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Fig. 18. Strict consensus trees resulting from a in Taxonomic and stratigraphic update of the material historically attributed to Megalosaurus from Portugal
Fig. 18. Strict consensus trees resulting from a cladistic analysis performed on a dentition-based data matrix and forcing the constrains defined by Hendrickx et al. (2020a) with the five tooth morphotypes from the Lusitanian Basin (A), simplified strict consensus tree resulting from the cladistic analysis pruning a priori all morphotypes from the Lusitanian Basin but Morphotype 1 (B), and simplified strict consensus tree resulting from the analysis pruning a priori all morphotypes from the Lusitanian Basin but MNHN/UL.EPt.023 (C).
Fig. 17 in Taxonomic and stratigraphic update of the material historically attributed to Megalosaurus from Portugal
Fig. 17. Tooth crowns attributed to cf. Ceratosaurus sp. from the Kimmeridgian–Tithonian Sobral Formation, Atalaia and Porto das Barcas (Lourinhã region, Portugal). A. MG 8777. B. MNHN/UL.EPt.021. Labial (A1, B1), distal (A2, B2), mesial (A3, B3), and lingual (A4, B4) views; basal cross-section A5, A6, B5); detail of the distal denticles (B6).
Fig. 16 in Taxonomic and stratigraphic update of the material historically attributed to Megalosaurus from Portugal
Fig. 16. Graphical results of the Linear Discriminant Analysis (LDA) of 581 tooth crowns belonging to twenty-two theropod taxa and the isolated specimens from the Lusitanian Basin studied in this work. Eigenvalue of axis 1 = 8.2989 (which accounts for 67.28% of the total variation) and eigenvalue of axis 2 = 1.129 (which accounts for 9.152% of the total variation). AL, apical length; CBW, crown base width; CH, crown height; DA, distoapical denticle density; DB, distobasal denticle density; DC, distocentral denticle density; MA, mesioapical denticle density; MB, mesiobasal denticle density; MC, mesiocentral denticle density; MCL, mid-crown length; MCW, mid-crown width; MDE, mesiobasal denticles extent.
Fig. 15 in Taxonomic and stratigraphic update of the material historically attributed to Megalosaurus from Portugal
Fig. 15. Partial anterior caudal vertebra (MMLT.002528) attributed to an indeterminate Titanosauriformes sauropod from the Kimmeridgian–Tithonian Sobral Formation, Porto das Barcas (Lourinhã region, Portugal) right lateral (A1), left lateral (A2), posterior (A3), anterior (A4), dorsal (anterior to the left, A5), and ventral (anterior to the right, A6) views.
Fig. 14 in Taxonomic and stratigraphic update of the material historically attributed to Megalosaurus from Portugal
Fig. 14. Portion of the proximal end of a right humerus (MG 8812) attributed to an indeterminate eusauropod dinosaur from the Kimmeridgian Alcobaça Formation, Ourém region (Portugal) in posterior (A1) and anterior (A2) views.
Fig. 25 in Taxonomic and stratigraphic update of the material historically attributed to Megalosaurus from Portugal
Fig. 25. Mesial tooth crowns attributed to allosauroid theropod Allosaurus sp. from different Upper Jurassic localities of Portugal. A. MG 4817,?Atalaia Lourinhã region). B. MG 8775, Ribamar (Lourinhã region). C. MNHN/UL.EPt.019, unknown locality (Pombal region). Lingual (A1, B1, C1), labial (A2, B4, C5), distal (A3, B3, C2), and mesial (A4, B2, C4), views; basal cross-section (B5, C3); detail of the distal denticles from the central and basal sector of the crown respectively (C6, C7); detail of the mesial denticles from the central and basal sector of the crown respectively (C8, C9).
Fig. 13 in Taxonomic and stratigraphic update of the material historically attributed to Megalosaurus from Portugal
Fig. 13. Posterior caudal centrum (MNHN/UL.EPt.024) attributed to an iguanodontian dinosaur from the Tithonian Bombarral Formation, Praia de Areia Branca (Lourinhã region, Portugal) in right lateral (A1), left lateral (A2), anterior (A3), ventral (anterior to the left, A4), dorsal (anterior to the left, A5), and posterior (A6) views.
Fig. 12 in Taxonomic and stratigraphic update of the material historically attributed to Megalosaurus from Portugal
Fig. 12. Vertebrae attributed to indeterminate iguanodontian dinosaurs from the Kimmeridgian Alcobaça Formation and the Tithonian Bombarral Formation, Portugal. A. Sacral vertebra, MG 8786, Torrinhas (Batalha region). B. Dorsal vertebra, MG 4825, Cesareda (Óbidos region). C. Two articulated anterior caudal vertebrae, MG 4820, Casais da Pedreira (Lourinhã region). Left lateral (A1–C1), right lateral (A2–C2), anterior (A3–C3), posterior (A4, B4, C6), ventral A5, B5, C4), and dorsal (A6, B6, C5) views.
