Results 71 to 80 of about 893 (201)
Did lingering ice sheets moderate anoxia in the early Palaeozoic of Libya?
The Hirnantian glaciation of West Gondwana produced a glacially sculpted topography, which is draped by organic-rich latest Ordovician and early Silurian ‘hot shales’.
Meinhold, Guido +3 more
core +1 more source
Composition and significance of the Katian (Upper Ordovician) conodont fauna of the Vaux Limestone (‘Calcaire des Vaux’) in Normandy, France [PDF]
Study of new conodont collections from the Vaux Limestone exposed at its classical locality at Saint-Hilaire-la-Gérard in the Sées syncline, the conodont fauna of which was previously described in a preliminary way by Weyant et al.
Annalisa Ferretti +2 more
doaj +1 more source
Abstract An unusually rich and diverse suite of virgianid brachiopods, hitherto poorly known, is systematically described here for the first time from the Ordovician–Silurian boundary interval (late Katian – Aeronian) of North Greenland. The Late Ordovician virgianids comprise typical taxa of the warm‐water Tcherskidium fauna (e.g.
Jisuo Jin +3 more
wiley +1 more source
The Upper Ordovician of Estonia: facies, sequences, and basin development [PDF]
Sequence stratigraphic analysis of the NabalaâPorkuni regional stages (RSs; upper KatianâHirnantian) of Estonia clarifies the Late Ordovician evolution of the Estonian ShelfâLivonian Basin.
Mark T. Harris +7 more
doaj +1 more source
Taking the Late Ordovician Wufeng Formation (WFF) shale in the Upper Yangtze region as an example, we conducted a lithofacies distribution, thickness quantification, and paleo-topographic reconstruction of the Late Ordovician graptolite zones ...
Sun Shasha +4 more
doaj +1 more source
Orbital and Millennial‐Scale Cycles Through the Hirnantian (Late Ordovician) in Southern China
Abstract The Hirnantian period, making the end of the Ordovician with significant mass extinctions and large ice‐sheets, is a critical interval for studying paleoclimate variations. This research represents the first cyclostratigraphic study of this period, utilizing high‐resolution (1 mm sampling rate) geochemical data from the ∼7‐m thick SH‐1 drill ...
Siding Jin +5 more
wiley +1 more source
A new species of graptolite from the western margin of the Kufra Basin, Libya
Normalograptus kufraensis sp. nov. occurs as monospecific assemblages in the Tanezzuft Formation at the western margin of the Kufra Basin (Jabal Eghei), southern Libya.
Elgardy, Mohamed +3 more
core +1 more source
Microfloristic assemblages have been recovered from the Hirnantian-aged Hassi el Hadjar (‘Argiles Microconglomratiques’) and M’Kratta formations in borehole Nl-2, northeast Algerian Sahara.
SPINA, AMALIA
core +1 more source
Wufeng–Longmaxi Formation and Qiongzhusi Formation are the significant shale gas exploration strata in China. The former has made a major breakthrough, and the exploration of the latter is restricted. At present, it shows good exploration potential in the Qiongzhusi Formation.
Majia Zheng +9 more
wiley +1 more source
Astronomical control on upper ordovician – lower silurian organic matter enrichment in South China
Astronomical forcing governed Late Ordovician–Early Silurian climate dynamics, yet high-resolution Astronomical Time Scales (ATS) and organic enrichment mechanisms during the end-Ordovician extinction remain poorly constrained.
Jinjie Yong +7 more
doaj +1 more source

