Results 231 to 240 of about 45,582 (298)
Insights on the enigmatic millipede order Siphoniulida (Myriapoda, Diplopoda): a new species bearing ozopores and its phylogenetic implications. [PDF]
Recuero E, López-Estrada EK, Harden CW.
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Impact of Paleoclimatic Variability on Shale Oil Enrichment in Deep to Semi-Deep Lacustrine Facies: A Case Study of the Second Member of the Funing Formation, Qintong Depression, Subei Basin, Eastern China. [PDF]
Tang S +9 more
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A Reassessment of the Coprostane Biomarker in the Ediacaran With Implications for Dickinsonia. [PDF]
Mulligan C, Gold DA.
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Discovery of fossil avian footprints from Late Holocene sediments of Allahbund uplift in Great Rann of Kachchh of Western India. [PDF]
Padia D, Desai B, Chauhan S, Vaghela B.
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The olfactory bulb endocast as a proxy for mammalian olfaction. [PDF]
Martinez Q +14 more
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Short Courses in Paleontology, 1992
The study of fossil footprints began soon after the birth of vertebrate paleontology. The Reverend Henry Duncan started a study of footprints from the New Red Sandstone (Permian) of Scotland in 1824 (Sarjeant, 1987). Even earlier reports of footprints are known, but the fossils were not studied until later (Sarjeant, 1975).
Mark F. Schult, James O. Farlow
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The study of fossil footprints began soon after the birth of vertebrate paleontology. The Reverend Henry Duncan started a study of footprints from the New Red Sandstone (Permian) of Scotland in 1824 (Sarjeant, 1987). Even earlier reports of footprints are known, but the fossils were not studied until later (Sarjeant, 1975).
Mark F. Schult, James O. Farlow
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Geological Magazine, 1997
A different approach to the naming of trace fossils is advocated. The primary ichnotaxobase should be the form of the burrow actually occupied, and the secondary ichnotaxobase should be the morphology of the structure that reflects the manner in which this burrow has been displaced and/or extended.
R. GOLDRING, J. E. POLLARD, A. M. TAYLOR
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A different approach to the naming of trace fossils is advocated. The primary ichnotaxobase should be the form of the burrow actually occupied, and the secondary ichnotaxobase should be the morphology of the structure that reflects the manner in which this burrow has been displaced and/or extended.
R. GOLDRING, J. E. POLLARD, A. M. TAYLOR
openaire +1 more source

