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Fig. 6 in Observation Of Eurasian Otter'S Diel Activity Using Camera Trapping In Central-Eastern Romania
Fig. 6. Seasonal activity patterns of Lutra lutra in the study area during the study period based on the number of otter crossings through the observation sites.
UAS survey on a small earthen dam in Romania
<p>The present dataset provides the UAS imagery and the GPCs of a survey carried out within the HARMONIOUS COST Action on the earthen dam of Pischia in Romania. The subset could be used to test SfM methods and the results can be compared with those provided on the manuscript by Manfreda et al. (2019). It important to clarify that this is just a subset of the series of surveys described in the mentioned manuscript and is made available for training exercises. </p> <p>Reference</p> <p>Manfreda, S., P. Dvorak, J. Mullerova, S. Herban, P. Vuono, J.J. Arranz Justel, M. Perks, <strong>Assessing the Accuracy of Digital Surface Models Derived from Optical Imagery Acquired with Unmanned Aerial Systems</strong>, <strong>Drones</strong>, 3(1), 15; (doi: 10.3390/drones3010015), 2019.</p>
Fireball events detected in Romania by the FRIPON-MOROI network
<p>In this table we present the fireball events detected by the Fireball Recovery and Inter Planetary Observation Network (FRIPON) (Colas et al., 2020) with the use of the Meteorite Orbits Reconstruction by Optical Imaging (MOROI) network (Nedelcu et al. 2018). The data include events recorded by at least two different fireball cameras installed over the Romanian territory. For each event we provide: the name, the stations that detected it, whether it has noticeable deceleration (V<sub>f</sub>/V<sub>0</sub> < 0.8, where V<sub>f</sub> is the velocity of the meteoroid at the end of the luminous trajectory and V<sub>0</sub> is the initial velocity of the meteoroid).</p> <p>The events are named by the time when they were captured as follows: year, month, day followed by hour, minute, second in UT.</p> <p><strong>The events with noticeable deceleration are analysed in (Boaca et al. 2022), https://iopscience.iop.org/article/10.3847/1538-4357/ac8542.<br> If using this data, please reference the above publication. </strong></p> <p><em>The online presentation of the paper can be found on the AAS youtube channel:</em></p> <p>https://www.youtube.com/watch?v=Wx186QB5ZVE</p> <p> </p>
FRIPON (MOROI) Stations installed in Romania and coordinates
<p>In this table we present the coordinates all-sky cameras of The Fireball Recovery and Inter Planetary Observation Network (FRIPON) (Colas et al., 2020) installed over the Romanian territory with the use of the Meteorite Orbits Reconstruction by Optical Imaging (MOROI) network (Nedelcu et al. 2018). Those cameras were installed over the course of the year 2021.</p> <p>The detection of meteors is made with the use of fish-eye lens with the focal length of 1.25 mm and the detector Sony ICX445.</p> <p><strong>Detections made by the FRIPON-MOROI cameras over the time period January 2021 - April 2022 are characterised in (Boaca et al. 2022)</strong> (https://iopscience.iop.org/article/10.3847/1538-4357/ac8542 ).</p> <p><strong>If using this data, please reference the above publication. </strong></p> <p><em>The online presentation of the paper can be found on the AAS youtube channel</em></p> <p>(https://www.youtube.com/watch?v=Wx186QB5ZVE).</p>
FIGURE 21 in Spatial And Temporal Distribution Of The Island-Dwelling Kogaionidae (Mammalia, Multituberculata) In The Uppermost Cretaceous Of Transylvania (Western Romania)
FIGURE 21. Latest Cretaceous Transylvanian kogaionid occurrences, highlighting the spatial distribution of the different chronofaunal tiers represented. Numbers within kogaionid silhouettes refer to their respective tiers (see fig. 3). A. Hațeg Basin; B. southwestern Transylvanian Basin; C. Rusca Montană Basin.
