JOURNAL OF CRUSTACEAN BIOLOGY, 23(3): 644–661, 2003 PROPOSED NEW STANDARDIZED ANATOMICAL TERMINOLOGY FOR THE TANAIDACEA (PERACARIDA) Kim Larsen Department of Oceanography, Texas A. and M. University, Box 3146, College Station, Texas 77843-3146, U.S.A. ([email protected]) ABSTRACT A summary of terminologies and nomenclature currently or previously employed to describe tanaidacean appendages and somites are presented together with a proposed new standardized terminology for the order Tanaidacea. Standardized expressions and nomenclatures are suggested for all tanaidacean somites, appendages, and their articles, as well as for the orientation of tanaidacean appendages. The lack of consensus in tanaidacean terminology has long been an obstacle for taxonomical and systematics studies. Much of the present-day confusion in the tanaidacean systematics is caused by this lack of a common terminology or by authors mixing structural terms and terms derived from homology with other crustaceans. For example, identifying specific characters on ‘‘pereopod II’’ is bound to lead to disaster if the observer is not aware that by ‘‘pereopod II’’ many authors actually mean the ‘‘first walking leg.’’ This is just the most obvious problem among a host of inconsistencies within the tanaidacean terminology and, particularly, within the nomenclature (Table 1). A number of papers have dealt with tanaidacean terminology and nomenclature (Lang, 1953a; Wolff, 1956; Gardiner, 1975; Sieg, 1977a; Messing, 1981; Holdich and Jones, 1983; Dojiri and Sieg, 1997), but few of them agree, and they contain many inconsistencies or even errors. This paper is an attempt to resolve this subject by reviewing the different terminologies in use. The relatively less important questions of spelling and transliteration are not treated in this report. For additional information about terminology of other crustacean groups, see McLaughlin (1980). TERMINOLOGY AND NOMENCLATURE Cephalothorax versus Carapace The head and following two somites (thoracomeres) of tanaidaceans are fused to form a cephalothorax that is covered dorsally by a heavily calcified carapace. Sieg (1973) used the term cephalothorax instead of carapace for all references to this region and adopted the definition of Zimmer (1927), that the carapace only covers the posterior part of the cephalothorax (the fused thoracomeres) and not the head. The definitions of ‘‘carapace’’ proposed by Stebbing (1893) and others are somewhat different and perceive the carapace as a lateral and dorsal shield covering the cephalothorax (both head and following fused thoracomeres). Zimmer’s definition is supported by the embryological study of Scholl (1963), although the exact boundary between the head and somites cannot be identified. If Zimmer’s definition of ‘‘carapace’’ requires a suture separating the head from the following thoracomeres, then it is problematic. Such a suture cannot be identified in the Tanaidomorpha (the largest tanaidacean suborder) and only with uncertainty in the other tanaidacean suborders. To apply two different terms in the different suborders clearly would be counterproductive. Given this information, the term ‘‘cephalothorax’’ would be appropriate when describing the region, while ‘‘carapace’’ should be applied when describing external features. In cases of morphometric analysis, one would get the same results regardless of usage. Pereonites and Pleonites All malacostracans possess eight somites (thoracomers) between the head and the abdomen, but two of these are fused with the head and covered by the carapace. The six (or rarely five) free somites after the cephalothorax are together called the ‘‘pereon,’’ and ‘‘pereonites’’ individually, in the tanaidacean literature. The 644 645 LARSEN: STANDARDIZED TANAIDACEAN TERMINOLOGY Table 1. Different terminologies and nomenclatures for tanaidacean appendages. Bate, 1856 First cephalic appendage First or anterior antennae Second cephalic Second or appendage external antennae Fourth cephalic First appendage maxilla Fifth cephalic Second appendage maxilla First Maxilliped thoracopod Second 1. Gnathopod thoracopod Third 2. Gnathopod thoracopod Following thoracopods Pereiopods 1–5 G. O. Sars, 1896 Whitelegge, 1901 Hansen, 1913 Tattersall, 1925 Sieg, 1977 Superior antennae Upper antenna Antennule Antennule Antenna 1 Inferior antennae Lower antenna Antenna Antenna Antenna 2 Anterior maxillae Posterior maxillae Maxilliped First Maxillule maxilla Second Maxilla maxilla (not mentioned) Maxilliped (not mentioned) Maxilla 1 (not mentioned) Maxilla 2 (not mentioned) Maxilliped Cheliped or First leg first leg Second leg, Second leg Pereiopod 1, Fossorial leg (in Apseudidae), Ambulatory leg (in Tanaididae) Pereiopods 2–6 Legs 3–7 pereonites are part of the thorax, but the thoracomers are not necessarily pereonites (McLaughlin, 1980). Unfortunately, this definition has not been followed by all workers on the Tanaidacea. Some workers have considered the fused somites covered by the carapace as being part of the pereon, but those workers have not even agreed on how many should be included (Messing, 1981: 98). The next five somites are termed ‘‘pleonites’’ and together with a sixth pleonite fused to the telson (pleotelson), this region is termed the ‘‘pleon’’ (Gardiner, 1975). While few or no problems exist with the nomenclature of the pleonites, which are numbered one to five (or less if fusion occurs), major confusion is encountered with the nomenclature of the pereonites. Previously, authors have been numbering the pereonites in several different ways. One system, which unfortunately is still in use, is the nomenclature of Hansen (1913). This system is derived from the concept that only one thoracomer is fused to the head (Hansen, 1913: 8), and Hansen therefore numbers the first free pereonite as number 2. This approach has caused much confusion over time. Firstly, it does not follow the crustacean homologies as there are two fused thoracomeres covered by the carapace; secondly, the fused thoracomers should not be counted as pereonites; and thirdly, Cheliped Cheliped/ Cheliped/ Pereopod 1 2nd thoracic limb Pereopod 1 Pereopod 2 3rd thoracic limb Pereopods 3–7 Thoracic limbs 4–8 Pereopods 2–6 it suffers from not having identifiable structures. The most serious problem from this system arises when dealing with the corresponding appendages (see discussion of cheliped and pereopods). Tattersall (1925) used a numbering system based on homologies. Realizing that two thoracomeres are fused to the head, this author numbered the first free pereonite as ‘‘thoracomer three.’’ While essentially correct, this system is also the least used. The failure of this system to be widespread lies in the desire for identifiable structures which is not possible, because the first and second thoracomeres cannot be identified as separate structures. A third, and probably the most widespread, system is the one provided by G. O. Sars (1896) assigning the first free pereonite as number 1 and subsequent pereonites as 2 through 6. The advantage of this system is apparent when dealing with appendages, and if we consider pereonites as ‘‘free thoracomers,’’ this system also follows the concept of homologies. All these three nomenclatures result in different terms for the tanaidacean appendages (see discussion of cheliped and pereopods). The system of Sars has the most advantages of these different systems: 1) it is the most widely accepted; 2) all structures are easily identifiably, requiring no prior knowledge of how many somites are fused and ‘‘hidden’’; and 3) it conforms well to 646 JOURNAL OF CRUSTACEAN BIOLOGY, VOL. 23, NO. 3, 2003 both homologies and the suggested nomenclature of the pereopod system of ‘‘first walking leg ¼ pereopod 1’’ (see discussion of pereopods). Antennule and Antenna The terminology of the first cephalic appendages differs mainly because of cultural differences between the Anglo-American and Continental European traditions for naming. Anglo-American authors prefer different names for different appendages, while the Continental authors seem to prefer different numbering of different appendages of a common function. Thus the different terminologies have caused name conflicts such as ‘‘antennule’’ versus ‘‘antenna I’’ and ‘‘maxillule’’ versus ‘‘maxilla I.’’ This difference, however, does not seem to have caused any serious confusion. Most authors divide the antennule and antenna into a stout basal part, the ‘‘peduncle,’’ and a slender distal part, the ‘‘flagellum,’’ as in other peracarids. In species with biramous antennules, the basal part proximal from the separation of rami is the ‘‘peduncle.’’ The biramous part distal to the separation of rami is termed ‘‘flagellum’’: outer and inner (accessory flagellum). This is consistent with most other peracarid terminologies but leads to a number of problems. Firstly, it fails when applied to species with uniramous antennae. In most species of Tanaidomorpha and Neotanaidomorpha, it is not obvious where the flagellum starts, if it exists at all (Fig. 1). Secondly, there seems to be no consensus as to which part the common article of biramous antennules belongs. Some authors include it in the peduncle (Gardiner, 1973; Sieg; 1986a; Bamber, 1998), some the flagellum (McSweeny, 1982), and others do not count it at all (Lang, 1968; Guţu, 1996). To leave the common article out altogether is clearly untenable, and, because the word peduncle means ‘‘stem to which something is attached,’’ it is here suggested to include this article in the peduncle (Fig. 1A). One interesting way to determine the boundary between the flagellum and peduncle, as suggested by a reviewer, is to look at the ‘‘swimming males’’ of certain tanaidomorphan taxa. In these males, the peduncle consists of two stout articles and one reduced asymmetric article. The flagellum consists of several articles, all with dense ventral tufts of aesthetascs. The problem is that this definition is useless when dealing with taxa where the males are not of the swimming type and the antennule is radically different. Another problem is that the peduncle of Tanaidomorpha and Apseudomorpha will then not be of the same length. Regarding the antenna, some authors count the squama-bearing article (article 2) as the last peduncle article (Lang, 1968; Sieg et al., 1982; Viskup and Heard, 1989), and others believe that the ‘‘peduncle’’ of the antenna goes beyond the article with the squama (Guţu, 1996; Bamber, 1998) and apparently use the size of the articles to decide where they belong. Several workers on Apseudomorpha (McSweeny, 1982; Meyer and Heard, 1989) and most on Neotanaidomorpha (Gardiner, 1975; Larsen 1999a) and Tanaidomorpha (Lang, 1968; Shiino, 1978; Sieg, 1986a; Larsen, 2002) refrain from using the term peduncle at all and assign numbers to the articles. Because peduncle means ‘‘stem’’ and flagellum means ‘‘whip’’, it is unsatisfactory to limit the peduncle to the part proximal to the squama, when robust articles extend beyond the squama in many taxa (Fig. 2A). To use size as the only character seems also to be a dubious approach, as many species (for example in the Pagurapseudidae) experience a steady and indistinct decline in article size in the distal direction (Fig. 2B). There are also no obvious serially repeating articles in the antennal flagellum of either Tanaidomorpha or Neotanaidomorpha (Fig. 2C, D). The musculature of the antennal flagellum articles in those Apseudomorpha that do have an obvious flagellum is rudimentary, but in those species without serially repeating articles, there appears to be no discrete difference in the musculature of distal/proximal articles. The degree of spination/ setation is also not different in the distal/proximal antennular articles of most tanaidomorphans or neotanaidomorphans (Fig. 2C, D). In the case of the antenna in general, and in the tanaidomorphan and neotanaidomorphan antennule, the best approach seems to be simply assigning numbers to the articles in a proximaldistal direction. This approach would eliminate much of the confusion even if it may be a bit tedious when dealing with taxa with multiarticulated antennae. Mouthparts The labrum has only been given one other term, the ‘‘upper lip’’ (Boesch, 1973), but the consensus is to use the term labrum (see discussion of the labium). Băcescu (1987) named the labrum a ‘‘process on the clypeus.’’ LARSEN: STANDARDIZED TANAIDACEAN TERMINOLOGY 647 Fig. 1. Antennule peduncle. A, Apseudomorpha. B, Neotanaidomorpha. C, Tanaidomorpha. Because clypeus is the region of the head where the labrum is attached, this is not wrong, but the labrum is a more precise term for this structure. The labium has been given several different terms. ‘‘Paragnath’’ was used by Shiino (1937), but Shiino switched to the term ‘‘labium’’ in his later publications. Dojiri and Sieg (1997) and Guţu and Sieg (1999) also mentioned the term paragnath, as well as ‘‘hypopharynx,’’ but did not use those terms in any of their descriptions. ‘‘Lower lip’’ is another term found in the literature (Boesch, 1973). Although this term is just the English word for labium, the latter must be preferred because labium has a much higher representation in the literature. The palp of the labium has been termed ‘‘palp’’ by most authors (Sieg, 1986; Meyer and Heard, 1989; Dojiri and Sieg, 1997; Guţu and Sieg, 1999; Hansknecht et al., 2001), although a number of other terms have appeared in the literature: 1) ‘‘Last segment’’ (Guţu, 1975), and it is indeed the last segment (article) of two of the labium, but this is not very consistent with the terminology of other mouthparts; 2) ‘‘anterolateral plate’’ was used by Wolff (1956) but was not followed by other workers; 3) several different word combinations ending in ‘‘lobes’’ have been applied to this structure (Wolff, 1956; Lang, 1968, Gardiner, 1973; Shiino, 1978; Guţu, 1998; Larsen, 1999b). To use the term ‘‘lobes’’ is, however, unfortunate because this is also the term used for the circular basal structures of the labium (Lang, 1968; Shiino, 1965; Sieg, 1980; Larsen, 2000). Because the palp is articulated from the labium in the Apseudomorpha and Neotanaidomorpha (although different degrees of fusion may obscure this, particularly within the Neotanai- 648 JOURNAL OF CRUSTACEAN BIOLOGY, VOL. 23, NO. 3, 2003 Fig. 2. Antenna peduncle. A, Carpoapseudes. B, Pagurapseudes. C, Neotanais. D, Tanaella. domorpha), ‘‘lobes’’ would be erroneous. In the Tanaidomorpha, a structure can sometimes be present on the lateral corners and has been termed ‘‘processes’’ because no articulation can be identified. It is possible that these ‘‘labium processes’’ are rudiments of the palp but could also be secondarily evolved. The solution here would be to call this distal structure ‘‘palp’’ when articulation exists and ‘‘process’’ when no articulation is found, and reserve the term ‘‘lobes’’ for the basal rounded structures (Fig. 3). The mandibles seem to have been spared from terminological confusion, although Dojiri and Sieg (1997) used the term ‘‘pars molaris’’ for the molar and ‘‘pars incisiva’’ for the incisor. The maxillule and maxilla have been termed ‘‘Maxilla 1’’ and ‘‘Maxilla 2’’ (Sieg, 1972 and others) or ‘‘Anterior maxillae’’ and ‘‘Posterior maxillae’’ (G. O. Sars, 1896). This appears not to have caused any major confusion, and consensus is now moving towards the opinion of Bate (1856), who used the terms maxillule and maxilla. The different subdivisions of the maxilla, however, have had several terms applied. The maxilla of Neotanaidomorpha and Apseudomorpha consists of a movable (outer) endite, divided into two lobes, and a fixed (inner) endite, also divided into two lobes (Guţu, 1996). ‘‘Inner’’ here represents the side facing the median plane of the animal (Figs. 4 and 12). Hansknecht et al. (2002) used the term ‘‘inner endite’’ instead of ‘‘fixed endite,’’ and Larsen (1999b) used ‘‘inner process’’ instead of ‘‘inner endite.’’ Gamo (1984) used the term ‘‘distal portion’’ for the outer lobe of the fixed endite. Lang (1968) used the term ‘‘fixed endite’’ solely for the outer lobe of the fixed endite. Lang (1968) did not name the part of the maxilla that is generally named as the inner lobe, and described the setal row on this region as a ‘‘rostral row of setae.’’ This was followed by a number of authors (Gardiner, 1973; Sieg, 1986a; Viskup and Heard, 1989), although these authors used the term ‘‘medial row’’ instead of ‘‘rostral row.’’ As this region is clearly a distinct part of the fixed endite, it is here suggested that it be called ‘‘inner lobe of fixed endite’’ and that the row of setae on it be described as ‘‘being on the inner lobe of the fixed endite’’ instead of just calling it medial or rostral. The maxilla of Tanaidomorpha is reduced to an almost featureless ovoid structure and has thus been spared terminological disputes. The maxilliped is the first thoracic appendage even though the somite from which it originates is fused with the head. Most authors agree thus far, and the term maxilliped is not under dispute. However, associated with the maxilliped is an additional structure, the epignath, the affinity of which has been under dispute. The epignath has a ventilatory function in tanaidaceans (Siewing, 1951; Johnson and Attramadal, 1982a, 1982b) and is believed by some to be the original exopod of the maxilliped because of a clear muscle connection, although no articulation has been demonstrated (Claus, 1884; Dennell, 1937; Sieg, 1984). An affinity with the cheliped has also been suggested (Lauterbach, 1970), while some authors consider it an independent appendage (Blanc, 1884; Siewing, 1953, 1957). While the authors contest the affinity, only LARSEN: STANDARDIZED TANAIDACEAN TERMINOLOGY 649 Fig. 3. Labium, palp, lobes and processes. A, Apseudomorpha. B, Neotanaidomorpha. C, Tanaidomorpha (Bathytanais). D, Tanaidomorpha (Leptochelia). Barnard (1935) uses a different term, ‘‘epipod,’’ for this structure. The term epignath can thus be applied without confusion. Cheliped and Pereopods The confusion in the nomenclature of the pereonites as described above results in a similar confusion regarding nomenclature of the ap- pendages attached to them. Several authors have given different versions of appendage numbering in tanaids as seen in Table 1, and Messing (1981) has given a good review into the background of many of the terms. Following the system by Tattersall (1925), the cheliped is ‘‘thoracopod II,’’ and the first walking leg will be ‘‘thoracopod 3.’’ While it is Fig. 4. A, Maxilla, endites and lobes (Apseudomorpha/Neotanaidomorpha). B, Maxilla (Tanaidomorpha). 650 JOURNAL OF CRUSTACEAN BIOLOGY, VOL. 23, NO. 3, 2003 true to the concept of homologies that the cheliped is a thoracopod, the problem with this system is that nonspecialists will automatically search for the ‘‘missing’’ thoracopods (Fig. 5A) as chelipeds and maxillipeds rarely are termed thoracopods. According to Hansen (1913) the cheliped is ‘‘thoracopod I,’’ and the first walking leg thus becomes ‘‘pereopod 2’’ (Fig. 5B). Hansen was not alone with this misconception, as Whitelegge (1901) had applied the same nomenclature but called the cheliped the ‘‘first leg’’ and numbered the pereopods as 2–7. Lang (1953a) realized that the cheliped is the second thoracopod but retained the terms ‘‘cheliped’’ and ‘‘pereopod 2.’’ He (Lang, 1953a: 342) presented a table of terms previously used for the first three ‘‘legs’’ [sic]. This table is, however, confusing, because Lang used terms for the first four thoracopods in his three ‘‘leg’’ columns. Lang was followed by Wolff, although he (Wolff, 1956: 189) suggested that the cheliped was the ‘‘second leg’’ as well as the ‘‘first pereopod,’’ because he considered the first thoracic somite (fused to the head and bearing the maxilliped) not to be part of the pereon while the second thoracic somite (also fused to the head, bearing the chelipeds) was. The confusion is apparent with this system, and nonspecialists have little chance of using it correctly. If we follow the definition of McLaughlin (1980), the somites that are fused to the head are thoracomers, not pereonites, and thus the cheliped should never be termed the ‘‘first pereopod.’’ The cheliped was also termed ‘‘first gnathopod’’ by Bate (1856), and he also termed the first walking leg ‘‘second gnathopod,’’ following amphipod terminology (Fig. 5C). Bate argued that this is the proper term because this limb is rarely used for walking (which is correct but only for some taxa). Bate also used a nomenclature where the second free pereonite is numbered 3, while the leg it is carrying is numbered pereopod 1, which makes the confusion complete. This system was followed by Norman and Stebbing (1886). Barnard (1935) mixed the systems and termed the cheliped ‘‘gnathopod 1,’’ while the first walking leg was ‘‘pereopod 2.’’ G. O. Sars (1896) first used the terms ‘‘cheliped’’ for the cheliped and ‘‘pereopod 1’’ for the first walking leg, although he was not consistent. He (G. O. Sars 1896: 1–5) called the cheliped the ‘‘first leg’’ and the first walking leg Fig. 5. Nomenclatures of the anterior thoracopods. A, According to Tattersall (1925). B, According to Hansen (1913). C, According to Bate (1856). D, According to Sieg (1977a). the ‘‘second leg,’’ while later in the same publication (G. O. Sars, 1896: 6–44) the cheliped was then called ‘‘cheliped’’ and the first walking leg was called the ‘‘fossorial leg’’ in the Apseudidae and ‘‘first ambulatory leg’’ in the Tanaididae. Sieg (1977a) also used the terms ‘‘cheliped’’ for the cheliped and ‘‘pereopod 1’’ for the first walking leg, whether it is used for LARSEN: STANDARDIZED TANAIDACEAN TERMINOLOGY walking or not, and at least he was consistent (Fig. 5D). The existence of such different nomenclatures is clearly confusing and untenable. Furthermore, any student or worker not familiar with the history of Tanaidacea literature will be confused by a numbering system describing the first walking leg as anything but number 1. For simplicity alone, the nomenclature of pereopods 1 through 6 seems to be causing the least confusion. Furthermore, there seem to be much confusion as to what ‘‘pereopod’’ means. Bate (1856: 27) and Messing (1981: 98), stated that the word means ‘‘walking leg’’ (Greek: pereon ¼ ‘‘to walk about’’ þ pod ¼ foot). Wolff (1956) stated that Bate was incorrect and that pereon means crossing over (Greek: pereion ¼ ‘‘to bring to the other side’’ or ‘‘to cross to the other side’’). One reviewer stated that it actually means transport. According to my dictionary (Pring, 1982), Wolff is correct. However, no matter who is correct in this translation issue, all translations indicate function and not homology. If this is correct, then it would be misleading to apply the term pereopod to the cheliped and maxilliped, as also would be the conclusion if we follow the definition of pereon by McLaughlin (1980). 