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FIGURE 9 in On the "screamer-like" birds from the British London Clay: An archaic anseriform-galliform mosaic and a non-galloanserine "barb-necked" species of Perplexicervix
FIGURE 9. Comparison of selected skeletal elements of Perplexicervix paucituberculata, sp. nov. and Eupodotis senegalensis (Otidiformes) to illustrate similar proportions and morphologies. A‒C, E. senegalensis (SMF 21520), first three cervical vertebrae (A), left coracoid (B), and right humerus (C). D‒G, P. paucituberculata, sp. nov., first three cervical vertebrae (D), left coracoid (E), and proximal and distal ends of right humerus (F, G) (D: holotype, NMS.Z.2021.40.7; E, F: tentatively referred specimen NMS.Z.2021.40.91; G: tentatively referred specimen NMS.Z.2021.40.92). Abbreviations: cbp, crista bicipitalis; cdd, condylus dorsalis; cdv, condylus ventralis; cph, caput humeri; ppc, processus procoracoideus. The scale bars equal 10 mm.
FIGURE 1 in On the "screamer-like" birds from the British London Clay: An archaic anseriform-galliform mosaic and a non-galloanserine "barb-necked" species of Perplexicervix
FIGURE 1. Overview of the main bones preserved in the specimens of Danielsavis nazensis Houde et al., 2023 from the London Clay of Walton-on-the-Naze (Essex, UK). A, holotype, NMS.Z.2021.40.1 (not shown are the radii, which were figured by Houde et al., 2023: figure 5Q, R). B, referred specimen NMS.Z.2021.40.2 (the two separate blocks of matrix containing the beak and the neurocranium, respectively, were assembled for the photo; not shown is the cranial portion of the sternum, which was figured by Houde et al., 2023: figure 7E, F). C, referred specimen NMS.Z.2021.40.3. D, referred specimen NMS.Z.2021.40.6. Abbreviations: for, foramen piercing skull roof; wdn, widening of scapus claviculae. The scale bars equal 10 mm.
FIGURE 4 in On the "screamer-like" birds from the British London Clay: An archaic anseriform-galliform mosaic and a non-galloanserine "barb-necked" species of Perplexicervix
FIGURE 4. Danielsavis nazensis Houde et al., 2023, comparison of the vertebrae with those of other galloanserine birds. A, D. nazensis, cranialmost five cervical vertebrae (atlas: NMS.Z.2021.40.1; axis, third, and fourth vertebra: NMS.Z.2021.40.2; fifth vertebra: NMS.Z.2021.40.3). B‒D, cranialmost five cervical vertebrae of B, Chauna torquata (Anhimidae, Anseriformes; SMF 11885); C, Dendrocygna arborea (Anatidae, Anseriformes; SMF 6591); D, Alectura lathami (Megapodiidae, Galliformes; SMF 7243). E, D. nazensis, selected cervical and thoracic vertebrae of the holotype (NMS.Z.2021.40.1); the arrows denote enlarged details of the bones to show irregular lamellate projections. F‒I, axis in lateral view of F, D. nazensis (NMS.Z.2021.40.2); G, C. torquata (SMF 11885); H, D. arborea (SMF 6591); I, A. lathami (SMF 7243). J, D. nazensis, fourth cervical vertebra of the holotype (NMS.Z.2021.40.1) in dorsal and lateral view. K, D. nazensis, fourth cervical vertebra of the referred specimen NMS.Z.2021.40.2 in dorsal and lateral view. L, D. nazensis, thoracic vertebra in lateral view (NMS.Z.2021.40.3). Abbreviations: dns, dens; for, foramen; ftv, foramen transversarium; ntc, notch; ote, ossified tendons; pno, pneumatic opening; ptr, processus transversus; pvt, processus ventralis; zcd, zygapophysis caudalis; zcr, zygapophysis cranialis. The scale bars equal 5 mm.
FIGURE 11 in On the "screamer-like" birds from the British London Clay: An archaic anseriform-galliform mosaic and a non-galloanserine "barb-necked" species of Perplexicervix
FIGURE 11. Results of the analysis of the emended dataset 1 of Houde et al. (2023). A, strict consensus tree of three most parsimonious trees (length = 317, consistency index = 0.69, retention index = 0.50). B, majority rule consensus tree with values indicating the percentage of trees in which the respective node is retained.
