Six new, unusually small ants of the genus Leptomyrmex (Hymenoptera: Formicidae)

Zootaxa ◽  
2009 ◽  
Vol 2142 (1) ◽  
pp. 57-68 ◽  
Author(s):  
DEREK J. SMITH ◽  
STEVE SHATTUCK

The ant genus Leptomyrmex contains 41 named taxa which are limited to eastern Australia, New Guinea and New Caledonia. While most species are large and distinctive, a few species are much smaller and have only recently been recognised as belonging to this genus. These six species, informally called micro-Leptomyrmex, are restricted to rainforests and wet sclerophyll forests in two relatively small regions of eastern Australia. All are described here for the first time and include L. aitchisoni n. sp., L. burwelli n. sp., L. dolichoscapus n. sp., L. garretti n. sp., L. pilosus n. sp. and L. ramorniensis n. sp.

1992 ◽  
Vol 6 (1) ◽  
pp. 1 ◽  
Author(s):  
AD Austin ◽  
PC Dangerfield

The genera of microgastrine braconid wasps present in the Australasian region (defined as Australia, New Zealand, New Caledonia, New Guinea, Solomon Is, Fiji Is, Samoan Is, Cook Is, but not French Polynesia) are reviewed. An illustrated key to genera, comments on their taxonomy, and information on the distribution and host relationships of species are provided. Following examination of holotypes, the generic placement of all species recorded from the region is reassessed since a recent generic reclassification of the subfamily left most of the Australasian species incorrectly placed. Parapanteles Ashmead (N.T.), Fornicia Brullé (Qld) and Deuterixys Mason (Qld) are recorded from Australasia for the first time, while Buluka De Seager, Parenion Nixon, Snellenius Westwood and Wilkinsonellus Mason, previously known from Australasia, are recorded from mainland Australia for the first time. The genus Austrocotesia is described as new [with A. exigua, sp. nov. (Papua New Guinea) as the type species], along with the following 14 species: Austrocotesia delicata, sp. nov. (Papua New Guinea, Qld), A. paradoxa, sp. nov. (Papua New Guinea), Buluka collessi, sp. nov. (Qld), Deuterixys anica, sp. nov. (Vic., N.S. W., Qld), Fornicia commoni, sp. nov. (Qld), Glyptapanteles deliasa, sp. nov. (S.A.), Microgaster nixoni, sp. nov. (Tas., N.S.W.), Parapanteles masoni, sp. nov. (N.T.), Parenion beelaronga, sp. nov. (Qld), P. bootha, sp. nov. (Qld), Sathon albicoxa, sp. nov. (Tas., Vic., N.S.W.), S. naryciae, sp. nov. (Vic.), Wilkinsonellus amplus, sp. nov. (Qld, N.T.) and W. tomi, sp. nov. (Papua New Guinea, New Britain, Qld). Glyptapanteles guyanensis (Cameron), comb. nov. is excluded from the Australasian fauna; the name Glyptapanteles fullawayi, nom. nov. (Samoa) is proposed for Apanteles opercuiinae var. polita Fullaway; lectotypes are designated for Cotesia deliadis (Bingham), comb. nov. (Qld), C. philoeampa (Cameron), comb. nov. (N.S.W) and C. rufiventris (Bingham), comb. nov. (Qld); Glyptapanteles operculinae (Fullaway), comb. nov. (Samoa), Microgaster kuchingensis Wilkinson (Papua New Guinea) and Sathon moratus (Wilkinson), comb. nov. (Vic., S.A., W.A.) are redescribed; and 41 additional new combinations are proposed.


