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:
Pacific
North Atlantic
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
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spelling ftoceanrep:oai:oceanrep.geomar.de:35912 2023-05-15T17:28:57+02:00 Deep-sea carbonates: Pleistocene dissolution cycles Berger, Wolfgang H. 1973 text 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 en eng Cushman Foundation for Foraminiferal Research https://oceanrep.geomar.de/id/eprint/35912/1/Berger.pdf Berger, W. H. (1973) Deep-sea carbonates: Pleistocene dissolution cycles. The Journal of Foraminiferal Research, 3 (4). pp. 187-195. DOI 10.2113/gsjfr.3.4.187 <https://doi.org/10.2113/gsjfr.3.4.187>. doi:10.2113/gsjfr.3.4.187 info:eu-repo/semantics/restrictedAccess Article PeerReviewed 1973 ftoceanrep https://doi.org/10.2113/gsjfr.3.4.187 2023-04-07T15:30:47Z 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. Article in Journal/Newspaper North Atlantic OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) Pacific The Journal of Foraminiferal Research 3 4 187 195
institution Open Polar
collection OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel)
op_collection_id ftoceanrep
language English
description 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.
format Article in Journal/Newspaper
author Berger, Wolfgang H.
spellingShingle Berger, Wolfgang H.
Deep-sea carbonates: Pleistocene dissolution cycles
author_facet Berger, Wolfgang H.
author_sort Berger, Wolfgang H.
title Deep-sea carbonates: Pleistocene dissolution cycles
title_short Deep-sea carbonates: Pleistocene dissolution cycles
title_full Deep-sea carbonates: Pleistocene dissolution cycles
title_fullStr Deep-sea carbonates: Pleistocene dissolution cycles
title_full_unstemmed Deep-sea carbonates: Pleistocene dissolution cycles
title_sort deep-sea carbonates: pleistocene dissolution cycles
publisher Cushman Foundation for Foraminiferal Research
publishDate 1973
url 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
geographic Pacific
geographic_facet Pacific
genre North Atlantic
genre_facet North Atlantic
op_relation https://oceanrep.geomar.de/id/eprint/35912/1/Berger.pdf
Berger, W. H. (1973) Deep-sea carbonates: Pleistocene dissolution cycles. The Journal of Foraminiferal Research, 3 (4). pp. 187-195. DOI 10.2113/gsjfr.3.4.187 <https://doi.org/10.2113/gsjfr.3.4.187>.
doi:10.2113/gsjfr.3.4.187
op_rights info:eu-repo/semantics/restrictedAccess
op_doi https://doi.org/10.2113/gsjfr.3.4.187
container_title The Journal of Foraminiferal Research
container_volume 3
container_issue 4
container_start_page 187
op_container_end_page 195
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