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484 results for “southern South America”
Figure 6 in Biodiversity of the scentless plant bugs (Hemiptera: Rhopalidae) in southern South America
Figure 6. Distribution of Jadera Stål species in Argentina. Pale colour: known distributions. The number of known species for each province is provided, with an asterisk indicating the number of newly recorded species.
Figure 1 in Biodiversity of the scentless plant bugs (Hemiptera: Rhopalidae) in southern South America
Figure 1. Distribution of Liorhyssus Stål species in Argentina. Pale colour: known distributions; dark colour: new distributions. The number of known species for each province is provided, with an asterisk indicating the number of newly recorded species.
Figure 7 in Biodiversity of the scentless plant bugs (Hemiptera: Rhopalidae) in southern South America
Figure 7. Known records for the species of Rhopalidae from Argentina over the years (cumulative relative frequencies 0–100%).
TABLE 5 in Paleoclimate estimates for the Paleogene-Neogene in southern South America using fossil leaves as proxies
<p>TABLE 5 — Fossil locations from Southern South America and age in million of years.Studied geological formations and sites used for comparison in the discussion.</p><table><thead><tr><th><b>Fossil Site</b></th><th><b>Geological Formation</b></th><th><b>Age (Ma)</b></th><th><b>Source</b></th></tr></thead><tbody><tr><th>Pico Quemado</th><td>Ñirihuau</td><td>middle Miocene?</td><td>Caviglia 2018</td></tr><tr><th>Cancha Carreras, Estancia Tres Marías</th><td>Río Guillermo</td><td>≤21.7 ± 0.3 to ≤23.5 ± 0.3</td><td>Fosdick <i>et al.</i> 2011; 2015a, b</td></tr><tr><th>Aluminé Basin</th><td>Rancahué</td><td>25.0 ± 1.4 to 26.0 ± 1.5</td><td>Brea <i>et al.</i> 2015; Franzese <i>et al.</i> 2011</td></tr><tr><th>Sierra Baguales</th><td>Río Leona</td><td>33.0 ± 2.8</td><td>Gutiérrez <i>et al.</i> 2017, 2019</td></tr><tr><th>Upper Río Turbio</th><td>Río Turbio</td><td>≤26.6 ± 0.2 to ≤33.4 to</td><td>Fosdick <i>et al.</i> 2015a</td></tr><tr><th>Lower Río Turbio</th><td>Río Turbio</td><td>≤46.3 ± 1.3 to ≤47.1 ± 2.7</td><td>Fosdick <i>et al.</i> 2015a</td></tr><tr><th>Río Pichileufú</th><td>Ventana</td><td>47.46 ± 0.05</td><td>Wilf <i>et al.</i> 2005</td></tr><tr><th>Laguna del Hunco</th><td>La Huitrera</td><td>51.91 ± 0.22</td><td>Wilf <i>et al.</i> 2005</td></tr><tr><th>Ligorio Márquez</th><td>Ligorio Márquez</td><td><57</td><td>Suárez <i>et al.</i> 2000; Hinojosa 2005</td></tr><tr><th>Palacio de los Loros</th><td>Salamanca</td><td>61.7</td><td>Iglesias <i>et al.</i> 2007</td></tr></tbody></table>
TABLE 2 in Paleoclimate estimates for the Paleogene-Neogene in southern South America using fossil leaves as proxies
<p>TABLE 2 — Estimated values of temperature and precipitation for the upper Río Turbio Formation member. *Scarce fossil material.</p><table><thead><tr><th><b>Upper RTF</b></th><th></th><th><b>Equation</b></th><th><b>Dataset</b></th><th><b>R</b> <b>2</b></th><th><b>Error</b></th><th><b>Source</b></th></tr></thead><tbody><tr><th>Temperature (°C)</th><td>15.3</td><td colspan="2">MAT = 3.25 + 0.24*% non-tooth CLAMP 3B SA</td><td>0.9</td><td>2.1°C</td><td>Hinojosa 2005; Hinojosa & Villagrán 2005</td></tr><tr><th>Temperature (°C)</th><td>14.3</td><td>MAT = 26.03pE + 1.31</td><td>SA</td><td>0.82</td><td>2.8°C</td><td>Hinojosa <i>et al.