Orbitolina, a cretaceous larger foraminifer, from flemish cap: paleoceanographic implications.
The Tethyan larger foraminiferal genus Orbitolina has been found in the easternmost part of the western North Atlantic continental shelf at 46 degrees 30'N. All other known occurrences of the genus in North America are south of 33 degrees N. The species is Orbitolina conoidea Gras; its abundance in a grainsupported limestone indicates a tropical neritic environment and precludes the influence of Arctic waters in the Flemish Cap region in Early or Middle Cretaceous times.
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