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1,817 results for “Late Cretaceous”
Fig. 21 in On the "Coccodus" lindstroemi species complex (Pycnodontiformes, Gladiopycnodontidae) from the marine Late Cretaceous of Lebanon, with the description of two new genera
Fig. 21. Pankowskichthys libanicus gen. et sp. nov. A scute-like body scale of holotype, IRSNB P 9278.
Fig. 19 in On the "Coccodus" lindstroemi species complex (Pycnodontiformes, Gladiopycnodontidae) from the marine Late Cretaceous of Lebanon, with the description of two new genera
Fig. 19. Pankowskichthys libanicus gen. et sp. nov. Reconstruction of the skull and the pectoral girdle based on holotype, IRSNB P 9278.
Fig. 18 in On the "Coccodus" lindstroemi species complex (Pycnodontiformes, Gladiopycnodontidae) from the marine Late Cretaceous of Lebanon, with the description of two new genera
Fig. 18. Pankowskichthys libanicus gen. et sp. nov. General reconstruction based on holotype, IRSNB P 9278.
Fig. 16 in On the "Coccodus" lindstroemi species complex (Pycnodontiformes, Gladiopycnodontidae) from the marine Late Cretaceous of Lebanon, with the description of two new genera
Fig. 16. Joinvillichthys kriweti gen. et sp. nov. Holotype, CLC S-137. A. Dorsal ridge scutes. B. Anterior flake-like body scales. C. Posterior scute-like body scale. D. Ventral keel scutes.
Fig. 14 in On the "Coccodus" lindstroemi species complex (Pycnodontiformes, Gladiopycnodontidae) from the marine Late Cretaceous of Lebanon, with the description of two new genera
Fig. 14. Joinvillichthys kriweti gen. et sp. nov. Reconstruction of the skull and the pectoral girdle based on holotype, CLC S-137.
Fig. 13 in On the "Coccodus" lindstroemi species complex (Pycnodontiformes, Gladiopycnodontidae) from the marine Late Cretaceous of Lebanon, with the description of two new genera
Fig. 13. Joinvillichthys kriweti gen. et sp. nov. General reconstruction based on holotype, CLC S-137.
Fig. 15 in On the "Coccodus" lindstroemi species complex (Pycnodontiformes, Gladiopycnodontidae) from the marine Late Cretaceous of Lebanon, with the description of two new genera
Fig. 15. Joinvillichthys kriweti gen. et sp. nov. Caudal skeleton of holotype, CLC S-137. The arrows indicate the positions of the most external dorsal and ventral procurrent rays of the caudal fin.
Fig. 10 in On the "Coccodus" lindstroemi species complex (Pycnodontiformes, Gladiopycnodontidae) from the marine Late Cretaceous of Lebanon, with the description of two new genera
Fig. 10. Joinvillichthys lindstroemi (Davis, 1890). Hypochordal elements of sample CLC S-138. The arrows indicate the position of the most external dorsal and ventral procurrent ray of the caudal fin.
Fig. 11 in On the "Coccodus" lindstroemi species complex (Pycnodontiformes, Gladiopycnodontidae) from the marine Late Cretaceous of Lebanon, with the description of two new genera
Fig. 11. Joinvillichthys lindstroemi (Davis, 1890). A. Dorsal ridge scutes of sample IRSNB N° P 9276. B. Anterior flake-like body scales of sample CLC S-138. C. Posterior scute-like body scale of sample CLC S-138. D. Ventral keel scutes of sample CLC S-138.
Fig. 6 in On the "Coccodus" lindstroemi species complex (Pycnodontiformes, Gladiopycnodontidae) from the marine Late Cretaceous of Lebanon, with the description of two new genera
Fig. 6. Joinvillichthys lindstroemi (Davis, 1890). Reconstruction of the skull and the pectoral girdle based on holotype, NRM PZ P. 2073, and samples IRSNB N° P 9276, CLC S-138 and CLC S-324. The scale refers to sample CLC S-138.
Fig. 41 in Morphology Of The Late Cretaceous Crocodylomorph Shamosuchus Djadochtaensis And A Discussion Of Neosuchian Phylogeny As Related To The Origin Of Eusuchia
Fig. 41. Phylogeny of Crocodyliformes calibrated against geological time. The solid grey line highlights the presence of an extensive ghost lineage that trace the origins of advanced neosuchians back to the Early Jurassic. This extension implies a long unknown period in their history that predates their first appearance by more than 50 million years. Such a remote origin, coupled with the worldwide distribution of the group can be indicative of an initial diversification prior to the effective separation of the major continental landmasses.
