Late Triassic

Results: 47



#Item
21Crurotarsans / Chinle Formation / Saurischians / Petrified Forest National Park / Revueltosaurus / Aetosaur / Coelophysis / Phytosaur / Triassic / Herpetology / Mesozoic / Triassic dinosaurs

NEW DISCOVERIES OF LATE TRIASSIC DINOSAURS FROM PETRIFIED FOREST NATIONAL PARK, ARIZONA ADRIAN P. HUNT AND JEREMIAH WRIGHT Mesalands Dinosaur Museum, Mesa Technical College, 911 South Tenth Street, Tucumcari, NM 88401

Add to Reading List

Source URL: www.nature.nps.gov

Language: English - Date: 2001-06-06 17:31:34
22REVIEW doi:[removed]nature09678 Has the Earth’s sixth mass extinction already arrived?

REVIEW doi:[removed]nature09678 Has the Earth’s sixth mass extinction already arrived?

Add to Reading List

Source URL: ib.berkeley.edu

Language: English - Date: 2011-03-02 23:54:03
23Proc. R. Soc. B[removed], 507–513 doi:[removed]rspb[removed]Published online 7 October 2008 A thin-shelled reptile from the Late Triassic of North America and the origin of the turtle shell

Proc. R. Soc. B[removed], 507–513 doi:[removed]rspb[removed]Published online 7 October 2008 A thin-shelled reptile from the Late Triassic of North America and the origin of the turtle shell

Add to Reading List

Source URL: www.nmnaturalhistory.org

Language: English - Date: 2014-06-06 05:23:16
24A RT I C L E S Methane Release from Igneous Intrusion of Coal during Late Permian Extinction Events Gregory J. Retallack and A. Hope Jahren1 Department of Geological Sciences, University of Oregon, Eugene, Oregon[removed]

A RT I C L E S Methane Release from Igneous Intrusion of Coal during Late Permian Extinction Events Gregory J. Retallack and A. Hope Jahren1 Department of Geological Sciences, University of Oregon, Eugene, Oregon[removed]

Add to Reading List

Source URL: jahrenlab.com

Language: English - Date: 2012-08-21 20:45:07
25Middle-Late Permian mass extinction on land Gregory J. Retallack† Christine A. Metzger Department of Geological Sciences, University of Oregon, Eugene, Oregon[removed], USA Tara Greaver

Middle-Late Permian mass extinction on land Gregory J. Retallack† Christine A. Metzger Department of Geological Sciences, University of Oregon, Eugene, Oregon[removed], USA Tara Greaver

Add to Reading List

Source URL: jahrenlab.com

Language: English - Date: 2012-08-21 20:54:57
26MARTIN FORMATION LATE DEVONIAN (Frasnian) 374 to 367 Million Years Ago LITHOLOGY:

MARTIN FORMATION LATE DEVONIAN (Frasnian) 374 to 367 Million Years Ago LITHOLOGY:

Add to Reading List

Source URL: www.westcarb.org

Language: English - Date: 2011-04-26 14:54:05
27(Fundy Gp., Argo & Eurydice Fms.) OR P HE US G R AB E N Figure 5: Simplified paleogeographic reconstruction of the Scotian Basin during the Late Triassic (Rhaetian) ca. 210 mya. Salt deposition likely was

(Fundy Gp., Argo & Eurydice Fms.) OR P HE US G R AB E N Figure 5: Simplified paleogeographic reconstruction of the Scotian Basin during the Late Triassic (Rhaetian) ca. 210 mya. Salt deposition likely was

Add to Reading List

Source URL: www.callforbids.cnsopb.ns.ca

- Date: 2012-07-27 11:49:39
    28(Fundy Gp., Argo & Eurydice Fms.) OR P HE US G R AB E N Figure 5: Simplified paleogeographic reconstruction of the Scotian Basin during the Late Triassic (Rhaetian) ca. 210 mya. Salt deposition likely was

    (Fundy Gp., Argo & Eurydice Fms.) OR P HE US G R AB E N Figure 5: Simplified paleogeographic reconstruction of the Scotian Basin during the Late Triassic (Rhaetian) ca. 210 mya. Salt deposition likely was

    Add to Reading List

    Source URL: www.callforbids.cnsopb.ns.ca

    - Date: 2012-07-27 11:44:55
      29(Fundy Gp., Argo & Eurydice Fms.) OR P HE US G R AB E N Figure 5: Simplified paleogeographic reconstruction of the Scotian Basin during the Late Triassic (Rhaetian) ca. 210 mya. Salt deposition likely was

      (Fundy Gp., Argo & Eurydice Fms.) OR P HE US G R AB E N Figure 5: Simplified paleogeographic reconstruction of the Scotian Basin during the Late Triassic (Rhaetian) ca. 210 mya. Salt deposition likely was

      Add to Reading List

      Source URL: www.callforbids.cnsopb.ns.ca

      - Date: 2012-07-27 11:41:00
        30THE SOIL IS ALIVE! LOSS OF BIODIVERSITY NATURAL RATE OF EXTINCTION If the Earth was in equilibrium, the natural extinction rate (i.e. normal evolution) would be around 1 species for every million species per year. This

        THE SOIL IS ALIVE! LOSS OF BIODIVERSITY NATURAL RATE OF EXTINCTION If the Earth was in equilibrium, the natural extinction rate (i.e. normal evolution) would be around 1 species for every million species per year. This

        Add to Reading List

        Source URL: eusoils.jrc.ec.europa.eu

        Language: English - Date: 2008-06-12 09:07:05