FIGURE 3 in On the "screamer-like" birds from the British London Clay: An archaic anseriform-galliform mosaic and a non-galloanserine "barb-necked" species of Perplexicervix
FIGURE 3. Cranial elements and hyoid bone of Danielsavis nazensis Houde et al., 2023 in comparison with those of other galloanserine birds. A‒F, D. nazensis (holotype, NMS.Z.2021.40.1), right (A‒D) and left (E, F) quadrate in lateral (A, E), caudal (B), medial (C, F), and ventral (D) view. G, H, D. nazensis (NMS.Z.2021.40.2), left (G) and right (H) quadrate in lateral view. I, J, right quadrate of Pipile jacutinga (Cracidae, Galliformes; SMF 4139) in lateral (I) and medial (J) view. K, L, mirrored left quadrate of Anseranas semipalmata (Anseranatidae, Anseriformes; SMF 11276) in lateral (K) and medial (L) view. M, N, Anachronornis anhimops from the late Paleocene of Wyoming (holotype, coated with ammonium chloride; from Houde et al., 2023: figure 1, published under a CC BY 4.0 license), left quadrate in lateral (M) and medial (N) view. O‒R, D. nazensis (holotype, NMS.Z.2021.40.1), right (O, P) and left (Q, R) pterygoid in dorsal (O, Q) and medial (P, R) view. S, D. nazensis (NMS.Z.2021.40.2), basiurohyal in dorsal view. T, U, D. nazensis (holotype, NMS.Z.2021.40.1), basiurohyal and putative paraglossum in lateral (T) and dorsal (U) view. V, Alectura lathami (Megapodiidae, Galliformes; SMF 19785), basiurohyal and paraglossum in dorsal view. W, Chauna torquata (Anhimidae, Anseriformes; SMF 19920), basiurohyal and paraglossum in dorsal view; the arrow denotes an enlarged detail of the basihyal. X, A. semipalmata (SMF 19902), basiurohyal and paraglossum in dorsal view; the arrow denotes an enlarged detail of the basihyal. Abbreviations: arf, articular facet for pterygoid; bsh, os basihyale; cbr, os ceratobranchiale; cdl, condylus lateralis; cdm, condylus medialis; cdp, condylus pterygoideus; cpo, capitulum oticum; cps, capitulum squamosum; cqj, cotyla quadratojugalis; fab, facies articularis basipterygoidea; fpb, foramen pneumaticum basiorbitale; fpc, foramen pneumaticum caudomediale; fqv, facies quadratojugalis ventralis; orb, processus orbitalis; pgl, os paraglossum; tsc, tuberculum subcapitulare; urh, os urohyale. The scale bars equal 5 mm.
FIGURE 7 in On the "screamer-like" birds from the British London Clay: An archaic anseriform-galliform mosaic and a non-galloanserine "barb-necked" species of Perplexicervix
FIGURE 7. Specimens of Perplexicervix paucituberculata, sp. nov. and Perplexicervix sp. from the early Eocene London Clay of Walton-on-the-Naze (Essex, UK). A, P. paucituberculata, sp. nov. (holotype, NMS.Z.2021.40.7). B, cf. P. paucituberculata, sp. nov. (NMS.Z.2021.40.91). C, cf. P. paucituberculata, sp. nov. (NMS.Z.2021.40.92). D, Perplexicervix sp. (NMS.Z.2021.40.9). E, Perplexicervix sp. (NMS.Z.2021.40.10). Abbreviation: for, foramen perforating caudoventral portion of corpus pygostyli. The scale bars equal 10 mm.
