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Figure 9 in Micromammalian distribution and abundance in the Western Cape Province, South Africa, as evidenced by Barn owls Tyto alba (Scopoli)

Figure 9. Proportional representation of 3-month age classes (C1–8) of Otomys irroratus at Geelbek in the West Coast National Park by month and season.

Figure 10 in Micromammalian distribution and abundance in the Western Cape Province, South Africa, as evidenced by Barn owls Tyto alba (Scopoli)

Figure 10. Proportion of total measured Otomys irroratus individuals born per month at Geelbek in the West Coast National Park during 1984–8, based on material collected during 1985–8, compared with mean monthly rainfall at Langebaanweg for the same period.

Figure 8 in Micromammalian distribution and abundance in the Western Cape Province, South Africa, as evidenced by Barn owls Tyto alba (Scopoli)

Figure 8. Variation in (A) maxillary and (B) mandibular alveolar length in Tatera afra from selected sites with mean annual precipitation increasing from left to right. SFN and SFS, Steenbokfontein North and South (139 mm); AGA, Andriesgrond (248 mm); BBS, Blombos (464 mm); KFN, Kraaifontein (569 mm); STB, Stellenbosch Airfield (629 mm).

Figure 6 in Micromammalian distribution and abundance in the Western Cape Province, South Africa, as evidenced by Barn owls Tyto alba (Scopoli)

Figure 6. Dominant species in quarter-degree squares where the micromammalian sample comprises>100 individuals. Blank squares yielded samples of fewer than 100 individuals. Ch, Cryptomys hottentotus; Da, Desmodillus auricularis; Mm, Mus minutoides; Mv, Myosorex varius; Oi, Otomys irroratus; Rp, Rhabdomys pumilio; Sv, Suncus varilla; Ta, Tatera afra.

Figure 1 in Micromammalian distribution and abundance in the Western Cape Province, South Africa, as evidenced by Barn owls Tyto alba (Scopoli)

Figure 1. Location of the Western Cape Province in South Africa (A) and of Western Cape Province quarterdegree squares yielding Tyto alba pellet samples discussed in this paper (B).

Figure 5 in Micromammalian distribution and abundance in the Western Cape Province, South Africa, as evidenced by Barn owls Tyto alba (Scopoli)

Figure 5. Distribution of Gerbillinae (A, B) and Soricidae (C–F) whose remains have been found in Tyto alba pellets from 10 or more Western Cape Province quarter-degree squares. White circles indicate dominance in squares yielding remains of at least 100 individuals.

Figure 7 in Micromammalian distribution and abundance in the Western Cape Province, South Africa, as evidenced by Barn owls Tyto alba (Scopoli)

Figure 7. Significant correlation of seasonal variation in percentage representation of Suncus varilla and Steatomys krebsii and climate variables in the De Hoop Nature Reserve (Geelbek and Bottelary). (A) Same-season rainfall and proportions of S. varilla; (B) same-season minimum monthly temperature and S. krebsii; (C) previous-season minimum monthly temperature and S. varilla. See text for further details.

Figure 3 in Micromammalian distribution and abundance in the Western Cape Province, South Africa, as evidenced by Barn owls Tyto alba (Scopoli)

Figure 3. Distribution of Murinae whose remains have been found in Tyto alba pellets from 10 or more Western Cape Province quarter-degree squares. White circles indicate dominance in squares yielding remains of at least 100 individuals.

Figure 2 in Micromammalian distribution and abundance in the Western Cape Province, South Africa, as evidenced by Barn owls Tyto alba (Scopoli)

Figure 2. Distribution of Chrysochloridae (A), Macroscelididae (B), Bathyergidae (C, D) and Vespertilionidae (E) whose remains have been found in Tyto alba pellets from 10 or more Western Cape Province quarter-degree squares. White circles indicate dominance in squares yielding remains of at least 100 individuals.

Figure 4 in Micromammalian distribution and abundance in the Western Cape Province, South Africa, as evidenced by Barn owls Tyto alba (Scopoli)

Figure 4. Distribution of Otomyinae (A–C) and Dendromurinae (D–F) whose remains have been found in Tyto alba pellets from 10 or more Western Cape Province quarter-degree squares. White circles indicate dominance in squares yielding remains of at least 100 individuals.

