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...
Published in: | The Journal of Foraminiferal Research |
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Language: | English |
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Cushman Foundation for Foraminiferal Research
1973
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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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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 |
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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 |
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3 |
container_issue |
4 |
container_start_page |
187 |
op_container_end_page |
195 |
_version_ |
1766122231953358848 |