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Identifying and Implementing Relevant Research Data Management Services for the Library at the University of Dodoma, Tanzania
<p>This data set presents the results of research conducted at the University of Dodoma, Tanzania. The purpose of the research was to identify and report on relevant RDM services that need to be implemented so that researchers and university management could collaborate and make our research data accessible to the international community.</p> <p>The data set was used to support both the mini-dissertation as well as a paper published in the Data Science Journal. The journal paper presents findings on important issues for consideration when planning to develop and implement RDM services at a developing country, academic institution. The paper also mentions the requirements for the sustainability of these initiatives.</p>
VAMDC extraction with identifier = e2352465-ebdb-4347-abc2-96c83da81c73
<div>This is a dataset extracted from https://cdms.astro.uni-koeln.de/cdms/tap/ VAMDC node.</div><div>Query originating this dataset: query=select * where ( inchikey = 'bojpitgaffyfjk-uhfffaoysa-n' ); </div><div> Data source version: 2019-11-27</div><div>Data format: XSAMS 12.07</div><div>Query uuid in VAMDC query store: e2352465-ebdb-4347-abc2-96c83da81c73</div>
VAMDC extraction with identifier = 4bac99d4-20a0-4625-aac1-e6255edb376e
<div>This is a dataset extracted from http://topbase.obspm.fr/12.07/vamdc/tap/ VAMDC node.</div><div>Query originating this dataset: query=select * where ( radtranswavelength <= 4819.05078125 and radtranswavelength >= 4816.38671875 ); </div><div> Data source version: 2017-01-30</div><div>Data format: XSAMS 12.07</div><div>Query uuid in VAMDC query store: 4bac99d4-20a0-4625-aac1-e6255edb376e</div>
Fig. 20 A in New Trees Identified In The Petrified Forest Of Middle Miocene From Zarand, Apuseni Mountains, Romania.
Fig. 20 A transect by the reconstructed Badenian forest of Zarand (from Iamandei, S., 2002). identified tree species allow a phytoecological analysis, structure. Also, the structure of fibro-vascular bundles revealing the plants' thermal tolerance, the soil and air may suggest the current group of palm trees as extant relatives (Tomlinson, 1961, 1990). humidity, the palaeoaltitude, the relationships and inter- The sclerenchyma cap of "lunaria" type (Stenzel, 1904), actions within the biocoenosis, the palaeophytocoenosis the f/v ratio less than 1, the sieved plate of undivised itself, the succession of phenophases in a mixed conifertype, the metaxylem vessels in number of 5-7, of which ous forest, and the dynamics of the local vegetation durtwo are larger and laterally arranged, the group of 7-11 ing the Late Badenian. The paleoclimate analysis is relatsmaller protoxylem vessels with thickened walls, protect- ed to the neighborhood of the Paratethys, where the ed by a sheath of parenchyma whose the marginal cells Zarand Basin evolved. That forest was a mixed mesoare thickened and sclerified walls, the absence of the tab- phytic forest, attitudinally storied, with remains of preular parenchyma could suggest some resemblance to our Miocene sempervirent vegetation of paratropical or subspecimen with a current Sabaloid Palms. tropical climate, suggesting a Miocene pluvial mixed The comparison with fossil taxa described until now mesophytic forest of warm-temperate climate. shows a possible resemblance to the form described by This mixed mesophytic forest with Lauraceae and Coni- Grambast (1962), but since the longitudinal sections are fers, include the following genera: Tetraclinoxylon, Thunot very revealing and due to the xylotomical similitudes joxylon, Chamaecyparixylon, Cupressinoxylon, Taxodiof our specimen with the current Sabaloid Palms, we