Results 81 to 90 of about 1,166 (193)
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
Bioturbators as ecosystem engineers in space and time
Abstract Biogenic sedimentary structures offer a unique perspective for understanding the role of the biosphere in the interaction with other Earth subsystems and the building up of our planet. The record of their ancient equivalents provides a wealth of information for reconstructing the role of bioturbators as ecosystem engineers using multiple ...
M. Gabriela Mángano +3 more
wiley +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
A Hirnantian deep-water refuge for warm-water ostracods in Baltoscandia [PDF]
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
The carbonates associated with the Late Ordovician (Katian–Hirnantian) Boda mounds of the Siljan district, Sweden, contain a rich cephalopod fauna.
Jan Ove R. Ebbestad +3 more
core +1 more source
We present a 13Ccarb chemostratigraphy for the Late Ordovician Hirnantian Stage based on 208 whole-rock samples from six outcrops in the Oslo-Asker district, southern Norway.
Lehnert, Oliver, +17 more
core +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
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
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
Herein is reported the first occurrence of ostracodes from the Iapó Formation, an uppermost Ordovician unit of the Rio Ivaí Group in the Paraná basin, Brazil.
Do Carmo, Dermeval Aparecido +19 more
core +1 more source

