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Fig. 6 in The reinstated identity of agglutinated foraminifer Campanellula capuensis from the Lower Cretaceous of southern Italy by means of a 3D model investigation

Fig. 6. Lituolinid foraminifer Campanellula capuensis De Castro, 1964, Castel Morrone, Italy, upper Hauterivian–lower Barremian, Lower Cretaceous. Sub)axial sections (A–E), oblique sections (F, G, I, J), transverse section (H). A. Thin section DiSTARBA.4418.2 with two individuals (A1, A2); the dashed line in A2 points out alternated chambers resulting from the trochospiral arrangement. B. Thin section DiSTARBA.4418.3 with two individuals (B1, B2). C. Thin section DiSTARBA.4418.12. D. Thin section DiSTARBA.4418.15. E. Thin section DiSTARBA.4418.1 with two individuals (E1, E2). F. Thin section DiSTARBA.4418.13. G. Thin section DiSTARBA.4418.11. H. Thin section DiSTARBA.4418.3. I. Thin section DiSTARBA.4418.4. J. Thin section DiSTARBA.4418.2. Abbreviation: co, columella.

Fig. 3 in The reinstated identity of agglutinated foraminifer Campanellula capuensis from the Lower Cretaceous of southern Italy by means of a 3D model investigation

Fig. 3. Lituolinid foraminifer Campanellula capuensis De Castro, 1964, San Lorenzello section, Italy, upper Hauterivian–lower Barremian, Lower Cretaceous (A–J, L) and Križ section, Mljet Island, Croatia, Lower Cretaceous (K); various (sub)axial sections. A. Thin section DiSTARL29 with two individuals (A1, A2). B. Thin section DiSTARL8. C. Thin section DiSTARL392 with three individuals (C1–C3). D. Thin section DiSTARL361 with two individuals (D1, D2). E. Thin section DiSTARL391. F. Thin section DiST/SL9091.1. G. Thin section DiSTARL35. H. Thin section DiSTARL36. I. Thin section DiSTARL41. J. Thin section DiST/SL99C.2. K. Thin section IGZMK with two individuals (K1, K2), after Husinec and Sokač (2006: fig. 7J and I). L. Thin section DiSTARL37. Rather largesized specimens (A, K2) might belong to microspheric generation. Abbreviation: ch, chamber.

Fig. 12 in The reinstated identity of agglutinated foraminifer Campanellula capuensis from the Lower Cretaceous of southern Italy by means of a 3D model investigation

Fig. 12. Palaeobiogeographic distribution of species of Campanellula De Castro, 1964. Occurrence of species has been plotted on an Early Cretaceous ca.120 Ma) paleogeographic map, after http://portal.gplates.org/.

Fig. 11 in The reinstated identity of agglutinated foraminifer Campanellula capuensis from the Lower Cretaceous of southern Italy by means of a 3D model investigation

Fig. 11. Scheme of the species of Campanellula De Castro, 1964. A. Campanellula capuensis De Castro, 1964, IPA.281.1, holotype (drawing from De Castro 1964: pl. 1: 1), Castel Morrone, Italy, upper Hauterivian–lower Barremian, Lower Cretaceous. B. Campanellula herishtensis Schlagintweit, Rashidi, and Hanifzadeh, 2019, T 726 (number Gmm 13950F110), holotype (drawing from Schlagintweit et al. 2019: fig. 5L), Ardakan, Province of Yazd, Central Iran, lower Gargasian, Aptian, Lower Cretaceous.

Fig. 9 in The reinstated identity of agglutinated foraminifer Campanellula capuensis from the Lower Cretaceous of southern Italy by means of a 3D model investigation

Fig. 9. Lituolinid foraminifer Campanellula capuensis De Castro, 1964, from Castel Morrone, Italy, upper Hauterivian–lower Barremian, Lower Cretaceous. A. DiSTARL36.1, transversal section showing six chambers per whorl (A1), compared with the 3D model transversally cut (upper view displaying eight chamber per whorl (A2), also represented in lateral view (A3). B. DiSTARL36.1 tangential section (B1), compared with the 3D model tangentially cut (frontal view of the section, B2), also represented in lateral view (B3). C. DiSTARL35.1, tangentialoblique section (C1), compared with the 3D sectioned model cut in frontal view, C2), also represented in lateral view (C3). D. DiSTARL34.1, oblique section through last tours (D1), compared with the 3D sectioned model (cut in frontal view, D2), also represented in lateral view (D3). Scale bars 100 μm.

