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sedimentary rocks
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sedimentary rocks
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Landeyran Formation
EARLY ORDOVICIAN AGNOSTOID TRILOBITES FROM THE SOUTHERN MONTAGNE NOIRE, FRANCE
Figure 6 —Mitrocystitidan mitrates. 1–2, Ovocarpus moncereti, Landeyran ...
Figure 4 —Plating diagrams of lower surfaces of Ovocarpus moncereti , Lan...
Sedimentary facies and trilobite and conodont faunas of the Ordovician Rann Formation, Ras Al Khaimah, United Arab Emirates
Figure 3 —Plate homology in primitive mitrates (not to scale). 1, Lobocar...
The Upper Ordovician Trinucleid Trilobite Bancroftolithus from the Precordillera of Argentina
New rhenopyrgid edrioasteroids (Echinodermata) and their implications for taxonomy, functional morphology, and paleoecology
Early Ordovician trilobites from the Iruya area (Cordillera Oriental, northwestern Argentina) and their stratigraphic significance
A NEW MITRATE (ECHINODERMATA, STYLOPHORA) FROM THE TREMADOC OF SHROPSHIRE (ENGLAND) AND THE ORIGIN OF THE MITROCYSTITIDA
MORPHOLOGICAL AND PALEOECOLGICAL ANALYSIS OF THE ORDOVICIAN ANKYROID LAGYNOCYSTIS (STYLOPHORA: ECHINODERMATA)
LATEST CAMBRIAN CORNUTES (ECHINODERMATA: STYLOPHORA) FROM THE TAEBAEKSAN BASIN, KOREA
A critical graptolite correlation into the Lower Ordovician of Gondwana
NEW AND REVISED OCCURRENCES OF ORDOVICIAN CRINOIDS FROM SOUTHWESTERN EUROPE
A synopsis of Ordovician trilobite distribution and diversity
Abstract Ordovician trilobites are reviewed based on a new species-level relational database. The stratigraphical ranges of all 56 families with occurrences in the Ordovician are documented and the content, phylogenetic status, diversity and Ordovician distribution by major palaeocontinent/terrane are discussed. Aspects of higher classification are also dealt with. Global sampling is heavily biased towards a small number of highly sampled areas. Much of the world has a very limited record of formally named trilobite species. Even within heavily sampled units, sampling is patchy by environment and time. Genus endemism was at a peak in Laurentia, Baltic, and Avalonia in the Floian and declined more-or-less steadily through the remainder of the Ordovician.