FIGURE 23 in Spatial And Temporal Distribution Of The Island-Dwelling Kogaionidae (Mammalia, Multituberculata) In The Uppermost Cretaceous Of Transylvania (Western Romania)
FIGURE 23. Chronostratigraphic distribution of the sedimentary facies represented, combined with the nature of the kogaionid remains recovered, at the different uppermost Cretaceous Transylvanian kogaionid sites. Dark gray, marine deposits; light gray, continental deposits.
FIGURE 22 in Spatial And Temporal Distribution Of The Island-Dwelling Kogaionidae (Mammalia, Multituberculata) In The Uppermost Cretaceous Of Transylvania (Western Romania)
FIGURE 22. Chronostratigraphic distribution of the estimated body sizes of known latest Cretaceous Transylvanian kogaionid occurrences. Dark gray, marine deposits; light gray, continental deposits.
FIGURE 20 in Spatial And Temporal Distribution Of The Island-Dwelling Kogaionidae (Mammalia, Multituberculata) In The Uppermost Cretaceous Of Transylvania (Western Romania)
FIGURE 20. Chronostratigraphic distribution of the different kogaionid taxa identified in the uppermost Cretaceous beds of Transylvania. Dark gray, marine deposits; light gray, continental deposits. For color-coding of the taxa, see legend in figure 19.
FIGURE 12 in Spatial And Temporal Distribution Of The Island-Dwelling Kogaionidae (Mammalia, Multituberculata) In The Uppermost Cretaceous Of Transylvania (Western Romania)
FIGURE 12. In situ remains of the referred specimen of Barbatodon transylvanicus, LPB (FGGUB) M.1635, Pui Beds, site PB3, documenting their associated nature. A. Remains of M.1635 as first spotted in the field, July 2002, showing the dentaries and one of the femora exposed on the bed surface by river erosion. B. Closeup from the initial preparation stage of the plaster jacket containing the partial skeleton M.1635, with the fully exposed dentaries and right femur. C. Presence of further postcranial remains revealed within the plaster jacket; boxed area in left center (B) highlights the position of the first discovered remains. Abbreviations: de, dentary; fe, femur; fi, fibula; l, left; r, right.
FIGURE 14 in Spatial And Temporal Distribution Of The Island-Dwelling Kogaionidae (Mammalia, Multituberculata) In The Uppermost Cretaceous Of Transylvania (Western Romania)
FIGURE 14. Isolated kogaionid teeth from the Pui Beds, site PB4. A–C. Isolated left I2, LPB (FGGUB) M.1706, in A. labial, B. distal, and C. mesial views. D–F. Isolated left I3, LPB (FGGUB) M.1670, in D. mesial, E. labial, and F. distal views. Arrows in B, C, and F point to the demarcation line between thicker and thinner enamel cover. G. Isolated left M1, LPB (FGGUB) M.1671, in occlusal view. H. Holotype of Litovoi tholocephalos, LPB (FGGUB) M.1700, left M1 in occlusal view, for comparison.
FIGURE 16 in Spatial And Temporal Distribution Of The Island-Dwelling Kogaionidae (Mammalia, Multituberculata) In The Uppermost Cretaceous Of Transylvania (Western Romania)
FIGURE 16. Kogaionid-bearing fossiliferous localities from the Densuș-Ciula Formation, Hațeg Basin. A. The Tuștea-Oltoane nesting locality, corresponding to site DC1; large-scale excavation on the newly created platform, August 1998. B. Close-up of the fossiliferous bed at Vălioara-Fântânele, hosting site DC2; C. Close-up of the fossiliferous bed at Vălioara-Fântânele 2, location of site DC3. D. Ravines north of Livezi with outcrops of uppermost Cretaceous continental beds; in the middle foreground, below the grass cover, is site DC4; E. Limited exposures of the uppermost Cretaceous continental beds north of General Berthelot, locality GB1, with the lower red silty mudstones hosting site DC5.
FIGURE 19 in Spatial And Temporal Distribution Of The Island-Dwelling Kogaionidae (Mammalia, Multituberculata) In The Uppermost Cretaceous Of Transylvania (Western Romania)
FIGURE 19. Latest Cretaceous Transylvanian kogaionid occurrences, highlighting the spatial distribution of the different taxa; estimated body sizes taken from figure 18. A. Hațeg Basin; B. southwestern Transylvanian Basin; C. Rusca Montană Basin. Question-mark refers to taxonomical uncertainty concerning the small kogaionid taxon from site RB1, in the Hațeg Basin.
