Results 11 to 20 of about 802 (179)

Trends in Ocean S‐Isotopes May Be Influenced by Major LIP Events

open access: yesGeophysical Monograph Series, Page 341-376., 2021

Exploring the links between Large Igneous Provinces and dramatic environmental impact

An emerging consensus suggests that Large Igneous Provinces (LIPs) and Silicic LIPs (SLIPs) are a significant driver of dramatic global environmental and biological changes, including mass extinctions.
Ross. R. Large   +5 more
wiley  

+8 more sources

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

The Precambrian paleogeography of Laurentia [PDF]

open access: yes, 2021
Laurentia is the craton that forms the Precambrian core of North America and was a major continent throughout the majority of the Proterozoic following its amalgamation 1.8 billion years ago. The paleogeographic position of Laurentia is key to the development of reconstructions of Proterozoic paleogeography including the Paleoproterozoic to ...
openaire   +6 more sources

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