1. Triassic and Jurassic together have an accumulated sediment thickness of 1,000–1,700 m.

2. The Asylum Transplants You to Triassic World and More Mockbuster Madness

3. Triassic phylloid algae have recently been discovered in a reef in the southern Yukon.

4. The bedrock underlying Birmingham was mostly laid down during the Permian and Triassic periods.

5. The palaeogeographical evolution sensitively responds to the tectonism in the whole Triassic.

6. The Triassic of Cyprus represents a time of epirogenetic movements with occasional volcanic activity.

7. Therocephalians included both carnivorous and herbivorous forms; both died out after the Early Triassic.

8. 19 By the beginning of the Upper Triassic, rhynchosaurs were still the dominant herbivores.

9. Together with the subsequent vulcanism of the Upper Permian and Lower Triassic occurred lead-zinc-barite deposits.

10. The earliest Calcareous nannofossils are found from the late Triassic period (around 225 million years ago)

11. The lungfish's greatest diversity was in the Triassic period; today there are fewer than a dozen genera left.

12. In South China this mixed fauna is associated withOtoceras woodwardi, the index ammonite of the Lowermost Triassic.

13. The true "Age of Dinosaurs" is during the following Jurassic and Cretaceous periods, rather than the Triassic.

14. Soil type consisting of marl and limestone common in Alsace dating back from the Upper Triassic period.

15. Associated evolution of bipedality and Cursoriality among Triassic archosaurs: a phylogenetically controlled evaluation Tai Kubo and Mugino O

16. Foraminifera (the same species as in the Alpine Upper Triassic; in additionFoliotortus PILLER & SENOWBARI-DARYAN and amphora-like tests (Cucurbita, Amphorella etc., until now only known from the Upper Triassic of the Western Carpathians and from the Hohe Wand near Vienna, Austria); 7.

17. Crinoids recovered during the Triassic and re-occupied almost all ecological niches they had held in Palaeozoic times

18. Fluorite-mineralizations in fissures of the Gutenstein Strata (Anis—Mid-Triassic) are located in tectonic zones, near evaporites.

19. During the Carnian (early part of the Late Triassic), some advanced cynodonts gave rise to the first mammals.

20. The goal of the project ET MICROBIALITES (Formation mechanisms of Early Triassic microbialites in the aftermath of the greatest mass extinction at the Permian-Triassic-Boundary) was to understand microbialite formation in periods of Earth’s history typified by changing environments and ecosystems.

21. Amphibolite from an abyssal sea floor or marginal basin environment of either Permian or Triassic age originally was low-potassium basalt.

22. Belemnites are an extinct cephalopod that existed between the late Triassic and Late Cretaceous, related to modern cuttlefish and squid

23. The southern edge of the dome is overlain by sandstones of Triassic age though they barely impinge on the National Park.

24. The Belemnites are a diverse order of widespread cephalopod mollusks from the Late Triassic-Late Cretaceous of the entire world

25. There exists an extended set of early Triassic intermediate-acid volcanics closely related to microdot gold ore in Southwestern Guangxi.

26. Angularia: genus: belongs to Neotaenioglossa: second hand: Sepkoski, 2002: Angularia: genus: belongs to Purpurinidae: stated with evidence: Nützel and Erwin, 2004: Status (PBDB) extinct: Taxon Size (PBDB) 5: First Recorded Appearance: 235 - 232 Ma Late Triassic: Last Recorded Appearance: 212 - 206 Ma Late Triassic:

27. Soil type consisting of various compositions of sandstone, marl, dolomite, and shingle common in Alsace dating back from the Middle Triassic period.

28. The deposit is explained as a kind of an ancient superficial pavement formed under arid climatic conditions of the Lower Triassic.

29. Belemnite [ bĕl ′əm-nīt′ ] Any of various extinct cephalopod mollusks of the order Belemnoidea that lived from the Triassic into the Tertiary Period

30. The first Mesozoic record of the extinct Apterygote insect genus Dasyleptus (Insecta: Archaeognatha: Monura: Dasyleptidae) from the Triassic of Monte San Giorgio (Switzerland)

31. Another family of prehistoric reptile, called the Archosaurs, coexisted with the therapsids (as well as the other land reptiles that survived the Permian/Triassic extinction).

32. Near Sydney, Australia, unconsolidated aeolian and alluvial sediments of Quaternary age form the Botany Sands aquifer and lie unconformably on Triassic-age sandstone (Narrabeen Group).

33. Fossil Ensifera are found from the late Carboniferous period (300 Mya) onwards, and the true crickets, Gryllidae, from the Triassic period (250 to 200 Mya).