Fig. 39 in Morphology Of The Late Cretaceous Crocodylomorph Shamosuchus Djadochtaensis And A Discussion Of Neosuchian Phylogeny As Related To The Origin Of Eusuchia
Fig. 39. Reduced strict consensus of the 39 most parsimonious trees obtained in the exploratory analysis with the addition of five taxa (highlighted in grey) that have been preliminary scored to test their positions as well as the robustness of the relationships proposed in figure 37. This analysis includes Isisfordia duncani, Susisuchus anatoceps, Pachycheilosuchus trinquei, Glichristosuchus palatinus, and Allodaposuchus precedens, in addition to the previously included taxa. Two of the alternative positions retrieved for Glichristosuchus palatinus are indicated with a dashed grey line. Other optimal positions depict this taxon nested within Crocodylia.
Fig. 36 in Morphology Of The Late Cretaceous Crocodylomorph Shamosuchus Djadochtaensis And A Discussion Of Neosuchian Phylogeny As Related To The Origin Of Eusuchia
Fig. 36. Ventral osteoderms of the referred specimen of Shamosuchus djadochtaensis IGM 100/1195. See appendix 5 for abbreviations.
Fig. 33 in Morphology Of The Late Cretaceous Crocodylomorph Shamosuchus Djadochtaensis And A Discussion Of Neosuchian Phylogeny As Related To The Origin Of Eusuchia
Fig. 33. Metatarsal III (A) and metatarsal IV (B) of the referred specimen of Shamosuchus djadochtaensis IGM 100/1195 in anterior and posterior views.
Fig. 27 in Morphology Of The Late Cretaceous Crocodylomorph Shamosuchus Djadochtaensis And A Discussion Of Neosuchian Phylogeny As Related To The Origin Of Eusuchia
Fig. 27. Close-up of proximal portion of left radius of referred specimen of Shamosuchus djadochtaensis IGM 100/1195 in lateral view. See appendix 5 for abbreviations.
Fig. 30 in Morphology Of The Late Cretaceous Crocodylomorph Shamosuchus Djadochtaensis And A Discussion Of Neosuchian Phylogeny As Related To The Origin Of Eusuchia
Fig. 30. Distal end of left femur of the referred specimen of Shamosuchus djadochtaensis IGM 100/1195 in all views.
Fig. 25 in Morphology Of The Late Cretaceous Crocodylomorph Shamosuchus Djadochtaensis And A Discussion Of Neosuchian Phylogeny As Related To The Origin Of Eusuchia
Fig. 25. Left humerus and proximal left radius of the referred specimen of Shamosuchus djadochtaensis IGM 100/1195 in dorsal view. See appendix 5 for abbreviations.
Fig. 26 in Morphology Of The Late Cretaceous Crocodylomorph Shamosuchus Djadochtaensis And A Discussion Of Neosuchian Phylogeny As Related To The Origin Of Eusuchia
Fig. 26. Distal half of left humerus of referred specimen of Shamosuchus djadochtaensis IGM 100/1195 in all views. See appendix 5 for abbreviations.
Fig. 29 in Morphology Of The Late Cretaceous Crocodylomorph Shamosuchus Djadochtaensis And A Discussion Of Neosuchian Phylogeny As Related To The Origin Of Eusuchia
Fig. 29. Partial right ischium of referred specimen of Shamosuchus djadochtaensis IGM 100/1195 in lateral (left) and medial (right). See appendix 5 for abbreviations.
Fig. 23 in Morphology Of The Late Cretaceous Crocodylomorph Shamosuchus Djadochtaensis And A Discussion Of Neosuchian Phylogeny As Related To The Origin Of Eusuchia
Fig. 23. Anterior dorsal ribs of the referred specimen of Shamosuchus djadochtaensis IGM 100/1195. See appendix 5 for abbreviations.
ScienceDex guides
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These curated guides explain access requirements, typical timelines, costs, and reuse considerations for widely used research datasets.
Allen Brain Atlas
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DANDI Archive for NWB datasets
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International Brain Laboratory public data
The International Brain Laboratory public data releases expose standardized mouse decision-making experiments, including Neuropixels recordings, widefield calcium imaging, behavior, and session metadata accessed through the ONE API.
OpenNeuro
OpenNeuro is a free, open platform for sharing neuroimaging datasets, with public search, dataset pages, and download paths for web, S3, DataLad, and the OpenNeuro CLI.