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Supplemental Figure 1 for Macrophage Secreted TGF-β1 Contributes to Fibroblast Activation and Ureteral Stricture Following Ablation Injury
<p>Supplemental Figure 1. TGF-β1 (brown) and Masson Trichrome (blue) staining of healthy ureteral wall adjacent to the site of IRE treatment. A-D) Sparse numbers of spindle shaped cells (fibroblasts, arrows) can be seen in healthy ureter adjacent to IRE treated ureter but their numbers were not different from what was observed in untreated control ureter. F-H) Ureteral wall adjacent to the site of IRE treatment stains positive for collagen (blue) but the levels remain invariant through different timepoints. The muscularis (asterisk) of the ureteral wall is preserved, with no evidence of scarring.</p>
Fig. 1. – Echium montenielluense Delage. A in Notes et contributions à la flore de Corse, Contribution 42 Echium montenielluense (Boraginaceae), une nouvelle espèce endémique de Corse
Fig. 1. – Echium montenielluense Delage. A. Inflorescence et rosette; B. Méricarpe (face dorsale); C. méricarpe (face ventrale); D. Détail de la fleur à l'anthèse; E. Corolle étalée après ouverture dorsale; F. Anthère. [Dessins: A. Delage]
Fig. 2. – Echium montenielluense Delage. A in Notes et contributions à la flore de Corse, Contribution 42 Echium montenielluense (Boraginaceae), une nouvelle espèce endémique de Corse
Fig. 2. – Echium montenielluense Delage. A. Inflorescence et rosette; B. Détail d'une cyme; C. Rosette; D. Détail de l'indument de la tige; E. Détail de l'indument du limbe; F. Vue générale de l'habitat au Monte Niellu; G. Détail de l'habitat. [Photos: A. Delage]
List of 10-most funded projects from the Instrument contributing to Stability and Peace 2018
<p>List of 10-most funded projects from the Instrument contributing to Stability and Peace 2018 - This is a dataset from the research financed by the research and innovation programme Horizon 2020 of the European Union in light of the grant agreement Marie Sklodowska-Curie No 660933 - PARADOXGREATLAKES.</p>
Figure 2 in Contribution to the knowledge of Brazilian troglobitic Pseudoscorpiones (Arachnida): description of Pseudochthonius lubueno sp. nov. (Chthoniidae) from Serra do Ramalho karst area, state of Bahia, Brazil
Figure 2. Gruna da Altina cave: (A) details of the microhabitat of P. lubueno sp. nov., Photo A. Gambarini; (B) Guano piles, a typical substrate of occurrence of the new species, Photo: M.E. Bichuette.
Figure 1 in Contribution to the knowledge of Brazilian troglobitic Pseudoscorpiones (Arachnida): description of Pseudochthonius lubueno sp. nov. (Chthoniidae) from Serra do Ramalho karst area, state of Bahia, Brazil
Figure 1. Map showing the distribution of Pseudochthonius lubueno sp. nov. in Gruna da Altina cave, located in Serra do Ramalho, Bahia, and the distribution of Brazilian epigean and hypogean Pseudochthonius species, with the troglobitic representatives
Figure 4 in Contribution to the knowledge of Brazilian troglobitic Pseudoscorpiones (Arachnida): description of Pseudochthonius lubueno sp. nov. (Chthoniidae) from Serra do Ramalho karst area, state of Bahia, Brazil
Figure 4. Pseudochthonius lubueno sp. nov., male holotype (A-F) and female paratype (G): (A) carapace dorsal view; (B) detail of the anterior margin, with the epistome; (C) left chelicera; (D) rallum; (E) coxal spines of coxae I–II; (F) genital opening; (G) genital opening, paratype. Scale bars: A, C, E, F-G = 0.05 mm, B = 0.2 mm, D = 0.02 mm.
Figure 2 in Soil fauna contribution to winter decomposition in subalpine grasslands
Figure 2. Litter mass loss of Patzkea paniculata, Dactylis glomerata and the mixture in small mesh (white bars) and large mesh (grey bars) and litterbags, for each location (pots and field), after winter decomposition. The results of the 6 pairwise tests are shown for each location and litter type (ns: p> 0.3, **: p <0.01, ***: p <0.001).