Fig. 6. A in Description of Metopograpsus cannicci, new species, a pseudocryptic crab species from East Africa and the Western Indian Ocean (Decapoda: Brachyura: Grapsidae)

Fig. 6. A, Grapsus thukuhar Owen, 1839, original plate; B, Metopograpsus intermedius H. Milne Edwards, 1853, lectotype, male (MNHN-IU-2014-11210); C, Metopograpsus eydouxi H. Milne Edwards, 1853, lectotype, male (MNHN-IU-2000-3547); D, Pachygrapsus parallelus Randall, 1840, syntype, male (ANSP CA3545); E, Metopograpsus thukuhar (Owen, 1839), neotype, male (ZRC 2020.0219). Black or white bar = 10 mm.

Fig. 5. Female gonopores. A in Description of Metopograpsus cannicci, new species, a pseudocryptic crab species from East Africa and the Western Indian Ocean (Decapoda: Brachyura: Grapsidae)

Fig. 5. Female gonopores. A, Metopograpsus cannicci, new species, paratype (MZUF 5008); B, Metopograpsus thukuhar (ZRC 2000.0405).

Fig. 4 in Description of Metopograpsus cannicci, new species, a pseudocryptic crab species from East Africa and the Western Indian Ocean (Decapoda: Brachyura: Grapsidae)

Fig. 4. First left pleopod (G1), dorsal view. A, Metopograpsus cannicci, new species, holotype, male (MZUF 4865); B, Metopograpsus thukuhar (Owen, 1839), neotype, male (ZRC 2020.0219); C, Metopograpsus intermedius H. Milne Edwards, 1853, lectotype, male (MNHN-IU-2014-11210). Scale bar = 0.5 mm. Photographs by S. Bambi (A, B) and L. Corbari (C).

Fig. 8 in Description of Metopograpsus cannicci, new species, a pseudocryptic crab species from East Africa and the Western Indian Ocean (Decapoda: Brachyura: Grapsidae)

Fig. 8. Genotype network of Metopograpsus thukuhar and Metopograpsus cannicci, new species, based on an alignment of seven 28S sequences (1286 bp) and constructed with PopART v1.7. The size of the circles is proportional to the number of individuals carrying that genotype. Transverse lines indicate the number of mutational steps between genotypes.

Fig. 7 in Description of Metopograpsus cannicci, new species, a pseudocryptic crab species from East Africa and the Western Indian Ocean (Decapoda: Brachyura: Grapsidae)

Fig. 7. Metopograpsus cannicci, new species, live male from Mida Creek mangrove forest (Kenya), July 2004, specimen not collected. Photograph by S. Cannicci.

Fig. 2. A in Description of Metopograpsus cannicci, new species, a pseudocryptic crab species from East Africa and the Western Indian Ocean (Decapoda: Brachyura: Grapsidae)

Fig. 2. A, Metopograpsus cannicci, new species, holotype, male (MZUF 4865); B, Metopograpsus thukuhar (Owen, 1839), neotype, male (ZRC 2020.0219), detail of the suborbital tooth. Photographs by S. Bambi.

Fig. 1. A in Description of Metopograpsus cannicci, new species, a pseudocryptic crab species from East Africa and the Western Indian Ocean (Decapoda: Brachyura: Grapsidae)

Fig. 1. A, Metopograpsus cannicci, new species, holotype, male, Egypt: Ras Mohammad (MZUF 4865); B, Metopograpsus thukuhar (Owen, 1839), neotype, male, Hawaii: Oahu, Kewalo, Ala Moana area, Waikiki (ZRC 2020.0219). Scale bar = 10 mm. Photographs by S. Bambi.

Fig. 3. A in Description of Metopograpsus cannicci, new species, a pseudocryptic crab species from East Africa and the Western Indian Ocean (Decapoda: Brachyura: Grapsidae)

Fig. 3. A, left cheliped of Metopograpsus cannicci, new species, holotype, male (MZUF 4865); B, left cheliped of Metopograpsus thukuhar (Owen, 1839), neotype, male (ZRC 2020.0219). Photographs by S. Bambi.

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Text-fig. 6. Distribution of Oligocene continental sediments of Africa, revealing the patchy and incomplete coverage of the occurrences. The Tunisian sedimentary outcrops represent an important resource for the north-western part of the continent. in Arsinoitherium (Embrithopoda) And Other Large Mammals And Plants From The Oligocene Of Tunisia

Text-fig. 6. Distribution of Oligocene continental sediments of Africa, revealing the patchy and incomplete coverage of the occurrences. The Tunisian sedimentary outcrops represent an important resource for the north-western part of the continent.