Graptolite rhabdosomes display a diverse suite of morphologies. The range of morphotypes present within most moderate to high diversity assemblages from the Ordovician and Silurian is similar, despite the different taxonomic composition of the faunas at different times. Survivorship analyses of graptolite faunas from the Ordovician and Silurian demonstrate strong similarities in the mortality rates of unrelated graptolites of similar functional morphology. It also shows a strong correlation of decreasing mortality rates amongst more mature colonies with increasing rhabdosome complexity. This similarity in both functional morphology and life history of graptolites suggests that they lived within a very stable planktic community structure. ❑ ...
There are several different types of variation in populations of fossil organisms. These include int...
Abstract: The extinctions that occurred in the latest Ordovician and earliest and latest Wenlock, we...
Morphometric analysis of graptolites from the persculptus and acuminatus biozones of central Wales i...
Graptolite rhabdosomes display a diverse suite of morphologies. The range of morphotypes present wit...
Three large populations of graptoloids from the Utica Shale contain Orthograptus quadrimucronatus mi...
An integrated approach has been used to assess the palaeoecology of graptolites both as a discrete g...
Main trends and dynamics of evolution in the late graptoloids are traced on the basis of their morph...
SUMMARY: The variation of taxonomically important characters commonly used in the classification of ...
This thesis presents new graptoloid biostratigraphic range charts for the Ordovician and Silurian of...
Graptolites are common fossils in Lower Palaeozoic strata, but little is known of their...
Graptolites were colonial organisms that first appeared in the Cambrian. In early Ordovician times t...
The morphological study of extinct taxa allows for analysis of a diverse set of macroevolutionary hy...
The progressive loss of stipes through the Ordovician and the appearance of uniserial forms in the S...
Graptoloid evolutionary dynamics show a marked contrast from the Ordovician to the Silurian. Subdued...
Marine shales directly overlying lower Hirnantian (uppermost Ordovician) glacially related sediments...
There are several different types of variation in populations of fossil organisms. These include int...
Abstract: The extinctions that occurred in the latest Ordovician and earliest and latest Wenlock, we...
Morphometric analysis of graptolites from the persculptus and acuminatus biozones of central Wales i...
Graptolite rhabdosomes display a diverse suite of morphologies. The range of morphotypes present wit...
Three large populations of graptoloids from the Utica Shale contain Orthograptus quadrimucronatus mi...
An integrated approach has been used to assess the palaeoecology of graptolites both as a discrete g...
Main trends and dynamics of evolution in the late graptoloids are traced on the basis of their morph...
SUMMARY: The variation of taxonomically important characters commonly used in the classification of ...
This thesis presents new graptoloid biostratigraphic range charts for the Ordovician and Silurian of...
Graptolites are common fossils in Lower Palaeozoic strata, but little is known of their...
Graptolites were colonial organisms that first appeared in the Cambrian. In early Ordovician times t...
The morphological study of extinct taxa allows for analysis of a diverse set of macroevolutionary hy...
The progressive loss of stipes through the Ordovician and the appearance of uniserial forms in the S...
Graptoloid evolutionary dynamics show a marked contrast from the Ordovician to the Silurian. Subdued...
Marine shales directly overlying lower Hirnantian (uppermost Ordovician) glacially related sediments...
There are several different types of variation in populations of fossil organisms. These include int...
Abstract: The extinctions that occurred in the latest Ordovician and earliest and latest Wenlock, we...
Morphometric analysis of graptolites from the persculptus and acuminatus biozones of central Wales i...