Research Article |
Corresponding author: Oscar Lisi ( olisi@unict.it ) Academic editor: Sandra McInnes
© 2019 Oscar Lisi, Anisbeth Daza, Rosana Londoño, Sigmer Quiroga, Giovanni Pilato.
This is an open access article distributed under the terms of the Creative Commons Attribution License (CC BY 4.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.
Citation:
Lisi O, Daza A, Londoño R, Quiroga S, Pilato G (2019) Meplitumen aluna gen. nov., sp. nov. an interesting eutardigrade (Hypsibiidae, Itaquasconinae) from the Sierra Nevada de Santa Marta, Colombia. ZooKeys 865: 1-20. https://doi.org/10.3897/zookeys.865.30705
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A new genus of Itaquasconinae, Meplitumen gen. nov., and a new species, Meplitumen aluna sp. nov., are described. The new genus has characters present in other genera of Itaquasconinae but in a unique combination. The spiral thickening of the bucco-pharyngeal tube is also present anteriorly to the insertion point of the stylet supports, excluding only the short portion where the apophyses for the insertion of the stylet muscles (AISM) are present. This character is similar to Astatumen Pilato, 1997 but Meplitumen gen. nov. differs from this genus as stylet furcae are shaped differently and as stylet supports and placoids are present. The presence of a spiral thickening in a portion of the buccal tube anterior to the stylet supports distinguishes the new genus from Mesocrista Pilato, 1987, Platicrista Pilato, 1987 and Itaquascon de Barros, 1939. Meplitumen gen. nov. also differs from Mesocrista, in having the caudal processes of the AISM pointing laterally (instead of postero-laterally), and the apices of the caudal processes of the stylet furcae unswollen. From Itaquascon the new genus also differs by having more robust stylet supports, pharyngeal bulb with placoids, stylet furcae differently shaped. Meplitumen gen. nov. also differs from Platicrista in having caudal processes of the AISM more robust and not flexible, and more slender stylet supports. The new species, Meplitumen aluna sp. nov., has a cuticle with a very faint roughness at the caudal extremity of the body, and eyes probably absent. The pharyngeal bulb is long, with two long, narrow, rod-shaped macroplacoids; a microplacoid and septulum are absent. The claws are well developed with main branches provided with accessory points, and at the base of the claws, a structure interpretable as a very thin lunule is present. Other cuticular thickenings on the legs are absent.
Magdalena, phylogeny, Tardigrada, taxonomy, water bear
Rarely in the study of systematics and phylogeny is one so fortunate to encounter a taxon with characters that sheds light on phylogenetic directions within a group. While studying Colombian tardigrades, from the Sierra Nevada de Santa Marta, we found eight specimens and two exuviae with eggs of a new species of Hypsibiidae (Itaquasconinae), for which it is necessary to erect a new genus that we name Meplitumen gen. nov. This discovery is further confirmation of the biodiversity richness of this Neotropical region (
In the framework of the subfamily Itaquasconine Rudescu, 1964, the four genera Itaquascon de Barros, 1939, Mesocrista Pilato, 1987, Platicrista, Pilato, 1987 and Astatumen Pilato, 1997 are certainly related to one another, but until now it has not been possible to formulate any hypothesis about the phylogenetic relationships that exist among them. Our new genus shows characters that are present in these other genera but in a unique combination. This encouraged us to hypothesise possible evolutionary pathways that connect these five Itaquasconinae genera, which appear to constitute a homogeneous group within the subfamily.
The present work is part of a revision of the tardigradological collection of the Centro de Colecciones Biológicas de la Universidad del Magdalena (CBUMAG:TAR), Santa Marta, Colombia. The material studied with the new genus and species has been returned to the collection.
The original specimens had been extracted from moss and lichen samples collected in San Lorenzo and El Campano, Colombia. Complete information about localities and samples studied are included in the description of the new species under Material examined.
The studied specimens were mounted in polyvinyl alcohol mounting media (BioQuip #6371A). Measurements are given in micrometres (µm), and photomicrographs made under ×100 oil immersion under phase contrast and differential interference contrast microscopy, using a Leica “DMLB” Microscope equipped with “Canon S40” digital camera and a micrometre, a Zeiss Axio Scope A1 with CCD camera Zeiss AxioCam ICc5, and a Zeiss AxioLab A1 with a Zeiss Axiocam ERc 5s. Images were edited, and plates arranged, using Adobe Photoshop Elements 2.0 digital imaging software.
