Stratigraphic potential of Bolboforma significantly increased by new finds in the North Atlantic and South Pacific

Palaios
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Abstract

Until now, the genus Bolboforma, a problematic group of calcareous microfossils, has been recorded only in Oligocene to Pliocene marine sedimentary rocks, chiefly in the eastern North Atlantic region. We add to this eastern North Atlantic record six new sites and eleven undescribed species from the continental slopes of Ireland and Morocco. More significantly, we record, for the first time, abundant assemblages of Bolboforma on the western side of the North Atlantic and in the western South Pacific. Seven boreholes on the continental shelf and slope of New Jersey and Virginia contain ten species, three of which are new. Two species are present in two outcrops in eastern Mississippi and four are present in a borehole in the coastal plain of Virginia. On the Lord Howe Rise, west of New Zealand, a DSDP corehole has yielded a rich assemblage including four undescribed species. In addition to expanding the geographic distribution of Bolboforma, our work extends the known stratigraphic range downward into the upper Eocene on both sides of the North Atlantic and in the western South Pacific. Our findings firmly support the inference of a planktonic life style for Bolboforma, which implies a significant potential for biostratigraphic, paleobiogeographic, and paleoenvironmental studies, on both a local and global scale. We recommend a concerted effort to further document the nature and distribution of Bolboforma.

Publication type Article
Publication Subtype Journal Article
Title Stratigraphic potential of Bolboforma significantly increased by new finds in the North Atlantic and South Pacific
Series title Palaios
Volume 1
Issue 2
Year Published 1986
Language English
Publisher SEPM Society for Sedimentary Geology
Contributing office(s) Coastal and Marine Geology Program
Description 10 p.
First page 162
Last page 171
Country Ireland, Morocco
Online Only (Y/N) N
Additional Online Files (Y/N) N
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