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Fig. 1 in Moulladella Jourdanensis (Foury & Moullade, 1966) N. Gen., N. Comb.: Valanginian-Early Late Barremian Larger Benthic Foraminifera From The Northern Neotethyan Margin
Fig. 1 Location of the studied sections on the Romanian (A) and Serbian (B) territory showing the occurrence intervals (red lines) of Moulladella jourdanensis (Foury & Moullade) n. gen., nov. comb. A1 – location of the two studied sections in Romania; 1, Reşiţa-Moldova Nouă zone; 2, Dâmbovicioara zone, A2 – Succession of the Lower Cretaceous deposits from the Reşiţa- Moldova Nouă zone (modified from Bucur, 1997): 1, conglomerates and sandstones; 2, alternating sandstones and shales; 3, bedded bioclastic limestones; 4, massive bioclastic limestones; 5, chert-bearing limestones; 6, marly-limestones and marls; 7, micritic limestones; 8, micritic limestones with chert intercalations. A3 – Succession of the Lower Cretaceous deposits from Dâmbovicioara zone (modified from Bucur et al., 2011): 1, alternating marls and limestones; 2, marls with patch-reef limestone intercalations; 3, marly-limestones and marls; 4, glauconite-bearing limestones; 5, bedded limestones; CNM = Cetatea Neamţului Member. B1 – Location of the studied section in Serbia. JRA = Jerma River Area. B2 – Succession of the Lower Cretaceous deposits from the Jerma River Canyon (modified from Bucur et al., 1995): 1, conglomerates, sandstones and shales; 2, bedded limestones.
Fig. 6 in Moulladella Jourdanensis (Foury & Moullade, 1966) N. Gen., N. Comb.: Valanginian-Early Late Barremian Larger Benthic Foraminifera From The Northern Neotethyan Margin
Fig. 6 Moulladella jourdanensis (Foury & Moullade) n. gen., n. comb. (a) Axial section of a megalospheric specimen. (b, f) Subaxial sections. (c–d, g, l) Oblique sections. (e, k, m–n, p) Slightly oblique transverse sections. (h, o) Tangential sections. (i–j) Tangential-oblique sections. Central zone highlighted in grey. b, beam; d,?deuteroconch; f, foramen; is, initial spire; p, proloculus; s, septum. Thin-sections: 14098-4 (a, c), 12568-4 (b), 12562-2 (d), 9-Mandrisag (e), 272-Ciclova (f), 4222- Ilidia (g), M10-Crivina (h), 14729 (i, l), 14734 (j–k), Lo 11 (m–n), 14733 (o). Location and age: (a-d) Dâmbovicioara area, Southern Carpathian, Romania (Early Valanginian); (e-h) Reşiţa-Moldova Nouă zone, Southern Carpathians, Romania (Early Barremian); (i-l, o) Jerma River Canyon, Eastern Serbia (Early Valanginian); (m-n) Losenstein, Northern Calcareous Alps, Austria (Early Barremian, cobbles in Albian-Cenomanian conglomerates).
Figure 5 in Temporal variability of the macroinvertebrate community associated with Eichhornia azurea (Swarts) Kunth (Pontederiaceae) in a lake marginal to a tropical river
Figure 5. Relative contribution (%) of taxa to the total density (expressed in ind.gDW–1) of the macroinvertebrate community associated with E. azurea in Barbosa Lake during the study period. The group "Others" corresponds to Gomphidae, Leptophlebiidae, Dytiscidae, Noteridae, Belostomatidae, Mesoveliidae, and Veliidae.
Figure 3 in Temporal variability of the macroinvertebrate community associated with Eichhornia azurea (Swarts) Kunth (Pontederiaceae) in a lake marginal to a tropical river
Figure 3. Means and standard deviations of monthly cumulated precipitation values (mm) recorded from 1996 to 2012 (A); monthly accumulated precipitation (mm) (B) and daily water level values (m) (C) recorded in the study site between February 2013 and January 2014.
Retreat of the Greenland Ice Sheet leads to divergent patterns of reconfiguration at its freshwater and tidewater margins
<p>Datasets to accomany paper.</p>
Unraveling the Geodynamic Evolution of the Pre– and Early–Andean Margin: Insights from Numerical Modeling
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Divergent responses of Organic Carbon to Sedimentary Environment Transformation in a River-dominated Marginal Sea
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Strong Lateral Variations of Small-Scale Crustal Scattering across the Eastern Margin of the Tibetan Plateau: Implications for Geodynamic Processes [Dataset]
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Dataset for the paper: Factors influencing sea-ice algae abundance, community composition, and distribution in the marginal ice zone of the Southern Ocean during winter.
