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FIGURE 2 in Late Holocene land vertebrate fauna from Cueva de los Nesofontes, Western Cuba: Stratigraphy, chronology, diversity, and paleoecology
FIGURE 2. Cueva de los Nesofontes indicating geological, stratigraphic, and deposition features. 1, a gallery with main doline or sinkhole indicating areas of fauna collection. Smaller A-D letters pertain to the upper deposits/profiles described here. E-F are two test pits conducted on the lower level. G is the source location for the 14C-dated domestic dog mentioned in the text. 2, the upper area where the main test pits described are located: A is the test pit from 1985, B-C was dug between April 1995 and December 2003. The cross-section a-a' is the approximate source for the stratigraphic profiles illustrated in the following figures. Angles of inclination and heights above the main level are indicated. 3, cross-section (indicated b-b' on 1). Arrows indicate areas of sediment and raptor-derived pellet deposits and roost.
FIGURE 11 in Late Holocene land vertebrate fauna from Cueva de los Nesofontes, Western Cuba: Stratigraphy, chronology, diversity, and paleoecology
FIGURE 11. Plant, invertebrate, and reptile remains. 1-3, Anolis cf. chamaleolis (no. 606), scale bar 10 mm (Level I). 4, unidentified insect extremity ~1 mm (Level IV). 5, photid fly pupa, scale 10 mm (Level IV). 6, fungus spore (?), scale ~50μm. 7, plant seeds, scale 5 mm (All from level II and III). 8-9, seeds, scale 5 mm. 10, leaf fragment, scale ~50 μm (Level II). 11, plant spores, likely a conifer, Pinus? (Level IV), scale ~50μm.
FIGURE 9. Nesophontes left hemimandibles 1-2 in Late Holocene land vertebrate fauna from Cueva de los Nesofontes, Western Cuba: Stratigraphy, chronology, diversity, and paleoecology
FIGURE 9. Nesophontes left hemimandibles 1-2, Nesophontes cf. longirostris. 3, Nesophontes major (image inverted).
FIGURE 13 in Late Holocene land vertebrate fauna from Cueva de los Nesofontes, Western Cuba: Stratigraphy, chronology, diversity, and paleoecology
FIGURE 13. Rarefaction curve of Cueva de los Nesofontes doline test pit D (Levels I–IV) in relation to other Cuban deposits. A, Cueva GEDA, Pinar del Río; B, Cuevas Blancas, Mayabeque; D, The Desmodus deposit described in Orihuela (2010). G, from Gato Jíbaro archaeological deposit described in Orihuela and Tejedor (2012). See text for discussion.
FIGURE 1 in Late Holocene land vertebrate fauna from Cueva de los Nesofontes, Western Cuba: Stratigraphy, chronology, diversity, and paleoecology
FIGURE 1. Location of Loma del Palenque and Cueva de los Nesofontes in northwestern Cuba. 1, Landsat image of the Mayabeque-Matanzas region, indicating the area of the Loma del Palenque (Palenque Hill). 2, Satellite image of Palenque Hill. The asterisks (*) indicate a flat scarp at ~260 m where red-clay soils have formed, are the main source of the allochthonous sediment inside the cave. 3, Map of the Cuban archipelago, indicating the localities mentioned in the text: 1, Cueva El Abrón, GEDA, and Mono Fósil, Pinar del Río; 2, Cueva de Paredones, Artemisa; 3, Cueva del Túnel, Mayabeque; 4, Cuevas Blancas, Mayabeque; 5, Cueva del Gato Jíbaro, Matanzas; 6, Cueva Calero, Matanzas; 7, Breas de San Felipe, and Cuevas de Hato Nuevo, Matanzas; 8, Cueva de los Masones and Jagüey, Trinidad, Las Villas; and 9, Cueva del Indio, Daiquirí, Santiago de Cuba.
FIGURE 10. Bats. 1 in Late Holocene land vertebrate fauna from Cueva de los Nesofontes, Western Cuba: Stratigraphy, chronology, diversity, and paleoecology
FIGURE 10. Bats. 1, left hemimandible of Artibeus anthonyi (no, 1663, lower Level III). 2, ventral view of Phyllops vetus incomplete skull (no. 37, Level II). Both specimens were radiocarbon-dated (14C). 3, four hemimandibles of Antrozous koopmani (no. 20, 75, 1429, 1430 from Levels II and IV, also 14C dated). These specimens were also dated, helping corroborate the chronology discussed. The scale bar equals 10 mm.
FIGURE 7 in Late Holocene land vertebrate fauna from Cueva de los Nesofontes, Western Cuba: Stratigraphy, chronology, diversity, and paleoecology
FIGURE 7. Nesophontes skulls on ventral view. 1-3, Nesophontes cf. longirostris, 3 is the holotype (AMNH 17626). 4-5, Nesophontes major. Small lines indicate discrete characters discussed in the text.