FIGURE 10 in On the "screamer-like" birds from the British London Clay: An archaic anseriform-galliform mosaic and a non-galloanserine "barb-necked" species of Perplexicervix
FIGURE 10. Undetermined birds that were likened to Danielsavis by Houde et al. (2023). A, partial skeleton of Aves indet. A (NMS.Z.2021.40.5). B, C, left tarsometatarsus of Aves indet. A (NMS.Z.2021.40.8) in plantar (B) and dorsal (C) view. D, partial skeleton of Aves indet. B (NMS.Z.2021.40.4). E‒H, right quadrate of Aves indet. A (NMS.Z.2021.40.5) in lateral (E), caudal (F), medial (G), and ventral (H) view. I, J, right pterygoid of Aves indet. B (NMS.Z.2021.40.4) in lateral (I) and dorsal (J) view. K, distal end of right tarsometatarsus of Aves indet. B (NMS.Z.2021.40.4) in distal view. L, distal end of left tarsometatarsus of Aves indet. A (NMS.Z.2021.40.8) in distal view. M, proximal end of left tarsometatarsus of Aves indet. A (NMS.Z.2021.40.8) in proximal view. Abbreviations: cdc, condylus caudalis; cdm, condylus medialis; cdp, condylus pterygoideus; cpo, capitulum oticum; cps, capitulum squamosum; for, foramen; orb, processus orbitalis; tsc, tuberculum subcapitulare. The scale bars equal 10 mm.
FIGURE 6 in On the "screamer-like" birds from the British London Clay: An archaic anseriform-galliform mosaic and a non-galloanserine "barb-necked" species of Perplexicervix
FIGURE 6. Danielsavis nazensis Houde et al., 2023, comparison of tibiotarsus, tarsometatarsus, pedal phalanges with other galloanserine birds. A, D. nazensis (holotype, NMS.Z.2021.40.1), distal end of right tibiotarsus; the arrow denotes an enlarged detail of the bone. B, distal end of right tibiotarsus of the anseriform Saintandrea chenoides from the late Oligocene of France (holotype, NMB Mar. 874e). C, mirrored distal end of left tibiotarsus of an unnamed galliform from the early Eocene of Egem in Belgium (IRSNB Av 168); coated with ammonium chloride. D‒G, D. nazensis (holotype, NMS.Z.2021.40.1), right tarsometatarsus in distal (D), proximal (E), dorsal (F), and plantar (G) view; the arrow denotes an enlarged detail of the proximal end of the bone. H, I, D. nazensis (NMS.Z.2021.40.3), proximal end of right tarsometatarsus in proximal (H) and plantar (I) view. J, D. nazensis (NMS.Z.2021.40.3), distal end of right tarsometatarsus in plantar view; the arrow denotes an enlarged detail of the bone. K, D. nazensis (holotype, NMS.Z.2021.40.1), non-ungual pedal phalanges; the asterisk indicates a mirrored phalanx. L, mirrored left foot of Chauna torquata (Anhimidae, Anseriformes; SMF 19920). M, right foot of Pavo cristatus (Phasianidae, Galliformes; SMF 20342). N, mirrored distal end of left tarsometatarsus of Anachronornis anhimops (holotype, coated with ammonium chloride; from Houde et al., 2023: figure 2, published under a CC BY 4.0 license) in plantar view. The dotted lines in A‒C indicate the midline of the distal tibiotarsus. The arrows in K‒M denote the length of the third phalanx of the fourth toe. Abbreviations: cdl, condylus lateralis; cdm, condylus medialis; cmh, crista medialis hypotarsi; ext, sulcus extensorius; fdl, sulcus for musculus flexor digitorum longus; fhl, sulcus for musculus flexor hallucis longus; ltr, lateral rim of plantar articular surface of trochlea metatarsi III; mdr, medial rim of plantar articular surface of trochlea metatarsi III; pst, pons supratendineus. The scale bars equal 10 mm.