FIGURE 9 in Spatial And Temporal Distribution Of The Island-Dwelling Kogaionidae (Mammalia, Multituberculata) In The Uppermost Cretaceous Of Transylvania (Western Romania)
FIGURE 9. Kogaionid remains from the Sînpetru Formation. A. Close-up of the left upper molars (M1 and M2) of Kogaionon ungureanui (ISER SPT/001), site SP1. B, C. Isolated right M2, LPB (FGGUB) M.1631, of an indeterminate kogaionid, site SP3, occlusal view as B. reflected light stereomicroscopic image; C. SEM image.
FIGURE 18 in Spatial And Temporal Distribution Of The Island-Dwelling Kogaionidae (Mammalia, Multituberculata) In The Uppermost Cretaceous Of Transylvania (Western Romania)
FIGURE 18. Latest Cretaceous Transylvanian kogaionid occurrences, highlighting the spatial distribution of their estimated body size (see text and figure 2 for identity of the fossiliferous sites marked in red in figures 18–23; see text and tables 4–7 for details of body size estimates). A. Hațeg Basin; B. southwestern Transylvanian Basin; C. Rusca Montană Basin.
FIGURE 5 in Spatial And Temporal Distribution Of The Island-Dwelling Kogaionidae (Mammalia, Multituberculata) In The Uppermost Cretaceous Of Transylvania (Western Romania)
FIGURE 5. Craniodental morphology of the Kogaionidae. Skull structure in dorsal view (A, B, D, E) and occlusal view of upper dentition (C, F) in different kogaionid genera (skulls and tooth rows, respectively, drawn to the same scale). A, B. Skull of Litovoi tholocephalos, A. Reconstructed, with missing elements (shaded) mirrored from their counterparts, and B. Simplified outline drawing (from Csiki-Sava et al., 2018). C. Left-side upper dentition of Litovoi tholocephalos (from Csiki-Sava et al., 2018). D. Skull of Kogaionon ungureanui, simplified outline drawing (from Rădulescu and Samson, 1996: Kielan-Jaworowska et al., 2004). E. Skull of Barbatodon transylvanicus, simplified outline drawing (from Smith and Codrea, 2015). F. Left-side upper dentition of Kogaionon ungureanui, in occlusal view (from Rădulescu and Samson, 1996).
FIGURE 3 in Spatial And Temporal Distribution Of The Island-Dwelling Kogaionidae (Mammalia, Multituberculata) In The Uppermost Cretaceous Of Transylvania (Western Romania)
FIGURE 3. Approximate chronostratigraphic distribution of the latest Cretaceous kogaionid occurrences from the Transylvanian area (red stars), alongside other important fossil sites (gray stars) using the biochronofaunal tier system developed by Csiki-Sava et al. (2016), in the main kogaionid-bearing successions: A, the Sînpetru Formation (SP sites); B, the Râul Mare Beds (RB sites); C, the Pui Beds (PB sites); D, the Densuș-Ciula Formation (DC sites), all in the Hațeg Basin; E, the Rusca Montană Basin (RM sites); F, the southwestern Transylvanian Basin, eastern (left column) and western (right column) outcropping areas (TB sites); dark gray, marine deposits; light gray, continental deposits. For kogaionid site abbreviations, see text and figure 2; for other abbreviations, see Csiki-Sava et al. (2016) and Botfalvai et al. (2021). Question mark added in the Râul Mare Beds succession reflects current lack of details as to the relative straigraphic positions of sites RB2 and RB3 (see text).
