The Jurassic of North-East Greenland: Maximum Middle Jurassic transgression in East Greenland: evidence from new ammonite finds, Bjørnedal, Traill Ø [PDF]
Geological Survey of Denmark and Greenland Bulletin, 2004 A Middle – lower Upper Jurassic sandstone-dominated succession, more than 550 m thick, with mudstone intercalations in the middle part is exposed in Bjørnedal on Traill Ø, North-East Greenland.
Alsen, Peter, Surlyk, Finn
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Carnets de Géologie, 2008 Since the end of the 19th century the interval comprising the uppermost Upper Albian, the Cenomamian, the Turonian and the basal Coniacian has been subdivided, first into ammonite zones, then, beginning in the middle of the 20th century, into zones of ...
Amédro Francis, Robaszynski Francis
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The Jurassic of North-East Greenland: Jurassic dinoflagellate cyst stratigraphy of Hold with Hope, North-East Greenland [PDF]
Geological Survey of Denmark and Greenland Bulletin, 2004 Dinoflagellate cysts of the Middle–Upper Jurassic succession on northern Hold with Hope have been studied in order to establish a biostratigraphic framework and to date the succession.
Piasecki, Stefan +3 more
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The physical basis of mollusk shell chiral coiling. [PDF]
Proc Natl Acad Sci U S A, 2021 Chirat R, Goriely A, Moulton DE.
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The stratigraphical significance of Cymaceras guembeli for the boundary between Platynota Zone and Hypselocyclum Zone, and the correlation between Swabian and Franconian Alb. [PDF]
, 2004 Schick, Herbert W.
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Geo Fossils-I: A synthetic dataset of 2D fossil images for computer vision applications on geology. [PDF]
Data Brief, 2023 Nathanail A.
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A calibrated composite section for the Late Jurassic Reuchenette Formation in northwestern Switzerland (?Oxfordian, Kimmeridgian sensu gallico , Ajoie-Region) [PDF]
, 2018 .: A new stratigraphical frame for Kimmeridgian sediments of northwestern Switzerland has been established by correlating seventeen closely spaced sections by means of lithological, sedimentological, and microfacial data as well as by ammonites.
Jank, Markus +2 more
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