oxylon, Sequoioxylon, Pinuxylon, Magnolioxylon, Cinname it Rhizopalmoxylon sp. aff. sabaloides. namomoxylon, Spiroplatanoxylon (not Icacinoxylon), Liquidambaroxylon, Eucaryoxylon, Rhysocaryoxyton, CONCLUSIONS Pterocaryoxylon (?), Fagoxylon, Quercoxylon, Alnoxylon, Populoxylon, Salicoxylon, Nyssoxylon, Pa- Twenty years ago we started the study of the Middle Mi- raphyllanthoxylon, Piranheoxylon, Aceroxylon, Fraxocene Petrified Forest from Zarand, Apuseni Mountains, inoxylon, and Rhizopalmoxylon, taking into account new and it still remained an important topic of further re- palaeoxylotomical identifications. searches even after many field trips in the region. Thus, In this paper we present some newly identified woods or many hundreds of petrified wood samples collected from reattributed to other taxon as new combinations from the there were prepared and studied, and much of them are Mid-Miocene Zarand Petrified Forest of Zarand that will still in various stages of study. Their identification in- complete the upward list with 15 new taxa, as it follows. crease the number of fossil trees from the Badenian forest Conifers: Cupressinoxylon sp., Thujoxylon sp., of the Tălagiu island. Chamaecyparixylon sp., Taxodioxylon taxodii Gothan, This study could support a more precise palaeoenviron- Sequoioxylon gypsaceum (Goepp.) Greguss, Sequoioxymental and palaeoclimatic reconstruction. The geological lon multiseriatum Ramanujam et Stewart, comb.nov. evolution of the Tălagiu caldera allowed the best condi- Agiosperms: Liquidambaroxylon speciosum Felix, Fagtions for silicification of the remains of the Mid-Miocene oxylon subcaucasicum Privé et Brousse, Fagoxylon crisforest occurring on the slopes of the volcano. Over 40 tallophorum van der Burgh, Quercoxylon sarmaticum Starostin & Trelea, Paraphyllanthoxylon botarii sp. nov.,
Fig. 18 in New Trees Identified In The Petrified Forest Of Middle Miocene From Zarand, Apuseni Mountains, Romania.
Fig. 18 Aceroxylon pravalense sp.nov. a - cross section: semi-ring-porous wood, solitary vessels, fine to broad rays, less distinct ring boundary - x50; b, c - cross-section: fine and multiseriate rays, solitary vessels, less distinct ring boundary - x100; d, e, f - tangential section: fine and multiseriate fusiform rays, vessels with almost horizontal simple perforated plates - x100; g, h, i - radial section: simple perforations (g), bad preserved opposite pitting (h) cystalliferous cross-field (i) - x200.
Fig. 15 in New Trees Identified In The Petrified Forest Of Middle Miocene From Zarand, Apuseni Mountains, Romania.
Fig. 15 Piranheoxylon perfectum sp. nov. a - cross section: diffuse-porous to semi-ring-porous wood, solitary and grouped vessels - x50; b, c - cross-section: 2-3-seriate rays with obvious dilations at the ring boundary, solitary vessels, thick-walled fibres - x100; d - tangential section: biseriate rays, tall - x100; Photos e-f - tangential section: scalariform intervascular pitting - x200; g - radial section: storeyed scalariform perforations - x100; h, i - radial section: scalariform perforation (h), crossfields with numerous scalariform piting - x200.
Fig. 14 in New Trees Identified In The Petrified Forest Of Middle Miocene From Zarand, Apuseni Mountains, Romania.
Fig. 14 Paraphyllanthoxylon botarii sp. nov. a, b - cross section: semi-ring-porous wood, solitary and grouped vessels, 1-3- seriate rays, parenchyma as short tangential lines - x50; c - cross-section: solitary vessels, thick-walled fibres - x100; d-f - tangential section: 2-3-seriate fusiform, parenchyma, septate fibers, alternate, numerous intervascular pitting - x100; g, h, i - radial section: simple perforations, cross-fields with numerous simple pitting - x200.
Fig. 11 in New Trees Identified In The Petrified Forest Of Middle Miocene From Zarand, Apuseni Mountains, Romania.