651 same structure (Fig. 6C). Because this structure is a sclerite of the carapace (Larsen 2001), the name sclerite is appropriate. To further complicate the issue, a few taxa (Nesotanais, Paranarthrura) within the Tanaidomorpha have a subdivision of the cheliped basis (Fig. 6D). This ‘‘basis subdivision’’ was first described by Hansen (1913) and later by Lang (1971), who considered the subdivision to be reflecting a fusion of the coxa and the basis and thus used the term ‘‘coxa’’ for the proximal subdivision of the cheliped basis. This is entirely possible but unlikely, because no other tanaidomorphans have a coxa (see above). Shiino (1968), however, thought it was a division of the basis and ischium. This is also a possibility but equally unlikely, because no other tanaidomorphans have even a vestigial cheliped ischium. Shiino (1968) used the term ‘‘basis’’ for the proximal subdivision of the cheliped basis. Sieg (1984) was more uncertain about the origin of this structure and introduced the term ‘‘pseudocoxa.’’ Whether this structure is indeed a coxa, a basis, an ischium, or a totally unrelated structure remains to be determined, and until then, the term pseudocoxa is recommended for this structure. Articles of the Cheliped and Pereopods Cheliped Ischium, Merus, Carpus, Propodus, and Fixed Finger The basic division of articles in the tanaidacean appendage is as follows: Coxa (if any), basis, ischium (if any), merus, carpus, propodus, and dactylus. However, not even this division is without controversy. Only in some taxa within the Apseudomorpha (Fig. 6A) is the cheliped attached to the cephalothorax via a small true coxa (Sieg, 1984; Guţu and Sieg, 1999). An analogous structure found in the Neotanaidomorpha (Fig. 6B) has also been termed ‘‘coxa’’ (Hansen, 1913; Gardiner, 1975; Messing, 1977), but this structure is not homologous with the coxa and, rather, is derived from the cephalothorax and thus not an article of the appendage itself (Lauterbach, 1970). This neotanaidomorphan structure is homologous with the sidepiece in the Tanaidomorpha (Lauterbach, 1970). Sieg (1976a) called this structure ‘‘coxa,’’ but in 1984 and later publications, Sieg used the term ‘‘sidepiece’’ for this structure in the Tanaidomorpha, while retaining the term coxa for the neotanaidomorphan equivalent. Still later, the terms ‘‘triangular plate’’ (Larsen and Wilson, 1998) and ‘‘sclerite’’ (Larsen, 2001) appeared in the literature describing the Most Tanaidacea do not have a cheliped ischium. Apart from the potential ischium-basis described by Shiino (1968) and mentioned above, we only find a vestigial ischium within the Neotanaidomorpha (Gardiner, 1975; Sieg, 1984). This ischium (Fig. 6B) consists of an incomplete ring surrounded by an articulated membrane and frequently partly covered by the basis (Larsen, 1999a). Most authors accept that the article after the cheliped basis is the merus (Lang, 1968; Gardiner, 1975; Sieg, 1986a). Yet Hansen (1913: 8) was of the opinion that this article was the ischium, and that the following article was a fusion of the carpus and merus. Monod (1935: 453) was of the opinion that the carpus was a fusion of the ischium and a preischium. It is apparent that neither of these authors was aware of the vestigial ischium found in the Neotanaidomorpha, which clearly demonstrates that the carpus and merus are two separate articles not including the ischium. The propodus of the tanaidacean cheliped is equipped with a process termed the ‘‘fixed finger’’ of the chelae. This structure is 652 JOURNAL OF CRUSTACEAN BIOLOGY, VOL. 23, NO. 3, 2003 Fig. 6. The cheliped coxa, sclerite, pseudocoxa, and ischium. A, Apseudomorpha. B, Neotanaidomorpha. C, Tanaidomorpha (Paratanais). D, Tanaidomorpha (Paranarthrura). frequently described separately from the propodus but is rarely perceived as an independent article. Exceptions to this were Hansen (1925: 115) and Monod (1935: 435), who described the propodus (inclusive the fixed finger) as the ‘‘carpus-propodus.’’ Terminal Structure of the Pereopod Dactylus The shape of the pereopod dactylus is important in making family designations for many taxa (Sieg, 1984; Larsen and Wilson, 2002). Unfortunately, many different terms have been used for the terminal structure of the dactylus, including nail (Norman and Stebbing, 1886), claw (Hansen, 1913), hook (Shiino, 1965), terminal spine (Sieg, 1977a), dactyloclaw (Băcescu, 1980), terminal seta (Larsen and Rayment, 2002), and unguis (Boesch, 1973)(Fig. 7). This terminal dactylus structure is actually just the sclerotized tip of the dactylus and not an article in itself. The term ‘‘claw’’ is thus justified, in a sense, because this structure is analogous with the mammalian analogues. The term claw is, however, potentially confusing, because this term is also used to describe the claw-shaped combination of the dactylus/ unguis found on the last three pairs of pereopods in several tanaidacean taxa, as described in Pseudoleptochelia (Sieg, 1976b), Heterotanaoides (Sieg, 1977b), Nototanais (Sieg, 1980), Paratanais (Sieg, 1981), Tanaissus (Jones and Holdich, 1983), Leptochelia (Larsen and Rayment, 2002), and others. To name this structure a ‘‘spine’’ may also be justified if one chooses to consider this as a pointed extension of the dactylus cuticle, but this is more dubious, because it is actually only a thickening of the cuticle rather than an extension. The term ‘‘terminal seta’’ appeared in Larsen and Rayment (2002), after a reviewer commented that ‘‘since Watling (1989) had established the definition of setae as being articulated from the cuticle, this structure should be termed ‘seta’ and not ‘spine’ as it displays an articulation.’’ The term was used in a number of following papers (Larsen, 2002; Larsen and Wilson, 2002), which is unfortunate because this structure has nothing to do with a seta, and the suture between it and the dactylus proper is not a true articulation. We may hope that this term will not be used in the future. Another term for this structure is unguis (Boesch, 1973; Jones and Holdich, 1983), which actually means nail or claw (Latin). This term is used for the homologous structure in isopods (Wilson, 1989) and insects; and as it cannot be confused, it must be the preferred term. A homologous structure is sometimes found on the tips of the cheliped dactylus and fixed LARSEN: STANDARDIZED TANAIDACEAN TERMINOLOGY 653 Fig. 7. Pereopod unguis. A, Not fused with dactylus to form a ‘‘claw’’ (Tanaella). B, Fused with dactylus to form a ‘‘claw’’ (Paratanais). finger. The one on the fixed finger was called a ‘‘tooth’’ by Shiino (1937). There really is no need for a different term for this structure, because it is just a thickening of the cuticle and thus homologous with the unguis of the pereopods. Furthermore, the term tooth is unfortunate because it can be confused with the processes and denticles on the margin of the fixed finger that are sometimes called ‘‘teeth.’’ The Proximal Uropodal and Pleopodal Article: Protopod, Peduncle, Sympodite, Basis, Basipodite, or Basal Article The proximal article of the uropod that connects the uropod to the pleotelson also has several terms in the literature. ‘‘Basis’’ is a term used by many authors (Lang, 1968; Bird and Holdich, 1984; Ishimaru, 1985; Bamber, 1990). Because ‘‘basis’’ means foundation, the term is literally correct. However, it remains to be shown that this article really is derived from the basis. It might be a coxa or a fused coxa/basis. The question also arises whether such terms should be applied to nonleg appendages at all; because coxa means ‘‘hip,’’ it relates to ‘‘legs.’’ The fact that this word has been applied to both the maxilliped and the cheliped is a different topic. The term ‘‘protopodite’’ was introduced by Shiino (1963), although he used peduncle in earlier publications, and ‘‘protopod’’ was used by Gardiner (1973) to alleviate this problem by considering this article to be, at least, either a coxa, a basis, or a fused coxa and basis. Protopod (¼ coxa þ basis) was therefore considered a more accurate term. However, this is homologous with standard crustacean terminology (as one reviewer pointed out) only if it really is a fusion of the coxa and basis. There is no way to tell, so this term does not solve the problem. Dojiri and Sieg (1997) introduced the term ‘‘sympodite’’ without justification. In a later review of the Tanaidacea (Guţu and Sieg, 1999), this term appeared again but was not consistently applied throughout that paper. Guţu does not seem to use the term in any later papers either. 654 JOURNAL OF CRUSTACEAN BIOLOGY, VOL. 23, NO. 3, 2003 Fig. 8. Setae and spines. A, Simple seta. B, Pinnate/pappose/plumose/sensory/setulose/broom seta. C, Serrated seta. D, Feather/plumose seta. E, Bipinnate/douple sided setulose seta. F, Pinnate/single sided setulated seta. G, Spiniform seta. H, Bifurcate seta. I, Leaf-shaped seta. J, Short flat seta. K, Coupling hook. L, Circumplumose seta. M, Spines. Fig. 9. Mancas. A, Manca I hatchling, after Bückle-Ramirez (1965). B, Manca II. C, Manca III. D, Juvenile. LARSEN: STANDARDIZED TANAIDACEAN TERMINOLOGY 655 Fig. 10. Appendage orientation. A, Ventral/dorsal for the animal in situ. B, Ventral/dorsal for the cheliped in situ. C, Ventral/dorsal for the pereopods in situ. D, The orientation of inner and outer relative to ventral and dorsal. ‘‘Peduncle’’ was used by a number of authors (Wolff, 1956; Lang, 1957; Müller, 1992; Edgar, 1997) as an analog to the part of the antennule, proximal to the separation of rami. This term may be applied but not without conflict. On biramous uropods, it is easy to distinguish between this article and other exo-endopod articles, but in uniramous uropods, it is not so obvious and we end up with the same problem as for the antenna. Because all tanaids have only one article proximal from the separation of the rami, it is here proposed to call this article the ‘‘basal article,’’ following the procedure for the antenna. Most of this paragraph applies to the proximal article of the pleopods as well. In case of uniramous pleopods (and uropods), it is generally accepted that the endopod is retained, and this term thus should be applied. Setae, Spines, and Cuticular Scales The long-standing discussion of what are considered spines and what are setae has caused significant damage to tanaidacean systematics as well as to the systematics of most other crustaceans. It is obvious that some tanaid workers (Sieg, 1986a; Guţu 1996; Bird, 1999) considered a thick seta as being a ‘‘spine,’’ while others did not (Viskup and Heard, 1989; Larsen 1999a; Bamber, 2000; Hansknecht et al., 2001) and still others were not consistent in their usage (Lang, 1968). Sieg (1986a, b) claimed that the presence of ‘‘spines’’ on certain articles of certain appendages was of major 656 JOURNAL OF CRUSTACEAN BIOLOGY, VOL. 23, NO. 3, 2003 Fig. 11. Application of terms for the pereopod orientation. A, Appendage orientation in situ according to the system of Sieg, 1977a, with the terms rostral/caudal applied. B, Appendage orientation in situ as seen in a tube-dwelling tanaidacean, with the terms inner/outer applied and how these conflict with the system of Sieg, 1977a. phylogenetic value and used this character to separate families. If a character is important systematically, then there must be agreement on its terminology or the character will be rendered useless. It is therefore easy to understand how the systematics has become unclear if the workers did not agree on how to define a ‘‘spine.’’ The issue is still debated, but there is a trend towards accepting the definitions based on homology put forward by Watling (1989). Setae are thus defined as elongated structures of rather variable shape that extend from a point under the cuticle and have innervation and articulation. Spines are extensions of the cuticle itself forming pointed structures. Spines are longer than wide at the base and are not innervated or articulated. Scales are cuticular projections without innervation and are broader at the base than long. To further complicate this issue, it has been observed that in larger (older?) specimens of Leptochelia, setae can become fused with the cuticle and lose their articulation (R. Heard, LARSEN: STANDARDIZED TANAIDACEAN TERMINOLOGY Fig. 12. The orientation of the mouthparts (generalized tanaid) seen from below. personal communication). Whether this loss includes innervation is yet to be determined. The Tanaidacea display a rich variety of more or less specialized setae, and it would waste space here to describe them all or to mention all the different names that have been applied to them. A short selection of the most common and important types are found in Fig. 8 with the most commonly used terms underlined in the caption. There is generally no need to standardize the many different descriptive terms authors have applied to setae. Although the terms describing specialized setae are not identical, they are usually descriptive enough to avoid misunderstanding. Mancas The manca stages have also been subjected to several different nomenclatures. Lang (1953b) used the term ‘‘manca I’’ for a free-living manca but omitted any remarks on the stage found only within the female marsupium. Bückle-Ramirez (1965), however, used the term ‘‘manca I’’ (Fig. 9A) for the newly hatched embryo, and this was followed by Sieg (1972). ‘‘Manca II’’ (Fig. 9B) was the term used for the individual newly released from the marsupium (Bückle-Ramirez, 1965). Messing (1981) observed that there is no ecdysis between these ‘‘manca I’’ and ‘‘manca II’’ and suggested that the manca I is better termed ‘‘lecithotrophic hatchling’’ or ‘‘early stage’’ of the ‘‘manca I’’ and that the newly released individual is really the manca I. The 657 difference between these two stages is so obvious that they must be given two different terms (ecdysis or not). It is clearly a problem to apply two different names without an ecdysis, but to apply the same term to these different forms would be an even bigger problem. Because both types have differentiated chelipeds and pereopods (Fig. 9A, B), it