Text-fig. 3. Schematic geological section of the Kristina Mine near Hrádek/N. (state in 1963–1964) – height/length ratio 3:1. Explanations: vertical hatching – lignite seam, seamlet; dotted – coarse-grained sand, pea-gravel; short lines – sandy clay; white – clay; black lines – clay ironstone concretions; black dots – individual fossiliferous horizons designated as (A) plastic clay from the upper part of the main xylitic seam (about 5 m under t of the seam, (B) clay and "Blätterkohle" from the uppermost part of the first seamlet (split off the Main Coal Seam), (C) slightly sandy brown clay under the uppermost part of the Main Coal Seam, (D) base of the sandy clay with large concretions of the clay ironstone above the Main Coal Seam, (E) sandy clay (incl. clay ironstone) supplying most of leaf material with cuticles (F) 1–2 cm thin silty lenticles or thin beds of the sandy clay with xylites and Eomastixia within peagravels and coarse-grained sands, (G) coarse-grained sands with clayish silts with Fagus, Ocotea, Pterocarya, Tectocarya, (H) brown sandy clay underlying the uppermost seamlet, (I) lignite clay, base of the uppermost seamlet (J) Glyptostrobus – "Blätterkohle", base of the uppermost seamlet (according to Holý 1975, modified). in A Review Of The Early Miocene Mastixioid Flora Of The Kristina Mine At Hrádek Nad Nisou In North Bohemia (The Czech Republic)
Text-fig. 3. Schematic geological section of the Kristina Mine near Hrádek/N. (state in 1963–1964) – height/length ratio 3:1. Explanations: vertical hatching – lignite seam, seamlet; dotted – coarse-grained sand, pea-gravel; short lines – sandy clay; white – clay; black lines – clay ironstone concretions; black dots – individual fossiliferous horizons designated as (A) plastic clay from the upper part of the main xylitic seam (about 5 m under t of the seam, (B) clay and "Blätterkohle" from the uppermost part of the first seamlet (split off the Main Coal Seam), (C) slightly sandy brown clay under the uppermost part of the Main Coal Seam, (D) base of the sandy clay with large concretions of the clay ironstone above the Main Coal Seam, (E) sandy clay (incl. clay ironstone) supplying most of leaf material with cuticles (F) 1–2 cm thin silty lenticles or thin beds of the sandy clay with xylites and Eomastixia within peagravels and coarse-grained sands, (G) coarse-grained sands with clayish silts with Fagus, Ocotea, Pterocarya, Tectocarya, (H) brown sandy clay underlying the uppermost seamlet, (I) lignite clay, base of the uppermost seamlet (J) Glyptostrobus – "Blätterkohle", base of the uppermost seamlet (according to Holý 1975, modified).
Text-fig. 1. A – outline map of the Slovak Republic, Gombasek Quarry marked; B – Gombasek needle – Gombasecká ih a in the Gombasek Quarry, the sample was collected at the right side of the pillar; C – typical lithology, gray coloured clay. in Tracing Of Palynomorphs In The Eastern Slovakian Karst
Text-fig. 1. A – outline map of the Slovak Republic, Gombasek Quarry marked; B – Gombasek needle – Gombasecká ih a in the Gombasek Quarry, the sample was collected at the right side of the pillar; C – typical lithology, gray coloured clay.
Text-fig. 6. Geological plan of Malo-Mikhaylovka. 1 – andesito-dacite; 2 – coarse-grained tuff; 3 – argillitic tuffite; 4 – tuffitic sandstone; 5 – lignite, coal clay; 6 – lenses of tuffitic conglomerate; 7 – acidic tuff; 8 – dacite; 9 – andesito-basalt; 10 – basalt; 11 – sandstone; 12 – andesite; 13 – break; 14 – inclination/direction of beds; 15 – plant-bearing levels; 16 – talus. in Mid-Latitude Palaeogene Floras Of Eurasia Bound To Volcanic Settings And Palaeoclimatic Events - Experience Obtained From The Far East Of Russia (Sikhote-Alin') And Central Europe (Bohemian Massif)
Text-fig. 6. Geological plan of Malo-Mikhaylovka. 1 – andesito-dacite; 2 – coarse-grained tuff; 3 – argillitic tuffite; 4 – tuffitic sandstone; 5 – lignite, coal clay; 6 – lenses of tuffitic conglomerate; 7 – acidic tuff; 8 – dacite; 9 – andesito-basalt; 10 – basalt; 11 – sandstone; 12 – andesite; 13 – break; 14 – inclination/direction of beds; 15 – plant-bearing levels; 16 – talus.