Fig. 11 Fagoxylon subcaucasicum Privé et Brousse, 1969. a, b - cross section: difuse-porous wood, two sized rays, ray dilation at ring boundary - x50; Photo c - cross-section: distinct ring boundary, diffuse porous structure - x100; d, e - tangential section: broad fusiform rays, vessels - x100; f - tangential section: badly preserved pitting - oval horizontal opposite pits to scalariform - x200; g, h - radial section: simple perforation, and scalariform piting on vessels - x200; i - radial section: scalariform cross fields with vessels - x200.
Fig. 7 Taxodioxylon taxodii Gothan, 1906. a in New Trees Identified In The Petrified Forest Of Middle Miocene From Zarand, Apuseni Mountains, Romania.
Fig. 7 Taxodioxylon taxodii Gothan, 1906. a - cross section: distinct growth-ring boundary - x50; b, c - cross-section: distinct growth boundary thick-walled tracheids in late wood, dispersed parenchyma - x100; d - tangential section: tracheids few pitted, parenchyma with resin content - x200; e, f - tangential section: tracheids few spaced pitted, parenchyma with resin content (e) and end horizontal denticulate walls (f) - x200; g-i - radial section: radial pitting on tracheids, cross-fields with 2-4 pits on two storeys - x200.
Fig. 6 in New Trees Identified In The Petrified Forest Of Middle Miocene From Zarand, Apuseni Mountains, Romania.
Fig. 6 Chamaecyparixylon sp. a, b - cross section: not very distinct growth-ring boundary, since early wood disorganization, very thick-walled tracheids in late-wood - x100; c - detail in the early wood disorganization - x200; d - very thick-walled tracheids in late-wood - x200; e - tangential section: uniseriate rays - x200; f-i – radial section: radial uniseriate pits on tracheids, cross-fields pits - x200.
Fig. 5 in New Trees Identified In The Petrified Forest Of Middle Miocene From Zarand, Apuseni Mountains, Romania.
Fig. 5 Thujoxylon sp. a, b - cross section: distinct growth-ring boundary, linear rays, very thick-walled tracheids in late-wood - x100-x200; c, d - tangential section: high uniseriate rays - x100; e, f - tangential section: rare small tangential pits on tracheids - x200; g, h - radial section: uniseriate spaced pitting - x200; i - radial section: cross-field pitting - x200.
Fig. 4 in New Trees Identified In The Petrified Forest Of Middle Miocene From Zarand, Apuseni Mountains, Romania.
Fig. 4 Cupressinoxylon sp. a, b - cross section: distinct growth-ring boundary, thick-walled tracheids in late-wood - x100- x200; c - tangential section: uniseriate rays, striated tracheids - x100; d - radial section: pits and striations on tracheids, crossfields - x100; e, f - radial section: striations on tracheids, cupressoid cross-fields - x200; g - radial section: 2-3 seriate pits and striations on tracheids, cupressoid cross-fields - x100; h, i - radial section: 2-3 seriate pits with crassulae on striated tracheids, cupressoid cross-fields - x200.
Fig. 2 in New Trees Identified In The Petrified Forest Of Middle Miocene From Zarand, Apuseni Mountains, Romania.
Fig. 2 Stratigraphical position of the plant remains in Zarand Mountains (from Berbeleac et al., 1984, modified).
Fig. 3 in New Trees Identified In The Petrified Forest Of Middle Miocene From Zarand, Apuseni Mountains, Romania.
Fig. 3 Samples of fossil wood from Mid-Miocene Petrified Forest of Zarand hosted in the National Geological Museum from Bucharest (photo, Iamandei, 2002).
Fig. 1 a in New Trees Identified In The Petrified Forest Of Middle Miocene From Zarand, Apuseni Mountains, Romania.
Fig. 1 a Geological sketch of Romania, with location of Tălagiu caldera in the Apuseni Mountains (Geological Institute editor); b Detail of Tălagiu caldera with the studied area, in rectangle (Excerpt from Geological Map of Romania, Scale 1:200,000 - Sheet 17-Brad, Geological Institute editor).