</i> 2011</td></tr><tr><th>Temperature (°C)</th><td>14.8</td><td>MAT = 0.204*E + 4.6</td><td>LMA</td><td>0.58</td><td>4.8°C</td><td>Peppe <i>et al.</i> 2011</td></tr><tr><th>Precipitation (mm)</th><td>*</td><td>Ln(MAP) = 1.63 + 0.49*MLnA</td><td>CLAMP 3B SA</td><td>0.6</td><td>Ln(0.5) cm</td><td>Hinojosa 2005; Hinojosa & Villagrán 2005</td></tr><tr><th>Precipitation (mm)</th><td>*</td><td>lnMAP = 0.283(MlnA) + 2.92</td><td>LAA</td><td>0.23</td><td>0.61</td><td>Peppe <i>et al.</i> 2011</td></tr></tbody></table>
TABLE 3 in Paleoclimate estimates for the Paleogene-Neogene in southern South America using fossil leaves as proxies
<p>TABLE 3 — Estimated values of temperature and precipitation for the Río Guillermo Formation.</p><table><thead><tr><th><b>RGF</b></th><th></th><th><b>Equation</b></th><th><b>Dataset</b></th><th><b>R</b> <b>2</b></th><th><b>Error</b></th><th><b>Source</b></th></tr></thead><tbody><tr><th>Temperature (°C)</th><td>5.3</td><td>MAT = 3.25 + 0.24*% non-tooth</td><td>CLAMP 3B SA</td><td>0.9</td><td>2.1°C</td><td>Hinojosa 2005; Hinojosa & Villagrán 2005</td></tr><tr><th>Temperature (°C)</th><td>3.5</td><td>MAT = 26.03pE + 1.31</td><td>SA</td><td>0.82</td><td>2.8°C</td><td>Hinojosa <i>et al.</i> 2011</td></tr><tr><th>Temperature (°C)</th><td>6.3</td><td>MAT = 0.204E + 4.6</td><td>LMA</td><td>0.58</td><td>4.8°C</td><td>Peppe <i>et al.</i> 2011</td></tr><tr><th>Precipitation (mm)</th><td>682</td><td>Ln(MAP) = 1.63 + 0.49*MLnA</td><td>CLAMP 3B SA</td><td>0.6</td><td>Ln(0.5) cm</td><td>Hinojosa 2005; Hinojosa & Villagrán 2005</td></tr><tr><th>Precipitation (mm)</th><td>829</td><td>lnMAP = 0.283(MlnA) + 2.92</td><td>LAA</td><td>0.23</td><td>0.61</td><td>Peppe <i>et al.</i> 2011</td></tr></tbody></table>
TABLE 1 in Paleoclimate estimates for the Paleogene-Neogene in southern South America using fossil leaves as proxies
<p>TABLE 1 — Estimated values of temperature and precipitation for the lower Río Turbio Formation member.</p><table><thead><tr><th><b>Lower RTF</b></th><th></th><th><b>Equation</b></th><th><b>Dataset</b></th><th><b>R</b> <b>2</b></th><th><b>Error</b></th><th><b>Source</b></th></tr></thead><tbody><tr><th>Temperature (°C)</th><td>16.5</td><td>MAT = 3.25 + 0.24*% non-tooth</td><td>CLAMP 3B SA</td><td>0.9</td><td>2.1°C</td><td>Hinojosa 2005; Hinojosa & Villagrán 2005</td></tr><tr><th>Temperature (°C)</th><td>15.7</td><td>MAT = 26.03pE + 1.31</td><td>SA</td><td>0.82</td><td>2.8°C</td><td>Hinojosa <i>et al.</i> 2011</td></tr><tr><th>Temperature (°C)</th><td>15.6</td><td>MAT = 0.204E + 4.6</td><td>LMA</td><td>0.58</td><td>4.8°C</td><td>Peppe <i>et al.</i> 2011</td></tr><tr><th>Temperature (°C)</th><td>16.9</td><td>See manuscript (1)</td><td>DiLP</td><td>0.7</td><td>4°C</td><td>Peppe <i>et al.</i> 2011</td></tr><tr><th>Precipitation (mm)</th><td>1764</td><td>Ln(MAP) = 1.63 + 0.49*MLnA</td><td>CLAMP 3B SA</td><td>0.6</td><td>Ln(0.5) cm</td><td>Hinojosa 2005; Hinojosa & Villagrán 2005</td></tr><tr><th>Precipitation (mm)</th><td>1435</td><td>lnMAP = 0.283(MlnA) + 2.92</td><td>LAA</td><td>0.23</td><td>0.61 cm</td><td>Peppe <i>et al.</i> 2011</td></tr><tr><th>Precipitation (mm)</th><td>1303</td><td>See manuscript (2)</td><td>DiLP</td><td>0.27</td><td>0.6 cm</td><td>Peppe <i>et al.</i> 2011</td></tr></tbody></table>
