Results 51 to 60 of about 4,379 (215)
Abstract Lepidodendron aculeatum is an arborescent lycopod that populated the vast coal swamps in north‐western and central Europe during the late Carboniferous (Pennsylvanian) from the Bashkirian onwards, dominating the lush vegetation of tropical wetlands.
Christian Pott, Lothar Schöllmann
wiley +1 more source
Devonian conodonts from Jones Island, northwest Washington
Two small outcrops of limestone on Jones Island, northwest Washington, have yielded Devonian conodonts. Conodonts from locality 1, on the northern shore of the island, include Icriodus cf. I. brevis Stauffer, Icriodus cf. I.
Norman M. Savage
core +1 more source
Abstract The mechanisms by which new subduction zones form remain highly debated. Here we use Permo‐Triassic strata to evaluate potential mechanisms for initiation of the Talkeetna‐Bonanza Arc of the northern North American Cordillera. New mapping and analysis of Permian and Upper Triassic strata on the Alaska Peninsula suggest a period of uplift ...
Brandon M. Keough +2 more
wiley +1 more source
The Bol’shaya Barma, Akkyr, Ryauzyak and Kuk-Karauk sections in the western slope of the South Urals are considered to be perspective sections for the identification of Famennian Regional Boundary Stratotype Point (RBSP).
R. Ch. Tagarieva, A. G. Mizens
doaj +2 more sources
Dynamics of the conodont diversity in the Late Devonian–Early Carboniferous (Famennian–Serpukhovian)
Subject. The article is aimed to evaluate of the conodont diversity dynamics at the species level in the Famennian – Serpukhovian interval.Materials and methods.
A. V. Zhuravlev
doaj +1 more source
Abstract Heterostracans are pivotal in examining the evolution of feeding and the head in jawed vertebrates as the stem‐gnathostomes in which the oral apparatus is more commonly preserved. However, most analyses of their feeding, especially recent studies using modern 3D imaging methods, have focused on a specific subgroup, the Pteraspidiformes ...
Lisa Schnetz +9 more
wiley +1 more source
Conodonts in Biostratigraphy. A 300-million-years long journey through geologic time [PDF]
Conodonts are tooth -like elements of a primitive chordate and are generally abundant in many marine sedimentary rocks deposited from the late Cambrian to the latest Triassic.
Carlo Corradini +11 more
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Abstract Archosauriforms were the most successful reptiles of the Mesozoic, becoming widespread and diverse during the Triassic. Yet, little is known of their origin, although it seems clear that it was before the end‐Permian mass extinction. An additional source of information comes from the early archosauriform footprint record.
Lorenzo Marchetti, Hendrik Klein
wiley +1 more source
Scottish carboniferous conodonts [PDF]
1. Conodonts are rare in the Scottish Carboniferous Limestone but are slightly more abundant in the lower Dart of the Scottish Millstone Grit.2. Seventeen genera and 53 species (including one new genus, Dalryella, and 21 new species) of conodonts are
Clarke, William J.
core
Mississippian Conodonts in Iowa [PDF]
The literature on Mississippian conodonts in Iowa is reviewed. Conodont occurrences are noted from the McCraney, Prospect Hill, Hampton, Gilmore City, Burlington, Keokuk, War-saw, Spergen, St. Louis and Ste. Genevieve formations.
Anderson, W. I.
core +1 more source