Notwithstanding the presence of spiral thickening, we refer to the “buccal tube” as the entire portion of the bucco-pharyngeal tube anterior to the stylet supports, which seems to be almost rigid. A problem of interpretation and terminology with regard to that portion of the bucco-pharyngeal tube is discussed in the Appendix
Morphological measurements for the holotype, five paratypes, and the additional specimen of Meplitumen aluna sp. nov. The first three small specimens are probably juveniles or males. Measurements given in µm, with pbf and pt index values for relevant structures, and the percent ratio between the main branch and the total length of the external claw. Specimens ordered by buccal tube length (body length being a less precise measurement). The small specimens differ from the larger in the pt values relative to the buccal tube width, the macroplacoid length, and claw II and III length (less remarkably claw IV length), but the percent values of the main branch length with respect to the total claw lengths are compatible.
No. slide | 00376 | 00477 | 00476 | 00461 | 00545 | 00462 holotype | 00460 |
---|---|---|---|---|---|---|---|
Body length | 303 | 258 | 265 | 482 | 486 | 590 | 515 |
Bucco-pharyngeal tube length | 40.6 | 41.6 | 42.4 | 60.0 | 61.2 | 61.3 | ? |
Buccal tube length | 21.0 | 23.3 | 23.6 | 30.6 | 31.7 | 31.8 | 33.7 |
pbf | 51.7 | 56.0 | 55.7 | 51.0 | 51.8 | 51.9 | ? |
Buccal tube external width | 5.2 | 5.6 | 5.7 | 8.7 | 8.8 | 8.9 | 9.5 |
pt | 24.8 | 24.0 | 24.2 | 28.4 | 27.8 | 28.0 | 28.2 |
pt stylet supports insertion point | 100 | 100 | 100 | 100 | 100 | 100 | 100 |
First placoid | ? | 5.2 | 5.2 | 9.3 | 10.7 | 10.9 | 10.6 |
pt | ? | 22.3 | 22.0 | 30.4 | 33.7 | 34.3 | 31.4 |
Second placoid | ? | 14.3 | 14.5 | 25.6 | 29.0 | 29.0 | 29.0 |
pt | ? | 61.4 | 61.4 | 83.7 | 91.5 | 91.2 | 86.1 |
Placoid row | ? | 20.3 | 20.4 | 34.5 | 40.2 | 40.7 | 40.7 |
pt | ? | 87.1 | 86.4 | 112.7 | 126.8 | 128.0 | 120.8 |
External claw I | 14.5 | ? | 15.4 | 21.4 | 21.3 | ? | ? |
pt | 69.0 | ? | 65.3 | 69.9 | 67.2 | ? | ? |
External claw I - main branch | 10.4 | ? | 11.3 | 15.0 | 15.2 | ? | ? |
pt | 49.5 | ? | 47.9 | 49.0 | 47.9 | ? | ? |
External claw I - main branch % total | 71.7 | ? | 73.4 | 70.1 | 71.4 | ? | ? |
External claw I - base + secondary branch | 6.7 | ? | 7.3 | 11.3 | 11.8 | 12.1 | ? |
pt | 32.2 | ? | 30.9 | 36.9 | 37.2 | 38.1 | ? |
Internal claw I | ? | ? | 9.7 | 14.0 | 13.7 | ? | ? |
pt | ? | ? | 41.1 | 45.7 | 43.2 | ? | ? |
Internal claw I - main branch | ? | ? | 6.1 | 8.6 | 8.5 | ? | ? |
pt | ? | ? | 25,8 | 28.1 | 26.8 | ? | ? |
Internal claw I - main branch % total | ? | ? | 62.9 | 61.4 | 62.0 | ? | ? |
Internal claw I - base + secondary branch | ? | 6.2 | 6.1 | 9.0 | 9.1 | 10.2 | ? |
pt | ? | 26.6 | 25.8 | 29.4 | 28.7 | 32.1 | ? |
External claw II | 15.9 | 16.9 | ? | ? | ? | 29.0 | ? |
pt | 76.4 | 72.5 | ? | ? | ? | 91.2 | ? |
External claw II - main branch | 11.5 | 12.2 | ? | ? | ? | 20.0 | ? |
pt | 55.3 | 52.4 | ? | ? | ? | 62.9 | ? |
External claw II - main branch % total | 72.3 | 72.2 | ? | ? | ? | 69.0 | ? |
