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Royo-Torres, Rafael, Cobos, Alberto, Mocho, Pedro, Alcalá, Luis (2021): Origin and evolution of turiasaur dinosaurs set by means of a new 'rosetta' specimen from Spain. Zoological Journal of the Linnean Society 191: 201-227, DOI: 10.1093/zoolinnean/zlaa091

LOSILLASAURUS CASANOVAS ET AL., 2001 Figures: See Casanovas et al., 2001: figs 1–7; Figs 1–16; Supporting Information, File S3. Type species: Losillasaurus giganteus Casanovas et al. (2001). Holotype: Anterior caudal vertebra housed in the Museo de Ciencias Naturales de Valencia (MCNV). Paratype: Two anterior caudal vertebrae housed in the Museo de Ciencias Naturales de Valencia (MCNV). Type locality and horizon: La Cañada site (Valencia), V i l l a r d e l A r z o b i s p o Fo r m a t i o n (C a s a n o v a s et al., 2001; Royo-Torres et al., 2006). Dated as Kimmeridgian according to the data of Campos-Soto et al. (2019). Referred material: The material referred to Losillasaurus comes from the same specimen from where the holotype and paratype were selected. It consists of a skull fragment and partial postcranial skeleton (see Supporting Information, File S1). A second specimen, described in this paper, is from the San Lorenzo site (Riodeva, Teruel, Spain) in the Villar del Arzobispo Formation. It consists of a partial skull with teeth and partial postcranial skeleton (see the previous description section and Supporting Information, File S1). A third specimen referred to as Losillasaurus is a complete anterior caudal vertebra (SHN 180) found in Baleal (Peniche municipality, Portugal) in the Praia de Amoreira-Porto Novo Formation, dated as Upper Kimmeridgian–Lower Tithonian (Manuppella et al., 1999; Mocho et al., 2017b). Revised diagnosis: Losillasaurus is diagnosed by eight autapomorphies: (1) (new) lateral surface of the premaxilla and maxilla with dorsoventrally elongated grooves convergent with diplodocids and Nemegtosaurus (Mannion et al., 2019); (2) (new) a maxillary tooth with a secondary apex on the distal edge; (3) markedly curved neural spines of the proximal caudal vertebrae that in the first and second caudal vertebrae produce a pronounced cutlass-like shape in the lateral view (Casanovas et al., 2001; Upchurch et al., 2004a); (4) (new) presence of a dorsoventral ridge in the anterolateral surface of the spine at least between the fourth and tenthcaudal vertebrae (it is not clearly present in the first three caudal vertebrae and disappears in the 11 th caudal vertebra); (5) (new) caudal neural spines with a shallow dorsal groove with directed anteroposteriorly, bigger in the anteriormost caudal vertebrae, especially in the first and second bones and shallow from the third to the 30 th caudal vertebrae; (6) (new) the long-axis of the obturator foramen is perpendicular to the long-axis of the pubis; (7) (new) the lateral trochanter of the fibula is concave and rugose; and (8) (new) the tibial condyle of the femur is twice as large as the fibula condyle. Additional comments: The character, anteroposterior length at the base of the neural spines of the proximal caudal vertebrae being approximately half the height of the spine (ratio = 0.5), was included in the original diagnosis (Casanovas et al., 2001) and accepted in Upchurch et al. (2004a). However, this is not considered valid as the spines are compressed by taphonomic deformation., Published as part of Royo-Torres, Rafael, Cobos, Alberto, Mocho, Pedro & Alcalá, Luis, 2021, Origin and evolution of turiasaur dinosaurs set by means of a new ' rosetta' specimen from Spain, pp. 201-227 in Zoological Journal of the Linnean Society 191 on pages 219-220, DOI: 10.1093/zoolinnean/zlaa091, http://zenodo.org/record/5724151, {"references":["Casanovas ML, Santafe JV, Sanz JL. 2001. Losillasaurus giganteus, un nuevo sauropodo del transito Jurasico - Cretacico de la cuenca de \" Los Serranos \" (Valencia, Espana). Paleontologia i Evolucio 32 - 33: 99 - 122.","Royo-Torres R, Cobos A, Alcala L. 2006. A giant European dinosaur and a new sauropod clade. Science 314: 1925 - 1927.","Campos-Soto S, Benito MI, Cobos A, Caus E, Quijada IE, Suarez-Gonzalez P, Mas R, Royo-Torres R, Alcala L. 2019. Revisiting the age and palaeoenvironments of the Upper Jurassic - Lower Cretaceous? Dinosaur-bearing sedimentary record of eastern Spain: implications for Iberian palaeogeography. Journal of Iberian Geology 45: 471 - 510.","Manuppella G, Antunes MT, Pais J, Ramalho MM, Rey J. 1999. Noticia explicativa da Folha 30 A (Lourinha). Lisboa: Departamento de Geologia do Instituto Geologico e Mineiro, 83.","Mocho P, Royo-Torres R, Malafaia E, Escaso F, Ortega F. 2017 b. First occurrences of non-neosauropod eusauropod procoelous caudal vertebrae in the Portuguese Upper Jurassic record. Geobios 50: 23 - 36.","Mannion PD, Upchurch P, Schhwarz D, Wings O. 2019. Taxonomic affinities of the putative titanosaurs from the Late Jurassic Tendaguru Formation of Tanzania: phylogenetic and biogeographic implications for eusauropod dinosaur evolution. Zoological Journal of the Linnean Society 185: 784 - 909.","Upchurch P, Barrett PM, Dodson P. 2004 a. Sauropoda. In: Weishampel DB, Dodson P, Osmolska H, eds. The Dinosauria, 2 nd edn. Berkeley: University of California Press, 259 - 324."]}

El alpiste es un cereal invernal cultivado en zonas de clima templado. Su elevado valor nutricional y la ausencia de gluten en su composición, lo convierten en un cereal con un alto potencial para la elaboración o enriquecimiento de productos horneados para celiacos. En el presente trabajo se han elaborado galletas sin gluten del tipo "sugar-snap" sustituyendo harina de arroz por harina de alpiste refinada o integral en dosis del 50% y 100%, con el fin de estudiar el efecto que genera la introducción de este cereal. Se estudió el comportamiento reológico de las diferentes masas. Asimismo, se evaluaron las propiedades físicas de las distintas galletas y se realizó un análisis sensorial. Los resultados obtenidos revelaron que la introducción de alpiste reduce considerablemente la consistencia de las masas. Sin embargo, el empleo de harina integrar hizo que la masa fuese más consistente que la obtenida con harina refinada. La introducción de alpiste supuso una reducción de la dureza y un aumento del factor de propagación de las galletas. Las galletas elaboradas con harina de alpiste fueron aceptadas por los consumidores, siendo las mejor valoradas aquellas que se realizaron con harina integral. Todo ello indica que el alpiste es un ingrediente alternativo en la elaboración de galletas sin gluten. No obstante, es necesario seguir investigando sobre sus propiedades funcionales y tecnológicas con el objeto de optimizar la formulación de los productos., Máster en Calidad, Desarrollo e Innovación de Alimentos