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15 results for “Auca”
FIGURE 2 in A new species of Liolaemus (Squamata, Iguania, Liolaemini) endemic to the Auca Mahuida volcano, northwestern Patagonia, Argentina
FIGURE 2. Holotype of Liolaemus cyaneinotatus MLP.S 2618, adult male in dorsal and ventral view from Auca Mahuida volcano, Pehuenches Department, Neuquén province, Argentina.
FIGURE 3 in A new species of Liolaemus (Squamata, Iguania, Liolaemini) endemic to the Auca Mahuida volcano, northwestern Patagonia, Argentina
FIGURE 3. Complex landscape of northwestern Neuquén region; red line marks the Liolaemus cyaneinotatus approximate distribution. Yellow broken line mark limits of the Auca Mahuida Volcanic Field. Major mountain ranges, cities, and roads are also marked as reference. Inset: Region in South América.
FIGURE 5 in A new species of Liolaemus (Squamata, Iguania, Liolaemini) endemic to the Auca Mahuida volcano, northwestern Patagonia, Argentina
FIGURE 5. Bayesian consensus tree of relationships of Liolaemus cyaneinotatus with other species of the bibronii group; posterior probability values are shown at each node.
FIGURE 4 in A new species of Liolaemus (Squamata, Iguania, Liolaemini) endemic to the Auca Mahuida volcano, northwestern Patagonia, Argentina
FIGURE 4. Type locality of Liolaemus cyaneinotatus. Upper: general view of the area. Below: close view of the open areas where lizards were collected.
FIGURE 1 in A new species of Liolaemus (Squamata, Iguania, Liolaemini) endemic to the Auca Mahuida volcano, northwestern Patagonia, Argentina
FIGURE 1. Upper: Liolaemus cyaneinotatus, adult male in lateral view, showing cyan spots. Below: Liolaemus bibronii, adult male in lateral view from Puerto Deseado, Deseado Department, Santa Cruz Province (type locality).
FIGURE 7 in Molecular phylogenetic relationships of the Liolaemus rothi complex and a new species of lizard from Auca Mahuida Volcano (Squamata: Liolaemini)
FIGURE 7. Type locality of Liolaemus sitesi. Upper: general view of the area. Below: close view of the common outcrops where lizards were collected.
FIGURE 6 in Molecular phylogenetic relationships of the Liolaemus rothi complex and a new species of lizard from Auca Mahuida Volcano (Squamata: Liolaemini)
FIGURE 6. Map of northwestern Neuquén province showing the complex landscape of northern Patagonian Andes. Red dot marks the Liolaemus sitesi type locality. Red circle mark approximate distribution of Liolaemus sitesi on the slopes of Auca Mahuida Volcano; main mountain ranges, cities, and roads are also marked. Yellow outline: approximate boundaries of the Auca Mahuida Volcanic Field. Inset: Region in South América.
FIGURE 5 in Molecular phylogenetic relationships of the Liolaemus rothi complex and a new species of lizard from Auca Mahuida Volcano (Squamata: Liolaemini)
FIGURE 5. Liolaemus sitesi sp. nov., variation in color pattern of individuals of the type series. Dorsal and ventral view of males (upper) and females (below).
FIGURE 4 in Molecular phylogenetic relationships of the Liolaemus rothi complex and a new species of lizard from Auca Mahuida Volcano (Squamata: Liolaemini)
FIGURE 4. Liolaemus sitesi sp. nov., paratype LJAMM-CNP 13382, adult female in dorsal view; type locality details given in Fig. 2 caption.
FIGURE 3 in Molecular phylogenetic relationships of the Liolaemus rothi complex and a new species of lizard from Auca Mahuida Volcano (Squamata: Liolaemini)
FIGURE 3. Liolaemus sitesi sp. nov., holotype adult male in dorsal and ventral view (MLP.S 2637); type locality details given in Fig. 2 caption.
FIGURE 1 in Molecular phylogenetic relationships of the Liolaemus rothi complex and a new species of lizard from Auca Mahuida Volcano (Squamata: Liolaemini)
FIGURE 1. Phylogenetic relationships of described species of the Liolaemus rothi complex and other related species of the boulengeri complex and representatives of the fitzingerii and donosobarrosi groups. Numbers on nodes correspond to posterior probabilities.
