Fossils in the Phylogeny of the Isopod Crustaceans

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Fossils in the Phylogeny of the Isopod Crustaceans The Impact of Isopod Fossils George D.F. Wilson Australian Museum

outline The Isopoda a diverse group of Crustaceans Classification Better known fossils Fossils in isopod phylogeny, morphological analysis Time of isopod origin, fossils in Bayesian analysis

Thanks to Tom Hegna, Western Illinois University Luana Lins, Tae-yoon Park, & the Isopod Group at the Australian Museum Luana Lins Tae-yoon Park Tim Lee Torben Riehl

Isopoda fresh water & land Ponderella SW Queensland, Australia Protamphisopus baii, Triassic, China Phreatoicidea Gondwana Freshwater Fossils Carboniferous to Jurassic Oniscidea Terrestrial & Diverse Fossils Eocene or Miocene

Asellota 30 families Asellidae Stenetriidae Stenetriidae Janiridae Stenasellidae Desmosomatidae* Nannoniscidae* Dendrotionidae* Munnopsidae* Munnidae *Primarily deep-sea taxa

Shallow marine Isopoda Morphologically Diverse CYMOTHOIDA Sphaeromatidae Idoteidae Paranthuridae Limnoriidae Cymothoidae Gnathiidae Anthuridae Tridentellidae Aegidae Cirolanidae Bopyridae

Classification Isopoda Phreatoicidea Asellota Oniscidea Cymothoida Anthuridea Cymothoidea Cirolanoidea Valvifera Sphaeromatida Limnoriidea + other taxa of undecided affinities e.g. Tainisopus

When did this diversity begin? Devonocaris Brooks, 1962 Malacostracans began appearing in Devonian: e.g., Eocarids Earliest isopod fossil Carboniferous Hesslerella Schram (1970) suggested an earlymiddle Devonian age for ancestral peracarids

Hesslerella shermani Schram, 1970 Middle Pensylvanian Essex fauna, Mazon Creek FMNH PE 16527, latex cast Composite photo by Tom Hegna

Protamphisopus Nicholls, 1943 Triassic, Yunnan Province, China Also Jurassic, Antarctica (in progress!) Triassic, Eastern Australia

Archaeoniscus from Korea

Archaeoniscus reconstruction Park, Wilson et al., 2012. J. Paleont. Cretaceous, Aptian to Albian, freshwater facies

Brunnaega scavenging Cirolanidae Lower Cretaceous (Albian) of Queensland, Australia, in carcass of fish, Pachyrhizodus marathonensis (marine) Wilson, G. D. F., J. R. Paterson and B. P. Kear. 2011. Palaeontology 54:1053-1068

Triassphaeroma Basso & Tintori, 1995 Reconstruction in progress, Park & Wilson Marine Sphaeromatoid, Late Triassic (middle-late Norian)

Schweglerella strobli Polz, 1998 Solnhofen Plattenkalk, Bavaria, Jurassic (Lower Tithonian)

outgroups Phreatoicidea Protamphisopus Asellota (freshwater) Asellota (mostly marine) Oniscidea Sphaeromatida Valvifera Blue = fossil taxa Morphology (taxa=73;chr=202) Archaeoniscus Triassphaeroma Limnoriidea Cymothoida Brunnaega

Using Isopod fossils to date events in isopod evolution GenBank & new sequences: 18S, 28S, 16S, Cox I Select well-defined fossils Infer phylogeny (Bayesian) Anchor nodes based on dates from fossils Establish time credibility intervals using clock assumption (Beast & Phylobayes) Lins et al., 2012. Biol. Lett.

Fossil calibration Taxa MY Reference Calibration point 150.8 155.7 Polz, 2005 Cirolanidae, Cymothoida Protamphisopus baii 237-245 Fu et al., 2010 Amphisopidae, Phreatoicidea Hesslerella 307 Schram,1970; 1974, Phreatoicidea root 1977 93.5 99.6 N.Morel, pers.comm Joeropsididae, Asellota Ophthalmdiastylis parvulorostrum 318.1-328.3 Schram et al., 2003 Cumacea, peracarid outgroup Securicaris spinosus 318.1-328.3 Schram et al., 2003 Cumacea, peracarid outgroup Rehbachiella 499 Walossek, 1993 1Brunnaega roperi 2 3shermani 4Joeropsididae Crustacea Root

Bayesian analysis Lins et al., 2012. Biol. Lett. 4 1 2 3 Error bars indicate age credibility

In summary Isopod fossils can be used with extant taxa in phylogenetic analyses Most fossils in or related to crown groups Embedded in distal branches Little influence on morphological analysis Bayesian estimates of modern taxa Fossils provide estimate age of nodes Ordovician-Devonian origin

The way forward Planned analyses: Extend morphological databases with fossil data Obtain key sequences (e.g., Gnathia; Limnoria) Combined analysis using all data (morphological; genetic; fossil)

Thank you for your attention. Any questions? K. Osborn