2021 ◽  
Author(s):  
◽  
Zelia Dos Santos

<p>Northern Zealandia lies between Australia, New Zealandia, and New Caledonia. It has an area of 3,000,000 km2 and is made up of bathymetric rises and troughs with typical water depths of 1000 to 4000 m. I use 39,309 line km of seismic-reflection profiles tied to recent International Ocean Discovery Program (IODP) drilling and three boreholes near the coast of New Zealand to investigate stratigraphic architecture and assess the petroleum prospectivity of northern Zealandia.  Sparse sampling requires that stratigraphic and petroleum prospectivity inferences are drawn from better-known basins in New Zealand, Australia, New Caledonia, TimorLeste and Papua New Guinea. Five existing seismic-stratigraphic units are reviewed. Zealandia Seismic Unit U3 is sampled near New Zealand and may contain Jurassic Muhiriku Group coals. Elsewhere, Seismic Unit 3 may have oil-prone equivalents of the Jurassic Walloon Coal Measure in eastern Australia; or may contain Triassic-Jurassic marine source rocks, as found in offshore Bonaparte Basin, onshore Timor-Leste, and the Papuan Basin in Papua New Guinea. Seismic Unit U2b (Mid-Cretaceous) is syn-rift and may contain coal measures, as found in Taranaki-Aotea Basin and New Caledonia. Seismic Unit U2a (Late Cretaceous to Eocene) contains coaly source rocks in the southeastern part of the study area, and may also contain marine equivalent carbonaceous mudstone, as found at Site IODP U1509. Unit U2a is transgressive, with coaly source rocks and reservoir sandstones near its base, and clay, marl and chalk above that provides a regional seal. Seismic Unit U1b (Eocene-Oligocene) is mass-transport complexes and basin floor fans related to a brief phase of convergent deformation that created folds in the southern part of the study area and regionally uplifted ridges to create new sediment source areas. Basin floor fans may contain reservoir rock and Eocene folding created structural traps. Seismic Unit U1a is Oligocene and Neogene chalk, calcareous ooze, and marl that represents overburden. Mass accumulation rates (MAR) and climatic temperatures were high in the late Miocene and early Pliocene, resulting in peak thermal maturity and hydrocarbon expulsion at ~ 3 Ma.  Approximately one-fifth of the region has adequate source rock maturity for petroleum expulsion at the base of Seismic Unit U2: Fairway Basin (FWAY), southern New Caledonia Trough (NCTS) and Reinga Basin (REIN). Plays may exist in either Seismic Unit U3 or U2, with many plausible reservoir-seal combinations, and several possible trapping mechanisms: unconformities, normal faults, folds, or stratigraphic pinch-out. The rest of the region could be prospective, but requires a source rock to exist within Seismic Unit U3, which is mostly unsampled and remains poorly understood.</p>


2021 ◽  
Author(s):  
◽  
Zelia Dos Santos

<p>Northern Zealandia lies between Australia, New Zealandia, and New Caledonia. It has an area of 3,000,000 km2 and is made up of bathymetric rises and troughs with typical water depths of 1000 to 4000 m. I use 39,309 line km of seismic-reflection profiles tied to recent International Ocean Discovery Program (IODP) drilling and three boreholes near the coast of New Zealand to investigate stratigraphic architecture and assess the petroleum prospectivity of northern Zealandia.  Sparse sampling requires that stratigraphic and petroleum prospectivity inferences are drawn from better-known basins in New Zealand, Australia, New Caledonia, TimorLeste and Papua New Guinea. Five existing seismic-stratigraphic units are reviewed. Zealandia Seismic Unit U3 is sampled near New Zealand and may contain Jurassic Muhiriku Group coals. Elsewhere, Seismic Unit 3 may have oil-prone equivalents of the Jurassic Walloon Coal Measure in eastern Australia; or may contain Triassic-Jurassic marine source rocks, as found in offshore Bonaparte Basin, onshore Timor-Leste, and the Papuan Basin in Papua New Guinea. Seismic Unit U2b (Mid-Cretaceous) is syn-rift and may contain coal measures, as found in Taranaki-Aotea Basin and New Caledonia. Seismic Unit U2a (Late Cretaceous to Eocene) contains coaly source rocks in the southeastern part of the study area, and may also contain marine equivalent carbonaceous mudstone, as found at Site IODP U1509. Unit U2a is transgressive, with coaly source rocks and reservoir sandstones near its base, and clay, marl and chalk above that provides a regional seal. Seismic Unit U1b (Eocene-Oligocene) is mass-transport complexes and basin floor fans related to a brief phase of convergent deformation that created folds in the southern part of the study area and regionally uplifted ridges to create new sediment source areas. Basin floor fans may contain reservoir rock and Eocene folding created structural traps. Seismic Unit U1a is Oligocene and Neogene chalk, calcareous ooze, and marl that represents overburden. Mass accumulation rates (MAR) and climatic temperatures were high in the late Miocene and early Pliocene, resulting in peak thermal maturity and hydrocarbon expulsion at ~ 3 Ma.  Approximately one-fifth of the region has adequate source rock maturity for petroleum expulsion at the base of Seismic Unit U2: Fairway Basin (FWAY), southern New Caledonia Trough (NCTS) and Reinga Basin (REIN). Plays may exist in either Seismic Unit U3 or U2, with many plausible reservoir-seal combinations, and several possible trapping mechanisms: unconformities, normal faults, folds, or stratigraphic pinch-out. The rest of the region could be prospective, but requires a source rock to exist within Seismic Unit U3, which is mostly unsampled and remains poorly understood.</p>