34. Archosaurs ([Greek for 'ruling lizards') are a group of diapsid reptiles that first evolved from Archosauriform ancestors during the Olenekian (Lower Triassic Period).They are represented today by birds and crocodiles.Archosaurs are set apart by having socketed teeth (a feature that inspired the traditional name, 'thecodonts', for the Triassic forms) and four-chambered hearts, among other

35. (also Conodont animal) A fossil marine animal of the Cambrian to Triassic periods, having a long wormlike body, numerous small teeth, and a pair of eyes

36. The jaw apparati of Paleozoic and Triassic ammonoids are simìlar in shape to parrots’ beaks; they possess sharp cutting-edges and consist of chitinous material.

37. Any of various small marine chordates of the group Conodonta of the Paleozoic Era and the Triassic Period, preserved primarily in the form of their conelike teeth

38. Both of these reproduced by spores rather than seeds and are considered to be links between ferns and the gymnosperms which evolved in the Triassic period.

39. Triassic corresponds to an extraordinary transgression in the sense of a new onlap of the sedimentary realm, a reconquest of ancient areas by new deposits, however their facies may be.

40. 11 Based on the Middle-Late Paleozoic pillow lava and Permian-Triassic tectonic melange, this paper shows that there is a melange zone along Qinzhou-Cenxi-Luoding-Yunfu.

41. Any of various small marine chordates of the group Conodonta of the Paleozoic Era and the Triassic Period, preserved primarily in the form of their conelike teeth

42. This study aims to reveal the mineralogical characteristics of the carbonate and pelitic rocks in the Lower Triassic Cigli Group in the Uludere-Uzungecit (Sirnak) region from Southeast Anatolian Autochthone (SEAA).

43. Conodont biostratigraphy across the Permian–Triassic boundary at the Dawen section, Great Bank of Guizhou, Guizhou Province, South China: implications for the Late Permian extinction and correlation with Meishan

44. New finds of fossils including bivalves, ammonoids, brachiopods and palynomorphs from the Middle Triassic Reifling Formation significantly improve the age assignment for this unit in Liechtenstein and Vorarlberg.

45. The scientists speculate that this impact may have caused the Permian–Triassic extinction event, although its age is bracketed only between 100 million and 500 million years ago.

46. In a first period of exploration, until the beginning of our century, the Mediterranean or Alpine Triassic advanced to be a standard type of the marine development of that period.

47. Archosaurs have a nearly 250 million year record that originated shortly after the Permian-Triassic extinction event and is continued today by two extant clades, the crocodylians and the avians

48. Conodonts occur in sediments from the CAMBRIAN to the TRIASSIC and are thought to be associated with the mouth-parts of primitive chordates such as members of the AGNATHA.

49. Conodonts occur in sediments from the CAMBRIAN to the TRIASSIC and are thought to be associated with the mouth-parts of primitive chordates such as members of the AGNATHA

50. Kō'nə-dŏnt', kŏn'ə- Any of various small marine chordates of the group Conodonta of the Paleozoic Era and the Triassic Period, preserved primarily in the form of their conelike teeth.

51. These rocks were formed offshore in island arcs and adjacent basins (Vallier, 1967, 1977; Brooks, 1979) and were Accreted to the North American continent between Late-Triassic and mid-Cretaceous time

52. Living Archosaurs comprise birds (dinosaurs), and their sister group, the crocodilians. Archosaurs appeared in fossil record sometime in the Triassic and are thought to have evolved ears sensitive to airborne sound sometime later.

53. Authigenous quartz, muscovite and orthoclase were singled out from Triassic carbonate rocks that had been subjected to alteration in the surrounding fault breccia of Mangishlac (MLJRAVYOV, The origin of each of these minerals was 1964)

54. Geocoma and Sinosura share small adpressed arm spines with Aplocoma d’Orbigny 1852. Aplocoma is represented by a number of Triassic and Jurassic species, and the subfamily Aplocominae is proposed herein for the three genera.

55. Archosaurs (“ruling reptiles”) are members of a subclass that also includes the dinosaurs, the pterosaurs (flying reptiles), and several groups of extinct forms, mostly from the Triassic Period (251 million to 200 million years ago)

56. Synonyms: Allosaur; Allosaurus Hypernyms ("Allosaur" is a kind of): bird-footed dinosaur; theropod; theropod dinosaur (any of numerous carnivorous dinosaurs of the Triassic to Cretaceous with short forelimbs that walked or ran on strong hind legs)

57. Post-triassic, during phase III, occured a dislocation metamorphism, and a local crystallization of sericite, albite, biotite, and microcline at the lower boundary of the greenschist-facies under low pressure (Abukuma-type). Phase IV was a jolting in west-east-direktion without recrystallization.

