Results 151 to 160 of about 1,858 (206)
Marine microfossils: Tiny archives of ocean changes through deep time. [PDF]
Sremac J +4 more
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The Cabrières Biota (France) provides insights into Ordovician polar ecosystems. [PDF]
Saleh F +20 more
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Influence of quartz types on mechanical parameters in the early silurian Longmaxi shale, Sichuan Basin. [PDF]
Zhang Q +9 more
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The rise of lichens during the colonization of terrestrial environments. [PDF]
Becker-Kerber B +31 more
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Graptolites in British Stratigraphy [PDF]
Abstract697 taxa of planktonic graptolites are recorded, and their stratigraphical ranges are given, through 60 biozones and subzones in the Ordovician and Silurian strata of England, Wales and Scotland, in the first such stratigraphical compilation for Great Britain since the synthesis of Elles & Wood (1901–1918).
Mark Williams, D K Loydell, R B Rickards
exaly +5 more sources
The Wufeng–Longmaxi Formations (Ordovician-Silurian) contain abundant graptolite-bearing shales, which have proven to be one of the most successful shale gas exploration targets in China and can provide an opportunity to study the organic petrology of ...
Qingyong Luo +2 more
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The Use of Computational Fluid Dynamics in Reconstructing the Hydrodynamic Properties of Graptolites
Graptolites are some of the most commonly preserved Silurian planktonic organisms. The interpretation of graptolite functional morphology is rendered problematic by their lack of close modern analogues or homologues. Physical modelling of graptolites has
Gavin Tabor, Susan Rigby
exaly +2 more sources
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Graptolite ontogeny and the size of the graptolite zooid
Geological Magazine, 1995AbstractTwo methods of estimating the size of the graptolite zooid are described and discussed. It is possible to size a zooid by reference to cortical bandages or with reference to modem Rhabdopleura and its tubes. These two methods give very different results, with the first suggesting small zooids relative to thecal size and the second suggesting ...
Susan Rigby, Margaret Sudbury
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Geological Society, London, Special Publications, 1979
Summary Graptoloids became extinct in latest Early Devonian (Pragian) times, and dendroids in the late Carboniferous. There is insufficient information for the other six graptolite orders to suggest when they might have become extinct, so that in these cases it is impossible as yet to speculate how extinction occurred.
T. N. Koren’, R. B. Rickards
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Summary Graptoloids became extinct in latest Early Devonian (Pragian) times, and dendroids in the late Carboniferous. There is insufficient information for the other six graptolite orders to suggest when they might have become extinct, so that in these cases it is impossible as yet to speculate how extinction occurred.
T. N. Koren’, R. B. Rickards
openaire +1 more source

