Sea level changes, carbonate dissolution and history of the Benguela Current in the Oligocene-Miocene off Southwest Africa (DSDP Site 362, Leg 40)-Reference-Cited by-同舟云学术

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Sea level changes, carbonate dissolution and history of the Benguela Current in the Oligocene-Miocene off Southwest Africa (DSDP Site 362, Leg 40)

Published:1988-03 Issue:3-4 Volume:79 Page:213-242
ISSN:0025-3227
Container-title:Marine Geology
language:en
Short-container-title:Marine Geology

Author:

Diester-Haass L.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology,Oceanography

Reference71 articles.

1. Sediment cores from the East Pacific;Arrhenius;Rep. Swedish Deep-Sea Expedition 1947–1948,1952

2. Planktonic foraminifera: selective solution and the lysocline;Berger;Mar. Geol.,1970

3. Foraminifera on the deep-sea floor: Lysocline and dissolution rate;Berger;Oceanol. Acta,1982

4. Sedimentology, petrology, and cyclic sedimentation patterns, Walvis Ridge Transect, Leg 74, Deep Sea Drilling Project;Borella,1984

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1. Late Quaternary responses to glacial-interglacial climate cycles of offshore Benguela region and associated foraminifera in the southeast Atlantic along Namibia and western South Africa;Deep Sea Research Part II: Topical Studies in Oceanography;2024-10

2. Oceanographic and climatic evolution of the southeastern subtropical Atlantic over the last 3.5 Ma;Earth and Planetary Science Letters;2018-06

3. Orbitally Forced Hyperstratification of the Oligocene South Atlantic Ocean;Paleoceanography and Paleoclimatology;2018-05

4. Steps in the intensification of Benguela upwelling over the Walvis Ridge during Miocene and Pliocene;International Journal of Earth Sciences;2016-03-12

5. Geology of the Cenozoic Namakwa Sands Heavy Mineral Deposit, West Coast of South Africa: A World-Class Resource of Titanium and Zircon;Economic Geology;2015-07-13

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