Size-frequency distribution and mode of occurrence of a Late Cretaceous inoceramid bivalve Inoceramus hobetsensis NAGAO & MATSUMOTO, 1939 were examined. A large number of samples, all of which were recovered from the Upper Cretaceous of the Tappu area, northwestem Hokkaido, show chronological change in the size-frequency distribution pattern. The proportion of the frequency of relatively small individuals (20-40 cm in size) tends to increase toward the upper sequence of the range of this species. The relative frequency of huge individuals (60-80 cm in size) also increases in the upper part, although the mode of fossil occurrence indicates that the size-frequency distribution might be biased by post-mortem taphonomic processes. The result of...
Two groups of bivalves, the inoceramids and buchiids, are particularly useful zone fossils in the Me...
Phanerozoic trends in shell and life habit traits linked to postmortem durability were evaluated for...
Marine invertebrate taxa that survived the late Permian (latest Changhsingian) mass extinction event...
Size-frequency distribution and mode of occurrence of a Late Cretaceous inoceramid bivalve Inoceramu...
Variation of the external shell sculpture in three species of Late Cretaceous inoceramid bivalve Sph...
Cretaceous inoceramid bivalves were widely distributed. They did not thrive in very shallow or very ...
Reduction in body size of organisms following mass extinctions is well‐known and often ascribed to t...
The last inoceramid bivalves in Antarctica are no younger than mid- to late Campanian in age. They o...
Cretaceous/Tertiary boundary sections located in the Biscay region of southwestern France and northe...
Biometric studies of coccoliths, the remains of coccolithophores, offer the opportunity to survey si...
Biostratigraphic correlations of inoceramid bivalves between the North Pacific and Euramerican provi...
Changes in body size have been the subject of numerous palaeontological and neontological studies, b...
Fossil communities in the wake of mass extinction are often characterised by small sized individuals...
Exceptionally well preserved specimens of the bivalve mollusc Modiola major were collected from a Lo...
Fossils in the immediate aftermath of mass extinctions are often of small size, a phenomenon attribu...
Two groups of bivalves, the inoceramids and buchiids, are particularly useful zone fossils in the Me...
Phanerozoic trends in shell and life habit traits linked to postmortem durability were evaluated for...
Marine invertebrate taxa that survived the late Permian (latest Changhsingian) mass extinction event...
Size-frequency distribution and mode of occurrence of a Late Cretaceous inoceramid bivalve Inoceramu...
Variation of the external shell sculpture in three species of Late Cretaceous inoceramid bivalve Sph...
Cretaceous inoceramid bivalves were widely distributed. They did not thrive in very shallow or very ...
Reduction in body size of organisms following mass extinctions is well‐known and often ascribed to t...
The last inoceramid bivalves in Antarctica are no younger than mid- to late Campanian in age. They o...
Cretaceous/Tertiary boundary sections located in the Biscay region of southwestern France and northe...
Biometric studies of coccoliths, the remains of coccolithophores, offer the opportunity to survey si...
Biostratigraphic correlations of inoceramid bivalves between the North Pacific and Euramerican provi...
Changes in body size have been the subject of numerous palaeontological and neontological studies, b...
Fossil communities in the wake of mass extinction are often characterised by small sized individuals...
Exceptionally well preserved specimens of the bivalve mollusc Modiola major were collected from a Lo...
Fossils in the immediate aftermath of mass extinctions are often of small size, a phenomenon attribu...
Two groups of bivalves, the inoceramids and buchiids, are particularly useful zone fossils in the Me...
Phanerozoic trends in shell and life habit traits linked to postmortem durability were evaluated for...
Marine invertebrate taxa that survived the late Permian (latest Changhsingian) mass extinction event...