1985 ◽  
Vol 33 (1) ◽  
pp. 27 ◽  
Author(s):  
TG Hartley

The genus Medicosma Hooker f., which has traditionally been considered to be monotypic and endemic to Australia, consists of 22 species. Six of these are endemic to eastern Australia, one is endemic to southern New Guinea and 15 are endemic to New Caledonia. The genus is described and its taxonomic history and relationships to other genera are discussed. The species are described, keyed and their relationships are outlined and discussed. Seventeen species are described as new, namely M. elliptica, M. obovata, M, glandulosa, M, diversifolia, M. articulata, M. parvifolia, M. obliqua, M. tahafeana, M. emarginata, M. verticillata, M. congests, M. latifolia, M. subsessilis, M. suberosa, M. petiolaris, M. exigua and M. gracilis, and new combinations are made for M. fareana (F. Mueller) T. Hartley, M. sessiliflora (C. T. White) T. Hartley, M. riparia (van Royen) T. Hartley and M. leratii (Guillaumin) T. Hartley.


Zootaxa ◽  
2011 ◽  
Vol 3046 (1) ◽  
pp. 1 ◽  
Author(s):  
PETER JÄGER

The genera Nilus O. Pickard-Cambridge 1876, Sphedanus Thorell 1877 and Dendrolycosa Doleschall 1859 are revised. Nilus is recognised as junior synonym of Thalassius Simon 1885; accordingly all species previously placed in Thalassius including nomina dubia are transferred to Nilus. Nilus curtus O. Pickard-Cambridge 1876 is recognised as senior synonym of Thalassius spinosissimus Karsch 1879. Nilus decoratus (Patel & Reddy) comb. nov. from India is transferred from Pisaura Simon 1885. Nilus amazonicus Simon 1898 from Brazil is transferred to the genus Architis Simon 1898: Architis amazonica (Simon 1898) comb. nov. Nilus oblongus Pavesi 1897 from Ethiopia and N. marginatus (Simon 1888) from the Andaman Islands are considered nomina dubia. Sphedanus Thorell 1877 is removed from the synonymy with Nilus and recognised as a senior synonym of Eurychoera Thorell 1897. The type species, S. undatus Thorell 1877, is redecribed and its copulatory organs are illustrated for the first time. Two species previously placed in the genus Eurychoera are transferred: Sphedanus banna (Zhang, Zhu & Song 2004) comb. nov. and Sphedanus quadrimaculatus (Thorell 1897) comb. nov. Campostichommides Strand 1911 and Dianpisaura Zhang, Zhu & Song 2004 are recognised as junior synonyms of Dendrolycosa. Nilus lanceolatus Simon 1898 and Pisaura lizhii Zhang 2000 are proposed as junior synonyms of Dendrolycosa robusta Thorell 1895. Four species are described as new: D. bairdi spec. nov. from Laos (male, female), D. duckitti spec. nov. from Laos (male, female), D. sierwaldae spec. nov. from New Guinea (female) and D. yuka spec. nov. from Australia (female). Eight species previously placed in the genera Nilus, Campostichommides Strand 1911, Pisaura Simon 1885 and Dianpisaura Zhang, Zhu & Song 2004, respectively are transferred to Dendrolycosa: D. ornata (Berland 1924) comb. nov. from New Caledonia, D. spadicaria (Simon 1897) comb. nov. from India (nomen dubium), D. bobbiliensis (Reddy & Patel 1993) comb. nov. from India, D. gitae (Tikader 1970) comb. nov. from India, D. inquirenda (Strand 1911) comb. nov. nomen dubium from Indonesia, D. parangbusta (Barrion & Litsinger 1995) comb. nov. from Philippines, D. putiana (Barrion & Litsinger 1995) comb. nov. from Philippines, D. songi (Zhang 2000) comb. nov. from Yunnan, China. Dendrolycosa stauntoni Pocock 1900 is considered a nomen dubium. One species originally described in Dendrolycosa is transferred to the genus Hygropoda: H. gracilis (Thorell 1891) comb. nov. Two species previously placed in the genus Tinus F. O. Pickard-Cambridge 1901 are transferred to Hygropoda: H. sikkimus (Tikader 1970) comb. nov., H. chandrakantii (Reddy & Patel 1993) comb. nov.


