Results 181 to 190 of about 8,547 (241)

Evolutionary pathway and genetic mechanisms of fin-to-limb transition in vertebrates. [PDF]

Front Cell Dev Biol
Bayramov AV, Mednikov DN, Zaraisky AG.
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Sedimentary conditions drive modern pyrite burial flux to exceed oxidation. [PDF]

Nat Geosci
Mertens C, Paradis S, Hemingway JD.
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On the Billefjorden fault zone in Garmdalen, central Spitsbergen: implications for the mapping of major fault zones during geological fieldwork and for the tectonic history of Svalbard. [PDF]

Open Res Eur
Koehl JP, Stokmo EMB, Muñoz-Barrera JM.
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Constraints of middle-late Permian granites in Eastern Inner Mongolia on the final subduction of the Paleo Asian Ocean. [PDF]

Sci Rep
Zhao C, Yu Y, Liu Y, Cai H, He J, Gao X.
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Controls of reservoir quality for submarine fan of F4 Formation in the Z oilfield, Illizi Basin, Algeria. [PDF]

Sci Rep
Li C, Li W, Ye HM, Zhu Q, Shan X, Wang H, Wang S, Zhang Z, Zhou X, Xue Z, Ma R.   +10 more
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Silurian to Lower Devonian Communities of Sardinia

, 1999
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FERRETTI, Annalisa, GNOLI, Maurizio, G. B. VAI   +2 more
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A cyanolichen from the Lower Devonian Rhynie chert

American Journal of Botany, 1997
The 400 million‐year‐old Rhynie chert has provided a wealth of information about various types of fungal interactions that existed in this Early Devonian paleoecosystem. In this paper we report the first unequivocal evidence of a lichen symbiosis from the Rhynie chert.
T, Taylor, H, Hass, H, Kerp
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The Lower Devonian Knoydart faunas

Journal of the Linnean Society of London, Zoology, 1967
The presence of Traquairaspis symondsi and Ptertispis (Simopteraspis) whitei in the Knoydart Formation of Arisaig and Pictou Counties, Nova Scotia, has been taken as good evidence of the upper part of the Downtonian and the lower part of the Dittonian stages, respectively. Further discoveries of P.
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The Devonian of Ferques, (Lower Boulonnais)

Quarterly Journal of the Geological Society of London, 1920
Introduction. The Palæozoic rocks of the Boulonnais are classic ground, and received the attention, among others, of De Verneuil, Murchison, Rigaux, and above all Godwin-Austen and Gosselet. Owing to the occurrence of coal, however, most attention has been given to the Carboniferous deposits, and, except for palaeontological work by Rigaux ...
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