Text-fig. 1. Geological section of the south-western coast in the Nakatova Bay, 28 km south of De Kastri village showing interbedding plant-bearing clays with tuffaceus argillites. 1 – tuff; 2 – tuffaceous argillate; 3 – sandy tuffite; 4 – interbed with lignitic fragments in bedded andesite; 5 – tuffitic conglomerate; 6 – basaltoid agglomerate; 7 – unconformity; 8 – plant-bearing level. in Mid-Latitude Palaeogene Floras Of Eurasia Bound To Volcanic Settings And Palaeoclimatic Events - Experience Obtained From The Far East Of Russia (Sikhote-Alin') And Central Europe (Bohemian Massif)
Text-fig. 1. Geological section of the south-western coast in the Nakatova Bay, 28 km south of De Kastri village showing interbedding plant-bearing clays with tuffaceus argillites. 1 – tuff; 2 – tuffaceous argillate; 3 – sandy tuffite; 4 – interbed with lignitic fragments in bedded andesite; 5 – tuffitic conglomerate; 6 – basaltoid agglomerate; 7 – unconformity; 8 – plant-bearing level.
Text-fig. 3 Pollen diagram from the locality of Bohutín. 0-0.01 m – sandy soil mixed with humus, slightly clayey, sample B11; 0.05 m – grey-blue strongly sandy clay, sample B10; 0.10-0.25 m – brown-grey sandy clay with plant remains and mixed with a small amount of peat, sample B9, sample B8 (0.15 m), sample B7 (0.20 m), sample B6 (0.25 m); 0.30-0.35 m – dark sandy clay mixed with peat and plant remains, sample B5, sample B4 (0.35 m); 0.40 m – grey strongly sandy clay mixed with peat, sample B3; 0.45-0.50 m – grey-blue strongly sandy clay, sample B2, sample B1 (0.50 m). in Reconstruction Of Vegetation Development On The Floodplain Of The Litavka River In The Holocene (Central Bohemia, Brdy Mts.)
Text-fig. 3 Pollen diagram from the locality of Bohutín. 0-0.01 m – sandy soil mixed with humus, slightly clayey, sample B11; 0.05 m – grey-blue strongly sandy clay, sample B10; 0.10-0.25 m – brown-grey sandy clay with plant remains and mixed with a small amount of peat, sample B9, sample B8 (0.15 m), sample B7 (0.20 m), sample B6 (0.25 m); 0.30-0.35 m – dark sandy clay mixed with peat and plant remains, sample B5, sample B4 (0.35 m); 0.40 m – grey strongly sandy clay mixed with peat, sample B3; 0.45-0.50 m – grey-blue strongly sandy clay, sample B2, sample B1 (0.50 m).
Text-fig. 3. Cave deposits exposed in Section No. 2 and recorded paleomagnetic polarities. 1 – reworked deposits; 2 – clayey silt, light brown with abundant black dots, structureless; 3 – clayey silt to silty clay, brown, chaotically deposited; 4 – clayey silt, light brown, structureless; 5 – clayey silt, light brown, laminated; 6 – clayey silt to silty clay, brown, structureless; 7 – clayey silt to silty clay, light brown, structureless; 8 – clayey silt, brown with abundant white carbonate clasts; 9 – clayey sandy silt, brown with abundant lighter clayey fragments; 10 – clayey sandy silt, brown with sporadic lighter clayey fragments. Geomagnetic polarity scale: black (N) – normal polarities, white (R) – reversed polarities, grey – intermediate or uninterpretable polarities. For more details see text. in New Updated Results Of Paleomagnetic Dating Of Cave Deposits Exposed In Za Hájovnou Cave, Javoříčko Karst
Text-fig. 3. Cave deposits exposed in Section No. 2 and recorded paleomagnetic polarities. 1 – reworked deposits; 2 – clayey silt, light brown with abundant black dots, structureless; 3 – clayey silt to silty clay, brown, chaotically deposited; 4 – clayey silt, light brown, structureless; 5 – clayey silt, light brown, laminated; 6 – clayey silt to silty clay, brown, structureless; 7 – clayey silt to silty clay, light brown, structureless; 8 – clayey silt, brown with abundant white carbonate clasts; 9 – clayey sandy silt, brown with abundant lighter clayey fragments; 10 – clayey sandy silt, brown with sporadic lighter clayey fragments. Geomagnetic polarity scale: black (N) – normal polarities, white (R) – reversed polarities, grey – intermediate or uninterpretable polarities. For more details see text.