2002 ◽  
Vol 16 (1) ◽  
pp. 7 ◽  
Author(s):  
Robert A. Wharton

The Australian species of Alysiini are revised. Fourteen genera are treated, with eight of these recorded from Australia for the first time. Two of the genera, one from eastern Australia and one from New Guinea, are described as new. Two new subgenera are described, Idiasta Foerster (Apiasta, subgen. nov.) and Leptolarthra Fischer (Cratocarpa, subgen. nov.). Forty-nine species are described, 43 of them new: one in Aphaereta Foerster; eight in Aspilota Foerster; six in Cratospila Foerster; 13 in Dinotrema Foerster; one in Heleomyzophaga, gen. nov.; one in Heratemis Walker; one in Hovhoa, gen. nov.; four in Idiasta; three in Leptolarthra; three in Orthostigma Ratzeburg; one in Phaenocarpa Foerster; and one in Tanycarpa Foerster. Keys are presented to all genera of Alysiinae known from Australia as well as the Australian species of Asobara, Aspilota, Cratospila, Dinotrema and Orthostigma. Additionally, the world genera are reviewed and their relationships discussed to provide a context for an assessment of the Australian fauna. The status of 80 available genus-group names is discussed. The following nomenclatural changes are proposed: Neorthostigma Belokobylskij and Patriaspilota Fischer are treated as subgenera of Orthostigma; Acrobela Foerster as a synonym of Tanycarpa; Idiolexis Foerster as a synonym of Phaenocarpa; Eudinostigma Tobias as a synonym of Dinotrema; and Leptotrema van Achterberg as a subgenus of Dinotrema. The following new combinations are in addition to those associated with the above nomenclatural changes: Aspilota magnareata (Fischer); Dinotrema hardyi (Fischer); Dinotrema parvimaxillatum (Fischer); Dinotrema rotatum (Fischer); Dinotrema schoenmanni (Fischer); Leptolarthra cubiceps (Bischoff); and Orthostigma orthostigmoides (Fischer). Host records are included for two of the newly described species. Heleomyzophaga collessi, gen. nov. et sp. nov. was reared from a heleomyzid fly and Dinotrema monstrosum, sp. nov. was reared from a platypezid fly. A third species, Idiasta minor, sp. nov., was collected from pitfall traps baited with carrion.