is hardly a larva in the sense of a nauplius, and this term should not be applied to any of these forms. The terminology and nomenclature of Bückle-Ramirez (1965) are thus workable, but I here propose the application of the suffix ‘‘hatchling’’ to the term ‘‘manca I,’’ while retaining the term ‘‘manca II’’ for the following stage. The term would be ‘‘manca I hatchling,’’ and this should eliminate most of the confusion. The manca II can then be defined as the newly released manca which does not yet possess pleopods, any traces of pereopod 6, and only a very reduced pereonite 6 of the same size as a pleonite. Manca III, on the contrary, does possess a fully developed pereonite 6 and a vestigal pereopod 6, but no pleopods. Juveniles have a fully developed pereopod 6 and pleopods, but these are vestigal and without setation. Note that most adult female deep-sea species lack pleopods and some possess rudimentary pleopods, but these usually do have some kind of setation. Orientation of Tanaidacean Appendage The terms ‘‘sternal’’ and ‘‘tergal’’ were originally synonymous with ‘‘ventral’’ and ‘‘dorsal,’’ and were intended to identify the margins of the chelipeds and pereopods as oriented on a live animal (Sieg, 1977a; Dojiri and Sieg, 1997). They are used extensively in recent tanaid literature. However, while Sieg’s application of sternal/tergal correctly correspond to ventral/dorsal for the cheliped, the opposite holds true for the pereopods (Fig. 10). Therefore, to use the terms tergal/sternal as synonymous with dorsal and ventral in this situation would be erroneous and confusing (Larsen and Rayment, 2002). It is proposed that the terms sternal and tergal be abandoned when describing the different margins of the tanaidacean appendage and that, instead, the terms dorsal/ ventral should be applied in the arrangement shown in Figs. 10B and 10C. This system would remain stable because this is the orientation in which all tanaidacean thoracopods are held in situ. The terms ‘‘rostral’’ and ‘‘caudal’’ were employed as synonyms to anterior and posterior 658 JOURNAL OF CRUSTACEAN BIOLOGY, VOL. 23, NO. 3, 2003 Table 2. Proposed standardized terminology in anterior to posterior direction. Origin Proposed standardized name Carput Antennule Carput Carput Carput Carput Carput Carput Carput Antenna Cephalothorax Carapace Labrum Mandibles Maxillule Maxilla Carput Thorax Thorax Thorax Labium Maxilliped Epignath Cheliped Subdivision Peduncle (including common article) and flagellum (in Apseudomorpha), inner and outer rami. Article number (in Neotanaidomorpha and Tanaidomorpha) Article number, inner rami, squama (in Apseudomorpha) Head, thoracomer 1, thoracomer 2 Occasionally divided into separate plates, covering the entire cephalothorax Incisor, lacinia mobilis, setal row, molar, palp Inner endite, outer endite, palp, terminal spiniform setae Inner and outer lobe of movable endite, inner and outer endite of fixed endite (in Apseudomorpha and Neotanaidomorpha) Palp, lobes, processes Coxa, basis, endites, palp Lobes, terminal seta True coxa (Apseudomorpha), pseudocoxa (Tanaidomorpha), sclerite (Neotanaidomorpha and Tanaidomorpha), basis, ischium (Neotanaidomorpha), merus, carpus, propodus, fixed finger, dactylus Thorax Pereonites 1—as many as are present Thorax Pereopods 1—as many as are present Coxa, basis, ischium, merus, carpus, propodus, dactylus, unguis Abdomen Pleonites 1—as many as are present Abdomen Pleopods 1—as many as are present Basal article, endopod, exopod Abdomen Pleotelson Abdomen Uropod Basal article, endopod, exopod N/A Appendix orientation Ventral/dorsal, inner/outer, proximal/distal sides on the cheliped and pereopods, assuming that the pereopods were held straight out from the body (Sieg, 1977a). It is informative to know which sides of the chelipeds face outwards, but the use of the terms ‘‘inner’’ and ‘‘outer’’ surface should be used, because the chelipeds are much more anteriorly directed than perpendicular to the body. For the pereopods, the situation is more complicated. The old system (Sieg, 1977a; Dojiri and Sieg, 1997) assumes that all pereopods are held in the same orientation (see Fig. 11A). However, most often the three anterior pairs of pereopods are held facing anteriorly, while the three posterior pairs are held facing posteriorly, particularly in tube-dwelling taxa (see Fig. 11B). Thus, the inner and outer surfaces of the posterior pairs are reversed relative to the side of the anterior pairs. Because the side of the limb facing outwards shares characters (in armament) with that side of the other limbs facing outwards, regardless of which side is facing anterior (if held perpendicular to the body), the system of Sieg (1977a) is not optimal. To overcome this problem, it is here proposed to apply, by convention, the terms ‘‘inner’’ and ‘‘outer’’ in the manner shown in Fig. 10D as modified from Sieg (1977a). For the mouthparts, a similar system is proposed. All the mouthparts are held in a ventral/dorsal manner in situ, and the paired mouthparts always face each other on the ‘‘inner’’ side and are anteriorly directed (Fig. 12). One is never in doubt about the orientation of the mouthparts. The only modification is that the labrum is as much ventrally as anteriorly directed, but this should cause little confusion. Articles, Joints, and Segments Several authors (G. O. Sars, 1896; Shiino, 1952) have used the term ‘‘segment’’ instead of ‘‘article,’’ and sometimes this term is used instead of ‘‘somite.’’ This seems not to have caused any confusion in the tanaidacean literature. However, Hansen (1913), Shiino (1937, 1951), and Sieg (1981) used the term ‘‘joints’’ instead of article, and this term may be confused with the actual joints (or articulations) between the articles, which was not what any author intended. This synonymy of joints and articles is undesirable. The consensus seems to be moving towards using the term ‘‘article’’ for the individual units of the tanaidacean appendage (Guţu, 1972; Bird and Holdich, 1984; Bamber, 1990; Larsen 1999a). DISCUSSION A common terminology is essential for understanding the homologies necessary for conducting any phylogenetic analysis. Therefore, this suggested terminology is based mainly LARSEN: STANDARDIZED TANAIDACEAN TERMINOLOGY on homology. A standardized terminology is proposed in Table 2 for all tanaidacean somites, appendages, and their articles, as well as orientations. It is not expected that every worker on the Tanaidacea will uncritically adopt this proposed terminology and nomenclature. Rather, the object of this paper is to clarify the terminology and to identify the problem that several different terminologies and nomenclatures have been employed. If tanaid specialists could be inspired to include a section in their publications about which terminology they adhere to, much confusion could be avoided. Particularly, those workers new to the fascinating group of Tanaidacea would benefit tremendously from such a change in behavior. ACKNOWLEDGEMENTS The funding for this project was provided by the BP Deep-Sea Biodiversity Fellowship, hosted by the Department of Oceanography, Texas A. and M. University. Part of the work took place at the Gulf Coast Research Laboratory, and my thanks are extended to this institution. I am grateful for critical reading of the manuscript by Dr. Fain Hubbard and thankful to several colleagues for productive (and sometimes heated) discussions on the subject. LITERATURE CITED Băcescu, M. 1980. Contribution to the knowledge of some Kalliapseudidae (Crustacea, Tanaidacea) from the NW of the Indian Ocean.