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North American microtektites from the Caribbean Sea and their fission track age
Authors:B.P. Glass  R.N. Baker  D. Storzer  G.A. Wagner
Affiliation:Geology Department, University of Delaware, Newark, Delaware 19711, USA;Max-Planck-Institute für Kernphysik, Heidelberg, Germany
Abstract:Over 6000 microscopic glass spherules between 125 μm and 1 mm in diameter were found in a sediment core (RC9-58) from the Caribbean Sea. These glassy objects are mostly confined to a zone ~ 40 cm thick at a depth of ~ 250 cm. We believe that the microscopic glass objects are microtektites belonging to the North American strewnfield, based on their geographical location, appearance, physical properties, stratigraphic age (middle Upper Eocene), fission track age (~34.6 my) and major element compositions. The occurrence of North American microtektites in the Caribbean Sea indicates that the North American strewnfield is two to three times larger than previously indicated. An estimate on the abundance of microtektites in core RC9-58 indicates that the North American strewnfield may contain greater than 1017 g of tektite material.
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