Results 1 to 10 of about 776 (129)

A new Cambrian catillicephalid trilobite from the Shallow Bay Formation of western Newfoundland, Canada [PDF]

open access: yesActa Palaeontologica Polonica, 2022
Species of Catillicephala are known from sites around the mid-Cambrian margin of Laurentian North America, including Vermont, Quebec, Newfoundland and North Greenland. Catillicephala cifellii sp. nov.
STEPHEN R. WESTROP, ALYCE A. DENGLER
doaj   +1 more source

Developing a phylogenetic framework for tiny Ordovician brachiopods (Atrypida: Anazyginae and Catazyginae) from the eastern United States [PDF]

open access: yesEstonian Journal of Earth Sciences, 2023
Elucidating how environmental change can facilitate the differentiation of evolutionary lineages and the establishment of new species is a critical issue for understanding both the history of life and modern biota. Notably, speciation events are known to
Mariana Vilela-Andrade   +1 more
doaj   +1 more source

Where are all the Ordovician sea cucumbers (Echinodermata)? [PDF]

open access: yesEstonian Journal of Earth Sciences, 2023
The Ordovician Period witnessed the first evidence of appearance of all modern echinoderm clades as well as it is the most concentrated interval of echinoderm diversity in Earth’s history.
Mike Reich
doaj   +1 more source

Upper Ordovician hardgrounds – from localized surfaces to global biogeochemical events [PDF]

open access: yesEstonian Journal of Earth Sciences, 2023
Upper Ordovician hardgrounds display a spectrum of complexity reflecting a range of local to global-scale processes. Hardgrounds are cemented seafloor surfaces typically marked by the presence of encrusting taxa and borings.
Timothy R. Paton   +4 more
doaj   +1 more source

The late Katian Elkhorn event: precursor to the Late Ordovician mass extinction [PDF]

open access: yesEstonian Journal of Earth Sciences, 2023
The late Katian Elkhorn event is a biogeochemical perturbation preceding the Late Ordovician mass extinction (LOME) with an exceptional record in the United States (U.S.).
Patrick I. McLaughlin   +8 more
doaj   +1 more source

Early Tremadocian graptolites from the Arivechi area, Sonora, northern Mexico [PDF]

open access: yesEstonian Journal of Earth Sciences, 2023
Graptolites from the early Tremadocian Anisograptus matanensis Biozone are identified from east-central Sonora, northwestern Mexico, within a carbonate-shelf succession deposited on the southwestern continental shelf margin of Laurentia.
Dulce Raquel Reyes-Montoya   +5 more
doaj   +1 more source

First palaeoscolecid from the Cambrian (Drumian, Miaolingian) Marjum Formation of western Utah, USA [PDF]

open access: yesActa Palaeontologica Polonica, 2021
The middle Marjum Formation is one of five Miaolingian Burgess Shale-type deposits in Utah, USA. It preserves a diverse non-biomineralized fossil assemblage, which is dominated by panarthropods and sponges.
Wade W. Leibach   +4 more
doaj   +1 more source

Late Ordovician jawed polychaete fauna from the Spiti Valley, northern India [PDF]

open access: yesEstonian Journal of Earth Sciences, 2023
The final part of the Ordovician Period was characterised by major perturbations in climate, environments and ecosystems, as proved by numerous studies. These changes resulted in one of the biggest extinctions in Earth’s history. Most research in early
Petra Tonarová   +3 more
doaj   +1 more source

Implications of Timanian thrust systems in the Barents Sea and Svalbard on using paleontological constraints for plate tectonics reconstructions

open access: yesOpen Research Europe, 2023
Background The Svalbard Archipelago is commonly believed to have been located at comparable latitude and, possibly, to have been attached to Laurentia in the early Paleozoic (500–420 Ma) based on
Jean-Baptiste P. Koehl
doaj   +1 more source

Pathways and mechanisms of Late Ordovician (Katian) faunal migrations of Laurentia and Baltica [PDF]

open access: yesEstonian Journal of Earth Sciences, 2015
Late Ordovician strata within the Cincinnati Basin record a mass faunal migration event during the C4 and C5 depositional sequences. The geographic source region for the invaders and the paleoceanographic conditions that facilitated dispersal into the ...
Adriane R. Lam, Alycia L. Stigall
doaj   +1 more source

Home - About - Disclaimer - Privacy