Results 91 to 100 of about 893 (201)
A Hirnantian deep-water refuge for warm-water ostracods in Baltoscandia
The latest Ordovician is marked by a severe climate change, the Hirnantian glaciation. This climatic event affected many marine taxa including ostracods. Rich and abundant ostracod assemblages of the Baltic Palaeobasin were severly impoverished.
Meidla, T., Truuver, K.
core
Post-glacial Hirnantian (upper Ordovician) bryozoans from western Argentina: implications for survival and extinction patterns [PDF]
Two bryozoan taxa occurring in the Hirnatian (Upper Ordovician) deposits in western Argentina document a first postglacial community associated with a mid-to high-latitude brachiopod assemblage, known as the typical Hirnantia fauna, in the Argentine ...
Halpern, Karen, Carrera, Marcelo Gabriel
core +1 more source
(Uploaded by Plazi from the Biodiversity Heritage Library) No abstract provided.
Štorch, Petr, Loydell, David K
openaire +2 more sources
87th Annual Meeting of the Meteoritical Society 2025: Abstracts
Meteoritics &Planetary Science, Volume 60, Issue S1, Page 30-350, August 2025.
wiley +1 more source
Based on the drilling, logging and field analysis, this paper discusses the lithofacies paleogeography of the Ordovician and its petroleum potential in the Middle-Upper Yangtze Area, South China.
Wenzheng Li +9 more
doaj +1 more source
Rapid marine oxygen variability: Driver of the Late Ordovician mass extinction. [PDF]
Kozik NP +8 more
europepmc +1 more source
Marine shales directly overlying lower Hirnantian (uppermost Ordovician) glacially related sediments in Mauritania (North-West Africa) have produced a rich graptolite fauna spanning the Ordovician-Silurian boundary in an area of high palaeolatitude.
Underwood, Charlie J. +2 more
core
Characteristics, distribution, and origin of ferruginous deposits within the Late Ordovician glaciogenic setting of Arabia. [PDF]
Alqubalee A +4 more
europepmc +1 more source
Carbon and nitrogen isotope records of the Hirnantian glaciation [PDF]
The Hirnantian mass extinction was the second largest of the Phanerozoic. A global sea level fall resulting from a glaciation on Gondwanaland caused significant changes in ocean circulation patterns and nutrient cycling that is recorded as a worldwide ...
LaPorte, Dan F
core

