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Fig. 8 in The Berriasian-Valanginian And Aptian Deposits From The North-Western Part Of The Piatra Craiului Massif: Stratigraphic Relationships, Facies And Depositional Environments
Fig. 8 Microfossils from the Aptian breccia and conglomerate pebbles in the Padinile Frumoase area. a-c, f, g Unidentified orbitolinids. d Rectodyctioconus giganteus Schroeder. e Mesorbitolina parva (Douglass). h Unidentified?involutinid foraminifer. i Montsalevia salevensis (Charollais, Brönnimann & Zaninetti). j unidentified biserial foraminifer. k Pfenderina neocomiensis (Pfender). l Palorbitolina lenticularis (Blumenbach); m Terebella lapilloides Münster. n Neomeris cretacea Steinmann. o Griphoporella sp. p Carpathoporella occidentalis Dragastan. q Clypeina parasolkani Farinacci & Radoičić. r Lithocodium aggregatum Elliott. s Coscinophragma cribrosa (Reuss). a, b, sample 266; c, e, m, n, p, s, sample 271; d, i, j, k, q, r, sample 275; f, h, o, sample 279; g, sample 272; l, sample 568. Scale bar = 1 mm (a-c, f); 0.5 mm (d, e, g, h, o, q); 0.25 mm (i-m, p).
Fig. 7 in The Berriasian-Valanginian And Aptian Deposits From The North-Western Part Of The Piatra Craiului Massif: Stratigraphic Relationships, Facies And Depositional Environments
Fig. 7 Facies and microfacies from the upper Valanginian (a-b) and Aptian (c-h). a-b Bioclastic intraclastic floatstone. Intraclasts consist of peloidal packstone with echinoderms (a1, b1), bioclastic packstone with sponge spicules and coral fragments (a2), and peloidal packstone with small foraminifera (b2). The matrix (m) contains calpionellids and calcispheres. The arrows in a are delineating the shape of the intraclasts. c Limestone-rich breccia. Clasts are embedded in a micritic/clay-rich matrix that contains silt-sized quartz. The matrix contains orbitolinids (indicated by the small yellow arrows). d Marly clast with bioclasts and glauconite. e Coral-rich bioconstruction with dissolved corals. f Clast containing abundant sponge and Lithocodium crusts (center). In the upper right corner the carbonate components of the clast are dissolved. g Clasts from an orbitolinid-rich peloidal bioclastic grainstone; orbitolinids are present both in the matrix and the clasts. h Clast composed of an orbitolinid/green algae-bearing packstone (left) and clast that contains peloidal fenestral wackestone (right) (detail from photo g). a, b, sample 258; c-f, sample 266; g, h, sample 272. Scale
Fig. 6 in The Berriasian-Valanginian And Aptian Deposits From The North-Western Part Of The Piatra Craiului Massif: Stratigraphic Relationships, Facies And Depositional Environments
Fig. 6 Microfossils from the lower Valanginian limestones and the upper Valanginian limestones/marly-limestones. a-c Pseudocyclammina lituus (Yokoyama); d Coscinoconus cf. cherchiae (Arnaud-Vanneau, Boisseau & Darsac); e-j Montsalevia salevensis (Charollais, Brönnimann & Zaninetti); k-o Meandrospira favrei (Charollais, Brönnimann & Zaninetti); p-s Unidentified calpionellids; t, u Cadosina fusca Wanner; v, w Crustocadosina semiradiata Wanner; x, y Stomiosphaera echinata Nowak. a, h, sample 12817; b, i, sample 256; c, d, sample 257; e, sample 260; f, g, p, u, sample 12818; j, x, y, sample 249; k, r, sample 252; l,q, v, w, sample 12816; m, n, o, s, t, sample 258. Scale bar = 0.5 mm (a-b); 0.25 mm (c-o); 0.125 mm (p-y).
Fig. 3 Padinile Frumoase outcrop a in The Berriasian-Valanginian And Aptian Deposits From The North-Western Part Of The Piatra Craiului Massif: Stratigraphic Relationships, Facies And Depositional Environments
Fig. 3 Padinile Frumoase outcrop a The lower Valanginian-upper Valanginian unconformity (yellow line) and the transgressive contact between the Valanginian limestones and the Aptian deposits (breccia and conglomerates) (white line). b Monomictic breccia. c The first outcrop located above the contact area (~3m). d Monomictic orthoconglomerates with common carbonate pebbles. e Monomictic paraconglomerates with carbonate pebbles. 272, 280, 291 = sample numbers. Scale bar for b, d, e = 2 cm.