External claw II - base + secondary branch | 7.1 | ? | 7.4 | ? | ? | 13.8 | ? |
pt | 34.1 | ? | 31.3 | ? | ? | 43.4 | ? |
Internal claw II | ? | 10.5 | 10.9 | ? | ? | 18.4 | ? |
pt | ? | 45.1 | 46.2 | ? | ? | 57.9 | ? |
Internal claw II - main branch | ? | 7.5 | 7.7 | ? | ? | 12.9 | ? |
pt | ? | 32.2 | 32.6 | ? | ? | 40.2 | ? |
Internal claw II - main branch % total | ? | 71.4 | 70.6 | ? | ? | 70.1 | ? |
Internal claw II - base + secondary branch | ? | 6.6 | 6.3 | ? | ? | 11.2 | ? |
pt | ? | 28.3 | 26.7 | ? | ? | 35.2 | ? |
External claw III | ? | 18.1 | 17.4 | ? | ? | 28.6 | 29.0 |
pt | ? | 77.7 | 73.7 | ? | ? | 89.9 | 86.1 |
External claw III - main branch | ? | 13.0 | 11.8 | ? | 18.2 | 19.5 | 19.6 |
pt | ? | 55.8 | 50.0 | ? | 57.4 | 61.3 | 58.2 |
External claw III - main branch % total | ? | 71.8 | 67.8 | ? | ? | 68.2 | 67.6 |
pt | ? | 36.1 | 33.1 | 38.6 | ? | 42.1 | 39.2 |
Internal claw III | 10.3 | 10.9 | ? | ? | 17.4 | 19.3 | ? |
pt | 49.5 | 46.8 | ? | ? | 54.9 | 60.7 | ? |
Internal claw III - main branch | ? | 7.3 | ? | ? | 11.4 | 12.7 | ? |
pt | ? | 31.3 | ? | ? | 36.0 | 39.9 | ? |
Internal claw III - main branch % total | ? | 67.0 | ? | ? | 65.5 | 65.8 | ? |
Internal claw III - base + secondary branch | ? | 6.6 | 6.3 | ? | ? | 11.4 | 11.1 |
pt | ? | 28.3 | 26.7 | ? | ? | 35.8 | 32.9 |
Posterior claw IV | ? | 20.0 | 20.2 | ? | ? | 30.5 | 30.5 |
pt | ? | 85.8 | 85.6 | ? | ? | 95.9 | 90.5 |
Posterior claw IV - main branch | ? | 14.5 | 14.1 | ? | ? | 21.8 | 21.3 |
pt | ? | 62.2 | 59.7 | ? | ? | 68.6 | 63.2 |
Posterior claw IV - main branch % total | ? | 69.0 | 70.1 | ? | ? | 71.5 | 69.8 |
Posterior claw IV - base + secondary branch | ? | 9.8 | 10.1 | 14.0 | ? | 15.3 | 14.7 |
pt | ? | 42.1 | 42.8 | 45.8 | ? | 48.1 | 43.6 |
Anterior claw IV | ? | 10.9 | 11.0 | 16.2 | ? | 17.6 | 18.1 |
pt | ? | 46.8 | 46.6 | 52.9 | ? | 55.3 | 53.7 |
Anterior claw IV - main branch | ? | 7.7 | 7.7 | 11.3 | ? | 12.1 | 12.2 |
pt | ? | 33.0 | 32.6 | 36.9 | ? | 38.0 | 36.2 |
Anterior claw IV - main branch % total | ? | 70.6 | 70.0 | 69.7 | ? | 68.7 | 67.4 |
Anterior claw IV - base + secondary branch | ? | ? | 9.1 | 12.7 | ? | 13.6 | 13.0 |
pt | ? | ? | 38.6 | 41.5 | ? | 42.8 | 38.6 |
Claws of the Hypsibius type showing the criteria used to take the measurements in Meplitumen aluna gen. nov., sp. nov. A claw orientation chosen for measuring the entire length B claw orientation and referring points chosen for various claw portion measurement. The claws shown, used as example, belong to Platicrista angustata (Murray, 1905).
For comparison, we have examined specimens of: Mesocrista spitzbergensis (Richters, 1903) from Tatra Mountains (border between Poland and Slovakia); Platicrista angustata (Murray, 1905) from Ligorzano (Modena, Italy); Itaquascon cambewarrense Pilato, Binda & Claxton, 2002 from Cambewarra Mountain (Australia), and types of Astatumen trinacriae (Arcidiacono, 1962) from Nebrodi Mounts (Sicily). All these specimens are deposited in the Binda and Pilato collection (Museum of the Department of Biological, Geological and Environmental Sciences, University of Catania, Italy).
