Results 191 to 200 of about 27,665 (229)
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Conodonts from near the Middle/Upper Devonian boundary in North Cornwall
1970(Uploaded by Plazi from the Biodiversity Heritage Library) No abstract provided.
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Tabulate corals from the Ilfracombe Beds (Middle-Upper Devonian) of North Devon
1968(Uploaded by Plazi from the Biodiversity Heritage Library) No abstract provided.
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Ameghiniana, 2010
The surveyed microflora was recovered from six cores from the Tonono x-1 well in northwestern Argentina. Most of the studied interval corresponds to the Tonono Formation, i.e., the upper part to the Jollin Member and the basal part of the interval may be related to the Michicola Formation. The microflora totals 73 species represented by trilete spores (
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The surveyed microflora was recovered from six cores from the Tonono x-1 well in northwestern Argentina. Most of the studied interval corresponds to the Tonono Formation, i.e., the upper part to the Jollin Member and the basal part of the interval may be related to the Michicola Formation. The microflora totals 73 species represented by trilete spores (
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Acta Geologica Sinica - English Edition, 2009
Abstract:The Caiziyan Middle and Upper Devonian boundary section is located approximately 30 km northeast of Guilin. It hosts relatively abundant benthic and common‐rare pelagic fossils, including brachiopods, corals, tentaculites, and conodonts, which may serve as a better suitable section for pelagic and neritic stratigraphic correlation.
Hua LI, Xueping MA, Longming WEI
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Abstract:The Caiziyan Middle and Upper Devonian boundary section is located approximately 30 km northeast of Guilin. It hosts relatively abundant benthic and common‐rare pelagic fossils, including brachiopods, corals, tentaculites, and conodonts, which may serve as a better suitable section for pelagic and neritic stratigraphic correlation.
Hua LI, Xueping MA, Longming WEI
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Earth and Environmental Science Transactions of the Royal Society of Edinburgh, 2018
ABSTRACTEach piece of data is valuable for unearthing the earliest history of tetrapod origin. Despite frequently incomplete preservation, each skeletal element provides important information on the morphology, phylogeny and faunistic diversity of early tetrapodomorphs. We describe here new and earlier collected material from the fossil vertebrate site
Lebedev, Oleg, Clément, Gaël
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ABSTRACTEach piece of data is valuable for unearthing the earliest history of tetrapod origin. Despite frequently incomplete preservation, each skeletal element provides important information on the morphology, phylogeny and faunistic diversity of early tetrapodomorphs. We describe here new and earlier collected material from the fossil vertebrate site
Lebedev, Oleg, Clément, Gaël
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Geological Society of America Bulletin, 1973
The discovery of Rensselandia cloudi Frost and Langenheim in the Samaria Limestone Member at the base of the Hyrum Formation in north-central Utah has revived the question of the age of the member and has led to a detailed study of ranges of the various elements of the fauna in the member.
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The discovery of Rensselandia cloudi Frost and Langenheim in the Samaria Limestone Member at the base of the Hyrum Formation in north-central Utah has revived the question of the age of the member and has led to a detailed study of ranges of the various elements of the fauna in the member.
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AAPG Bulletin, 1990
The Snipe Lake BHL 'A' pool reef is one of a number of large Swan Hills atoll reef complexes of Late Devonian age in central Alberta. This study has developed a model for predicting the distribution of reservoir facies in the Snipe Lake A' pool. The reservoir description is an integral component for tailoring an appropriate depletion plan.
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The Snipe Lake BHL 'A' pool reef is one of a number of large Swan Hills atoll reef complexes of Late Devonian age in central Alberta. This study has developed a model for predicting the distribution of reservoir facies in the Snipe Lake A' pool. The reservoir description is an integral component for tailoring an appropriate depletion plan.
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2020
Organic carbon-rich mudstones, or ‘black shales’, record highly anomalous perturbations of local or earth systems at critical times in earth history. Paleoenvironmental parameters, including primary productivity, redox conditions, and sedimentation rate, have been widely recognized as the controls for organic matter (OM) accumulation in shales. However,
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Organic carbon-rich mudstones, or ‘black shales’, record highly anomalous perturbations of local or earth systems at critical times in earth history. Paleoenvironmental parameters, including primary productivity, redox conditions, and sedimentation rate, have been widely recognized as the controls for organic matter (OM) accumulation in shales. However,
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Misener Sandstone (Middle-Upper Devonian), North-Central Oklahoma
AAPG Bulletin, 1972openaire +1 more source
New finds of middle-upper Devonian radiolarians in the Rudnyi Altai region
Doklady Earth Sciences, 2009M. S. Afanas’eva +2 more
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