<p>Dataset for the paper: Factors influencing sea-ice algae abundance, community composition, and distribution in the marginal ice zone of the Southern Ocean during winter. </p> <p> </p>
Fig. 3 in Asymmetry of the Sutural Margins of Elytra: Implications for the Generic Classification of Haliplidae (Coleoptera)
Fig. 3. The number of genera as a function of the proportion of sinistral specimens for
Fig. 2 in Asymmetry of the Sutural Margins of Elytra: Implications for the Generic Classification of Haliplidae (Coleoptera)
Fig. 2. The number of species as a function of the proportion of sinistral specimens for
Fig. 1 in Asymmetry of the Sutural Margins of Elytra: Implications for the Generic Classification of Haliplidae (Coleoptera)
Fig. 1. Transverse cross-sections through the elytral margins at approximately mid-
Fig. 5 in Tectonic history and the biogeography of the freshwater fishes from the coastal drainages of eastern Brazil: an example of faunal evolution associated with a divergent continental margin
Fig. 5. Schematic diagram of origin and erosional SE-NW retreat of Serra do Mar coastal range in region between inland Paraná basin, and the Santos basin, coast of SE Brazil. 1- Eroded Senonian uplift, allowing deposition in both Santos and Paraná basins. Alkaline volcanism (A); Santos Fault (F). 2- Development of the Japi Erosional Surface at the end of Senonian. 3- Paleocene deformation of the Japi Surface (isostatic adjustment). Serra do Mar (SM) is generated at Santos Fault (F), system of continental rifts originated and continental platform formed in coast (P). 4- Erosional retreat (R) of Serra do Mar toward present position. The approximate position of Depressão Periférica is indicated (DP). Alkaline intrusions represent islands. Conventions: 1. Santos formation deposits, 2. Phanerozoic cover beneath the Serra Geral basalt, 3. Serra Geral Formation, 4. Alkaline bodies, 5. Bauru Group, 6. Faults (fromAlmeida & Carneiro, 1998).
Fig. 1 in Tectonic history and the biogeography of the freshwater fishes from the coastal drainages of eastern Brazil: an example of faunal evolution associated with a divergent continental margin
Fig. 1. Crustal provinces of South America. I – South American Platform; II – Patagonian massif; III – Andean orogenic belt; IV – foreland basins; AM = Amazon craton; SL = São Luis craton; SF = São Francisco craton; LA = Luiz Alves craton; RP = Rio de la Plata craton; B = Borborema province; T = Tocantins province; M = Mantiqueira province; DF = Dom Feliciano belt. (Modified from Cordani et al., 2000 and Cordani & Sato, 1999).
FIGURE 6 in New species and records of Chasmogenus Sharp, 1882 from the southwestern margin of the Guiana Shield (Coleoptera: Hydrophilidae: Acidocerinae)
FIGURE 6: Distribution of new Chasmogenus spp.
Figure 4 from: Corbera J (2012) Rare and new cumaceans (Crustacea, Peracarida) from the southern margin of the Cap Ferret Canyon (Bay of Biscay). ZooKeys 235: 73-85. https://doi.org/10.3897/zookeys.235.4027
Figure 4 - Ithyleucon sorbei gen. et sp. n. preadult female paratype (ICMU12101902): A maxilliped 3 B pereopod 1 C pereopod 2 D pereopod 3 E pereopod 4 F pereopod 5 G uropod.
Figure 1 from: Corbera J (2012) Rare and new cumaceans (Crustacea, Peracarida) from the southern margin of the Cap Ferret Canyon (Bay of Biscay). ZooKeys 235: 73-85. https://doi.org/10.3897/zookeys.235.4027
Figure 1 - Hemilamprops normani Bonnier, 1896: A preadult female, telson and left uropod peduncle B manca, telson and right uropod. Mesolamprops denticulatus Ledoyer, 1983 C preadult female, telson and right uropod. Scale bar: 0.2 mm.
Figure 3 from: Corbera J (2012) Rare and new cumaceans (Crustacea, Peracarida) from the southern margin of the Cap Ferret Canyon (Bay of Biscay). ZooKeys 235: 73-85. https://doi.org/10.3897/zookeys.235.4027
Figure 3 - Ithyleucon sorbei gen. et sp. n. preadult female paratype (ICMU12101902): A antenna 1 B antenna 2 C left mandible D maxilla 1 E maxilla 2 F maxilliped 1 G maxilliped 2.
Figure 5 from: Corbera J (2012) Rare and new cumaceans (Crustacea, Peracarida) from the southern margin of the Cap Ferret Canyon (Bay of Biscay). ZooKeys 235: 73-85. https://doi.org/10.3897/zookeys.235.4027
Figure 5 - Schizocuma spinoculatum (Jones, 1984): A carapace in lateral view B uropod. Schizocuma molosa (Zimmer, 1907) from Bellingshausen Sea, Antarctica: C carapace in lateral view D uropod.
Figure 2 from: Corbera J (2012) Rare and new cumaceans (Crustacea, Peracarida) from the southern margin of the Cap Ferret Canyon (Bay of Biscay). ZooKeys 235: 73-85. https://doi.org/10.3897/zookeys.235.4027
Figure 2 - Ithyleucon sorbei gen. et sp. n. A preadult female holotype (ICMU12101901), whole animal in lateral view B preadult male paratype (ICMU12101904) C carapace of immature male paratype (ICMU12101906).
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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.