Deep-sea carbonates: Pleistocene dissolution cycles

Foraminiferal evidence from the eastern equatorial Pacific and from the North Atlantic indicates that the dissolution of deep-sea carbonates was intensified during interglacials rather than during glacials, in contrast to widespread opinion. Pleistoccne dissolution cycles introduce a systematic bias...

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Bibliographic Details
Published in:The Journal of Foraminiferal Research
Main Author: Berger, Wolfgang H.
Format: Article in Journal/Newspaper
Language:English
Published: Cushman Foundation for Foraminiferal Research 1973
Subjects:
Online Access:https://oceanrep.geomar.de/id/eprint/35912/
https://oceanrep.geomar.de/id/eprint/35912/1/Berger.pdf
https://doi.org/10.2113/gsjfr.3.4.187
Description
Summary:Foraminiferal evidence from the eastern equatorial Pacific and from the North Atlantic indicates that the dissolution of deep-sea carbonates was intensified during interglacials rather than during glacials, in contrast to widespread opinion. Pleistoccne dissolution cycles introduce a systematic bias into the Interpretation of calcareous fossil assemblages near and below the lysocline zone.