Abstract
The estimated mid-Cretaceous primary production rates are as much as an order of magnitude lower than those measured in today's oceans. An evaluation of dissolved oxygen budgets using a simple oceanic circulation model indicates very low deep-water renewal rates in mid-Cretaceous oceans.-from Authors
Original language | English (US) |
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Pages (from-to) | 614-618 |
Number of pages | 5 |
Journal | Geology |
Volume | 12 |
Issue number | 10 |
DOIs | |
State | Published - 1984 |
All Science Journal Classification (ASJC) codes
- Geology