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Fig. 1 in Reproductive seasonality of Geophagus steindachneri Eigenmann & Hildebrand, 1922 (Perciformes: Cichlidae) in a tropical mountain river
Fig. 1. Monthly variation of environmental variables: (a) rainfall pattern, (b) pH and temperature, and (c) conductivity and transparency.
Fig. 4 in Reproductive seasonality of Geophagus steindachneri Eigenmann & Hildebrand, 1922 (Perciformes: Cichlidae) in a tropical mountain river
Fig. 4. Differences between females that were not performing parental care and mouth-brooding females: (a) stage of ovary maturity, with circle size indicating number of females in each condition; (b) liver and ovary weight.
Figure 7 in The non-acarine Arachnida of the Amathole Mountains, South Africa
Figure 7. Selected Pseudoscorpiones from the Amathole Mountains, Eastern Cape, South Africa; A, Catatemnus sp., female (Atemidae); B, unidentified species of Cheliferidae, female; C, Afrogarypus triangularis, female (Geogarypidae); D, Gymnobisium cuneatum, female (Gymnobisiidae); E, Gymnobisium hogsbackense, male (Gymnobisiidae); F, Afrochthonius godfreyi, female (Pseudotyrannochthoniidae); G, Afrochthonius aff. inequalis, female (Pseudotyrannochthoniidae); H, Anaulacodithella mordax, female (Tridenchthoniidae); I, unidentified species of Withiidae, female. Photos: C. Haddad.
Figure 5 in The non-acarine Arachnida of the Amathole Mountains, South Africa
Figure 5. Selected web-building spiders from the Amathole Mountains, Eastern Cape, South Africa; A, Funnel-web of Agelena sp. (Agelenidae); B, Caerostris sexcuspidata, female (Araneidae); C, Cyclosa insulana, female in web (Araneidae); D, Neoscona subfusca, female (Araneidae); E, Trichonephila fenestrata, female (Araneidae); F, Menneus camelus, female, with net-casting web (Deinopidae); G, Same, male (above) and female (below), resting on a twig; H, Microlinyphia sterilis, female (Linyphiidae); I, Themacrys sp., female (Phyxelididae); J, Leucauge decorata, female (Tetragnathidae); K, Leucauge festiva, female (Tetragnathidae). Photos: C. Haddad.
Figure 6 in The non-acarine Arachnida of the Amathole Mountains, South Africa
Figure 6. Selected harvestmen and scorpions from the Amathole Mountains, Eastern Cape, South Africa; A, Rhampsinitus sp., male (Phalangiidae); B, Rhampsinitus aff. silvaticus, female (Phalangiidae); C, possible Adaeum sp., female (Triaenonychidae); D, Parabuthus planicauda, female (Buthidae); E, Uroplectes formosus, female (Buthidae); F, Uroplectes triangulifer, male (Buthidae); G, Hadogenes trichiurus, juvenile (Hormuridae); H, Opistacanthus validus, male (Hormuridae); I, Opistophthalmus latimanus, female (Scorpionidae). Photos: A–C, G, H, C. Haddad; D, C. Hobson; E, I, S. Christie; F, G. Diedericks.
Figure 2 in The non-acarine Arachnida of the Amathole Mountains, South Africa
Figure 2. Afromontane Forest sampled at Mpofu Fort Fordyce Nature Reserve (A, B) and Katberg State Forest (C, D) in the Amathole Mountains, Eastern Cape, South Africa. Photos: C. Haddad.
Figure 3 in The non-acarine Arachnida of the Amathole Mountains, South Africa
Figure 3. Selected wandering spiders from the Amathole Mountains, Eastern Cape, South Africa: A, Copa kei, female (Corinnidae); B, Lepthercus mandelai, female (Entypesidae); C, Same, burrow opening among leaves; D, Drassodella amatola, female (Gallieniellidae); E, Proevippa bruneipes, female (Lycosidae); F, Microstigmata amatola, female (Microstigmatidae); G, Asemonea amatola, male (Salticidae); H, Myrmarachne lesserti, female (Salticidae); I, Myrmarachne sp., female (Salticidae); J, Rumburak hilaris, female (Salticidae); K, Rumburak mirabilis, male (Salticidae); L, Thyenula alotama, female (Salticidae). Photos: C. Haddad.
