Abstract
A large (30-40 m), rapid (≪1 m.y.), earliest Maastrichtian sealevel drop inferred from New Jersey sequence stratigraphic records correlates with synchronous δ18O increases in deep-water benthic and low-latitude surface-dwellin planktonic foraminifera. The coincidence of these events argues for the development of a moderate-sized ice sheet during the early Maastrichtian.
| Original language | English (US) |
|---|---|
| Pages (from-to) | 783-786 |
| Number of pages | 4 |
| Journal | Geology |
| Volume | 27 |
| Issue number | 9 |
| DOIs | |
| State | Published - Sep 1999 |
All Science Journal Classification (ASJC) codes
- Geology
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