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Fig. 10 in Ontogeny and autecology of an Early Cretaceous trigoniide bivalve from Neuquén Basin, Argentina

Fig. 10. Field pictures of Myophorella garatei Leanza, 1981 in life position at Bajada del Agrio, late Valanginian. A. Individual with anomalous costae. B. Two other individuals (B ), a detail of the one on the right (B ). Scale (chisel edge width) 10 mm.

Fig. 9 in Ontogeny and autecology of an Early Cretaceous trigoniide bivalve from Neuquén Basin, Argentina

Fig. 9. Changes implied on costae shape for the two recognized post-larval growth stages with oblique costae. Changes for the first stage (A→B). Changes for the second stage (B→C). Landmark-semilandmark reconstruction (A 1–C1), reconstruction represented by individuals of the ontogenetic series (A2–C2). Scale bars 2 mm.

Fig. 5 in Ontogeny and autecology of an Early Cretaceous trigoniide bivalve from Neuquén Basin, Argentina

Fig. 5. Individuals of Myophorella garatei Leanza, 1981 representing different size categories on the ontogenetic series; late Valanginian, Cerro Mesa. A–C. Stages recovered from growth lines; MCF-PIPH-428, drawn by camera lucida on lateral view (A2, B2, C2), enlargements (A1, B1, C1). D, E. Stages recovered from growth lines and photographed on lateral view. D. MCF-PIPH-428. E. MCF-PIPH-429. F–H. Individuals recovered on their final growth stage on lateral view. F. MCF-PIPH-428. G. MCF-PIPH-427. H. MCF-PIPH-429. I–K. Dorsal view of some individuals on different stages. I. MCF- PIPH-428. J. MCF-PIPH-429. K. MCF-PIPH-427.

Fig. 8 in Ontogeny and autecology of an Early Cretaceous trigoniide bivalve from Neuquén Basin, Argentina

Fig. 8. Allometry analysis for the width compared to the umbo-posterior point distance; black diamonds, first stage (isometric); white diamonds, second stage (allometric). A. Cartesian graphic of width vs. umbo-posteri- or point distance. B. Cartesian graphic of the same variables with both of them converted to logarithm; black continuous line, line of slope 1; grey dashed line, regression line for the first stage; black dashed line, regression line for the second stage.

Fig. 4 in Ontogeny and autecology of an Early Cretaceous trigoniide bivalve from Neuquén Basin, Argentina

Fig. 4. SEM photographs of the umbonal region of Myophorella garatei Leanza, 1981; late Valanginian, Cerro Mesa. A. MCF-PIPH-428, umbonal region of left valve showing the preserved prodissoconch (pd); detail of the prodissoconch (A1); same picture showing the discontinuities identified on the shell surface and their possible interpretation (A2). B. MCF-PIPH-428, prodissoconch in lateral (B1) and ventral (B2) views, together with early postmetamorphic shell; white arrow on B1 points to the antecarinal sulcus, white arrows on B2 indicate a discontinuity on the shell, probably the margin of prodissoconch I. C. MCF-PIPH-428, prodissoconch in ventral view together with early postmetamorphic shell. D. MCF-PIPH-428, umbonal region showing early postmetamorphic flank costae with Haidaia type ornamentation (white arrows) and early area development.

Fig. 7 in Ontogeny and autecology of an Early Cretaceous trigoniide bivalve from Neuquén Basin, Argentina

Fig. 7. Changes implied on general shell shape in lateral view for the two recognized post-larval growth stages. Changes for the first stage (AĄB). Changes for the second stage (BĄC). Landmark-semilandmark reconstruction (A 1 –C 1), reconstruction represented by individuals of the ontogenetic series (A –C ). Scale bars 2 mm.

Fig. 1 in Ontogeny and autecology of an Early Cretaceous trigoniide bivalve from Neuquén Basin, Argentina

Fig. 1. Schematic drawing of the shell of an adult specimen of Myopohorella garatei Leanza, 1981 showing the main features of trigoniides shell morphology. A. Left lateral view. B. Dorsal view.

Fig. 6 in Ontogeny and autecology of an Early Cretaceous trigoniide bivalve from Neuquén Basin, Argentina

Fig. 6. PCA of the general shell shape in lateral view, showing PC 1 (65.6% of variance), PC 2 (11.8% of variance) and PC 3 (9.1% of variance); black diamonds, first growth stage; white diamonds, second growth stage. A. PC 1 versus PC 2. B. PC 1 versus PC 3.

Fig. 3 in Ontogeny and autecology of an Early Cretaceous trigoniide bivalve from Neuquén Basin, Argentina

Fig. 3. Landmarks and semilandmarks used on geometric morphometric analyses; black dots, landmarks; grey dots, semilandmarks; white dots, helper points. A. Landmarks and semilandmarks used for the general shell shape analyses; 1, landmark 1, the umbo; 2, landmark 2, intersection between the escutcheon carina and the posterior margin; 3, landmark 3, intersection between the marginal carina and the posterior margin. B. Landmarks and semilandmarks used for the costae shape analysis.

