Results 41 to 50 of about 3,102 (219)
Geophysical Research Letters, Volume 53, Issue 10, 28 May 2026.Abstract An investigation of the relationships among large igneous province (LIP), carbon cycling, and climate change is central to understanding Earth system. During Glacial III, the most intense phase of Late Paleozoic Ice Age, the influence of coeval LIP on the carbon cycle and climate remains debated.
Yuzhu Ge +5 more
wiley +1 more source
Conodonts in Ordovician biostratigraphy
, 2017 The long time interval after Pander's (1856) original conodont study can in terms of Ordovician conodont biostratigraphical research be subdivided into three periods, namely the Pioneer Period (1856-1955), the Transition Period (1955-1971) and the Modern
FERRETTI, Annalisa +3 more
core +1 more source
Литосфера, 2015 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)
Литосфера, 2019 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
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The Depositional Record, Volume 12, Issue 2, April 2026.We studied the Permian–Triassic successions of south‐western Türkiye at five locations, synthesised sedimentological and palaeontological data, putting it into a consistent stratigraphic framework and incorporating 3D digital outcrop models. Abstract The Permian–Triassic transition is characterised by major environmental changes and the largest known ...
Baran Karapunar +12 more
wiley +1 more source
Scottish carboniferous conodonts [PDF]
, 1953 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.
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Geochemistry, Geophysics, Geosystems, Volume 27, Issue 4, April 2026.Abstract Mafic continental large igneous provinces (LIPs) erupted rapidly and may have overwhelmed Earth's atmospheric and biospheric systems. However, the exact balance and interplay between short‐term climate warming caused by CO2 emissions and long‐term cooling due to LIP weathering remains poorly understood.
Kunyue Ling +5 more
wiley +1 more source
Conodonts from the Davidsville Group, northeastern Newfoundland
, 1980 Conodonts from the basal part of the Davidsville Group, Botwood Zone of Newfoundland, are assigned a late Llanvirn to early Llandeilo age. Other fossil groups suggest a time range of Llanvirn to early Caradoc, and the conodonts are in accordance with ...
Svend Stouge
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Tectonics, Volume 45, Issue 4, April 2026.Abstract Our understanding of subduction initiation remains limited by the difficulty of making direct observations of geologically recent examples. In the geologic record, supra‐subduction zone ophiolites are often interpreted to record syn‐initiation slab rollback and upper plate extension. Unfortunately, many ophiolites are decoupled from records of
B. M. Keough +3 more
wiley +1 more source
Early Triassic conodonts in Western Tethys
, 2023 Conodonts are phosphatic, tooth-like elements of extinct jawless vertebrates that are classified in the independent class Conodonta. Due to their rapid evolution, wide palaeogeographic distribution and high resistance, conodonts are one of the most ...
Kolar-Jurkovšek, Tea
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