Figure. Investigated localities in this study: 1. Adıyaman, 2. Aksaray, 3. Amasya, 4. Ankara, 5. Artvin, 6. Aydın, 7. Bartın, 8. Bayburt, 9. Bolu, 10. Çanakkale, 11. Çankırı, 12. Çorum, 13. Diyarbakır, 14. Edirne, 15. Elazığ, 16. Erzincan, 17. Eskişehir, 18. Giresun, 19. Gümüşhane, 20. Isparta, 21. Karabük, 22. Kastamonu, 23. Kayseri, 24. Kırklareli, 25. Kırşehir, 26. Konya, 27. Kütahya, 28. Malatya, 29. Mardin, 30. Nevşehir, 31. Ordu, 32. Rize, 33. Samsun, 34. Sivas, 35. Şanlıurfa, 36. Tekirdağ, 37. Tokat, 38. Trabzon, 39. Tunceli, 40. Yozgat, 41. Zonguldak. in Additional contributions to the Opiinae fauna of Turkey (Hymenoptera: Braconidae)
Figure. Investigated localities in this study: 1. Adıyaman, 2. Aksaray, 3. Amasya, 4. Ankara, 5. Artvin, 6. Aydın, 7. Bartın, 8. Bayburt, 9. Bolu, 10. Çanakkale, 11. Çankırı, 12. Çorum, 13. Diyarbakır, 14. Edirne, 15. Elazığ, 16. Erzincan, 17. Eskişehir, 18. Giresun, 19. Gümüşhane, 20. Isparta, 21. Karabük, 22. Kastamonu, 23. Kayseri, 24. Kırklareli, 25. Kırşehir, 26. Konya, 27. Kütahya, 28. Malatya, 29. Mardin, 30. Nevşehir, 31. Ordu, 32. Rize, 33. Samsun, 34. Sivas, 35. Şanlıurfa, 36. Tekirdağ, 37. Tokat, 38. Trabzon, 39. Tunceli, 40. Yozgat, 41. Zonguldak.
Figure. Provinces situated in the Eastern Anatolia Region, Turkey. Asterisks indicate the sampled provinces in the present study. in Contributions to the knowledge of Agathidinae fauna of the Eastern Anatolia Region of Turkey
Figure. Provinces situated in the Eastern Anatolia Region, Turkey. Asterisks indicate the sampled provinces in the present study.
Text-fig. 1. Distribution of the Králův Dvůr Formation (Upper Katian) in the Prague Basin of the Czech Republic, the location of the localities noted in text (modified, after Štorch and Mergl 1989). in Lingulate And Craniate Brachiopods From The Top Of The Králův Dvůr Formation (Latest Katian) And Their Contribution To Palaeogeography
Text-fig. 1. Distribution of the Králův Dvůr Formation (Upper Katian) in the Prague Basin of the Czech Republic, the location of the localities noted in text (modified, after Štorch and Mergl 1989).
Text-fig. 3. Pseudopholidops anteglacialis sp. nov., Králův Dvůr Formation, 'Perník bed', Praha-Řeporyje locality. Bar = 1 mm. A – Dorsal valve, internal mould, PCZCU 1843. B – Dorsal valve, internal mould, PCZCU 1840. C, K – Ventral valve, internal and external moulds, PCZCU 1831. D – Ventral valve, internal mould, PCZCU 1827. E – Dorsal valve, internal mould, PCZCU 1826. F – Ventral valve, internal mould, PCZCU 1830. G – Ventral valve, internal mould, PCZCU 1832. H – Dorsal valve, internal mould, PCZCU 1841. I, J – Holotype, ventral valve, internal and external moulds, PCZCU 1835. L – Exterior, external mould, PCZCU 1836. in Lingulate And Craniate Brachiopods From The Top Of The Králův Dvůr Formation (Latest Katian) And Their Contribution To Palaeogeography
Text-fig. 3. Pseudopholidops anteglacialis sp. nov., Králův Dvůr Formation, 'Perník bed', Praha-Řeporyje locality. Bar = 1 mm. A – Dorsal valve, internal mould, PCZCU 1843. B – Dorsal valve, internal mould, PCZCU 1840. C, K – Ventral valve, internal and external moulds, PCZCU 1831. D – Ventral valve, internal mould, PCZCU 1827. E – Dorsal valve, internal mould, PCZCU 1826. F – Ventral valve, internal mould, PCZCU 1830. G – Ventral valve, internal mould, PCZCU 1832. H – Dorsal valve, internal mould, PCZCU 1841. I, J – Holotype, ventral valve, internal and external moulds, PCZCU 1835. L – Exterior, external mould, PCZCU 1836.
Text-fig. 1. Bohemian Massif with position of the Prague Basin (in black) and distribution of Ordovician rocks in the Prague Basin, with geographic position of main localities of the siliceous nodules. in Porambonites Havliceki Sp. Nov., A New Brachiopod From The Šárka Formation (Darriwilian) From Bohemia And Its Contribution To Early History Of The Porambonitidae
Text-fig. 1. Bohemian Massif with position of the Prague Basin (in black) and distribution of Ordovician rocks in the Prague Basin, with geographic position of main localities of the siliceous nodules.