Fig. 6 in A new monofenestratan pterosaur from the Kimmeridge Clay Formation (Kimmeridgian, Upper Jurassic) of Dorset, England
Fig. 6. Variation in cranial angle (subtended between the squamosal−quadrate and jugal−maxilla−premaxilla jaw line from a selection of Jurassic monofenestratans. A. Cuspicephalus scarfi gen et sp. nov. from the Upper Jurassic, Kimmeridge Bay, Dorset. B. Darwinopterus robustodens Lü, Xu, Chang, and Zhang, 2011b. C. Darwinopterus linglongtaensis (Lü, Unwin, Jin, Liu, and Ji, 2010). D. Kunpengopterus sinensis Wang, Kellner, Jiang, Cheng, Meng, and Rodrigues, 2010. E. Pterodactylus antiquus Sömmerring, 1812. F. Germanodactylus cristatus (Wiman, 1925). G. Gnathosaurus subulatus Meyer, 1834. H. "Germanodactylus" rhamphastinus (Wagner, 1851). B after Lü et al. (2011b); C–D after Wang et al. (2010); E–H after Wellnhofer (1970).
Fig. 2. A in A new monofenestratan pterosaur from the Kimmeridge Clay Formation (Kimmeridgian, Upper Jurassic) of Dorset, England
Fig. 2. A monofenestratan pterosaur Cuspicephalus scarfi gen. et sp. nov. from the Upper Jurassic of Kimmeridge Bay, England; MJML K1918. A. Original skull on slab of mudstone, lacking the mandible and dentition. B. Outline diagram of preserved bone. Light grey is bone, dark grey is fibrous bone of sagittal crest, black is dental alveoli where unambiguous. C. Restoration of skull outline, with hypothetical lower jaw. Scale bar 50 mm.
Fig. 5 in A new monofenestratan pterosaur from the Kimmeridge Clay Formation (Kimmeridgian, Upper Jurassic) of Dorset, England
Fig. 5. Sagittal crest of Cuspicephalus scarfi gen. et sp. nov. from the Upper Jurassic, Kimmeridge Bay, Dorset (A) compared with Darwinopterus modularis (Lü, Unwin, Jin, Liu, and Ji, 2010) (B) (from Lü et al. 2009b), Kunpengopterus sinensis Wang, Kellner, Jiang, Cheng, Meng, and Rodrigues, 2010 (C) (based on Wang et al. 2010), Germanodactylus cristatus (Wiman, 1925) (D) (based on Wellnhofer 1970), and the elaborate crestbearing Pterorhynchus wellnhoferi Czerkas and Ji, 2002 (E) (based on Czerkas and Ji 2002). Drawings not to scale.
Fig. 1 in A new monofenestratan pterosaur from the Kimmeridge Clay Formation (Kimmeridgian, Upper Jurassic) of Dorset, England
Fig. 1. Simplified geological map showing the distribution of the Kimmeridge Clay Formation on the Isle of Purbeck and the location of Kimmeridge Bay where Cuspicephalus scarfi was discovered.
Fig. 3. A in A new monofenestratan pterosaur from the Kimmeridge Clay Formation (Kimmeridgian, Upper Jurassic) of Dorset, England
Fig. 3. A monofenestratan pterosaur Cuspicephalus scarfi gen. et sp. nov. from the Upper Jurassic, Kimmeridge Bay, Dorset; MJML K1918. A. Posterior of skull showing near complete orbit. B. Distal tip of rostrum showing anteriorly directed alveolus 1. C. Rostrum anterior of nasoantorbital fenestra. D. Sagittal crest. Scale bars 10 mm.
Fig. 4. A in A new monofenestratan pterosaur from the Kimmeridge Clay Formation (Kimmeridgian, Upper Jurassic) of Dorset, England
Fig. 4. A monofenestratan pterosaur Cuspicephalus scarfi gen et sp. nov. from the Upper Jurassic, Kimmeridge Bay, Dorset; MJML K1918. A. Left exoccipital and occipital condyle. Scale bar 10 mm. B. Outline of right jugal showing triangular shape of anteroventral border of orbit.
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Allen Brain Atlas
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Annotated Behaviour and Observability Dataset (ABODe)
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