result of the AU test rejects the hypothesis that A. reynaudii does not belong to Caridea (P = 0.027).
The two-marker analysis including 190 species of carideans in 29 families (out of 35 currently recognised) has the most comprehensive species level taxon coverage for carideans to date. This phylogenetic tree (Fig. 3, Supplementary Table S2) demonstrates that A. reynaudii is nested within Pandalidae, but with moderate support from ML (Pp = 1.0, MLb = 57). Although A. reynaudii is sister to the genus Heterocarpus (with three species in the present analysis), the support is not very strong (Pp = 1.0, MLb ≤ 50). Result of the AU test shows that the hypothesis that A. reynaudii does not belong to Pandalidae cannot be rejected (P = 0.145). The relationships among the various families of Caridea in our current analysis are similar to previous studies17,19 and demonstrate para- and polyphyly of certain families (e.g. Pasiphaeidae, Palaemonidae).
Our results demonstrate strongly that Amphionides reynaudii is a decapod (Fig. 2), and more specifically a caridean shrimp, and find no support for separate order status despite being considered a sister group to Decapoda on the basis of morphology2,12. In line with this result, we thus formally invalidate the order Amphionidacea Williamson, 1973. Accurately placing the taxon within Caridea is more problematic. Although the alignment suggests a close affinity to Pandalidae, the result of the AU test (p = 0.145) does not confirm the taxon as unambiguously within Pandalidae, although they are likely to be closely related. A potential close relationship between Amphionides and Pandalidae has already been suggested, primarily based on the morphology of younger larvae4.
The recovered placement of Amphionides as a caridean shrimp raises several questions. Only three adult males have ever been found5, although these are two specimens originally deemed female10,20 and a single early postlarval specimen (named postlarva I)4. All three were re-assigned as males5 based on the perceived advanced development of the testis and vasa differentia compared to earlier zoeal stages. Williamson5 further remarked that if they would not be sexually mature they then would indeed be decapodids (i.e. a late larval stage). However, sexually mature males in Caridea are characterised by the presence of an appendix masculina on the second pleopod21, with only two known exceptions, the genera Synalpheus (Alpheidae) and Janicella (Oplophoridae). According to Williamson5, sexual differentiation in Amphionides starts in zoeal stage IX, and two distinct morphotypes are present after this stage, based on the thickness of the antennular segment and flagellar length, with no distinction made on the basis of the second pleopod. In none of the specimens so far illustrated in the literature4,5,10,20,22 is an appendix masculina visible, nor is it discussed in the text. It further appears that no author has ever seen a fully intact adult female, with the well-known illustration in Williamson5 being a composite of 43 damaged specimens, considered to be female. Kutschera et al.22, on the basis of the developmental stages in Williamson5, did assume that one specimen in their study was male and one female, but made no comment on sexual maturity. It thus appears that the vast majority of reported specimens are larvae, with the purported sexually mature specimens based on somewhat dubiously interpreted internal characters. Gurney10 suggested that the observed testis and ovaries in previous studies were instead the posterior diverticula of the stomach. The lack of an appendix masculina in purported adult males, a near universal characteristic of Caridea, provides ample credence that no real adults have ever been found of Amphionides. Although an outside possibility remains that Amphionides is a neotenic form, on balance the available evidence overwhelmingly suggests that Amphionides is a larval form, not yet linked to a known adult form. Exotic larval morphologies abound in the Decapoda, for instance phyllosoma larvae, and a plethora of nominal taxa of larval forms not yet linked to adult taxa is known within Caridea23. In recent years, some of these forms have been linked to adult genera, either on the basis of direct rearing or molecular evidence. For instance, Eretmocaris was shown to be the zoeal stage of Lysmata based on laboratory rearing24, whilst COI data conclusively showed Galatheacaris to be the decapodid stage of Eugonatonotus15 and Icotopus to be the late larvae of Plesionika25.