For phylogenetic analysis, a character matrix was prepared and a parsimony analysis applied with a Nearest Neighbor Interchange (NNI) heuristic method, using the software Mesquite (Maddison and Maddison).
Meplitumen aluna sp. nov.
Claws of the Hypsibius-type. Bucco-pharyngeal apparatus of Itaquasconinae model but buccal tube with a spiral thickening also present anteriorly to the stylet support insertion point (Fig.
Bucco-pharyngeal tube of Meplitumen aluna gen. nov., sp. nov. A holotype (slide No. 00462), was invaded by fungal hyphae. The spiral thickening also anterior to the stylet supports insertion point is visible (arrow ‘a’). The arrow ‘b’ indicates the stylet supports. Arrow ‘c’ indicates the caudal processes pointing sideways of the wide and flat AISM B paratype (slide No. 00460). The spiral thickening also anterior to the stylet supports insertion point is visible (arrow ‘a’). Scale bar: 20 µm.
Bucco-pharyngeal apparatus of Meplitumen aluna gen. nov., sp. nov. A holotype B paratype (slide No. 00477); the arrow indicates a row of small teeth C detail of the pharyngeal bulb of the holotype with the long placoids well visible D bucco-pharyngeal apparatus of a paratype (slide No. 00461); the arrow indicates a stylet furca. Scale bar: 20 µm.
According to the definition in
Shape of the stylet furca (arrow ‘a’) in species of various genera of Itaquasconinae A Mesocrista spitzbergensis (Richters, 1903) B Platicrista angustata (Murray, 1905) C Itaquascon cambewarrense Pilato, Binda & Claxton, 2002 D Astatumen trinacriae (Arcidiacono, 1962). Arrow ‘b’ indicates the stylet supports. Scale bar: 10 µm.
Etymology. Considering that the bucco-pharyngeal apparatus of the new genus has characters present in Mesocrista, Platicrista, Itaquascon and Astatumen, we have chosen Meplitumen as generic name using the first letters of the name of the first three genera (Me-, Pl-, It-) and the final part of the name Astatumen (-umen).
San Lorenzo, Sierra Nevada de Santa Marta, Magdalena, Colombia.
Holotype (slide No. 00462), 5 paratypes (slides Nos. 00460, 00461, 00476, 00477), and two exuviae (slide No. 00492) from a sample dominated by lichens (Usnea, and Parmotrema) mixed with bryophytes (Sematophyllum, Frullania, Microlejeunea, and Leucolejeunea), collected in San Lorenzo (Colombia) at 11°06'16.9"N and 74°03'31.2"W, 2517 m a.s.l.. One paratype (slide No. 00545) collected in the type locality but in a different sample containing lichens (Parmotrema, Heterodermia, and Hypotrachyna) mixed with bryophytes (Meteoridium, Frullania, and Archilejeunea). One additional specimen (slide No. 00376) of a sample of liverworts (Frullania and Cheilolejeunea), collected in El Campano (Colombia) at 11°6'23.2"N and 74°5'19.2"W, 1368 m a.s.l. The type material was collected by Anisbeth Daza, Rosana Londoño and Sigmer Quiroga on 31 July 2015. The remainder of the material was collected by Anisbeth Daza, Rosana Londoño, Paula Sepúlveda and Sigmer Quiroga, on 21 March 2015.
The holotype and paratypes, and the additional specimen, are deposited in the Centro de Colecciones Biológicas de la Universidad del Magdalena (CBUMAG:TAR), Santa Marta, Colombia.
Body uncoloured. A faint, though difficult to see, cuticular roughness visible on the caudal portion of the body. Eyes probably absent (definitely absent after mounting and no information record when mounted). Bucco-pharyngeal apparatus of the Meplitumen-type of Itaquasconinae model (as described above). Mouth terminal. A row of small teeth is present in the caudal portion of the buccal cavity (Fig.
We found eight specimens and two exuviae with eggs and it is interesting to note that three specimens were small and of similar body size, whereas the others are markedly longer and certainly adults as demonstrated by the size of the exuviae with eggs. Unfortunately, we have not been able to establish the sex of the specimens; in particular, whether the smallest were three young, or new-born specimens, or were males. It is interesting to note that some metric characters of the smaller specimens are very similar to those of the larger specimens, while others were markedly different (see Table
Body length 590 µm, uncoloured, cuticle with a faint, very difficult to see roughness in the caudal body portion (Fig.
