Current characterizations of early dinosaur evolution are incomplete: existing palaeobiological and phylogenetic scenarios are based on a fossil record dominated by saurischians and the implications of the early ornithischian record are often overlooked. Moreover, the timings of deep phylogenetic divergences within Dinosauria are poorly constrained owing to the absence of a rigorous chronostratigraphical framework for key Late Triassic–Early Jurassic localities. A new dinosaur from the earliest Jurassic of the Venezuelan Andes is the first basal ornithischian recovered from terrestrial deposits directly associated with a precise radioisotopic date and the first-named dinosaur from northern South America. It expands the early palaeogeographical range of Ornithischia to palaeoequatorial regions, an area sometimes thought to be devoid of early dinosaur taxa, and offers insights into early dinosaur growth rates, the evolution of sociality and the rapid tempo of the global dinosaur radiation following the end-Triassic mass extinction, helping to underscore the importance of the ornithischian record in broad-scale discussions of early dinosaur history.
Laquintasaurus Treefile
Treefile with results of published analyses
Laquinta analysis_Treefile
Laquintasaura_TNT dataset
Original TNT data for early ornithischian phylogenetic analysis
Figure2A
High resolution image of Figure 2(a). Osteohistological section of small tibia (MBLUZ P.5021), from a juvenile individual: (a) complete section in normal-polarized transmitted light and (b) close-up of cortex in cross-polarized light using lambda compensator. The entire compacta consists of parallel-fibred bone subdivided by two growth annuli (marked by arrowheads). The bone tissue is vascularized by simple primary canals and woven bone is absent.
Figure2B
High resolution version of Figure 2(b). Figure 2. Osteohistological section of small tibia (MBLUZ P.5021), from a juvenile individual: (a) complete section in normal-polarized transmitted light and (b) close-up of cortex in cross-polarized light using lambda compensator. The entire compacta consists of parallel-fibred bone subdivided by two growth annuli (marked by arrowheads). The bone tissue is vascularized by simple primary canals and woven bone is absent.
Supplement_S6A
High resolution image of Supplementary Figure 6(a). Overview images of thin-sections of smaller right tibia P.5021 (A, B) and partial larger tibia P.5020 (C) sampled. Image A is in normal transmitted, B and C in polarised light using lambda compensator.
Supplement_S6B
High resolution image of Supplementary Figure 6(b). Figure S6. Overview images of thin-sections of smaller right tibia P.5021 (A, B) and partial larger tibia P.5020 (C) sampled. Image A is in normal transmitted, B and C in polarised light using lambda compensator.
Supplement_S6C
High resolution version of Figure S6(c). Overview images of thin-sections of smaller right tibia P.5021 (A, B) and partial larger tibia P.5020 (C) sampled. Image A is in normal transmitted, B and C in polarised light using lambda compensator.
Supplement_S7A
High resolution version of Supplementary Figure 7(a). Figure S7. Thin-sections of smaller right tibia P.5021 (A–C, F), the indeterminate long bone P.5023 (D) and femur P.5023 (E). Image C is in normal transmitted, A, D and E in polarised, and B and F in polarised light using lambda compensator. A, B. Cortical bone showing parallel-fibred bone tissue subdivided by two annuli (marked by arrowheads). C. Higher magnification of the cortical bone. The bone tissue is vascularized by numerous primary vascular canals, which are oriented longitudinally or obliquely. D. Close-up view of the cortical parallel-fibred bone tissue with reticular vascularisation pattern. E. Close-up of cortex with laminar organisation of vascular spaces. F. Remnant of endosteal lamellar bone tissue (marked by arrowheads) surrounding in part the medullary cavity. PC, primary vascular canals; PFB, parallel-fibred bone.
Supplement_S7B
High resolution version of Supplementary Figure 7(b). Figure S7. Thin-sections of smaller right tibia P.5021 (A–C, F), the indeterminate long bone P.5023 (D) and femur P.5023 (E). Image C is in normal transmitted, A, D and E in polarised, and B and F in polarised light using lambda compensator. A, B. Cortical bone showing parallel-fibred bone tissue subdivided by two annuli (marked by arrowheads). C. Higher magnification of the cortical bone. The bone tissue is vascularized by numerous primary vascular canals, which are oriented longitudinally or obliquely. D. Close-up view of the cortical parallel-fibred bone tissue with reticular vascularisation pattern. E. Close-up of cortex with laminar organisation of vascular spaces. F. Remnant of endosteal lamellar bone tissue (marked by arrowheads) surrounding in part the medullary cavity. PC, primary vascular canals; PFB, parallel-fibred bone.
Supplement_S7C
High resolution version of Supplementary Figure 7(c). Figure S7. Thin-sections of smaller right tibia P.5021 (A–C, F), the indeterminate long bone P.5023 (D) and femur P.5023 (E). Image C is in normal transmitted, A, D and E in polarised, and B and F in polarised light using lambda compensator. A, B. Cortical bone showing parallel-fibred bone tissue subdivided by two annuli (marked by arrowheads). C. Higher magnification of the cortical bone. The bone tissue is vascularized by numerous primary vascular canals, which are oriented longitudinally or obliquely. D. Close-up view of the cortical parallel-fibred bone tissue with reticular vascularisation pattern. E. Close-up of cortex with laminar organisation of vascular spaces. F. Remnant of endosteal lamellar bone tissue (marked by arrowheads) surrounding in part the medullary cavity. PC, primary vascular canals; PFB, parallel-fibred bone.
