http://www.collembola.org/publicat/crustacn.htm - Last updated on 2006.02.20 by Frans Janssens
Checklist of the Collembola: Are Collembola terrestrial Crustacea?

Peter Nolan Lawrence, 9 Weald Close, Bromley Common, Kent, BR2 9PD, UK
Frans Janssens, Department of Biology, University of Antwerp (RUCA), Antwerp, B-2020, Belgium

Introduction

Although morphological features of Collembola do not support a close relationship with Crustacea, the molecular evidence for a 'crustacean-like' ancestor of Collembola and other 'hexapods' is compelling (Hopkin, 1997:21-22).
Traditionally, a semi-aquatic origin of Collembola has been proposed (Shear & Kukalová-Peck 1990, 1991 cited from D'Haese 2002:1143).
Hopkin (1997:26) presents the following random list of events that may have taken place during the evolution of terrestrial Collembola from a hypothetical aquatic, many-segmented, many-legged, crustacean-like ancestor:
- the second antennae were lost as they were no longer needed for swimming (as occured also in oniscidian isopods in their transition to land).
- the number of segments was reduced until only the head and the three thoracic and six abdominal segments remained.
- the legs on the thoracic segments were retained.
- the legs of the fourth abdominal segment were modified to form the furca.
- the legs of the third abdominal segment were reduced and became the tenaculum that holds the furca in rest position.
- the legs of the first abdominal segment developed thiny-walled vesicles and evolved into the ventral tube.
- the legs on the second, fifth and sixth abdominal segments were suppressed.

However, D'Haese (2002:1150) rejects the semi-aquatic origin of Collembola. The semi-aquatic lifestyle is a secondary acquisition that occured several times independently in the evolution of Collembola. An edaphic lifestyle is the ancestral state.

While there is consensus that Arthropoda is monophyletic, there is none on the relationships of its subordinates. Almost every possible alternative has been offered (Giribet & Ribera, 2000:205):
Arthropoda = Chelicerata + Mandibulata (Crustacea + Atelocerata (Myriapoda + Hexapoda)) according to Snodgrass, 1938; Weygoldt, 1979; Wågele, 1993; Wheeler et al., 1993; Wheeler, 1995, 1998 (cited from Giribet & Ribera, 2000:205).
Arthropoda = Chelicerata + Mandibulata (Myriapoda + Pancrustacea (Crustacea + Hexapoda)) according to Giribet et al., 1996; Giribet & Ribera, 1998; Zrzavy et al., 1998 (cited from Giribet & Ribera, 2000:205).
Arthropoda = (Chelicerata + Myriapoda) + Pancrustacea (Crustacea + Hexapoda) according to Turbeville et al., 1991; Friedrich & Tautz, 1995; Giribet et al., 1996 (cited from Giribet & Ribera, 2000:205); Dove & Stollewerk, 2003.
Arthropoda = Schizoramia (Chelicerata + Crustacea) + Atelocerata (Myriapoda + Hexapoda) according to Cisne, 1974; Briggs et al., 1992; Budd, 1993 (cited from Giribet & Ribera, 2000:205).

Many studies unite Crustacea and Atelocerata in the Mandibulata (Snodgrass, 1938; Weygoldt, 1979; Wågele, 1993; Wheeler et al., 1993; Wheeler, 1995,1998; Giribet et al., 1996; Giribet & Ribera, 1998; Zrzavy et al., 1998). Others align Crustacea with Chelicerata in the Schizoramia (Cisne, 1974; Briggs et al., 1992; Budd, 1993). Supporters of Mandibulata do not agree whether Atelocerata is monophyletic and sister of Crustacea (the traditional and majority position), or whether Crustacea is sister of Hexapoda (the Pancrustacea hypothesis). For a comprehensive overview of the rival hypotheses, see Giribet & Ribera (2000:222-225). Given the conflicting morphological (Atelocerata), molecular (Pancrustacea) and paleontological (Schizoramia) hypotheses, only a simultaneous analysis of all data from extinct and extant taxa might offer a solution (Giribet, Edgecombe & Wheeler, 1999:197).