Claws of the Hypsibius-type well developed (Fig.
A–C claws of Meplitumen aluna sp. nov. (paratypes) A claws III B and C claws IV. The arrow indicates the structure interpretable as a very thin lunule D claws III of Platicrista angustata (Murray, 1905). It is evident that in Meplitumen aluna sp. nov. the claw secondary branches are longer and thinner than those of Platicrista angustata. Scale bar: 20 µm.
We found two exuviae, one with 5 and the other with 6 smooth eggs.
The specific epithet refers to the term “Aluna” which in Ika, the native language of the Kogui (an Amerindian ethnic group inhabiting the Sierra Nevada de Santa Marta), means the non-visible or spiritual world. Aluna is a name in apposition.
As mentioned above, the three smaller specimens (Fig.
The particular combination of the characters of the bucco-pharyngeal apparatus distinguishes the new species from all known species of Itaquasconinae. It is possible that the presence of spiral thickening in the “buccal tube”, and the lateral orientation of the caudal processes of the AISM was missed in some previously described species. In this case, any species found with these characters should be transferred into the new genus Meplitumen, though this may result in Meplitumen aluna sp. nov. becoming a junior synonym. Therefore, to avoid this remote risk, we found it opportune to compare the new species with all the similar, known species of Itaquasconinae independently from the extension of the spiral thickening.
It is unnecessary to compare all Itaquascon species, as the presence in Meplitumen aluna sp. nov. of true macroplacoids, a more developed and differently shaped stylet furca (with longer branches) (Figs
The differences with Mesocrista species are also clear, as
We carefully examined Platicrista angustata (Murray, 1905) and ascertained the absence of spiral thickening in the buccal tube wall (Fig.
Platicrista affine (Mihelčič, 1951) is considered a nomen dubium (
Preliminary discussion
The new genus Meplitumen is, in our opinion, particularly interesting as it possesses characters which allow us to imagine the evolutionary pathways that connect the five genera of Itaquasconinae Mesocrista, Platicrista, Meplitumen gen. nov., Itaquascon and Astatumen which constitute a homogeneous group inside that subfamily.
Above all, the absence of molecular data for Bindius and Parascon and the fact that we have not had the good fortune to examine Sarascon, we prefer in this paper to concentrate our attention on the five genera Mesocrista, Platicrista, Meplitumen, Itaquascon and Astatumen that certainly, within the family Itaquasconinae, constitute a homogeneous group.
Taking into account the morphology of the Hypsibiidae, some easily recognisable evolutionary tendencies can be noticed in the group of genera we are considering.
The first regards the shape of the AISM, which tend to become wide and flat and whose caudal processes only in Mesocrista point postero-laterally, as in all the other Parachela, while in Platicrista, Meplitumen, Itaquascon and Astatumen they point laterally. These processes are definitely more robust in Mesocrista and Meplitumen, while they are thinner in Platicrista, and extremely thin, even flexible, in Itaquascon and in Astatumen.
A second evolutionary trend regards the shape and size of the stylet furcae. In Mesocrista only are the furca processes well developed and with swollen apices (Fig.
A third evolutionary trend regards the stylet supports, which are normally developed in Mesocrista, Meplitumen and Platicrista, very thin in Itaquascon (Fig.
The fourth evolutionary direction is that of the placoids, which are present, long and slender in Mesocrista, Meplitumen, and Platicrista. In Itaquascon and Astatumen these are substituted by a long, simple cuticular thickening, which can also be (or seem to be) absent in some species.
Some of these evolutionary tendencies are also recognisable in the genera Bindius, Parascon and Sarascon but, as mentioned above, we are not considering these three genera in this paper.
A parsimony analysis of the character matrix shown in Table
Character matrix used for the phylogenetic analysis. AISM = apophyses for the insertion of the stylet muscles.
AISM shape | AISM caudal process development | AISM caudal process orientation | Stylet furcae | Stylet furcae apices | Anterior tube spiral thickening | Placoids | Stylet supports | |
Mesocrista | moderately wide | robust | postero-lateral | “big” with developed branches | swollen | absent | present (slender) | present (normal) |
Meplitumen | moderately wide | robust | lateral | “big” with developed branches | non-swollen | present | present (slender) | present (normal) |
Platicrista | very wide | thin | lateral | “big” with developed branches | non-swollen | absent | present (slender) | present (normal) |
Itaquascon | very wide | extremely thin, even flexible | lateral | small with reduced branches | non-swollen | absent | reduced to a thin bar or absent | present (slendered) |
Astatumen | very wide | extremely thin, even flexible | lateral | small with reduced branches | non-swollen | present | reduced to a thin bar or absent | absent |
Most supported phylogenetic tree, according to character matrix in Table
Mesocrista is the genus which most closely resembles the other Hypsibiidae (i.e. ancestor “0” in Fig.