Text-fig. 2. Stratigraphic ranges of selected porambonitid taxa in West Gondwana (Iberica), Baltica, Perunica and Avalonia. Arrows indicate derivation of early Baltic porambonitids from Gondwanan Poramborthis (1), derivation of Porambonites in Perunica and Avalonia from Baltica (2), and expansion of Porambonites from Baltica and/or Avalonia to West Gondwana (3). in Porambonites Havliceki Sp. Nov., A New Brachiopod From The Šárka Formation (Darriwilian) From Bohemia And Its Contribution To Early History Of The Porambonitidae
Text-fig. 2. Stratigraphic ranges of selected porambonitid taxa in West Gondwana (Iberica), Baltica, Perunica and Avalonia. Arrows indicate derivation of early Baltic porambonitids from Gondwanan Poramborthis (1), derivation of Porambonites in Perunica and Avalonia from Baltica (2), and expansion of Porambonites from Baltica and/or Avalonia to West Gondwana (3).
Fig. 10 in Contributions To The Study Of The Early Jurassic Petrified Forest Of Holbav And Cristian Areas (Brașov Region, South Carpathians, Romania). 1 Part
Fig. 10 Palaeoginkgoxylon sp. - material - inventory no. 27746 (field no. 1023). a-c Cross section: indistinct growth-ring boundary, thick-walled polygonal tracheids with rounded corners, and linear rays. d-f Tangential section: unpitted tracheids, uniseriate rays, and biseriate with long endings; polygonal-rounded ray-cells. g-i Radial section: radial piting on tracheids of mixed type, cross-fields with 1-2 rows of oculipores.
Fig. 6 in Contributions To The Study Of The Early Jurassic Petrified Forest Of Holbav And Cristian Areas (Brașov Region, South Carpathians, Romania). 1 Part
Fig. 6 Brachyoxylon holbavicum sp. nov. - paratype - inventory no. 27635 (field no. 1039). a-c Cross-section: quite distinct growth-ring boundary, thick-walled tracheids polygonal with rounded corners, and linear rays. d-f Tangential section: unpitted tracheids, uniseriate rays with biseriate storeys. g-i Radial section: radial piting on tracheids of mixed type, araucarioid cross fields with 2-3 superposed rows of cupressoid pits.
Fig. 5 in Contributions To The Study Of The Early Jurassic Petrified Forest Of Holbav And Cristian Areas (Brașov Region, South Carpathians, Romania). 1 Part
Fig. 5 Brachyoxylon holbavicum sp. nov. - holotype - inventory no. 27614 (field no. 1008). a-c Cross-section: distinct growth-ring boundary, thick-walled tracheids polygonal with rounded corners; linear rays. d-f Tangential section: unpitted tracheids, parenchyma, uniseriate rays. g-i Radial section: radial piting of mixed type on tracheids, araucarioid cross fields with 2-3 superposed rows of cupressoid pits.
Fig. 2 in Contributions To The Study Of The Early Jurassic Petrified Forest Of Holbav And Cristian Areas (Brașov Region, South Carpathians, Romania). 1 Part
Fig. 2 Location of the Holbav area on the Geological Map of Romania, 1:50000, Sheet 110b ZărneȘti (excerpt), Geological Institute of Romania (excerpt), and Google Earth image (2018 CNES/Airbus) showing the location on the Maiului brook (star 1) and on the Bisericii brook (star 2) where the Early Jurassic woods were collected. Symbols: P-w1,– Permian-lower Werfenian (Lower Triassic), w2 – upper Werfenian (Lower Triassic); an – Anisian (Middle Triassic).
Fig. 1 in Contributions To The Study Of The Early Jurassic Petrified Forest Of Holbav And Cristian Areas (Brașov Region, South Carpathians, Romania). 1 Part
Fig. 1 Location of the Holbav (1) and Cristian (2) areas on the Geological Map of Romania, Scale 1:100000000, ed.1978, Geological Institute of Romania (excerpt). Inset map shows the location of the BraȘov region (encircled star), in the easternmost part of the Southern Carpathians.
Fig. 7 in Contributions To The Study Of The Early Jurassic Petrified Forest Of Holbav And Cristian Areas (Brașov Region, South Carpathians, Romania). 1 Part
Fig. 7 Brachyoxylon cristianicum sp. nov. - holotype - inventory no. 27639 (field no. 1019cr). a-c Cross-section: distinct growthring boundary, thick-walled tracheids, polygonal with rounded corners, and linear rays. d-f Tangential section: unpitted tracheids, parenchyma with pits and crystals; uniseriate rays. g-i Radial section: uniseriate radial piting on tracheids of mixed type, cross fields with 1-2 rows of oculipores.
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Allen Brain Atlas
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Annotated Behaviour and Observability Dataset (ABODe)
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