Protaetia (Eupotosia) affinis (Andersch, 1797) y Protaetia (Eupotosia) mirifica (Mulsant, 1842) en el sudoeste de la provincia de Salamanca (Coleoptera: Scarabaeoidea: Cetoniidae, Cetoniini)

Esta investigación fue financiada en parte por el Ministerio de Ciencia e Innovación (CGL2011-23658), Ministerio de Economía y Competitividad (CGL2012-31669) y Generalitat Valenciana (proyectos PROMETEO/2013/03412 y ACOMP/2014/140). A. R. H. agradece la beca predoctoral del programa Santiago Grisolía de la Generalitat Valenciana (GRISOLIA/2010/080).

De propitio coeli valentini climate, et soli mirifica ubertate, atque de eiusdem incolarum industria [Texto impreso] : praesenti latitant auctoris nomina signo...

Hay un ejemplar encuadernado con: Discursos gratulatorios que en las visitas publicas... practicadas por la... ciudad de Valencia... (XVIII/4278)

Polyanthea medicis speciosa, chirurgis mirifica myrepsicis valde vtilis & necessaria : in quinque partes diuisa /

Mode of access: Internet.

Thomae Cantipratani ... De apibus : in quo mirifica apum repub. uniuersa vitae bene et christiane instituendae ratio traditur, et artificiose pertractatur ... /

Mode of access: Internet.

De veritate contritionis : aureum opus de veritate contritionis in quo mirifica docume[n]ta eterne salutis aperiuntur ... /

CCBE S. XVI, V 1288.

Quaternary through early Eocene benthic foraminifera off Peru

Stratigraphic assemblages of Quaternary through early Eocene benthic foraminifers were recovered among 10 Peru margin drill sites. Various hiatuses and intervals barren in foraminifers characterize the sections, but numerous samples contain abundant, well-preserved benthic foraminifers. Bathymetry of the extant species and California-based estimates of the paleobathymetry of the extinct species permit recognition of Quaternary sea-level fluctuations between shelf and upper bathyal depths that produced vertical migrations of oxygenated and low-oxygen habitats at the six shallow sites. Assemblages from lower-slope sites at about 9° and 11°S indicate a general subsidence of the continental margin from shelf or upper bathyal depths in Eocene time to the present lower bathyal depths. Data from 11°S suggest a major part of this subsidence occurred in late Oligocene to early Miocene time. Downslope-transported shelf specimens, particularly the small biserial species, Bolivina costata and B. vaughani, are major contributors to these lower bathyal assemblages from the middle Miocene through Quaternary time.

[Missale]

Copia digital: Biblioteca valenciana, 2010

On nomenclature and identity of Scarabaeus aeruginosus Linnaeus, S. aeruginosus Drury and S. speciosissimus Scopoli (Coleoptera: Scarabaeoidea: Cetoniinae and Rutelinae)

The valid name for the largest European species of Cetoniinae is Protaetia speciosissima (Scopoli, 1786), with Protaetia aeruginosa (Medvedev, 1964) as a junior synonym. The specimen illustrated by Scopoli in the original description is designated as the lectotype of Scarabaeus speciosissimus Scopoli, 1786. Since the lectotype is lost, a neotype from Piedmont, Italy, is designated and deposited in the Museo Civico di Storia Naturale Carmagnola, Italy. The name Scarabaeus aeruginosus Drury, 1773 is unavailable since Drury did not describe a new species but misidentified Scarabaeus aeruginosus Linné, 1767. A specimen figured by Gronovius in 1764 and cited by Linné is designated as the lectotype of Scarabaeus aeruginosus Linné, 1767. This species remains dubious, but it can be assigned to the ruteline subtribe Anticheirina.