Zootaxa ◽  
2008 ◽  
Vol 1708 (1) ◽  
pp. 1 ◽  
Author(s):  
SHANE T. AHYONG

Deepwater crabs from seamounts and chemosynthetic habitats off eastern New Zealand are reported. Of the 30 species reported, eight are new to science: Cymonomus clarki sp. nov. (Cymonomidae), Dicranodromia delli sp. nov. (Homolodromiidae), Ethusina castro sp. nov. and E. rowdeni sp. nov. (Dorippidae), Trichopeltarion janetae sp. nov. (Atelecyclidae), Mathildella mclayi (Mathildellidae), Neopilumnoplax nieli sp. nov. (Mathildellidae), and Garthambrus tani sp. nov. (Parthenopidae). The dorippids, parthenopids and mathidellids reported here are the first members of these families to be described from New Zealand. Three previously described species are recorded for the first time from New Zealand waters: Dicranodromia spinulata Guinot, 1995 (Homolodromiidae), Intesius richeri Crosnier & Ng, 2004 (Mathildellidae) and Miersiograpsus australiensis Türkay, 1978 (Plagusiidae). The majority of brachyurans from New Zealand seamounts and chemosynthetic habitats are ‘typical’ deepwater forms of which thirteen species are presently unique to New Zealand. At species level, 43% of the seamount and cold-seep brachyurans are apparent New Zealand endemics, with strongest affinities with the eastern Australian fauna (37%). At the generic level, however, congeners of most species reported herein occur widely in the Indo-West Pacific (including eastern Australia and New Caledonia), suggesting that the New Zealand seamount and cold-seep brachyuran fauna is an extension of the tropical Indo-West Pacific fauna. Thirty-three percent (10 of 30 species) of the known New Zealand seamount and cold-seep brachyurans have only been recently discovered indicating that species richness is probably strongly underestimated. A key to the Brachyura known from New Zealand seamounts and chemosynthetic habitats is given.


Author(s):  
D., P. Gold

Biostratigraphic data from exploration wells in Papua, West Papua of Indonesia, Papua New Guinea and Australia were reviewed, revised and updated using modern stratigraphic interpretations. Revised stratigraphic interpretations were combined with zircon U-Pb geochronologic data to produce new tectonic reconstructions of the Indonesian provinces of West Papua and Papua. Zircon U-Pb geochronologic data used in this study include new results from the Papuan Peninsula, combined with existing datasets from West Papua, Papua New Guinea, eastern Australia and New Caledonia. Supplementary geochronologic data were used to provide independent validation of the biostratigraphic data. Findings from a compilation of biostratigraphic and zircon age data provide a framework to produce new tectonic models for the origin of New Guinea’s terranes. Two hypotheses are presented to explain observations from the biostratigraphic and geochronologic data. The ‘Allochthonous Terrane’ Model suggests that many of the terranes are allochthonous in nature and may have been derived from eastern Australia. The ‘Extended Rift’ Model suggests that the New Guinea Terranes may have been separated from north-eastern Australia by an elongate rift system far more extensive than previously described. These new tectonic models are essential for our geological understanding of the regional and can be used to drive successful petroleum exploration in this frontier area.


Zootaxa ◽  
2010 ◽  
Vol 2688 (1) ◽  
pp. 1 ◽  
Author(s):  
ANDREA LUCKY ◽  
PHILIP S. WARD