Fig. 5 in The Berriasian-Valanginian And Aptian Deposits From The North-Western Part Of The Piatra Craiului Massif: Stratigraphic Relationships, Facies And Depositional Environments
Fig. 5 Lower Valanginian limestones and upper Valanginian limestones/marly-limestones (enlargement view of the left area in Fig. 3a). a The unconformity between the lower Valanginian limestones and upper Valanginian limestones/marly limestones (yellow line). The thin-bedded upper Valanginian carbonate beds are lying over thick-bedded shallow-water lower Valanginian limestones. b Bioclastic intraclastic grainstone; note the presence of dissolution structures filled with vadous silt. c Peloidal bioclastic packstone with dissolution structures. d Bioclastic wackestone passing to a peloidal bioclastic packstone. e, f Peloidal bioclastic packstone, with sintaxial overgrowth cement being developed on the echinoderm plates. g Peloidal bioclastic packstone/grainstone with Lithocodium nodules. b, c, sample 12817; d, e, sample 12816; f, sample 11827; g, sample 12819. Scale bar = 1 mm (b-g).
Fig. 10 in The Berriasian-Valanginian And Aptian Deposits From The North-Western Part Of The Piatra Craiului Massif: Stratigraphic Relationships, Facies And Depositional Environments
Fig. 10 Microfacies and microfossils identified in the limestone pebbles of the Aptian breccia and conglomerates from the Drumul lui Lehman section. a Bioclastic intraclastic floatstone with intraclasts of bioclastic wackestone; the matrix contains orbitolinids, echinoderm plates and silt-sized quartz extraclast. b Intraclasts composed of fenestral wackestone and peloidal fenestral grainstone. c Pebbles originating form reefal bioconstructions. The corals are encrusted by microproblematic organisms. d Rudist fragment and sponges (chaetetids). e Pebble consisting of a peloidal bioclastic packstone with?Vercorsella sp. (indicated by the arrows). f Carbonate pebble with dissolution structures; cavities are bordered by fine crystalline, schalenoedric cements. The interior is filled with clay minerals and iron oxides. g Pebble consisting of a peloidal fenestral packstone; the fenestral structures are filled with vadous silt and sediment derived from the breccia's matrix. h Intensely dissolved carbonate clasts; the clasts and the cavities are bordered by fine crystalline, schalenoedric cement. a,
Fig. 1 in The Berriasian-Valanginian And Aptian Deposits From The North-Western Part Of The Piatra Craiului Massif: Stratigraphic Relationships, Facies And Depositional Environments
Fig. 1 Location of the Aptian deposits on the geological map of the northern part of the Piatra Craiului Massif [based on the maps 1:50000, sheets110a to 110d (Dimitrescu et al., 1971; Patrulius et al., 1971; Săndulescu et al., 1972; Dimitrescu et al., 1974), redrawn with minor changes]
Fig. 1 in Anthropozoonotic significance, risk factors and spatial distribution of Giardia spp. infections in quenda (Isoodon obesulus) in the greater Perth region, Western Australia
Fig. 1. Geographical distribution of Giardia spp. infection in Perth quenda. Quenda were mapped using the GPS position of the location at which they were trapped. GPS points are jittered, and icons for uninfected quenda are 50% transparent, to improve visualisation of the relative distribution of Giardia spp. infection. By Kulldorff's spatial scan statistic, the circle in the north-west region represents a cluster of relatively decreased Giardia spp. infection risk in Perth quenda (OR of infection <0.001, compared to quenda trapped elsewhere in Perth; p <0.001).
Figure 4 in New record of an oyster species from Chilika Lagoon, Odisha, north-western Bay of Bengal
Figure 4. Ligament area, hinge dentition and white layer showing layer of mother pearl in I. ephippium.
Figure 6 in New record of an oyster species from Chilika Lagoon, Odisha, north-western Bay of Bengal
Figure 6. Sessile organisms on the shell of I. ephippium. A. Calcareous tube of marine polychaeta, B. Gastropod full egg capsule, C. Reminiscent of attached bivalve and barnacles, D. Empty gastropods egg capsule over oyster shell collected from "Arakhkuda" region.
Figure 3 in New record of an oyster species from Chilika Lagoon, Odisha, north-western Bay of Bengal
Figure 3. (A&B). Exterior of the Bivalve Isognomon ephippium, (C&D). Internal part of I. ephippium.
Figure 5. A in New record of an oyster species from Chilika Lagoon, Odisha, north-western Bay of Bengal
Figure 5. A. Mangrove vegetation at outer channel area of Chilika lagoon. B. Large bivalve colony exposed during low tide period at mangrove vegetation of "Bhabakundaleswar" region, C. Occurrence of multiple colonies of Isognomon ephippium in the sea grass bed at "Arakhkuda", D. Single colony of I.ephippium from mangrove vegetation.
