The phosphate-bearing rocks (phosphate rocks and phosphorites) were studied over a 45-meter interval of the Moyero river section, covering the upper part of the Darriwilian and the lower part of the Sandbian stages of the Ordovician.
Lykov Nikita Andreevich +2 more
doaj +1 more source
ABSTRACT Filamentous, anastomosing spar‐filled networks in Phanerozoic carbonates have been interpreted as the mineralised remains of keratose (non‐spiculate) sponges, yet their recognition remains contested because fabrics of broadly similar appearance may arise from microbial, diagenetic or physical processes. This study combines direct fossil–modern
Jeong‐Hyun Lee +2 more
wiley +1 more source
Cornulitids (tubeworms) from the Late Ordovician Hirnantia fauna of Morocco
Two species of cornulitids, Cornulites gondwanensis sp. nov. and C. aff. shallochensis Reed are described from the Hirnantian of Morocco, within an assemblage representative of the Hirnantia brachiopod fauna occurring near the Ordovician South Pole.
Gutiérrez Marco, Juan Carlos +4 more
core +1 more source
Cascading trend of Early Paleozoic marine radiations paused by Late Ordovician extinctions. [PDF]
Rasmussen CMØ +3 more
europepmc +1 more source
A common arthropod from the Late Ordovician Big Hill Lagerstätte (Michigan) reveals an unexpected ecological diversity within Chasmataspidida. [PDF]
Lamsdell JC, Gunderson GO, Meyer RC.
europepmc +1 more source
Mercury Spikes Indicate a Volcanic Trigger for the Late Ordovician Mass Extinction Event: An Example from a Deep Shelf of the Peri-Baltic Region. [PDF]
Smolarek-Lach J +3 more
europepmc +1 more source
Tempo of the Late Ordovician mass extinction controlled by the rate of climate change. [PDF]
Zhang Z +10 more
europepmc +1 more source
Identifying the most surprising victims of mass extinction events: an example using Late Ordovician brachiopods. [PDF]
Finnegan S, Rasmussen CMØ, Harper DAT.
europepmc +1 more source
Late Ordovician eurypterid preserves oldest euchelicerate musculature in pyrite. [PDF]
Bicknell RDC, Gaines RR, Hopkins MJ.
europepmc +1 more source
Late Ordovician to Silurian evolution of Eastern Avalonia during Iapetus closure.
This chapter contains sections titled: Palaeocontinental Setting: Eastern Avalonia Converges with Baltica and Laurentia Changes in Global Sea Level and Climate Large-Scale Stratigraphic Signatures Post-Volcanic Transgressions and Mud Blankets (Late ...
Woodcock, N. H.
core +1 more source