Any direct relationship between Hexapoda and Myriapoda is becoming more and more doubtful and therefore the polyphyly of Atelocerata seems increasingly certain (Dove & Stollewerk, 2003). As more nuclear, mitochondrial gene order and protein-encoding gene data have been examined for an ever-wider set of taxa, little or no support has been found for any of the possible groupings alternative to Pancrustacea (Cranston & Gullan, 2003:883). In this paper, we will question whether or not Collembola are Insecta, Hexapoda or Crustacea within the context of the Pancrustacea theory. Hexapody originated at least twice independantly in Arthropoda, making the Hexapoda paraphyletic (Nardi et al., 2003). We will show that Collembola are not so called primitive apterous insects, but a unique and ancient group of well adapted terrestrial crustaceans.

Paleontological considerations

Fig.r. Rhyniella praecursor
After Scourfield (1940).
Based on the discovery of the fossil collembolan Rhyniella praecursor by Hirst & Maulik in the Devonian chert beds in Scotland in 1926, and the striking resemblance it shows with extant species, Tillyard (1928) concludes that Collembola are primary, ancestral, and archaic terrestrial arthropodans and not forms readapted by retrograde evolution as claimed by Handlirsch (1908) (cited from Handschin, 1955:41,49).
Rhyniella praecursor Hirst & Maulik, 1926 has been assigned to different families, respectively to Poduridae (Poduromorpha) by Tillyard (1928), to Entomobryomorpha, possibly Protentomobryidae by Scourfield (1940), to Rhyniellidae by Paclt (1956), to Protentomobryidae by Salmon (1964), to Neanuridae by Massoud (1967), and to Isotomidae by Greenslade & Whalley 1986:320.
Crowson (1985) questioned whether or not the Rhyniella fossils are recent contaminations, because of the finding of a thysanopteran nymph in the deposit which was clearly a later contaminant. However it has been shown that the Collembola are securely embedded in the rock and that there was only a single phase of mineralisation (Whalley & Jarembowski, 1981 cited from Greenslade & Whalley 1986:319). Most recent dating using argon/argon techniques have confirmed the chert as being over 400 million years old (Greenslade & Whalley 1986:319).
Direct fossil evidence of Collembola before the Devonian is lacking (Lehmann & Hillmer, 1983 cited from Hopkin, 1997:23).
The discovery of coprolites (fossil faeces) in Upper Silurian rocks of 412 million years in age, which could be derived from springtails, suggests that Collembola were an important component of the earliest terrestrial ecosystems (Edwards, Selden, Richardson & Axe, 1995 cited from Hopkin, 1997:23).

Hexapody did not evolve as an adaptation to terrestrial locomotion, but was already developed in the marine habitat, as demonstrated by the ectognathous marine hexapod Devonohexapodus bocksbergensis from the Lower Devonian Hunsrück Slates (Haas, Waloszek & Hartenberger, 2003:39,46). This finding demonstrates that stem lineage Insecta coexisted during the Devonian with the more derived Collembola (Haas, Waloszek & Hartenberger, 2003:52). Cambronatus brasseli and Wingertshellicus backesi from the Lower Devonian, are described by Briggs & Bartels (2001) as "crustaceanomorphs", while Haas, Waloszek & Hartenberger (2003:49) suggest a close relationship to Hexapoda. The marine Tesnusocaris goldichi Brooks, 1955, from the Carboniferous, redescribed by Emerson & Schram (1991) as a representative of the Remipedia, is condsidered to be more close to Hexapoda by Haas, Waloszek & Hartenberger (2003:49).

Reinterpretation of a fossil insect fragment Rhyniognatha hirsti Tillyard, 1928 from the early Devonian Rhynie cherts of Scotland indicates that insects originated in the Silurian period (Engel & Grimaldi, 2004:627-630). This is supported by the fossil records of Archaeognatha (= Microcoryphia) that have been listed from the early Devonian of Quebec (Labandeira & al., 1988 cited from Bach de Roca, Gaju-Ricart & Compte-Sart, 1999:387) and from the Devonian of New York (Shear & al., 1984 cited from Bach de Roca, Gaju-Ricart & Compte-Sart, 1999:387), suggesting a parallel evolution of Insecta and Collembola. Rhyniella praecursor Hirst & Maulik, 1926, the oldest known collembolan fossil from the Devonian red sandstone Rhynie chert beds, Scotland, resembles extant Collembola up to such an extent that this might be an indication that Collembola reached their evolutionary climax already 400 million years ago. Therefore, Handschin (1955:49) considers Collembola as living fossils.