Supplement_S7D
High resolution version of Supplementary Figure 7(d). Figure S7. Thin-sections of smaller right tibia P.5021 (A–C, F), the indeterminate long bone P.5023 (D) and femur P.5023 (E). Image C is in normal transmitted, A, D and E in polarised, and B and F in polarised light using lambda compensator. A, B. Cortical bone showing parallel-fibred bone tissue subdivided by two annuli (marked by arrowheads). C. Higher magnification of the cortical bone. The bone tissue is vascularized by numerous primary vascular canals, which are oriented longitudinally or obliquely. D. Close-up view of the cortical parallel-fibred bone tissue with reticular vascularisation pattern. E. Close-up of cortex with laminar organisation of vascular spaces. F. Remnant of endosteal lamellar bone tissue (marked by arrowheads) surrounding in part the medullary cavity. PC, primary vascular canals; PFB, parallel-fibred bone.
Supplement_S7E
High resolution version of Supplementary Figure 7(e). Figure S7. Thin-sections of smaller right tibia P.5021 (A–C, F), the indeterminate long bone P.5023 (D) and femur P.5023 (E). Image C is in normal transmitted, A, D and E in polarised, and B and F in polarised light using lambda compensator. A, B. Cortical bone showing parallel-fibred bone tissue subdivided by two annuli (marked by arrowheads). C. Higher magnification of the cortical bone. The bone tissue is vascularized by numerous primary vascular canals, which are oriented longitudinally or obliquely. D. Close-up view of the cortical parallel-fibred bone tissue with reticular vascularisation pattern. E. Close-up of cortex with laminar organisation of vascular spaces. F. Remnant of endosteal lamellar bone tissue (marked by arrowheads) surrounding in part the medullary cavity. PC, primary vascular canals; PFB, parallel-fibred bone.
Supplement_S7F
High resolution version of Supplementary Figure 7(f). Figure S7. Thin-sections of smaller right tibia P.5021 (A–C, F), the indeterminate long bone P.5023 (D) and femur P.5023 (E). Image C is in normal transmitted, A, D and E in polarised, and B and F in polarised light using lambda compensator. A, B. Cortical bone showing parallel-fibred bone tissue subdivided by two annuli (marked by arrowheads). C. Higher magnification of the cortical bone. The bone tissue is vascularized by numerous primary vascular canals, which are oriented longitudinally or obliquely. D. Close-up view of the cortical parallel-fibred bone tissue with reticular vascularisation pattern. E. Close-up of cortex with laminar organisation of vascular spaces. F. Remnant of endosteal lamellar bone tissue (marked by arrowheads) surrounding in part the medullary cavity. PC, primary vascular canals; PFB, parallel-fibred bone.
Supplement_S8A
High resolution version of Supplementary Figure 8(a). Figure S8. Overview images of thin-sectioned mid-shaft region of rib P.5029 (A) and partial left scapula P.5012 (B). Image A is in normal transmitted, B in polarised light using lambda compensator.
Supplement_S8B
High resolution version of Supplementary Figure 8(b). Figure S8. Overview images of thin-sectioned mid-shaft region of rib P.5029 (A) and partial left scapula P.5012 (B). Image A is in normal transmitted, B in polarised light using lambda compensator.
Supplement_S9A
High-resolution image of Supplementary Figure 9(a). Figure S9. Thin-sections of smaller partial left scapula P.5012 (A–C). Image A is in normal transmitted, B in polarised, and C in polarised light using lambda compensator. All three images show the same section of cortical bone in higher magnification. The bone surface is towards the bottom of the image. The primary parallel-fibred bone tissue is in various stages of remodelling by secondary osteons and erosion cavities. Two widely spaced incremental growth marks (i.e., lines of arrested growth, LAGs) are indicated with white arrowheads, whereas an external fundamental system consisting of about seven incremental LAGs is situated in close proximity to the external bone surface. Note the peculiar colouration of the bone cell lacunae in image C (blue colours), due to the infilling with green mineral phase (visible in A), i.e., chlorite. EC, erosion cavity; EFS, external fundamental system; PFB, parallel-fibred bone; SO, secondary osteon.
Supplement_S9B
High-resolution image of Supplementary Figure 9(b). Figure S9. Thin-sections of smaller partial left scapula P.5012 (A–C). Image A is in normal transmitted, B in polarised, and C in polarised light using lambda compensator. All three images show the same section of cortical bone in higher magnification. The bone surface is towards the bottom of the image. The primary parallel-fibred bone tissue is in various stages of remodelling by secondary osteons and erosion cavities. Two widely spaced incremental growth marks (i.e., lines of arrested growth, LAGs) are indicated with white arrowheads, whereas an external fundamental system consisting of about seven incremental LAGs is situated in close proximity to the external bone surface. Note the peculiar colouration of the bone cell lacunae in image C (blue colours), due to the infilling with green mineral phase (visible in A), i.e., chlorite. EC, erosion cavity; EFS, external fundamental system; PFB, parallel-fibred bone; SO, secondary osteon.
Supplement_S9C
High-resolution image of Supplementary Figure 9(c). Figure S9. Thin-sections of smaller partial left scapula P.5012 (A–C). Image A is in normal transmitted, B in polarised, and C in polarised light using lambda compensator. All three images show the same section of cortical bone in higher magnification. The bone surface is towards the bottom of the image. The primary parallel-fibred bone tissue is in various stages of remodelling by secondary osteons and erosion cavities. Two widely spaced incremental growth marks (i.e., lines of arrested growth, LAGs) are indicated with white arrowheads, whereas an external fundamental system consisting of about seven incremental LAGs is situated in close proximity to the external bone surface. Note the peculiar colouration of the bone cell lacunae in image C (blue colours), due to the infilling with green mineral phase (visible in A), i.e., chlorite. EC, erosion cavity; EFS, external fundamental system; PFB, parallel-fibred bone; SO, secondary osteon.