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Siuge Member
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Wrinkled undersurface of soft-surface encrusters: A ) Stromatoporoid Eccl...
in THE REENGINEERING OF REEF HABITATS DURING THE GREAT ORDOVICIAN BIODIVERSIFICATION EVENT
> PALAIOS
Published: 01 September 2017
Fig. 10 . Wrinkled undersurface of soft-surface encrusters: A ) Stromatoporoid Ecclimadictyon , GIT 354-79. B ) Cystoporate bryozoans. Both from Siuge Member, Ärina Formation, Porkuni quarry, Estonia. Scale bar = 10 mm.
Journal Article
THE REENGINEERING OF REEF HABITATS DURING THE GREAT ORDOVICIAN BIODIVERSIFICATION EVENT
Journal: PALAIOS
Publisher: SEPM Society for Sedimentary Geology
Published: 01 September 2017
PALAIOS (2017) 32 (9): 584–599.
...Fig. 10 . Wrinkled undersurface of soft-surface encrusters: A ) Stromatoporoid Ecclimadictyon , GIT 354-79. B ) Cystoporate bryozoans. Both from Siuge Member, Ärina Formation, Porkuni quarry, Estonia. Scale bar = 10 mm. ...
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Journal Article
A new genus and species of cornulitid tubeworm from the Hirnantian (Late Ordovician) of Estonia
Journal: Journal of Paleontology
Publisher: Paleontological Society
Published: 01 January 2024
Journal of Paleontology (2024) 98 (1): 40–46.
... rocks of latest Katian to Rhuddanian age (Pirgu to Juuru regional stages) are exposed here (Hints et al., 2023 ) ( Fig. 2 ). The Ärina Formation (~2.5 m thick, Hirnantian) consists of various shallow-marine carbonates and contains the Siuge Member with characteristic kerogenous limestones...
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Journal Article
Ordovician reef and mound evolution: the Baltoscandian picture
Journal: Geological Magazine
Publisher: Cambridge University Press
Published: 08 June 2016
Geological Magazine (2017) 154 (4): 683–706.
... as baffler in the younger reef generation of the Tõrevere Member (compare Oraspõld, 1975 ; Hints, Oraspõld & Kaljo, 2000 ). Our own investigations in the Porkuni quarry (59.187346°N, 26.187433°E) indicate that small patch reefs, which developed within the older Vohilaid–Siuge Member of the Ärina...
