The species of Inoceramus enjoyed a worldwide distribution during the Cretaceous period. Many examples are found in the Pierre Shale of the Western Interior Seaway in North America. Inoceramus can also be found abundantly in the Cretaceous Gault Clay that underlies London. Other locations for this fossil include Vancouver Island, British Columbia, Canada; Texas, Tennessee, California and Alaska, USA; Spain, France, and Germany.
The clam had a thick shell paved with "prisms" of calcite deposited perpendicular to the surface, which gave it a pearly luster in life. Most species have prominent growth lines which appear as raised semicircles concentric to the growing edge of the shell. Paleontologists suggest that the giant size of some species was an adaptation for life in the murky bottom waters, with a correspondingly large gill area that would have allowed the animal to cope with oxygen-deficient waters.
McMurray formation foraminifera within the lower Albian (Lower Cretaceous) loon river shales of northern Alberta.(Report)
Nov 01, 2007; Abstract: Early Cretaceous paleogeography and biostratigraphy of western Canada are reviewed in light of a reassessment of...
Description and paleobiogeographic significance of a rare Cenomanian molluscan faunule from Bathurst Island, Northern Australia
May 01, 2002; ABSTRACT-A middle Cenomanian faunule from the Moonkinu Formation of Bathurst Island in Northern Australia contains the best--...