58. Allosaur - late Jurassic carnivorous dinosaur; similar to but somewhat smaller than tyrannosaurus Allosaurus bird-footed dinosaur , theropod , theropod dinosaur - any of numerous carnivorous dinosaurs of the Triassic to Cretaceous with short forelimbs that walked or ran on strong hind legs

59. The Junggar, Turfan and Alakol basins in northwestern China and Kazakhstan formed as Late Permian to ?Early Triassic extensional structures in a broad sinistral shear zone between large strike-slip faults that separate two main domains of the Altaid orogenic collage

60. Spondylosoma absconditum (Ladinian, Middle Triassic) lacks certain Dinosauriformes-Dinosauria characters (sigmoid curve and epipophyses in neck, distally placed deltopectoral crest on humerus) and those present (accessary hyposphene-hypantra vertebral articulations, three sacral vertebrae, elongate pubis) also occur in the Rauisuchia (Crurotarsi, Suchia, Rauisuchiformes).

61. The first ichthyosaurs from the upper Lower Triassic (Spathian) already show a suite of unique characters (very large eyes, elongate snout, deeply amphicoelous vertebrae, limb modified to fins) correlated with a fully aquatic existence and probably were unable to leave the water.

62. The oldest known freshwater Bivalves are from the Devonian, but the major non-marine radiation occurred in the Triassic with the appearance of the Unionoida, which today includes more than 960 species, and is one of the most endangered animal groups on …

63. Now, luckily, this Thrinaxodon, the size of a robin egg here: this is a skull I've discovered just before taking this picture -- there's a pen for scale; it's really tiny -- this is in the Lower Triassic, after the mass extinction has finished.

64. Using cluster and principal coordinates analyses, G. mordax was found to have closest phenetic affinities with Platypterygius americanus (Nace) of the North American Cretaceous, and with an undescribed ichthyosaur from the Middle Triassic of Switzerland, and least phenetic affinity with Ophthalmosaurus discus (Marsh).

65. Stretching for around 14 miles (23 km) between Cardiff and Porthcawl, the remarkable layers of these cliffs, situated on the Bristol Channel are a rhythmic decimetre scale repetition of limestone and mudstone formed as a late Triassic desert was inundated by the sea.

66. The fossil record of Anurans contains taxa having a tail with a few caudal vertebrae, which is the plesiomorphic state [e.g., Triassic Triadobatrachus massinoti and Czatkobatrachus polonicus ], followed by the sudden appearance of forms with a urostyle and no tail (Prosalirus bitis) (5, 6)

67. This took the form of a giant "Pac-Man" with an east-facing "mouth" constituting the Tethys sea, a vast gulf that opened farther westward in the mid-Triassic, at the expense of the shrinking Paleo-Tethys Ocean, an ocean that existed during the Paleozoic.

68. — Cardiids or marine cockles are one of the best known families of marine bivalves in the world, with a long history of study and collection given their large and accessible shells, a tractable level of biodiversity globally (~290 species) and a solid fossil record extending to the late Triassic.

69. The Upper Carnian-Lower Norian (Upper Triassic) Luning Formation at Berlin-Ichthyosaur State Park (BISP) in central NV (USA) has been sampled using for the first time the bed-by-bed approach for ammonoids, pelagic bivalves, and conodonts, more than 60 years after its first description by Silberling (U.S.

70. ABSTRACT – Cardiids or marine cockles are one of the best known families of marine bivalves in the world, with a long history of study and collection given their large and accessible shells, a tractable level of biodiversity globally (~290 species) and a solid fossil record extending to the late Triassic.

71. The results suggest that the creation of a low and continuous (but stable) recharge from the Triassic Limestone and Panjal Trap aquifers, due to blockage of groundwater flow between strata with contrasting hydraulic conductivity, attenuates the discharge and gives rise to small fluctuations in the alluvium- and Karewa-controlled springs.

72. Analyses of 42 Cretaceous rock samples from Deep Sea Drilling Project (DSDP) L Leg 32, in the northern Pacific, show that chert and porcellanite are enriched in Fe, Mn, P, Cu, Ba, Mo, Ni and Pb relative to both Triassic biogenic Cherts of central Japan and Cretaceous DSDP Cherts of Leg 62

73. Smok (meaning "dragon" in Polish) is an extinct genus of large carnivorous Archosaur.It lived during the latest Triassic period (latest Norian to early Rhaetian stage, between 205–200 Ma).Its remains have been found in Lisowice, southern Poland.The type species is Smok wawelski (after the Wawel Dragon) and was named in 2012.It is larger than any other known predatory Archosaur from the Late