Figure 4 in The non-acarine Arachnida of the Amathole Mountains, South Africa
Figure 4. Selected wandering spiders from the Amathole Mountains, Eastern Cape, South Africa: A, Anyphops amatolae, female (Selenopidae); B, Anyphops gilli, male (Selenopidae); C, Same, female; D, Palystes superciliosus, female (Sparassidae); E, Pachygnatha sp., female (Tetragnathidae); F, Oxytate ribes, female (Thomisidae); G, Thomisus australis, female (Thomisidae); H, Afroceto martini, female (Trachelidae); I, Platyoides walteri, female (Trochanteriidae). Photos: C. Haddad.
Figure 1 in The non-acarine Arachnida of the Amathole Mountains, South Africa
Figure 1. Biotopes sampled in the Hogsback area of the Amathole Mountains, Eastern Cape, South Africa; A, Part of Tyume Forest on a south-facing slope (Afromontane Forest); B, Understorey of Afromontane Forest; C, Open mesic grassland north of Hogsback; D, Pine plantation; E, Hogsback Arboretum, mixed indigenous and exotic trees; F, Canopy fogging a yellowwood sapling at Hogsback Arboretum. Photos: C. Haddad.
Figure 5 in Composition and structure of plant communities in the Moist Temperate Forest Ecosystem of the Hindukush Mountains, Pakistan
Figure 5. CCA plot Analysis of illustrating the influence of elevation on spreading pattern of plant communities in Lalkoo valley Swat.
Figure 4 in Composition and structure of plant communities in the Moist Temperate Forest Ecosystem of the Hindukush Mountains, Pakistan
Figure 4. Results of CCA joint biplot showing results for eleven plant communities' correlation with environmental variable. BAB-I: Berberis- Abies- Bergenia; PIP-II: Picea-Indigofera- Poa; APP-III: Abies- Parrotiopsis- Poa,QVP-IV:Quercus-Viburnum-Poa,PSP-V:PiceaSalix-Primula,AVP-VI:Abies-Viburnum -Poa; VTP-VII: ViburnumTaxus-Poa; PVL-VIII: Pinus-Viburnum-Lithospermum; ABC-IX: Abies-Berberis-Carex; PVP-X: Pinus-Viburnum-Poa; and PPP-XI: Parrotiopsis-Picea-Poa represents community types.
Figure 3 in Avifauna of the Adelbert Mountains, New Guinea: why is Fire-maned Bowerbird Sericulus bakeri the mountains' only endemic bird species?
Figure 3. Terrain map of north-east New Guinea. Areas above 500 m are coloured grey; areas between 300 and 500 m blue; and areas below 300 m green. 1 = the Gogol River valley, between the Adelbert Mts. to the north and the Finisterre Mts. of the Huon Peninsula to the south. 2 = the Ramu River valley, between the Adelberts to the north-east and the Central Range to the south-west. 3 = the upper Ramu River valley and its headwaters, between the Finisterre Mts. of the Huon Peninsula to the north and the Central Range to the south. 4 = the Sepik River basin, between the Adelbert Mts. to the east and Prince Alexander Mts. of the North Coastal Range to the west. Map kindly produced by Iain Woxvold.
Figure 2 in Avifauna of the Adelbert Mountains, New Guinea: why is Fire-maned Bowerbird Sericulus bakeri the mountains' only endemic bird species?
