In the Early to Middle Devonian shale sequences of Germany and Morocco, pyritised and secondarily limonitised cephalopod remains are common. Details of the soft−tissue attachment structures are sometimes preserved on the internal moulds of the body chamber and phragmocone of these cephalopods. Some of the studied Orthocerida show a very faint annular elevation and a dorsal furrow. A few Bactritida show a distinctive annular elevation with two circular bands. The bands form a paired or threefold lobe at the dorsum of the shell. Morphological differences between Orthocerida and Bactritida suggest different soft part morphologies. A comparison of the attachment scars shows that the Bactritida are intermediate between the Orthocerida and ammono...
Anomalocaridids, giant lightly sclerotized invertebrate predators, occur in a number of exceptionall...
The post‐mortem history of a prolific Maastrichtian ammonite and nautiloid fauna preserved as phosph...
The ammonoids from the middle Famennian black limestone nodules at Kattensiepen (Rhenish Mountains) ...
In the Early to Middle Devonian shale sequences of Germany and Morocco, pyritised and secondarily li...
Internal moulds of the relatively small − to moderate−size shells of Early Devonian ectocochleate ce...
Taxonomic position of the cephalopod Bactroceras sandbergeri (Barr., 1867) from the Ordovician of th...
Devonian condensed sections of the northern Tafilalt Platform (Anti-Atlas, Morocco) are often extrem...
Fluctuations in body size of orthoconic cephalopods are reported from late Silurian to Late Devonian...
Five cephalopod specimens from the Lower Devonian of Bohemia (Czech Republic) preserve colour patter...
Abstract: The number, outline and arrangement of muscle scars on the internal mould of the body cham...
Soft-tissue attachment scars of two genera and four species of Late Jurassic craspeditid ammonites f...
Tragoceras falcatum (Schlotheim, 1820) is a common, loosely coiled estonioceratid (Tarphycerida, Cep...
In the latest Famennian, black shale deposition occurred in many regions, some suggested a marine tr...
A discrete pair of muscle scars is described for the first time on the umbilical wall of the open-co...
It is widely accepted that the effects of global sea-level changes at the transition from the Devoni...
Anomalocaridids, giant lightly sclerotized invertebrate predators, occur in a number of exceptionall...
The post‐mortem history of a prolific Maastrichtian ammonite and nautiloid fauna preserved as phosph...
The ammonoids from the middle Famennian black limestone nodules at Kattensiepen (Rhenish Mountains) ...
In the Early to Middle Devonian shale sequences of Germany and Morocco, pyritised and secondarily li...
Internal moulds of the relatively small − to moderate−size shells of Early Devonian ectocochleate ce...
Taxonomic position of the cephalopod Bactroceras sandbergeri (Barr., 1867) from the Ordovician of th...
Devonian condensed sections of the northern Tafilalt Platform (Anti-Atlas, Morocco) are often extrem...
Fluctuations in body size of orthoconic cephalopods are reported from late Silurian to Late Devonian...
Five cephalopod specimens from the Lower Devonian of Bohemia (Czech Republic) preserve colour patter...
Abstract: The number, outline and arrangement of muscle scars on the internal mould of the body cham...
Soft-tissue attachment scars of two genera and four species of Late Jurassic craspeditid ammonites f...
Tragoceras falcatum (Schlotheim, 1820) is a common, loosely coiled estonioceratid (Tarphycerida, Cep...
In the latest Famennian, black shale deposition occurred in many regions, some suggested a marine tr...
A discrete pair of muscle scars is described for the first time on the umbilical wall of the open-co...
It is widely accepted that the effects of global sea-level changes at the transition from the Devoni...
Anomalocaridids, giant lightly sclerotized invertebrate predators, occur in a number of exceptionall...
The post‐mortem history of a prolific Maastrichtian ammonite and nautiloid fauna preserved as phosph...
The ammonoids from the middle Famennian black limestone nodules at Kattensiepen (Rhenish Mountains) ...