Does ice drive early Maastrichtian eustasy?
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Abstract
A large (30–40 m), rapid (≪1 m.y.), earliest Maastrichtian sea-level drop inferred from New Jersey sequence stratigraphic records correlates with synchronous δ18O increases in deep-water benthic and low-latitude surface-dwelling planktonic foraminifera. The coincidence of these events argues for the development of a moderate-sized ice sheet during the early Maastrichtian.
Publication type | Article |
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Publication Subtype | Journal Article |
Title | Does ice drive early Maastrichtian eustasy? |
Series title | Geology |
DOI | 10.1130/0091-7613(1999)027<0783:DIDEME>2.3.CO;2 |
Volume | 27 |
Issue | 9 |
Year Published | 1999 |
Language | English |
Publisher | Geological Society of America |
Description | 4 p. |
First page | 783 |
Last page | 786 |
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