The ants of the genus Leptomyrmex (Hymenoptera: Formicidae), commonly called ‘spider ants’, are distinctive members of the ant subfamily Dolichoderinae and prominent residents of intact wet forest and sclerophyll habitats in eastern Australia, New Caledonia and New Guinea. This revision redresses pervasive taxonomic problems in this genus by using a combination of morphology and molecular data to define species boundaries and clarify nomenclature. Twenty-seven Leptomyrmex species are recognized and are informally split into two groups: the macro-Leptomyrmex (21 species), and its sister group, the micro-Leptomyrmex (six species). Nine subspecies are elevated to species status: L. cnemidatus Wheeler 1915, L. geniculatus Emery 1914, L. melanoticus Wheeler 1934, L. nigriceps Emery 1914, L. rothneyi Forel 1902, L. ruficeps Emery 1895, L. rufipes Emery 1895, L. rufithorax Forel 1915 and L. tibialis Emery 1895. Nineteen new synonymies are proposed (senior synonyms listed first): L. cnemidatus Wheeler 1915 = L. erythrocephalus venustus Wheeler 1934 = L. erythrocephalus brunneiceps Wheeler 1934; L. darlingtoni Wheeler 1934 = L. darlingtoni fascigaster Wheeler 1934 = L. darlingtoni jucundus Wheeler 1934; L. erythrocephalus (Fabricius 1775) = L. froggatti Forel 1910 =4 · Zootaxa 2688 © 2010 Magnolia PressL. erythrocephalus mandibularis Wheeler 1915 = L. erythrocephalus unctus Wheeler 1934 = L. erythrocephalus clarki Wheeler 1934; L. fragilis (F. Smith 1859) = L. fragilis femoratus Santschi 1932 = L. fragilis maculatus Stitz 1938 = L. wheeleri Donisthorpe 1948; L. melanoticus Wheeler 1934 = L. contractus Donisthorpe 1947; L. niger Emery 1900 = L. lugubris Wheeler 1934; L. rufipes Emery 1895 = L. quadricolor Wheeler 1934; L. rufithorax Forel 1915 = L. erythrocephalus basirufus Wheeler 1934; L. tibialis Emery 1895 = L. nigriventris hackeri Wheeler 1934; L. varians Emery 1895 = L. erythrocephalus decipiens Wheeler 1915 = L. varians angusticeps Santschi 1929; L. wiburdi Wheeler 1915 = L. wiburdi pictus Wheeler 1915. Tools for identification of the macro-Leptomyrmex species include a revised species-level key based on the worker caste, keys to males in Australia and New Guinea, full descriptions of workers, images of known workers, males and queens, and illustration of male genitalia. Phylogenetic relationships among the macroand micro- Leptomyrmex species are discussed, as is the status of a putative fossil relative.


Zootaxa ◽  
2018 ◽  
Vol 4450 (2) ◽  
pp. 203
Author(s):  
WERNER MOHRIG ◽  
ELLEN KAUSCHKE ◽  
ADAM BROADLEY

The following 17 species are described as new for science: Austrosciara heterospinata sp. n., Aus. kalliesi sp. n., Aus. multispinulata sp. n., Aus. stockerae sp. n., Aus. trichovenosa sp. n., Bradysia chloroantennata sp. n., B. fuscovirgata sp. n., B. loudoni sp. n., B. macrotrichata sp. n., B. nigroantennata sp. n., B. parareflexa sp. n., Cratyna (Peyerimhoffia) subvagabunda sp. n., Euricrium (Austroeuricrium) australiensis sp. n., Phytosciara crocera sp. n., Pseudolycoriella latostylata sp. n., Psl. rubroalata sp. n., and Scatopsciara nigrothoracica sp. n. The following 4 species are new records for Australia: B. aspercera Mohrig, B. centidens Vilkamaa, Hippa & Mohrig (both from Papua New Guinea), B. gibbosa Vilkamaa, Hippa & Mohrig and Pseudolycoriella capillosa Vilkamaa, Hippa & Mohrig (both from New Caledonia). Euricrium australiensis sp. n. is the type species of the subgenus Austroeuricrium subgen. n. First detections of the species B. conjuncta (Skuse), B. exsequialis (Skuse), B. pernitida (Skuse) and B. pictipes (Skuse) were made after their description in the 19th century. One species was declared as a new synonym: B. centidens Vilkamaa, Hippa & Mohrig, 2012 = B. mutuata Mohrig, 2016 syn. n. Five species were excluded from the subgenus Peyerimhoffia. Four are newly combined in the genus Corynoptera, crassistylata group [C. sparsula (Shi & Huang) comb. n., C. brachypoda (Shi & Huang) comb. n., C. yunnana (Shi & Huang) comb. n., C. shennongjiana (Shi & Huang) comb. n.], one in Corynoptera s. str. [C. longiprojecta (Shi & Huang) comb. n.]. Corynoptera longiprojecta (Shi & Huang) is a junior synonym of Corynoptera diversicalcaria Mohrig, 2004 from Papua New Guinea. 


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