Fig. 1 in Air sac trematodes: Morishitium polonicum as a newly identified cause of death in the common blackbird (Turdus merula)
Fig. 1. Necropsy of Turdus merula, female. Gross lesions are represented by heavy parasite colonization of coelomic cavity. A. Many trematodes are clearly seen on different serosal membranes. Note the presence of parasites on the liver serosa, air sacs and pericardium (arrow). B. After removal of all the organs of the gastroenteric apparatus, an involvement of kidney and lungs serosa is also evident. Note the presence of an inflammatory focus with exudate at the periphery of the left lung (arrowhead).
Fig. 4 in Air sac trematodes: Morishitium polonicum as a newly identified cause of death in the common blackbird (Turdus merula)
Fig. 4. Maximum likelihood analyses of sequences of mitochondrial DNA loci of the newly isolated Morishitium polonicum and previously sequenced Cyclocoelidae. (A) CO1, (B) ND1. The bars indicate the number of substitutions per nucleotide.
Natural history specimens collected and/or identified and deposited.
Natural history specimen data collected and/or identified by Mary Elizabeth Barber, <a href="http://www.wikidata.org/entity/Q4937489">http://www.wikidata.org/entity/Q4937489</a>. Claims or attributions were made on Bionomia, <a href="http://bionomia.net">https://bionomia.net</a> using specimen data from the Global Biodiversity Information Facility, <a href="https://gbif.org">https://gbif.org</a>.
Figure. Original photos of chewing lice identified in this study: A, Anatoecus cygni (♀); B, Ciconiphilus cygni (♀); C, Ciconiphilus decimfasciatus (♀); D, Colpocephalum apivorus (♂); E, Colpocephalum apivorus (♀); F, Colpocephalum napiforme (♂); G, Kurodaia subpachygaster (♀); H, Ornithobius cygni (♀); I, Philopterus atratus (♀) (bar: 1 mm). in Contributions to the knowledge of the diversity of the chewing lice fauna in Turkey
Figure. Original photos of chewing lice identified in this study: A, Anatoecus cygni (♀); B, Ciconiphilus cygni (♀); C, Ciconiphilus decimfasciatus (♀); D, Colpocephalum apivorus (♂); E, Colpocephalum apivorus (♀); F, Colpocephalum napiforme (♂); G, Kurodaia subpachygaster (♀); H, Ornithobius cygni (♀); I, Philopterus atratus (♀) (bar: 1 mm).
Figure 3 in Occlusal surface variations in genetically-identified specimens of the genus Apodemus (Mammalia: Rodentia) distributed in the Northern Anatolia region and three Turkish islands: Gökçeada, Marmara Island, and Bozcaada
Figure 3. The variations observed in the left upper teeth and their locations. D1: Presence of a bis structure immediately adjacent to the t2 cusp in UM1, D2: Presence of the t12 cusp in UM1, D3: Presence of a spur structure extending posteriorly from the t3 cusp in UM1 but not merging with the t5 cusp, D4: Existence of a bridge between the t1 cusp and t5 cusp in UM1, D5: Connection through a bridge between the t4 cusp and t7 cusp in UM1, D6: Structural swelling and island-like condition of the t7 cusp in UM1, D7: Structural line-like condition of the t7 cusp in UM1, D8: Structural swelling and island-like condition of the t7 cusp in UM2, D9: Line-like structural condition of t7 in UM2, D10: Presence or absence of the t12 cusp in UM2, D11: Presence of a bridge-like structure between the t1 cusp and t5 cusp in UM2, D12: Presence of a bridge between the t4 cusp and t7 cusp in UM2, D13: Existence of a bridge structure between the t1 cusp and t5 cusp in UM3, D14: Presence of a connection between the t6 cusp and t8 cusp in UM3.
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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.