Fig. 11 in Taxonomic and stratigraphic update of the material historically attributed to Megalosaurus from Portugal
Fig. 11. Caudal vertebrae attributed to indeterminate stegosaurian dinosaurs from the Kimmeridgian–Tithonian Sobral Formation and Tithonian Bombarral Formation, Porto das Barcas and Casal de Labrusque (Lourinhã region, Portugal). A. Anterior caudal vertebra, MNHN/UL.EPt.020. B. Centrum of a posterior caudal vertebra, MNHN/UL.EPt.027. Left lateral (A1, B1), right lateral (A2, B2), dorsal (anterior to the right, A3), ventral (anterior to the left, A4, B5), anterior (A5, B3), and posterior (A6, B4) views.
Fig. 10 in Taxonomic and stratigraphic update of the material historically attributed to Megalosaurus from Portugal
Fig. 10. Dorsal vertebrae attributed to indeterminate stegosaurian dinosaurs from the Kimmeridgian–Tithonian Sobral Formation, Paimogo (Lourinhã region, Portugal) and from the Kimmeridgian Alcobaça Formation, Torrinhas (Batalha region, Portugal). A. MG 4823. B. MG 4827. Left lateral (A1, B1), right lateral (A2, B2), anterior (A3, B3), ventral (anterior to the right, A4, B4), dorsal (anterior to the left, A5, B5), and posterior (A6, B6) views.
Fig. 3 in Taxonomic and stratigraphic update of the material historically attributed to Megalosaurus from Portugal
Fig. 3. Geological and stratigraphical context of fossil sites in the northern part of the Consolação sub-basin and in the Bombarral sub-basin. A. Geological map of the region between Caldas da Rainha and Alcobaça with localities yielding fossil remains studied in this work (modified from Zbyszewski and Moitinho de Almeida 1960; Camarate França and Zbyszewski 1963). B. Map of the Lusitanian Basin with the main structural elements and the different sub-basins (sensu Fürsich et al. 2021). C. Simplified stratigraphy of the Upper Jurassic and Lower Cretaceous sequences in the Consolação-S. Martinho, Torres Vedras and Lourinhã coastal regions. The stratigraphy for Torres Vedras and Lourinhã based on Hill (1988) and Manuppella et al. (1999a) and for the littoral of Consolação-S. Martinho do Porto based on Manuppella et al. (1999a) and Azerêdo et al. (2010). Abbreviations: Chron., Chronostratigraphy; Fm., Formation; mb., member; l., lower; m., middle; Oxfor., Oxfordian; sb., sub-basin; u., upper.
Fig. 4 in Taxonomic and stratigraphic update of the material historically attributed to Megalosaurus from Portugal
Fig. 4. Geological and stratigraphical context of fossil sites in the Mamede sub-basin. A. Geological map of the region of Batalha and Ourém with localities yielding fossil remains studied in this work (modified from Teixeira et al. 1968; Manuppella et al. 2000). B. Map of the Lusitanian Basin with the main structural elements and the different sub-basins (sensu Fürsich et al. 2021). C. Simplified stratigraphy of the Upper Jurassic sequences in the Mamede sub-basin based on Kullberg et al. (2013) and Fürsich et al. (2021). Abbreviations: Chron., Chronostratigraphy; Fm., Formation; mb., member; l ., lower; m., middle; sb., sub-basin; u., upper.
Fig. 7 in Taxonomic and stratigraphic update of the material historically attributed to Megalosaurus from Portugal
Fig. 7. Geological and stratigraphical context of the Figeira de Foz and Aveiro region. A. Map of the Lusitanian Basin with the main structural elements and the different sub-basins (sensu Fürsich et al. 2021). B. Geological map of Figueira da Foz and Aveiro region (Aveiro sub-basin) with localities yielding fossil remains studied in this work (modified from Rocha et al. 1981 and Barbosa et al. 2008). C. Simplified stratigraphy of the Upper Cretaceous sequences in the Figueira da Foz and Aveiro sub-basins based on Barbosa et al. (2008). Abbreviations: Chron., Chronostratigraphy; Fm., Formation; mb., member; l., lower; m., middle; sb., sub-basin; u., upper.
Fig. 9 in Taxonomic and stratigraphic update of the material historically attributed to Megalosaurus from Portugal
Fig. 9. Cervical (MG 8798a) and dorsal (MG 8798b) vertebrae attributed to indeterminate stegosaurian dinosaurs from the Kimmeridgian–Tothonian Sobral Formation, Porto das Barcas (Lourinhã region, Portugal). A. MG 8798a. B. MG 8798b. Right lateral (A1, B1), left lateral (A2, B2), anterior (A3, B3), dorsal (anterior to the left, A4, B4), ventral (anterior to the right, A5, B5), and posterior (A6, B6) views.