Fig. 1 in New combinations and notes on Oxybasis (Amaranthaceae) from southern South America
Fig. 1. – Isotype of Chenopodium frigidum Phil. ( Oxybasis frigida (Phil.) Uotila) originating from the Aellen herbarium in G. [G00412681; Conservatoire et Jardin botaniques de Genève]
Figure 1 in A historical Australasian Shoveler Spatula rhynchotis specimen from southern South America
Figure 1 (above). Specimen of breeding-plumaged male Australasian Shoveler Anas rhynchotis in lateral, dorsal and ventral views, deposited at Museu Nacional (MN 19034), Rio de Janeiro, Brazil, and labelled as having been collected in Entre Ríos province, Argentina (Marco A. Crozariol) Figure 2 (left). Specimen labels, showing the earlier erroneous identifications of 'Anas cayennen[sis]' and 'Anas platalea'. The green label displays the specimen's catalogue number at Museu Nacional (MN 19034). (Marco A. Crozariol)
Fig. 8 in Populations of Odontesthes (Teleostei: Atheriniformes) in the Andean region of Southern South America: body shape and hybrid individuals
Fig. 8. Geometric Morphometric Analysis applied to O. hatcheri individuals. Left: plot of DF3 vs. DF2 showing means and 95% confidence intervals by sampling sites (locality labels as in Fig. 1) NIHL (white triangle), CDP (black circle), 7: PELE (gray square), PDA (black triangle), MITO (black diamond), CARI (white square), EPU (black and white diamond), RIV (gray circle), ROS (white diamond), AME (black square), CHU (gray diamond), MUS (gray triangle), LBA (white circle), and PUY (white triangle). Right: deformation grids correspond to a relative warps analysis involving only CDP, PDA, and NIHL and PUY. Arrowheads indicate displacement of landmarks relative to consensus. Shaded area remarks relative position of landmarks 5 (anterior insertion of the first dorsal fin) and 12 (distal tip of the pelvic fin onto fish body).
Fig. 6 in Populations of Odontesthes (Teleostei: Atheriniformes) in the Andean region of Southern South America: body shape and hybrid individuals
Fig. 6. Probability for taxonomically identified Odontesthes hatcheri individuals of being O. hatcheri (left) and probability of taxonomically identified O. bonariensis individuals of being O. bonariensis (right). Number of fish, median, quartiles, and data outside 10 and 90th percentile are indicated. Water bodies are named as in Fig. 1.
Fig. 5 in Populations of Odontesthes (Teleostei: Atheriniformes) in the Andean region of Southern South America: body shape and hybrid individuals
Fig. 5. Morphometric differences between species. DF1 and residual DF2 (of the regression of DF2 versus Standard length) vs. Standard length (SL). Odontesthes bonariensis (white circle), O. hatcheri (black circle), and presumptive hybrids (gray circle).
Fig. 4 in Populations of Odontesthes (Teleostei: Atheriniformes) in the Andean region of Southern South America: body shape and hybrid individuals
Fig. 4. Geometric Morphometric Analysis applied to Odontesthes individuals. RW2 versus RW1 and deformation grids (tied to group means) for Odontesthes bonariensis (white circle), O. hatcheri (black circle) and presumptive hybrids (gray circle). Arrowheads indicate displacement of landmarks relative to consensus. Shaded area shows relative position of landmarks 5 (anterior insertion of the first dorsal fin) and 12 (distal tip of the pelvic fin onto fish body).
