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870 results for “Ordovician”

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zenodo36/100

Fig. 1 in Sexual dimorphism and pore systems in Ordovician ostracodes

Fig. 1. Morphological terminology explained in Swantina pseudobliqua.

opencc-by-4.0Jun 2010View details →
zenodo36/100

Fig. 4 in A spinose appendage fragment of a problematic arthropod from the Early Ordovician of Morocco

Fig. 4. Reconstruction of Pseudoangustidontus duplospineus gen. et sp. nov.

opencc-by-4.0Dec 2006View details →
zenodo36/100

Fig. 2 in Concentrations of juvenile and small adult cephalopods in the Hirnantian cherts (Late Ordovician) of Porkuni, Estonia

Fig. 2. Sedimentology and stratigraphic division of the Porkuni section, Estonia.

opencc-by-4.0Dec 2007View details →
dryad36/100

Data for: Insights for modern invasion ecology from biotic changes of the Clarksville Phase of the Richmondian Invasion (Ordovician, Katian)

<p>The frequency of biotic invasions in modern ecosystems is increasing due to global trade moving taxa outside their native ranges and climate change facilitating establishment of taxa in previously inhospitable regions. Thus, developing a holistic understanding of biotic invasions and how they impact ecosystems over different timescales—from annual to geologic time scales—is vital. Herein we examine a geologically brief invasion event, the Clarksville Phase of the Richmondian Invasion. Prior analyses have established general ecological and evolutionary patterns across the entire Richmondian Invasion, but recent sequence stratigraphic refinement makes analysis of individual invasion pulses possible for the first time. We examine biotic change across the Clarksville Phase and identify invasion impacts on diversity, paleocommunity composition, and niche stability. Invader arrival and success were strongly linked to increased propagule pressure facilitated by sea level changes. Invaders initially colonized deep subtidal environments and then moved offshore facilitated by rapid niche evolution during the invasion interval. Invasive taxa that attained the largest population sizes belonged to previously underutilized ecological guilds. Overall, the introduction of the invasive taxa resulted in increased diversity that was maintained into the post-invasion interval accompanied by a change in community composition in which the invaders became dominant paleocommunity members. Combined these analyses document a biotic invasion facilitated by climate change which increased local diversity through invaders occupying underutilized ecospace and competition-related niche contraction on millennial time scales. Developing a long-term perspective to accompany shorter-term studies facilitates predicting the long-term impacts of modern invasions and creating better-informed policies and practices. </p>

opencc-zeroNov 2022View details →
dryad36/100

Phylogeny of the Ordovician and Silurian members of the order Atrypida

<p><span>The brachiopod order Atrypida originated in the Middle Ordovician and went extinct in the Late Devonian. Few cladistic studies have been undertaken for this group. Here we investigate their early evolution through the Silurian time. We present a parsimony-based phylogenetic analysis of 41 characters and 70 genera representing all the early taxonomic groups within the order. The stratigraphic record of the fossil genera analysed here strongly supports the parsimony phylogeny. Most currently recognized subfamilies and families may be identified within clades, except for the Atrypinae, Idiospirinae, and the Septatrypidae. This warrants subdivision of the former and redefinition of the two latter. The subfamily Atrypinae is redefined and a new subfamily of the Atrypidae, the Protatrypinae is split off. Tracing character evolution across the tree indicates that calcified spiralia and a jugum or jugal processes characterize all members of the Atrypida, except the most basal clade, the Cyclospiridae, that lacks a calcified jugum. Ribs are a homoplasious character, occurring in numerous clades throughout the tree. Darriwillian through Sandbian was a time with rapid evolution when most new autapomorphies seen in the atrypides evolved. This interval is part of the Great Ordovician Biodiversification Event (GOBE). Solid teeth, dorsal direction of spiralia, elaborate ornamentation, and frills evolved in the latest Katian into early Silurian time. Solid teeth and dorsally directed spiralia, seen in distantly related clades from the latest Katian on, may be analogous features. The Late Ordovician Mass Extinction (LOME) is indicated in the stratigraphic tree together with a possible event at the end of Aeronian. The tree supports the long-held assumptions that the Plectatrypinae evolved from the Spirigerininae. It further suggests that the genus <em>Tuvaella</em> is included with the Davidsonioidea. Likewise, the redefined Atrypinae is a sister group of the Lissatrypidae and a derived group in the phylogenetic tree. </span></p>

opencc-zeroDec 2021View details →
dryad36/100

Goryeocrinus pentagrammos n. gen. n. sp. (Rhodocrinitidae; Diplobathrida), the first record of camerate crinoid from the Middle Ordovician (Darriwilian) of South Korea (East Gondwana)

