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Three new species of longhorned beetles (Coleoptera: Cerambycidae) with notes on additional taxa
Abstract
The differences between Methia enigma Martins, 1981 and M. argentina Bruch, 1918 (Cerambycinae: Methiini) are discussed, and a new country record for the latter is provided. Sexual dimorphism in Pseudosparna Mermudes and Monné, 2009 (Lamiinae: Acanthocinini) is reported for the first time, and two new species of Pseudosparna (Lamiinae: Acanthocinini) are described from Panama: Pseudosparna dimitrisi sp. nov. and Pseudosparna marilenae sp. nov. The female of Pseudosparna mantis Devesa & Santos-Silva, 2020 is described for the first time. Eranina dariae sp. nov. (Lamiinae: Hemilophini) is described from French Guiana. The type locality of Bisaltes (Bisaltes) bimaculatus Aurivillius, 1904 (Lamiinae: Apomecynini) is reported, and a new country record is provided for the species. Aerenea subsulcicollis Breuning, 1948 (= A. sulcicollis subsulcicollis) (Lamiinae: Compsosomatini) is synonymized with A. sulcicollis Melzer, 1932, and a new country record is provided. A new state record is provided for Schmidarius kondratieffi Santos-Silva, Heffern, Botero & Nascimento, 2020 (Lamiinae: Hemilophini). Tucumaniella Breuning, 1943 (Apomecynini) is synonymized with Cacostola Fairmaire & Germain, 1859 (Onciderini), and Tucumaniella brevipes Breuning, 1943 is synonymized with Cacostola volvula (Fabricius, 1787).
... nov. is similar to P. flaviceps (Bates, 1863) (see photograph of the holotype male in Mermudes &Monné 2009 andBezark 2024) but differs by the metafemora wider and the prosternal process not laminiform centrally (respectively narrow and laminiform centrally in P. flaviceps). Pseudosparna carmenae is similar to some females of Pseudosparna dimitrisi Nearns, Swift & Santos Silva, 2023 (elytral color pattern dark in male) (see photograph of the holotype male and allotype female in Nearns et al. 2023 andBezark 2024), but differs mainly by the distribution of the elytral color pattern (mainly yellowish-orange in female of P. dimitrisi, while in P. carmenae the elytra are orangish only on sides of the anterior region), and the prosternal process laminiform centrally in P. dimitrisi (Fig. 20), meanwhile in P. carmenae the prosternal process is not laminiform (Fig.19). ...
Ongoing studies on Panamanian longhorn beetles (Cerambycidae) reveal new species, especially in the subfamily Lamiinae. Four new species of Lamiinae from Panama are described: Sternacutus akersae sp. nov.; Trichotithonus barrocoloradensis sp. nov.; Pseudosparna carmenae sp. nov. (Acanthocinini); and Piriana aielloae sp. nov. (Colobotheini).
... In recent years, studies of Central American longhorned beetles (Cerambycidae) continue to reveal new species and distribution records (e.g. Bezark et al. 2013, Lanuza-Garay & Santos Murgas 2018Wappes & Santos-Silva 2020;Lanuza-Garay 2022, Heffern & Santos Silva, 2022, Nearns et al. 2023. In 2002, my colleagues Roberto Cambra and Alonso Santos Murgas placed Malaise traps along the Cerro Pirre, Darien National Park, Darien province, Panama. ...
Sphallopataroides gen. nov, Sphallopataroides pirreanus sp. nov., and Pseudosparna iolandae sp. nov. are described from Panama. New country records from Panama are provided: Leptostylus armatus Monné & Hoffmann, 1981; Atrypanius cinerascens (Bates, 1864); and Colobothea chemsaki Giesbert, 1979.
Sphallopataroides gen. nov., Sphallopataroides pirreanus sp. nov., et Pseudosparna iolandae sp. nov. sont descrits du Panama. De nouvelles mentions nationales du Panama sont fournies: Leptostylus armatus Monné & Hoffmann, 1981; Atrypanius cinerascens (Bates, 1864); et Colobothea chemsaki Giesbert, 1979.