Fig. 2 in Ontogeny and autecology of an Early Cretaceous trigoniide bivalve from Neuquén Basin, Argentina

Fig. 2. Location map of Neuquén Basin for the late Valanginian–Hauterivian according to Legarreta and Uliana (1991), and of the localities of Cerro Mesa and Bajada del Agrio in Neuquén Province, Argentina.

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Dataset: Recruitment responses of shade-tolerant and heliophilous trees in human-degraded areas: the necessity of knowing the recruitment autecology of species for making reforestation decisions

This repository contains the files associated with the following article: Johanna Croce, Ernesto I. Badano, Andrés Tálamo. Recruitment responses of shade-tolerant and heliophilous trees in human-degraded areas: the necessity of knowing the recruitment autecology of species for making reforestation decisions Submitted to Land Degradation & Development. The first Microsoft Excel file (Dataset 01 - Microclimate.xlsx) contains two sheets with the microclimatic data (average, maximum and minimum soil temperatures, and volumetric soil water content) measured in Cerro Chachapoyas and Cerro Fachacano. These measurements were performed on three plots of each trearment, including shrub-protected treatment with high shade, shrub-protected treatment with medium shade, sunny treatment with high herbaceous cover, sunny treatment with medium herbaceous cover and controls. The second Microsoft Excel file (Dataset 02 -Plant responses.xlsx Dataset 02 - Plant responses.xlsx) contains three sheets with the data used to estimate the seedling emergence rates, plant survival rates and net aboveground growth rates of the tree species, including Anadenanthera colubrina and Ceiba chodatii in Cerro Chachapoyas, and Jacaranda mimosifolia in Cerro Fachacano.

FIGURES 20–31 in Taxonomy, distribution and autecology of Planothidium bagualensis sp. nov. (Bacillariophyta) a common monoraphid species from southern Brazilian rivers

FIGURES 20–31: Planothidium bagualensis SEM views. Fig. 20. External view of rapheless valve. Fig. 21. Internal view of rapheless valve with prominent cavum. Fig. 22. External view of raphe valve. Fig. 23. Internal view of raphe valve. Fig. 24. External detail of central area showing expanded and ligulated proximal raphe endings. Reduced striae forming a rounded wide central area. Striae composed (usually) 3–4 rows of small areolae. Fig. 25. Internal detail of raphe valve showing proximal raphe ends. Fig. 26. External detail of valve extremity of rapheless valve. Striae usually triseriate, interrupted at valve mantle junction. Groups of 4–6 areolae present on mantle at end of each striae. Figs 27–28. Detail of cavum aperture. Note the extremities of the border attached to neighbour striae. Figs 29–30. Terminal raphe ending. Note the higher number of areoale in the raphe valve with striae composed of rows with 4–5 round poroids, irregularly placed toward the ends. Areolae very scarce in valve mantle. Fig. 31. Internal view of rapheless valve areaolae. Scale bars: Figs 20–23, 26 = 5 µm; Figs 24–25, 28–30 = 3 µm; Figs 27 = 2 µm; Fig. 31 = 1 µm.

FIGURES 2–19 in Taxonomy, distribution and autecology of Planothidium bagualensis sp. nov. (Bacillariophyta) a common monoraphid species from southern Brazilian rivers

FIGURES 2–19: Planothidium bagualensis LM views. Figs 2–19. Valve views. Figs 2–10. Rapheless valves. Figs 11–19. Raphe valves. Rio Pardinho hydrographical basin, Rio Grande do Sul, Brazil. BR-4315. Fig. 4. Rapheless valve of designated holotype, BR- 4316. Scale bar represents 10 µm.

FIGURE 1 in Taxonomy, distribution and autecology of Planothidium bagualensis sp. nov. (Bacillariophyta) a common monoraphid species from southern Brazilian rivers

FIGURE 1: (A) Confirmed presence of Planothidium bagualensis in southern Brazil according to published and illustrated literature (see Table 1 for details). 1 = Lange-Bertalot & Krammer (1989); 2 = Rodrigues & Moreira Filho (1990); 3 = Krammer & Lange- Bertalot (1991); 4 = Ludwig & Flores (1995); 5 = Burliga et al. (2005); 6 = Ludwig & Bigunas (2006); 7 = Ferrari & Ludwig (2007); 8 = Leandrini et al. (2010); 9 = Bes et al. (2012); 10 = Fontana & Bicudo (2012); 11 = Bartozek et al. (2013). (B) Rio Pardo hydrographical basin in the State of Rio Grande do Sul (RS), Brazil, with location of sampling sites in the Rio Pardinho (S1-S6) and Rio Pardo sub-basins (S7 and S9) sampled during the years 2001–2004 (n=129).

FIGURE 32 in Taxonomy, distribution and autecology of Planothidium bagualensis sp. nov. (Bacillariophyta) a common monoraphid species from southern Brazilian rivers

FIGURE 32: Boxplot of relative abundance (%) of Planothidium bagualensis in the Rio Pardo hydrographical basin, RS, Brazil and relationships between phosphates (PO 3−; mg L−1), chemical oxygen demand (COD; mg L−1), total dissolved solids (TDS; mg L−1) and 4 pH. Percentages based in counting of at least 600 valves per sample (n=129). Dashed lines indicate weighted average optima.