—Travaux du Muséum d’Histoire Naturelle ‘‘Grigore Antipa’’ 22: 335–939. ———. 1987. Abyssal Apseudomorpha (Crustacea, Tanaidacea) of NW Madagascar.—Travaux du Muséum d’Histoire Naturelle ‘‘Grigore Antipa’’ 29: 19–33. Bamber, R. N. 1990. A new species of Zeuxo (Crustacea: Tanaidacea) from the French Atlantic coast.—Journal of Natural History 24: 1587–1596. ———. 1998. Tanaidaceans (Crustacea, Peracarida) from the Southeast of the South China Sea.—Asian Marine Biology 15: 169–197. ———. 2000. New peracarids (Crustacea; Malacostraca) from the Atlantic Deep Sea off Angola.—Species Diversity 5: 317–328. Barnard, K. H. 1935. Report on the Amphipoda, Isopoda and Tanaidacea in the collection of the Indian Museum.— Records of the Indian Museum 37: 279–319. Bate, C. S. 1856. On the British Edriophtamalma.—British Association for the Advancement of Science, Report for 1855: 18–62. Bird, G. J. 1999. A new species of Pseudotanais (Crustacea, Tanaidacea) from the cold seeps in the deep Caribbean, collected by the French submersible ‘‘Nautile’’.—Zoosystema 21: 445–451. ———, and D. M. Holdich. 1984. New deep-sea leptognathiid tanaids (Crustacea, Tanaidacea) from the northeast Atlantic.—Zoologica Scripta 13: 285–315. Blanc, H. 1884. Contribution a l’histoire naturelle des asselotes heteropteres. Observations faites sur la Tanais oerstedii Krøyer.—Recordes des Zoologie Suisse 1: 189–258. 659 Boesch, D. F. 1973. Three new Tanaids (Crustacea, Tanaidacea) from southern Queensland.—Pacific Science 27: 168–188. Bückle-Ramirez, L. F. 1965. Unterschungen über die Biologie von Heterotanais oerstedi (Krøyer).—Zeitchrift für Morphologie und Ökologie der Tiere 55: 711–782. Claus, C. 1884. Über Apseudes latreilli M. Edw. und die Tanaiden, II.—Arbeiten aus dem Zoologischen Instituten der Universität Wien 5: 319–332. Dennell, R. 1937. On the feeding mechanism of Apseudes talpa, and the evolution of the Peracarida.—Transcriptions of the Royal Society of Edinburgh 59: 57–78. Dojiri, M., and J. Sieg. 1997. The Tanaidacea. Pp. 181–278 in J. A. Blake and P. H. Scott, eds. Taxonomic Atlas of the Benthic Fauna of the Santa Maria Basin and Western Santa Barbara Channel. 11 – The Crustacea. Part 2 The Isopoda, Cumacea and Tanaidacea. I–V. Santa Barbara Museum of Natural History, Santa Barbara. Edgar, G. 1997. A new genus and three new species of Apseudomorpha Tanaidacean (Crustacea) from the Darwin region. Pp. 279–299 in J. R. Hanley, G. Caswell, D. Megirian, and H. K. Larson, eds. Proceedings of the Sixth International Marine Biological Workshop. The marine flora and fauna of Darwin Harbour, Northern Territory, Australia. Museum and Art Galleries of the Northern Territory and the Australian Marine Science Association: Darwin, Australia 1997. Gamo, S. 1984. A new remarkably giant tanaid, Gigapseudes maximus sp. nov. (Crustacea) from abyssal depths far off southeast of Mindanao, the Philippines.— Scientific Reports of Yokahoma Natural University Series 11: 1–12. Gardiner, L. F. 1973. Calozodion wadei, a new genus and species of apseudid tanaidacean (Crustacea) from Jamaica.— Journal of Natural History 7: 499–507. ———. 1975. The systematics, postmarsupial development, and ecology of the deep-sea family Neotanaidae (Crustacea: Tanaidacea).—Smithsonian Contributions to Zoology 170: 1–265. Guţu, M. 1972. Phylogenetic and systematic considerations upon the Monokonophora (Crustacea, Tanaidacea) with the suggestion of a new family and several new subfamilies.—Revue Roumaine de Biologie (Biologie Animale) 17: 297–305. ———. 1975. Carpoapseudes basescui n.sp and C. menziesi n.sp (Crustacea–Tanaidacea) from the PeruChile trench.—Revue Roumaine de Biologie (Biologie Animale) 20: 93–100. ———. 1996. Tanaidaceans (Crustacea, Peracarida) from Brazil, with descriptions of new taxa and some systematic remarks of several families.—Travaux du Muséum d’Histoire Naturelle ‘‘Grigore Antipa’’ 36: 23–133. ———. 1998. Description of three new species of Tanaidacea (Crustacea) from the Tanzanian coast.— Travaux du Muséum d’Histoire Naturelle ‘‘Grigore Antipa’’ 38: 259–327. ———, and J. Sieg. 1999. Odres des Tanaı̈dacés.— Mémoires de l’Institut océanographique, Monaco 19: 353–389. Hansen, H. J. 1913. Crustacea, Malacostraca. II.—Danish Ingolf Expedition 3: 1–127. ———. 1925. Studies on the Anthropoda. Vol 2. On the Comparative Morphology of the Appendages in the Arthropoda. A. Crustacea. Gyldendalske boghandel. Copenhagen. 80 pp. Hansknecht, T., R. W. Heard, and R. Bamber. 2002. Tanapseudes gutui, a new species of apseudomorphan 660 JOURNAL OF CRUSTACEAN BIOLOGY, VOL. 23, NO. 3, 2003 Tanaidacea (Crustacea: Peracarida) from the Caribbean Sea and the taxonomic status of the family Tanapseudidae Băcescu, 1978.—Gulf and Caribbean Research 14: 67–74. ———, ———, and J. W. Martin. 2001. Saltipedis navassensis, a new species of apseudomorph tanaidacean (Crustacea: Peracarida: Parapseudidae) from the tropical northwestern Atlantic.—Zootaxa 18: 1–11. Holdich, D. M., and J. A. Jones. 1983. British Tanaids. Synopsis of the British Fauna. 27. Cambridge University Press, Cambridge. 95 pp. Ishimaru, S.-i. 1985. A new species of Leptochelia (Crustacea, Tanaidacea) from Japan, with a redescription of L. savignyi (Krøyer, 1842).—Publications from the Seto Marine Laboratory 30: 241–267. Johnson, S. B., and Y. G. Attramadal. 1982a. A functionalmorphological model of Tanais cavolinii Milne-Edwards (Crustacea, Tanaidacea) adapted to a tubicolous lifestrategy.—Sarsia 67: 29–42. ———, and ———. 1982b. Reproductive behaviour and larval development of Tanais cavolinii Milne-Edwards (Crustacea, Tanaidacea).—Marine Biology 71: 11–16. Jones, J. A., and D. M. Holdich. 1983. A new species of the tanaid genus Tanaissus Norman & Scott from British waters.—Crustaceana 45: 214–219. Lang, K. 1953a. Apseudes hermaphroditicus n. sp. A hermaphroditic tanaid from the Antarctic.—Arkiv för Zoologi 2: 341–350. ———. 1953b. The postmarsupial development of the Tanaidacea.—Arkiv för Zoologi 2: 409–422. ———. 1957. Tanaidacea from Canada and Alaska.— Contribution du Départment des Pêcheries, Québec 52: 1–54. ———. 1968. Deep-sea Tanaidacea.—Galathea Reports 9: 23–209. ———. 1971. Taxonomische und phylogenetische Untersuchungen über die Tanaidaceen. 6. Revision der Gattung Paranarthrura Hansen, 1913 und Aufstellung von zwei neuen Familien, vier neuen Gattungen und zwei neuen Arten.—Arkiv för Zoologi 2: 361–401. Larsen, K. 1999a. Deep-sea tanaidacean (Crustacea: Peracarida) from the ‘‘Albatross’’ cruises 1885–86, with keys to the suborder Neotanaidomorpha.—Journal of Natural History 33: 1107–1132. ———. 1999b. A new species of the deep-sea genus Carpoapseudes (Crustacea: Tanaidacea) from southwestern Atlantic.—Zoosystema 21: 647–659. ———. 2000. Revision of the genus Collettea (Crustacea: Tanaidacea).—Invertebrate Taxonomy 14: 681–693. ———. 2001. Morphological and molecular investigation of polymorphism and cryptic species in tanaid crustaceans: implications for tanaid systematics and biodiversity estimates.—Zoological Journal of the Linnean Society 131: 353–379. ———. 2002. Tanaidacea (Crustacea: Peracarida) of the Gulf of Mexico, X: The question of being male.—Gulf and Caribbean Research 14: 53–66. ———, and H. Rayment. 