Fig. 5 in The reinstated identity of agglutinated foraminifer Campanellula capuensis from the Lower Cretaceous of southern Italy by means of a 3D model investigation

Fig. 5. Lituolinid foraminifer Campanellula capuensis De Castro, 1964, San Lorenzello section, Italy, upper Hauterivian–lower Barremian, Lower Cretaceous; various tangential sections. A. Thin section DiSTARL331. B. Thin section DiSTARL34. C. Thin section DiSTARL35 with two individuals (C1, C2). D. Thin section DiSTARL382. E. Thin section DiSTARL212. F. Thin section DiSTARL13. G. Thin section DiSTARL59. H. Thin section DiSTARL37 with two individuals (explain H1, H2). I. Thin section DiSTARL361 with three individuals (I1–I3). J. Thin section DiSTARL391 with two individuals (J1, J2). K. Thin section DiSTARL392. L. Thin section DiSTARL59. M. Thin section DiSTARL333. Rather largesized specimen (E) might belong to microspheric generation.

Fig. 8 in The reinstated identity of agglutinated foraminifer Campanellula capuensis from the Lower Cretaceous of southern Italy by means of a 3D model investigation

Fig. 8. Lituolinid foraminifer Campanellula capuensis De Castro, 1964, from Castel Morrone, Italy, upper Hauterivian–lower Barremian, Lower Cretaceous. IPA.281.1, 3D test reconstruction of the holotype (De Castro 1964: pl. 1: 1:). Left (A1) and frontal right (A2) views of the test.

Fig. 1 in The reinstated identity of agglutinated foraminifer Campanellula capuensis from the Lower Cretaceous of southern Italy by means of a 3D model investigation

Fig. 1. Position of the studied localities. A. A contour map of the Italian Peninsula showing location of the Campania Region. B. Enlargement of the Campania Region with the two studied localities: San Lorenzello section (Benevento Province; red star) and the type locality of Campanellula capuensis De Castro, 1964) near Castel Morrone village (Caserta Province; yellow star). C. Panoramic view of the San Lorenzello section (from Google Earth). D. Panoramic view of the Campanellula capuensis type locality along the SP174 road (from Google Earth).

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Fig. 1 in New population of Rosalia longicorn, Rosalia alpina, in Calabria (southern Italy) (Coleoptera: Cerambycidae)

Fig. 1 – Green areas: National Parks where Rosalia alpina is present; dotted blue line: Catena Costiera as an ecological corridor; red star: discovery point of the new population of R. alpina. Fig. 2 – SCI-SAC present in the study area (Image reworked from the maps downloadable from: http://retenatura2000. regione.calabria.it/).

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Fig. 3 in New population of Rosalia longicorn, Rosalia alpina, in Calabria (southern Italy) (Coleoptera: Cerambycidae)

Fig. 3 – Individual of Rosalia alpina photographed on a rotting beech trunk on the ground covered with moss into the new Calabrian site.

Fig. 55 in Rhizotrogus tedeschii, a new species from the alpine zone of the Pollino Massif, southern Italy (Coleoptera: Scarabaeidae, Melolonthinae)

Fig. 55 – Distribution of two diagnostic morphometric traits in males. BS: body length, head and pygidium excluded, ANTL/ANTW: elongation of antennomere 1.

Figs 53-54 in Rhizotrogus tedeschii, a new species from the alpine zone of the Pollino Massif, southern Italy (Coleoptera: Scarabaeidae, Melolonthinae)

Figs 53-54 – Habitat of Rhizotrogus tedeschii n. sp., main observing and sampling site near the top of Serra del Prete (39.911, 16.147), 1960 m. 53, view towards NE, where spare specimens were also observed along the crest (red circle); 54: detail of site, with extensive rocky debris, view towards SW.

