Planktonic foraminifera evidence for surface-water conditions off Southern Portugal during Mid-Pleistocene marine isotope stages 20 to 24 (790 – 940 ky)
Characterized by a drastic change in the deep thermohaline circulation, the Mid Pleistocene Transition (MPT) was a global climatic event resulted in more intense and longer lasting glacial periods and cooler sea -surface temperatures. The present study's objective is characterized surface -wate...
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| Other Authors: | , |
| Format: | conferenceObject |
| Language: | eng |
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2020
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| Subjects: | |
| Online Access: | http://hdl.handle.net/10400.1/14519 |
| Country: | Portugal |
| Oai: | oai:sapientia.ualg.pt:10400.1/14519 |