Systematic overview

Pancrustacea
Crustacea Hexapoda (= Insecta sensu Leach, 1815)
Apterygota (Pterygota)
Entognatha Insecta sensu Handschin, 1958 (= Ectognatha sensu Hennig, 1953)
Monocondylia Dicondylia
Ellipura Diplura Thysanura sensu Lameere, 1895 Pterygota
Collembola Protura Archaeognatha Zygentoma
Tab.I. Conventional classifications of related and higher taxa of Collembola,
in perspective of the Pancrustacea theory.
(Monophyletic taxa in bold. Paraphyletic assemblages not in bold)

Historically, single morphological character systems formed the basis for organising the hexapods into groups (Carpenter & Wheeler, 1999:333,344). Since the characters taken into account in such studies are independent of each other, each study results in a different phylogeny. Combining sets of independent characters into one study is the approach of the 'total evidence' of Kluge (1989) and 'simultaneous analysis' of Nixon and Carpenter (1996) to maximise parsimony of the tree (Carpenter & Wheeler, 1999:333,344). Given the high number of characters involved, a numerical cladistic analysis will simplify the work. Computer assisted analyses allow for combining a hugh amount of characters (morphological, molecular, ecological, physiological, etc.) to be taken into account simultaneously, allowing in this way simultaneous treatment of all available evidence. In the following discussion, the single character based groupings that lead to taxonomic units used in the systematic classifications are questioned by integrating manually the result of many single and multiple character studies in an attempt to confront the different opinions preliminary.

Are Collembola Ellipura?

Ellipura Börner, 1910 = Collembola + Protura.
Parainsecta Kukalová-Peck, 1991 (cited from Bach de Roca, Gaju-Ricart & Compte-Sart, 1999:387) = Ellipura Börner, 1910.

Are Collembola Entognatha?

Entognathi(sic) von Stummer-Traunfels, 1891 (cited from Börner, 1901:3,11) = Collembola + Entotrophi(=Diplura)
Entognatha Snodgrass, 1938 (cited from Wheeler, Whiting, Wheeler & Carpenter, 2001:114) = Collembola + Protura + Diplura
Entognatha Imms, 1948:221 nec von Stummer-Traunfels, 1891 = Diplura
Entognatha Kukalová-Peck, 1991 (cited from Bach de Roca, Gaju-Ricart & Compte-Sart, 1999:387) nec von Stummer-Traunfels, 1891 = Diplura
Entognatha Kukalová-Peck, 1998 (cited from Bach de Roca, Gaju-Ricart & Compte-Sart, 1999:393) nec von Stummer-Traunfels, 1891 = Diplura
Entognatha Koch, 1997 (cited from Bach de Roca, Gaju-Ricart & Compte-Sart, 1999:393) nec von Stummer-Traunfels, 1891 = Diplura
Entognatha Koch, 1998 (cited from Bach de Roca, Gaju-Ricart & Compte-Sart, 1999:393) nec von Stummer-Traunfels, 1891 = Diplura

Are Collembola Apterygota?

Apterygota Lang, 1889 (cited from Imms, 1948:211) = Collembola + Thysanura(=Diplura+Archaeognatha+Zygentoma).
Apterygota Imms, 1948:213 = Apterygota Lang, 1889 + Protura.
Apterygota Kukalová-Peck, 1991 (cited from Bach de Roca, Gaju-Ricart & Compte-Sart, 1999:387) nec Lang, 1889 = Zygentoma.

Are Collembola Insecta?