Figure 6 in Taxonomic reassessment of Eutropis macularia (Blyth, 1853) complex in the Western Ghats of India: Resurrection of Eutropis brevis (Günther, 1875), Eutropis dawsoni (Annandale, 1909) and synonymisation of Eutropis gansi (Das, 1991) (Reptilia: Squamata: Scincidae)
Figure 6. Profile photographs comparing the dorsal scales of (1) Eutropis macularia, (2) Eutropis brevis, and (3) Eutropis dawsoni. Note the differences in keel projections and scale differences. Images of type specimens – (A) Eutropis macularia (Holotype – ZSI 2344) (B, C & D) Eutropis brevis (Syntypes – NHMUK 1874.4.29.254-55 & 354) (E) Eutropis gansi (Holotype – ZSI 24826), and (F) Eutropis dawsonii (Lectotype – ZSI 16170).
Figure 1 in Taxonomic reassessment of Eutropis macularia (Blyth, 1853) complex in the Western Ghats of India: Resurrection of Eutropis brevis (Günther, 1875), Eutropis dawsoni (Annandale, 1909) and synonymisation of Eutropis gansi (Das, 1991) (Reptilia: Squamata: Scincidae)
Figure 1. Principal component analysis plot showing distinct clustering in Eutropis dawsoni near topotypical E. macularia and E. brevis.
Figures 9-16 in A new species of Choroterpes Eaton, 1881 (Ephemeroptera: Leptophlebiidae: Atalophlebiinae) from Western Himalaya, India
Figures 9-16. Larvae of Choroperpes (Choroterpes) girigangaensis sp. nov. 9. Maxilla; 10. Labium; 11. Foreleg; 12. Midleg; 13. Hindleg; 14. Hind tibia; 15. Hind tarsi. 16. Claw.
Figures 17-22 in A new species of Choroterpes Eaton, 1881 (Ephemeroptera: Leptophlebiidae: Atalophlebiinae) from Western Himalaya, India
Figures 17-22. Larvae of Choroperpes (Choroterpes) girigangaensis sp. nov. 17. Gill I; 18. Gill II; 19. Gill V; 20. Gill VI; 21. Gill VII; 22. Ventral view of segment VIII–X.
Plate 1 in Genitalic studies of four Limacodid species (Limacodidae Lepidoptera) including the description of a new species from Western Ghats, India
Plate 1. Aergina hilaris (Westwood): (A-B) adults, (C) male genitalia (ventral view), (D) aedeagus, (E-F) uncus, (G) female genitalia.
Plate 4 in Genitalic studies of four Limacodid species (Limacodidae Lepidoptera) including the description of a new species from Western Ghats, India
Plate 4. Parasa neoherbifera sp. nov.: (A) adult, (B) male genitalia (ventral view), (C) aedeagus, (D) Uncus, (E) valva, (F) uncus and gnathos (lateral view).
Plate 3 in Genitalic studies of four Limacodid species (Limacodidae Lepidoptera) including the description of a new species from Western Ghats, India
Plate 3. Parasa herbifera Walker: (A) adult, (B) male genitalia (ventral view), (C) aedeagus, (D) uncus, (E) valva, (F) uncus and gnathos (lateral view).
Figures 1-8 in A new species of Choroterpes Eaton, 1881 (Ephemeroptera: Leptophlebiidae: Atalophlebiinae) from Western Himalaya, India
Figures 1-8. Larvae of Choroperpes (Choroterpes) girigangaensis sp. nov. 1. Dorsal view; 2. Ventral view; 3. Labrum; 4. Labrum emargination; 5. Labrum emargination with unequal denticles 6. Hypopharynx; 7. Left mandible; 8. Right mandible.
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Allen Brain Atlas
Allen Brain Atlas is an Allen Institute collection of brain map atlases, datasets, APIs, and analysis tools covering mouse, human, and non-human primate brain resources.
Annotated Behaviour and Observability Dataset (ABODe)
ABODe is a University of Edinburgh DataShare dataset for behavior classification in group-housed mice using home-cage video, identities, bounding boxes, ground-plate positions, and annotator labels.
DANDI Archive for NWB datasets
DANDI is a BRAIN Initiative archive for publishing and sharing neurophysiology data, including electrophysiology, optophysiology, and behavioral data packaged as NWB and related standards.
International Brain Laboratory public data
The International Brain Laboratory public data releases expose standardized mouse decision-making experiments, including Neuropixels recordings, widefield calcium imaging, behavior, and session metadata accessed through the ONE API.
OpenNeuro
OpenNeuro is a free, open platform for sharing neuroimaging datasets, with public search, dataset pages, and download paths for web, S3, DataLad, and the OpenNeuro CLI.