FIGURE 2 in Molecular phylogenetic relationships of the Liolaemus rothi complex and a new species of lizard from Auca Mahuida Volcano (Squamata: Liolaemini)
FIGURE 2. Liolaemus sitesi sp. nov. Above: holotype MLP.S 2637, adult male from Park Ranger Post, 25.9 km S junction Provincial Road 6, Auca Mahuida Natural Protected Area, Pehuenches Department, Neuquén Province, Argentina. Below: unidentified paratype, adult male with typical dorsal coloration at full sun.
FIGURE 3 in Taxonomic Identification Of The Megaloolithid Egg And Eggshells From The Cretaceous Bauru Basin (Minas Gerais, Brazil): Comparison With The Auca Mahuevo (Argentina) Titanosaurid Eggs
FIGURE 3: Eggs and eggshells from the locality of Peirópolis, Marília Formation, Bauru Basin (from Magalhães Ribeiro, 2002). A: Note the elongated sub‑spherical shape of this titanosaurid egg. The presence of a single egg with eroded eggshell fragments combined with grain size of the silicoclastic sediments suggests that the egg was transported and the Peirópolis locality, in contrast to Auca Mahuevo (Patagonia), is not the primary nesting site of these dinosaurs. B: Similarly to the well‑identified titanosaurid eggs from Auca Mahuevo, the eggshell surficial ornamentation of the Peirópolis material displays single and coalescent nodes. C: Eggshell accumulation and compaction on a single slab suggesting that the egg was subjected to taphonomic forces as it was still unbroken, a process also observed in Auca Mahuevo. D: SEM view of the radial section of a Peirópolis eggshell that displays the same eggshell structure with radiating acicular crystals and shell units arrangements as those from Auca Mahuevo. E: TLM view of a Peirópolis eggshell that shows organic lines that cross horizontally the eggshell thickness as observed in specimens from Auca Mahuevo.
FIGURE 2 in Taxonomic Identification Of The Megaloolithid Egg And Eggshells From The Cretaceous Bauru Basin (Minas Gerais, Brazil): Comparison With The Auca Mahuevo (Argentina) Titanosaurid Eggs
FIGURE 2: Eggs and eggshells from the locality of Auca Mahuevo, Rio Colorado Formation, Neuquén Basin. A: Titanosaurid egg found on the surface of stratigraphic egg layer 3. Note the sub‑spherical shape of the specimen here considered either as a biological character of this saurischian family or influenced by taphonomic processes coupled with a certain eggshell plasticity due to its mono‑layered structure. B: The site of Auca Mahuevo is interpreted as a flood plain with seasonally over banking rivers where titanosaurid dinosaurs would exhibit colonial nesting and site fidelity behaviors. A large number of egg clutches are surfacing in several stratigraphic egg layers. C: Eggshell surficial ornamentation displays single and coalescent nodes (two black arrows where nodes coalesce). D: SEM image of the perfect nodular ornamentation of titanosaurid eggshells with round pore apertures located in the interstices between the nodes. E: SEM detail of figure 1D. F: cross section of a titanosaurid eggshell that shows a pore canal (arrow 1) transecting the entire thickness of the mono‑layered eggshell. Note the network of connecting vertical pores with a system of horizontal pore canals here only visible because of the MT preservation. G: TLM view of a thin section that contains two eggshell fragments facing each other. Note the cores of the shell units as shown by arrow 1, the shell units (arrows 2 and 3) crossed by lines that are interpreted as ex‑organic structures, and the MT (arrow 4) preserved only in one section of the slab.
FIGURE 1 in Taxonomic Identification Of The Megaloolithid Egg And Eggshells From The Cretaceous Bauru Basin (Minas Gerais, Brazil): Comparison With The Auca Mahuevo (Argentina) Titanosaurid Eggs
FIGURE 1: A) Location of the Peirópolis titanosaurid oological material in the Bauru Basin‑Brazil (after Riccomini 1997, modified): 1. Precambrian basement rocks; 2. Paraná Basin (Ordovician to Triassic); 3. Serra Geral Formation (Early Cretaceous); 4. Bauru Basin (Late Cretaceous). B) Stratigraphic relationships of the Bauru Group in the southeastern part of the Bauru Basin: 1. basaltic rocks; 2. cross‑bedded sansdstone; 3. massive to slightly stratified sandstone; 4. massive to slightly stratified sandstone interlayered with mudstones; 5. sandstone, siltstone and mudstone; 6. sandstone and mudstone; 7. sandstone and conglomerate with limestone cement.
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