Evidence for Permo-Triassic colonization of the deep sea by isopods.

The deep sea is one of the largest ecosystems on Earth and is home to a highly diverse fauna, with polychaetes, molluscs and peracarid crustaceans as dominant groups. A number of studies have proposed that this fauna did not survive the anoxic events that occurred during the Mesozoic Era. Accordingly, the modern fauna is thought to be relatively young, perhaps having colonized the deep sea after the Eocene/Oligocene boundary. To test this hypothesis, we performed phylogenetic analyses of nuclear ribosomal 18S and 28S and mitochondrial cytochrome oxidase I and 16S sequences from isopod crustaceans. Using a molecular clock calibrated with multiple isopod fossils, we estimated the timing of deep-sea colonization events by isopods. Our results show that some groups have an ancient origin in the deep sea, with the earliest estimated dates spanning 232-314 Myr ago. Therefore, anoxic events at the Permian-Triassic boundary and during the Mesozoic did not cause the extinction of all the deep-sea fauna; some species may have gone extinct while others survived and proliferated. The monophyly of the 'munnopsid radiation' within the isopods suggests that the ancestors of this group evolved in the deep sea and did not move to shallow-water refugia during anoxic events.

A new genus and species of groundwater isopod of the family Protojaniridae (Isopoda: Asellota: Gnathostenetroidoidea) from southern Chile.

A new asellotan isopod of the family Protojaniridae Fresi, Idato Scipione, 1980 is described from freshwater springs in the Osorno province, Los Lagos region, southern Chile. Wiyufiloides osornoensis gen. sp. n. is the third South American protojanirid species and the first known groundwater isopod in Chile. The new genus and species is principally characterized by the presence of a vestigial antennal scale, a strongly subchelate pereiopod I and the absence of an apical lobe on the protopod of pleopod II. The new taxon is described in detail and figures are given.

Redescriptions and new species in the 'emAustrosignum/em-Munnogonium' complex sensu Just amp; Wilson (2007), mainly from the Southern Hemisphere (Crustacea: Isopoda: Paramunnidae).

Type material is used to illustrate and redescribe the following species in the paramunnid Austrosignum-Munnogonium complex (classification sensu Just and Wilson 2007): Cryosignum incisum (Richardson, 1908), Cryosignum latifrons (Menzies, 1962) comb. nov., Meridiosignum kerguelensis (Vanhöffen, 1914), Munnogonium falklandicum (Nordenstam, 1933), Munnogonium globifrons (Menzies, 1962), and Munnogonium tillerae (Menzies Barnard, 1959,-topotypes). In addition, seven new species in the complex are described, Austrosignum pilosum, Austrosignum latum, Cryosignum nordenstami, Meridiosignum convexum, Meridiosignum macquariensis, Munnogonium longicaudatum, and Tethygonium monocuspis. Boreosignum Just and Wilson, 2007 is reported from Australia for the first time as Boreosignum specimens.                Keys to species in Austrosignum, Cryosignum, Meridiosignum, Munnogonium and Tethygonium are given. A summary of distribution with a list of all species in the complex including occurrence is presented.

The Eophreatoicus Nicholls, 1926 species flock from Kakadu and Arnhem Land, with a description of a new genus of Amphisopidae (Crustacea : Isopoda : Phreatoicidea).

We present descriptions of 28 new species of Amphisopidae from Arnhem Land and Kakadu National Park of Australia's Northern Territory. We identified five additional species that are not yet fully characterized and are not provided with formal species recognition. This is the first taxonomic treatment highlighting the high species richness within the Phreatoicidea that occur in Australia and likely elsewhere. We document each species fully with scanning electron and light micrographic images, diagnoses, detailed descriptions, keys to identification and justification of each species using parsimony analysis of their morphological and genetic characters. The distributional data show that all species, except for one, have microendemic distributions, with some sibling species occurring within a few kilometers of each other. Because of the age of this group of species, they appear to have spread throughout the region of the Arnhem sandstone plateau and then back-colonized the same habitats so that as many as three morphologically and genetically distinct species may co-occur syntopically. Our research has uncovered a new genus-level taxon of the family Amphisopidae, Kakadubeh gen. nov. This new genus is unlike Eophreatoicus, not only in its general appearance, but also in having an inferred reproductive strategy different from most of the other members of the family. While Eophreatoicus species have males that are much larger than the females and practice precopula, a form of pre-insemination mate guarding, males of the new species, Kakadubeh rangemyahwurd sp. nov., are much smaller than females. In addition, males of this species have a fourth walking leg that is not specialized for holding females, suggesting that they have a reproductive strategy that does not involve precopula of the form seen in Eophreatoicus and Eremisopus Wilson Keable, 2002a. Most of our research has been undertaken in Kakadu National Park, although recent collections have been made in Arnhem Land, yielding additional distinctive species. Given the size of unexplored territory around the Arnhem Plateau and the geographic frequency of discovering new species, we predict that the diversity of this group in the Northern Territory may be many more than the ~35 species described here. At this time, these microendemic isopods appear to be unthreatened by human activities, largely owing to the environmental protection afforded by Kakadu National Park and Arnhem Land, and their cryptic habits during the dry season. Because they are dependent on small springs of permanent groundwater, future changes in hydrology owing to water use and climate change, as well as invasive introduced species, may present risks to populations and species.