A checklist of the Cerambycidae (Coleoptera) of Panama is provided, including 1031 species and
subspecies distributed in 433 genera, 63 tribes and subtribes, and five subfamilies. In addition, provincial
distribution data are provided for each species. The following new country records for Panama are reported:
Ischioloncha lineata Bates, 1885 (Panama and Colon Province) (Lamiinae: Apomecynini), Oncideres macra
Thomson, 1868 (Panama and Panama Oeste Province), Oncideres minuta Thomson, 1868 (Panama province,
San Blas Comarca), Oncideres ochreostillata Dillon and Dillon, 1952 (Barro Colorado Island) (Lamiinae:
Onciderini). A new province record is presented for Rileyellus panamensis Wappes and Santo-Silva, 2020
(Darien Province) (Lamiinae: Desmiphorini). Additionally, distributional notes on Atenizus laticeps Bates,
1867 (Cerambycinae: Oemiini) and Desmiphora (Desmiphora) canescens Bates, 1874 (Lamiinae: Desmiphorini)
are provided. The following species are erroneous records: Parevander unicolor (Bates, 1880)
(Cerambycinae: Trachyderini), Psyrassa cuprina Garcia and Toledo, 2022 (Cerambycinae: Elaphidiini), Amphelictus
rugiscapus Fuchs, 1976 (Cerambycinae: Cerambycini: Sphallotrichina) and Dihammaphora dispar
Chevrolat, 1859 (Cerambycinae: Rhopalophorini). Justified emendations for some species-group names of
Panamanian longhorned beetle treated in this checklist are presented.
Second part of an inventory of longhorn beetles from French Guiana established from our own records, data bases, private collections and bibliography. Known localities are given for each species. This list comprises 690 described species: 675 Lamiinae and 15 Disteniinae. Among them, 45 taxa (Lamiinae) are listed for the first time from French Guiana.
A new species of Hemilophini, Adesmus lauropalui sp. nov. and a list of species of Cerambycidae from the Reserva Particular de Patrimonio Natural (RPPN) Sanctuary of Caraça are presented. The data are based on fieldwork and the MNRJ collection. Two hundred fifty-four species of Cerambycidae are recorded, of which 158 are new distribution records.
A checklist of the 1164 primary types of Cerambycidae, Disteniidae and Vesperidae (Coleoptera) deposited in the Museu de Zoologia, Universidade de São Paulo, São Paulo, Brazil is provided. Lectotype designations for 97 species are proposed.
A catalogue of the subfamiliy Cerambycinae (Coleoptera: Cerambycidae) of the Neotropical Region is presented. Fifty-seven tribes, 10 subtribes, 716 genera, 3789 species and 68 subspecies are listed in alphabetical order. Under each family-group name bibliographical references are given and under each species-group name, data on the type locality, the acronym of the institution where the type is deposited, the geographical distribution and detailed bibliographical references are provided. One new combination is presented: Plocaederus yucatecus (Chemsak & Noguera, 1997), new comb., from Brasilianus.
A list of the Cerambycidae of Bolivia is presented. It totals 1,259 species including 496 new country records. When available the known geographical distribution by department is shown for each species. Resumen: Se presenta una lista de los Cerambycidae de Bolivia. En total son 1.259 especies incluyendo 496 que son nuevas para el país. En los casos que ha sido posible, la distribución departamental se presenta para cada especie.
A survey of the Lamiinae species recorded in the Parque Nacional do Itatiaia, Rio de Janeiro State, Brazil, is presented. The data were based on literature, field work and in the collection of the Museu Nacional, Universidade Federal do Rio de Janeiro. Three hundred and twenty two species of Lamiinae are registered, and this represents about 30% of the species that occur in the Atlantic Rainforest. Forty two new distribution records are registered. One hundred and thirty five species are illustrated. A comparative table showing the respective number of genera and species of Lamiinae that occur in the Neotropical Region, Atlantic Rainforest and Parque Nacional do Itatiaia is given.
