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) |
|---|---|
| Pages (from-to) | 614-618 |
| Number of pages | 5 |
| Journal | Geology |
| Volume | 12 |
| Issue number | 10 |
| DOIs | |
| State | Published - 1984 |
UN SDGs
This output contributes to the following UN Sustainable Development Goals (SDGs)
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SDG 14 Life Below Water
All Science Journal Classification (ASJC) codes
- Geology
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