Figs 15-26 in Rhizotrogus tedeschii, a new species from the alpine zone of the Pollino Massif, southern Italy (Coleoptera: Scarabaeidae, Melolonthinae)

Figs 15-26 – Variability of endophalli of Rhizotrogus cicatricosus, frontal view. 15, Spain, Fuente del Tajo; 16, Spain, Font Partegat; 17, France, Cognac; 18, France, Clermont-le-Fort; 19-20, France, Massac; 21, France, St. Gély; 22, France, Le Beausset; 23-25, Italy, Casola Valsenio; 26, Italy, Camaldoli.

Figs 35-38 in Rhizotrogus tedeschii, a new species from the alpine zone of the Pollino Massif, southern Italy (Coleoptera: Scarabaeidae, Melolonthinae)

Figs 35-38 – Endophalli, oblique view, of R. cicatricosus (35, Spain, Fuente del Tajo; 36, France, Massac; 37, Italy, Casola Valsenio) and R. tedeschii (38, topotypical paratype). Arrowhead evidencing the difference in the degree of protrusion of diverticula.

Figs 4-12 in Rhizotrogus tedeschii, a new species from the alpine zone of the Pollino Massif, southern Italy (Coleoptera: Scarabaeidae, Melolonthinae)

Figs 4-12 – Anatomical details of R. tedeschii and R. cicatricosus. 4, aedeagus in lateral view of R. tedeschii (holotype); 5, paramera in dorsal view of R. tedeschii (holotype). 6-7, comparison between male antennae of R. tedeschii n. sp. (6, specimen with 9 antennomeres) and of R. cicatricosus (7); Arrowhead evidencing antennomere 1. 8-10, variability of female antenna of R. tedeschii n sp.: 8, common condition, with original antennomeres 4 and 5 non-disjointed and forming a thicker antennomere; 9, article 4+5 similar to others; 10, non-disjonction extending to original antennomere 6, resulting in a 8-segmented antenna; 11-12, variability of female antenna of R. cicatricosus: 11, normally 10-segmented antenna; 12, 9-segmented antenna with non-disjunction of antennomeres 5-6.

Fig. 1 in Rhizotrogus tedeschii, a new species from the alpine zone of the Pollino Massif, southern Italy (Coleoptera: Scarabaeidae, Melolonthinae)

Fig. 1 – Ranges of studied species and distribution of examined specimens. Red shadowing: range of Rhizotrogus cicatricosus (from Allenspach 1970; Coca-Abia & Martin-Piera 1998; Ballerio et al. 2014; Bezdek 2016; Schaffrath 2015; Haselböck 2018). Red dots: locations of the examined specimens of R. cicatricosus from W Europe (see material and methods); blue dots: locations of the examined specimens of R. cicatricosus from Appen- nines; green dot: R. tedeschii n. sp.

Figs 39-43 in Rhizotrogus tedeschii, a new species from the alpine zone of the Pollino Massif, southern Italy (Coleoptera: Scarabaeidae, Melolonthinae)

Figs 39-43 – Female terminalia (left side, accesory glands omitted) of R. cicatricosus (39-40, Italy, Casola Valsenio; 41, France, Martinet) and R. tedeschii (42-43, paratypes). Cx: coxite, Ep: epipleurite, Ht: hemitergite, Sc: subcoxite.

Fig. 56 in Rhizotrogus tedeschii, a new species from the alpine zone of the Pollino Massif, southern Italy (Coleoptera: Scarabaeidae, Melolonthinae)

Fig. 56 – Distribution of two morphometrics traits relative to epipleural setation in males. EAL/EAD: ratio between length of setae and their distance at the subapical round; EML/EAL: ratio between the length of setae at the medial part and at the subapical round.

Figs 27-34 in Rhizotrogus tedeschii, a new species from the alpine zone of the Pollino Massif, southern Italy (Coleoptera: Scarabaeidae, Melolonthinae)

Figs 27-34 – Variability of endophalli of Rhizotrogus tedeschii n. sp., frontal view (topotypical paratypes).