On the hypothesis that Amphionides is a larval stage, a question is opened about the conspecificity of all specimens noted to date. At present, A. reynaudii is thought to occur in the Atlantic, Pacific and Indian Oceans4,5, although considered to be much more abundant in the Atlantic Ocean4. Nevertheless, early larval stages of Amphionides are rare among the material from both plankton and micronekton surveys around the Canary Islands and Cape Verde26,27, and no specimens were encountered in an analysis of the crustacean larval community based on extensive plankton samples collected in oceanic and coastal waters off the Canary Islands-African transition zone28.
Few caridean species exhibit such a broad distribution as Amphionides, although examples do exist in the Oplophoridae (e.g. Acanthephyra eximia), Pasiphaeidae (e.g. Eupasiphaea gilesii, Glyphus marsupialis), Palaemonidae (e.g. Brachycarpus biunguiculatus, Gnathophyllum americanum) and Pandalidae (e.g. Chlorotocus crassicornis, Plesionika williamsi, Stylopandalus richardi). At a generic level such a wide distribution is much more common, especially in deep water and/or pelagic taxa, in families like Pasiphaeidae, Acanthephyridae, Oplophoridae and Pandalidae. There is thus a possibility that the nominal taxa (originally described from different geographic regions) and currently considered to be synonyms of A. reynaudii, are perhaps larval stages of congeneric species, rather than conspecific. For instance, Amphion reynaudii H. Milne Edwards, 1832 was described from “les mers d’Asie”, whilst Amphion provocatoris Spence Bate, 1888 has “south of the Azores” as its type locality, approximately the area from which the present specimens were collected.
The possibility remains, however, that Amphionides reynaudii as presently understood is the larval phase of a single species. Records of the depth distribution of the taxon are somewhat conflicting, but in general it is known that earlier larval stages are present from the surface down to 30–100 m, with later stages primarily known from 700–1700 m4,5. However, the present records also demonstrate that later stages can occur in shallower water. A bathymetric range down to 2000–5000 m has been postulated4 and it has been suggested that the taxon undergoes diel vertical migration (DVM) towards the surface4. Decapod crustaceans are indeed a dominant component of the mesopelagic community occurring at those depths and undergoing DVM, with Oplophoridae, Pasiphaeidae and Pandalidae being prominent29.
Our molecular data point strongly towards Amphionides being allied with if not part of Pandalidae, to the exclusion of many families analysed (Fig. 3). Six currently recognised caridean families were not included in the present analysis, namely Bresiliidae, Bythocarididae, Campylonotidae, Merguiidae, Physetocarididae and Pseudochelidae. All of these are unlikely to be allied to Amphionides, in view of their restricted ecology (e.g. Merguia, the sole genus in Merguiidae is a tropical mangrove inhabitant), biogeography (e.g. Campylonotus, the sole genus in Campylonotidae is sub-Antarctic) or indeed have known larval stages (e.g. Physetocaris). Our analysis does recover Crangonidae as a sister group to Pandalidae, with morphological similarities between early larval stages of that family and Amphionides already noted22. On the whole, however, later stages of crangonid larvae are rather conservative across the family and show no similarity to Amphionides. Several molecular analyses place Pandalidae in a larger clade17,19, somewhat similar in composition to the one recovered herein, and consistently featuring Hippolytidae sensu lato, now split into several families30. Although larval morphologies for most families of carideans appear rather conservative, hippolytoids are an exception and show a wide diversity of larval forms, even though molecular evidence is not supportive of a close link between hippolytoids and Amphionides.
In relation to the hypothesis that Amphionides is indeed a larval pseudo-taxon, and not a neotenic one (in the absence of secondary sexual characteristics), the question as to which known caridean taxon is the adult form remains open, largely caused by the limited molecular data in Caridea as a whole, and particularly within the family Pandalidae, to which Amphionides is allied. The current analysis for example, only has representatives of three pandalid genera included, out of a total of 23 genera23. Within the area from which the present specimen was taken (the Canary Islands), several genera and species of Pandalidae occur31, be it benthic or pelagic, shallow or deeper water. For many of these genera, the larvae are tolerably well known28 and show no morphological similarity to Amphionides. However, two genera, Bitias and Pantomus, have unknown larval morphologies and potentially could be candidates to be the adult form of Amphionides although neither taxon exhibits the global distribution of Amphionides (at species or generic level) adding further to the puzzle.
