A thorough understanding of how communities respond to extreme changes, such as biotic invasions, is essential to manage ecosystems today. Here we constructed fossil food webs to identify changes in Late Ordovician (Katian) shallow marine paleocommunity structure and functioning before and after the Richmondian Invasion, a well-documented ancient invasion. Food webs were compared using descriptive metrics and Cascading Extinction on Graphs models. Richness at intermediate trophic levels was underrepresented when using only data from the Paleobiology Database relative to museum collections, resulting in a spurious decrease in modeled paleocommunity stability. Therefore, museum collections and field sampling may provide more reliable sources ...
The Great Ordovician Biodiversification Event (GOBE) refers to one of the greatest increases in biod...
Besides helping to identify species traits that are commonly linked to extinction risk, the fossil r...
The morphological study of extinct taxa allows for analysis of a diverse set of macroevolutionary hy...
Biotic invasions in the fossil record provide natural experiments for testing hypotheses of niche st...
The set of environmental conditions under which a taxon can survive and maintain viable populations,...
The Ordovician is a time of drastic biological and geological change. Previous work has suggested th...
Extinction in the fossil record is most often measured by the percentage of taxa (species, genera, f...
Mass extinctions documented by the fossil record provide critical benchmarks for assessing changes t...
Mass extinctions affect the history of life by decimating existing diversity and ecological structur...
Mass extinctions have profoundly influenced the history of life, not only through the death of speci...
The late Mesozoic through early Cenozoic is an interval of significant biologic turnover and ecologi...
The Late Ordovician mass extinction was an interval of high extinction with inferred low ecological ...
Echinoderms make up a substantial component of Ordovician marine invertebrates, yet their speciation...
The end-Permian mass extinction, the largest extinction of the Phanerozoic, led to a severe reductio...
The Great Ordovician Biodiversification Event (GOBE) refers to one of the greatest increases in biod...
Besides helping to identify species traits that are commonly linked to extinction risk, the fossil r...
The morphological study of extinct taxa allows for analysis of a diverse set of macroevolutionary hy...
Biotic invasions in the fossil record provide natural experiments for testing hypotheses of niche st...
The set of environmental conditions under which a taxon can survive and maintain viable populations,...
The Ordovician is a time of drastic biological and geological change. Previous work has suggested th...
Extinction in the fossil record is most often measured by the percentage of taxa (species, genera, f...
Mass extinctions documented by the fossil record provide critical benchmarks for assessing changes t...
Mass extinctions affect the history of life by decimating existing diversity and ecological structur...
Mass extinctions have profoundly influenced the history of life, not only through the death of speci...
The late Mesozoic through early Cenozoic is an interval of significant biologic turnover and ecologi...
The Late Ordovician mass extinction was an interval of high extinction with inferred low ecological ...
Echinoderms make up a substantial component of Ordovician marine invertebrates, yet their speciation...
The end-Permian mass extinction, the largest extinction of the Phanerozoic, led to a severe reductio...
The Great Ordovician Biodiversification Event (GOBE) refers to one of the greatest increases in biod...
Besides helping to identify species traits that are commonly linked to extinction risk, the fossil r...
The morphological study of extinct taxa allows for analysis of a diverse set of macroevolutionary hy...