Fig. 1 in Populations of Odontesthes (Teleostei: Atheriniformes) in the Andean region of Southern South America: body shape and hybrid individuals
Fig. 1. Distribution of O. hatcheri (light gray) and O. bonariensis (dark gray) described by Dyer (2006) and sampling localities: ULLM, Ullum Reservoir; CARZ, Carrizal Reservoir; NIHL, Nihuil Reservoir; D, Lake San Lorenzo; URRE, Lake Urre Lauquen; CDP, Casa de Piedra Reservoir; PELE, Lake Pellegrini; PDA, Piedra del Aguila Reservoir; MITO, Lake Morenito; CARI, Lake Carilafquen; EPU, Lake Epuyén; RIV, Lake Rivadavia; ROS, Lake Rosario; AME, Florentino Ameghino Reservoir; CHU, Chubut River at Los Altares; MUS, Lake Musters; LBA, Lake Buenos Aires; PUY, Lake Pueyrredón. White triangles show the location of the three hatcheries (Estación Hidrobiológica de Chascomús 35º36'S, 58º01'W, Estación de Piscicultura de Embalse 32º13'S, 64º29'W, and Estación de Piscicultura Río Limay 38º59'S, 68º14'W), sources of stocking practices.
Figures 8–10 in On the identity of Colletes neoqueenensis (Colletidae: Colletinae) from southern South America
Figures 8–10. Female specimen of Colletes lycii Jörgensen from AMNH misidentified as C. neoqueenensis Friese. 8. Habitus, lateral view. 9. Face, frontal view. 10. Labels. Scale bars = 2mm.
Figures 5–7 in On the identity of Colletes neoqueenensis (Colletidae: Colletinae) from southern South America
Figures 5–7. Female specimen of Colletes lycii Jörgensen from SEMC misidentified as C. neoqueenensis Friese. 5. Habitus, lateral view. 6. Face, frontal view. 7. Labels. Scale bars = 2mm.
Figures 1–4 in On the identity of Colletes neoqueenensis (Colletidae: Colletinae) from southern South America
Figures 1–4. Female lectotype of Colletes neoqueenensis Friese. 1. Habitus, dorsal view. 2. Face, frontal view. 3. Habitus, lateral view. 4. Labels. Scale bars = 2mm.
Fig. 7. Geometric morphometric analyses. A. Principal Component Analysis. B in Early steps in the radiation of notoungulate mammals in southern South America: A new henricosborniid from the Eocene of Patagonia
Fig. 7. Geometric morphometric analyses. A. Principal Component Analysis. B. Canonical Variate Analysis.
Fig. 1. Landmark configurations maped onto a hypothetical generalized henricosborniid. A in Early steps in the radiation of notoungulate mammals in southern South America: A new henricosborniid from the Eocene of Patagonia
Fig. 1. Landmark configurations maped onto a hypothetical generalized henricosborniid. A. Upper molar: 1, metastyle; 2, metacone; 3, paracone; 4, parastyle; 5, protocone; 6, hypocone; 7, distolingual end of crochet; 8, mesiolabial end of crochet. B. Lower molar: 1, labial end of paralophid; 2, labial end of metalophid; 3, lingual end of metalophid; 4, mesial end of cristid obliqua; 5, hypoconulid; 6, entoconid/lingual end of entolophid.
Fig. 2 in Early steps in the radiation of notoungulate mammals in southern South America: A new henricosborniid from the Eocene of Patagonia
Fig. 2. Geochronology of SALMAs and litostratigraphic units mentioned in the text modified from Gelfo et al. (2009) and Krause et al. (2017). The formations outcrop in different localities: 1, Northwest Patagonia, Argentina; 2, Tiupampa, Bolivia; 3, San Jorge Basin, Patagonia, Argentina. Abbreviations: C., Cocatherium; Fm., Formation.
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Allen Brain Atlas
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DANDI Archive for NWB datasets
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OpenNeuro
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