Javascript must be enabled to continue!
Palaeobiology of Silurian Leptaeninae (Brachiopoda) from Gotland, Sweden
View through CrossRef
Leptaenine brachiopods are common and widespread on Gotland. Lepidoleptaena poulseni and Leptaena rhomboidalis retained a functional apical pedicle throughout ontogeny, and both had strong adductor muscles and robust ornamentation, allowing them to occupy shallow water and high energy environments. A pedicle-shortening muscle is present within the pedicle tube of Leptaena rhomboidalis. Leptaena sperion, L. depressa visbyensis, and L. depressa lata inhabited low energy environments, retaining very slender pedicles. L. depressa depressa and L. parvorugata atrophied the pedicle early and then lived ambitopically in deeper water. The presence or absence of the apical pedicle strongly influenced the cardinal process morphology. Leptaenine shells had a small gape. The lophophore was simple, similar to productids and Leptaenoidea. In closed valves, the inner epithelium of leptaenine trails remained exposed to the sea. This was probably important in gas exchange. The life position of pedically attached species was with the disc vertical. Some ambitopic specimens may have retained a similar attitude. Shells of L. depressa depressa and Lepidoleptaena poulseni commonly are encrusted by epibionts, apparently without problems for larger shells. Small shells are shown to have been killed by bryozoan epizoans. Repaired shell damage is rare on the disc but is common along the commisure.
Title: Palaeobiology of Silurian Leptaeninae (Brachiopoda) from Gotland, Sweden
Description:
Leptaenine brachiopods are common and widespread on Gotland.
Lepidoleptaena poulseni and Leptaena rhomboidalis retained a functional apical pedicle throughout ontogeny, and both had strong adductor muscles and robust ornamentation, allowing them to occupy shallow water and high energy environments.
A pedicle-shortening muscle is present within the pedicle tube of Leptaena rhomboidalis.
Leptaena sperion, L.
depressa visbyensis, and L.
depressa lata inhabited low energy environments, retaining very slender pedicles.
L.
depressa depressa and L.
parvorugata atrophied the pedicle early and then lived ambitopically in deeper water.
The presence or absence of the apical pedicle strongly influenced the cardinal process morphology.
Leptaenine shells had a small gape.
The lophophore was simple, similar to productids and Leptaenoidea.
In closed valves, the inner epithelium of leptaenine trails remained exposed to the sea.
This was probably important in gas exchange.
The life position of pedically attached species was with the disc vertical.
Some ambitopic specimens may have retained a similar attitude.
Shells of L.
depressa depressa and Lepidoleptaena poulseni commonly are encrusted by epibionts, apparently without problems for larger shells.
Small shells are shown to have been killed by bryozoan epizoans.
Repaired shell damage is rare on the disc but is common along the commisure.
Related Results
Lower Paleozoic stratigraphy and geology, Richardson Mountains, Yukon (with stratigraphic and paleontological appendices)
Lower Paleozoic stratigraphy and geology, Richardson Mountains, Yukon (with stratigraphic and paleontological appendices)
The Richardson Trough was a rift basin on the southern margin of an ancestral Iapetus Ocean. It was part of a complex paleogeography that included at least two major rift basins on...
Benthic response to the strong Silurian climatic fluctuations – implications from Gotland (Sweden)
Benthic response to the strong Silurian climatic fluctuations – implications from Gotland (Sweden)
Abstract
Climatically the Silurian was a most unstable period, as it is shows several strong d13C excursion, with the Lau excursion being the strongest short-lived positive...
Pterotheca (Gastropoda) from the Telychian (Silurian) Xiushan Formation of South China: taxonomy, paleoecology, and paleogeography
Pterotheca (Gastropoda) from the Telychian (Silurian) Xiushan Formation of South China: taxonomy, paleoecology, and paleogeography
AbstractPterotheca Salter, 1853 is an unusual but readily identifiable bellerophontoid gastropod that occurs in the Upper Ordovician to the Llandovery of the lower Silurian in many...
Main Ordovician–Silurian events in the South Ural and event stratigraphy regional tasks
Main Ordovician–Silurian events in the South Ural and event stratigraphy regional tasks
The main regional abiotic events of the Ordovician and Silurian of the Southern Urals are manifested in the restructuring of sedimentation in the paleobasin. Eustatic fluctuations ...
Geochemical analysis of the Late Ordovician–early Silurian black shales from the Xindi No.2 well in the Upper Yangtze area, South China: Implications for provenance, palaeoclimate and palaeoenvironmental change
Geochemical analysis of the Late Ordovician–early Silurian black shales from the Xindi No.2 well in the Upper Yangtze area, South China: Implications for provenance, palaeoclimate and palaeoenvironmental change
Abstract
The Ordovician-Silurian transition was a critical period in geological history, during which profound changes in climatic, biotic, and oceanic conditions occurred....
Silurian Ostracoda from Anticosti Island, Quebec
Silurian Ostracoda from Anticosti Island, Quebec
Anticosti Island, at the northern edge of the Appalachian structural province, presents the most complete sequence of Late Ordovician to Middle Silurian sedimentary rocks in easter...
Locomotory and morphological evolution of the earliest Silurian graptolite Demirastrites selected by hydrodynamics
Locomotory and morphological evolution of the earliest Silurian graptolite Demirastrites selected by hydrodynamics
AbstractInterpretation of the locomotion of biostratigraphically important graptolite taxa is rare, and rendered problematic due to a lack of close modern analogues and soft tissue...
Pre-Carboniferous geology of the northern part of the Arctic Islands: Northern Heiberg Fold Belt, Clements Markham Fold Belt, and Pearya; northern Axel Heiberg and Ellesmere islands
Pre-Carboniferous geology of the northern part of the Arctic Islands: Northern Heiberg Fold Belt, Clements Markham Fold Belt, and Pearya; northern Axel Heiberg and Ellesmere islands
This report describes and interprets the geology of three tectono-stratigraphic belts in the northernmost part of the Canadian Arctic Archipelago that differ in structural trend an...