Insecta Linnaeus, 1758 (cited from Kluge, 1999:348,369) = Arthropoda von Siebold & Stannius, 1848.
Amyocerata Remmington, 1955 (cited from Kluge, 1999:348,369) = Triplura(=Archaeognatha+Zygentoma) + Pterygota.
Insecta Handschin, 1958 (cited from Kluge, 1999:348,369) nec Linnaeus, 1758 = Amyocerata Remmington, 1955.
Insecta Kukalová-Peck, 1987 (cited from Giribet, Edgecombe & Wheeler, 1999:203) nec Linnaeus, 1758 = Insecta Handschin, 1958 + Diplura.
Insecta Kukalová-Peck, 1991 (cited from Bach de Roca, Gaju-Ricart & Compte-Sart, 1999:387) nec Linnaeus, 1758 = Insecta Kukalová-Peck, 1987 + Monura.
Insecta Kristensen, 1991 (cited from Bach de Roca, Gaju-Ricart & Compte-Sart, 1999:389) nec Linnaeus, 1758 = Kukalová-Peck, 1991 - Diplura.

Are Collembola Hexapoda?

Hexapoda Blainville, 1816 (cited from Kluge, 1999:348,369) = Insecta Leach, 1815 nec Linnaeus, 1758.
Hexapoda Koch, 1997 (cited from Bach de Roca, Gaju-Ricart & Compte-Sart, 1999:391) = Insecta Kukalová-Peck, 1987 + Collembola + Protura.
Insecta Larink, 1997 (cited from Bach de Roca, Gaju-Ricart & Compte-Sart, 1999:391) nec Linnaeus, 1758 = Insecta Kukalová-Peck, 1991 + Collembola + Protura.
Insecta Buckley & Cunningham, 2002:395,399

Are Collembola Crustacea?

Are Collembola Pancrustacea?

Exploring possible extra-pancrustacean ancestries of Collembola:

Do Collembola share characters with Arachnata?

Applying the Pancrustacea hypothesis to the definition of Arthropoda according to Cisne, 1974; Briggs et al., 1992; Budd, 1993 (cited from Giribet & Ribera, 2000:205): Myriapoda + Schizoramia (Arachnata + Pancrustacea), we will now summarise some arachnomorph characters in Collembola.

Discussion

Conventional hypothesis: Collembola are basal Hexapoda.
Pancrustacea
Crustacea
Hexapoda s.l.
Collembola Protura Diplura Insecta s.s. (= Ectognatha)
Archaeognatha
(= Monocondylia)
Dicondylia
Zygentoma Pterygota
Tab.II. Classification of related and higher taxa of Collembola.


		+---------- Insecta s.s. 
	     +--+
	     |  +---------- Diplura
	  +--+
	  |  |  +---------- Protura
	  |  +--+
	  |     +---------- Collembola
       +--+
       |  +---------------- Crustacea
    +--+
    |  |     +------------- Arachnida
    |  +-----+
 ---+        +------------- Xiphosura
    |
    +---------------------- Myriapoda

Fig.1. Simplified scheme of the systematic position of
Collembola in the Arthropoda
(conventional phylogeny)

Alternative hypothesis: Collembola are terrestrial Crustacea.
Pancrustacea
Crustacea s.l.
Hexapoda s.s.
Crustacea
s.s.
Collembola Protura Diplura Insecta s.s. (= Ectognatha)
Archaeognatha
(= Monocondylia)
Dicondylia
Zygentoma Pterygota
Tab.III. Classification of related and higher taxa of Collembola.
(modified after Shao, Zhang, Ke, Yue & Yin, 2000)


		    +------ Hexapoda s.s. 
		    |
	     +------------- Collembola
	     |      |
       +-----+------+------ Crustacea
    +--+
    |  |     +------------- Arachnida
    |  +-----+
 ---+        +------------- Xiphosura
    |
    +---------------------- Myriapoda

Fig.2. Simplified scheme of the systematic position of
Collembola in the Arthropoda
(modified after Shao, Zhang, Ke, Yue & Yin, 2000)

Alternative hypothesis 2: Collembola are terrestrial basal Crustacea.
Pancrustacea
Crustacea s.l.
Hexapoda s.s.
Crustacea
in pars
(Branchiopoda)
Collembola
Crustacea
in pars
(Malacostraca)
Protura Diplura Insecta s.s. (= Ectognatha)
Archaeognatha
(= Monocondylia)
Dicondylia
Zygentoma Pterygota
Tab.IV. Classification of related and higher taxa of Collembola.
(modified after Spears & Abele, 1997 cited from Lange & Schram, 1999; Aleshin & Petrov, 1999; Gibiret & Ribera, 2000:213,215,216,217,218)