In choosing the proposed phylogenetic tree, we have been careful not to allow character reversals. However, the spiral thickening on the anterior buccal tube is present in two separate branches of the tree (in Meplitumen and Astatumen), which we hypothesise is not a reversal but the character appearing twice, independently, in those two branches. This is the only weak point of the proposed tree but we want to stress that any change in the tree aimed at correcting this situation invariably produces multiple reversals in other characters. This double appearance of the anterior buccal spiral thickening character in Meplitumen and Astatumen might be explained by hypothesising that their common ancestor already possessed a genetic prerequisite (to form spiral thickening) thus requiring only one, or few mutations, to express the character.
In Mesocrista the annulation of the pharyngeal tube was described as double (
It is clear that in all cases, any attempt to reconstruct phylogenetic relationships requires making a hypothesis that can be tested, and which might give rise to doubts or different opinions. We think that a hypothesis can be proposed when clear characters and evolutionary tendencies are observed in known members of a taxon (for which the phylogeny is totally unknown). Such a proposed hypothesis is justified and needs to be brought to the attention of the scientific community, while awaiting new data to confirm or create a new, more convincing, phylogenetic reconstruction.
The present work also adds value to the biodiversity of Colombia, with a new species and a new genus that, at least for the moment, result endemic for the country. It is worth mentioning that we are about to publish another new genus (of a different family) from Colombia, proving the high potential of these investigations, since to date very little is known about the tardigradological fauna of the country. This encourages us to go on with our studies.
We thank Paula Sepúlveda for helping to collecting the samples; Claudia Morales and Kevin R. Roncallo for the identification of the bryophytes and lichens. This work was carried in the framework of the research projects “Diversidad de ositos de agua (Tadigrada) asociados a briófitos y líquenes epífitos en cultivos de café de la Sierra Nevada de Santa Marta, con un enfoque innovador para la apropiación social del conocimiento” and “Ositos de agua (Tardigrada) de la Sierra Nevada de Santa Marta: revisión taxonómica de la colección científica de referencia del Centro del Colecciones Biológicas de la Universidad del Magdalena ‘CBUMAG’”, supported by the Universidad del Magdalena (FONCIENCIAS 2015–2017 and FONCIENCIAS 2017–2019). This is a scientific contribution number 10 from de Centro de Colecciones Biológicas de la Universidad del Magdalena CBUMAG.
We are also grateful to the colleagues Roberto Bertolani and Barbara Weglarska who donated many years ago, respectively, the specimens of Platicrista angustata and Mesocrista spitzbergensis for the Binda and Pilato collection. Lastly, we want to thank the anonymous reviewers, and the editor (Sandra McInnes) for improving the quality of the manuscript.
The presence in Meplitumen of spiral thickening to almost the whole length of the bucco-pharyngeal tube gives rise to a problem of interpretation, and, as a consequence, terminology of the subdivisions of the Astatumen bucco-pharyngeal tube. In all tardigrades with bucco-pharyngeal tube divided into a rigid anterior portion without spiral thickening and a flexible posterior portion with spiral thickening, the spiral thickening and the stylet supports insertion point have been used to differentiate between the anterior buccal tube and the posterior “pharyngeal tube”. As a consequence, in Astatumen, which lacks stylet supports, only the spiral thickening has been taken as the reference point, and therefore the buccal tube has been considered to be only the very anterior portion where the AISM lie. However, the distinctive situation we have encountered in Meplitumen made us realise that the short portion defined buccal tube in Astatumen does not correspond to the equivalent buccal tube of the other genera, but only to its anterior part. The absence of stylet supports in Astatumen prevents the location of the exact border between what in other genera is defined buccal and pharyngeal tube. Having clarified this situation it would be necessary to modify the terminology, as well as the evaluation of the length of the buccal tube, to redefine the short anterior portion of buccal tube without spiral thickening. Nevertheless, the problem of fixing the exact border between the real buccal tube and pharyngeal tube, and calculating the exact lengths, would remain unsolved. In conclusion, we find it is important to have clarified the morphological and phylogenetic meaning of these structures, but for practical reasons we think that it would not be opportune to change the terminology.