The graptoloid prosicula (conus and cauda) forms the first part of the growing colony, and was probably secreted during a single continuous episode of growth. The wall is composed of a central unit of criss-cross fibrils (fusellar fabric), interlaced with parallel fibrils whose grouping appears as the spiral line (spiral line fabric). The conus is lined with a granular or felted sheet (sheet fabric). The diaphragm, at the apex of the conus, appears to be formed of fusellar fabric. The cauda is formed of fusellar and spiral fabrics with a central cavity apparently not open to the conus interior. An outer layer (diamond, mesh fabric) of fibrils forming a diamond mesh covers both conus and cauda, and is itself overlain by longitudinal rods. Th...
Graptovermids are redefined as resting terminal portions of unknown encrusting graptolites stolothec...
Unusual preservation of small primaspid trilobites may provide a key to the first recognition of a m...
An enigmatic clonal organism from the earliest Floian (Arenig) Fenxiang Formation at Tianjialing in ...
The graptoloid prosicula (conus and cauda) forms the first part of the growing colony, and was proba...
The fusellar tissue of an Ordovician graptoblast has been studied with ТЕМ. It was found that it is ...
The periderm of Ordovician Pterobranchites antiquus Kozłowski, 1967 has been examined with SEM. Four...
Abstract.- The ultrastructure of the organic coenecium in living Cephalodiscus (Cephalodiscus) inaeq...
Light microscopic, SEM and TEM investigations show that the periderm of the problematic Ordovician o...
The surfaces of rhabdosomes in dendroid and tuboid graptolites and in Mastigograptus were investigat...
Dissepiments or connecting bars between adjacent stipes in rhabdosomes of dendroid graptolites were ...
The surfaces of rhabdosomes in dendroid and tuboid graptolites and in Mastigo-graptus were investiga...
Graptolites are common fossils in Lower Palaeozoic strata, but little is known of their...
light microscopy, transmission electron microscopy, and scanning electron microscopy. The coenecium ...
The ultrastructure of the dendroid genera Acanthograptus, Dendrograptus, Desmograptus, Ptilograptus ...
The ultrastructure of the dendroid genera Acanthograptus, Dendrograptus, Desmograptus, Ptilograptus ...
Graptovermids are redefined as resting terminal portions of unknown encrusting graptolites stolothec...
Unusual preservation of small primaspid trilobites may provide a key to the first recognition of a m...
An enigmatic clonal organism from the earliest Floian (Arenig) Fenxiang Formation at Tianjialing in ...
The graptoloid prosicula (conus and cauda) forms the first part of the growing colony, and was proba...
The fusellar tissue of an Ordovician graptoblast has been studied with ТЕМ. It was found that it is ...
The periderm of Ordovician Pterobranchites antiquus Kozłowski, 1967 has been examined with SEM. Four...
Abstract.- The ultrastructure of the organic coenecium in living Cephalodiscus (Cephalodiscus) inaeq...
Light microscopic, SEM and TEM investigations show that the periderm of the problematic Ordovician o...
The surfaces of rhabdosomes in dendroid and tuboid graptolites and in Mastigograptus were investigat...
Dissepiments or connecting bars between adjacent stipes in rhabdosomes of dendroid graptolites were ...
The surfaces of rhabdosomes in dendroid and tuboid graptolites and in Mastigo-graptus were investiga...
Graptolites are common fossils in Lower Palaeozoic strata, but little is known of their...
light microscopy, transmission electron microscopy, and scanning electron microscopy. The coenecium ...
The ultrastructure of the dendroid genera Acanthograptus, Dendrograptus, Desmograptus, Ptilograptus ...
The ultrastructure of the dendroid genera Acanthograptus, Dendrograptus, Desmograptus, Ptilograptus ...
Graptovermids are redefined as resting terminal portions of unknown encrusting graptolites stolothec...
Unusual preservation of small primaspid trilobites may provide a key to the first recognition of a m...
An enigmatic clonal organism from the earliest Floian (Arenig) Fenxiang Formation at Tianjialing in ...