		     +----- Hexapoda s.s. 
		     |
		 +---+----- Crustacea partim 
		 |
	     +------------- Collembola
	     |   |
       +-----+---+--------- Crustacea partim 
    +--+
    |  |     +------------- Arachnida
    |  +-----+
 ---+        +------------- Xiphosura
    |
    +---------------------- Myriapoda

Fig.3. Simplified scheme of the systematic position of
Collembola in the Arthropoda
(modified after Spears & Abele, 1997
cited from Lange & Schram, 1999; Aleshin & Petrov, 1999;
Gibiret & Ribera, 2000:213,215,216,217,218)

New hypothesis: Collembola are terrestrial basal Pancrustacea.
Pancrustacea
Collembola
Crustacea
Hexapoda s.s.
Protura Diplura Insecta s.s. (= Ectognatha)
Archaeognatha
(= Monocondylia)
Dicondylia
Zygentoma Pterygota
Tab.V. Classification of related and higher taxa of Collembola.
(modified after Aleshin & Petrov, 1999:184,185; Gibiret & Ribera, 2000:214; Nardi et al., 2003)


	     +------------- Hexapoda s.s. 
	  +--+
	  |  +------------- Crustacea
       +--+
       |  +---------------- Collembola
    +--+
    |  |     +------------- Arachnida
    |  +-----+
 ---+        +------------- Xiphosura
    |
    +---------------------- Myriapoda

Fig.4. Simplified scheme of the systematic position of
Collembola in the Arthropoda
(modified after Aleshin & Petrov, 1999:184,185;
Gibiret & Ribera, 2000:214; Nardi et al., 2003)

New hypothesis 2: Collembola are terrestrial basal Pancrustacea (Hexapoda rejected).
Protura Diplura Pancrustacea
Collembola
Crustacea
Insecta s.s. (= Ectognatha)
Archaeognatha
(= Monocondylia)
Dicondylia
Zygentoma Pterygota
Tab.VI. Classification of related and higher taxa of Collembola.
(modified after Giribet & al., 2004:327)


	     +------------- Ectognatha  
	  +--+
	  |  +------------- Crustacea
       +--+
       |  +---------------- Collembola
    +--+
    |  |     +------------- Arachnida
    |  +- - -+
 ---+        +------------- Xiphosura
    |
    |                +----- Diplura
    +----------------+
    |                +----- Protura
    |
    +---------------------- Myriapoda


	  +---------------- Ectognatha  
	  |
       +--+---------------- Collembola
       |  |
       |  +---------------- Crustacea
    +--+
    |  |     +------------- Arachnida
    |  +- - -+
 ---+        +------------- Xiphosura
    |
    |                +----- Diplura
    +----------------+
    |                +----- Protura
    |
    +---------------------- Myriapoda

Fig.5. Simplified schemes of the systematic position of
Collembola in the Arthropoda
(modified after Giribet & al., 2004:327)