<p><em>Goryeocrinus</em> <em>pentagrammos</em> n. gen. n. sp. from the Jigunsan Formation of South Korea is described, which is the first diplobathrid record from Middle Ordovician (middle Darriwilian) of East Gondwana. Phylogenetic analyses suggest that <em>G</em>. <em>pentagrammos</em> is a member of the paraphyletic Rhodocrinitidae of the Diplobathrida and most closely related to <em>Paradiabolocrinus</em> from the Late Ordovician (Sandbian) of Laurentia. <em>G</em>. <em>pentagrammos</em> is characterized by having a pentameral, flat bowl-shaped calyx, conspicuous pentagrammatic ridge formed by bifurcated median ray ridge and pentagonal basal ridge, at least two interradials in the first row of regular interrays, and anitaxial ridge originating from CD interray but close to C ray radial, and lacking intrabrachials and interradials between secundibrachials. The occurrence of <em>G</em>. <em>pentagrammos</em> from South Korea (East Gondwana) drastically expands Ordovician paleogeographic range of the camerates which have otherwise been recorded from Laurentia, West Gondwana, Avalonia, and Baltica.</p>

opencc-zeroDec 2022View details →
dryad36/100

Data from: Comparisons of Late Ordovician ecosystem dynamics before and after the Richmondian Invasion reveal consequences of invasive species in benthic marine paleocommunities

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publicMay 2020View details →
dryad36/100

Data from: Late Ordovician and Early Silurian virgianid and stricklandioid brachiopods from North Greenland: Implications for a warm-water faunal province

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publicJan 2024View details →
dryad36/100

A Hirnantian holdover from the late Ordovician mass extinction: phylogeny and biogeography of a new Anthracocrinid crinoid from Estonia

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publicNov 2020View details →
dryad36/100

Data from: New taxa and revised stratigraphic distribution of the crinoid fauna from Anticosti Island, Québec, Canada (Late Ordovician-Early Silurian)

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publicApr 2019View details →
dryad36/100

Late Ordovician brachiopods from east-central Alaska, northwestern margin of Laurentia

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publicFeb 2020View details →
dryad36/100

Data from: Katian (Late Ordovician) trilobites of the North Qilian Mountains and their palaeogeographical implications for the Proto-Tethys Archipelagic Ocean (PTAO)

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publicOct 2023View details →
dryad36/100

Phylogeny of the Ordovician and Silurian members of the order Atrypida

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publicDec 2022View details →
dryad36/100

Data from: Latest Ordovician (Hirnantian) brachiopod faunal lists used for non-matric multidimensional scaling (NMDS) and network analyses

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publicDec 2023View details →
dryad36/100

Goryeocrinus pentagrammos n. gen. n. sp. (Rhodocrinitidae; Diplobathrida), the first record of camerate crinoid from the Middle Ordovician (Darriwilian) of South Korea (East Gondwana)

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publicDec 2022View details →
dryad36/100

Shifting speciation mode and biogeographic patterns during the Late Ordovician (Sandbian-Katian) in Laurentian brachiopods (Atrypida, Anazygidae)

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publicJun 2025View details →
dryad36/100

Data for: Insights for modern invasion ecology from biotic changes of the Clarksville Phase of the Richmondian Invasion (Ordovician, Katian)

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publicNov 2022View details →
dryad36/100

Phylogenetic position and stratigraphic uncertainty of a new flexible crinoid from the Ordovician–Silurian boundary of Anticosti Island (Quebec, Canada)

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publicMay 2025View details →
dryad36/100

Global factors constrain body size trends across the Great Ordovician Biodiversification Event at a regional scale: a case study from the Arbuckle Mountains of Oklahoma

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publicJul 2025View details →
dryad36/100

Middle Ordovician (middle Darriwilian) Archaeospicularia and Entactinaria (radiolarians) from the Table Cove Formation, Piccadilly Quarry, western Newfoundland, Canada

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publicNov 2021View details →

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