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Late Jurassic magnetic polarity sequence
Earth and Planetary Science Letters, 1975Abstract Polarity reversal sequences have been observed in the Brushy Basin Member of the Morrison Formation (Upper Jurassic, Kimmeridgian-Tithonian age) at two sites in western Colorado separated by 80 km. The two polarity reversal sequences display a good correlation of relative lengths and number of polarity intervals and thus may provide a ...
M.B. Steiner, C.E. Helsley
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A Late Jurassic Mafic Pluton in Newfoundland
Canadian Journal of Earth Sciences, 1974A small alkaline ultramafic intrusion in central Newfoundland is dated as 135 ± 8 m.y. old and 139 ± 9 m.y. old by the K–Ar method on biotite. This is the first known Mesozoic pluton (aside from dikes) in Newfoundland. The occurrence, composition and age of the pluton and associated igneous rocks is similiar to, and perhaps related in origin to ...
J. Helwig, J. Aronson, D. S. Day
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Late Jurassic Sauropods in Chilean Patagonia
Ameghiniana, 2015Abstract. A description is provided of the first sauropod remains (i.e., isolated vertebrae and appendicular bones) from the Late Jurassic of Aysen, in Chilean Patagonia (Toqui Formation, late Tithonian). Although the bones found are fragmentary, they still allow the recognition of an unsuspected sauropod diversity for this period in South America. The
Salgado, Leonardo +6 more
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Diversity and biogeography patterns of Late Jurassic neoselachians (Chondrichthyes: Elasmobranchii)
Geological Society, London, Special Publications, 2008Abstract The regional diversity and biogeographic patterns of Late Jurassic neoselachians at genus level in Europe were analysed based on samples and an extensive literature survey of about 40 localities ranging from the Oxfordian to Tithonian.
Kriwet, J, Klug, S
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A Late Jurassic Digging Mammal and Early Mammalian Diversification
Science, 2005A fossil mammal from the Late Jurassic Morrison Formation, Colorado, has highly specialized teeth similar to those of xenarthran and tubulidentate placental mammals and different from the generalized insectivorous or omnivorous dentitions of other Jurassic mammals.
Zhe-Xi, Luo, John R, Wible
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A basal tyrannosauroid dinosaur from the Late Jurassic of China
Nature, 2006The tyrannosauroid fossil record is mainly restricted to Cretaceous sediments of Laurasia, although some very fragmentary Jurassic specimens have been referred to this group. Here we report a new basal tyrannosauroid, Guanlong wucaii gen. et sp. nov., from the lower Upper Jurassic of the Junggar Basin, northwestern China. G.
Xing, Xu +7 more
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Indian Ocean sediment distribution since the Late Jurassic
Marine Geology, 1978Cores obtained by deep sea drilling in the Indian Ocean provide a sedimentary record from which are deduced changing patterns of sedimentation through the Late Mesozoic and Cenozoic. Comparisons between: (1) empirical subsidence curves and sediment sequences at individual sites; and (2) paleobathymetric reconstruction maps and past sediment ...
Robert B. Kidd, Thomas A. Davies
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The Late Jurassic–Early Cretaceous Rifting
2019During the Late Jurassic and Early Cretaceous, Iberia experienced extensional and transtensional stresses leading to a complex rifting time interval. Africa–America–Europe relative motions determined the definition of the Iberian plate boundaries and the generation of rifted sedimentary basins and sub-basins along its continental margins and in the ...
Javier Martín-Chivelet +45 more
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Fusion of caudal vertebrae in Late Jurassic sauropods
Journal of Vertebrate Paleontology, 1991ABSTRACT Fusion of caudal vertebrae in the sauropod dinosaurs Apatosaurus, Diplodocus, and Camarasaurus is explained as the result of ossification of ligaments spanning consecutive centra. The ossification does not involve the intervertebral space or the annulus fibrosus of the disc and therefore represents true bridging.
Bruce M. Rothschild, David S Berman
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Late Jurassic Climates, Vegetation, and Dinosaur Distributions
The Journal of Geology, 2004The Jurassic and Cretaceous are considered to have been warmer than today on the basis of various climate data and model studies. Here, we use the available global record of climate-sensitive sediments, plants, and dinosaurs to infer broadscale geographic patterns for the Late Jurassic.
P. McAllister Rees +3 more
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