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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Africa
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North Africa
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Algeria
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Laghouat (1)
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Asia
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Far East
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China
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Guangxi China (1)
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Yunnan China (1)
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Bathurst Island (1)
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Canada
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Eastern Canada
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Quebec
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Gaspe-Est County Quebec
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Gaspe Quebec (1)
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Nunavut
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Western Canada
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Europe
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Czech Republic
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North America
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North American Cordillera
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Canadian Cordillera (1)
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United States
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Eureka County Nevada (1)
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Lander County Nevada (1)
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Nye County Nevada (1)
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Toquima Range (1)
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fossils
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Graptolithina
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Graptoloidea
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Monograptina
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Monograptus
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Monograptus uniformis (1)
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Hemichordata (1)
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Invertebrata
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Brachiopoda (1)
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Cnidaria
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Anthozoa (1)
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microfossils
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Conodonta (1)
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geologic age
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Paleozoic
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Devonian
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Lower Devonian
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Lochkovian (1)
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Pragian (2)
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Silurian
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Middle Silurian (1)
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Upper Silurian (2)
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Primary terms
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Africa
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North Africa
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Algeria
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Laghouat (1)
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Asia
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Far East
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China
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Guangxi China (1)
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Yunnan China (1)
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biogeography (1)
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Canada
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Eastern Canada
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Quebec
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Gaspe-Est County Quebec
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Gaspe Quebec (1)
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Nunavut
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Devon Island (1)
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Ellesmere Island (1)
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Queen Elizabeth Islands
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Devon Island (1)
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Ellesmere Island (1)
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Western Canada
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Canadian Cordillera (1)
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Yukon Territory (1)
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continental shelf (1)
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Europe
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Central Europe
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Czech Republic
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Bohemia (1)
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Graptolithina
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Graptoloidea
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Monograptina
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Monograptus
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Monograptus uniformis (1)
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-
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Hemichordata (1)
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Invertebrata
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Brachiopoda (1)
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Cnidaria
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Anthozoa (1)
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North America
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North American Cordillera
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Canadian Cordillera (1)
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paleontology (1)
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Paleozoic
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Devonian
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Lower Devonian
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Lochkovian (1)
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Pragian (2)
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Silurian
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Middle Silurian (1)
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Upper Silurian (2)
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stratigraphy (5)
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United States
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Nevada
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Eureka County Nevada (1)
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Lander County Nevada (1)
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Nye County Nevada (1)
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Toquima Range (1)
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Monograptus aequabilis
Quelques graptolites du Silurien superieur du Sahara septentrional
Early Devonian graptolites and graptolite biostratigraphy, Arctic Islands, Canada
Early Devonian graptolites from the Qinzhou–Yulin region, southeast Guangxi, China
Graptolites from the Laforce and St. Léon Formations, Northern Gaspé, Quebec
Upper Silurian and Lower Devonian graptolites and graptolite biostratigraphy, northern Yukon, Canada
Early Devonian graptolites from southwest Yunnan, China
Comments on Graptolites
Silurian and Basal Devonian Stratigraphy of Northeastern Gaspé Peninsula, Québec
(A) “ Monograptus ” microdon curvatus Lenz and Kozłowska-Dawidziuk, 2004 ...
The latest encrinurid trilobites from the Lower Devonian of Xinjiang, Northwest China
THE SILURIAN-DEVONIAN BOUNDARY IN THE BARRANDIAN
Early Devonian Conodont-Graptolite Collation and Correlations with Brachiopod and Coral Zones, Central Nevada
Comments on Graptolites: REPLY
The Pristiograptus dubius (Suess, 1851) species group and iterative evolution in the Mid- and Late Silurian
Abstract Devonian rocks are exposed in every region of Thailand, commonly occurring in thick sequences of Lower to Upper Palaeozoic sedimentary and volcanic rocks (Fig. 4.1 ). However, a scarcity of marker fossils and generally discontinuous exposures have meant that Devonian rocks are frequently not distinguishable from older and younger rocks. In such cases, the Department of Mineral Resources (the DMR) have inferred Devonian rocks to be present and have mapped them as Silurian-Devonian, Silurian-Carboniferous, or Devonian-Carboniferous ( DMR 1999 ).
Brachiopod faunas, facies and biostratigraphy of the Pridolian to lower Eifelian succession in the Rhenish Massif (Rheinisches Schiefergebirge, Germany)
Abstract The succession of Pridolian to lower Eifelian (uppermost Silurian to lowermost Middle Devonian) rhynchonelliformean brachiopod faunas from the Rhenish Massif (Germany) is described and interpreted against the background of sedimentary sequences and facies development. The predominant rhenotypic (‘Rhenish’) facies is redefined as a neritic-siliciclastic facies type of the Devonian. It is subdivided into eurhenotypic, pararhenotypic and allorhenotypic subfacies, based on sedimentary features and specific brachiopod assemblages reflecting different shallow-marine palaeoenvironments under more or less terrigenous influence. The studied sedimentary successions are subdivided biostratigraphically on the basis of brachiopods, correlated on a supraregional scale, and calibrated in terms of the global chronostratigraphy. Stratigraphic intervals with characteristic brachiopod faunas are distinguished. Faunal turnovers between these are attributed to regional events in the context of short or more extended phases of palaeoenvironmental change presumably caused mainly by sea-level fluctuations in combination with varying crustal subsidence and sedimentation rates. These changes resulted in shelf-wide or more regional extinction or emigration of substantial parts of a brachiopod fauna and subsequent replacement by a largely new one. Finally, new taxa of brachiopods are introduced: Sartenaerirhynchus gen. nov., Paraspirifer ( Mosellospirifer ) subgen. nov., Paraspirifer ( Laurentispirifer ) subgen. nov., Iridistrophia ( Flabellistrophia ) subgen. nov. and Iridistrophia ( Flabellistrophia ) musculosa sp. nov.