Monsoon-influenced speciation patterns in a species flock of Eophreatoicus Nicholls (Isopoda; Crustacea).

A species flock of the freshwater isopod genus Eophreatoicus Nicholls lives in seeps, springs and perched aquifers at the base of the Arnhem Plateau and associated sandstone outliers in Australia's Northern Territory. These species have been found to have surprisingly high levels of genetic divergence and narrow range endemism, despite potential opportunities for dispersion during the summer monsoon season when streams flow continuously and have connectivity. Species of Eophreatoicus were identified morphologically as distinct taxa, sometimes with two or three species occurring at the same site. DNA sequence data from the mitochondrial 16S rRNA and cytochrome c oxidase subunit I genes corroborate our morphological concepts to a high level of resolution, with the exception of two distinct species that are identical genetically. The value of mtDNA data for identification of these species, therefore, is limited. These isopods disperse downstream from their home springs to a limited extent during the wet season, but the genetic data show that migration to non-natal springs, and reproduction there, may be rare. We argue that the multiplication of the narrow-range endemic species is the result of their homing behaviour combined with monsoonal alternation between aridity and flooding over recent and geological time scales since the Miocene period.

Arthropod Cladistics: Combined Analysis of Histone H3 and U2 snRNA Sequences and Morphology.

Morphological, developmental, ultrastructural, and gene order characters are catalogued for the same set of arthropod terminals as we have scored in a recent study of histone H3 and U2 snRNA sequences (D. J. Colgan et al., 1998, Aust. J. Zool. 46, 419-437). We examine the implications of separate and simultaneous analyses of sequence and non-sequence data for arthropod relationships. The most parsimonious trees based on 211 non-sequence characters (273 apomorphic states) support traditional higher taxa as clades, including Mandibulata, Crustacea, Atelocerata, Myriapoda, and Hexapoda. Combined analysis of morphology with histone H3 and U2 sequences with equal character weights differs from the morphological results alone in supporting Progoneata + Hexapoda (= Labiophora) in favor of a monophyletic Myriapoda, resolves the entognathous hexapods as a grade, and supports pycnogonids as sister group to Euchelicerata (rather than as basal euarthropods). Monophyly of Chelicerata (including pycnogonids), Mandibulata, Crustacea, Progoneata, Chilopoda, and Hexapoda is maintained under a range of transition/transversion and third codon weights, whereas Atelocerata and Myriapoda/Labiophora do not withstand all sensitivity analyses.

Evolution of the female cuticular organ in the asellota (crustacea, isopoda).

In an effort to understand the variation and probable origin of a female copulatory organ found in isopods of the asellote superfamily Janiroidea, the morphology of female reproductive structures among the Asellota was surveyed. Examples of four asellote superfamilies were studied using whole mount staining after potassium-hydroxide maceration or clearing with lactic acid. In contradiction to previous conclusions, the cuticular organ is shown to occur in the more primitive Asellota, although the position of its opening varies considerably. In the genera Asellus, and Stenetrium, Munna, and Santia, the cuticular organ originates adjacent to the oopore, and in the remaining janiroidean isopods, it is placed dorsally and usually anteriorly. This information permits a simple hypothesis explaining the origin of the cuticular organ: it was present in the proximate ancestor of the Asellota and evolved to the janiroidean condition by anterodorsal migration.