Segment Trilobita Arachnida Xiphosura Collembola Crustacea Ectognatha Segment
Acron - - - - - - Acron
1 + -1* Labrum Lat. eyes Lat. eyes Lat. eyes Labrum Lat. eyes Labrum Lat. eyes Labrum Lat. eyes 1 + -1*
2 + -2* Antennae Rostrum part 1 Rostrum part 1 Antennae Antennulae Antennae 2 + -2*
s.o. s.o.
3 Telopod Preepipod+gill Rostrum part 2 Rostrum part 2 Embryonic appendages Antennae Embryonic appendages 3
4 Telopod Preepipod+gill Chelicerae Chelicerae Mandibulae Mandibulae Mandibulae 4
5 Telopod Preepipod+gill Pedipalpae Pedipalpae Maxillae Maxillae Maxillae 5
6 Telopod Preepipod+gill Telopod tarsate Telopod chelate Labiae (cleft, bipartite labium) Maxillae Labium 6
7 Telopod Preepipod+gill Telopod tarsate Telopod chelate Telopod unguiate Maxillipod chelate Telopod tarsate 7
8 Telopod Preepipod+gill Telopod tarsate Telopod chelate Telopod unguiate Maxillipod chelate Telopod tarsate 8
9 Telopod Preepipod+gill Telopod tarsate Telopod chelate Telopod unguiate Maxillipod chelate Telopod tarsate 9
Telopod Preepipod+gill 10-1 Embryonic segment 10-1 Chilaria 10-1 Collophore 10-1 (Styli)
Telopod Preepipod+gill 11-2 Embryonic appendages 10-1 Pereopod 11-2 (Styli)
Telopod Preepipod+gill 13-3 Retinaculum 11-2 Pereopod 12-3 (Styli)
Telopod Preepipod+gill 14-4 Furca 12-3 Pereopod 13-4 (Styli)
Telopod Preepipod+gill 14-5 (Styli)
Telopod Preepipod+gill 15-6 (Styli)
Telopod Preepipod+gill 16-7 (Styli)
g.o. Telopod Preepipod+gill 11-2 Pectines g.o. 11-2 Opercula g.o. 15-5 - g.o. 13-4 Pereopod g.o.f. 17-8 Gonophysae g.o.f. g.o.
14-5 Pereopod
15-6 Pereopod g.o.m. 18-9 Gonophysae g.o.m.
Telopod Preepipod+gill 12-3 Booklung 12-3 Opercula Bookgill
Telopod Preepipod+gill 13-4 Booklung 13-4 Opercula Bookgill
Telopod Preepipod+gill 14-5 Booklung 14-5 Opercula Bookgill
Telopod Preepipod+gill 15-6 Booklung 15-6 Opercula Bookgill
Telopod Preepipod+gill 16-7 Booklung 16-7 Opercula Bookgill
Telopod Preepipod+gill 17-8 -
Telopod Preepipod+gill 18-9 - 17-8 Fossil segment 16-7 Pleopod
Telopod Preepipod+gill 19-10 - 18-9 Fossil segment 17-8 Pleopod
Telopod Preepipod+gill 20-11 - 19-10 Fossil segment 18-9 Pleopod
Telopod Preepipod+gill 21-12 - 19-10 Uropod 19-10 -
Telopod Preepipod+gill 22-13 - 20-11 Uropod 20-11 Cerci
Terminal a.o. ? Sting/whip/- Telson Anal "valves" Uropod Telson
Anal lobes
Proctodaeum
Terminal a.o.
Table VI. Schematic comparison of segmental bodyplan homologies in Arthropoda
(modified after Chamberlain, 1931:41; Störmer in Grassé, 1949:160-197; Weber, 1974:8,305; Haas, Waloszek & Hartenberger, 2003:46)
* Segments -1 and -2 are invaginated anterior segments. Segment -2 being the most anterior one. The ganglia of these five anterior segments have been fused into the superoesophagal ganglia complex.

Provisional conclusion

Collembola are difficult to position due to the discrepant results of morphological and molecular phylogenies; they are probably key taxa to explain arthropod relationships (Giberet & Ribera, 2000:225). The acceptance of nonmonophyly of Hexapoda s.l. implies that the tripartite and six-legged body plan typical of Hexapoda s.l. would be a convergent acquisition of Collembola, Protura, Diplura and Insecta s.s. Collembola diverged early from the ancestral pancrustacean line, even before Crustacea did, and the development of a matching body plan with Protura, Diplura and Insecta s.s. is likely the result of homology rather than direct ancestry.

The recent discovery of the marine hexapod Devonohexapodus bocksbergensis Haas, Waloszek & Hartenberger, 2003:42-53 from the Lower Devonian challenges the traditional association between terrestralisation and hexapody, making room for alternative hypotheses concerning collembolan origins (Nardi et al., 2003:1482e). The recent reinterpretation of a fragmentary insect fossil from the early Devonian Rhynie cherts of Scotland shows that the origin of insects is much earlier than conventionaly accepted (Engel & Grimaldi, 2004:627-630). This indicates that insects evolved independently in parallel with collembolans. Given the edaphic origin of Collembola (D'Haese, 2002), the collembolan ancestor must have completed the transition from marine aquatic habitats to littoral soil habitats already before the Lower Devonian.

Acknowledgments

References