A quantitative analysis of the various parameters influencing the thermal regime in orogenic belts and related foredeeps shows that (i) the increasing heat flow in internal zones is mainly due to the thickening of radiogenic layers, although there is no simple proportionality between crustal thickness and heat flow signal at large scale; (ii) in external zones, where the horizontal strain rate is large (such as in the Bolivian Andes), surface processes can be of first order within the first kilometers of the crust. Hence, they induce a large scatter in the thermal data which are acquired at shallow depths. The deep thermal regime can be restored only by a quantitative assessment of these parameters. Active erosion (respectively sedimentation) can increase (resp. reduce) the heat flow by a factor of 2 in the uppermost kilometers. The effects of fluid circulation percolating at depth can also generate significant local disturbances. Other processes such as heat advection during thrusting, surface morphology and climate change have a minor influence in most settings, compared to the aforesaid effects.In the Bolivian Sub Andean Zone, between 18°S and 22°S, the very active deformation enhances the surface thermal perturbations (particularly erosion and sedimentation) and disturb the thermal field. The analysis of these data accounting for the kinematics of the belt allows the lateral variations of the thermal regime at various scales to be assessed. A slight eastward increase in the thermal regime towards the Chaco plain is evidenced as well as towards the Boomerang area, as the Mesozoic and Cenozoic sedimentary cover gets thinner.
Foreland sedimentation in the Subandean Zone of south-central Bolivia spans from the Upper Oligocene to present. It records sediment dispersal patterns in an initially distal and later proximal retroarc foreland basin, and thereby contains stratigraphic information on the tectonic evolution of the adjacent Andean fold-thrust belt. Within the Neogene orogenic wedge individual siliciclastic-dominated depositional systems formed ahead of an eastward-propagating deformation regime.We defined, described, and interpreted eight architectural elements and 24 lithofacies from 15 outcrop locations representing the Neogene foreland basin in the Subandean Zone and the Chaco Plain. These are combined to interpret depositional settings. The up to 7.5 km-thick Neogene wedge is subdivided in five stratigraphic units on the basis of facies associations and overall architecture: (1) The basal, Oligocene–Miocene, up to 250 m-thick Petaca Formation consists dominantly of calcrete, reworked conglomeratic pedogenic clasts, and fluvial sandstone and mudstone. This unit is interpreted to represent extensive pedogenesis under an arid to semiarid climate with subordinate braided fluvial processes. (2) The overlying, Upper Miocene, up to 350 m thick Yecua Formation records numerous small-scale transgressive–regressive cycles of marginal marine, tidal, and shoreline facies of sandstone, ooid limestones, and varicoloured mudstone. (3) The Upper Miocene, up to 4500 m-thick Tariquia Formation principally consists of sandstone with interbedded sandstone–mudstone couplets representing frequent crevassing in anastomosing streams with an upsection-increasing degree of connectedness. (4) The up to 1500 m-thick Lower Pliocene Guandacay Formation represents braided streams and consists principally of granule to cobble conglomerate interbedded with sandstone and sandy mudstone. (5) The Upper Pliocene, up to 2000 m-thick Emborozu Formation consists predominantly of alluvial-fan-deposited cobble to boulder conglomerate interbedded with sandstone and sandy mudstone.The coarsening- and thickening-upward pattern and eastward progradation, coupled with the variable proportions of overbank facies, channel size, and degree of channel abandonment, in the Tariquia, Guandacay, and Emborozu Formations reflect a distal through proximal fluvial megafan environment. This long-lived megafan grew by high sedimentation rates and a northeast-through-southeast radial paleoflow pattern on large, coarse-grained sediment lobes. The marked overall upsection change in pattern and depositional styles indicate fluctuations in accommodation space and sediment supply, regulated by basin subsidence, and are attributable to Andean tectonics and climatic controls.
A catalogue of the subfamiliy Cerambycinae (Coleoptera: Cerambycidae) of the Neotropical Region is presented. Fifty-seven tribes, 10 subtribes, 716 genera, 3789 species and 68 subspecies are listed in alphabetical order. Under each family-group name bibliographical references are given and under each species-group name, data on the type locality, the acronym of the institution where the type is deposited, the geographical distribution and detailed bibliographical references are provided. One new combination is presented: Plocaederus yucatecus (Chemsak & Noguera, 1997), new comb., from Brasilianus.
Pseudolparna new genus is proposed to include four species: P. luteolineata new species (ty P. anzoena new species and P. aragua new species from Venezuela, and P. flavipes (Bates, pe species) from Equador, 1863) new combination, transferred from Lepturtrigona Gilmour, 1957. The four species are illustrated and keyed.
After the examination of specimens belonging to 333 species of Cerambycidae (Coleoptera), ninety six species (1 Prioninae, 1 Anoplodermatinae, 1 Lepturinae, 66 Cerambycinae, and 27 Lamiinae) are firstly re- corded from Paraguay, together with new records of localities of 240 species previously mentioned in the litera- ture, and some corrections of misidentified specimens.
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