On the basis of the above line of argumentation and in view of the inconclusive molecular data, we therefore elect to treat Amphionides reynaudii as incertae sedis within Caridea, pending further resolution. The genus has previously been placed in its own family within the Caridea, namely Amphionididae11, but this family could alternatively be added to the list of valid families in Caridea, which would effectively then make Amphionides a neotenic, planktonic form. However, making such a profound change to higher level systematics in Caridea appears premature, given the general unsettled relationships of caridean families and status as incertae sedis is considered to be a more elegant solution given the currently available data.
Six specimens of Amphionides reynaudii were collected north of Gran Canaria, NE Atlantic (28°31′N, 15°22’W) on the 1st April 2011. All six specimens were collected in the same trawl (Matsuda Oozeki Hu net, MOHT, 5 m2 net mouth, 4 mm mesh size). The trawl was taken one hour after the nocturnal ascent of the acoustic scattering layer from 150 m depth to the surface, with a towing speed of 3–4 knots29. All six specimens are larvae. Using the latest staging scheme22, two specimens (length of cephalothoracic shield (CtsL) at least 10.5 mm, anterior carapace detached; CtsL 12.5 mm, abdominal somite IV and telson missing) belong to stage 9 (thoracopod VIII present and all pleopods present), three specimens (CtsL 10.1, 11.2, 13.6 mm) belong to stage 8 (thoracopod VII present but thoracopod VIII absent, all pleopods present), and one specimen (CtsL 7.0 mm, without abdomen) belongs to stage 4 (thoracopod V moderately long). Specimens are deposited in the collection of the National Taiwan Ocean University (NTOU M01871, M01872).
Of the six Amphionides larvae obtained, the largest specimen (CtsL 13.6 mm, NTOU M01872, Fig. 1) was used for DNA analysis (GenBank accession nos. KT699039-KT699042). Total genomic DNA was extracted from the abdominal muscles using QIAGEN® DNeasy Blood and Tissue Kit (Cat. No. 69504, Valencia, CA) following the protocol of the manufacturer. Universal primer sets were used to amplify partial sequences of the targeted genes by polymerase chain reaction (PCR): 16 S rRNA (16Sar/16Sbr, ~500 bp32), 18 S rRNA (18SA/18SL, 18SC/18SY, 18SB/18SO, ~1900 bp17), 28 S rRNA (28 S Rd1.2a/28 S Rd4.2b, 28 S A/28 S B, 28 S Rd4.5a/28 S 6.2b, ~1800 bp33) and H3 (H3AF/H3AR, ~330 bp34). All amplifications were performed in 25 μL reactions with 50–250 ng of the DNA templates using TaKaRa TagTM kit, included 2.5 μL of 10 x polymerase buffer (Mg2+plus), 0.5 μL of 2.5 mM of deoxyribonucleotide mixture (dNTPs) and 0.5 U of Taq polymerase (5 U/μL) and additional 10–25 mM magnesium chloride (MgCl2) (depending on gene). Finally 0.5 μL of 10 μM for each primer (MISSION BIOTECH, Taipei, Taiwan) were added and supplemented with sterile double-distilled water (ddH2O) to a total volume of 25 μL volume. PCR cycling conditions were as follows: 5 min at 95 °C for first denaturation, then 40 cycles of 30 sec at 94 °C, 40 sec at 46–52 °C (depending on genes) and 40 sec at 72 °C, with final extension for 10 min at 72 °C. PCR products of correct size and quality checked by 1% agarose gel were sent to a commercial company (MISSION BIOTECH) for sequencing. The same PCR primer sets were also employed for sequencing on an ABI 3730 Genetic Analyzer (Applied Biosystems, Center for Integrated BioSystems, Logan, UT, USA). SeqMan ProTM (LASERGENE®; DNASTAR, Madison, WI, USA) was used to clean and edit the sequences for contig assembly.