FIGURE 11 in Spatial And Temporal Distribution Of The Island-Dwelling Kogaionidae (Mammalia, Multituberculata) In The Uppermost Cretaceous Of Transylvania (Western Romania)
FIGURE 11. Isolated kogaionid incisors from the Pui Beds, site PB1. A–E, Isolated left i1, ISER PUI.004, of an indeterminate kogaionid, A. Specimen identified as "ptilodontoid," puncturing-grasping type of i1; drawing from Rădulescu and Samson (1997). B. apical, C. labial, D. dorsal, and E. lingual views. F. Holotype of Litovoi tholocephalos, LPB (FGGUB) M.1700, left i1 in lingual view, for comparison. G–K, Isolated left I2, ISER PUI.003, of an indeterminate kogaionid, G. Specimen identified as "taeniolabidoid," gnawing type of i1; drawing from Rădulescu and Samson (1997), H. apical, I. labial, J. dorsal, and K. lingual views. L. Holotype of Litovoi tholocephalos, LPB (FGGUB) M.1700, right premaxilla with in situ I2–I3 in labial view, for comparison.
FIGURE 8 in Spatial And Temporal Distribution Of The Island-Dwelling Kogaionidae (Mammalia, Multituberculata) In The Uppermost Cretaceous Of Transylvania (Western Romania)
FIGURE 8. Kogaionid-bearing fossiliferous localities from the Hațeg Basin–Sînpetru Formation and potentially correlative units. A. Deposits of the lower section of the Sînpetru Formation exposed on the right side of Sibișel Valley, near site SP2. B. Deposits of the lower section of the Sînpetru Formation exposed on the left side of the Sibișel Valley, in the La Scoabă section hosting site SP3. C. Overview of the Râul Mare Beds cropping out in the bed of the Râul Mare River at Nălaț-Vad locality; site RB2 located roughly in the middle of the riverbed, aligned with the powergrid tower. D. General view of the middle-upper part of the Pui Beds deposits, position of site PB3 located near the small ledge in the middle of the image. E. Excavations at site PB4 (Pui-Micro), in the uppermost section of the Pui Beds. F. Looking for fossils at the newly discovered site PB6 (year 2012), in the upper part of the Pui Beds; the stratigraphically higher site PB4 is located near the small ledge in the right background.
FIGURE 17 in Spatial And Temporal Distribution Of The Island-Dwelling Kogaionidae (Mammalia, Multituberculata) In The Uppermost Cretaceous Of Transylvania (Western Romania)
FIGURE 17. Kogaionid-bearing fossiliferous localities from the Rusca Montană (A) and southwestern Transylvanian (B–F) basins. A. Exposures of uppermost Cretaceous continental beds along Fărcădeana Creek at Negoiu, Lunca Cernii de Sus, eastern Rusca Montană Basin. Hammer marks the position of the fossilfierous bed hosting site RM1. B. Overview of the Oarda de Jos A locality, south of Alba Iulia, on the right side of Sebeș River (in the foreground). The fossiliferous bed hosting site TB1 is located in the upper part of the outcropping succession. C. Strongly tilted beds of the continental Sebeș Formation outcropping at PetreștiArini, covered by flat-lying Quaternary sandy-pebbly deposits and recently created anthropic sediment heaps. D. Red mudstone-dominated part of the basal section of the Sebeș Formation at Petrești-Arini, hosting site TB2. E. Outcrops of the Sebeș Formation at Sebeș-Glod, along the Sebeș River, locality Sebeș-Glod A, with kogaionid site TB3 near the group of people to the left. F. The transitional sequence from the estuarinebrackish uppermost Bozeș Formation (right) to the continental, gray-colored basalmost Sebeș Formation (left, more ochre-colored rocks) at Petrești-Arini, hosting the Black Lens fossiliferous level (site TB4).
FIGURE 13 in Spatial And Temporal Distribution Of The Island-Dwelling Kogaionidae (Mammalia, Multituberculata) In The Uppermost Cretaceous Of Transylvania (Western Romania)
FIGURE 13. Isolated elements of the upper dentition, referred specimen of Barbatodon transylvanicus, LPB (FGGUB) M.1635, Pui Beds, site PB3. A–D. Left P3 in A. lingual, B. occlusal, and C. labial views; D. SEM microphotograph of the occlusal surface. E–G. Right M2 in E. occlusal, and F. lingual views; G. SEM microphotograph of the occlusal surface in slightly laterally oblique view to show relative development of cusps.
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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.