2002. New species of Leptochelia (Crustacea: Tanaidacea) from the Andaman Sea, Northeastern Indian Ocean.—Phuket Marine Biological Center, Special Publication 23: 17–31. ———, and G. D. F. Wilson. 1998. Tanaidomorphan systematics—Is it obsolete?—Journal of Crustacean Biology 18: 346–362. ———, and ———. 2002. Tanaidacean phylogeny. The first step: the superfamily Paratanaidoidea.—Journal of Zoological Systematics and Evolutionary Research 40: 205–222. Lauterbach, K. E. 1970. Der Cephalothorax von Tanais cavolinii Milne-Edwards (Crustacea-Malacostraca), ein Beitrag zur vergleichenden Anatomie und Phylogenie der Tanaidacea.—Zoologische Jahrbücher, Abteilung für Anatomie und Ontogenie der Tiere 87: 94–204. McLaughlin, P. 1980. Comparative Morphology of Recent Crustacea. W. H. Freeman and Co., San Francisco. 159 pp. McSweeny, E. S. 1982. A new Pagurapseudes (Crustacea: Tanaidacea) from southern Florida.—Bulletin of Marine Science 32: 455–466. Messing, C. G. 1977. Neotanais persephone, a new species of hadal Tanaidacea (Crustacea: Peracarida).—Bulletin of Marine Science 27: 511–519. ———. 1981. Notes on recent changes in tanaidacean terminology.—Crustaceana 41: 98–101. Meyer, G., and R. W. Heard. 1989. Tanaidacea (Crustacea: Peracarida) of the Gulf of Mexico. VII. Atlantapseudes lindae, n. sp. (Apseudidae) from the continental slope of the northern Gulf of Mexico.—Gulf Research Reports 8: 67–105. Monod, T. 1935. Contribution á l’étude faunistique de la reserve naturelle du Manampetsa. Crustacés.—Annales de Societe Scientifique Naturelle Zoologie Series 18: 449–466. Müller, H. G. 1992. Tanzanapseudes polynesiensis n. sp. first species of Tanzanapseudinae from the Pacific (Crustacea: Tanaidacea: Metapseudidae).—Cahiers Biologie Marine 33: 191–108. Norman, A. M., and T. R. R. Stebbing. 1886. On the Crustacea Isopoda of the ‘‘Lightning,’’ ‘‘Porcupine,’’ and ‘‘Valorous’’ Expeditions.—Transactions of the Zoological Society of London 12: 77–141. Pring, J. T. 1982. Oxford Greek Dictionary, Second edition. Oxford University Press, Oxford. 572 pp. Sars, G. O. 1896. Isopoda. Parts I and II. Apseudidae, Tanaidae.—An Account of the Crustacea of Norway with short descriptions and figures of all the species II: 1–40. Scholl, G. 1963. Embryologische Untersuchungen an Tanaidaceen (Heterotanais oerstedi Krøyer).—Zoologischer Jarhbuche (Anatomie) 80: 500–554. Shiino, S. M. 1937. On Apseudes nipponicus n. sp. (Crustacea Tanaidacea).—Annotations Zoologicae Japonenses 16: 53–62. ———. 1951. On two new species of the Family Apseudidae found at Seto.—Report of Faculty of Fisheries, Prefectural University of Mie 1: 11–25. ———. 1952. A new genus and two new species of the order Tanaidacea found at Seto.—Publications from the Seto Marine Biological Laboratory II: 53–68. ———. 1963. Tanaidacea collected by ‘‘Naga’’ Expedition in the Bay of Nha-Trang, South Viet-Nam.—Report of Faculty of Fisheries, Prefectural University of Mie 4: 437–507. ———. 1965. Tanaidacea from the Bismarck Archipelago.—Videnskabelige Meddelser fra Dansk Naturhistorisk Forening (Noona Dan Papers 17) 128: 177–203. ———. 1968. A tanaid crustacean, Nesotanais lacustris gen. et sp. nov. from Lake Tegano, Rennell Islands.— Natural History of the Rennell Islands and British Solomon Islands 5: 153–168. ———. 1978. Tanaidacea collected by French scientist on board the survey ship ‘‘Marion Dufresne’’ in the regions around the Kerguelen Islands and other LARSEN: STANDARDIZED TANAIDACEAN TERMINOLOGY subantarctic islands in 1972, ’74, ’75, ’76.—Scientific Reports of the Shima Marineland 5: 1–122. Sieg, J. 1972. Untersuchungen über Tanaidaceen.—Kieler Meeresforschungen 28: 232–236. ———. 1973 Ein Beitrag zum natürlichen System der Dikonophora Lang. Unpublished Thesis, Kiel University. 298 pp. ———. 1976a. Zum natürlichen System der Dikonophora Lang (Crustacea, Tanaidacea).—Zeitschrift für Zoologischer Systematik und Evolutionsforschung 14: 177–198. ———. 1976b. Crustacea Tanaidacea, gesammelt von Professor Dr. W. Noodt an der kuesten El Salvador und Peru.—Studies on the Neotropical Fauna and Environment 11: 65–85. ———. 1977a. Taxonomische Monographie der Familie Pseudotanaidae (Crustacea, Tanaidacea).—Mitteilungen aus dem Zoologischen Museum Berlin 53: 1–109. ———. 1977b. Eine neue Gattung (Heterotanaoides gen. n.) aus der familie Paratanaidae Lang (Tanaidacea).—Crustaceana 33: 203–209. ———. 1980. Revision der Gattung Nototanais Richardson, 1906 (Crustacea, Tanaidacea).—Mitteilungen Aus dem Zoologischen Museum Berlin 56: 45–71. ———. 1981. A new species of the genus Paratanais (Crustacea: Tanaidacea), P. spinanotandus from Seamount Vema.—Proceedings of the Biological Society of Washington 94: 1271–1278. ———. 1984. Neuere Erkenntnisse zum natürlichen System der Tanaidacea. Eine phylogenetische Studie.—Zoologica 136: 1–132. ———. 1986a. Crustacea Tanaidacea of the Antarctic and Subantarctic. 1. On material collected at Tierra del Fuego, Isla de los Estados, and the west coast of the Antarctic peninsula.—Biology of the Antarctic Seas 45: 1–180. ———. 1986b. Tanaidacea (Crustacea) von der Antarktis und Subantarktis. II. Tanaidacea gesammelt von Dr. J.W. Wägele während der Deutschen Antarktis Expedition 1983.—Mitteilungen aus der Zoologischen Museum der Universität Kiel 2: 1–80. ———, R. W. Heard, and J. T. Ogle. 1982. Tanaidacea (Crustacea: Peracarida) of the Gulf of Mexico. II. The occurrence of Halmyrapseudes bahamensis Băcescu and Guţu, 1974 (Apseudidae) in the eastern Gulf with 661 redescription and ecological notes.—Gulf Research Reports 7: 105–113. Siewing, R. 1951. Besteht eine engere Verwandstschaft zwischen Isopoden und Amphipoden?—Zoologischer Anzieger 147: 166–180. ———. 1953. Morphologische Untersuchungen an Tanaidaceen und Lophogastriden.—Zeitschrift für Wissenshaft (Zoologie) 157: 333–426. ———. 1957. Anatomie und Histologie von Thermosbaena mirabilis. Ein Beitrag zur Phylogenie der Reihe Pancarida (Thermosbaenacea).—Abhandlungen der Akademien für Wissenshaft und Literatur Mainz (Matematische und Zoologische Klassen) 7: 195–270. Stebbing, T. R. R. 1893. A History of Crustacea: Recent Malacostraca. Paul, Trench, Trueber and Co., London. 466 pp. Tattersall, W. M. 1925. New Tanaidacean and Isopods from the West Coast of Africa.—Bulletin Société Sciences Naturelles du Maroc 5: 77–84. Viskup, B. A., and R. W. Heard. 1989. Tanaidacea (Crustacea: Peracarida) of the Gulf of Mexico. VII. Pseudosphyrapus siegi, n.sp. (Sphyrapidae) from the continental slope of the northern Gulf of Mexico.—Gulf Research Reports 8: 107–115. Watling, L. 1989. A classification system for crustacean setae based on the homology concept. Pp. 15–27 in B. E. Felgenhauer, L. Watling, and A. B. Thistle, eds. Functional Morphology of Feeding and Grooming. Crustacean Issues 6. Whitelegge, T. 1901. Scientific results of the trawling expedition of H.M.C.S. ‘‘Thetis’’ on the coast of New South Wales. (Crustacea Part II; Isopoda Part I).— Memoirs of the Australian Museum 4: 203–225. Wilson, G. D. F. 1989. A systematic revision of the deep-sea subfamily Lipomerinae of the isopod crustacean family Munnopsidae.—Bulletin of the Scripps Institution of Oceanography 27: 1–138. Wolff, T. 1956. Crustacea Tanaidacea from depths exceeding 6000 meters.—Galathea Reports 2: 187–241. Zimmer, C. 1927. Crustacea. Pp. 277–304 in W. Kükennthal and T. Krumbach, eds. Handbuche der Zoologie 3. RECEIVED: 10 September 2002. ACCEPTED: 20 January 2003.
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