{"key":"ac064247-238f-4d72-9fcb-d099a7e3578b","installationKey":"7ce8aef1-9e92-11dc-8740-b8a03c50a999","publishingOrganizationKey":"7ce8aef0-9e92-11dc-8738-b8a03c50a862","doi":"10.15468/5u4kcu","external":false,"numConstituents":0,"type":"CHECKLIST","title":"New species of Cerambycidae and Disteniidae (Coleoptera) from the Neotropical Region","description":"

This dataset contains the digitized treatments in Plazi based on the original journal article Bezark, Larry G., Santos-Silva, Antonio, Botero, Juan Pablo (2023): New species of Cerambycidae and Disteniidae (Coleoptera) from the Neotropical Region. Faunitaxys 11 (1): 1-13, DOI: 10.57800/faunitaxys-11(1), URL: http://dx.doi.org/10.5281/zenodo.10622570

Résumé

Bezark L. G., Santos-Silva A. & Botero J. P., 2023.– Nouveaux Cerambycidae et Disteniidae (Coleoptera) de la région néotropicale. Faunitaxys, 11(1): 1 – 13.

Quatre nouvelles espèces sont décrites de la région néotropicale: Sternidius micromaculatus sp. nov. (Lamiinae, Acanthocinini), from Belize; Cymatonycha megagena sp. nov. (Lamiinae, Desmiphorini), from Mexico (Chiapas); Adesmus alboverticis sp. nov. (Lamiinae, Hemilophini); and Novantinoe pubescens sp. nov. (Disteniidae), from Guatemala. Une clé du genre Cymatonycha Bates, 1874 est proposée, et Novantinoe pubescens sp. nov. est incorporée dans la clé déjà connue.

Mots-clés. – Cerambycidae, Sternidius, Cymatonycha, Adesmus, Cymatonycha, longicorne, taxonomie, nouvelles espèces, région néotropicale.

Faunitaxys

Volume 11, Numéro 1, Janvier 2023

SOMMAIRE

Nouveaux Cerambycidae et Disteniidae (Coleoptera) de la région néotropicale. Larry G. Bezark, Antonio Santos-Silva & Juan Pablo Botero .............. 1 – 13

CONTENTS

New species of Cerambycidae and Disteniidae (Coleoptera) from the Neotropical Region. Larry G. Bezark, Antonio Santos-Silva & Juan Pablo Botero .............. 1 – 13

Illustration de la couverture:

Le Grand Trou Bleu est un cénote sous-marin situé au large de la côte du Belize, en Amérique centrale. Il fait partie du Récif Lighthouse et il est protégé au sein de la barrière de corail du Belize.

Le trou est quasiment circulaire, d'un diamètre de plus de 300 mètres et d'une profondeur mesurée de 124 mètres.

À l'origine de sa formation, pendant la dernière période glaciaire lorsque les niveaux de mer étaient beaucoup plus bas, c'était une grotte calcaire. Lorsque le niveau de l'océan s'est élevé, les cavités souterraines ont été inondées, et le toit de cette grotte s'est effondré.

Crédits:

Jesus Santiago Moure: Fig. 6. Antonio Santos -Silva: Fig. 1-5 & 7-39.

Tripadvisor - https://www.tripadvisor.fr/: Couverture.

Publié par l’Association Française de Cartographie de la Faune et de la Flore (AFCFF)

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