Fig. 6 in Taxonomic and stratigraphic update of the material historically attributed to Megalosaurus from Portugal
Fig. 6. Geological and stratigraphical context of fossil sites in the Setúbal sub-basin. A. Map of the Lusitanian Basin with the main structural elements and the different sub-basins (sensu Fürsich et al. 2021). B. Geological map of the Sesimbra to Cabo Espichel region with localities yielding fossil remains studied in this work (modified from Manuppella et al. 1999b). C. Simplified stratigraphy of the Lower Cretaceous sequences in the Setúbal sub-basin based on Manuppella et al. (1999b). The stratigraphic position of the Papo Seco Formation from which the studied fossils were collected is marked in green. Abbreviations: Chron., Chronostratigraphy; Fm., Formation; mb., member; l., lower; m., middle; sb., sub-basin; u., upper.
Fig. 2 in Taxonomic and stratigraphic update of the material historically attributed to Megalosaurus from Portugal
Fig. 2. Geological and stratigraphical context of fossil sites in the Consolação and Bombarral sub-basins, Portugal. A. Geological map of coastal region of Lourinhã and Peniche with localities yielding fossil remains studied in this work (modified from Camarate França et al. 1960; Manuppella et al. 1999a). B. Map of the Lusitanian Basin with the main structural elements and the different sub-basins (sensu Fürsich et al. 2021). C. Simplified stratigraphy of the Upper Jurassic and Lower Cretaceous sequences in the Torres Vedras and Lourinhã costal region and Consolação-S.Martinho do Porto coastal region based on Hill (1988), Manuppella et al. (1999a) and Azerêdo et al. (2010). Abbreviations: Assen., Assenta; Chron., Chronostratigraphy; Fm., Formation; mb., member; l., lower; m., middle; Oxfor., Oxfordian; sb., sub-basin; u., upper.
Fig. 5 in Taxonomic and stratigraphic update of the material historically attributed to Megalosaurus from Portugal
Fig. 5. Geological and stratigraphical context of fossil sites in the Mamede sub-basin. A. Map of the Lusitanian Basin with the main structural elements and the different sub-basins (sensu Fürsich et al. 2021). B. Geological map map of the region of Pombal and Leiria with localities yielding fossil remains studied in this work (modified from Teixeira et al. 1968; Manuppella et al. 1978). C. Simplified stratigraphy of the Upper Jurassic sequences in the Mamede sub-basin based on Kullberg et al. (2013) and Fürsich et al. (2021). Abbreviations: Berrias., Berriasian; Chron., Chronostratigraphy; Fm., Formation; mb., member; l., lower; m., middle; Oxf., Oxfordian; sb., sub-basin; u., upper.
Fig. 8 in Taxonomic and stratigraphic update of the material historically attributed to Megalosaurus from Portugal
Fig. 8. Cervical vertebrae attributed to a thalattosuchian crocodyliforms from the Kimmeridgian Alcobaça Formation, Fervença (Alcobaça region, Portugal). A. MG 4829a. B. MG 4829b. Right lateral (A1, B1), left lateral (A2, B2), anterior (A3, B3), dorsal (anterior to the right, A4, B4), ventral (anterior to the left, A5, B5), and posterior (A6, B6) views.
Fig. 1 in Taxonomic and stratigraphic update of the material historically attributed to Megalosaurus from Portugal
Fig. 1. Geological map (adapted from Oliveira et al. 1992) showing the Mesozoic levels and the main structures that delimit the different sectors (sensu Ribeiro et al. 1996 and Kullberg et al. 2006) and sub-basins (sensu Fürsich et al. 2021) of the Lusitanian Basin, Portugal.
Figure 2 in Changes in galling insect community on Caryocar brasiliense trees mediated by soil chemical and physical attributes
Figure 2. Principal components regressions among: (A) Eurytoma sp. galling insect adults (Eur.) with phosphorus-Mehlich 1 (mg dm-3) contents (P.C.) and silt (dag kg-1) (Si.); (B) numbers of Eurytoma sp. glodoid galls (E.G.G.) with pH in water, capacity of cationic exchange (cmol dm-3) (C.C.E.), and P.C.; (C) area (mm2) of Eurytoma sp. glodoid galls (A.E.G.) with pH and clay (dag kg-1) (Cl.); (D) c length of conglomerate of Eurytoma sp. globoid galls (L.G.E.) with pH and Cl.; (E) width of conglomerate of Eurytoma sp. globoid galls (W.G.E.) with pH and Cl.; and (F) number of Hymenopteran discoid galls (H.D.G.) with aluminum (cmol dm-3) contents (A.C.), C.C.E., c and percentage of soil base saturation of the capacity of cationic exchange to pH 7.0 (S.B.S.) on Caryocar brasiliense trees in three years. The symbols represent the averages and the bars the standard errors. n = 111.
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