Figure 2. Presence and absence of Sericulus bowerbirdsȱonȱNewȱGuinea'sȱnorthernȱwatershed,ȱmodifiedȱfromȱ Diamondȱ(1969).ȱEachȱfilledȱdotȱrepresentsȱrecordsȱbyȱoneȱobserver.ȱThereȱareȱonlyȱsevenȱdocumentedȱareasȱ of occurrence of the allospecies Masked Bowerbird S. aureus, numbered from west to east, with observer names in parentheses: 1 = Tamrau Mts. (E. T. Gilliard and B. M. Beehler) and Arfak Mts. (many observers) of the Vogelkop. 2 = Wandammen Mts. (E. Mayr). 3 = Weyland Mts. (F. Shaw-Mayer). 4 = Bernhard Camp (A. Rand). 5 = Foja Mts. (B. M. Beehler and J. Diamond). 6 = Mt. Nibo (J. Diamond). 7 = Mt. Turu (J. Diamond). The asterisk depicts the range of the allospecies Fire-maned Bowerbird S. bakeri in the Adelberts. X = areas surveyedȱintensivelyȱwithoutȱfindingȱanyȱSericulus.? = an undocumented report of S. aureus from the Jimi River.ȱExceptȱforȱtheȱlatter,ȱS. aureus is known mainly from outlying ranges (locations 1, 2, 5, 6 and 7). There are only two documented localities for it in the Central Range (3–4), and there is a large gap between the easternmost record of S. aureus (7) and the range of S. bakeri. The remaining Sericulus allospecies in New Guinea is Flame Bowerbird S. ardens of the southern watershed.
Figure 1 in Avifauna of the Adelbert Mountains, New Guinea: why is Fire-maned Bowerbird Sericulus bakeri the mountains' only endemic bird species?
Figure 1. New Guinea's principal mountain ranges: the Central Range forming New Guinea's backbone; and the ten outlying ranges along the north and north-west coasts, from Huon and Adelbert in the east, to Fakfak and Kumawa in the west.
Figure 20 in Baghuk Mountain (Central Iran): high-resolution stratigraphy of a continuous Central Tethyan Permian-Triassic boundary section
Figure 20. Succession of carbon isotopes (δ13 C) in the Baghuk carb Mountain 1 and C sections (Hambast Formation and Elikah Formation, respectively).
Figure 17 in Baghuk Mountain (Central Iran): high-resolution stratigraphy of a continuous Central Tethyan Permian-Triassic boundary section
Figure 17. Selected nautiloid specimens indicative for the environmental change from the early (d, e) to the late Wuchiapingian (a–c); all specimens stored in the collection of the Museum für Naturkunde, Berlin. (a) Endolobus sp.; specimen MB.C.30223. (b) Metacoceras sp.; specimen MB.C.30224. (c) Pleuronautilus sp.; specimen MB.C.30225. (d) Permonautilus sp.; specimen MB.C.30226. (e) Domatoceras sp.; specimen MB.C.30227. Scale bar units = 1 mm.
Figure 19 in Baghuk Mountain (Central Iran): high-resolution stratigraphy of a continuous Central Tethyan Permian-Triassic boundary section
Figure 19. Polished slab of a mushroom-shaped structure of possible microbial origin, enclosed in a burrowed, partly recrystallized lime mudstone with remains of sponge spicules and small stromatolitic buildups. Scale bar units = 1 mm.
Figure 16 in Baghuk Mountain (Central Iran): high-resolution stratigraphy of a continuous Central Tethyan Permian-Triassic boundary section
Figure 16. Example of ammonoid preservation in the upper Hambast Formation. Cross section of a specimen of Paratirolites sp. from Baghuk Mountain, MB.C.22215; note the different states of preservation of shell walls and septa: a – recrystallized but rather well-preserved shell wall and septa preferably in the mid-dorsal portion of the ammonoid conch; b – dissolved shell wall but sharp demarcation of the ammonoid's internal mould from the sediment at the lower side of the ammonoid conch; c – dissolved shell wall and nearly continuous transition from the ammonoid's internal mould towards the sediment on the upper side of the ammonoid conch (from Leda et al., 2014). Scale bar units = 1 mm.
Figure 6 in Baghuk Mountain (Central Iran): high-resolution stratigraphy of a continuous Central Tethyan Permian-Triassic boundary section
Figure 6. Columnar section of the Hambast Formation at Baghuk Mountain with correlation of the most important index horizons.
Figure 10 in Baghuk Mountain (Central Iran): high-resolution stratigraphy of a continuous Central Tethyan Permian-Triassic boundary section
Figure 10. Slab of a marly shale within the lowermost part of the Baghuk Member with small ammonoids (possibly Arasella sp.). Baghuk Mountain C section, at +0.05 m. Scale bar units = 10 mm.
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