FIGURE 14 in Late Holocene land vertebrate fauna from Cueva de los Nesofontes, Western Cuba: Stratigraphy, chronology, diversity, and paleoecology
FIGURE 14. Carbon stable isotopes signals from Nesophontes (filled square) and Artibeus spp. (open and closed circles), analyzed from bone collagen) at shown intervals.
FIGURE 3 in Recent dispersal and diversification within the clingfish genus Acyrtus (Actinopterygii: Gobiesocidae), with the description of a new western Atlantic species
FIGURE 3 | Bayesian phylogeny of Acyrtus based on the COI gene. Bayesian posterior probability values are shown and the biogeographic province of lineages presented in the right. SWA: southwestern Atlantic; NWA: northwestern Atlantic; EP: eastern Pacific.
FIGURE 1 in Recent dispersal and diversification within the clingfish genus Acyrtus (Actinopterygii: Gobiesocidae), with the description of a new western Atlantic species
FIGURE 1 | Acyrtus simon, holotype CIUFES 2915, 26.41 mm SL. A. Specimen alive, photo taken by J. L. Gasparini in June 2009; B–D. Specimen preserved, photo taken by R. M. Macieira on 31 October 2020. E. X-ray taken by M. M. Mincarone on 11 May 2022.
FIGURE 4 in Recent dispersal and diversification within the clingfish genus Acyrtus (Actinopterygii: Gobiesocidae), with the description of a new western Atlantic species
FIGURE 4 | Bayesian estimates of divergence time based on the mitochondrial COI gene. Posterior probability values reached 1–0.99 for all the main nodes (represented by the orange circle). The horizontal purple bars indicate 95% credibility intervals of node age estimation. The calibration nodes represent the divergence of the last common ancestors between (A) Pseudochromidae + Grammatidae + Gobiesocidae, (B) Grammatidae + Gobiesocidae, (F) all Gobiesocidae species, and (G) Acyrtus + Arcos + Gobiesox (see Conway et al., 2017).
FIGURE 2 in Using community phylogenetics to assess phylogenetic structure in the Fitzcarrald region of Western Amazonia
FIGURE 2 | Ultrametric cladogram of the Fitzcarrald region fish fauna (modified from S2) showing distributions of species in habitats and river basins. Red boxes indicate species presences in: Rivers, Stream, Lakes, Purus, Yuruá, Urubamba and Las Piedras. Note phylogenetic clustering in the Urubamba basin and the stream habitat.
FIGURE 4 in Phylogeography of the banded butterflyfish, Chaetodon striatus, indicates high connectivity between biogeographic provinces and ecosystems in the western Atlantic
FIGURE 4 | Migrate values (number of individuals) and error bars (standard error) of immigration and emigration of individuals of Chaetodon striatus per studied population in the western Atlantic: A. mtDNA concatenated (control region and cyt b) and B. rag 2.
FIGURE 1 in Phylogeography of the banded butterflyfish, Chaetodon striatus, indicates high connectivity between biogeographic provinces and ecosystems in the western Atlantic
FIGURE 1 | Map with all sampling sites along Chaetodon striatus distribution range (red line). Blue color on the map indicates freshwater.
Fig. 1 in Occurrence of the Lime Swallowtail Papilio demoleus Linnaeus, 1758 (Lepidoptera: Papilionidae) in Western Cuba
Fig. 1. Adult Papilio demoleus from Reparto Versalles, La Lisa Municipality, Havana, photographed alive in nature.
Fig. 2 in Occurrence of the Lime Swallowtail Papilio demoleus Linnaeus, 1758 (Lepidoptera: Papilionidae) in Western Cuba
Fig. 2. Geographical distribution of Papilio demoleus in Cuba: previous records (red symbols) and new records (yellow symbols). Image frame = 1,200 x 400 km. New eastern records reduced to selected but actual representative occurrences, in order to avoid an overloaded figure.
Figure 3 in Water mites (Acariformes: Hydrachnidia, Halacaroidea) of bogs of Western Siberia (Russia)
Figure 3. Seasonal dynamics of numbers of water mites and proportion of dominating species in bog No. 2.
Figure 2 in Water mites (Acariformes: Hydrachnidia, Halacaroidea) of bogs of Western Siberia (Russia)
Figure 2. Seasonal dynamics of numbers of water mites and proportion of dominating species in bog No. 1.
Figure 1 in Water mites (Acariformes: Hydrachnidia, Halacaroidea) of bogs of Western Siberia (Russia)
Figure 1. Dendrogram of faunal similarity of the studied bogs. Without taking into account bogs No. 4 and 7, in which one specimen of mites was indicated.
Figure 2 in The connection of the intensity of the plankton community luminescence and the age distribution of horse mackerel in the coastal waters of the south-western Crimea
Figure 2. The average monthly intensity of glow organisms 1 – in the winter (January-February); 2 – in the spring (May); 3 — in the summer (June-July) in the 2010-2015.
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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)
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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.