The phylogenetic relationship of Amphionides was elucidated by incorporating the sequences into a published 16 S, 18 S, 28 S and H3 dataset18, to which the infraorder Glypheidea was added (Laurentaeglyphea neocaledonica, GenBank accession nos. HQ241517, HQ241528, HQ241562, KT699043). The latest overall classification scheme of Decapoda was followed35, with family level systematics within Caridea updated23,29,36,37.
To resolve the phylogenetic position of Amphionides in relation to Caridea, sequence data were analysed along with a comprehensive caridean 16 S and 18 S dataset17, but only including taxa with both markers. Additional caridean species with sequence data of both 16 S and 18 S sequences available from GenBank were also incorporated in the analysis. Included as outgroups in the analysis were representatives of all suborders and infraorders of Decapoda35, but are not shown on the tree in Supplementary Figure S1.
Sequences were aligned with MAFFT v.738. GBlocks v.0.91b website server (http://molevol.cmima.csic.es/castresana/Gblocks_server.html)39 was used to remove divergent regions and poorly aligned positions in the DNA datasets. After elimination of highly divergent regions, each gene alignment for the four-gene dataset was trimmed to 406 bp of 16 S rRNA, 1675 bp of 18 S rRNA, 1477 bp of 28 S rRNA and 326 bp of H3. In the two-gene dataset, the 16 S and 18 S sequences were trimmed to 466 bp and 1768 bp, respectively. These alignments were then concatenated into the four-gene and two-gene datasets. The best model of DNA substitution and parameters for individual alignment (16 S and 18 S) of the two-gene dataset was determined by jModelTest v.2.1.340 based on Akaike’s criterion (AIC). Two analytical methods were employed to construct the phylogenetic trees: maximum likelihood (ML) using RAxML v.7.2.6 (Randomized Axelerated Maximum Likelihood41) and Bayesian inference (BI) by MrBayes v. 3.2.142. ML analysis settings followed the model of general time reversible with a gamma distribution and proportion invariant (GTRGAMMAI) for the two partitioned datasets. Branch confidence of the tree topology was assessed using 1000 bootstrap replicates (MLb)43. Three independent BI runs were performed with 10 million generations and sampled one tree every 1000 generations. Model parameters from jModelTest were applied on the partitioned dataset. Tracer v.1.644 was used to evaluate the convergence of Bayesian runs. Observed likelihood (-LnL) scores was employed to determine the burn-ins and stable distributions for the two datasets. The majority rule trees from the four- and two-gene datasets were constructed from the remaining trees to estimate the posterior probabilities (Pp).
The approximately unbiased (AU) test45 was carried out as implemented in Consel v.0.1i46 to test for two hypotheses: (i) Amphionides does not belong to the Caridea, and (ii) Amphionides does not belong to Pandalidae. The same two concatenated datasets were run for the ML analysis based on GTRGAMMA model in RAxML v.7.2.6. The alternative tree topologies were also constructed and optimized by RAxML. The algorithm ‘-f g’ was used to compute per site log-likelihood scores for those hypothetical trees and evaluate the significance (P < 0.05) with the present phylogenetic trees in Consel.
How to cite this article: De Grave, S. et al. Phylogenetics reveals the crustacean order Amphionidacea to be larval shrimps (Decapoda: Caridea). Sci. Rep. 5, 17464; doi: 10.1038/srep17464 (2015).
The present work was supported by research grants from the National Natural Science Foundation of China (project no. 41476146), and Ministry of Science and Technology, Taiwan. We are grateful to Alejandro Ariza from the Institute of Oceanography and Global Change (IOCAG, Spain) for the invitation to J.M.L. to participate in field work around the Canary Islands.
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